The Royal Agricultural Station Inthanon is His Majesty the King Personal Project for eliminating opium growing. Established in 1979, the Station servers as a research centre for a wide variety of the highland fisheries, in order to develop the livelihood of the hill tribe farmers. It also serves as a centre to disseminate knowledge and new innovation derived from the research of the sustainable highland farming to other regions.

 

Royal Agricultural Station Inthanon located on National Park DoiInthanon in AmpherJomthong, Chaiangmai Province. And average point above sea level is 1,200 meters. The agricultural research area in the station over 513 rai and there are 8 villages that the Station take responsible and these villages are hill tribe of Hmong and Karen.

www.royal-inthanon.com/English

Uploaded by : Beto marquez

 

Just an average working truck 2015 pete 389 525 hp 13 speed

Schweiz / Zürich - Rheinfall

 

The Rhine Falls (German: Rheinfall, pronounced [ˈʁaɪ̯nˌfal] (listen), singular) is a waterfall located in Switzerland and the most powerful waterfall in Europe. The falls are located on the High Rhine on the border between the cantons of Schaffhausen (SH) and Zürich (ZH), between the municipalities of Neuhausen am Rheinfall (SH) and Laufen-Uhwiesen/Dachsen (ZH), next to the town of Schaffhausen in northern Switzerland.

 

They are 150 metres (490 ft) wide and 23 metres (75 ft) high. In the winter months, the average water flow is 250 m3/s (8,800 cu ft/s), while in the summer, the average water flow is 600 m3/s (21,000 cu ft/s). The highest flow ever measured was 1,250 cubic metres per second (44,000 cu ft/s) in 1965; and the lowest, 95 cubic metres per second (3,400 cu ft/s) in 1921. The falls cannot be climbed by fish, except by eels that are able to worm their way up over the rocks.

 

Geology

 

The Rhine Falls were formed in the last ice age, approximately 14,000 to 17,000 years ago, by erosion-resistant rocks narrowing the riverbed. The first glacial advances created today's landforms approximately 500,000 years ago. Up to the end of the Wolstonian Stage approximately 132,000 years ago, the Rhine flowed westwards from Schaffhausen past Klettgau. This earlier riverbed later filled up with gravel.

 

About 132,000 years ago the course of the river changed southwards at Schaffhausen and formed a new channel, which also filled up with gravel. Part of the Rhine today includes this ancient riverbed.

 

During the Würm glaciation, the Rhine was pushed far to the south to its present course, over a hard Late Jurassic limestone bed. As the river flowed over both the hard limestone and the easily eroded gravel from previous glaciations, the current waterfall formed about 14,000 to 17,000 years ago. The Rheinfallfelsen, a large rock, is the remnant of the original limestone cliff flanking the former channel. The rock has eroded very little over the years because relatively little sediment comes down the Rhine from Lake Constance.

 

Economics

 

The north side of the falls is a millsite. In the 17th century, a blast furnace for smelting iron ore found in the limestone was built. It was in operation until the first half of the 19th century.

 

In 1887 the ironworks applied for permission to divert between one fifth to one half of the river's flow for electricity generation. The Swiss Alpine Club, the Schweizerische Naturforschende Gesellschaft (a nature group) and several scientific societies opposed the plan.

 

In 1913 an international competition was held for the best plan for a shipping route between Basel and Lake Constance.

 

In 1919, a company wanting to build power stations in northern Switzerland were told that any such station at the Rhine Falls "must serve the economic interest of the public".

 

In 1944, the Swiss Council of States granted permission to build the proposed power station. The permission was to become effective on 1 February 1948, with construction to begin in 1952. But in 1951, the Neuen Helvetischen Gesellschaft (New Swiss Society), under the leadership of Emil Egli, got 150,000 Swiss citizens to sign a petition protesting the project; among the signatories were 49 famous citizens, including Hermann Hesse and Carl Jacob Burckhardt. The petition not only scuttled the power station project, but effectively prevented all future hydropower and navigation engineering projects on the upper Rhine to the present day.

 

Today, the falls are still under consideration for hydropower projects. If the full water flow were used, the power generated would average approximately 50 MW. The economic value of the falls as a tourist attraction may be greater.

 

Tourism

 

The nearest community is Neuhausen am Rheinfall, where tourists can also view the Wörth Castle. Boat trips can be taken up the Rhine to the falls and the Rheinfallfelsen. There are also viewing platforms with views of the falls built on both sides of the Rhine. These are reached via steep and narrow stairs (access by fee on the Schloss Laufen side). Guided tours of various lengths start from Schloss Laufen on the Zürich side of the falls – a youth hostel is also located in Schloss Laufen. Various restaurants are located in Schloss Laufen, Schloss Wörth and the Rheinfall park.

 

The Rhine Falls are easily accessible by car, bicycle and public transport (SBB railway station "Neuhausen am Rheinfall" on the northern side of the falls and SBB railway station "Schloss Laufen am Rheinfall" on the southern banks of the river). Large pay-parking lots are located on both sides of the falls.

 

Tourists have been awed by the Rhine Falls for centuries. In the 19th century, the painter J. M. W. Turner made several studies and larger paintings of the falls, and the lyrical poet Eduard Mörike wrote of the falls:

 

Halte dein Herz, o Wanderer, fest in gewaltigen Händen!

Mir entstürzte vor Lust zitternd das meinige fast.

Rastlos donnernde Massen auf donnernde Massen geworfen,

Ohr und Auge, wohin retten sie sich im Tumult?

 

(Hold your heart, oh traveller, tightly in mighty hands!

Mine nearly collapsed, shivering with pleasure.

Restlessly thundering masses thrown upon thundering masses,

Ear and eye, whither can they save themselves in such an uproar?)

 

In 1840, author Mary Shelley visited the Falls while on a tour of Europe with her son. She described her visit in a travel narrative that she published in 1844, Rambles in Germany and Italy. She says: "A portion of the cataract arches over the lowest platform, and the spray fell thickly on us, as standing on it and looking up, we saw wave, and rock, and cloud, and the clear heavens through its glittering ever-moving veil. This was a new sight, exceeding anything I had ever before seen; however, not to be wet through, I was obliged quickly to tear myself away.".

 

(Wikipedia)

 

Der Rheinfall (alemannisch resp. schweizerdeutsch Rhyfall [ˈɾiːfal], französisch Chutes du Rhin, italienisch Cascate del Reno, rätoromanisch Cascada dal Rain), früher auch Grosser Laufen genannt (im Gegensatz zum Kleinen Laufen), gehört mit dem gleich hohen Sarpsfossen in Norwegen zu den drei grössten Wasserfällen in Europa. Dabei ist der Sarpsfossen mit durchschnittlich 577 m³/s wasserreicher, während der doppelt so hohe Dettifoss auf Island nur etwa halb so viel Wasser führt. Der Rheinfall befindet sich in der Schweiz auf dem Gebiet der Gemeinden Neuhausen am Rheinfall im Kanton Schaffhausen (rechtsufrig) und Laufen-Uhwiesen im Kanton Zürich (linksufrig), rund vier Kilometer westlich unterhalb der Stadt Schaffhausen.

 

Beschreibung

 

Auf dem Weg vom Bodensee nach Basel stellen sich dem Hochrhein mehrfach widerstandsfähige Gesteine in den Weg, die das Flussbett verengen und die der Fluss in Stromschnellen und einem Wasserfall, dem Rheinfall, überwindet.

 

Der Rheinfall hat eine Höhe von 23 Metern und eine Breite von 150 Metern. Der Kolk in der Prallzone hat eine Tiefe von 13 Metern. Bei mittlerer Wasserführung des Rheins stürzen im Rheinfall 373 Kubikmeter Wasser pro Sekunde über die Felsen (mittlerer Sommerabfluss: etwa 600 m³/s). Die höchste Abflussmenge wurde im Jahr 1965 mit 1250 Kubikmetern, die geringste Abflussmenge im Jahr 1921 mit 95 Kubikmetern pro Sekunde gemessen. Auch in den Jahren 1880, 1913 und 1953 war der Abfluss ähnlich gering.

 

Der Rheinfall ist von Fischen aufwärts nicht zu überwinden, ausser vom Aal. Dieser schlängelt sich seitwärts (ausserhalb des Flussbettes auf dem Land) über die Felsen hinauf.

 

Entstehung

 

Der Felsuntergrund, der viel älter ist als der Rheinfall selbst, wie auch die bedeutend jüngeren geologischen Vorgänge während des gegenwärtigen Eiszeitalters führten zur Entstehung des Rheinfalls. Durch die allgemeinen Temperatursenkungen setzten vor rund 500 000 Jahren die ersten Gletschervorstösse ins Mittelland ein und gestalteten die heutige Landschaft. Bis zum Ende der Riß-Kaltzeit vor ca. 200 000 Jahren floss der Rhein von Schaffhausen westlich durch den Klettgau. Dieses frühere Flussbett wurde wieder mit Alpenschotter (Molasse) aufgefüllt.

 

Vor etwa 120 000 Jahren wurde der Fluss bei Schaffhausen nach Süden abgelenkt und bildete die risszeitliche Rheinrinne. Der Rheinlauf unterhalb des Fallbeckens heute entspricht dieser Rinne, die wieder mit Schotter aufgefüllt wurde.

 

Während der letzten Eiszeit, der sogenannten Würmeiszeit, wurde der Rhein dann in weitem Bogen gegen Süden abgedrängt und erreichte oberhalb des Falles sein heutiges Bett auf hartem Malmkalk (Weissjura, Oberer Jura). Beim Übergang von den harten Malmkalken zur leicht abtragbaren risszeitlichen Schotterrinne entstand so vor rund 14 000 bis 17 000 Jahren der Rheinfall in seiner heutigen Form. Die Rheinfallfelsen (Grosser, besteigbarer Felsen und der Sage nach Seelentanzstein) bilden die Überreste der ursprünglich steil abfallenden Kalksteinflanke der einstigen Abflussrinne. Die sehr geringe bisherige erosive Überformung der Fallstrecke erklärt sich durch die geringe Schleppfracht (Flussgeschiebe) des Rheins unterhalb des Bodensees.

 

Tourismus

 

Auf ausgebauten Wegen erreicht man auf beiden Rheinseiten Aussichtsplattformen. Diese ragen teilweise weit über den Rhein hinaus. Am Rheinfallbecken in Neuhausen am Rheinfall liegt das Schlösschen Wörth. Von hier aus kann man mit Ausflugsbooten dicht an den Rheinfall heranfahren und sich auch am mittleren Felsen absetzen lassen. Die Besteigung der Aussichtsplattform mit naher Sicht auf den Fall erfolgt über schmale und steile Treppen. Ausserdem werden kleine und grosse Rheinfallrundfahrten sowie die Übersetzung zum Schloss Laufen angeboten, das in Laufen auf der Zürcher Seite über dem Rheinfall thront und u. a. von einer Jugendherberge genutzt wird. Auf der südlichen Seite beim Schloss Laufen sind die Wege im Jahr 2008 saniert worden und es wurde ein Glaslift installiert. Teile der Wege – der sogenannte Erlebnispfad, darunter die Aussichtsplattformen und der Lift – sind nun kostenpflichtig. Der Rheinfall wird regelmässig abends, jedoch nicht ganzjährig, durch eine Lichtanlage illuminiert. Im Jahr 2013 wurde er von 1 300 000 Besuchern besichtigt.

 

Am Rheinfall gibt es mehrere Restaurants und Verpflegungsstände aller Preisklassen. Einen besonderen Blick auf den Rheinfall bietet der Seilpark Adventure Park Rheinfall oberhalb des Schlössli Wörth. Den Rheinfall sowie weitere Schweizer Sehenswürdigkeiten und Landschaften im Massstab 1:87 (Spur H0) zeigt Smilestones, die grösste Miniaturwelt der Schweiz in einer ehemaligen Fabrikhalle der SIG beim Bahnhof Neuhausen Rheinfall.

 

Am und um den Rheinfall führen mehrere Wege:

 

Kleine Rundweg, 3,4 km, 1:00 h

Rheinfall Rundweg, 7,2 km, 1:53 h

 

Erreichbarkeit

 

Der Rheinfall ist per Auto, Velo (Fahrrad) und öffentlichen Verkehrsmitteln gut erreichbar. In Neuhausen und beim Schloss Laufen befinden sich grosse Parkplätze. Ab der Autostrasse A4 ist die Zufahrt zum Rheinfall ausgeschildert. Ab dem Schaffhauser Bahnhof gelangt man mit dem Trolleybus der Linie 1 Richtung Herbstäcker bis zur Haltestelle Neuhausen Zentrum (ebenfalls erreichbar mit der Autobus-Linie 6 Richtung Neuhausen SBB). Von dort aus folgt man zu Fuss den gelben Markierungen. Besuchern, die mit der Hochrheinbahn anreisen, empfiehlt sich der DB-Bahnhof Neuhausen Bad Bf. Dieser ist nur wenige Gehminuten vom Rheinfall entfernt (etwa 15 Minuten Fussweg). Seit 2016 befindet sich nördlich oberhalb des Rheinfalls die Haltestelle Neuhausen Rheinfall. Sie wird bedient von der SBB S-Bahn S-9 Schaffhausen–Neuhausen Rheinfall–Zürich–Uster, und S-22 Singen–Schaffhausen–Neuhausen Rheinfall–Jestetten. Zwei Personen-Aufzüge an der Haltestelle fahren direkt zum Rheinfall. Beim Schloss Laufen auf der anderen Seite des Rheins befindet sich zudem die SBB-Station Schloss Laufen am Rheinfall der Rheinfallbahn Schaffhausen–Winterthur.

 

Zwischen dem Rheinfall und der Schifflände in Schaffhausen verkehrt im Sommerhalbjahr die Bimmelbahn Rhyfall-Express und verbindet den Rheinfall mit den Schiffen der Schweizerischen Schifffahrtsgesellschaft Untersee und Rhein.

 

Wirtschaftliche Nutzung

 

Seit alters her wurden besonders auf der Nordseite Mühlen am Rheinfall betrieben, die kleine Teile der Wasserkraft nutzten. Im 17. Jahrhundert wurde auf der rechten Seite des Falles ein Hochofen zur Verhüttung von Bohnerzen gebaut und etwa ein Jahrhundert lang und dann noch einmal in der ersten Hälfte des 19. Jahrhunderts betrieben. Anfang des 19. Jahrhunderts bekam Johann Georg Neher Rechte zur Nutzung der Wasserkräfte am Rheinfall, die lange in dessen Familie verblieben. Das Kraftwerk versorgte die Schweizerische Waggons-Fabrik und ab 1889 das erste europäische Aluminiumwerk der Aluminium-Industrie-Aktien-Gesellschaft mit Energie. 1947 folgte eine Umfirmierung in Rheinkraftwerk Neuhausen AG.

 

Die Nutzwassermenge des Kraftwerks beträgt 25 m³/s, was sich auf die verbleibende Wassermenge des Rheinfalls wenig auswirkt. Bei 23 Meter Gefälle verfügt das Kraftwerk Neuhausen mit einer Turbine über 4,4 MW installierte Leistung. Im Vergleich dazu leistet das wenige Kilometer stromaufwärts gelegene Kraftwerk Schaffhausen mit zwei Turbinen 25,5 MW bei einem Durchfluss von 425 m³/s. Die Betriebsführung erfolgt durch das Kraftwerk Reckingen, die Geschäftsleitung liegt bei der EnAlpin AG, einer Tochtergesellschaft der Energiedienst Holding.

 

Frühere und neue Planungen zur Nutzung

 

Ein Konzessionsantrag der Firma J. G. Nehers Söhne & Cie. (Eisenwerk Laufen) im Jahr 1887, den Durchfluss im Kraftwerk auf 75 m³/s zu erhöhen, wurde von den Kantonen Zürich und Schaffhausen nicht genehmigt. Dagegen hatten sich im Besonderen Hermann Freuler, die Schweizerische Naturforschende Gesellschaft, der Schweizer Alpen-Club sowie wissenschaftliche Vereinigungen in der Schweiz gewehrt.

 

1913 wurde ein internationaler Wettbewerb zur Planung eines Schifffahrtswegs von Basel bis zum Bodensee ausgeschrieben. Gemäss dem Projektentwurf aus dem Anfang der 1960er Jahre sollte der Rheinfall als Naturdenkmal mittels eines 552 Meter langen Schifffahrtstunnels und einer Schleuse hinter dem Schloss Laufen umgangen werden. 1919 wurde vom Baudirektor der Nordschweizerischen Kraftwerke erklärt, dass der Bau eines Rheinfall-Kraftwerks «den wirtschaftlichen Interessen der Allgemeinheit dienstbar gemacht werden müsse».

 

Da das Landschaftsbild am Rheinfall unberührt bleiben sollte, entstand am Rheinfall selbst kein grosses Wasserkraftwerk. 1944 bewilligte aber der Schweizerische Bundesrat die Konzession zum Bau des Kraftwerks Rheinau, das unterhalb des Rheinfalls liegt und den Rhein bis zum Rheinfallbecken aufstaut. Der Baubeginn folgte 1952. 1951 wurde eine Volksinitiative gegen die Schiffbarmachung des Hochrheins von über 150 000 Schweizer Bürgern eingereicht, 1952 eine weitere Volksinitiative gegen den weiteren Bau eines Kraftwerkes der Neuen Helvetischen Gesellschaft unter Federführung von Emil Egli, die von 49 angesehenen Schweizer Bürgern, darunter Hermann Hesse und Carl Jacob Burckhardt, unterzeichnet wurde. Über die Eingabe von 1952 fand 1954 eine Abstimmung statt, die mit 69 % der Stimmen abgelehnt wurde. Die Planungen für die Schiffbarmachung des Hochrheins wurden später eingestellt.

 

Am 10. April 2013 berichtete das Nachrichtenmagazin 10 vor 10 des Schweizer Fernsehens über ein neues Kraftwerksprojekt der Schaffhauser Kraftwerke am Rheinfall, welches den Fluss oberhalb des Rheinfalls anzapfen und so die Wassermenge in der Nacht erheblich reduzieren würde. Die Eidgenössische Natur- und Heimatschutzkommission und der Kanton Schaffhausen signalisierten ihre Zustimmung, der Rheinaubund seine strikte Ablehnung. Eine Änderung des kantonalen Wasserwirtschaftsgesetzes, das ein weiteres Kraftwerk oberhalb des Rheinfalls ermöglicht hätte, wurde am 18. Mai 2014 vom Volk abgelehnt.

 

Befahrung

 

Die Befahrung des Rheinfalls galt lange Zeit als unmöglich. Dennoch wurde der Rheinfall mehrmals mit Kajaks befahren. 1999 wurde die Bootsfahrt zwischen Flurlinger Brücke und Rheinfall offiziell verboten. Es erfolgen jedoch weiterhin vereinzelt Befahrungen mit Kajaks, mindestens einmal mit Handpaddel (April 2007), oder selten auch im Kanadier (Januar 1997). Die Bilder und Videos werden zum Teil im Internet veröffentlicht. Wenn die Paddler von der Polizei gefasst werden, drohen ihnen bis zu 5'000 Franken Strafe.

 

Eine irrtümliche Befahrung mit einem Boot, die beinahe in einer Katastrophe endet, kommt in der Filmkomödie Drei Mann in einem Boot aus dem Jahr 1961 vor.

 

Der Mittelfelsen des Rheinfalls, auf dem die Schweizer Flagge gehisst ist, kann durch einen Bootsverkehr mit kleinen Booten erreicht werden.

 

Rheinfallschaum

 

Seit den 1970er Jahren wird unterhalb des Rheinfalls im Sommer eine starke Schaumbildung beobachtet, die Schaumfahnen sind auch kilometerweit unterhalb noch zu sehen. Untersuchungen der kantonalen Ämter haben gezeigt, dass es sich dabei nicht um befürchtete Wasserverschmutzung durch Waschmittelrückstände oder andere Abwässer handelt. Christian Wegner von der Friedrich-Schiller-Universität in Jena hat in seiner Doktorarbeit nachgewiesen, dass die Ursache des Schaums beim Flutenden Wasserhahnenfuss (Ranunculus fluitans) zu suchen ist.

 

Darstellungen in der Kunst

 

Erstmals wurde der Rheinfall von Joachim Patinir im Gemälde Taufe Christi (1515–1520) bildlich wiedergegeben. Von Sebastian Münster existiert in der Cosmographia (1544) ein Holzschnitt des Rheinfalls. Die bedeutendste Darstellung dürfte jene von William Turner sein, das Gemälde ist ausgestellt im Museum of Fine Arts in Boston.

 

Beschreibungen in der Literatur

 

Zahlreiche – auch berühmte – Schriftsteller besuchten den Rheinfall und beschrieben ihn, so Goethe, Wilhelm Heinse, Mörike und weitere.

 

Eduard Mörike schrieb über den Wasserfall: «Halte dein Herz, o Wanderer, fest in gewaltigen Händen! Mir entstürzte vor Lust zitternd das meinige fast. Rastlos donnernde Massen auf donnernde Massen geworfen, Ohr und Auge, wohin retten sie sich im Tumult?»

 

(Wikipedia)

Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah. More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations. The park contains the highest density of natural arches in the world.

 

The park consists of 310.31 square kilometres (76,680 acres; 119.81 sq mi; 31,031 ha) of high desert located on the Colorado Plateau. The highest elevation in the park is 5,653 feet (1,723 m) at Elephant Butte, and the lowest elevation is 4,085 feet (1,245 m) at the visitor center. The park receives an average of less than 10 inches (250 mm) of rain annually.

 

Administered by the National Park Service, the area was originally named a national monument on April 12, 1929, and was re designated as a national park on November 12, 1971. The park received more than 1.6 million visitors in 2018.

 

As stated in the foundation document in U.S. National Park Service website:

 

The purpose of Arches National Park is to protect extraordinary examples of geologic features including arches, natural bridges, windows, spires, and balanced rocks, as well as other features of geologic, historic, and scientific interest, and to provide opportunities to experience these resources and their associated values in their majestic natural settings.

 

The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago (Mya) when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 200 Mya), desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Mya), was deposited on top of the Navajo. Over 5,000 feet (1,500 m) of younger sediments were deposited and have been mostly eroded. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.

 

The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual "salt anticlines" or linear regions of uplift. Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center.

 

As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer-cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches.

 

Although the park's terrain may appear rugged and durable, it is extremely fragile. More than 1 million visitors each year threaten the fragile high-desert ecosystem. The problem lies within the soil's crust, which is composed of cyanobacteria, algae, fungi, and lichens that grow in the dusty parts of the park. Factors that make Arches National Park sensitive to visitor damage include being a semiarid region, the scarce, unpredictable rainfall, lack of deep freezing, and lack of plant litter, which results in soils that have both a low resistance to and slow recovery from, compressional forces such as foot traffic. Methods of indicating effects on the soil are cytophobic soil crust index, measuring of water infiltration, and t-tests that are used to compare the values from the undisturbed and disturbed areas.

 

Geological processes that occurred over 300 million years ago caused a salt bed to be deposited, which today lies beneath the landscape of Arches National Park.[ Over time, the salt bed was covered with sediments that eventually compressed into rock layers that have since been named Entrada Standstone. Rock layers surrounding the edge of the salt bed continued to erode and shift into vertical sandstone walls called fins. Sand collected between vertical walls of the fins, then slightly acidic rain combined with carbon dioxide in the air allowed for the chemical formation of carbonic acid within the trapped sand. Over time, the carbonic acid dissolved the calcium carbonate that held the sandstone together. Many of the rock formations have weaker layers of rock on bottom that are holding stronger layers on top. The weaker layers would dissolve first, creating openings in the rock. Gravity caused pieces of the stronger rock layer to fall piece by piece into an arch shape. Arches form within rock fins at points of intense fracturing localization, or weak points in the rock's formation, caused by horizontal and vertical discontinuities. Lastly, water, wind, and time continued this erosion process and ultimately created the arches of Arches National Park. All of the arches in the park are made of Entrada Sandstone, however, there are slight differences in how each arch was developed. This allows the Entrada Sandstone to be categories into 3 groups including Slick rock members, Dewey rock members, and Moab members. Vertical arches can be developed from Slick rock members, a combination of Slick rock members and Moab members, or Slick rock members resting above Dewey rock members. Horizontal arches (also called potholes) are formed when a vertical pothole formation meets a horizontal cave, causing a union into a long arch structure. The erosion process within Arches National Park will continue as time continues to pass. Continued erosion combined with vertical and horizontal stress will eventually cause arches to collapse, but still, new arches will continue to form for thousands of years.

 

Humans have occupied the region since the last ice age 10,000 years ago. Fremont people and Ancestral Puebloans lived in the area until about 700 years ago. Spanish missionaries encountered Ute and Paiute tribes in the area when they first came through in 1775, but the first European-Americans to attempt settlement in the area were the Mormon Elk Mountain Mission in 1855, who soon abandoned the area. Ranchers, farmers, and prospectors later settled Moab in the neighboring Riverine Valley in the late 1870s. Word of the beauty of the surrounding rock formations spread beyond the settlement as a possible tourist destination.

 

The Arches area was first brought to the attention of the National Park Service by Frank A. Wadleigh, passenger traffic manager of the Denver and Rio Grande Western Railroad. Wadleigh, accompanied by railroad photographer George L. Beam, visited the area in September 1923 at the invitation of Alexander Ringhoffer, a Hungarian-born prospector living in Salt Valley. Ringhoffer had written to the railroad to interest them in the tourist potential of a scenic area he had discovered the previous year with his two sons and a son-in-law, which he called the Devils Garden (known today as the Klondike Bluffs). Wadleigh was impressed by what Ringhoffer showed him, and suggested to Park Service director Stephen T. Mather that the area be made a national monument.

 

The following year, additional support for the monument idea came from Laurence Gould, a University of Michigan graduate student (and future polar explorer) studying the geology of the nearby La Sal Mountains, who was shown the scenic area by local physician Dr. J. W. "Doc" Williams.

 

A succession of government investigators examined the area, in part due to confusion as to the precise location. In the process, the name Devils Garden was transposed to an area on the opposite side of Salt Valley that includes Landscape Arch, the longest arch in the park. Ringhoffer's original discovery was omitted, while another area nearby, known locally as the Windows, was included. Designation of the area as a national monument was supported by the Park Service in 1926 but was resisted by President Calvin Coolidge's Interior Secretary, Hubert Work. Finally, in April 1929, shortly after his inauguration, President Herbert Hoover signed a presidential proclamation creating the Arches National Monument, consisting of two comparatively small, disconnected sections. The purpose of the reservation under the 1906 Antiquities Act was to protect the arches, spires, balanced rocks, and other sandstone formations for their scientific and educational value. The name Arches was suggested by Frank Pinkely, superintendent of the Park Service's southwestern national monuments, following a visit to the Windows section in 1925.

 

In late 1938, President Franklin D. Roosevelt signed a proclamation that enlarged the Arches to protect additional scenic features and permit the development of facilities to promote tourism. A small adjustment was made by President Dwight Eisenhower in 1960 to accommodate a new road alignment.

 

In early 1969, just before leaving office, President Lyndon B. Johnson signed a proclamation substantially enlarging the Arches. Two years later, President Richard Nixon signed legislation enacted by Congress, which significantly reduced the total area enclosed, but changed its status. Arches National Park was formally dedicated in May 1972.

