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The complex is located inside Osówka Mountain (German: Säuferhöhen) 50°40′22″N 16°25′14″E. It is accessible by tunnel number 1 (120 m) with chambers for guardrooms and tunnel number 2 (456 m), bored 10 m below the level of the main underground, with guardrooms close to completion. Behind them there is a connection of two levels created by the collapse of the ceiling.The structure is a grid of tunnels (1,750 m, 6,700 m2, 30,000 m3) and underground halls, up to 8 m in height. Only 6.9% is reinforced by concrete.There is a shaft leading to the surface with a diameter of 6 m (48 m).[99] Tunnel number 3 (107 m) is not connected to the complex. It is 500 m away and 45 m below the main underground.It contains two dams and hydraulic equipment of an unknown purpose.
Above ground are foundations of buildings, machinery, a ramp for transportation of mine cars to different levels, a reservoir of water and depots, some with systems of heating up building materials in winter.The largest structure is a single-storey, concrete building (680 m2, 2,300 m3) with walls 0.5 m thick and roof adapted for camouflage by vegetation (0.6 m). A utility tunnel (1.25 m x 1.95 m, 30 m) was under construction to connect it with the shaft. Another structure of unknown purpose is a concrete monolith (30.9 m x 29.8 m) with tens of pipes, drains and culverts, buried into the rock at least 4.5 m.A narrow gauge railway network connected the tunnels with the railway station in the village of Głuszyca Górna (German: Oberwüstegiersdorf).
In August 1944, AL Säuferwasser was established for prisoners of concentration camps 50°40′17″N 16°24′50″E.[88][38] They were Jews, citizens of Poland, Hungary, and Greece. The remains of the camp can still be found in the vicinity of the tunnel number 3. Its evacuation took place in February 1945.
The result of a 'CCBS only' build session with my son for Hero February! There is something uniquely intuitive and inspriring about CCBS for kids, it works perfectly for what it sets out to do - be an accessible system to create characters quickly! My son built the hero while I was on villain duty (of course) and he named his character and we came up with a scenario.
I quote: The hero is called 'Mutt', has lava, fire and plasma powers, is strong (!), and his silver armor pieces are 'instructible'. (sic)
That last bit apparently meant indestructible!
Also, technically a collab?
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When a group of archaeologists brought back an alien monolith from an uninhabited planet to Makuhero City's museum, little did they know it was an ancient containment device for a malevolent being whose body is fluid - and that they inadvertently unsealed it.
When the creature escaped after eons of imprisonment, it occupied another exhibit - an incomplete, ancient suit of armor - and went on a rampage while looking for a more suitable vessel, one it wouldn't be constantly dripping out of.
Rookie hero 'Mutt' was deployed to the location, where he used his lava and plasma powers to subdue the creature and seal it back. At least, most of it...
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More images: www.instagram.com/p/DF6dw7sIjci
Today, I'm starting a new series focusing on tiki drinks. The goal is to learn the ins and outs of tiki and rum. In order to make this more accessible, nearly all of these recipes will be achievable six rums. Certainly, one could (as I have) buy and use far more rums, but with these six rum types should empower your bar in order to make a diverse menu.
Dark Jamaican rum: One of the most frequently used rums in tiki. It's strong and funky and can stand up to potent other flavors in your tiki exotics.
Recommended bottles: Hamilton Jamaican Pot Still Black, Coruba, Myer's (in a pinch)
White Cuban-style rum: Another frequently used rum. This is the counter-balance to the dark Jamaican rum's intensity. These rums are quite dry, more subtle.
Recommended bottles: Caña Brava 3 year, Flor de Caña 4 year, Plantation 3 Stars
Aged Barbados rum: A versatile rum for adding a lot rum character with oak/wood aging flavor and another frequently used rum throughout most tiki recipes. These rums bring their own tropical flavor notes not always found in the above rums. Recommended bottles: Plantation Barbados 5 year, Mount Gay Black Barrel, Real McCoy 5 year
Aged Jamaican rum: Some recipes would be woefully incomplete without this gem, like the Zombie. Like its dark cousin, this offers the strong funky, but this is without the extra molasses flavor. Instead we get the aged oak/wood character.
Recommend bottles: Appleton Signature (or Reserve, or 12 year), Plantation Xaymaca Special Dry
Rhum Agricole Blanc: This is the black sheep of the group so far. These rums only come from Martinique and are made with fresh sugarcane juice, not molasses. The flavor is grassy, a little funk and dry. Admittingly, not as common, but still critical for drinks like the Mai Tai.