 

In 1980, vandals attempted to use an abrasive kitchen cleanser to deface ancient petroglyphs in the park, prompting park officials to recruit physicist John F. Asmus, who specialized in using lasers to restore works of art, to use his technology to repair the damage. Asmus "zapped the panel with intense light pulses and succeeded in removing most of the cleanser".

 

Climbing Balanced Rock or any named or unnamed arch in Arches National Park with an opening larger than 3 ft (0.9 m) is banned by park regulations. Climbing on other features in the park is allowed but regulated; in addition, slacklining and BASE jumping are banned parkwide.

 

Climbing on named arches within the park had long been banned by park regulations, but following Dean Potter's successful free climb on Delicate Arch in May 2006, the wording of the regulations was deemed unenforceable by the park attorney. In response, the park revised its regulations later that month, eventually imposing the current ban on arch climbing in 2014.

 

Approved recreational activities include auto touring, hiking, bicycling, camping at the Devils Garden campground, backpacking, canyoneering, and rock climbing, with permits required for the last three activities. Guided commercial tours and ranger programs are also available.

 

Astronomy is also popular in the park due to its dark skies, despite the increasing light pollution from towns such as Moab.

 

Delicate Arch is the subject of the third 2014 quarter of the U.S. Mint's America the Beautiful Quarters program commemorating national parks and historic sites. The Arches quarter had the highest production of the five 2014 national park quarters, with more than 465 million minted.

 

American writer Edward Abbey was a park ranger at Arches National Monument in 1956 and 1957, where he kept journals that became his book Desert Solitaire. The success of Abbey's book, as well as interest in adventure travel, has drawn many hikers, mountain bikers, and off-pavement driving enthusiasts to the area. Permitted activities within the park include camping, hiking along designated trails, backpacking, canyoneering, rock climbing, bicycling, and driving along existing roads, both paved and unpaved. The Hayduke Trail, an 812 mi (1,307 km) backpacking route named after one of Edward Abbey's characters, begins in the park.

 

An abundance of wildlife occurs in Arches National Park, including spadefoot toads, antelope squirrels, scrub jays, peregrine falcons, many kinds of sparrows, red foxes, desert bighorn sheep, kangaroo rats, mule deers, cougars, midget faded rattlesnakes, yucca moths, western rattlesnakes, and collared lizards.

 

A number of plant species are common in the park, including prickly pear cactus, Indian ricegrass, bunch grasses, cheatgrass, moss, liverworts, Utah juniper, Mormon tea, blackbrush, cliffrose, four-winged saltbrush, pinyon pine, evening primrose, sand verbena, yucca, and sacred datura.

 

Biological soil crust consisting of cyanobacteria, lichen, mosses, green algae, and microfungi is found throughout southeastern Utah. The fibrous growths help keep soil particles together, creating a layer that is more resistant to erosion. The living soil layer readily absorbs and stores water, allowing more complex forms of plant life to grow in places with low precipitation levels.

 

Among the notable features of the park are the following:

Balanced Rock – a large balancing rock, the size of three school buses

Courthouse Towers – a collection of tall stone columns

Dark Angel – a free-standing 150 ft-tall (46 m) sandstone pillar at the end of the Devils Garden Trail

Delicate Arch – a lone-standing arch that has become a symbol of Utah and the most recognized arch in the park

Devils Garden – many arches and columns scattered along a ridge

Double Arch – two arches that share a common end

Fiery Furnace – an area of maze-like narrow passages and tall rock columns (see biblical reference, Book of Daniel, chapter 3)

Landscape Arch – a very thin and long arch in the Devils Garden with a span of 290 ft (88 m) (the longest arch in the park)

Petrified Dunes – petrified remnants of dunes blown from the ancient lakes that covered the area

The Phallus – a rock spire that resembles a phallus

Wall Arch – located along the popular Devils Garden Trail; collapsed sometime on August 4/5, 2008

The Three Gossips –a mid-sized sandstone tower located in the Courthouse Towers area.

 

Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.

 

Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.

 

People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.

 

Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.

 

The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.

 

Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.

 

The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:

 

use of the bow and arrow while hunting,

building pithouse shelters,

growing maize and probably beans and squash,

building above ground granaries of adobe or stone,

creating and decorating low-fired pottery ware,

producing art, including jewelry and rock art such as petroglyphs and pictographs.

 

The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.

 

These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.

 

In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.

 

In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.

 

Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.

 

At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.

 

The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.

 

A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.

 

Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.

 

Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.

 

Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.

 

Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.

 

Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.

 

The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.

 

Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.

 

Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.

 

In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.

 

The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.

 

Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.

 

After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.

 

As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.

 

Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.

 

Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.

 

Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.

 

Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.

 

On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.

 

Main article: Latter Day Saint polygamy in the late-19th century

During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.

 

The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.

 

Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:

 

William Torrington in Carson City (then a part of Utah territory), 1859

Thomas Coleman (Black man) in Salt Lake City, 1866

3 unidentified men at Wahsatch, winter of 1868

A Black man in Uintah, 1869

Charles A. Benson in Logan, 1873

Ah Sing (Chinese man) in Corinne, 1874

Thomas Forrest in St. George, 1880

William Harvey (Black man) in Salt Lake City, 1883

John Murphy in Park City, 1883

George Segal (Japanese man) in Ogden, 1884

Joseph Fisher in Eureka, 1886

Robert Marshall (Black man) in Castle Gate, 1925

Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).

 

Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.

 

Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.

 

During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.

 

In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.

 

Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.

 

Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.

 

As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.

 

One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.

 

It is estimated that 1,450 soldiers from Utah were killed in the war.

The kiang (Equus kiang) is the largest of the wild asses. This equine is native to the Tibetan Plateau, where it inhabits montane and alpine grasslands from 4000 to 7000 meters elevation. Its current range is restricted to Ladakh in Jammu and Kashmir, plains of the Tibetan plateau and northern Nepal along the Tibetan border.

 

Other common names for this species include Tibetan wild ass, khyang, and gorkhar.

 

The Kiang is the largest of the wild asses, with an average shoulder height of 13.3 hands (55 inches, 140 cm). It has a large head, with a blunt muzzle and a convex nose. The mane is upright and relatively short. The coat is a rich chestnut colour, darker brown in winter and a sleek reddish brown in late summer, molting its woolly fur. The summer coat is 1.5 centimeters long and the winter coat is double the length. The legs, undersides and ventral part of the nape, end of the muzzle, and the inside of the pinnae are all white. A broad, dark chocolate-coloured dorsal stripe extends from the mane to the end of the tail, which ends in a tuft of blackish brown hairs. Kiang have very slight sexual dimorphism.

 

The only real predator other than humans is the wolf. Kiangs defend themselves by forming a circle and, with heads down kick out violently. As a result wolves usually attack single animals who have strayed from the group.

en.wikipedia.org/wiki/Kiang

en.wikipedia.org/wiki/Red_Sea

   

The Red Sea (alternatively Arabian Gulf[1] or Gulf of Arabia[2][3]) is a seawater inlet of the Indian Ocean, lying between Africa and Asia. The connection to the ocean is in the south through the Bab el Mandeb strait and the Gulf of Aden. In the north, there is the Sinai Peninsula, the Gulf of Aqaba, and the Gulf of Suez (leading to the Suez Canal). The Red Sea is a Global 200 ecoregion. The sea is underlain by the Red Sea Rift which is part of the Great Rift Valley.

The Red Sea has a surface area of roughly 438,000 km² (169,100 mi²).[4][5] It is about 2250 km (1398 mi) long and, at its widest point, 355 km (220.6 mi) wide. It has a maximum depth of 2211 m (7254 ft) in the central median trench, and an average depth of 490 m (1,608 ft). However, there are also extensive shallow shelves, noted for their marine life and corals. The sea is the habitat of over 1,000 invertebrate species, and 200 soft and hard corals. It is the world's northernmost tropical sea.

  

Extent

The International Hydrographic Organization defines the limits of the Red Sea as follows:[6]

On the North. The Southern limits of the Gulfs of Suez [A line running from Ràs Muhammed (27°43'N) to the South point of Shadwan Island (34°02'E) and thence Westward on a parallel (27°27'N) to the coast of Africa] and Aqaba [A line running from Ràs al Fasma Southwesterly to Requin Island (

27°57′N 34°36′E) through Tiran Island to the Southwest point thereof and thence Westward on a parallel (27°54'N) to the coast of the Sinaï Peninsula].

On the South. A line joining Husn Murad (

12°40′N 43°30′E) and Ras Siyan (

12°29′N 43°20′E).

   

Name

 

Red Sea is a direct translation of the Greek Erythra Thalassa (Ερυθρὰ Θάλασσα) and Latin Mare Rubrum (alternatively Sinus Arabicus, literally "Arabian Gulf"), Arabic Al-Baḥr Al-Aḥmar (البحر الأحمر) or Baḥr Al-Qalzam(بحر القلزم), Somali Badda Cas and Tigrinya Qeyyiḥ bāḥrī (ቀይሕ ባሕሪ). The name of the sea may signify the seasonal blooms of the red-coloured Trichodesmium erythraeum near the water's surface.[7] A theory favored by some modern scholars[who?] is that the name red is referring to the direction South, just as the Black Sea's name may refer to North. The basis of this theory is that some Asiatic languages used color words to refer to the cardinal directions.[8] Herodotus on one occasion uses Red Sea and Southern Sea interchangeably.[9]

The association of the Red Sea with the Biblical account of the Israelite Crossing the Red Sea is ancient, and was made explicit in the Septuagint translation of the Book of Exodus from Hebrew to Koine Greek in approximately the third century B.C. In that version, the Hebrew Yam Suph (ים סוף) is translated as Erythra Thalassa (Red Sea). (See also the more recent suggestion that the Yam Suph of the Exodus refers to a Sea of Reeds). The Red Sea is one of four seas named in English after common color terms — the others being the Black Sea, the White Sea and the Yellow Sea. The direct rendition of the Greek Erythra thalassa in Latin as Mare Erythraeum refers to the north-western part of the Indian Ocean, and also to a region on Mars.

  

History

 

The earliest known exploration of the Red Sea was conducted by Ancient Egyptians, as they attempted to establish commercial routes to Punt. One such expedition took place around 2500 BC, and another around 1500 BC ( by Hatshepsut ). Both involved long voyages down the Red Sea.[10] The Biblical Book of Exodus tells the story of the Israelites' miraculous crossing of a body of water, which the Hebrew text calls Yam Suph. Yam Suph is traditionally identified as the Red Sea. The account is part of the Israelites' escape from slavery in Egypt. Yam Suph can also been translated as Sea of Reeds.

In the 6th century BC, Darius the Great of Persia sent reconnaissance missions to the Red Sea, improving and extending navigation by locating many hazardous rocks and currents. A canal was built between the Nile and the northern end of the Red Sea at Suez. In the late 4th century BC, Alexander the Great sent Greek naval expeditions down the Red Sea to the Indian Ocean. Greek navigators continued to explore and compile data on the Red Sea. Agatharchides collected information about the sea in the 2nd century BC. The Periplus of the Erythraean Sea ("Periplus of the Red Sea"), a Greek periplus written by an unknown author around the 1st century AD, contain a detailed description of the Red Sea's ports and sea routes.[11] The Periplus also describes how Hippalus first discovered the direct route from the Red Sea to India.

 

The Red Sea was favored for Roman trade with India starting with the reign of Augustus, when the Roman Empire gained control over the Mediterranean, Egypt, and the northern Red Sea. The route had been used by previous states but grew in the volume of traffic under the Romans. From Indian ports goods from China were introduced to the Roman world. Contact between Rome and China depended on the Red Sea, but the route was broken by the Aksumite Empire around the 3rd century AD.[12]

During the Middle Ages, the Red Sea was an important part of the Spice trade route. In 1513, trying to secure that channel to Portugal, Afonso de Albuquerque laid siege to Aden.[13] but was forced to retreat. They cruised the Red Sea inside the Bab al-Mandab, as the first European fleet to have sailed this waters.

In 1798, France ordered General Bonaparte to invade Egypt and take control of the Red Sea. Although he failed in his mission, the engineer Jean-Baptiste Lepère, who took part in it, revitalised the plan for a canal which had been envisaged during the reign of the Pharaohs. Several canals were built in ancient times from the Nile to the Red Sea along or near the line of the present Sweet Water Canal, but none lasted for long. The Suez Canal was opened in November 1869. At the time, the British, French, and Italians shared the trading posts. The posts were gradually dismantled following the First World War. After the Second World War, the Americans and Soviets exerted their influence whilst the volume of oil tanker traffic intensified. However, the Six Day War culminated in the closure of the Suez Canal from 1967 to 1975. Today, in spite of patrols by the major maritime fleets in the waters of the Red Sea, the Suez Canal has never recovered its supremacy over the Cape route, which is believed to be less vulnerable.

   

Oceanography

 

The Red Sea lies between arid land, desert and semi-desert. The main reasons for the better development of reef systems along the Red Sea is because of its greater depths and an efficient water circulation pattern, The Red Sea water mass exchanges its water with the Arabian Sea, Indian Ocean via the Gulf of Aden. These physical factors reduce the effect of high salinity caused by evaporation water in the north and relatively hot water in the south.

The climate of the Red Sea is the result of two distinct monsoon seasons; a northeasterly monsoon and a southwesterly monsoon. Monsoon winds occur because of the differential heating between the land surface and sea. Very high surface temperatures coupled with high salinities makes this one of the hottest and saltiest bodies of seawater in the world. The average surface water temperature of the Red Sea during the summer is about 26 °C (79 °F) in the north and 30 °C (86 °F) in the south, with only about 2 °C (3.6 °F) variation during the winter months. The overall average water temperature is 22 °C (72 °F). Today surface water temperatures remain relatively constant at 21–25 °C (70–77 °F). Temperature and visibility remain good to around 200 m (656 ft). The sea is known for its strong winds and unpredictable local currents.

The rainfall over the Red Sea and its coasts is extremely low, averaging 0.06 m (2.36 in) per year. The rain is mostly in the form of showers of short spells, often associated with thunderstorms and occasionally with dust storms. The scarcity of rainfall and no major source of fresh water to the Red Sea result in the excess evaporation as high as 205 cm (81 in) per year and high salinity with minimal seasonal variation. A recent underwater expedition to the Red Sea offshore from Sudan and Eritrea[14] found surface water temperatures 28 °C in winter and up to 34 °C in the summer, but despite that extreme heat the coral was healthy with much fish life with very little sign of coral bleaching, and there were plans to use samples of these corals' apparently heat-adapted commensal algae to salvage bleached coral elsewhere.

 

Salinity

 

The Red Sea is one of the most saline bodies of water in the world, due to high evaporation. Salinity ranges from between ~36 ‰ in the southern part due to the effect of the Gulf of Aden water and reaches 41 ‰ in the northern part, due mainly to the Gulf of Suez water and the high evaporation. The average salinity is 40 ‰. (Average salinity for the world's seawater is ~35 ‰ on the Practical Salinity Scale, or PPS; that translates to 3.5 % actual dissolved salts.)

In terms of salinity, the Red Sea is greater than the world average, approximately 4 percent. This is due to several factors:

1.High rate of evaporation and very little precipitation.

2.Lack of significant rivers or streams draining into the sea.

3.Limited connection with the Indian Ocean, which has lower water salinity.

 

Tidal range

In general tide ranges between 0.6 m (2.0 ft) in the north, near the mouth of the Gulf of Suez and 0.9 m (3.0 ft) in the south near the Gulf of Aden but it fluctuates between 0.20 m (0.66 ft) and 0.30 m (0.98 ft) away from the nodal point. The central Red Sea (Jeddah area) is therefore almost tideless, and as such the annual water level changes are more significant. Because of the small tidal range the water during high tide inundates the coastal sabkhas as a thin sheet of water up to a few hundred metres rather than inundating the sabkhas through a network of channels. However, south of Jeddah in the Shoiaba area the water from the lagoon may cover the adjoining sabkhas as far as 3 km (2 mi) whereas, north of Jeddah in the Al-kharrar area the sabkhas are covered by a thin sheet of water as far as 2 km (1.2 mi). The prevailing north and northeastern winds influence the movement of water in the coastal inlets to the adjacent sabkhas, especially during storms. Winter mean sea level is 0.5 m (1.6 ft) higher than in summer. Tidal velocities passing through constrictions caused by reefs, sand bars and low islands commonly exceed 1–2 m/s (3–6.5 ft/s). Coral reefs in the Red Sea are near Egypt, Saudi Arabia, Israel and Sudan.

 

Current

In the Red Sea detailed current data is lacking, partially because they are weak and variable both spatially and temporally. Temporal and spatial currents variation is as low as 0.5 m (1.6 ft) and are governed all by wind. During the summer, NW winds drive surface water south for about four months at a velocity of 15–20 cm/s (6–8 in/s), whereas in winter the flow is reversed resulting in the inflow of water from the Gulf of Aden into the Red Sea. The net value of the latter predominates, resulting in an overall drift to the northern end of the Red Sea. Generally, the velocity of the tidal current is between 50–60 cm/s (20–23.6 in/s) with a maximum of 1 m/s (3.3 ft) at the mouth of the al-Kharrar Lagoon. However, the range of the north-northeast current along the Saudi coast is 8–29 cm/s (3–11.4 in/s).

 

Wind regime

With the exception of the northern part of the Red Sea, which is dominated by persistent north-west winds, with speeds ranging between 7 km/h (4.3 mph) and 12 km/h (7.5 mph), the rest of the Red Sea and the Gulf of Aden are subjected to the influence of regular and seasonally reversible winds. The wind regime is characterized by both seasonal and regional variations in speed and direction with average speed generally increasing northward.

Wind is the driving force in the Red Sea for transporting the material either as suspension or as bedload. Wind induced currents play an important role in the Red Sea in initiating the process of resuspension of bottom sediments and transfer of materials from sites of dumping to sites of burial in quiescent environment of deposition. Wind generated current measurement is therefore important in order to determine the sediment dispersal pattern and its role in the erosion and accretion of the coastal rock exposure and the submerged coral beds.

 

Geology

 

The Red Sea was formed by Arabia splitting from Africa due to movement of the Red Sea Rift. This split started in the Eocene and accelerated during the Oligocene. The sea is still widening and it is considered that the sea will become an ocean in time (as proposed in the model of John Tuzo Wilson). In 1949, a deep water survey reported anomalously hot brines in the central portion of the Red Sea. Later work in the 1960s confirmed the presence of hot, 60 °C (140 °F), saline brines and associated metalliferous muds. The hot solutions were emanating from an active subseafloor rift. The highly saline character of the waters was not hospitable to living organisms.[15]

Sometimes during the Tertiary period the Bab el Mandeb closed and the Red Sea evaporated to an empty hot dry salt-floored sink. Effects causing this would be:

•A "race" between the Red Sea widening and Perim Island erupting filling the Bab el Mandeb with lava.

•The lowering of world sea level during the Ice Ages due to much water being locked up in the ice caps.

A number of volcanic islands rise from the center of the sea. Most are dormant, but in 2007 Jabal al-Tair island, in the Bab el Mandeb strait, erupted violently. An eruption among the nearby Zubair islands followed in 2011.[16]

  

Mineral resources

In terms of mineral resources the major constituents of the Red Sea sediments are as follows:

•Biogenic constituents:

Nanofossils, foraminifera, pteropods, siliceous fossils

•Volcanogenic constituents:

Tuffites, volcanic ash, montmorillonite, cristobalite, zeolites

•Terrigenous constituents:

Quartz, feldspars, rock fragments, mica, heavy minerals, clay minerals

•Authigenic minerals:

Sulfide minerals, aragonite, Mg-calcite, protodolomite, dolomite, quartz, chalcedony.

•Evaporite minerals:

Magnesite, gypsum, anhydrite, halite, polyhalite

•Brine precipitate:

Fe-montmorillonite, goethite, hematite, siderite, rhodochrosite, pyrite, sphalerite, anhydrite.

 

Living resources

The Red Sea is a rich and diverse ecosystem. More than 1200 species of fish[17] have been recorded in the Red Sea, and around 10% of these are found nowhere else.[18] This also includes 42 species of deepwater fish.[17]

 

The rich diversity is in part due to the 2,000 km (1,240 mi) of coral reef extending along its coastline; these fringing reefs are 5000–7000 years old and are largely formed of stony acropora and porites corals. The reefs form platforms and sometimes lagoons along the coast and occasional other features such as cylinders (such as the Blue Hole (Red Sea) at Dahab). These coastal reefs are also visited by pelagic species of red sea fish, including some of the 44 species of shark.

The Red Sea also contains many offshore reefs including several true atolls. Many of the unusual offshore reef formations defy classic (i.e., Darwinian) coral reef classification schemes, and are generally attributed to the high levels of tectonic activity that characterize the area.

The special biodiversity of the area is recognized by the Egyptian government, who set up the Ras Mohammed National Park in 1983. The rules and regulations governing this area protect local marine life, which has become a major draw for diving enthusiasts.

Divers and snorkellers should be aware that although most Red Sea species are innocuous, a few are hazardous to humans: see Red Sea species hazardous to humans.[19]

Other marine habitats include sea grass beds, salt pans, mangroves and salt marshes.

 

Desalination plants

There is extensive demand of desalinated water to meet the requirement of the population and the industries along the Red Sea.

There are at least 18 desalination plants along the Red Sea coast of Saudi Arabia which discharge warm brine and treatment chemicals (chlorine and anti-scalants) that may cause bleaching and mortality of corals and diseases to the fish stocks. Although this is only a localized phenomenon, it may intensify with time and have a profound impact on the fishing industry.[20]

The water from the Red Sea is also utilized by oil refineries and cement factories for cooling purposes. Used water drained back into the coastal zones may cause harm to the nearshore environment of the Red Sea.

 

Security

The Red Sea is part of the sea roads between Europe, the Persian Gulf and East Asia, and as such has heavy shipping traffic. Piracy in Somalia occurs principally near the area of the Gulf of Aden south of the sea. Government-related bodies with responsibility to police the Red Sea area include the Port Said Port Authority, Suez Canal Authority and Red Sea Ports Authority of Egypt, Jordan Maritime Authority, Israel Port Authority, Saudi Ports Authority and Sea Ports Corporation of Sudan.

 

Facts and figures

•Length: ~2,250 km (1,398.1 mi) - 79% of the eastern Red Sea with numerous coastal inlets

•Maximum Width: ~ 306–355 km (190–220 mi)– Massawa (Eritrea)

•Minimum Width: ~ 26–29 km (16–18 mi)- Bab el Mandeb Strait (Yemen)

•Average Width: ~ 280 km (174.0 mi)

•Average Depth: ~ 490 m (1,607.6 ft)

•Maximum Depth: ~2,211 m (7,253.9 ft)

•Surface Area: 438-450 x 10² km² (16,900–17,400 sq mi)

•Volume: 215–251 x 10³ km³ (51,600–60,200 cu mi)

•Approximately 40% of the Red Sea is quite shallow (under 100 m/330 ft), and about 25% is under 50 m (164 ft) deep.

•About 15% of the Red Sea is over 1,000 m (3,300 ft) depth that forms the deep axial trough.

•Shelf breaks are marked by coral reefs

•Continental slope has an irregular profile (series of steps down to ~500 m/1,640 ft)

•Centre of Red Sea has a narrow trough (~ 1,000 m/3,281 ft; some deeps may exceed 2,500 m/8,202 ft)

 

Tourism

 

The sea is known for its spectacular recreational diving sites, such as Ras Mohammed, SS Thistlegorm (shipwreck), Elphinstone, The Brothers, Dolphin Reef and Rocky Island in Egypt and less known sites in Sudan such as Sanganeb, Abington, Angarosh and Shaab Rumi.

The Red Sea became known as a sought-after diving destination after the expeditions of Hans Hass in the 1950s, and later by Jacques-Yves Cousteau. Popular tourist resorts include El Gouna, Hurghada, Safaga, Marsa Alam, on the western shore of the Red Sea, and Sharm-El-Sheikh, Dahab, and Taba on the Egyptian side of Sinaï, as well as Aqaba in Jordan and Eilat in Israel in an area known as the Red Sea Riviera.

The popular tourist beach of Sharm el-Sheikh was closed to all swimming in December 2010 due to several serious shark attacks, including one fatal one. As of December 2010, scientists are investigating the attacks and have identified, but not verified, several possible causes including over fishing which causes large sharks to hunt closer to shore, tourist boat operators who chum the waters just offshore to present shark-photo opportunities, and reports of passing ships throwing dead livestock overboard. Furthermore the geography of some parts of the Red Sea is such that large sharks can sometimes wander close to shore. This is due to the sea's narrow width, significant depth, and sharp drop-offs, all of which combine to form a geography where large deep-water sharks can roam in hundreds of meters of water, yet be within a hundred meters of swimming areas.

 

Bordering countries

The Red Sea may be geographically divided into three sections: the Red Sea proper, and in the north, the Gulf of Aqaba and the Gulf of Suez. The six countries bordering the Red Sea proper are:

•Eastern shore:

o Saudi Arabia

o Yemen

•Western shore:

o Egypt

o Sudan

o Eritrea

o Djibouti

The Gulf of Suez is entirely bordered by Egypt. The Gulf of Aqaba borders Egypt, Israel, Jordan and Saudi Arabia.

In addition to the standard geographical definition of the six countries bordering the Red Sea cited above, areas such as Somalia and Ethiopia are sometimes also described as Red Sea territories. This is primarily due to their proximity to and geological similarities with the nations facing the Red Sea and/or political ties with said areas.[21][22]

 

Towns and cities

Towns and cities on the Red Sea coast (including the coasts of the Gulfs of Aqaba and Suez) include:

• Al Hudaydah (الحديدة)

• Al Lith (الليِّث)

• Al Qunfudhah (القنفذة)

• Al-Qusair (القصير)

• Al Wajh (الوجه)

• Aqaba (العقبة)

• Asseb (ዓሳብ)

• Dahab (دهب)

• Duba (ضباء)

• Eilat (אילת)

• El Gouna (الجونة)

• El Suweis (السويس)

• / Hala'ib (حلايب) (disputed)

• Haql (حقل)

• Hirgigo (ሕርጊጎ)

• Hurghada (الغردقة)

• Jeddah (جدة)

• Jazan (جازان)

• Marsa Alam (مرسى علم)

• Massawa (ምጽዋ)

• Nuweiba (نويبع)

• Port Safaga (ميناء سفاجا)

• Port Sudan (بورت سودان)

• Rabigh (رابغ)

• Sharm el Sheikh (شرم الشيخ)

• Soma Bay (سوما باي)

• Suakin (سواكن)

• Taba (طابا)

• Thuwal (ثول)

• Yanbu (ينبع)

   

~Mark Twain

 

This is another shot from the University of Pittsburgh campus, of Heinz Chapel

 

Not necessary, but they always seem better large!

 

Have a great weekend my friends!

 

Explored July 25, #191

 

Thank you so much for all of your comments and views!

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The Bergische Museumsbahn is a heritage tram museum situated in the German city of Wuppertal. It operates its own tram line south of Wuppertal on original rails with original cars. Wuppertal operates still the "Schwebebahn", a unique overhead railway.

 

The museum line begins about 50 m east of the Kohlfurth bridge, where the depot may be found with its exhibition of vehicles and a bookshop. A track coming from the bridge is currently out of use. East of the depot the line winds its way south and then swings around in a 180° curve in order to follow the Kaltenbach valley north. The end of the line is currently at Greuel halt, although it has long been planned to work the section beyond that to Möschenborn.