Recommend bottles: La Favorite Blanc, Neisson Blanc, Rhum J.M. Blanc
Overproof Demerara rum: Unique to tiki is a bit of danger with this firestarter (it is quite flammable actually). These rums bring a lot of intensity, which is why we use them sparingly.
Recommended bottles: Hamilton Demerara 151, Lemon Hart & Son 151, Plantation O.F.T.D.
Liqueurs: Falernum is a rum based liqueur with lime and spices and it's frequently used and key to many recipes.
Recommend bottles: John D. Taylor Velvet Falernum, Bitter Truth Golden Falernum
Dry Curaçao is an orange liqueur and critical to the flavor of many classic tiki drinks.
Recommended bottles: Pierre Ferrand Dry Curaçao
Herbsaint or Absinthe are very anise-forward and used in small amounts for certain recipes, especially from Donn the Beachcomber.
Angostura bitter, you should have this.
Syrups: Simple syrup is compulsory. Honey Syrup and Grenadine are frequently used and are often the lynch to getting a recipe just right. Orgeat is an almond based syrup and often that odd quality that makes something go from pedestrian to exotic rum rhapsody. Making your own is possible, but laborious. Commercial bottles vary widely in quality, so don't cheap out.
Recommend orgeats: Small Hand Foods, Giffard, Bougie Syrups. Avoid Monin or anything with artificial flavors. These tastes like chemicals and will ruin your drinks.
Fruit: Limes. So many limes. Don't buy bottled juice. Fresh is critical.
Lemons, again. Fresh, not bottled.
Oranges and Grapefruit are where I'm okay with bottled. This partly because juicing them is tiresome and frustrating low yield. Plus you can drink the juice with breakfast. That said, fresh still has better flavor.
Pineapple are used a few ways. There's the juice which you will need. Bottled juice is acceptable, but fresh is ridiculously better. Juicing your own pineapple is definitely a labor of love since you'll need a blender and a sieve. Pineapple chunks and leaves make great garnishes. Also, you can eat it for a healthy snack.
Coconut. So don't try fresh...please. These only get used twice (Piña Colada and Painkiller), but this wouldn't be complete without discussing this. I use a 4:1 blend of Coco Lopez and unsweetened coconut milk throughly mixed together and stored in a jar in the fridge.
Schweiz / Berner Oberland - Jungfraujoch
Aletsch Glacier seen from Sphinx Observatory.
Aletschgletscher gesehen vom Sphinx-Observatorium.
The Jungfraujoch (German: lit. "maiden saddle") is a saddle connecting two major 4000ers of the Bernese Alps: the Jungfrau and the Mönch. It lies at an elevation of 3,463 metres (11,362 ft) above sea level and is directly overlooked by the rocky prominence of the Sphinx. The Jungfraujoch is a glacier saddle, on the upper snows of the Aletsch Glacier, and part of the Jungfrau-Aletsch area, situated on the boundary between the cantons of Bern and Valais, halfway between Interlaken and Fiesch.
Since 1912, the Jungfraujoch has been accessible to tourists by the Jungfrau line, a railway from Interlaken and Kleine Scheidegg, running partly underground through a tunnel through the Eiger and Mönch. The Jungfraujoch railway station, at an elevation of 3,454 metres (11,332 ft) is the highest in Europe. It lies east of the saddle, below the Sphinx station, and is connected to the Top of Europe building, which includes several panoramic restaurants, shops, exhibitions, and a post office. Several tunnels lead outside, where secured hiking trails on the crevassed glacier can be followed, in particular to the Mönchsjoch Hut. The normal route to the Jungfrau and Mönch starts from there.
The Sphinx Observatory, one of the highest astronomical observatories in the world, provides an additional viewing platform at a height of 3,572 metres (11,719 ft), the second-highest in Switzerland. It can be reached by an elevator from the Jungfraujoch. The observatory houses one of the Global Atmosphere Watch's atmospheric research stations. The Jungfraujoch radio relay station, which is not accessible to the public, is installed west of the Jungfraujoch, on the Jungfrau ridge. It is Europe's highest radio relay station.
Etymology
Swiss and Austro-Bavarian German Joch (lit. 'yoke') is a term for 'ridge between two higher peaks' recorded in the 14th century (Grimm, Deutsches Wörterbuch "bereits im 14. jahrh. als ortsname: des gotzhus zwing und ban vahet an Rotenhalden und denne die roten bachtalen uf unz an den grat, und den grat obnan hin ob Grüblen hin iemerme, unz an Joch. und ab Joch unz an Stoerben. weisth. 1, 4 (Zürich)").
The name Jungfrau ('maiden, virgin'), which refers to the highest mountain overlooking the Jungfraujoch, is most likely derived from the name Jungfrauenberg given to Wengernalp, so named for the nuns of Interlaken Monastery, its historical owner. However, the "virgin" peak was heavily romanticized as a "goddess" or "priestess" only in late 18th- to 19th-century Romanticism. After the first ascent in 1811 by Swiss alpinist Johann Rudolf Meyer, the peak was jokingly referred to as Mme Meyer (Mrs. Meyer).
Geographic setting
The Jungfraujoch is a snow saddle located directly between the summits of Mathildespitze (west) and Sphinx (east). It is, however, most notably the lowest point between the Jungfrau and the Mönch, respectively third and fourth highest mountains in the Bernese Alps, and the key col of the former. The south side (canton of Valais), almost flat, is constituted by the Jungfraufirn, one of the branches of the Aletsch Glacier, the longest in the Alps. From the south, the Jungfraujoch can be relatively easily accessed by mountaineers in two days from the region of Fiesch, via the Konkordia Hut. The north side (canton of Bern) is almost vertical with a difference of height of nearly 3,000 metres from the bottom of the valley at Interlaken, with no easy natural access. For those reasons, the only easy and quick access to the Jungfraujoch is through the 7 kilometre-long tunnel of the Jungfrau Railway, accessed via Kleine Scheidegg on the north side, the railway pass between Lauterbrunnen and Grindelwald.
Administrativelly, the Jungfraujoch is split between the territories of the municipalities of Lauterbrunnen and Fieschertal. Nearly all built infrastructure, including the Jungfraujoch railway station, Top of Europe complex and the Sphinx Observatory, are on the Valais side of the border, therefore in the municipality of Fieschertal. The ridge between the Jungfrau and the Mönch is a major European watershed as well. The north side is drained by the Weisse Lütschine, the Aare and the Rhine. The south side is drained by the Massa and the Rhone.
First crossing
There is a tradition in the Bernese Oberland, supported by some documentary evidence, that a pass existed between Grindelwald and Fiesch in Valais in the late medieval period, later lost to the advancing glaciers. With the early development of tourism in Switzerland and the exploration of the High Alps in the 19th century, there were once again attempts to traverse the great ridge that encloses the head of the Aletsch Glacier, and connecting Fiesch with Grindelwald and Wengernalp. Four such routes were found, with the Jungfraujoch and the Eigerjoch being among the most difficult passes in the Alps, despite the former having a relatively easy southern approach on the Aletsch Glacier.
The first ascent of the north side of the Jungfraujoch succeeded in July 1862, by a party of six English climbers and six Swiss guides: Leslie Stephen, F. J. Hardy, H. B. George, Living, Moore, and Morgan, with Christian Almer, Christian and Peter Michel, Ulrich Kauffmann, P. Baumann, and C. Bohren as guides. The time of ascent from Wengernalp was nine hours.
The party turned back on the first day at a bergschrund, returning on the following day with a ladder 25 ft (7.6 m) in length, carried by Peter Rubi, a porter from Grindelwald. The way lay at first by the rocky buttress of the Mönch, separating the Eiger and Guggi glaciers. From the buttress the route descended a short distance in order to reach the Guggi Glacier, which could be ascended to a plateau. This halting place was reached in about three hours.
Above the bergschrund was a second and smaller plateau which was situated immediately under the long slopes of broken neve that lay below the saddle. The final and very arduous stage in the ascent was a single patch of dark rocks jutted out from the snow in the ridge connecting the Jungfrau with the Mönch. After more than an hour of climbing, a great wall of ice, whose projecting cornice of snow was fringed by long icicles, had to be avoided bearing left in the direction of the Mönch, along the base of the wall by a slippery pathway of ice formed from the dripping from the icicles above. At a point where the pathway thinned out nearly to a point, and was cut across by a transverse crevasse, the wall became low enough to be scaled by the ladder. This was the last serious obstacle: a moderate slope of névé, unbroken by crevasses, then led up to the summit of the saddle.
After reaching the first patch of rocks, a short way below the saddle on the south side, the party divided: George and Moore, with C. Almer and U. Kaufmann went down to the Eggishorn and Fiesch, therefore completing the first crossing of the Jungfraujoch, while the remainder of the party returned to Grindelwald by the Mönchsjoch.
Jungfrau Railway
History
Adolf Guyer-Zeller first thought of the idea of a tunnel in 1893, and at that point, he had planned to have seven stations inside the tunnel before reaching the peak of the Sphinx. The building of the tunnel started on July 27, 1896 and took 16 years to complete.[6] The construction phase was troubled by many problems including monetary shortages, inclement weather and mounting deaths due to construction accidents. The worst accident occurred in 1908, when 30 tons of dynamite accidentally exploded.