 

Near Möschenborn halt the old line turns south again in order to reach Cronenberg.

 

The route has a height difference of about 150 metres, which means that it has an average incline of 5%. The largest part of the route cuts through a wood and is therefore typical of the former overground tramway network. On the other had the route does not really have any town sections. There are seven stops.

 

www.tram-info.de/bmb/

The Amazon river dolphin (Inia geoffrensis), also known as the Boto or pink river dolphin, is a species of toothed whale classified in the family Iniidae.

 

The Amazon river dolphin is the largest species of river dolphin, with adult males reaching 185 kilograms (408 lb) in weight, and 2.5 metres (8.2 ft) in length. Adults acquire a pink color, more prominent in males, giving it its nickname "pink river dolphin". Sexual dimorphism is very evident, with males measuring 16% and weighing 55% more than females. Like other toothed whales, they have a melon, an organ that is used for bio sonar. The dorsal fin, although short in height, is regarded as long, and the pectoral fins are also large. The fin size, unfused vertebrae, and its relative size allow for improved manoeuvrability when navigating flooded forests and capturing prey.

 

They have one of the widest ranging diets among toothed whales, and feed on up to 53 different species of fish, such as croakers, catfish, tetras and piranhas. They also consume other animals such as river turtles and freshwater crabs.

 

The Amazon river dolphin is the largest river dolphin. Adult males reach a maximum length and weight of 2.55 metres (8.4 ft) (average 2.32 metres (7.6 ft)) and 185 kilograms (408 lb) (average 154 kilograms (340 lb)), while females reach a length and weight of 2.15 metres (7.1 ft) (mean 2 metres (6.6 ft)) and 150 kilograms (330 lb) (average 100 kilograms (220 lb)). It has very evident sexual dimorphism, with males measuring and weighing between 16% and 55% more than females, making it unique among cetaceans, where females are generally larger than males.

 

The texture of the body is robust and strong but flexible. Unlike oceanic dolphins; the cervical vertebrae are not fused, allowing the head to turn 90 degrees. The flukes are broad and triangular, and the dorsal fin, which is keel-shaped, is short in height but very long, extending from the middle of the body to the caudal region. The pectoral fins are large and paddle-shaped. The length of its fins allows the animal to perform a circular movement, allowing for exceptional maneuverability to swim through the flooded forest but decreasing its speed.

 

The body colour varies with age. Newborns and the young have a dark grey tint, which in adolescence transforms into light grey, and in adults turns pink as a result of repeated abrasion of the skin surface. Males tend to be pinker than females due to more frequent trauma from intra-species aggression.

 

The colour of adults varies between solid and mottled pink and in some adults the dorsal surface is darker. It is believed that the difference in color depends on the temperature, water transparency, and geographical location.

  

Amazon river dolphins have a heterodont dentition

The skull of the species is slightly asymmetrical compared to the other toothed whales. It has a long, thin snout, with 25 to 28 pairs of long and slender teeth to each side of both jaws. Dentition is heterodont, meaning that the teeth differ in shape and length, with differing functions for both grabbing and crushing prey. Anterior teeth are conical and later have ridges on the inside of the crown. Despite small eyes, the species seems to have good eyesight in and out of the water. It has a melon on the head, the shape of which can be modified by muscular control when used for biosonar. Breathing takes place every 30 to 110 seconds.

Rather average pain jobs. I like them all without helmets better.

average,boring, complete

The Mount Elliott Mining Complex is an aggregation of the remnants of copper mining and smelting operations from the early 20th century and the associated former mining township of Selwyn. The earliest copper mining at Mount Elliott was in 1906 with smelting operations commencing shortly after. Significant upgrades to the mining and smelting operations occurred under the management of W.R. Corbould during 1909 - 1910. Following these upgrades and increases in production, the Selwyn Township grew quickly and had 1500 residents by 1918. The Mount Elliott Company took over other companies on the Cloncurry field in the 1920s, including the Mount Cuthbert and Kuridala smelters. Mount Elliott operations were taken over by Mount Isa Mines in 1943 to ensure the supply of copper during World War Two. The Mount Elliott Company was eventually liquidated in 1953.

 

The Mount Elliott Smelter:

 

The existence of copper in the Leichhardt River area of north western Queensland had been known since Ernest Henry discovered the Great Australia Mine in 1867 at Cloncurry. In 1899 James Elliott discovered copper on the conical hill that became Mount Elliott, but having no capital to develop the mine, he sold an interest to James Morphett, a pastoralist of Fort Constantine station near Cloncurry. Morphett, being drought stricken, in turn sold out to John Moffat of Irvinebank, the most successful mining promoter in Queensland at the time.

 

Plentiful capital and cheap transport were prerequisites for developing the Cloncurry field, which had stagnated for forty years. Without capital it was impossible to explore and prove ore-bodies; without proof of large reserves of wealth it was futile to build a railway; and without a railway it was hazardous to invest capital in finding large reserves of ore. The mining investor or the railway builder had to break the impasse.

 

In 1906 - 1907 copper averaged £87 a ton on the London market, the highest price for thirty years, and the Cloncurry field grew. The railway was extended west of Richmond in 1905 - 1906 by the Government and mines were floated on the Melbourne Stock Exchange. At Mount Elliott a prospecting shaft had been sunk and on the 1st of August 1906 a Cornish boiler and winding plant were installed on the site.

 

Mount Elliott Limited was floated in Melbourne on the 13th of July 1906. In 1907 it was taken over by British and French interests and restructured. Combining with its competitor, Hampden Cloncurry Copper Mines Limited, Mount Elliott formed a special company to finance and construct the railway from Cloncurry to Malbon, Kuridala (then Friezeland) and Mount Elliott (later Selwyn). This new company then entered into an agreement with the Queensland Railways Department in July 1908.

 

The railway, which was known as the 'Syndicate Railway', aroused opposition in 1908 from the trade unions and Labor movement generally, who contended that railways should be State-owned. However, the Hampden-Mount Elliott Railway Bill was passed by the Queensland Parliament and assented to on the 21st of April 1908; construction finished in December 1910. The railway terminated at the Mount Elliott smelter.

 

By 1907 the main underlie shaft had been sunk and construction of the smelters was underway using a second-hand water-jacket blast furnace and converters. At this time, W.H. Corbould was appointed general manager of Mount Elliott Limited.

 

The second-hand blast furnace and converters were commissioned or 'blown in' in May 1909, but were problematic causing hold-ups. Corbould referred to the equipment in use as being the 'worst collection of worn-out junk he had ever come across'. Corbould soon convinced his directors to scrap the plant and let him design new works.

 

Corbould was a metallurgist and geologist as well as mine/smelter manager. He foresaw a need to obtain control and thereby ensure a reliable supply of ore from a cross-section of mines in the region. He also saw a need to implement an effective strategy to manage the economies of smelting low-grade ore. Smelting operations in the region were made difficult by the technical and economic problems posed by the deterioration in the grade of ore. Corbould resolved the issue by a process of blending ores with different chemical properties, increasing the throughput capacity of the smelter and by championing the unification of smelting operations in the region. In 1912, Corbould acquired Hampden Consols Mine at Kuridala for Mount Elliott Limited, followed with the purchases of other small mines in the district.

 

Walkers Limited of Maryborough was commissioned to manufacture a new 200 ton water jacket furnace for the smelters. An air compressor and blower for the smelters were constructed in the powerhouse and an electric motor and dynamo provided power for the crane and lighting for the smelter and mine.

 

The new smelter was blown in September 1910, a month after the first train arrived, and it ran well, producing 2040 tons of blister copper by the end of the year. The new smelting plant made it possible to cope with low-grade sulphide ores at Mount Elliott. The use of 1000 tons of low-grade sulphide ores bought from the Hampden Consols Mine in 1911 made it clear that if a supply of higher sulphur ore could be obtained and blended, performance, and economy would improve. Accordingly, the company bought a number of smaller mines in the district in 1912.

 

Corbould mined with cut and fill stoping but a young Mines Inspector condemned the system, ordered it dismantled and replaced with square set timbering. In 1911, after gradual movement in stopes on the No. 3 level, the smelter was closed for two months. Nevertheless, 5447 tons of blister copper was produced in 1911, rising to 6690 tons in 1912 - the company's best year. Many of the surviving structures at the site were built at this time.

 

Troubles for Mount Elliott started in 1913. In February, a fire at the Consols Mine closed it for months. In June, a thirteen week strike closed the whole operation, severely depleting the workforce. The year 1913 was also bad for industrial accidents in the area, possibly due to inexperienced people replacing the strikers. Nevertheless, the company paid generous dividends that year.

 

At the end of 1914 smelting ceased for more than a year due to shortage of ore. Although 3200 tons of blister copper was produced in 1913, production fell to 1840 tons in 1914 and the workforce dwindled to only 40 men. For the second half of 1915 and early 1916 the smelter treated ore railed south from Mount Cuthbert. At the end of July 1916 the smelting plant at Selwyn was dismantled except for the flue chambers and stacks. A new furnace with a capacity of 500 tons per day was built, a large amount of second-hand equipment was obtained and the converters were increased in size.

 

After the enlarged furnace was commissioned in June 1917, continuing industrial unrest retarded production which amounted to only 1000 tons of copper that year. The point of contention was the efficiency of the new smelter which processed twice as much ore while employing fewer men. The company decided to close down the smelter in October and reduce the size of the furnace, the largest in Australia, from 6.5m to 5.5m. In the meantime the price of copper had almost doubled from 1916 due to wartime consumption of munitions.

 

The new furnace commenced on the 16th of January 1918 and 77,482 tons of ore were smelted yielding 3580 tons of blister copper which were sent to the Bowen refinery before export to Britain. Local coal and coke supply was a problem and materials were being sourced from the distant Bowen Colliery. The smelter had a good run for almost a year except for a strike in July and another in December, which caused Corbould to close down the plant until New Year. In 1919, following relaxation of wartime controls by the British Metal Corporation, the copper price plunged from about £110 per ton at the start of the year to £75 per ton in April, dashing the company's optimism regarding treatment of low grade ores. The smelter finally closed after two months operation and most employees were laid off.

 

For much of the period 1919 to 1922, Corbould was in England trying to raise capital to reorganise the company's operations but he failed and resigned from the company in 1922. The Mount Elliott Company took over the assets of the other companies on the Cloncurry field in the 1920s - Mount Cuthbert in 1925 and Kuridala in 1926. Mount Isa Mines bought the Mount Elliott plant and machinery, including the three smelters, in 1943 for £2,300, enabling them to start copper production in the middle of the Second World War. The Mount Elliott Company was finally liquidated in 1953.

 

In 1950 A.E. Powell took up the Mount Elliott Reward Claim at Selwyn and worked close to the old smelter buildings. An open cut mine commenced at Starra, south of Mount Elliott and Selwyn, in 1988 and is Australia's third largest copper producer producing copper-gold concentrates from flotation and gold bullion from carbon-in-leach processing.

 

Profitable copper-gold ore bodies were recently proved at depth beneath the Mount Elliott smelter and old underground workings by Cyprus Gold Australia Pty Ltd. These deposits were subsequently acquired by Arimco Mining Pty Ltd for underground development which commenced in July 1993. A decline tunnel portal, ore and overburden dumps now occupy a large area of the Maggie Creek valley south-west of the smelter which was formerly the site of early miner's camps.

 

The Old Selwyn Township:

 

In 1907, the first hotel, run by H. Williams, was opened at the site. The township was surveyed later, around 1910, by the Mines Department. The town was to be situated north of the mine and smelter operations adjacent the railway, about 1.5km distant. It took its name from the nearby Selwyn Ranges which were named, during Burke's expedition, after the Victorian Government Geologist, A.R. Selwyn. The town has also been known by the name of Mount Elliott, after the nearby mines and smelter.

 

Many of the residents either worked at the Mount Elliott Mine and Smelter or worked in the service industries which grew around the mining and smelting operations. Little documentation exists about the everyday life of the town's residents. Surrounding sheep and cattle stations, however, meant that meat was available cheaply and vegetables grown in the area were delivered to the township by horse and cart. Imported commodities were, however, expensive.

 

By 1910 the town had four hotels. There was also an aerated water manufacturer, three stores, four fruiterers, a butcher, baker, saddler, garage, police, hospital, banks, post office (officially from 1906 to 1928, then unofficially until 1975) and a railway station. There was even an orchestra of ten players in 1912. The population of Selwyn rose from 1000 in 1911 to 1500 in 1918, before gradually declining.

 

Source: Queensland Heritage Register.

In the last century alone, galaxy NGC 6946 has experienced 10 observed supernovae, earning its nickname as the Fireworks Galaxy. In comparison, our Milky Way averages just 1-2 supernova events per century. This Hubble Space Telescope image shows the stars, spiral arms, and various stellar environments of NGC 6946 in phenomenal detail.

 

NGC 6946 is a face-on galaxy, which means that we see the galaxy facing us, rather than seeing it from the side (known as edge-on). The Fireworks Galaxy is further classified as an intermediate spiral galaxy and as a starburst galaxy. The former means the structure of NGC 6946 sits between a full spiral and a barred spiral galaxy, with only a slight bar in its center, and the latter means it has an exceptionally high rate of star formation.

 

The galaxy resides 25.2 million light-years away, along the border of the northern constellations of Cepheus and Cygnus (The Swan).

 

Credit: ESA/Hubble & NASA, A. Leroy, K. S. Long

 

For more information, visit: esahubble.org/images/potw2101a/

 

Find us on Twitter, Instagram, Facebook and YouTube

 

Former one-room schoolhouse Stardale S.S # 5 in the community of Stardale, Township of East Hawkesbury, Ontario, Canada. Still researching when it was erected and when it ceased to function as a school. It figures in a 1912 listing of Separate Schools in the province of Ontario, with an average attendance of 21 students. Unlike many one-room schoolhouses, this one has two front doors.

at Bryn Oh's Gathering

 

maps.secondlife.com/secondlife/Immersiva/12/108/23

Greyhope Bay, Aberdeen.

Fort Lauderdale is a city in the U.S. state of Florida, 25 miles (40 km) north of Miami. It is the county seat of Broward County. As of the 2019 census, the city has an estimated population of 182,437. Fort Lauderdale is a principal city of the Miami metropolitan area, which was home to an estimated 6,198,782 people in 2018.

 

The city is a popular tourist destination, with an average year-round temperature of 75.5 °F (24.2 °C) and 3,000 hours of sunshine per year. Greater Fort Lauderdale which takes in all of Broward County hosted 12 million visitors in 2012, including 2.8 million international visitors. The city and county in 2012 collected $43.9 million from the 5% hotel tax it charges, after hotels in the area recorded an occupancy rate for the year of 72.7 percent and an average daily rate of $114.48. The district has 561 hotels and motels comprising nearly 35,000 rooms. Forty six cruise ships sailed from Port Everglades in 2012. Greater Fort Lauderdale has over 4,000 restaurants, 63 golf courses, 12 shopping malls, 16 museums, 132 nightclubs, 278 parkland campsites, and 100 marinas housing 45,000 resident yachts.

 

Fort Lauderdale is named after a series of forts built by the United States during the Second Seminole War. The forts took their name from Major William Lauderdale (1782–1838), younger brother of Lieutenant Colonel James Lauderdale. William Lauderdale was the commander of the detachment of soldiers who built the first fort. However, development of the city did not begin until 50 years after the forts were abandoned at the end of the conflict. Three forts named "Fort Lauderdale" were constructed; the first was at the fork of the New River, the second at Tarpon Bend on the New River between the Colee Hammock and Rio Vista neighborhoods, and the third near the site of the Bahia Mar Marina.

 

The area in which the city of Fort Lauderdale would later be founded was inhabited for more than two thousand years by the Tequesta Indians. Contact with Spanish explorers in the 16th century proved disastrous for the Tequesta, as the Europeans unwittingly brought with them diseases, such as smallpox, to which the native populations possessed no resistance. For the Tequesta, disease, coupled with continuing conflict with their Calusa neighbors, contributed greatly to their decline over the next two centuries. By 1763, there were only a few Tequesta left in Florida, and most of them were evacuated to Cuba when the Spanish ceded Florida to the British in 1763, under the terms of the Treaty of Paris (1763), which ended the Seven Years' War. Although control of the area changed between Spain, the United Kingdom, the United States, and the Confederate States of America, it remained largely undeveloped until the 20th century.

 

The Fort Lauderdale area was known as the "New River Settlement" before the 20th century. In the 1830s there were approximately 70 settlers living along the New River. William Cooley, the local Justice of the Peace, was a farmer and wrecker, who traded with the Seminole Indians. On January 6, 1836, while Cooley was leading an attempt to salvage a wrecked ship, a band of Seminoles attacked his farm, killing his wife and children, and the children's tutor. The other farms in the settlement were not attacked, but all the white residents in the area abandoned the settlement, fleeing first to the Cape Florida Lighthouse on Key Biscayne, and then to Key West.

 

The first United States stockade named Fort Lauderdale was built in 1838, and subsequently was a site of fighting during the Second Seminole War. The fort was abandoned in 1842, after the end of the war, and the area remained virtually unpopulated until the 1890s. It was not until Frank Stranahan arrived in the area in 1893 to operate a ferry across the New River, and the Florida East Coast Railroad's completion of a route through the area in 1896, that any organized development began. The city was incorporated in 1911, and in 1915 was designated the county seat of newly formed Broward County.

 

Fort Lauderdale's first major development began in the 1920s, during the Florida land boom of the 1920s. The 1926 Miami Hurricane and the Great Depression of the 1930s caused a great deal of economic dislocation. In July 1935, an African-American man named Rubin Stacy was accused of robbing a white woman at knife point. He was arrested and being transported to a Miami jail when police were run off the road by a mob. A group of 100 white men proceeded to hang Stacy from a tree near the scene of his alleged robbery. His body was riddled with some twenty bullets. The murder was subsequently used by the press in Nazi Germany to discredit US critiques of its own persecution of Jews, Communists, and Catholics.

 

When World War II began, Fort Lauderdale became a major US base, with a Naval Air Station to train pilots, radar operators, and fire control, operators. A Coast Guard base at Port Everglades was also established.

 

On July 4, 1961, African Americans started a series of protests, wade-ins, at beaches that were off-limits to them, to protest "the failure of the county to build a road to the Negro beach". On July 11, 1962, a verdict by Ted Cabot went against the city's policy of racial segregation of public beaches.

Today, Fort Lauderdale is a major yachting center, one of the nation's largest tourist destinations, and the center of a metropolitan division with 1.8 million people.

 

Credit for the data above is given to the following website:

en.wikipedia.org/wiki/Fort_Lauderdale,_Florida

 

© All Rights Reserved - you may not use this image in any form without my prior permission.

 

When I saw her, I went, "Daaayum!" She has some seriously long legs and I knew I needed to get a photo of her

 

She must have stood about 6'2" without the heels. While taking her photo, another average height girl walked by. I left her in as a point of comparison.

 

If this girl isn't a model, she should be. She has legs that go on 'til next week. And, yep, I *told* her that. Even Gaia was amazed by her legs.

View Large

 

Most people (anyway, most consumers of media in the west) have seen this place before. A lot. During the week you can practically assume you'll see some kind of filming or photography happening here.

 

And why not? It's a weird, beautiful, fantastic place. It's easy for film crews and average people to access. As a Los Angeles County Park, it's free to visit (you'll need to buy a permit for major filming though). People come here to hike, picnic, and climb the rocks (as the pair in this picture have done, even though lightning is crashing bumptiously from the sky not far to the east.) The park itself is much more than just this particular set of rocks, but these are the most iconic ones. The park comprises almost 1,000 acres of this freakish, alien, haphazard terrain created by sandstone strata tossed about willy-nilly by the ever fascinating San Andreas Fault.

 

And so, given that photographing and filming this place is almost a cliche, why do I keep coming back here to shoot? Maybe because the landscape of Vasquez Rocks is ingrained in my being. I came of age yearning to be roaming in landscapes like this when instead I was trapped in classrooms not that far away. When I was able, weekends and after school, I did roam in a landscape much like this, either hiking or riding horseback, dreaming of different ways I could conspire to be someone else. Someone not me. Vasquez Rocks is like that place I came of age in, only moreso. More of everything. Bolder, vaster, bigger, stranger: In a word, it's even more landscapey.

 

Occasionally, when I close my eyes, I see this place without meaning to--without even desiring to. I drive by here every evening and when I think the light is just right, I stop and shoot. It doesn't matter to me how many times this place has "been done." I'll keep coming back with a camera as long as there is sweet light and as long as I remain happy to be me.

 

Here's a partial list of where you may have seen Vasquez Rocks before:

Movies:

Star Trek (2009), Alpha Dog (2007), Bone Eater (2007; TV), A.I. Assault / Shockwave (2006), Cars (2006), Little Miss Sunshine (2006), Holes (2003), Joe Dirt (2001), Jay and Silent Bob Strike Back (2001), Planet of the Apes (2001), Bubble Boy (2001), Epoch (2000), Very Bad Things (1998), Free Enterprise (1998), Austin Powers: International Man of Mystery (1997), Guns of El Chupacabra (1997), Jingle All the Way (1996), Mighty Morphin Power Rangers: The Movie (1995,) The Flintstones (1994), In the Army Now (1994), Army of Darkness (1993), Mom and Dad Save the World (1992), Bill & Ted's Bogus Journey (1991), The Rapture (1991), Star Trek IV: The Voyage Home (1986), My Stepmother Is an Alien (1988) Hell Comes to Frogtown (1987), Short Circuit (1986), Metalstorm: The Destruction of Jared-Syn (1983), Parasite (1982), Hearts of the West (1975), Blazing Saddles (1974), Apache (1954), A Thousand and One Nights (film) (1945), Werewolf of London (1935), Dracula (1931)

 

Television:

CSI: Crime Scene Investigation, Saving Grace, From The Earth To The Moon—episode 10: "Galileo Was Right", The Twilight Zone (the original series), Medium, Have Gun—Will Travel, The Man from U.N.C.L.E., The Rifleman, Maverick, Broken Arrow, Mission: Impossible, 24, Airwolf, Bonanza, Buck Rogers in the 25th Century, Buffy the Vampire Slayer, Mighty Morphin Power Rangers, Roswell, Star Trek: The Original Series (notably the episodes "Arena", "The Alternative Factor", "Shore Leave", and "Friday's Child"), Star Trek: The Next Generation ("Who Watches the Watchers"), Star Trek: Voyager ("Initiations"), Star Trek: Enterprise, NCIS ("South By Southwest"), The Outer Limits, Korg: 70,000 BC, Alias, Mr. Show with Bob and David, The Fugitive (TV series), Alien Hunter, Alias Smith and Jones Hunter, Helltown, The Invaders, MacGyver, The Rat Patrol, Space: Above and Beyond, Charmed, Sliders, Friends, Fear Factor, Lassie, Las Vegas, Logan's Run, Zorro, Voyagers!, Daniel Boone, Alien Nation, The Adventures of Rin Tin Tin The Big Valley, Buffalo Bill Jr., Cimarron Strip, The Cisco Kid, Stories of the Century, The High Chaparral, Johnny Ringo The Range Rider, The Bionic Woman, Numb3rs, The Middleman, Prey, Street Hawk, Dinosaurs (TV series)

 

Commercials, Music Videos, Fashion Shoots, Magazine Spreads and other Advertising:

Way too many to list. Seriously. (list of productions snagged from wikipedia)

++++ FROM WIKIPEDIA +++++

 

Inle Lake (Burmese: အင်းလေးကန်, pronounced [ʔɪ́ɴlé kàɴ]), is a freshwater lake located in the Nyaungshwe Township of Taunggyi District of Shan State, part of Shan Hills in Myanmar (Burma). It is the second largest lake in Myanmar with an estimated surface area of 44.9 square miles (116 km2), and one of the highest at an elevation of 2,900 feet (880 m). During the dry season, the average water depth is 7 feet (2.1 m), with the deepest point being 12 feet (3.7 m), but during the rainy season this can increase by 5 feet (1.5 m).

 

The watershed area for the lake lies to a large extent to the north and west of the lake. The lake drains through the Nam Pilu or Balu Chaung on its southern end. There is also a hot spring on its northwestern shore.

 

Although the lake is not large, it contains a number of endemic species. Over twenty species of snails and nine species of fish are found nowhere else in the world. Some of these, like the silver-blue scaleless Sawbwa barb, the crossbanded dwarf danio, and the Lake Inle danio, are of minor commercial importance for the aquarium trade. It hosts approximately 20,000 brown and black head migratory seagulls in November, December and January.[1]

 

In June 2015, it became Myanmar's first designated place of World Network of Biosphere Reserves.[2] It was one of 20 places added at the Unesco's 27th Man and the Biosphere (MAB) International Coordinating Council (ICC) meeting.[3]

 

Contents

 

1 People and culture

2 Climate

3 Environmental concerns

4 Tourism

5 Cuisine

6 See also

7 References

8 External links

 

People and culture

  

The people of Inle Lake (called Intha), some 70,000 of them, live in four cities bordering the lake, in numerous small villages along the lake's shores, and on the lake itself. The entire lake area is in Nyaung Shwe township. The population consists predominantly of Intha, with a mix of other Shan, Taungyo, Pa-O (Taungthu), Danu, Kayah, Danaw and Bamar ethnicities. Most are devout Buddhists, and live in simple houses of wood and woven bamboo on stilts; they are largely self-sufficient farmers.

 

Transportation on the lake is traditionally by small boats, or by somewhat larger boats fitted with single cylinder inboard diesel engines. Local fishermen are known for practicing a distinctive rowing style which involves standing at the stern on one leg and wrapping the other leg around the oar. This unique style evolved out of necessity as the lake is covered by reeds and floating plants, making it difficult to see above them while sitting. Standing provides the rower with a view beyond the reeds. However, the leg rowing style is only practiced by the men. Women row in the customary style, using the oar with their hands, sitting cross legged at the stern.

Lotus thread is used to weave a special robe for the Buddha.

On the way home from harvesting weeds in the lake

 

Fish caught from the lake - the most abundant kind is called nga hpein locally (Inle carp, Cyprinus intha) - are a staple of the local diet. A popular local dish is htamin gyin - 'fermented' rice kneaded with fish and/or potato - served with hnapyan gyaw (literally twice fried - Shan tofu). In addition to fishing, locals grow vegetables and fruit in large gardens that float on the surface of the lake. The floating garden beds are formed by extensive manual labor. The farmers gather up lake-bottom weeds from the deeper parts of the lake, bring them back in boats and make them into floating beds in their garden areas, anchored by bamboo poles. These gardens rise and fall with changes in the water level, and so are resistant to flooding. The constant availability of nutrient-laden water results in these gardens being incredibly fertile. Rice cultivation and consumption is also significant facet of the local diet and agricultural tradition.

Climate

 

Inle Lake is suffering from the environmental effects of increased population and rapid growth in both agriculture and tourism. During the 65-year period from 1935 to 2000, the net open water area of Inle Lake decreased from 69.10 km² to 46.69 km², a loss of 32.4%, with development of floating garden agriculture, which occurs largely on the west side of the lake (a practice introduced in the 1960s).[4]

 

Lumber removal and unsustainable cultivation practices (slash and burn farming techniques) on the hills surrounding the lake are causing ever-increasing amounts of silt and nutrients to run off into the rivers that feed the lake, especially along its western and northern watershed areas. This silt fills up the lake; the nutrients encourage the growth of weeds and algae. More important however is the development of floating garden agriculture, largely along the western side of the lake. This practice encroaches into the diminishing area of the lake, since over time, the floating beds become solid ground. About 93% (nearly 21 km²) of the recent loss in open water area of the lake, largely along its western side, is thought to be due to this agricultural practice. Direct environmental impacts associated with these combined agricultural activities within the wetlands and surrounding hills of the lake include sedimentation, eutrophication, and pollution.[4]

 

The water hyacinth, a plant not native to the lake, also poses a major problem. It grows rapidly, filling up the smaller streams and large expanses of the lake, robbing native plants and animals of nutrients and sunlight. At one time, all boats coming into Nyaung Shwe were required to bring in a specified amount of water hyacinth. Over the past twenty years, large-scale use of dredges and pumps has been employed with some success in controlling the growth of this plant. On a smaller scale, public awareness education and small-scale control have also been successful.

 

Another cause for concern is the planned introduction of non-native fish species, such as the Grass Carp (Ctenopharyngodon idella)] intended to improve fishery.

 

Sanitation in the villages around the lake is an ongoing concern for public health authorities, due to untreated sewage (with 72% of households using open pits, not latrines) and waste water flowing into the lake.[5] To ensure fresh and clean water, some villages now have enclosed wells and public access to the well water. Some studies of the lake's surface water quality indicates that the water is not safe for consumption.[5] Water from Inle Lake has dissolved oxygen ranges lower than those necessary for fisheries and aquatic life, while nitrite, nitrate and phosphate ranges are unusually high.[5]

 

Noise pollution is also a noticeable issue. The noise from the cheaper poorly muffled diesel engines driving the stern drive propellers is significant, and can be a distraction to the otherwise tranquil lake.

 

The summer of 2010 registered very high temperatures causing the water level of the lake to drop so low, the lowest in nearly 50 years, that drinking water had to be fetched from elsewhere and the floating market was in danger of disappearing.[6] One other serious consequence was that the hydroelectric plant at Lawpita, where the former capital Yangon received its power supply from, could not operate at its full capacity.[7]

 

In 2015 the United Nations added Inle lake to its World Network Biosphere Reserves. There are a total of 651 sites in 120 countries in this network, but Inle Lake is the first biosphere reserve to be added for Myanmar.[8]

 

Tourism

Inle Lake is a major tourist attraction, and this has led to some development of tourist infrastructure. Many small and large privately owned hotels and tour operations have arisen during the past few years. Local shops are flooded with consumer items, both local and foreign. The nearest airport is Heho Airport which is 35 km away. There are flights from both Yangon and Mandalay. Yangon is 660 km away by road, Mandalay 330 km.

 

A number of festivals occur from August to October on Inle Lake and in the surrounding areas. The ceremonial Hpaung Daw U Festival, which lasts for a total of 18 days, is closely followed by the Thadingyut festival of lights. Inthas and Shan turn out in their best clothes in great numbers to celebrate the Buddhist Lent. Traditional boat racing, with dozens of leg-rowers in traditional Shan dress compete on teams with a team on each boat. These boat races are locally one of the most anticipated affairs during the Hpaung Daw U Festival.[9]

Inle Boat Miniature

 

One of the tourist attractions in the village on the lake itself is the traditional silversmithing, which has fed into the local tourist economy. The silver is brought in from the mines that line the hills surrounding the lake and is boated into the village. Almost all the houses in the village on the lake itself sit on stilts and are made of woven bamboo. Tourists can satisfy their need for trinkets and memorable tokens by observing the silver being smithed and purchase items on-site. If silversmithing doesn't interest a visitor there are also local silk workshops that operate on the lake in a very similar manner as the silversmiths.[10]

Floating farm

 

Hand-made goods for local use and trading are another source of commerce. Typical products include tools, carvings and other ornamental objects, textiles, and cheroots. A local market serves most common shopping needs and is held daily but the location of the event rotates through five different sites around the lake area, thus each of them hosting an itinerant market every fifth day.[11] When held on the lake itself, trading is conducted from small boats. This 'floating-market' event tends to emphasize tourist trade much more than the other four.

 

The Inle lake area is renowned for its weaving industry. The Shan-bags, used daily by many Burmese as a tote-bag, are produced in large quantities here. Silk-weaving is another very important industry, producing high-quality hand-woven silk fabrics of distinctive design called Inle longyi. A unique fabric from the lotus plant fibers is produced only at Inle lake and is used for weaving special robes for Buddha images called kya thingahn (lotus robe).[12]

 

While hot air balloon flights are more popular in Bagan, they are also provided over Inle Lake with Balloons Over Bagan. There is also a winery near the lake, called Red Mountain Estate.[13]

Cuisine

 

Inle cuisine is different from Shan cuisine, as it incorporates local natural produce. The most well-known Inle dish would be the Htamin jin - a rice, tomato and potato or fish salad kneaded into round balls dressed and garnished with crisp fried onion in oil, tamarind sauce, coriander and spring onions often with garlic, Chinese chives roots (ju myit), fried whole dried chili, grilled dried fermented bean cakes (pè bouk) and fried dried tofu (topu jauk kyaw) on the side.

Analeigh

 

This week the girl had to show of their sexy and seductive side while still keeping their high fashion look.

 

Give all the girls a score from 1-10. I appreciate comments and critique to the girls if you want so they know what to improve to next week. You also have to comment on ALL the girls photos to have your scores counted! The girls will get an average score and the girl with the highest score will receive top photo. The 2 girls with the lowest scores will face the bottom 2. From there, I will choose the girl that gets to stay and and which one of them will be going home.

Current estimates of average nodule abundance in four major locations.

 

For any form of publication, please include the link to this page:

www.grida.no/resources/7366

 

This photo has been graciously provided to be used in the GRID-Arendal resources library by: GRID-Arendal

Künstler Sir Tony Cragg, Standort Bonn

Photo Copyright 2012, dynamo.photography.

All rights reserved, no use without license

 

++++++++ from wikipedia.org ++++++++

 

The Alishan National Scenic Area is a mountain resort and natural preserve located in the mountains of Chiayi County in Taiwan.[citation needed]

 

Contents

 

1 Geography

2 Climate

3 Topography

4 Vegetation and wildlife

5 History

6 Attractions and landmarks

7 See also

8 References

9 Bibliography

10 External links

 

Geography

Alishan Forest Park.

Dawn view from Alishan.

 

Alishan is 415 square kilometres (41,500 ha) in area. Notable characteristics include mountain wilderness, four villages, waterfalls, high altitude tea plantations, the Alishan Forest Railway, and a number of hiking trails. The area is popular with tourists and mountain climbers. Alishan, or Mount Ali, itself has become one of the major landmarks associated with Taiwan. The area is famous for its production of high mountain tea and wasabi.[citation needed]

 

Alishan is well known for its sunrises, and on a suitable morning one can observe the sun come up on a sea of clouds in the area between Alishan and Yüshan. Alishan and Sun Moon Lake are two of the best known scenic spots in Asia. The indigenous people of the area, the Thao people, have only recently been recognized as a discrete ethnic group. They have long been confused with the Tsou people.

Climate

 

Alishan National Scenic Area spans a broad range in altitude. Lower elevations, such as in Leye Township, share the same subtropical and tropical climate as the rest of southern Taiwan, while the climate changes to temperate and alpine as the elevation increases. Snow sometimes falls at higher elevations in the winter.[citation needed]

 

Alishan National Scenic Area covers most, but not all, of Alishan Rural Township in Chiayi County, as well as parts of neighboring townships in Taiwan.[citation needed]

 

Average temperatures are moderate:[citation needed]

 

Low elevations: 24 °C in the summer, 16 °C in the winter.

Medium elevations: 19 °C in the summer, 12 °C in the winter.

High elevations: 14 °C in the summer, 5 °C in the winter.

 

Topography

 

Alishan is mountainous:[citation needed]

 

Number of peaks above 2000 meters: 25

Highest point: Da Ta Shan (大塔山), 2,663 meters.

Average height of Alishan Mountain Range: 2,500 meters.

 

Vegetation and wildlife

 

Important trees in the area include:[citation needed]

 

Taiwania cryptomerioides, a large coniferous tree in the cypress family Cupressaceae (the same family as the next three species)

Chamaecyparis formosensis, or Formosan Cypress

Chamaecyparis taiwanensis

Cunninghamia konishii

Pinus taiwanensis, or Taiwan Red Pine

Picea morrisonicola, or Yüshan Spruce

Pseudotsuga sinensis var. wilsoniana, or Taiwan Douglas-fir

Abies kawakamii, a species of conifer in the Pinaceae family, only found in Taiwan

Tsuga chinensis var. formosana, Taiwan or Chinese Hemlock

Ulmus uyematsui, a species of elm only found in the Alishan region

 

History

Longyin Temple of Chukou Village in Alishan National Scenic Area.

Boardwalk at Alishan National Scenic Area.

 

The Alishan area was originally settled by the Tsou tribe of the Taiwanese aborigines; the name derives from the aboriginal word Jarissang. Ethnic Han Chinese settlers first settled on the plains near modern-day Chiayi as early as the late Ming Dynasty (around the mid-17th century), but did not move into the mountains until the late 18th century, establishing the towns of Ruili (瑞里), Ruifeng (瑞峰), Xiding (隙頂), and Fenqihu (奮起湖). The resulting armed clashes between the settlers and the aborigines pushed the aborigines even further into the mountains.[citation needed]

 

Following the cession of Taiwan to Japan at the end of the First Sino-Japanese War, Japanese expeditions to the area found large quantities of cypress (檜木, or hinoki in Japanese). This led to the development of the logging industry in the area and the export of local cypress and Taiwania wood. A series of narrow-gauge railways were built in the area during this time to facilitate the transportation of lumber from the mountains to the plains below, part of which continues to operate as the Alishan Forest Railway. Several new villages also began to sprout up along the railway lines. It was also during this time that the first tourists began to visit the area. Plans were even drawn up to incorporate the area into the new Niitaka (New Highest) Arisan National Park (新高阿里山国立公園).[citation needed]

 

With the exhaustion of forest resources by the 1970s, domestic and international tourism overtook logging to become the primary economic activity in the area. The tourism industry continued to expand with the completion of the Alisan highway in the 1980s, displacing the railroad as the primary mode of transportation up the mountain. To combat the problems associated with the growing crowds of tourists and the expanding tea and wasabi plantations, the area was declared a national scenic area in 2001.[citation needed]

 

On 1 December 2014, fire broke out at Alishan spreading over more than 5 hectares of land. The area affected was located near Tapang No. 3 Bridge. The fire was believed to happen due to dry ground which was vulnerable to fire because of the absence of rain in the area for months.[1]

Attractions and landmarks

A Japanese-built train on the Alishan Forest Railway.

 

Fenqihu (奮起湖) is a small town of low wooden buildings built into the mountainside at 1,400 meters, midpoint of the Alishan Forest Railway. It is famous for natural rock formations, mountain streams, forests, and the ruins of a Shinto temple in the vicinity, as well as for its production of high altitude food products such as bamboo shoots and aiyu jelly (愛玉). The local box lunches (奮起湖便當, Fenqihu bento), which were once sold to passengers on the rail line, are also well known.[citation needed]

 

Taiwan (/ˌtaɪˈwɑːn/ (About this sound listen)), officially the Republic of China (ROC), is a state in East Asia. Its neighbors include China (officially the People's Republic of China, PRC) to the west, Japan to the northeast, and the Philippines to the south. Taiwan is the most populous state that is not a member of the United Nations and the largest economy outside the UN.

 

The island of Taiwan, formerly known as Formosa, was inhabited by Taiwanese aborigines before the 17th century, when Dutch and Spanish colonies opened the island to mass Han immigration. After a brief rule by the Kingdom of Tungning, the island was annexed by the Qing dynasty, the last dynasty of China. The Qing ceded Taiwan to Japan in 1895 after the Sino-Japanese War. While Taiwan was under Japanese rule, the Republic of China (ROC) was established on the mainland in 1912 after the fall of the Qing dynasty. Following the Japanese surrender to the Allies in 1945, the ROC took control of Taiwan. However, the resumption of the Chinese Civil War led to the ROC's loss of the mainland to the Communists, and the flight of the ROC government to Taiwan in 1949. Although the ROC continued to claim to be the legitimate government of China, its effective jurisdiction has since the loss of Hainan in 1950 been limited to Taiwan and its surrounding islands, with the main island making up 99% of its de facto territory. As a founding member of the United Nations, the ROC continued to represent China at the United Nations until 1971, when the PRC assumed China's seat, causing the ROC to lose its UN membership.

 

In the early 1960s, Taiwan entered a period of rapid economic growth and industrialization, creating a stable industrial economy. In the 1980s and early 1990s, it changed from a one-party military dictatorship dominated by the Kuomintang to a multi-party democracy with a semi-presidential system. Taiwan is the 22nd-largest economy in the world, and its high-tech industry plays a key role in the global economy. It is ranked highly in terms of freedom of the press, healthcare,[15] public education, economic freedom, and human development.[d][13][16] The country benefits from a highly skilled workforce and is among the most highly educated countries in the world with one of the highest percentages of its citizens holding a tertiary education degree.[17][18]

 

The PRC has consistently claimed sovereignty over Taiwan and asserted the ROC is no longer in legitimate existence. Under its One-China Policy the PRC refused diplomatic relations with any country that recognizes the ROC. Today 20 countries recognize the ROC as the sole legal representative of China,[19] but many other states maintain unofficial ties through representative offices and institutions that function as de facto embassies and consulates. Although Taiwan is fully self-governing, most international organizations in which the PRC participates either refuse to grant membership to Taiwan or allow it to participate only as a non-state actor. Internally, the major division in politics is between the aspirations of eventual Chinese unification or Taiwanese independence, though both sides have moderated their positions to broaden their appeal. The PRC has threatened the use of military force in response to any formal declaration of independence by Taiwan or if PRC leaders decide that peaceful unification is no longer possible.[20]

 

Contents

 

1 Etymology

2 History

2.1 Prehistoric Taiwan

2.2 Opening in the 17th century

2.3 Qing rule

2.4 Japanese rule

2.5 After World War II

2.6 Chinese Nationalist one-party rule

2.7 Democratization

3 Geography

3.1 Climate

3.2 Geology

4 Political and legal status

4.1 Relations with the PRC

4.2 Foreign relations

4.3 Participation in international events and organizations

4.4 Opinions within Taiwan

5 Government and politics

5.1 Major camps

5.2 Current political issues

5.3 National identity

6 Military

7 Administrative divisions

8 Economy and industry

9 Transportation

10 Education, research, and academia

11 Demographics

11.1 Ethnic groups

11.2 Languages

11.3 Religion

11.4 Largest cities

12 Public health

13 Culture

13.1 Sports

13.2 Calendar

14 See also

15 Notes

16 References

16.1 Citations

16.2 Works cited

17 Further reading

18 External links

18.1 Overviews and data

18.2 Government agencies

 

Etymology

See also: Chinese Taipei, Formosa, and Names of China

Taiwan

Taiwan (Chinese characters).svg

"Taiwan" in Traditional (top) and Simplified (bottom) Chinese characters

Chinese name

Traditional Chinese 臺灣 or 台灣

Simplified Chinese 台湾

Transcriptions

Standard Mandarin

Hanyu Pinyin Táiwān

Bopomofo ㄊㄞˊ ㄨㄢ

Gwoyeu Romatzyh Tair'uan

Wade–Giles T'ai²-wan¹

Tongyong Pinyin Táiwan

IPA [tʰǎi.wán]

other Mandarin

Xiao'erjing تَاَىْوًا‎

Wu

Romanization The平-uae平

Xiang

IPA dwɛ13 ua44

Hakka

Romanization Thòi-vàn

Yue: Cantonese

Yale Romanization Tòiwāan

Jyutping Toi4waan1

Southern Min

Hokkien POJ Tâi-oân

Tâi-lô Tâi-uân

Eastern Min

Fuzhou BUC Dài-uăng

China

Traditional Chinese 中國

Simplified Chinese 中国

Literal meaning Middle or Central State[21]

Transcriptions

Standard Mandarin

Hanyu Pinyin Zhōngguó

Bopomofo ㄓㄨㄥ ㄍㄨㄛˊ

Gwoyeu Romatzyh Jong'gwo

Wade–Giles Chung1-kuo2

Tongyong Pinyin Jhongguó

MPS2 Jūng-guó

IPA [ʈʂʊ́ŋ.kwǒ]

other Mandarin

Xiao'erjing ﺟْﻮﻗُﻮَع

Sichuanese Pinyin Zong1 gwe2

Wu

Romanization Tson平-koh入

Gan

Romanization Tung-koe̍t

Xiang

IPA Tan33-kwɛ24/

Hakka

Romanization Dung24-gued2

Yue: Cantonese

Yale Romanization Jūnggwok

Jyutping Zung1gwok3

Southern Min

Hokkien POJ Tiong-kok

Eastern Min

Fuzhou BUC Dṳ̆ng-guók

Pu-Xian Min

Hinghwa BUC De̤ng-go̤h

Northern Min

Jian'ou Romanized Dô̤ng-gŏ

Republic of China

Traditional Chinese 中華民國

Simplified Chinese 中华民国

Postal Chunghwa Minkuo

Transcriptions

Standard Mandarin

Hanyu Pinyin Zhōnghuá Mínguó

Bopomofo ㄓㄨㄥ ㄏㄨㄚˊ ㄇㄧㄣˊ ㄍㄨㄛˊ

Gwoyeu Romatzyh Jonghwa Min'gwo

Wade–Giles Chung¹-hua² Min²-kuo²

Tongyong Pinyin Jhonghuá Mínguó

MPS2 Jūng-huá Mín-guó

IPA [ʈʂʊ́ŋxwǎ mǐnkwǒ]

other Mandarin

Xiao'erjing ﺟْﻮ ﺧُﻮَ مٍ ﻗُﻮَع

Wu

Romanization tson平 gho平 min平 koh入

Gan

Romanization tung1 fa4 min4 koet7

Hakka

Romanization Chûng-fà Mìn-koet

Yue: Cantonese

Yale Romanization Jūngwà màn'gwok

Jyutping Zung1waa4 man4gwok3

Southern Min

Hokkien POJ Tiong-hôa Bîn-kok

Tâi-lô Tiong-hûa Bîn-kok

Eastern Min

Fuzhou BUC Dṳ̆ng-huà Mìng-guók

Japanese name

Kanji 台湾

Kana たいわん

Kyūjitai 臺灣

Transcriptions

Romanization Taiwan

 

There are various names for the island of Taiwan in use today, derived from explorers or rulers by each particular period. The former name Formosa (福爾摩沙) dates from 1542,[verification needed] when Portuguese sailors sighted the main island of Taiwan and named it Ilha Formosa, which means "beautiful island".[22] The name "Formosa" eventually "replaced all others in European literature"[23] and was in common use in English in the early 20th century.[24]

 

In the early 17th century, the Dutch East India Company established a commercial post at Fort Zeelandia (modern-day Anping, Tainan) on a coastal sandbar called "Tayouan",[25] after their ethnonym for a nearby Taiwanese aboriginal tribe, written by the Dutch and Portuguese variously as Taiouwang, Tayowan, Teijoan, etc.[26] This name was also adopted into the Chinese vernacular (in particular, Hokkien, as Pe̍h-ōe-jī: Tāi-oân/Tâi-oân) as the name of the sandbar and nearby area (Tainan). The modern word "Taiwan" is derived from this usage, which is seen in various forms (大員, 大圓, 大灣, 臺員, 臺圓 and 臺窩灣) in Chinese historical records. The area of modern-day Tainan was the first permanent settlement by Western colonists and Chinese immigrants, grew to be the most important trading centre, and served as the capital of the island until 1887. Use of the current Chinese name (臺灣) was formalized as early as 1684 with the establishment of Taiwan Prefecture. Through its rapid development, the entire Formosan mainland eventually became known as "Taiwan".[27][28][29][30]

 

In his Daoyi Zhilüe (1349), Wang Dayuan used "Liuqiu" as a name for the island of Taiwan, or the part of it near to Penghu.[31] Elsewhere, the name was used for the Ryukyu Islands in general or Okinawa, the largest of them; indeed the name Ryūkyū is the Japanese form of Liúqiú. The name also appears in the Book of Sui (636) and other early works, but scholars cannot agree on whether these references are to the Ryukyus, Taiwan or even Luzon.[32]

 

The official name of the state is the "Republic of China"; it has also been known under various names throughout its existence. Shortly after the ROC's establishment in 1912, while it was still located on the Chinese mainland, the government used the short form "China" Zhōngguó (中國), to refer to itself, which derives from zhōng ("central" or "middle") and guó ("state, nation-state"), [e] A term which also developed under the Zhou Dynasty in reference to its royal demesne[f] and the name was then applied to the area around Luoyi (present-day Luoyang) during the Eastern Zhou and then to China's Central Plain before being used as an occasional synonym for the state under the Qingera .[34] During the 1950s and 1960s, after the government had fled to Taiwan due to losing the Chinese Civil War, it was commonly referred to as "Nationalist China" (or "Free China") to differentiate it from "Communist China" (or "Red China").[36] It was a member of the United Nations representing "China" until 1971, when it lost its seat to the People's Republic of China. Over subsequent decades, the Republic of China has become commonly known as "Taiwan", after the island that comprises 99% of the territory under its control. In some contexts, especially official ones from the ROC government, the name is written as "Republic of China (Taiwan)", "Republic of China/Taiwan", or sometimes "Taiwan (ROC)."[37] The Republic of China participates in most international forums and organizations under the name "Chinese Taipei" due to diplomatic pressure from the People's Republic of China. For instance, it is the name under which it has competed at the Olympic Games since 1984, and its name as an observer at the World Health Organization.[38]

History

Main articles: History of Taiwan and History of the Republic of China

See the History of China article for historical information in the Chinese Mainland before 1949.

Prehistoric Taiwan

Main article: Prehistory of Taiwan

A young Tsou man

 

Taiwan was joined to the mainland in the Late Pleistocene, until sea levels rose about 10,000 years ago. Fragmentary human remains dated 20,000 to 30,000 years ago have been found on the island, as well as later artefacts of a Paleolithic culture.[39][40][41]

 

Around 6,000 years ago, Taiwan was settled by farmers, most likely from mainland China.[42] They are believed to be the ancestors of today's Taiwanese aborigines, whose languages belong to the Austronesian language family, but show much greater diversity than the rest of the family, which spans a huge area from Maritime Southeast Asia west to Madagascar and east as far as New Zealand, Hawaii and Easter Island. This has led linguists to propose Taiwan as the urheimat of the family, from which seafaring peoples dispersed across Southeast Asia and the Pacific and Indian Oceans.[43][44]

 

Han Chinese fishermen began settling in the Penghu islands in the 13th century, but Taiwan's hostile tribes and its lack of valuable trade products meant that few outsiders visited the island until the 16th century, when visits to the coast by fishermen from Fujian and Chinese and Japanese pirates became more frequent.[45]

Opening in the 17th century

Main articles: Dutch Formosa, Spanish Formosa, and Kingdom of Tungning

Fort Zeelandia, the Governor's residence in Dutch Formosa

 

The Dutch East India Company attempted to establish a trading outpost on the Penghu Islands (Pescadores) in 1622, but were militarily defeated and driven off by the Ming authorities.[46]

 

In 1624, the company established a stronghold called Fort Zeelandia on the coastal islet of Tayouan, which is now part of the main island at Anping, Tainan.[30] David Wright, a Scottish agent of the company who lived on the island in the 1650s, described the lowland areas of the island as being divided among 11 chiefdoms ranging in size from two settlements to 72. Some of these fell under Dutch control, while others remained independent.[30][47] The Company began to import labourers from Fujian and Penghu (Pescadores), many of whom settled.[46]

 

In 1626, the Spanish Empire landed on and occupied northern Taiwan, at the ports of Keelung and Tamsui, as a base to extend their trading. This colonial period lasted 16 years until 1642, when the last Spanish fortress fell to Dutch forces.

 

Following the fall of the Ming dynasty, Koxinga (Zheng Chenggong), a self-styled Ming loyalist, arrived on the island and captured Fort Zeelandia in 1662, expelling the Dutch Empire and military from the island. Koxinga established the Kingdom of Tungning (1662–1683), with his capital at Tainan. He and his heirs, Zheng Jing, who ruled from 1662 to 1682, and Zheng Keshuang, who ruled less than a year, continued to launch raids on the southeast coast of mainland China well into the Qing dynasty era.[46]

Qing rule

Main article: Taiwan under Qing Dynasty rule

Hunting deer, painted in 1746

 

In 1683, following the defeat of Koxinga's grandson by an armada led by Admiral Shi Lang of southern Fujian, the Qing dynasty formally annexed Taiwan, placing it under the jurisdiction of Fujian province. The Qing imperial government tried to reduce piracy and vagrancy in the area, issuing a series of edicts to manage immigration and respect aboriginal land rights. Immigrants mostly from southern Fujian continued to enter Taiwan. The border between taxpaying lands and "savage" lands shifted eastward, with some aborigines becoming sinicized while others retreated into the mountains. During this time, there were a number of conflicts between groups of Han Chinese from different regions of southern Fujian, particularly between those from Quanzhou and Zhangzhou, and between southern Fujian Chinese and aborigines.

 

Northern Taiwan and the Penghu Islands were the scene of subsidiary campaigns in the Sino-French War (August 1884 to April 1885). The French occupied Keelung on 1 October 1884, but were repulsed from Tamsui a few days later. The French won some tactical victories but were unable to exploit them, and the Keelung Campaign ended in stalemate. The Pescadores Campaign, beginning on 31 March 1885, was a French victory, but had no long-term consequences. The French evacuated both Keelung and the Penghu archipelago after the end of the war.

 

In 1887, the Qing upgraded the island's administration from Taiwan Prefecture of Fujian to Fujian-Taiwan-Province (福建臺灣省), the twentieth in the empire, with its capital at Taipei. This was accompanied by a modernization drive that included building China's first railroad.[48]

Japanese rule

Main articles: Taiwan under Japanese rule and Republic of Formosa

Japanese colonial soldiers march Taiwanese captured after the Tapani Incident from the Tainan jail to court, 1915.

 

As the Qing dynasty was defeated in the First Sino-Japanese War (1894–1895), Taiwan, along with Penghu and Liaodong Peninsula, were ceded in full sovereignty to the Empire of Japan by the Treaty of Shimonoseki. Inhabitants on Taiwan and Penghu wishing to remain Qing subjects were given a two-year grace period to sell their property and move to mainland China. Very few Taiwanese saw this as feasible.[49] On 25 May 1895, a group of pro-Qing high officials proclaimed the Republic of Formosa to resist impending Japanese rule. Japanese forces entered the capital at Tainan and quelled this resistance on 21 October 1895.[50] Guerrilla fighting continued periodically until about 1902 and ultimately took the lives of 14,000 Taiwanese, or 0.5% of the population.[51] Several subsequent rebellions against the Japanese (the Beipu uprising of 1907, the Tapani incident of 1915, and the Musha incident of 1930) were all unsuccessful but demonstrated opposition to Japanese colonial rule.