When construction finally finished, the railway reached only to the height of the Jungfraujoch saddle, rather than the summit of the Sphinx, and had only two intermediate stations. However, even in its current state, the Jungfraubahn is a significant achievement in engineering and construction, still holding the title for highest railway in Europe.
Railway
The train into the mountain leaves from Kleine Scheidegg, which can be reached by trains from Grindelwald and Lauterbrunnen. The train enters the tunnel running eastward through the Eiger shortly after leaving Kleine Scheidegg.
It runs close behind the Eiger's north face, stopping at Eigerwand, where there is a window about 8 m long and a metre high, halfway up the face. The windows have been placed in holes used to remove excavated rock from the tunnel during construction, and are also occasionally used as access points, by climbers, and also rescue parties. This window was used for one of the final scenes of a Clint Eastwood spy movie, The Eiger Sanction. There one can get off the train to admire the view before the train continues five minutes later. The tunnel then turns west, heading towards the Jungfrau. There is a second stop at a window looking out on the Eismeer ("Sea of Ice") before the train continues to the Jungfraujoch. The tunnel was constructed between 1898 and 1912; it is about 7 kilometers (4.3 mi) long, with gradients of up to 25%. The journey from Kleine Scheidegg to Jungfraujoch takes approximately 50 minutes including the stops at Eigerwand and Eismeer; the downhill return journey taking only 35 minutes.
The Jungfraujoch complex plays an important role in John Christopher's The Tripods novels.
Climate
Located above the permanent snow line, the Jungfraujoch is officially the coldest place in Switzerland, although other higher locations with no weather station, for example the top of the nearby Jungfrau and Finsteraarhorn, probably experience a more extreme climate. According to Köppen climate classification, the Jungfraujoch has an alpine climate on the border between tundra climate (ET) and ice cap climate (EF) with long, cold winters lasting most of the year and a brief period during summer where the average daily highs rise above freezing.
(Wikipedia)
The Aletsch Glacier (German: Aletschgletscher, German pronunciation: [ˈalɛtʃˌɡlɛtʃɐ]) or Great Aletsch Glacier (Grosser Aletschgletscher) is the largest glacier in the Alps. It has a length of about 23 km (14 mi) (2014), has about a volume of 15.4 km3 (3.7 cu mi) (2011), and covers about 81.7 km2 (31.5 square miles) (2011) in the eastern Bernese Alps in the Swiss canton of Valais. The Aletsch Glacier is composed of four smaller glaciers converging at Konkordiaplatz, where its thickness was measured by the ETH to be still near 1 km (3,300 ft). It then continues towards the Rhône valley before giving birth to the Massa. The Aletsch Glacier is – like most glaciers in the world today – a retreating glacier. As of 2016, since 1980 it lost 1.3 kilometres (0.81 mi) of its length, since 1870 3.2 kilometres (2.0 mi), and lost also more than 300 metres (980 ft) of its thickness.
The whole area, including other glaciers is part of the Jungfrau-Aletsch Protected Area, which was declared a UNESCO World Heritage Site in 2001.
Geography
The Aletsch Glacier is one of the many glaciers located between the cantons of Bern and Valais on the Bernese Alps located east of the Gemmi Pass. The whole area is considered to be the largest glaciated area in western Eurasia. The Fiescher and Aar Glaciers lying on the east have similar extensions.
Except the Finsteraarhorn, all the highest summits of the Bernese Alps are located within the drainage basin of the glacier. The Jungfrau and Mönch constitute the northern boundary; the Gross Fiescherhorn and Gross Wannenhorn lie on its east side; finally the culminating point, the Aletschhorn (4,193 m (13,757 ft)) is located on the west side.
Before reaching the maximum flow, four smaller glaciers converge at Konkordiaplatz:
From the western mouth flows the Grosser Aletschfirn, which runs along the northern foot of the Aletschhorn and Dreieckhorn. The Grosser Aletschfirn is supplied from the north by three notable firns: the Äbeni Flue-Firn, the Gletscherhornfirn, and the Kranzbergfirn. All of these firns have their starting points at around 3,800 m (12,500 ft). From the Äbeni Flue-Firn to the Konkordiaplatz, the Grosser Aletschfirn is 9 km (5.6 mi) long and is on average about 1.5 km (0.93 mi) wide. On the west, the Grosser Aletschfirn connects with the Langgletscher over the 3,158 m (10,361 ft) high glacier pass, the Lötschenlücke, into the Lötschental.
From the northwestern mouth flows the Jungfraufirn. This firn in fact represents the straight continuation of the Aletsch Glacier, yet is the shortest of the four tributary glaciers. It has its origin on the southern flank of the Mönch and at the eastern flank of the Jungfrau with the Jungfraujoch in-between. Up to the Konkordiaplatz, the Jungfraufirn is a scarce 7 km (4.3 mi) long, and returns to flank the Kranzberg in the west and the Trugberg in the east. At its highest point, it is 2 km (1.2 mi) wide, and further down it is still a good 1 km (0.62 mi) wide.
From the northern mouth flows the Ewigschneefäld ("Eternal snow field"), where its starting point takes the east flank of the Mönch. In an elbow, it flanks from Trugberg in the west and the Gross Fiescherhorn and Grünhorn in the east, flowing on to the Konkordiaplatz. Up to here, it is about 8 km (5.0 mi) long and averages about 1.2 km (0.75 mi) wide.
The mouth at the Konkordiaplatz it follows over a rise with a descent from 25 to 30 percent; here, the glacier is sharply split. Against the north is the Ewigschneefäld over the snow-covered pass of the Unners Mönchsjoch (3,518 m (11,542 ft)), connected with the catchment area of the Ischmeer (Wallis German for "Ice Sea"). Through the Obere Mönchsjoch (3,624 m (11,890 ft)) between the Mönch and the Trugberg stands a connection to the Jungfraufirn.
From the east, the smallest firn arrives at the Konkordiaplatz: the Grüneggfirn. Its northern arm begins below the Grünegghorn (3,860 m (12,660 ft)). The southern arm collects its snow and ice in the pot flanked by the Wyssnollen, Fiescher Gabelhorn (3,866 m (12,684 ft)), and the Chamm. Between the peaks Wyssnollen and Grünhörnli another glacier pass, the Grünhornlücke (3,279 m (10,758 ft)), connects to the Fieschergletscher. The Grüneggfirn enters the Konkordiaplatz in a gap between the mountainsides Grünegg to the north and the Fülberg to the south. On the western side of the Fülberg the Konkordia hut (mountain hut) overlooks the whole Konkordiaplatz at an altitude of 2,850 m (9,350 ft).
South of Konkordiaplatz, the glacier runs towards the valley of the Oberwallis (Upper Valais); on the east side, near Bettmeralp, lies a small glacier lake, Märjelensee (2,301 m (7,549 feet)); from the western side used to enter the Mittelaletschgletscher, but since the end of the 20th century the connection with the Aletsch Glacier has been lost. Further down, until about 1880, the Oberaletschgletscher did also enter the Aletsch Glacier at its mouth. But since then both glaciers have been retreating so far that they do not connect anymore (the Upper Aletsch Glacier did retreat about 1.3 km (0.81 mi) from its connecting point with the Aletsch Glacier), but both serve now only as the source of the river Massa. The river flows through the Lake Gibidum (a reservoir, and coincidentally representing the glacier's mouth region in the 19th century, which is a retreat of more than 4 km (2.5 mi)) and a gorge of the same name before reaching the Rhône near Brig.
Tourism
The area of the Aletsch Glacier and some surrounding valleys is on the UNESCO World Heritage list, thus it is protected and the facilities are mostly restricted to the external zones. The region between Belalp, Riederalp and Bettmeralp (which is called Aletsch Region) in Valais gives access to the lower part of the glacier. The Bettmerhorn and Eggishorn are popular view points and are accessible by cable car. The Massa river can be crossed since 2008 by a suspension bridge, thus allowing hikes between the left and the right part of the glacier.
The Jungfraujoch railway station (3,450 m) gives a direct access to the upper Aletsch Glacier as well as the normal route to the Jungfrau. It can be reached only from Interlaken in the canton Bern. Hiking paths pass the Konkordia Hut or the Hollandia Hut, eventually reaching other glaciers in the massif.
On the Riederfurka, at 2,065 metres between Riederalp and the glacier, is located the historic Villa Cassel, former summer residence of many famous and influential guests from the worlds of politics and finance. The house is now one of the centers of the environmental organization Pro Natura, which hosts a permanent exhibition about the site.
Panorama
Also at the mouth of the Konkordiaplatz from the east is the small but important Grüneggfirn (3 km long and averaging 600 m wide). This firn is connected in the over the glacier pass Grünhornlücke (3280 m high) to the Fiescher Glacier in the east.
From the Konkordiaplatz, the Aletsch Glacier has a width of approximately 1.5 km and moves at a rate of 180 m per year to the southeast on course with the Rhône valley, bordering the Dreieckhorn in the west and the great Wannenhorn in the east. It then takes a great right turn and bends ever closer to the southwest, running through the edge of the Eggishorn and Bettmerhorn of the Rhône valley. The lowest part of the great Aletsch Glacier is largely covered with detritus of the lateral and medial moraines. The glacier's toe currently lies about 1560 m high, far beneath the local tree line. From it springs the Massa stream, which flows through the Massa Canyon and is used to generate hydroelectric power. It continues through the upper half of the Brig, eventually entering into the Rhône.