 

Japanese colonial rule was instrumental in the industrialization of the island, extending the railroads and other transportation networks, building an extensive sanitation system, and establishing a formal education system.[52] Japanese rule ended the practice of headhunting.[53] During this period the human and natural resources of Taiwan were used to aid the development of Japan and the production of cash crops such as rice and sugar greatly increased. By 1939, Taiwan was the seventh greatest sugar producer in the world.[54] Still, the Taiwanese and aborigines were classified as second- and third-class citizens. After suppressing Chinese guerrillas in the first decade of their rule, Japanese authorities engaged in a series of bloody campaigns against the mountain aboriginals, culminating in the Musha Incident of 1930.[55] Also, those intellectual and labours who participated in left-wing movement of Taiwan were arrested and massacred (e.g. Tsiúnn Uī-Suí(蔣渭水), masanosuke watanabe(渡辺政之辅)).[56]

 

Around 1935, the Japanese began an island-wide assimilation project to bind the island more firmly to the Japanese Empire and people were taught to see themselves as Japanese under the Kominka Movement, during which time Taiwanese culture and religion were outlawed and the citizens were encouraged to adopt Japanese surnames.[57] The "South Strike Group" was based at the Taihoku Imperial University in Taipei. During World War II, tens of thousands of Taiwanese served in the Japanese military.[58] For example, former ROC President Lee Teng-hui's elder brother served in the Japanese navy and was killed in action in the Philippines in February 1945. The Imperial Japanese Navy operated heavily out of Taiwanese ports. In October 1944, the Formosa Air Battle was fought between American carriers and Japanese forces based in Taiwan. Important Japanese military bases and industrial centres throughout Taiwan, like Kaohsiung, were targets of heavy American bombings.[59] Also during this time, over 2,000 women were forced into sexual slavery for Imperial Japanese troops, now euphemistically called "comfort women."[60]

 

In 1938, there were 309,000 Japanese settlers in Taiwan.[61] After World War II, most of the Japanese were expelled and sent to Japan.[62]

After World War II

Main article: Taiwan after World War II

General Chen Yi (right) accepting the receipt of General Order No. 1 from Rikichi Andō (left), the last Japanese Governor-General of Taiwan, in Taipei City Hall

 

On 25 October 1945, the US Navy ferried ROC troops to Taiwan in order to accept the formal surrender of Japanese military forces in Taipei on behalf of the Allied Powers, as part of General Order No. 1 for temporary military occupation. General Rikichi Andō, governor-general of Taiwan and commander-in-chief of all Japanese forces on the island, signed the receipt and handed it over to General Chen Yi of the ROC military to complete the official turnover. Chen Yi proclaimed that day to be "Taiwan Retrocession Day", but the Allies considered Taiwan and the Penghu Islands to be under military occupation and still under Japanese sovereignty until 1952, when the Treaty of San Francisco took effect.[63][64] Although the 1943 Cairo Declaration had envisaged returning these territories to China, in the Treaty of San Francisco and Treaty of Taipei Japan has renounced all claim to them without specifying to what country they were to be surrendered. This introduced the problem of the legal status of Taiwan.

 

The ROC administration of Taiwan under Chen Yi was strained by increasing tensions between Taiwanese-born people and newly arrived mainlanders, which were compounded by economic woes, such as hyperinflation. Furthermore, cultural and linguistic conflicts between the two groups quickly led to the loss of popular support for the new government, while the mass movement led by the working committee of the communist also aimed to bring down the Kuomintang government.[65][66] The shooting of a civilian on 28 February 1947 triggered island-wide unrest, which was suppressed with military force in what is now called the February 28 Incident. Mainstream estimates of the number killed range from 18,000 to 30,000. Those killed were mainly members of the Taiwanese elite.[67][68]

Chinese Nationalist one-party rule

Main articles: Chinese Civil War, Chinese Communist Revolution, and History of the Republic of China § Republic of China on Taiwan (1949–present)

For the history of Republic of China before 1949, see Republic of China (1912–49).

The Nationalists' retreat to Taipei: after the Nationalists lost Nanjing (Nanking) they next moved to Guangzhou (Canton), then to Chongqing (Chungking), Chengdu (Chengtu) and Xichang (Sichang) before arriving in Taipei.

 

After the end of World War II, the Chinese Civil War resumed between the Chinese Nationalists (Kuomintang), led by Chiang Kai-shek, and the Communist Party of China, led by Mao Zedong. Throughout the months of 1949, a series of Chinese Communist offensives led to the capture of its capital Nanjing on 23 April and the subsequent defeat of the Nationalist army on the mainland, and the Communists founded the People's Republic of China on 1 October.[69]

 

On 7 December 1949, after the loss of four capitals, Chiang evacuated his Nationalist government to Taiwan and made Taipei the temporary capital of the ROC (also called the "wartime capital" by Chiang Kai-shek).[70] Some 2 million people, consisting mainly of soldiers, members of the ruling Kuomintang and intellectual and business elites, were evacuated from mainland China to Taiwan at that time, adding to the earlier population of approximately six million. In addition, the ROC government took to Taipei many national treasures and much of China's gold reserves and foreign currency reserves.[71][72][73]

 

After losing most of the mainland, the Kuomintang held remaining control of Tibet, the portions of Qinghai, Xinjiang, and Yunnan provinces along with the Hainan Island until 1951 before the Communists subsequently captured both territories. From this point onwards, the Kuomintang's territory was reduced to Taiwan, Penghu, the portions of the Fujian province (Kinmen and Matsu Islands), and two major islands of Dongsha Islands and Nansha Islands. The Kuomintang continued to claim sovereignty over all "China", which it defined to include mainland China, Taiwan, Outer Mongolia and other areas. On mainland China, the victorious Communists claimed they ruled the sole and only China (which they claimed included Taiwan) and that the Republic of China no longer existed.[74]

A Chinese man in military uniform, smiling and looking towards the left. He holds a sword in his left hand and has a medal in shape of a sun on his chest.

Chiang Kai-shek, leader of the Kuomintang from 1925 until his death in 1975

 

Martial law, declared on Taiwan in May 1949,[75] continued to be in effect after the central government relocated to Taiwan. It was not repealed until 1987,[75] and was used as a way to suppress the political opposition in the intervening years.[76] During the White Terror, as the period is known, 140,000 people were imprisoned or executed for being perceived as anti-KMT or pro-Communist.[77] Many citizens were arrested, tortured, imprisoned and executed for their real or perceived link to the Communists. Since these people were mainly from the intellectual and social elite, an entire generation of political and social leaders was decimated. In 1998 law was passed to create the "Compensation Foundation for Improper Verdicts" which oversaw compensation to White Terror victims and families. President Ma Ying-jeou made an official apology in 2008, expressing hope that there will never be a tragedy similar to White Terror.[78]

 

Initially, the United States abandoned the KMT and expected that Taiwan would fall to the Communists. However, in 1950 the conflict between North Korea and South Korea, which had been ongoing since the Japanese withdrawal in 1945, escalated into full-blown war, and in the context of the Cold War, US President Harry S. Truman intervened again and dispatched the US Navy's 7th Fleet into the Taiwan Strait to prevent hostilities between Taiwan and mainland China.[79] In the Treaty of San Francisco and the Treaty of Taipei, which came into force respectively on 28 April 1952 and 5 August 1952, Japan formally renounced all right, claim and title to Taiwan and Penghu, and renounced all treaties signed with China before 1942. Neither treaty specified to whom sovereignty over the islands should be transferred, because the United States and the United Kingdom disagreed on whether the ROC or the PRC was the legitimate government of China.[80] Continuing conflict of the Chinese Civil War through the 1950s, and intervention by the United States notably resulted in legislation such as the Sino-American Mutual Defense Treaty and the Formosa Resolution of 1955.

With President Chiang Kai-shek, the US President Dwight D. Eisenhower waved to crowds during his visit to Taipei in June 1960.

 

As the Chinese Civil War continued without truce, the government built up military fortifications throughout Taiwan. Within this effort, KMT veterans built the now famous Central Cross-Island Highway through the Taroko Gorge in the 1950s. The two sides would continue to engage in sporadic military clashes with seldom publicized details well into the 1960s on the China coastal islands with an unknown number of night raids. During the Second Taiwan Strait Crisis in September 1958, Taiwan's landscape saw Nike-Hercules missile batteries added, with the formation of the 1st Missile Battalion Chinese Army that would not be deactivated until 1997. Newer generations of missile batteries have since replaced the Nike Hercules systems throughout the island.

 

During the 1960s and 1970s, the ROC maintained an authoritarian, single-party government while its economy became industrialized and technology oriented. This rapid economic growth, known as the Taiwan Miracle, was the result of a fiscal regime independent from mainland China and backed up, among others, by the support of US funds and demand for Taiwanese products.[81][82] In the 1970s, Taiwan was economically the second fastest growing state in Asia after Japan.[83] Taiwan, along with Hong Kong, South Korea and Singapore, became known as one of the Four Asian Tigers. Because of the Cold War, most Western nations and the United Nations regarded the ROC as the sole legitimate government of China until the 1970s. Later, especially after the termination of the Sino-American Mutual Defense Treaty, most nations switched diplomatic recognition to the PRC (see United Nations General Assembly Resolution 2758).

 

Up until the 1970s, the government was regarded by Western critics as undemocratic for upholding martial law, for severely repressing any political opposition and for controlling media. The KMT did not allow the creation of new parties and those that existed did not seriously compete with the KMT. Thus, competitive democratic elections did not exist.[84][85][86][87][88] From the late 1970s to the 1990s, however, Taiwan went through reforms and social changes that transformed it from an authoritarian state to a democracy. In 1979, a pro-democracy protest known as the Kaohsiung Incident took place in Kaohsiung to celebrate Human Rights Day. Although the protest was rapidly crushed by the authorities, it is today considered as the main event that united Taiwan's opposition.[89]

Democratization

Main articles: Democratic reforms of Taiwan and Elections in Taiwan

 

Chiang Ching-kuo, Chiang Kai-shek's son and successor as the president, began to liberalize the political system in the mid-1980s. In 1984, the younger Chiang selected Lee Teng-hui, a Taiwanese-born, US-educated technocrat, to be his vice-president. In 1986, the Democratic Progressive Party (DPP) was formed and inaugurated as the first opposition party in the ROC to counter the KMT. A year later, Chiang Ching-kuo lifted martial law on the main island of Taiwan (martial law was lifted on Penghu in 1979, Matsu island in 1992 and Kinmen island in 1993). With the advent of democratization, the issue of the political status of Taiwan gradually resurfaced as a controversial issue where, previously, the discussion of anything other than unification under the ROC was taboo.

 

After the death of Chiang Ching-kuo in January 1988, Lee Teng-hui succeeded him as president. Lee continued to democratize the government and decrease the concentration of government authority in the hands of mainland Chinese. Under Lee, Taiwan underwent a process of localization in which Taiwanese culture and history were promoted over a pan-China viewpoint in contrast to earlier KMT policies which had promoted a Chinese identity. Lee's reforms included printing banknotes from the Central Bank rather than the Provincial Bank of Taiwan, and streamlining the Taiwan Provincial Government with most of its functions transferred to the Executive Yuan. Under Lee, the original members of the Legislative Yuan and National Assembly(a former supreme legislative body defunct in 2005）,[90] elected in 1947 to represent mainland Chinese constituencies and having held the seats without re-election for more than four decades, were forced to resign in 1991. The previously nominal representation in the Legislative Yuan was brought to an end, reflecting the reality that the ROC had no jurisdiction over mainland China, and vice versa. Restrictions on the use of Taiwanese Hokkien in the broadcast media and in schools were also lifted.[citation needed]

US Secretary of State Hillary Clinton and Taiwan's special envoy to the APEC summit, Lien Chan, November 2011

 

Democratic reforms continued in the 1990s, with Lee Teng-hui re-elected in 1996, in the first direct presidential election in the history of the ROC.[91] During the later years of Lee's administration, he was involved in corruption controversies relating to government release of land and weapons purchase, although no legal proceedings commenced. In 1997,"To meet the requisites of the nation prior to national unification",[92] the Additional Articles of the Constitution of the Republic of China was passed and then the former "constitution of five powers" turns to be more tripartite. In 2000, Chen Shui-bian of the Democratic Progressive Party was elected as the first non-Kuomintang (KMT) President and was re-elected to serve his second and last term since 2004. Polarized politics has emerged in Taiwan with the formation of the Pan-Blue Coalition of parties led by the KMT, favouring eventual Chinese reunification, and the Pan-Green Coalition of parties led by the DPP, favouring an eventual and official declaration of Taiwanese independence.[93][clarification needed] In early 2006, President Chen Shui-bian remarked: “The National Unification Council will cease to function. No budget will be ear-marked for it and its personnel must return to their original posts...The National Unification Guidelines will cease to apply."[94]

The ruling DPP has traditionally leaned in favour of Taiwan independence and rejects the so-called "One-China policy".

 

On 30 September 2007, the ruling DPP approved a resolution asserting a separate identity from China and called for the enactment of a new constitution for a "normal country". It also called for general use of "Taiwan" as the country's name, without abolishing its formal name, the Republic of China.[95] The Chen administration also pushed for referendums on national defence and UN entry in the 2004 and 2008 elections, which failed due to voter turnout below the required legal threshold of 50% of all registered voters.[96] The Chen administration was dogged by public concerns over reduced economic growth, legislative gridlock due to a pan-blue, opposition-controlled Legislative Yuan and corruption involving the First Family as well as government officials.[97][98]

 

The KMT increased its majority in the Legislative Yuan in the January 2008 legislative elections, while its nominee Ma Ying-jeou went on to win the presidency in March of the same year, campaigning on a platform of increased economic growth and better ties with the PRC under a policy of "mutual nondenial".[96] Ma took office on 20 May 2008, the same day that President Chen Shui-bian stepped down and was notified by prosecutors of possible corruption charges. Part of the rationale for campaigning for closer economic ties with the PRC stems from the strong economic growth China attained since joining the World Trade Organization. However, some analysts say that despite the election of Ma Ying-jeou, the diplomatic and military tensions with the PRC have not been reduced.[99]

Please take a large view!

 

Niagara Falls

 

Niagara Falls is a set of massive waterfalls located on the Niagara River in eastern North America, on the border between the United States and Canada. Niagara Falls (French: les Chutes du Niagara) comprises three separate waterfalls: the Horseshoe Falls (sometimes called the Canadian Falls), the American Falls, and the smaller, adjacent Bridal Veil Falls. While not exceptionally high, Niagara Falls is very wide. With more than 6 million cubic feet (168,000 m³) of water falling over the crestline every minute in high flow, and almost 4 million cubic feet (110,000 m³) on average, it is the most powerful waterfall in North America

 

Geographically, Niagara Falls is located about Twenty (20) minutes away from the U.S. city of Buffalo and about an hour and a half (90 Minutes) away from the Canadian city of Toronto.

 

Some sources erroneously quote that the Niagara River has an average flow of about 12 million cubic feet per minute (200,000 cu ft/s) or even slightly more. This figure is derived from the average rate of flow (202,000 cu ft/s) of the Niagara River. This volume would pass over the falls if there were no hydroelectric water diversion upstream from the falls; however, water is diverted continuously from Niagara and this figure is approximately three times the actual average flow volume over the falls.

 

Niagara Falls is renowned for its beauty, and is both a valuable source of hydroelectric power and a challenging project for environmental preservation. A popular tourist site for over a century, the natural wonder is shared between the twin cities of Niagara Falls, Ontario and Niagara Falls, New York.

  

From Wikipedia, the free encyclopedia

Ring-tailed lemurs are threatened, largely because the sparse, dry forests they love are quickly vanishing.

 

Average life span in the wild: up to 18 years

 

Ring-tailed lemurs live in groups known as troops. These groups may include 6 to 30 animals, but average about 17. Both sexes live in troops, but a dominant female presides over all.

 

Ring-tailed lemurs have powerful scent glands and use their unique odor as a communication tool and even as a kind of weapon. Lemurs mark their territory by scent, serving notice of their presence to all who can smell. During mating season, male lemurs battle for dominance by trying to outstink each other. They cover their long tails with smelly secretions and wave them in the air to determine which animal is more powerful.

 

Lemurs use their hands and feet to move nimbly through the trees, but cannot grip with their tails as some of their primate cousins do. Ring-tailed lemurs also spend a lot of time on the ground, which is unusual among lemur species. They forage for fruit, which makes up the greater part of their diet, but also eat leaves, flowers, tree bark, and sap.

Medium size tree averaging a height of 20-30 Feet...Similar to the Japanese Maple but the Canopy is more roundly developed

RBG Kew. London. England. U.K.

After transitioning off the Jacob's Ladder Trestle, Mt. Washington Cog Railway trains tackle this stretch of track, known as "Long Trestle", with an average grade of 25%....which is damn steep! The trestle is not named for someone named Long, but is so-named purely because of its length. This structure affords the passengers an awesome view of the 1900 ft. deep Burt Ravine on the left side of the train. Folks who are squeamish about heights might want to avoid sitting on the left side here, as it's a pretty steep drop-off. A quick look to the right reveals that we're pretty much reaching the tree line here. This is the last of the Krummholtz. From here on up, this mountain is nothing but grass and granite. There is a reason it is called "The Rockpile."

 

In this image, you can see the results of the recent re-railing effort undertaken by the railway. For over 100 years, the rails used here were 25 lb. light rail, spiked to support timbers (called "side pieces"), which sat on top of the ties. The side pieces were necessary to build the rail up to the height of the cog rack, which also sits on similar support timbers (called "center pieces.") Needless to say, the additional lumber supporting the rails was a constant maintenance headache. The light rail also made for a rougher ride and was never designed to handle the heavy diesel hydraulic locomotives in use now, or the increased train traffic. To improve the situation, the railway has replaced all of the 25 lb. rail with 100 lb. rail, which is tall enough to no longer require the side pieces. The track is now more robust and the ride is smoother. The cog rack still sits on support timbers, but unlike the rails, it has to be replaced periodically, as it does wear out, so the wood is replaced when this happens. Why was the cog rack elevated to begin with? Mainly because the gearing for the cog wheels on the steam locomotives hangs below the level of the wheels which ride on the rails, so both the rails and the cog rack needed to be tall enough to allow the gears to clear the cross-ties. Got all of that?

Our average rainfall for one year is 11 inches. That shows you that any rain is a big deal in Southern California who is coming out of a years long drought.

 

Last year we got only 8 inches for the whole year and I think this current round of showers will match that. We have a test at our house: if the wall gets all the way wet it really rained, not showered. As you can see, this current rain hasn't quite made the test yet but we have promises of several more days of off and on showers.

 

You can see Hyacinth, Gemma and Julian, the mango bench (my mistake - TOO bright) and the succulent in the left front that started 2 inches high and burst its pot long ago and keeps growing.

Round trip tickets are just $2.50. A far cry from tourists attractions in Chicago. I like the fact that the average Joe can see the city like this without having to own / rent a dwelling that's priced out of reach. Yea cool view.

 

Originally steam powered, the Duquesne Incline was built to carry cargo up and down Mt. Washington in the late 19th century. It later carried passengers, particularly Mt. Washington residents who were tired of walking up footpaths to the top. Inclines were then being built all over Mt. Washington. But as more roads were built on “Coal Hill” most of the other inclines were closed. By the end of the 1960s, only the Monongahela Incline and the Duquesne Incline remained.

 

In 1962, the incline was closed, apparently for good. Major repairs were needed, and with so few patrons, the incline's private owners did little. But local Duquesne Heights residents launched a fund-raiser to help the incline. It was a huge success, and on July 1, 1963, the incline reopened under the auspices of a non-profit organization dedicated to its preservation.

 

The incline has since been totally refurbished. The cars, built by the J. G. Brill and Company of Philadelphia, have been stripped of paint to reveal the original wood. An observation deck was added at the top affording a view of Pittsburgh's "Golden Triangle", and the Duquesne Incline is now one of the city's most popular tourist attractions.

 

*Source: Wikipedia en.wikipedia.org/wiki/Duquesne_Incline

The magnetic motor will be cheaper than a standard motor to make, as the rotor and stator assemblies can be set into plastic housings, due to the fact that the system creates very little heat. Further, with the motor's energy efficiency, it will be well suited for any application where a motor has limited energy to drive it. While development is still focused on replacing existing devices, Minato says that his motor has sufficient torque to power a vehicle. With the help of magnetic propulsion, it is feasible to attach a generator to the motor and produce more electric power than was put into the device. Minato says that average efficiency on his motors is about 330 percent.

 

Mention of Over Unity devices in many scientific circles will draw icy skepticism. But if you can accept the idea that Minato's device is able to create motion and torque through its unique, sustainable permanent magnet propulsion system, then it makes sense that he is able to get more out of the unit than he puts in in terms of elctrical power. Indeed, if the device can produce a surplus of power for longer periods, every household in the land will want one.

 

"I am not in this for the money," Minato says. "I have done well in my musical career, but I want to make a contribution to society -- helping the backstreet manufacturers here in Japan and elsewhere. I want to reverse the trends caused by major multinationals. There is a place for corporations. But as the oil industry has taught us, energy is one area where a breakthrough invention like this cannot be trusted to large companies."

 

Minato was once close to making a deal with Enron. But today, he is firmly on a mission to support the small and the independent -- and to go worldwide with them and his amazing machine. "Our plan is to rally smaller companies and pool their talent, and to one day produce the technology across a wide range of fields."

 

When we first got the call from an excited colleague that he'd just seen the most amazing invention -- a magnetic motor that consumed almost no electricity -- we were so skeptical that we declined an invitation to go see it. If the technology was so good, we thought, how come they didn't have any customers yet?

We forgot about the invitation and the company until several months later, when our friend called again. "OK," he said. "They've just sold 40,000 units to a major convenience store chain. Now will you see it?" In Japan, no one pays for 40,000 convenience store cooling fans without being reasonably sure that they are going to work.

 

The Maestro ~

 

The streets of east Shinjuku are littered with the tailings of the many small factories and workshops still located there -- hardly one's image of the headquarters of a world-class technology company. But this is where we are first greeted outside Kohei Minato's workshop by Nobue Minato, the wife of the inventor and co-director of the family firm. The workshop itself is like a Hollywood set of an inventor's garage. Electrical machines, wires, measuring instruments and batteries are strewn everywhere. Along the diagram-covered walls are drill presses, racks of spare coils, Perspex plating and other paraphernalia. And seated in the back, head bowed in thought, is the 58-year-old techno maestro himself. Minato is no newcomer to the limelight. In fact, he has been an entertainer for most of his life, making music and producing his daughter's singing career in the US. He posseses an oversized presence, with a booming voice and a long ponytail. In short, you can easily imagine him onstage or in a convertible cruising down the coast of California -- not hunched over a mass of wires and coils in Tokyo's cramped backstreets. Joining us are a middle-aged banker and his entourage from Osaka and accounting and finance consultant Yukio Funai. The banker is doing a quick review for an investment, while the rest of us just want to see if Minato's magnetic motors really work. A prototype car air conditioner cooler sitting on a bench looks like it would fit into a Toyota Corolla and quickly catches our attention. Seeing is Believing ~

Nobue then takes us through the functions and operations of each of the machines, starting off with a simple explanation of the laws of magnetism and repulsion. She demonstrates the "Minato Wheel" by kicking a magnet-lined rotor into action with a magnetic wand. Looking carefully at the rotor, we see that it has over 16 magnets embedded on a slant -- apparently to make Minato's machines work, the positioning and angle of the magnets is critical. After she kicks the wheel into life, it keeps spinning, proving at least that the design doesn't suffer from magnetic lockup. She then moves us to the next device, a weighty machine connected to a tiny battery. Apparently the load on the machine is a 35kg rotor, which could easily be used in a washing machine. After she flicks the switch, the huge rotor spins at over 1,500 rpms effortlessly and silently. Meters show the power in and power out. Suddenly, a power source of 16 watt or so is driving a device that should be drawing at least 200 to 300 watts. Nobue explains to us that this and all the other devices only use electrical power for the two electromagnetic stators at either side of each rotor, which are used to kick the rotor past its lockup point then on to the next arc of magnets. Apparently the angle and spacing of the magnets is such that once the rotor is moving, repulsion between the stators and the rotor poles keeps the rotor moving smoothly in a counterclockwise direction. Either way, it's impressive. Next we move to a unit with its motor connected to a generator. What we see is striking. The meters showed an input to the stator electromagnets of approximately 1.8 volts and 150mA input, and from the generator, 9.144 volts and 192mA output. 1.8 x 0.15 x 2 = 540mW input and 9.144 x 0.192 = 1.755W out. But according to the laws of physics, you can't get more out of a device than you put into it. We mention this to Kohei Minato while looking under the workbench to make sure there aren't any hidden wires. Minato assures us that he hasn't transcended the laws of physics. The force supplying the unexplained extra power out is generated by the magnetic strength of the permanent magnets embedded in the rotor. "I'm simply harnessing one of the four fundamental forces of nature," he says. Although we learned in school that magnets were always bipolar and so magnetically induced motion would always end in a locked state of equilibrium, Minato explains that he has fine-tuned the positioning of the magnets and the timing of pulses to the stators to the point where the repulsion between the rotor and the stator (the fixed outer magnetic ring) is transitory. This creates further motion -- rather than a lockup. (See the sidebar on page 41 for a full explanation). Real Products ~ Nobue Minato leads us to the two devices that might convince a potential investor that this is all for real. First, she shows us the cooling fan prototype that is being manufactured for a convenience store chain's 14,000 outlets (3 fans per outlet). The unit looks almost identical to a Mitsubishi-manufactured fan unit next to it, which is the unit currently in wide use. In a test, the airflow from both units is about the same. The other unit is the car air conditioning prototype that caught our eye as we came in. It's a prototype for Nippon Denso, Japan's largest manufacturer of car air conditioners. The unit is remarkably compact and has the same contours and size as a conventional unit. Minato's manufacturing skills are clearly improving.

The Banker and his Investment ~

Minato has good reason to complain about Japan's social and cultural uniformity. For years, people thought of him as an oddball for playing the piano for a living, and bankers and investors have avoided him because of his habit of claiming that he'd discovered a breakthrough technology all by himself -- without any formal training. However, the Osaka banker stands up after the lecture and announces that before he goes, he will commit \100 million to the investment pool. Minato turns to us and smiles. We brought him good luck, and this was his third investor in as many weeks to confirm an interest. Bringing the Tech to the Table ~ With the audience gone, we ask Minato what he plans to do to commercialize the technology. His game plan is simple and clear, he says. He wants to retain control, and he wants to commercialize the technology in Japan first -- where he feels he can ensure that things get done right. Why doesn't he go directly to the US or China? His experiences in both countries, he suggests, have been less than successful. "The first stage is critical in terms of creating good products and refining the technology. I don't want to be busy with legal challenges and IP theft while doing that." Still, the export and licensing of the technology are on his agenda, and Minato is talking to a variety of potential partners in other countries. Whereas another inventor might be tempted to outsource everything to a larger corporation, part of what drives Minato is his vision of social justice and responsibility. The 40,000 motors for the convenience store chain are being produced by a group of small manufacturers in Ohta-ku and Bunkyo-ku, in the inner north of Tokyo -- which is becoming a regional rust belt. Minato is seized with the vision of reinvigorating these small workshops that until the 80s were the bedrock of Japan's manufacturing and economic miracle. Their level of expertise will ensure that the quality of the motors will be as good as those from any major company. International Prep " Despite his plan to do things domestically first, Minato is well prepared for the international markets. He is armed with both six years of living and doing business in Los Angeles in the early 90s -- and with patent protection for over 48 countries. His is hardly a provincial perspective. His US experience came after playing the piano for a living for 15 years. He began tinkering with his invention in the mid-70s. The idea for his magnetic motor design came from a burst of inspiration while playing the piano. But Minato decided to drop everything in 1990 to help his daughter Hiroko, who at the age of 20 decided that she wanted to be a rhythm and blues star in the US. Minato is a strong believer in family: If Hiroko was going to find fame and fortune in the US, Dad had better be there to help manage her. He suceeded in helping Hiroko to achieve a UK dance chart number one hit in 1995. In 1996 Minato returned to Japan and his magnetic motor project. The following year he displayed his prototypes to national power companies, government officials and others at a five-day conference in Mexico City. Interest was palpable, and Minato realized that his invention might meet a global need for energy-saving devices.