The great Aletsch Glacier shows considerable ice cover. At the Konkordiaplatz, it has an ice cover of more than 900 m, but as it moves to the south, the greater part of the ice melts, gradually decreasing the cover to around 150 m.
The characteristically dark medial moraine, situated almost in the middle of the glacier, runs protracted in two bands from the Konkordiaplatz along the whole length to the glacier's toe-zone. This medial moraine is collected from the ice of three large ice fields, which all run together. The westernmost medial moraine has been named the Kranzbergmoräne, and the easternmost carries the name Trugbergmoräne.
Formation and evolution
The Aletsch Glacier resulted from the accumulation and compaction of snow. Glaciers generally form where snow and ice accumulation exceed snow and ice melt. As the snow and ice thicken it reaches a point where it begins to move due to a combination of gravity and pressure of the overlying snow and ice.
During the last glacial periods, the Aletsch Glacier was much larger than now. 18,000 years ago the lower part of the ridge, between Riederalp and the glacier, was completely covered by ice. Only the summits of the Bettmerhorn, Eggishorn and the Fusshörner were above the glacier. After an important retreat, the glacier again advanced 11,000 years ago during the last glacial period. The glacier reached the Rhône valley, and its ice the Riederfurka. Remaining moraines are still visible in the Aletsch Forest.
Since the last glaciation, the glacier generally retreated. However slight climatic changes happened and, in 1860, the glacier was 3 km longer and the ice level 200 m higher.
As for many other glaciers, records show a major longer-term retreat trend. The Aletsch Glacier receded by 3.2 km (2.0 mi) since 1870, including 1.3 km (0.81 mi) since 1980.[6] A record retreat of 114.6 metres (376 ft) happened in 2006 alone.
Since the end of the Little Ice Age in 1850 the glacier has lost 20 percent of its ice mass, considerably less than other glaciers in Switzerland, which have lost up to 50 percent. This is explained with the large size of the Aletsch Glacier, which reacts much slower to climate change than smaller glaciers. It is however estimated that, by 2100, the glacier will have only one tenth of its 2018 ice mass.
Photo opportunity
On August 18, 2007, photographer Spencer Tunick used hundreds of naked people in a "living sculpture" on the Aletsch Glacier in a photo shoot which he said was intended to draw attention to global warming and the shrinking of the world's glaciers. The temperature was about 10 °C (50 °F) at the time of the photo shoot. The 600 participants on the shrinking glacier said that they had volunteered for Tunick (a collaboration with Greenpeace) to let the world know about the effects of global warming on the melting Swiss glaciers.
(Wikipedia)
Das Jungfraujoch ist mit 3466 m ü. M. der tiefste Punkt im Verbindungsgrat zwischen dem Mönch und der Jungfrau in den Berner Alpen, auf der Grenze zwischen den Kantonen Bern und Wallis. Das Joch ist weit und stark überfirnt. Aufgrund der auch dort stattfindenden Gletscherschmelze sinkt es jedes Jahr im Schnitt einige Dezimeter ab. Es gehört zu den bedeutendsten Reisezielen in der Schweiz. Etwa 1 Million Touristen (Stand 2018) fahren jährlich zum höchstgelegenen Bahnhof Europas.
Umgebung
In der Umgebung des Jungfraujochs befinden sich einige Viertausender der Berner Alpen. Im Nordosten befinden sich der Mönch (4107 m ü. M.) sowie der Eiger (3967 m ü. M.) und im Südwesten die Jungfrau (4158 m ü. M.). Im Süden des Jungfraujochs ist hinter dem Konkordiaplatz das Aletschhorn zu sehen. 200 Meter westlich befindet sich auf dem Grat zur Jungfrau die 3557 Meter hohe Mathildespitze, etwa 600 Meter östlich des Jochs erhebt sich die Sphinx, eine markante kleine Spitze mit einer Höhe von 3571 Metern. Sie trägt eine Aussichtsplattform und ein wissenschaftliches Observatorium (Sphinx-Observatorium). In ihrem Innern befindet sich auf 3454 Metern Höhe die Endstation der Jungfraubahn. Diese Station ist der höchstgelegene Bahnhof Europas (daher der Beiname Top of Europe). Durch einen Stollen gelangt man von hier aus auf die Walliser Seite und zum Aletschgletscher. Der schnellste Aufzug der Schweiz führt auf den Gipfel der Sphinx. Ein im Sommer üblicherweise für Spaziergänger präparierter Weg führt vom Jungfraujoch zur Mönchsjochhütte. Beim Jungfraujoch selbst gibt es für Besucher keine Übernachtungsmöglichkeit. Die Stollen werden nachts verschlossen, so dass auch freies Biwakieren nicht möglich ist.