Subsequent previews and speeches in Korea and Singapore further consolidated his commitment to bringing the invention to fruition, and he was able to bring in several early-stage investors.

During the late 90s, Minato continued to refine his prototypes. He also stayed in constant contact with his lawyer, registering patents in major countries around the world. Through his experiences in the US he realized that legal protection was critical, even if it meant delaying release of the technology by a couple of years. Ironically, by the time he'd won patents in 47 countries, the Japanese patent office turned him down on the grounds that "[the invention] couldn' t possibly work" and that somehow he was fabricating the claims. But a few months later they were forced to recant their decision after the US patent office recognized his invention and gave him the first of two patents. As Minato notes: "How typical of Japan's small-minded bureaucrats that they needed the leadership of the US to accept that my invention was genuine." By 2001, the Minatos had refined their motors and met enough potential investors to enter into a major international relationship, initially with a Saudi company, to be followed thereafter by companies in the US and elsewhere. However, fate dealt the investors and Minato's business a serious blow when the World Trade Center was attacked in New York. The Saudis retreated, and Minato's plans fell back to square one. Now Minato is once again ready to move. With the first order in the works and more orders pending successful prototypes, he has decided that investors don't have to be primary partners. He is actively accepting inquiries from corporate investors who can bring strategic advantages and corporate credibility with them. His company, Japan Magnetic Fan, will make a series of investment tie-up announcements in the first and second quarters of 2004. Implications ~ Minato's motors consume just 20 percent or less of the power of conventional motors with the same torque and horse power. They run cool to the touch and produce almost no acoustic or electrical noise. They are significantly safer and cheaper (in terms of power consumed), and they are sounder environmentally. The implications are enormous. In the US alone, almost 55 percent of the nation's electricity is consumed by electric motors. While most factory operators buy the cheapest motors possible, they are steadily being educated by bodies like NEMA (National Electrical Manufacturers Association) that the costs of running a motor over a typical 20-year lifespan comprise a purchase price of just 3 percent of the total, and electricity costs of 97 percent. It is not unusual for a $2,000 motor to consume $80,000 of electricity (at a price of .06 cents per kilowatt hour). Since 1992, when efficiency legislation was put into place at the US federal level, motor efficiency has been a high priority -- and motors saving 20 percent or so on electrical bills are considered highly efficient. Minato is about to introduce a motor which saves 80 percent, putting it into an entirely new class: The $80,000 running cost will drop to just $16,000. This is a significant savings when multiplied by the millions of motors used throughout the USA and Japan -- and eventually, throughout the world. The Devices ; Minato's invention and its ability to use remarkably less power and run without heat or noise make it perfect for home appliances, personal computers, cellphones (a miniature generator is in the works) and other consumer products.

  

Content provided by J@pan Inc. Magazine -- www.japaninc.com

  

US Patent # 4,751,486

(Cl. 335/272)

 

Magnetic Rotation Apparatus

 

(June 14. 1998)

 

Kohei Minato

 

Abstract --- The magnetic rotation apparatus of the present invention has first and second rotors rotatably supported and juxtaposed. The first and second rotors are connected so as to be rotatable in opposite directions in a cooperating manner. A number of permanent magnets are arranged on a circumferential portion of the first rotor at regular intervals, and just as many permanent magnets are arranged on a circumferential portion of the second rotor at regular intervals. Each permanent magnet has one magnetic polarity located radially outward from the rotors, and has the other magnetic polarity located radially inward toward the rotors. The polarity of each permanent magnet, which is located radially outward from the rotors, is identical. When the first and second rotors are rotated in a cooperating manner, the phase of rotation of the permanent magnets of one rotor is slightly advanced from that of the permanent magnets of the other rotor. One of the permanent magnets of one rotor is replaced with the electromagnet. The radially outward polarity of the electromagnet can be changed by reversing the direction in which a current is supplied to the electromagnet.

  

TECHNICAL FIELD

 

The present invention relates to a magnetic rotation apparatus in which a pair of rotors are rotated by utilizing a magnetic force.

 

BACKGROUND ART

 

An electromotor is well known as a rotation apparatus utilizing a magnetic force. For example, an AC electromotor comprises a rotor having a coil, a stator surrounding the rotor, and a plurality of electromagnets, disposed on the stator, for generating a rotating magnetic field. An electric power must be constantly supplied to the electromagnets in order to generate the rotating magnetic field and keep the rotor rotating, i.e., an external energy, or electric energy, is indispensable for the rotation of the rotor. Under the circumstances, a magnetic rotation apparatus, which employs permanent magnets in lieu of electromagnets and can rotate a rotor only by a magnetic force of the permanent magnets, is highly desirable. The present application proposes a magnetic rotation apparatus which comprises a pair of rotors rotatable in opposite directions in a cooperating manner, and a plurality of permanent magnets stationarily arranged at regular intervals on the peripheral portion of each rotor. One end portion of each permanent magnet of both rotors, which has the same polarity, is located radially outward of the rotors. When the two rotors are rotated in a cooperating fashion, a permanent magnet on one rotor and a corresponding permanent magnet on the other, which form a pair, approach and move away from each other periodically. In this case, the phase of rotation of the magnet on one rotor advances a little from that of the corresponding magnet on the other rotor. When the paired permanent magnets approach each other, magnetic repulsion causes one rotor to rotate. The rotation of one rotor is transmitted to the other rotor to rotate the same. In this manner, other pairs of magnets on both rotors sequentially approach each other, and magnetic repulsion occurs incessantly. As a result, the rotors continue to rotate. In the above apparatus, in order to stop the rotation of the rotors, a brake device is required. If an ordinary brake device is mounted on the magnetic rotation apparatus, the entire structure of the apparatus becomes complex, and a driving source for the brake device must be provided separately. The present invention has been developed in consideration of the above circumstances, and its object is to provide a magnetic rotation apparatus including a brake device for suitably stopping the rotation of rotors.,DISCLOSURE OF THE INVENTION The magnetic rotation apparatus of the present invention is provided with magnetic force conversion means which is substituted for at least one pair of permanent magnets of the paired rotors. In a normal state, the magnetic force conversion means causes a magnetic repulsion, as in the other pairs of permanent magnets. When it is intended for the rotors to stop, the magnetic force conversion means causes a magnetic attraction force. Since a magnetic attraction force can be produced between the rotors at any time, the magnetic attraction force serves to stop the rotors. The brake device constituted by the magnetic force conversion means differs from an ordinary brake device which forcibly stops a pair or rotors by using a frictional force. In the brake device of this invention, by converting a magnetic repulsion force to a magnetic attraction force, the rotors can be braked in the state that the movement of the rotors is reduced. Thus, the rotors can be stopped effectively. BRIEF DESCRIPTION OF THE DRAWINGS

FIG. 1 is a schematic perspective view showing a magnetic rotation apparatus according to an embodiment of the invention;

FIG. 2 is a schematic plan view showing the relationship between the first and second rotors; FIG. 3 is a perspective view of a permanent magnet; FIG. 4 shows an electromagnet, a permanent magnet cooperating with the electromagnet, and a driving circuit the electromagnet; and FIG. 5 is a view for explaining how a pair of rotors rotate. BEST MODE OF CARRYING OUT THE INVENTION FIG. 1 shows a magnetic rotation apparatus embodying the present invention. The magnetic rotation apparatus has frame 1. Frame 1 is provided with a pair of rotation shafts 2 which extend vertically and in parallel to each other. Shafts 2 are located at a predetermined distance from each other. Upper and lower ends of each shaft 2 are rotationally supported on frame 1 via bearing 3. First rotor 4a is mounted on one of rotation shafts 2, second rotor 4b is mounted on the other rotation shaft 2. First and second rotors 4a and 4b are arranged on the same level. Rotors 4a and 4b have similar structures. For example, each rotor 4a (4b) comprises two ring-shaped plates 5 which are spaced apart from each other in the axial direction of the rotation shaft 2. Gears 6a and 6b made of synthetic resin are, as cooperating means, attached to lower surfaces of first and second rotors 4a and 4b. The diameters of gears 6a and 6b are identical but larger than those of rotors 4a and 4b. Gears 6a and 6b mesh with each other. First and second rotors 4a and 4b are thus rotatable in opposite directions in a cooperating manner. In FIG. 1, reference numeral 7 indicates support arms for supporting first and second rotors 4a and 4b.

For example, 16 magnets are arranged at regular intervals on a peripheral portion of first rotor 4a. These magnets are secured between two ring-shaped plates 5. In this embodiment, among the 16 magnets, one is electromagnet 9a (see FIG. 2), and the others are permanent magnets 8a. FIG. 2 shows only some of permanent magnets 8a. As shown in FIG. 3, permanent magnet 8a comprises case 10, and a plurality of rod-like ferromagnetic members 11 housed in case 10. Ferromagnetic member 11 is, for example, a ferrite magnet. Ferromagnetic members 11 of each permanent magnet 8a are arranged such that ferromagnetic members 11 have the same polarity at one end. In first rotor 4a, for example, an N-polarity end portion of each permanent magnet 8a faces radially outward, and an S-polarity end portion of magnet 8a faces radially inward. As shown in FIG. 2, when each permanent magnet 8a is located between two shafts 2, angle C formed by longitudinal axis A of magnet 8a and imaginary line B connecting two shafts 2 is, for example, set to 30.degree. C. On the other hand, electromagnet 9a is, as shown in FIG. 4, constituted by U-shaped iron core 12, and coil 13 wound around core 12. Electromagnet 9a is arranged such that both N- and S-polarity end portions face radially outward of first rotor 4a, and the above-mentioned angle C is formed, similarly to the case of permanent magnet 8a. The same number of permanent magnets (8b,9b) as the total number of all permanent magnets and electromagnet (8a,9a) of first rotor 4a are secured on a peripheral portion of second rotor 4b at regular intervals. In FIG. 2, when first and second rotors 4a and 4b are rotated in opposite directions, each permanent magnet of second rotor 4b periodically moves toward and away from the corresponding one of the magnets (8a,9a) of first rotor 4a. The permanent magnets (8b,9b) of second rotor 4b will now be described in greater detail. Permanent magnets 8b of second rotor 4b, which periodically move toward and away from permanent magnets 8a of first rotor 4a in accordance with the rotation of rotors 4a and 4b, have a structure similar to that of permanent magnets 8a of first rotor 4a. The polarity of that end portion of each permanent magnet 8b which is located radially outward from second rotor 4b, is identical with that of the end portion of each permanent magnet 8a of first rotor 4a. That is, the radially outward portion of each permanent magnet 8b has an N-polarity. Permanent magnet 9b of second rotor 4b, which periodically moves toward and away from electromagnet 9a of first rotor 4a, has a structure shown in FIG. 4. Permanent magnet 9b has a structure similar to that of permanent magnets 8a. Both polarities of electromagnet 9a face radially outward from first rotor 4a. Permanent magnet 9b has two different polarities which face radially outward from second rotor 4b and correspond to both polarities of electromagnet 9a. As shown in FIG. 2, when each permanent magnet 8b,9b is located between two rotation shafts 2, angle E formed by longitudinal axis D of the magnet (8b,9b) and imaginary line B connecting two shafts 2 is, for example, set to 56.degree. C. In addition, when rotors 4a and 4b are rotated in opposite directions, as shown by arrows, the magnets (8a,9a) of first rotor 4a move a little ahead of the corresponding permanent magnets (8b,9b) of second rotor 4b, in a region in which both magnets (8a,9a; 8b,9b) approach one another. In other words, the phase of rotation of the magnets (8a,9a) of first rotor 4a advances by a predetermined angle in relation to the permanent magnets (8b,9b) of second rotor 4b. As shown in FIG. 4, electromagnet 9a of first rotor 4a is electrically connected to drive circuit 14. Drive circuit 14 includes a power source for supplying an electric current to coil 13 of electromagnet 9a. While rotors 4a and 4b rotate, drive circuit turns on electromagnet 9a upon receiving a signal from first sensor 15 only when electromagnet 9a and permanent magnet 9b are in a first region in which they periodically approach each other. First sensor 15 is an optical sensor comprising a light-emitting element and a light-receiving element. As shown in FIG. 1, first sensor 15 is attached to a portion of frame 1 above first rotor 4a. First sensor 15 emits light in a downward direction. The light is reflected by reflection plate 16 projecting radially inward from the inner edge of first rotor 4a. First sensor 15 receives the reflected light, and feeds a signal to drive circuit 14. Thus, drive circuit 14 turns on electromagnet 9a. The circumferential length of reflection plate 16 is equal to that of the above-mentioned first region. When magnets 9a and 9b enter the first region, first sensor 15 is turned on, and when they leave the first region, first sensor 15 is turned off. When drive circuit 14 receives a signal from first sensor 15, it excites electromagnet 9a such that both polarities of electromagnet 9a correspond to those of permanent magnet 9b of second rotor 4b. Drive circuit 14 is electrically connected to switching circuit 17. When brake switch 18 is operated, switching circuit 17 reverses the direction in which an electric current is supplied to electromagnet 9a. When the current supplying direction of drive circuit 14 is reversed, drive circuit 14 excites electromagnet 9a only in a time period in which drive circuit 14 receives a signal from second sensor 19. Second sensor 19 has a structure similar to that of first sensor 15, and is attached to frame 1 so as to be located closer to the center of rotor 4a than first sensor 15. Reflection plate 20, which corresponds to the position of second sensor 19, is formed integral to an inner edge portion of reflection plate 16. As shown in FIG. 2, compared to reflection plate 16, reflection plate 20 extends in rotational direction of first rotor 4a, indicated by the arrow. The operation of the above-described magnetic rotation apparatus will now be explained with reference to FIG. 5. In FIG. 5, rotation shaft 2 of first rotor 4a is denoted by 01, and rotation shaft 2 of second rotor 4b is denoted by 02. Only the radially outward polarity, that is, N-polarity, of the magnets of rotors 4a and 4b is shown, for the sake of convenience. Although electromagnet 9a and permanent magnet 9b have both polarities located radially outward, only the N-polarity thereof is shown. When first and second rotors 4a and 4b are put in a position shown in FIG. 5, magnetic pole Nb1 of one permanent magnet of second rotor 4b is located in a line connecting shafts 01 and 02. In this case, polarity Na1 of first rotor 4a, which is paired with polarity Nb1, is a little advanced from polarity Nb1 in the rotational direction of first rotor 4a. For example, as shown in FIG. 5, magnetic pole Na1 is advanced from polarity Nb1 by an angle of X.degree.. Polarities Na1 and Nb1 exert repulsion force F1 upon each other along line L. Supposing that an angle, formed by line M, which is drawn from shaft 01 perpendicularly to line L, and the line connecting shafts 01 and 02 is represented by Y, and that the length of line K is represented by R, torques Ta1 and Tb1 caused by repulsion force F1 to rotate first and second rotors 4a and 4b can be given by: Ta1=F1.multidot.R.multidot.cos (Y-X)

Tb1=F1.multidot.R.multidot.cos Y Since cos (Y-X)>cos Y, Ta1>Tb1.

As shown in FIG. 5, since magnetic pole Na1 is advanced from magnetic pole Nb1 by angle X.degree., first rotor 4a receives a greater torque than second rotor 4b. Thus, first rotor 4a forwardly rotates in the direction of the arrow in FIG. 5. Mention is now made of paired magnets of rotors 4a and 4b in the vicinity of magnetic poles Na1 and Nb1. Magnetic poles Nan and Nan-1 of first rotor 4a are advanced ahead of magnetic pole Nal in the rotational direction. Magnetic poles Nan and Nan-1 receive a torque produced by a repulsion force acting between magnetic poles Nan and Nan-1 and corresponding magnetic poles Nbn and Nbn-1. In FIG. 5, magnetic poles Nan and Nan-1 receive a smaller torque, as they rotate farther from the location of magnetic pole Na1. It is well known that a torque of first rotor 4a, which is caused by a repulsion force acting on magnetic poles Nan and Nan-1, is decreased in inverse proportion to the square of the distance between paired magnetic poles Na and Nb.

Magnetic poles Na2 and Na3, behind magnetic pole Na1, receive a torque which tends to rotate rotor 4a in the reverse direction. This torque is considered to be counterbalanced with the torque acting on magnetic poles Nan and Nan-1. In FIG. 5, attention should be paid to the region of magnetic poles Na1 and Na2. As first rotor 4a forwardly rotates, the direction in which a torque applies to magnetic pole Na2, is changed from the reverse direction to the forward direction, before magnetic pole Na2 reaches the position of magnetic pole Na1. The torque for forwardly rotating rotor 4a is larger than that for reversely rotating rotor 4a. Therefore, first rotor 4a is easily rotated in the direction shown in FIG. 2. Second rotor 4b is considered to receive a torque in a direction reverse to the direction shown in FIG. 2, as seen from the description of first rotor 4a. It is obvious that second rotor 4b receives a maximum torque at the position of magnetic pole Nb1. As seen from the above formula, torque Tb1 applied to second rotor 4b in a direction reverse to that denoted by the arrow is smaller than torque Ta1 applied to first rotor 4a in the forward direction. The rotation of first rotor 4a is transmitted to second rotor 4b through gears 6a and 6b. By determining the relationship between the strengths of torques Ta1 and Tb1, second rotor 4b is thus rotated in a direction reverse to the rotational direction of first rotor 4a, against the torque applied to second rotor in the direction. As a result, first and second rotors 4a and 4b are kept rotating, since a torque for rotating rotors 4a and 4b in a cooperating manner is produced each time magnetic poles Na of first rotor 4a pass across the line connecting shafts 01 and 02. In a diagram shown in the right part of FIG. 5, a solid line indicates a torque applied to first rotor 4a, and a broken line indicates a torque applied to second rotor 4b. The ordinate indicates a distance between each magnetic pole and the line connecting shafts 01 and 02 of rotors 4a and 4b. The first region in which electromagnet 9a of first rotor 4a is turned on is set in a range of Z during which a torque is applied to first rotor 4a in the forward direction. In order to stop the cooperative rotation of rotors 4a and 4b, brake switch is turned on to operate switching circuit 17. Thus, the direction in which drive circuit 14 supplies a current to electromagnet 9a is reversed. The polarities of electromagnet 9a are reversed. The torque applied to electromagnet 9a in the forward direction is stopped. When electromagnet 9a approaches permanent magnet 9b, a magnetic attract:on force is produced. As a result, the rotation of rotors 4a and 4b is effectively slowed down and stopped. Since the second region, in which electromagnet 9a is excited, is larger than the first region, a large braking force can be obtained from a magnetic attraction force. In the above embodiment, since electromagnet 9a is excited only in a specific region, a large electric power is not required. In addition, since electromagnet 9a rotates and brakes rotors 4a and 4b, a braking mechanism for a magnetic rotation apparatus can be obtained without having to make the entire structure of the apparatus complex. The present invention is not restricted to the above embodiment. With the exception of the paired electromagnet and permanent magnet, all permanent magnets of the rotors are arranged such that their end portions of the same polarity face radially outward from the rotors. However, it is possible that the polarities of the radially outward end portions of the permanent magnets are alternately changed. Namely, it should suffice if the polarities of the radially outward end portions of the first rotor are identical to those of the corresponding radially outward end portions of the second rotor. The magnets may have different magnetic forces. Furthermore, an electric power for exciting the electromagnet can be derived from the rotation of the rotors or from the revolving magnetic field of the permanent magnet.

Angles C and E are not restricted to 30.degree. and 56.degree.. They may be freely determined in consideration of the strength of the magnetic force of the permanent magnet, a minimum distance between adjacent magnets, angle x, and the like. The number of magnets of the rotor is also freely chosen.

Industrial Applicability ~ As described above, the magnetic rotation apparatus of the present invention can be used as a driving source in place of an electric motor, and as an electric generator. US Patent # 5,594,289 (Cl. 310/152) Magnetic Rotating Apparatus (January 14, 1997) Kohei Minato Abstract --- On a rotor which is fixed to a rotatable rotating shaft, a plurality of permanent magnets are disposed along the direction of rotation such that the same magnetic pole type thereof face outward. In the same way, balancers are disposed on the rotor for balancing the rotation of this rotor. Each of the permanent magnets is obliquely arranged with respect to the radial direction line of the rotor. At the outer periphery of the rotor, an electromagnet is disposed facing this rotor, with this electromagnet intermittently energized based on the rotation of the rotor. According to the magnetic rotating apparatus of the present invention, rotational energy can be efficiently obtained from permanent magnets. This is made possible by minimizing as much as possible current supplied to the electromagnets, so that only a required amount of electrical energy is supplied to the electromagnets. Claims --- [ Claims not included here ] Description BACKGROUND OF THE INVENTION 1. Field of the Invention The present invention relates to a magnetic rotating apparatus, and more particularly, to a magnetic rotating apparatus which utilizes repulsive forces produced between a permanent magnet and an electromagnet.

2. Description of the Prior Art In a conventional electric motor, an armature as a rotor consists of turns of wires, and electric field as a stator consists of a permanent magnet. In such the conventional electric motor, however, current must be usually supplied to windings of the armature which is rotated. When the current is supplied, heat is generated, which gives rise to the problem that not much driving force is efficiently generated. This, in turn, gives wise to the problem that the magnetic forces cannot be efficiently obtained from the permanent magnet. In addition, in the conventional electric motor, since the armature is so constructed as consisting of the windings, the moment of inertia cannot be made very high, so that enough torque cannot be obtained. To overcome the above-described problems of such the conventional electric motor, the inventor proposed, in Japanese Patent Publication No. 61868/1993 (U.S. Pat. No. 4,751,486) a magnetic rotating apparatus in which a plurality of the permanent magnets are disposed along the two rotors, respectively, at a predetermined angle, and in which an electromagnet is disposed at one of the rotors. In a generally constructed conventional electric motor, there is a limit as to how much the efficiency of energy conversion can be increased. In addition, the torque of the electric motor cannot be made high enough. For the above reasons, hitherto, various improvements have been made on existing electric motors, without any success in producing an electric motor so constructed has providing satisfactory characteristics. In the magnetic rotating apparatus disclosed in Japanese Patent Publication No. 6868/1993 (U.S. Pat. No. 4,751,486) a pair of rotors is rotated. Therefore, it is necessary for each of the rotors to have high precision, and in addition, measures must be taken for easier rotation control. SUMMARY OF THE INVENTION In view of the above-described problems, the object of the present invention is to provide a magnetic rotating apparatus in which rotational energy can be efficiently obtained from the permanent magnet with a minimum amount of electrical energy, and in which rotation control can be carried out relatively easily. According to one aspect of the present invention, there is provided a magnetic rotating apparatus comprising a rotating shaft; a rotor which is fixed to the rotating shaft and which has disposed thereon permanent magnet means and means for balancing rotation, the permanent magnet means being disposed such that a plurality of magnetic poles of one (or first) polarity type is arranged along an outer peripheral surface in the direction of rotation, and a plurality of magnetic poles of the other (or second) polarity type arranged along an inner peripheral surface, with each pair of corresponding magnetic poles of one and the other polarities obliquely arranged with respect to a radial line; electromagnet means, which is disposed facing this rotor, for developing a magnetic field which faces the magnetic field of the permanent magnet means of the rotor and detecting means for detecting rotating position of the rotor to allow the electromagnet means to be energized. According to another aspect of the present invention, there is provided a magnetic rotating apparatus comprising a rotating shaft a rotor which is fixed to the rotating shaft and which has disposed thereon a plurality of permanent magnets and balancers for balancing rotation, the permanent magnets being disposed such that one magnetic polarity type is arranged along an outer peripheral surface in the direction of rotation and the other magnetic polarity type arranged along an inner peripheral surface, with each pair of corresponding magnetic poles of one and the other polarities obliquely arranged with respect to a radial line; an electromagnet, which is disposed facing this rotor, for developing a magnetic field which produces the other magnetic polarity type on the facing surface; and energizing means for intermittently energizing the electromagnet means from where the leading permanent magnet, based on the rotation of the rotor, passes the facing surface of the electromagnet in the direction of rotation. According to still another aspect of the present invention, there is provided magnetic rotating apparatus comprising a rotating shaft; a first rotor which is fixed to the rotating shaft and which has disposed thereon permanent magnet means and means for balancing rotation, the permanent magnet means being disposed such that a plurality of magnetic poles of the second polarity type is arranged along an outer peripheral surface in the direction of rotation, and a plurality of magnetic poles of the first pole type arranged along an inner peripheral surface, with each pair of corresponding magnetic poles of one and the other polarities obliquely arranged with respect to a radial line; a second rotor which rotates along with the first rotor and is fixed to the rotating shaft, having disposed thereon a plurality of permanent magnets and balancers for balancing rotation, the permanent magnets being disposed such that one magnetic polarity type is arranged along an outer peripheral surface in the direction of rotation and the other magnetic polarity type arranged along an inner peripheral surface, with each pair of corresponding magnetic poles of one and the other polarities obliquely arranged with respect to a radial line a first and a second electromagnet means, which are magnetically connected and disposed facing the first and second rotors, respectively, for developing a magnetic field which faces the magnetic field of the permanent magnet means of the first and second rotors; and detecting means for detecting rotating position of the rotors to allow the electromagnet means to be energized. The nature, principle and utility of the invention will become more apparent from the following detailed description when read in conjunction with the accompanying drawings.

BRIEF DESCRIPTION OF THE DRAWINGS In the accompanying drawings: FIG. 1 is a perspective view schematically illustrating a magnetic rating apparatus according to one embodiment of the present invention FIG. 2 is a side view of the magnetic rotating apparatus illustrated in FIG. 1; FIG. 3 is a plan view of a rotor of the magnetic rotating apparatus illustrated in FIGS. 1 and 2;

FIG. 4 is a circuit diagram illustrating a circuit in the magnetic rotating apparatus shown in FIG. 1; FIG. 5 is a plan view showing a magnetic field distribution formed between the rotor and the electromagnet of the magnetic rotating apparatus shown in FIGS. 1 and 2, and FIG. 6 is an explanatory view illustrating a torque which causes rotation of the rotor of the magnetic rotating apparatus shown in FIGS. 1 and 2. DESCRIPTION OF THE PREFERRED EMBODIMENTS The magnetic field developed by an electromagnet means and that of a permanent magnet means of a rotor repel each other. In addition, the magnetic field of the permanent magnet means is flattened by the magnetic fields of other nearby permanent magnets and electromagnet means. Therefore, a torque is produced therebetween to efficiently rotate the rotor. Since the rotor has a high inertial force, when the rotor starts rotating, its speed increases by the inertial force and the turning force. A magnetic rotating apparatus related to one embodiment of the present invention will be described with reference to the following drawings. FIGS. 1 and 2 are schematic diagrams of a magnetic rotating apparatus related to one embodiment of the present invention. In the specification, the term "magnetic rotating apparatus" will include an electric motor, and from its general meaning of obtaining turning force from the magnetic forces of permanent magnets, it will refer to a rotating apparatus utilizing the magnetic forces. As shown in FIG. 1, in the magnetic rotating apparatus related to one embodiment of the present invention, a rotating shaft 4 is rotatably fixed to a frame 2 with bearings 5. To the rotating shaft 4, there are fixed a first magnet rotor 6 and a second magnet rotor 8, both of which produce turning forces and a rotated body 10, which has mounted therealong a plurality of rod-shaped magnets 9 for obtaining the turning forces as energy. They are fixed in such a manner as to be rotatable with the rotating shaft 4. At the first and second magnet rotors 6 and 8, there are provided, as will be described later in detail with reference to FIGS. 1 and 2, a first electromagnet 12 and a second electromagnet 14 respectively are energized in synchronism with rotations of the first and second magnet rotors 6 and 8, both of which face each other and are each disposed in a magnetic gap. The first and second electromagnets 12 and 14 are respectively mounted to a yoke 16, which forms a magnetic path. As shown in FIG. 3, the first and second magnet rotors 6 and 8 each have disposed on its disk-shaped surface a plurality of tabular magnets 22A through 22H for developing a magnetic field for generating the turning forces and balancers 20A through 20H, made of non-magnetic substances, for balancing the magnet rotors 6 and 8. In the embodiments, the first and second magnet rotors 6 and 8 each have disposed along the disk-shaped surface 24 at equal intervals the eight tabular magnets 22A through 22H along half of the outer peripheral area and +the eight balancers 20A through 20H along the other half of the outer peripheral area.

As shown in FIG. 3, each of the tabular magnets 22A through 22H are disposed so that its longitudinal axis 1 makes an angle D with respect to a radial axis line 11 of the disk-shaped surface 24. In the embodiment, an angle of 30 degrees and 56 degrees have been confirmed for the angle D. An appropriate angle, however, can be set depending on the radius of the disk-shaped surface 24 and the number of tabular magnets 22A through 22H to be disposed on the disk-shaped surface 24. As illustrated in FIG. 2, from the viewpoint of effective use of the magnetic field, it is preferable that the tabular magnets 22A through 22H on the first magnet rotor 6 are positioned so that their N-poles point outward, while the tabular magnets 22A through 22H on the second magnet rotor 8 are positioned so that their S-poles point outward. Exterior to the first and second magnet rotors 6 and 8, the first and second electromagnets 12 and 14 are disposed facing the first and second magnet rotors 6 and 8 respectively in the magnetic gap. When the first and second electromagnets 12 and 14 are energized, they develop a magnetic field identical in polarity to the their respective tabular magnets 22A through 22H so that they repel one anther. In other words, as shown in FIG. 2, since the tabular magnets 22A through 22H on the first magnet rotor 6 have their N-poles facing outwards, the first electromagnet 12 is energized so that the side facing the first magnet rotor 6 develops an N-polarity. In a similar way, since the tabular magnets 22A through 22H on the second magnet rotor 8 have their S-poles facing outwards, the second electromagnet 14 is energized so that the side facing the tabular magnets 22A through 22H develops a S-polarity. The first and second electromagnets 12 and 14, which are magnetically connected by the yoke 16, are magnetized so that the sides facing their respective magnet rotors 6 and 8 are opposite in polarity with respect to each other. This means that the magnetic fields of the electromagnets 12 and 14 can be used efficiently. A detector 30, such as microswitch, is provided to either one of the first magnet rotor 6 or second magnet rotor 8 to detect the rotating position of the magnet rotors 6 and 8. That is, as shown in FIG. 3, in a rotational direction 32 of the tabular magnets 22A through 22H, the first and the second magnet rotors 6 and 8 are respectively energized when the leading tabular 22A has passed. In other words, in the rotational direction 32, the electromagnet 12 or 14 is energized when starting point So, located between the leading tabular magnet 22A and the following tabular magnet 22B coincides with the center point Ro of either the electromagnet 12 or 14. In addition, as illustrated in FIG. 3, in the rotational direction 32 of the tabular magnets 22A through 22H, the first and the second magnet rotors 6 and 8 are de-energized when the last tabular magnet 22A has passed. In the embodiment, an end point Eo is set symmetrical to the starting point So on the rotating disk-shaped surface 24. When the end point Eo coincides with the center point Ro of either the electromagnet 12 or 14, the electromagnet 12 or 14 is de-energized, respectively. As will be described later, with the center point Ro of the electromagnet 12 or 14 arbitrarily set between the starting point So and the end point Eo, the magnet rotors 6 and 8 start to rotate when the electromagnets 12 and 14 and their tabular magnets 22A through 22H face one another. When a microswitch is used as the detector 30 for detecting the rotating position, the contact point of the microswitch is allowed to slide along the surface of the rotating disk-shaped surface 24. A step is provided for the starting point So and the end point Eo so that the contact of the microswitch closes between the starting point So and the end point Eo. The area along the periphery therebetween protrudes beyond the other peripheral areas of the rotating disk-shaped surface 24. It is apparent that a photo sensor or the like may be used instead of the microswitch as the detector 30 for detecting the rotating position. As shown in FIG. 4, the windings of the electromagnets 12 and 14 are connected to a DC power source 42 through a movable contact of a relay 40, which is connected in series with the windings. A series circuit containing the relay 40 (solenoid) and the detector 30 or microswitch is connected to the DC power source 42. In addition, from the viewpoint of energy conservation, a charger 44 such as a solar cell is connected to the DC power source 42. It is preferable that the DC power source 42 is constantly chargeable using solar energy or the like. In the magnetic rotating apparatus illustrated in FIGS. 1 and 2, a magnetic field distribution shown in FIG. 5 is formed between the tabular magnets 22A through 22H, disposed on each of the magnet rotors 6 and 8, and the electromagnets 12 and 14 which face them, respectively. When the electromagnet 12 or 14 is energized, a magnetic field of a tabular magnet of the tabular magnets 22A through 22H, adjacent to the electromagnet 12 or 14, is distorted in the longitudinal direction in correspondence with the rotational direction. This results in the generation of a repulsive force therebetween. As is apparent from the distortion of the magnetic field, the repulsive force has a larger component in the longitudinal or perpendicular direction, and produces a torque, as shown by an arrow 32. Similarly, a magnetic field of a tabular magnet of the tabular magnets 22A through 22H, which next enters the magnetic field of the electromagnet 12 or 14, is distorted. the repulsive force produced between the tabular magnets of the tabular magnets 22A through 22H, which have already entered the magnetic field of the electromagnets, a repulsive force operates between both of the poles M and M' of the tabular magnet at the rotating side and the electromagnet at the stationary side, respectively. Therefore, from the relationship illustrated in FIG. 6, an angular torque T is generated based on the formula: T=F. a.cos (.alpha.-.beta.), where in a is a constant. The angular torque starts the rotation of the rotating disk-shaped surface 24. After the rotating disk-shaped surface 24 has started rotating, its rotating speed gradually increases due to an inertial moment thereof, which allows a large turning driving force to be produced. After a stable rotation of the rotating disk-shaped surface 24 has been produced, when a necessary electromotive force can be developed in an electromagnetic coil (not illustrated) by externally bringing it near a rotated body 10 to be rotated along with the rotating disk-shaped surface 24. This electric power can be used for other applications. This rotating principle is based on the rotating principle of the magnetic rotating apparatus already disclosed in Japanese Patent Publication No. 61868/1993 (U.S. Pat. No. 4,751,486) by the inventor. That is, even if an electromagnet, provided for one of the rotors of the magnetic rotating apparatus disclosed in the same Patent Application, is fixed, it is rotated in accordance with the rotating principle disclosed therein. For details, refer to the above Japanese Patent Publication No. 61868/1993 (U.S. Pat. No. 4,751,486).

The number of tabular magnets 22A through 22H is not limited to "8" as shown in FIGS. 1 and 3. Any number of magnets may be used. In the above-described embodiment, although the tabular magnets 22A through 22H are disposed along half of the peripheral area of the disk-shaped surface 24, and the balancers 20A through 20H are disposed along the other half of the peripheral area, the tabular magnets may further be disposed along other areas of the disk-shaped surface 24. It is preferable that balancers, in addition to magnets, are provided along a portion of the peripheral area on the disk-shaped surface. The counter weights, which do not need to be formed into separate blocks, may be formed into one sheet of plate which extends on the outer peripheral area of the disk-shaped surface. In addition, in the above-described embodiments, while the construction is such as to allow the electromagnets to be energized for a predetermined period of time for every rotation of the rotating disk-shaped surface, the circuit may be so constructed as to allow, upon increased number of rotations, energization of the electromagnets for every rotation of the rotating disk-shaped surface, starting from its second rotation onwards. Further, in the above-described embodiment, a tabular magnet has been used for the permanent magnet, but other types of permanent magnets may also be used. In effect, any type of magnet may be used as the permanent magnet means as long as a plurality of magnetic poles of one type is disposed along the outer surface of the inner periphery and a plurality of magnetic poles of the other type are disposed along the inner peripheral surface of the disk-shaped surface, so that a pair of corresponding magnetic poles of one and the other polarities is obliquely arranged, with respect to the radial line 11, as shown in FIG. 3. Although the tabular magnets 22A through 22H are mounted on the magnet rotors 6 and 8 in the above embodiment, they may be electromagnets. In this case, the electromagnets 12 and 14 may be the alternative of electromagnets or permanent magnets.

According to the magnetic rotating apparatus of the present invention, rotational energy can be efficiently obtained from permanent magnets. This is made possible by minimizing as much as possible current supplied to the electromagnets, so that only a required amount of electrical energy is supplied to the electromagnets. It should be understood that many modifications and adaptations of the invention will become apparent to those skilled in the art and it is intended to encompass such obvious modifications and changes in the scope of the claims appended hereto. KeelyNet: BBS Posting from Henry Curtis (11-18-1997)

Korean Magnetic Perpetual Motion Wheel I must apologize for not having all the details of this interesting device but will update the file when I get more info from the source. In email communications with John Schnurer, I happened to mention it and he's been on me since then to send him a diagram, yet I felt like it would simply be confusing because its operation is not clear or readily apparent from the information I had.The information that I have comes directly from long time friend Henry Curtis of Colorado. We both attended the 1997 ISNE conference in Denver and Henry was telling about this interesting machine he had seen while on a trip to the Phillipines. He said there was a free energy conference held there and he noticed a spinning bicycle wheel that was attached to a stand that sat on a table.The wheel was running when he first saw it, yet there did not appear to be any driving force such as a motor, belts, gears, etc..Henry said he watched it for quite awhile and it never stopped running. On expressing curiosity about the wheel, he was invited to stop it and start it up without any outside assistance.Henry reports the wheel was brought to a complete stop, then he gave it a spin with his hand and it began moving on its own. I am uncertain if it followed the tendency of other such devices to establish its own speed. Some devices like this can be spun up to high speed from an outside source, then will slow to a speed which is determined by the geometry and strength of the repelling or attracting forces that operate it.Henry swears it was the neatest thing he'd ever seen and drew a crude diagram of the arrangement on my notepad. Unfortunately, we were a bit rushed and I did not achieve a complete understanding of how it operated. That is why I did not want to blow smoke about it until more detail had been received, god knows, we don't need any more of that.However, perhaps someone can figure it out from the limited information I do have. The following drawing shows the wheel arrangement, one half was weighted, the other half had slanted magnets. I do not know whether they are all repelling, attracting or a mix of these forces. As you can imagine, the weight of the magnets must equal the weight of the other half of the wheel to balance out. Apparently the force of the magnetic repulsion or attaction provides the actual imbalance.Henry also said there was a patent on this device that is dated January 14, 1997. The inventor is a Japanese man named Minatu. The spelling of this name is uncertain. I did a search on the IBM server but found nothing even remote. Henry specifically said this was a United States patent. So, here it is. Perhaps Henry can come up with some more detail which can be used to update this file in future. Good luck.... KeelyNet: Update and Corrections from Henry Curtis (Wed, 19 Nov 1997) ~

From: Henry Curtis ~ To: Jerry Decker Subject: Bicycle wheel correction and update Jerry, Again we see that communication is difficult and memories are fallable. Obviously I am remiss in not having sent this to you months ago as I intended to, but as a sage of old observed "The spirit is willing, but the flesh is slow." During the first weekend of May, 1997, a group in Soeul, Korea headed up by Mr. Chi San Park, held The First International New Energy Conference in Seoul, Korea. I attended this conference and gave a talk on various approcahes to free energy. It was at this conference in Seoul, Korea that I saw the bicycle wheel and had the opportunity to work with it unattended by anyone else.The inventor is Kohei Minato, a Japanese rock musician, who reports that he has spent a million dollars out of his own pocket developing magnetic motors, because the world needs a better source of energy. He has several patents in various countries. His latest patent that I am aware of is United States Patent # 5,594,289. His development efforts have gone in the general direction of the Adams motor which the above patent is similar to. He had a working prototype of this design at the conference and reported that it used 150 watts power input and produced 450 watts output on a sustained basis. About a year ago CNN (in the US) had a 10 minute segment about him and his motors. In this video he is shown demonstrating two of his magnetic motors. I have a copy of this film clip that he gave to me. I will make a copy and send it to you. Unfortunately, the editors were not attuned to technical details and the pictures of the running machines show little useful detail. The Phillipine connection that you mention is completely erroneous. It was in Korea. The drawing on the web site is essentially correct with the following exceptions. The counter weight is a single curved piece of aluminum covering 180 degrees. Each of the several individual magnets on the other half of the wheel are slightly asymmetric, crescent shaped and nested. They are magnetised end to end with the N poles out. The motor is actuated by moving the N pole of a large permanet magnet (the drive magnet) toward the wheel. As this magnet is moved toward the wheel, the wheel starts to spin. As the magnet is moved closer to the wheel it spins faster. The acceleration of the wheel is rapid. So rapid in fact, as to be startling. To put it another way I was very impressed. The motor works. And it works very well. In the film clip a slight pumping action of Minato's hand holding the magnet is apparent. When I braced my hand so that there was no pumping action, the motor still ran. In fact it seemed to run better. Pumping action by the hand held magnet is not the power that drives the motor. When the drive magnet is moved away from the wheel it coasts rather quickly to a stop and comes to rest in a manner typical of any spinning bicycle wheel. Again when the wheel is at rest and a large magnet is moved up to the wheel it starts to spin. At no time is it necessary to touch the wheel to get it to rotate. Simply bring the N pole of a large magnet several inches from the wheel. The particular orientation of the wheel when it is at rest seems to have no effect on how well it starts to turn. Irrespective of how the wheel and the magnets on it are sitting; move the drive magnet near, it starts to spin. Move the magnet closer it spins faster. Move the magnet further away it slows up. The wheel was mounted on a stand made of aluminum angle pieces bolted together similar to the diagram in the above mentioned patent. The axle of the wheel was mounted parellel to the surface of the planet. I have attached a rough diagram of the wheel. Apparently the geometry of the magnets on the wheel is very important and subtle. I have built several small models none of which have shown the free energy effects of Minato's machine. The conference in Seoul was attended by several hundred people, most appeared to be under 40 and evenly divided between men and women. Presenters were from Korea, US, Japan, and China. Simultaneous translation was provided for all talks in the 3 day conference. Jerry, I hope this information is useful. I may be contacted by e-mail at mailto:hcurtis@mindspring.com or by phone at 303.344.1458.

KeelyNet: Email from Gene Mallove at Infinite Energy ~ I spoke to Bob Vermillion of Tri-Cosmos Development (Los Angeles, CA 310-284-3250 or fax 310-284-3260) today, just before he left for the three-day demonstrations of the Minato magnetic motor being held in Mexico City, Mexico on July 8, 9, 10th.Three (3) Minato Motors (MM), covered by US Patents # 5,594,289 (Jan 14, 1997) and # 4,751,486 (June 14, 1988), have been brought over from Japan. One was allegedly tested last evening by Grupo Bufete Industrial (supposedly one of the largest power generation construction companies in Mexico and South America). The company engineers were said (by Vermillion) to have measured an output /input ratio of 4.3 / 1. The printed literature, which I received in a Fedex packet from Vermillion states that the device can put out 500 watts (maximum) with an input of 34 watts.For those of you who wonder why the device is not self-sustaining -- oral info from Vermillion is that Minato *will* in the course of one of the demonstrations *remove the battery power supply* and let the device self-run -- presumably with a load. The press release makes no bones about the physics-busting character of the MM: "As rotations per minute (rpm's) increase, the electromagnetic consumption of the stator decreases. This phenomenon is in direct conflict with accepted laws of physics and is achieved through the repelling magnetic fields. It operates without heat, noise, or pollution of any kind. It can be produced in size from ultra-small to very large." It is said in the press release that applications from cell phones to laptop computers are under development. Vermillion told me of other parties who were planning to attend the demonstrations, which will be conducted both in public displays and with private party measurements. These include: ENRON, Bechtel, Tejas (a division of Shell Oil Corporation), Fluor Daniels, Kellogg Corp. .He told me that Hal Fox of New Energy News and the Fusion Information Center will be there (I confirmed with Hal that he will be there and will give us a full report.) I considered going myself (I was invited), but I trust Hal Fox to provide a full report --

www.japaninc.com/article.php?articleID=1302

  

en.wikipedia.org/wiki/Permanent_magnet_motor

Tried something a bit different today. Got up at 5am to go downtown Houston to shoot some early morning shots. Came back with this that I was surprisingly happy with.

 

****I see now this is a bit confusing as to what you all are actually looking at.

 

This is a building, and I am looking almost VERTICAL up the wall and into the sky. A very mind melting perspective.

First letter reads: T. Proctor Hall / M.A., PH.D., M.D. / 1801 Davie Street / Vancouver, Canada - Sunday, Dec. 19, 1920 - Dear Vic, I have written the Abbott Alk. Co. to send to your address a few bottles of medicine and two gross empty bottles. The value of the empty bottles and corks is about $3; and of the medicines an average of $1.25 per bottle. Technically they are all called "pills". Take all the wrappers of the medicines, and they will not take much room among your things. Mrs Cook was buried yesterday. Mrs Cartwright was at the funeral and returns to Seattle tomorrow. We are expecting you Friday morning. If you have a lot of books it is better to pack them in a separate box and, if you have accepted a position in U.S., store them with dome delivery Co. until your return, when they can be sent directly to the Station. Au revoir, ma chere fille, (Goodbye my dear daughter) - signed T. P. Hall

 

added on the bottom of the letter: Dear Vic, If you pack your few medicines discreetly you will not have any bother with them. R.M.H. (Ruth Maude Hall / her stepmother) - Money is over 18%.

 

His second wife - Ruth Maude (nee McManus) Hall

(b. 1868 in Iowa, United States – d. 8 September 1942 at age 74 in Vancouver, British Columbia, Canada) - they were married - 10 September 1902 in Chicago, Cook County, Illinois, USA)

 

Clipped from - The Province newspaper - Vancouver, British Columbia, Canada - 8 September 1942 - Dr. Ruth M. Hall Called by Death Pioneer woman physician, Dr. Ruth Maude Hall, died on Tuesday in her 76th year. She lived at Garrow Bay, Whytecliff, B.C. Born in Cedar Rapids, Iowa, she first took up nursing and then became Interested In medicine, graduating from National Medical College in Chicago in 1902. She married Dr. T. P. Hall in 1902 and came with him to British Columbia in 1905. In 1906 the two opened the Hillside Hospital at Burrard and Barclay in collaboration with Dr Ernest Hall and Dr. Robert Telford. In 1908 her husband entered private practice and until his death in 1931 she aided him in his work. Surviving are one son, Dr. Vernon K. Hall, Garrow Bay; two daughters, Miss A, V. Hall of Seattle and Miss U. F. Hall of Vancouver, and three nieces, Miss E. Mildred McManes and Mrs. R. E. Taylor of Vancouver and Mrs. Roy Stchman of Bremerton, Wash., and three granddaughters, The funeral will be held Thursday at 3:30 p.m. from the T. Edwards Chapel to Capllano View Cemetery.

 

Second letter reads: T. Proctor Hall / M.A., PH.D., M.D. / 1801 Davie Street / Vancouver, Canada - Tuesday night (21 December 1920) - Dear Vio, I have just seen Mr. Dougan at the Child - welfare meeting. He today got word from Nanaimo that they depend on him for two teachers; one in Drawing, Algebra and French. But he knows there is a teacher there who is well up in French, and there would probably be little trouble in adjusting to work among the six teachers. The salary is $1900. I told him we would all like it better to have you nearer home; and to wire Nanaimo whether your services would be acceptable. If so, he will wire you by Wed. night. (page 2) If this position is offered you to at once (or telephone, if it is late) to the man who got you the Idaho position; tell him the conditions and ask him to wire Idaho (at your expense) requesting a release, because offered a much better salary near home. In such cases it is usually easy to find a substitute, and the request is very seldom refused. Stay another day in Seattle, if necessary, to get things cleared up. Of course if Mr. Dougan's offer is not definite and positive no action need be taken. But if it is, act promptly. T. P. Hall (her father)

 

Clipped from - Times Colonist newspaper - Victoria, British Columbia, Canada - 25 March 1931 - DR. THOMAS PROCTOR HALL OF VANCOUVER DIED TO-DAY - Brother of Dr. Ernest Hall, Victoria Physician, Succumbs in Terminal City - Dr. Thomas Proctor Hall, seventy-two, physician, scientist and educationist, died at 4 o'clock this morning at the family residence, Crown Crescent, Vancouver, following an illness from heart disease, it was learned here to-day. He was a brother of Dr. Ernest Hall, well-known Victoria physician, and practiced here for a short period many years ago. Dr. Hall, who had resided in Vancouver for the last twenty-six years, had patented literally dozens of inventions and had made many scientific discoveries for which he had not taken out patents. They ranged from a system of reproducing the human voice almost a quarter of a century ago, to taking the flicker out of the early type motion pictures, an automatic stop for gramophones and a model for demonstrating the theory of the fourth dimension. Of unusual ability, he was a specialist In physical science and In mathematics as well as his chosen profession of medicine. Of so retiring and modest a disposition was he, however, than even many of his close friends were unaware of all his talents. With the exception of a new type of therapeutic lamp, his inventions have never been placed on the market. Dr. Hall, among his other scientific investigations, had done a great deal of research work in connection with X-ray. Besides the degrees of B.A.. M.A. and M.D. he was entitled to carry after his name, he had been awarded the degree of Doctor of Philosophy, both by Clark University and the Illinois Wesleyan University. He was an honor graduate of the University of Toronto, McMaster University, Toronto, and the National Medical University in Chicago. FOURTH DIMENSION MODEL - Forty years ago he left at Clark University, a model to demonstrate the theory of the fourth dimension. From 1883 to 1884 Dr. Hall was a fellow of Toronto University. For the following five years he was science master at Woodstock College, Ontario. His teaching record was a varied one, including also professorships in natural science at Tabor College, Iowa; physics, Kansas City University; physics and chemistry, National-Medical University, Chicago, and electro-physics, Chicago College of X-ray and Electro-therapy. LEAVES RELATIVES Dr. Vernon K. Hall, his son, practices medicine in Vancouver. Two daughters. Miss A. Violet Hall and Miss Unina S. Hall, reside in Vancouver. Mrs. R. E. Taylor, Mrs. I. Brodigan and Miss Mildred McManus, nieces of the late Dr. Hall, made their home with him for many years. Besides Dr. Ernest Hall, another brother, John Hall, resides in Denver and a nephew. Kenneth McManus, lives in San Francisco. Dr. Ernest Hall left Victoria this afternoon to attend the funeral.

Me, sporting covid hair, wearing mask by Joe Average.

 

WIKI - "Joe Average (born October 10, 1957) is a Canadian artist who resides in Vancouver, British Columbia. Diagnosed HIV+ at age 27, Average made the decision to commit the rest of his life to art."

 

Joe is a beloved national icon, philanthropist and humanitarian. joeaverageart.com/

What you see is an average day, of a Targeted Individual, in the United States.

 

I was in Goodyear, Arizona. I drove by an Autozone store and decided to pull in and get a few parts. They were common parts, for routine maintenance on the motorhome. I had searched a few of the parts, the night before, on my cell phone. I had just left a laundromat, where the local police made an intentional presence. The Autozone was on the way home. I missed my turn, so I took the next road, and came in from the back. As I approached the back of the store; I was cut off by two guys in a large black truck. Yep, another one of those damn; Billy Bob Trucks. They pulled around to the front, and went in quickly.

I parked in front of the store. Then took Koda over to an area, where he could take a pee. As I walked towards the entrance; I saw a young guy standing beside a vintage Honda motorcycle. I’ve had a few in my younger years, so I stopped and had a pleasant conversation with him. I noticed his plates had expired in 2021. I didn’t mention it, and went inside. I thought the guy with the motorcycle was leaving, but he later came back into the store.

As Koda and I walked into the store, the two men in the black truck rushed out quickly, without a purchase. I walked over to an area, to grab a part I needed; but it wasn’t there. I went up to the counter and asked an older man, about the part. He walked over to the display I was looking at, and they didn’t have it. He reached down, and put his hand in Koda’s face. I said politely, “sir, he’s a service dog, please leave him alone”. Koda was wearing his large red, service dog, collar.

We went to the counter, so he could look up another part I needed. He spent a long time on the computer, went to the back, came back to the front and said “we don’t have it”. He was fidgeting with a few items I placed on the counter. As he did, he stood there staring directly into Koda’s eyes. As, you can see, in the screenshot above. He continued to stare at Koda’s eyes, after I repeatedly asked him not to. He finally told the man to stop, dogs take it as an act of aggression. Koda’s still laying at my left side. We were at the counter for a while, so Koda laid down, after setting. Which I’ve trained him to do.

The guy told me they didn’t have the part, left it at that, instead of seeing if another store had one. Again, a very common automotive part. I asked if he could locate one for me. As he took his time, with a pissy attitude, the guy in the top screenshot came from behind the counter. He leaned over, sat his backpack on the floor, right beside Koda. Once he stood up, something in the backpack startled the hell out of Koda. He jumped up, and was pulling away from the backpack. This is extremely uncommon for him. There was something in the backpack, that was frightened him. He wanted to get the both of us, away from it. The young guy, just stood there smiling. He was the same guy, I was talking with, about his motorcycle. Police will follow me from store to store, but won’t bother him, and his expired plates.

I wonder why????

Koda, has acted similar, when I took him to a couple doggy, day care facilities, on a second visit. One place in Gilbert, Arizona, he won’t even get out of the car. He just sat there trembling. It almost brought me to tears. Wondering what they had done to him, on a previous visit. I’ve had this happen at three facilities, I’ve taken him too. When I have MRIs, or X-rays, the VA, won’t allow him there. Unless someone can watch him in the waiting area. That’s just the VA. The last two weeks, I’ve had MRI’s and X-rays, at two different facilities, they allowed him, and loved him. He would lay on the floor, by a chair; after giving him the command to Wait. The last place, he sat up quickly, when the pain in my neck, produced pheromones. I explained to the technicians, they were amazed. He really is Magnificat.