Passübergang
Als Übergang für Fuss- oder Skitouristen vom Berner Oberland ins Wallis oder umgekehrt besitzt das Jungfraujoch praktisch keine Bedeutung. Der Weg vom Wallis über den Aletschgletscher hinauf ist – von der Spaltengefahr im Jungfraufirn abgesehen – leicht. Der Aufstieg vom Berner Oberland her ist jedoch eine beschwerliche Hochtour (Steileis, G 5-6, zeitweise unmöglich).
Erschliessung
Seit dem 1. August 1912 ist das Jungfraujoch durch die Jungfraubahn erschlossen. Von Grindelwald oder Lauterbrunnen erreicht man mit der Wengernalpbahn die Station Kleine Scheidegg. Diese Station auf 2061 m ü. M. ist die „Talstation“ der Jungfraubahn. Von hier aus muss die Jungfraubahn 9,34 Kilometer bezwingen, davon verlaufen die letzten 7,32 km unterirdisch, bis sie am Jungfraujoch ankommt. Die unterirdische Endstation auf 3454 m ü. M. ist der höchste Bahnhof Europas. Auf ihrem Weg hält die Bahn an zwei Stationen: Eigergletscher (2320 m) und Eismeer (3158 m). Seit dem 11. Dezember 2016 wird die Station Eigerwand (2864 m) nicht mehr bedient.
Bauten und Anlagen
Seit 1912, mit der Eröffnung der Jungfraubahn, wird für das Wohlergehen der Besucher auf dem Jungfraujoch gesorgt. Mehrere Restaurants, aber auch spezielle Aussichtsplattformen und Erlebnisse wurden eigens dafür geplant und realisiert.
Restaurants
Bereits bei der Eröffnung weihte man das provisorische „Touristenhaus“ mit dem höchstgelegenen Restaurant Europas ein. Mit seiner Eröffnung in 1924 ergänzte das neue „Berghaus Jungfraujoch“ – mit Giebeldach und in die Felswand gebaut – dieses Touristenhaus. Es wurde als „Das Haus über den Wolken“ bekannt. Im Erdgeschoss befanden sich eine geräumige Wartehalle mit geheiztem Fussboden, Bahn- und Postschaltern und ein Bazar. Besonders ins Auge stach die „Walliserstube“, die mit der Arvenholztäfelung und Anwendung von Naturstein eine besondere Charakteristik erhielt. Gäste aus aller Welt übernachteten in einem der 18 gemütlichen, holzgetäfelten Schlafzimmer mit Waschbecken und Krügen auf dem Nachttisch. Auf der Aussichtslaube stand man am Ursprung des längsten und grössten zusammenhängenden Gletschers der Alpen, dem Aletschgletscher. 1972 wütete im Berghaus ein Feuer mit erheblichen Folgen: Lediglich das Bahnbüro, die Perronanlage in der rückwärtigen Felsenkaverne sowie die Forschungsstation konnten vor dem Feuer geschützt werden. Nach dem Unglück lud die Jungfraubahn Architekten zu einem Wettbewerb ein, ein neues Gebäude zu entwerfen. Der Gewinner war Ernst E. Anderegg mit dem im Hang eingefügten „Top of Europe“, das 1987 eingeweiht wurde.
Sphinx-Observatorium und Forschungsstation
Bereits vor Baubeginn der Jungfraubahn war die Einrichtung eines Observatoriums und einer meteorologischen Forschungsstation vom Gründer der Bahn, Adolf Guyer-Zeller, geplant. 1931 konnten die Laboratorien für Meteorologie, Glaziologie, Strahlungsforschung, Astronomie, Physiologie und Medizin auf (3571 m ü. M.) mit einem Felsenheim für 13 Forscher eingeweiht werden. 1937 wurde das Sphinx-Observatorium bezogen. 1950 wurde dem Observatorium die Kuppel für astronomische Beobachtungen aufgesetzt, die seither immer wieder den modernsten Erfordernissen der Wissenschaft angepasst wird. Das Forschungsgebäude selbst ist nicht zu besichtigen.
Unterhalb des Sphinx-Observatoriums und östlich des Bahnhofs und der Restaurants befindet sich die Hochalpine Forschungsstation, eine an die Universität Bern angegliederte Forschungseinrichtung der International Foundation High Altitude Research Stations Jungfraujoch and Gornergrat. Die Gästezimmer der Forschungsstation sind die einzige Übernachtungsmöglichkeit auf dem Jungfraujoch, aber nur Wissenschaftlern und den Betreuern vorbehalten.