So, the guy finally said there was another store close, they had the part I wanted. He said I could pay for the part there, and pick it up at the other store. I had a $10.00 coupon, with a barcode on my phone. I paid for the parts, and was headed out the door. Just ahead of me, was a woman with pink and purple hair. There was a guy, standing directly in front of my car. I hit the keyphob, didn’t hear the doors unlock. I pulled on the handle, it was unlocked. I locked it when we got out, but now, it’s unlocked. The guy standing in front of my car; looks at me and smiles. Once, in the car; I looked over my receipt, the $10, wasn’t deducted. I had to go back in. The guy argued with me, kept saying “you saw me scan it”. After some more bullshit, I got the $10.

Koda and I headed to the other store, to get the part I had paid for. As we walked in, an employee was leaving. I see at the counter, the woman with the pink and purple hair, from the other store we were just at. She, and the woman behind the counter, were talking away, stalling as much as they could. There was another guy, at a different register. I told him I had a paid part, to pick up. He pointed at the two women, said, she can help you. The women continued their conversation, while Koda and I stood there waiting. Koda, has amazing facial expressions, he knew I was getting a bit frustrated, and gives me his WTF, look. I patiently waited. Once at the counter, the woman was pleasant, and gave me my part. There was still another part I needed, so we were off to a different parts store. It wasn’t an Autozone, They didn’t have the part. The guy at the counter, gave me the name of another store, so Koda and I went out to the car to call them. I was on the phone forever, the person on the other end, stalling. It was a transmission pan, plug kit. Something that most auto parts stores carry. It was a part, I was looking at on Amazon, the night before. As Koda, and I set in the car, I’m still on the phone; a man pulls up beside us. He gets out, puts on a black backpack. He slowly walks across the front of our car, takes both hand, pushes up the bottom of the backpack, as he looks at us and smiles. Again, Koda tilts his head, gives me the WTF, look. Just after, the guy walks pass, here come another, Goodyear, AZ, police car. Driving slowing, across the front of our car. I finally gave up on the person, on the phone. We pull out of the parking lot, to the first intersection. We caught a red light. While setting there; here comes a perp, riding a bicycle on the sidewalk. He had a bright orange helmet, a basket on the back of his bicycle, filled with America Flags. I’ve caught trucks and vans before, dropping this kind of trash off, along my routs. It’s just another kick in the nuts. They love to throw the American flag, in my face, after the bullshit we just went through. Yep, folks, these people are proud as hell, for harassing a total stranger, and his service dog. By Golly, this is the United States of Merica. I’m sure you have seen, the Village Idiot, driving around in his big truck. Brandishing a huge American flag, in the truck bed. Doing this with pride, totally ignorant, of our own Constitution.

After I got home, I decided to check the 1st Autozone store, I went to. I wanted to see if they did have the part I needed. Yes, they did. I put in the Autozone store #2784, at 435 N Litchfield, Goodyear, Arizona. I searched the part number, and they had it in stock, the whole time. I took a screenshot, just to cover myself.

 

Any given week; tens of thousands, of Americans, are treated like this. This is what many Americans, are teaching their children. The many involved in Gangstalking, and Workplace Mobbing. This is why, the American workplace, has become so toxic. This is what pushes many Americans, over their limits. This is one of the many reasons, we have trouble keeping quality Law Enforcement.

 

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Average November rainfall in Brasília is 227mm (9 inches). Rains yesterday pushed November total to over 50% above average.

Best viewed in lightbox - please click on the image or press L.

 

Z to zoom in.

  

© All rights reserved R.Ertug

Please do not use this image without my explicit written permission.

 

Spring and fall are the best times of year for sightseeing in Istanbul. The weather is pleasant, with comfortable temperatures averaging around 15°C. While spring is high season in Istanbul, crowds don’t reach their peak until late May. In the fall, the number of tourists who arrive begins to dwindle, with the crowds thinning by early October. Many feel that spring is the best time of all, and particularly April, when the entire city is in bloom for the International Tulip Festival held throughout the month. Still, autumn is the time when the city comes alive in a gamut of colors, both somber and bright, while the light rain and glorious sunsets make for an impressionist painting of sorts. When visiting in the spring, summer or fall, the most pleasant time to experience Istanbul’s top sights is early in the morning, soon after opening, or late in the day. Popular Topkapi Palace is best visited on a Monday morning when it’s usually at its quietest. In winter, you can usually arrive at any time and find no queue or crowds. Summer is just the opposite, arguably the worst time to visit due to the sweltering heat, massive amounts of people visiting the city, and the lines for attractions and other tourist sites. As the major sights in Istanbul all have their own closing days and slightly different operating hours, be sure to check with each one before planning your itinerary.

 

EMIRGAN PARK -

  

The Emirgan Park is a historical urban park located at the Emirgan neighbourhood in the Sarıyer district of Istanbul, Turkey, on the European coast of the Bosphorus. It is one of the largest public parks in Istanbul.

 

In the Byzantine era, the entire area, where today the park stretches, was covered with cypress trees and known as "Kyparades" or "Cypress Forest". It became known as "Feridun Bey Park", when the uninhabited land was granted in the mid-16th century to Nişancı Feridun Bey, a Lord Chancellor in rank in the Ottoman Empire.

 

In the 17th century, Ottoman sultan Murad IV (reigned 1623-1640) presented the estate to Emir Gûne Han, a Safavid Persian commander, who surrendered his sieged castle without any resistance, and followed him back to Istanbul. The name "Feridun Bey Park" was changed to "Emirgûne", which in time became corrupted to "Emirgan".

During the centuries, the estate's owner changed several times, and by the end of the 1860s, it was owned by Khedive Ismail Pasha (reigned 1863-1879), Ottoman governor of Egypt and Sudan. The area was used as the backyard of a large wooden yalı that he built on the shore of the Bosphorus. Further, he built within the park area three wooden pavilions, which still exist.

The heirs of the Khedive's family sold the estate in the 1930s to Satvet Lütfi Tozan, a wealthy Turkish arms dealer, who granted the park grounds, the three pavilions included, later in the 1940s to the City of Istanbul during office of Governor and Mayor Lütfi Kırdar (1938-1949).

 

The park today-

 

A pond with fountain in the Emirgan Park

The park, owned and administered today by the Metropolitan Municipality of Istanbul, covers an area of 117 acres (470,000 m2) on a hillside, and is enclosed by high walls.

Inside the park with two decorative ponds are plants of more than 120 species. The most notable rare trees of the park's flora are: Stone Pine, Turkish pine, Aleppo Pine, Blue Pine, Eastern White Pine, Maritime Pine, Japanese Cedar, Norway Spruce, Blue Spruce, Atlas Cedar, Lebanon Cedar, Himalayan cedar, Beech, Ash tree, Sapindus, Babylon Willow, Hungarian Oak, Colorado White Fir, Maidenhair tree, California incense-cedar, Coast Redwood and Camphor tree.

Many jogging tracks and picnic tables make the Emirgan Park a very popular recreation area for the local people, especially during the weekends and holidays.The three historic pavilions, called after their exterior color as the Yellow Pavilion, the Pink Pavilion and the White Pavilion were restored in time between 1979-1983 by the Touring and Automobile Club of Turkey under its CEO Çelik Gülersoy, and opened to the public as cafeteria and restaurant.

The Emirgan Park is closely associated with the tulip, the traditional flower, which gave its name to an era (1718-1730) of the Ottoman Empire. A special garden was established in Emirgan Park in the 1960s to revive the city's tradition of tulip cultivation. Since 2005, an annual international tulip festival is organized here every April making the park attractive and very colorful with these flowers.

  

The Yellow Pavilion - Sarı Köşk is a large wooden mansion in the form of a chalet built by Khedive Ismail Pasha between 1871-1878 as a hunting lodge and guest house.

Situated in the center of the park and overlooking the Bosphorus, the two-storey mansion with one balcony, one terrace and a basement is constructed on an area of 400 m2 (4,300 sq ft). It consists of four rooms, one hall and a kitchen in the lower floor and three rooms and one salon in the upper floor. Its layout reflects the architecture of the traditional Ottoman house with a salon encircled by many living rooms.

 

The ornaments at the ceilings and the walls were the work of the court architect Sarkis Balyan. The ceilings are enriched with oil painted flower figures and the facades with outstanding carvings. The high doors and windows, as well as the opulent interior decorations in bright colors reflect the glory of that era.

A pond is situated to the northeast, next to the mansion.

Used only by the owners from the very beginning, the pavilion was restored within four months in the beginning of the 1980s with due diligence, furnished with antiques and opened to the public as a cafeteria.The Yellow Pavilion, the main base of the park, is run since 1997 by Beltur, the tourism company of the Metropolitan Municipality of Istanbul. Up to 100 guests can be served at the premise in summer and winter time.

 

The Pink Pavilion - Pembe Köşk, one of the three mansions in the park built by Khedive Ismail Pasha, is a two-storey, typical Ottoman house. Named after its exterior's original color of cranesbill flower pink, the pavilion reflects the glory of its history with fine ornaments.

The pavilion is used as a cafeteria on weekends. Furthermore, it available for conventions and wedding ceremonies. In the summer months, the premise can accommodate up to 350 guests, for cocktails up to 500 people. In the winter time, groups of up to 150 guests can be served.

  

The White Pavilion - Beyaz Köşk is the third mansion within the Emirgan Park built by Khedive Ismail Pasha. It is only 150 m (490 ft) far from the Yellow Pavilion. The two-storey wooden building bears the architectural characteristics of the neo-classical style.

The mansion is used in the daytime as a cafeteria and in the evenings as a restaurant of Turkish-Ottoman cuisine.

  

via Instagram ift.tt/2fOjBAO

Grind: Extra Fine (Average Circles & Effect: Auto Adjust), Brew: Rings (No Pic & Full Blended Circles), Serve: Black (Flash Burn Tone & Smooth Texture)

Chartwell House is only a half hour drive from us so during the quiet season we sometimes visit for a walk in the grounds. On this particular occasion the house was swathed in fog and pretty much deserted. You could almost feel the presence of its former owner.

 

For those of you not aware Chartwell was the principal adult home of Sir Winston Churchill, Britain's famous wartime leader. Churchill and his wife Clementine bought the property, located two miles south of Westerham, Kent, England, in 1922. Extensive renovations simplifying and modernising the home were undertaken directly, completely transforming it when complete.

 

When it became clear to the Churchill's in 1946 that they could not afford to run the property, a consortium of wealthy businessmen organised by Lord Camrose purchased the estate. The arrangement was that for payment of nominal rent both Sir Winston and Lady Churchill would have the right to live there until they both died, at which point the property would be presented to the National Trust. When Sir Winston died in 1965, Clementine decided to present Chartwell to the National Trust immediately.

 

6 exposure, tripod mounted hdr -3 to +2 at 1ev spacing. pp with acr, photomatix, photoshop, topaz clarity & de-noise. Fuji X-E2 with 18-55 f2.8-4 at 18mm, f16, average exposure 1/13 sec, ISO 200. I'm still getting to grips with this lightweight marvel.

Deutschland / Baden-Württemberg - Mainau

 

Mainau [ˈmaɪnaʊ] also referred to as Mav(e)no(w), Maienowe (in 1242), Maienow (in 1357), Maienau, Mainowe (in 1394) and Mainaw (in 1580) is an island in Lake Constance (on the Southern shore of the Überlinger See near the city of Konstanz, Baden-Württemberg, Germany). It is maintained as a garden island and a model of excellent environmental practices. Administratively, the island has been a part of Konstanz since December 1, 1971, when the municipality of Litzelstetten, of which Mainau was part, was incorporated into Konstanz. Mainau is still part of Litzelstetten, now one of 15 wards (administrative subdivisions) of Konstanz.

 

The island belongs to the Lennart Bernadotte-Stiftung (eng. The Lennart Bernadotte Foundation), an entity created by Prince Lennart Bernadotte, Count of Wisborg, originally a Prince of Sweden and Duke of Småland. It is one of the main tourist attractions of Lake Constance. Beside flowers there is a park landscape with views on the lake. There is a greenhouse as well with tropical climate and thousands of butterflies.

 

Mainau Bay is the location of their university's sailing club.

 

Geography

 

Position

 

The island averages out at a height between 395 metres (1,296 ft) (roughly equals the lake’s average medium water-level) and 425 meters (1,394 ft) above sea level. Its highest peak is located at the Großherzog-Friedrich Terrace (historic water reservoir). Mainau Island is 610 metres (2,000 ft) long from North to South and a 1,050 meters (3,440 ft) wide from West to East. The island’s circumference is about three kilometers (1.9 mi). The shortest distance between the downwelling molasse slice and the lake’s shore is about 130 meters (430 ft).

 

Population

 

Few people inhabit Mainau Island. Due to its small amount of inhabitants, it is considered a hamlet. Meyer’s Lexikon’s issue of 1888 declared that 28 people lived on Mainau Island. During the census of 1961, a population of 123 was verified. Count Björn Bernadotte is living in the castle on Mainau Island.

 

Parks and gardens

 

Mainau Island is a "flowering island" notable for its parks and gardens. Frederick I, Grand Duke of Baden, created the island's arboretum, which now contains 500 species of deciduous and coniferous trees, many exotic and valuable, including fine specimens of Sequoiadendron giganteum (1864) and Metasequoia glyptostroboides (1952). The island also contains about 200 rhododendron and azalea varieties.

 

Due to the advantageous climate at the lake, palm trees and other Mediterranean plants can grow on the drop-shaped island. Because of its rich subtropical and partly even tropical vegetation, Mainau Island is also called "flowering island in the Lake Constance". Count Lennart Bernadotte, who died in 2004, liked to call his island "Blumenschiff" (engl. flower ship). He also described the famous destination as follows: "She is a coquettish little Lady, Mainau Island, who constantly demands much attention, even more love and ceaselessly new clothes." - Lennart Bernadotte. By "new clothes", he probably meant the blossoms, plants and flower-beds which are constantly renewed by the gardeners.

 

Apart from the historic buildings, the centerpiece of Mainau Island is the Arboretum with its 500 different types of rare and valuable broad-leaved trees and conifers, which was created in 1856 by grand duke Friedrich I. Among those is one of Germany's "oldest" dawn redwood trees (Metasequoia glyptostroboides). The tree, which originated from China, was planted on the island in 1952, when it was just 70 centimeters (28 in) tall. Particularly mighty are some exemplars of the giant redwood (Sequoiadendron giganteum). Their seeds came from California in 1853 and were planted on the island in 1864, which makes them one of the oldest of their kind in Europe. You can find the above-mentioned giant redwoods as well as Cedars, Dawn Redwoods and Tulip Poplars on the island. The Arboretum expands towards the north-west of the island.

 

Spring marks the beginning of the "Blumenjahr" (eng. Flower Year) with an exhibition of orchids. From March to May you can see several types of flowers in full bloom, like Tulips, Daffodils, Primroses, Forget-Me-Nots and Hyacinths. To show the full beauty of all these flowers the so-called „Frühlingsallee“ (eng. Spring Alley) was opened, which is a path across the island surrounded by beds of these plants. From May to June over 200 kinds of Rhododendrons and Azaleas are in full bloom. To the west of the "Comturey-Keller" you can find an Italian rose garden commissioned by Friedrich I. This rose garden is strictly geometric and consists of pergolas, sculptures and fountains. In general, over 1200 kinds of roses can be found on the island.

 

„Frühlingsallee“ leads to „Mediterran-Terrassen“ (eng. Mediterranean Terrace) where exotic plants such as palm families, agaves, cacti and bougainvillea are presented in pails during summer. Lake Constance and its surroundings as well as the Alps can be seen in a panoramic view from here. In July the blossoms of brugmansia and hibiscus are blooming on Mainau Island and in August the blossoms of passion flowers bloom.

 

On the southern end you can find “Südgarten” (eng. South Garden) where in autumn fields of dahlia with approximately 20,000 dahlia bushes and 250 varieties gleam from September until October. Spring and summer flowers such as different kinds of fuchsia are growing on the affiliated shore garden to the eastern side of “Südgarten”.

 

The “Bodenseerelief” (eng. Relief of Lake Constance) is a very popular photo motive. It is a relief with the picture of a flower which is changed by season. A small harbor with a landing place is situated to the northern side of Mainau Island. Excursion boats lay in here and another entrance to “Frühlingsallee” can be found here.

 

History

 

Until the Napoleonic mediatisations and secularisations of small German fiefs this island belonged to the Order of Teutonic Knights. It was later sold into private ownership. In 1853 Grand Duke Frederick I of Baden purchased the island as his personal property and used the palace built by the Teutonic Knights as summer palace. At the end of World War I Baden became a republic with the abdication of Grand Duke Frederick II, son of Frederick I. The former Grand Duke retained his private property including Mainau. When he died childless in 1928 the island passed to his sister Victoria of Baden, wife of King Gustaf V of Sweden. Upon her death two years later she bequeathed the island to her second son Prince Wilhelm, Duke of Södermanland and his descendants. In 1932 Prince Wilhem gave Mainau to his only child Lennart Bernadotte who owned it until 1974 when he transferred the island to a foundation. Count Bernadotte formed Enterprise Mainau GmbH in 1991 as a private enterprise to manage the island for the benefit of the Lennart Bernadotte-Stiftung. The Count remained active in managing Mainau until his death in 2004 but had appointed his second wife Sonja co-manager in 2001. Widowed, she and their children ran both the foundation and the management company until 2007. Since January 2007 Bettina Bernadotte, the eldest daughter of Lennart and Sonja, directs the Mainau GmbH as current manager, and since 2011 her brother Björn Bernadotte has joined her.

 

Pre- and Early History

 

In 1862, signs of an earlier population were discovered along the south banks of Mainau and soon exploited by domain administrator Walter: among the items were wedges, a potsherd, flint splinters, an axe and a muller. The pile dwelling settlement made up of six houses was uncovered in the 1930s and dated back to the Neolithic Age ( 3.000 b.c.). Lake-dwelling settlements of the Neolithic and the Bronze Age were located along the northern shore and the southwestern island along the shallow water zone.

 

(Wikipedia)

 

Die Insel Mainau, als Mav(e)no(w), Maienowe (1242) bzw. Maienow (1357), Maienau, Mainowe (1394) und Mainaw (1580) erwähnt, ist mit etwa 45 Hektar Fläche die drittgrößte Insel im Bodensee. Der Molassekalkfelsen befindet sich im Überlinger See genannten, nordwestlichen Teil des Bodensees. Sie ist vom Südufer des Überlinger Sees über eine Brücke zu erreichen und verfügt über einen Schiffsanleger, der von Kurs- und Ausflugsschiffen der Weißen Flotte bedient wird. Die nächsten größeren Städte sind Konstanz, Meersburg und Überlingen. Die Insel gehört zum Stadtteil Litzelstetten der Stadt Konstanz und befindet sich seit 1974 im Besitz der von Graf Lennart Bernadotte gegründeten gemeinnützigen „Lennart-Bernadotte-Stiftung“. Die gräfliche Familie ist bis heute wichtiger Teil der Attraktion der Mainau. Die Insel liegt an der Oberschwäbischen Barockstraße.

 

Geographie

 

Lage

 

Die Insel liegt auf einer Höhe zwischen 395 (Seeniveau bei mittlerem Wasserstand) und 425 Meter über Normalnull. Der höchste Punkt ist laut amtlichen Karten bei der Großherzog-Friedrich-Terrasse (historisches Wasserreservoir auf dem Vogelherd). Ihre Nord-Süd-Ausdehnung beträgt 610 Meter, ihre größte Breite (West-Ost) rund 1050 Meter. Der Umfang der Insel beträgt rund drei Kilometer. Die kürzeste Entfernung der abgesunkenen Molassescholle zum Seeufer beträgt 130 Meter.

 

Bevölkerung

 

Die Insel Mainau hat nur wenige Einwohner, Meyers Konversationslexikon von 1888 gab eine Bevölkerung von 28 an. Zur Volkszählung 1961 war eine Bevölkerung von 123 nachgewiesen. Auf der Insel Mainau lebt Björn Graf Bernadotte mit seiner Familie.

 

Anlage

 

Park- und Gartenanlagen

 

Bedingt durch das günstige Bodenseeklima wachsen auf der tropfenförmigen Insel Palmen und andere mediterrane Pflanzen. Wegen ihrer reichen subtropischen, teilweise auch tropischen Vegetation wird die Mainau auch als „Blumeninsel im Bodensee“ bezeichnet. Der 2004 verstorbene Graf Lennart Bernadotte nannte seine Insel gerne das „Blumenschiff“. Weiterhin beschrieb er das bekannte und für Besucher gegen Eintrittsgelder zugängliche Ausflugsziel mit folgenden Worten:

 

„Sie ist eine kokette kleine Dame, diese Mainau, die stets und ständig große Aufmerksamkeit fordert, noch mehr Liebe und vor allem unaufhörlich neue Kleider.“

 

– Lennart Bernadotte

 

Wobei er mit den „neuen Kleidern“ zuerst den immer wieder neu von Gärtnerhand gewebten Blütenüberwurf gemeint haben mag.

 

Herzstück der „Blumeninsel“ ist neben den historischen Gebäuden das von Großherzog Friedrich I. ab 1856 angelegte parkähnliche Arboretum der Insel Mainau mit seinen 500 verschiedenen Arten von zum Teil seltenen und wertvollen Laub- und Nadelgehölzen. Darunter befindet sich einer der ältesten Urweltmammutbäume (Metasequoia glyptostroboides) Deutschlands. Der aus China stammende Baum war 1952 als 70 Zentimeter großes Bäumchen im Ufergarten ausgepflanzt worden. Besonders mächtig sind einige Exemplare des Riesenmammutbaums (Sequoiadendron giganteum). Die Samen dieser Bäume kamen 1853 aus Kalifornien, und 1864 ließ Friedrich I. zahlreiche Bäume auf der Mainau pflanzen. Damit gehören sie zu den ältesten ihrer Art in Europa. Neben den riesigen Mammutbäumen befinden sich Zedern, Metasequoien und Tulpenbäume. Das Arboretum dehnt sich nordwestlich vom Schloss auf der Hochfläche aus.

 

Im Frühjahr Ende März/Anfang April beginnt auf der Mainau das Blumenjahr im Palmenhaus mit einer großen Orchideenschau. Von Ende März bis Mitte Mai blühen auf der Mainau Tulpen, Narzissen und Hyazinthen. Hierzu wurden im östlichen Teil der Insel an der sogenannten „Frühlingsallee“ parallel zum Weg Tausende von Tulpen-, Narzissen- und Hyazinthenzwiebeln gepflanzt. Ebenfalls im Frühjahr gedeihen auf der Insel Stiefmütterchen, Vergissmeinnicht und Primeln.

 

In der Übergangszeit von Mai und Juni zeigen sich die Blüten der 200 Rhododendren- und Azaleensorten. Westlich des Comturey-Kellers kommt man zu dem ebenfalls durch Großherzog Friedrich I. im italienischen Stil angelegten Rosengarten. Der sogenannte „italienische Rosengarten“ ist eine streng geometrische Anlage mit Pergolen, Skulpturen und Brunnen. Im Sommer betört der Duft der rund 500 verschiedenen Rosensorten, vor allem Beetrosen. Auf der ganzen Insel finden sich etwa 30.000 Rosenstöcke von 1200 Sorten. Eine Barocktreppe führt hinauf zur aussichtsreichen Schlossterrasse.

 

Die „Frühlingsallee“ führt zu den „Mediterran-Terrassen“ mit ihren exotischen Kübelpflanzen, wo im Sommer Palmengewächse, Agaven, Kakteen und Bougainvilleen gezeigt werden. Von hier hat man ein Panorama auf die Bodenseelandschaft. Im Juli zeigen sich auf der Mainau die Blüten der Engelstrompeten und des Hibiskus, im August die der Passionsblumen.

 

Südlich breitet sich der „Südgarten“ aus, wo im Herbst von September bis Oktober die Dahlienfelder mit etwa 20.000 Dahlienbüschen von 250 Sorten blühen. Im östlich anschließenden Ufergarten wachsen Frühlings- und Sommerblumen, darunter eine Sammlung verschiedener Fuchsienarten. Ein beliebtes Fotomotiv ist das Bodenseerelief, ein nach Jahreszeit unterschiedlich gestaltetes Blütenbild in Form des Bodensees.

 

An der Nordseite der Insel liegt der kleine Hafen mit Schiffsanlegestelle, wo die Ausflugsschiffe anlegen und es einen weiteren Eingang gibt.

 

Im ganzjährig geöffneten Schmetterlingshaus auf der Insel, mit etwa 1000 Quadratmeter das zweitgrößte seiner Art in Deutschland, können Besucher zwischen 25 °C und 30 °C Wärme und 80 bis 90 Prozent Luftfeuchtigkeit durch eine tropisch anmutende Umgebung mit Wasserfällen und exotischen Gewächsen gehen. Je nach Saison fliegen 700 bis 1000 bunte Falter bis zu 80 verschiedener Schmetterlingsarten, vor allem südamerikanischer Herkunft, frei zwischen den Besuchern. Rund ein Drittel der gezeigten Schmetterlingsarten vermehrt sich hier auf natürliche Weise. Doch ist es ganz unterschiedlich, wie viele Nachkommen es gibt. Aus diesen Gründen bekommt das Schmetterlingshaus wöchentliche Lieferungen von 400 Puppen von Züchtern aus Costa Rica, England und Holland. Rund 20.000 Euro beträgt das Budget im Jahr für neue Raupen. Die Gartenanlage rund um das Schmetterlingshaus wurde als Lebensraum für heimische Schmetterlinge gestaltet. Angeschlossen ist ein Duftgarten mit mehr als 150 Duftpflanzenarten.

 

Außer den Park- und Gartenanlagen gibt es einen Streichelzoo mit Ziegen und Ponys und den „Mainauer Bauernhof“ mit Alpakas, Hasen, Hühnern, Eseln, Schafen und Katzen sowie einige gastronomische Einrichtungen.

 

Für Kinder gibt es das rund 1100 Quadratmeter große Mainauer Kinderland „Wasserwelt“, einen Spielplatz mit einem 60 Zentimeter tiefen Wasserbecken, das von Flusssteinen mit einem Gesamtgewicht von rund 130 Tonnen eingefasst wird. In der Mitte des mit 170 Kubikmeter Wasser gefüllten Sees liegt eine Insel. Auf dem See können die Kinder mit Flößen umherfahren oder sich mit einer Holzfähre hinüberziehen. Rundherum stehen Holzhäuser als Klettergerüste, die laut Planern an die Zeit der Pfahlbauten erinnern sollen. Verbunden sind die Häuschen durch Hängebrücken und Kettenstege. Dazu gibt es Wasserrinnen und extra Matschtische. Falls ein Kind beim Spielen allzu tief in die Wasserwelt eingetaucht sein sollte, haben die beiden Mainauplaner Matthias Wagner und Markus Zeiler auch vorgesorgt: Am Spielplatz wurde in einem Kiosk ein Wäschetrockner aufgestellt, in dem die Eltern nasse Kleidungsstücke selbst trocknen können. Die Spiellandschaft wird wie alle anderen Spielplätze vom TÜV SÜD abgenommen und regelmäßig inspiziert.

 

(Wikipedia)