Das Observatorium ist mit einem 111,4 Meter langen Lift erschlossen. Die Aussichtsplattform bietet den Besuchern bei schönem Wetter einen Ausblick bis in die Nachbarländer Frankreich, Deutschland und Italien. 1993 wurde die Sphinx für die Besucher renoviert. Drei Jahre waren nötig, um sie gemeinsam mit der schnellsten Liftanlage der Schweiz, der verglasten Aussichtshalle und der rund um das Gebäude verlaufenden Terrasse fertigzustellen.
Eispalast
Zwei Bergführer begannen in den 30er Jahren eine gewaltige Halle aus dem Gletschereis zu schneiden. In Handarbeit, mit Eispickel und Säge, entstand ein 1'000 Quadratmeter grosses Labyrinth – der Eispalast. Das 1934 begonnene Werk ist nie vollendet worden. Durch die Ausdünstung der tausenden Besucher muss die Grotte auf minus drei Grad künstlich klimatisiert werden. Die Decken und das Gewölbe der Gänge müssen regelmässig nachgehauen werden. 1992 bekam der Eispalast einen neuen Zugang und ist seit 2002 durch den Ice-Gateway erreichbar.
Post
Auf dem Jungfraujoch liegt auch das höchstgelegene Postbüro Europas mit der eigenen Postleitzahl 3801. Obwohl die Postleitzahl gemäss Schweizerischer Post dem Kanton Wallis zugewiesen ist, so befindet sie sich dennoch im Zahlengebiet 38xx der im Tal liegenden Gemeinden des Kantons Bern.
Richtstrahlstation Ostgrat
Am Ostgrat der Jungfrau auf nicht ganz 3700 Meter Höhe befand sich die 2011 abgebaute Richtstrahlstation Ostgrat. Vom Jungfraujoch führen eine teilweise durch den Gletscher geführte Stollenbahn sowie eine einspurige Standseilbahn zur Anlage. In der Mitte der Standseilbahnstrecke befindet sich eine Zwischenstation, welche für Forschungszwecke genutzt wird. Es existieren dort Photovoltaik-Testanlagen.
Versorgung
Die intensive Sonnenstrahlung bietet sich zur Energienutzung an. So wird die tagsüber einfallende Wärme für die Nacht gespeichert. Aber auch die zahlreichen sonst kaum beachteten Wärmequellen – von Lampen über Elektrogeräte bis zur Körperwärme der anwesenden Personen – werden in die Regulierung der Raumtemperatur einbezogen. So gibt es im gesamten Berghaus keinen Heizkörper. Sogar wenn die Sonne nicht scheint und die Aussentemperatur bei minus 30 °C liegt, kann tagsüber auf zusätzliche Heizungen verzichtet werden. Nur nachts wird über die Lüftungsanlage mit elektrischer Energie so viel Wärme zugeführt, dass eine Raumtemperatur von mindestens 18 °C erhalten bleibt.
Brauchwasser wird aus Schnee gewonnen und aufbereitet. In Trockenperioden muss es nach wie vor mit Zisternenwagen auf der Schiene von der Kleinen Scheidegg heraufgebracht werden. Für das Jahr 2012 ist ein neues Projekt geplant, bei dem das Wasser durch Leitungen von der Kleinen Scheidegg mit Druckluft hinauf auf das Jungfraujoch gepumpt wird. Somit können die Zisternentransporte reduziert werden.
Das Abwasser lässt sich nicht mehr in den Gletscherschrund einleiten. Deshalb wurde eine 9,4 Kilometer lange Abwasserleitung ins Tal installiert. Sämtliche Abwässer aus Küchen, Unterkünften und Toiletten können auf diese Weise umweltfreundlich entsorgt werden.
Klima
Auf dem Jungfraujoch herrschen extreme Klimabedingungen. Die mittlere Jahrestemperatur beträgt −6,7 °C mit Schwankungen von −37 °C bis +13 °C. Die Windgeschwindigkeit kann bis zu 260 km/h betragen. Die Sonne scheint jährlich durchschnittlich 1773 Stunden. Zu jeder Jahreszeit muss mit starken Vereisungen, Schneefall und Lawinen gerechnet werden. Die Messstation von MeteoSchweiz liegt auf einer Höhe von 3571 m ü. M.
Tiere
Bis zum Jahr 2009 waren auf dem Gletscher täglich 25 Polarhunde im Einsatz. Auf einer präparierten Piste (rund 500 Meter lang) zogen die Hunde Schlitten mit Besuchern, waren aber auch für Postsendungen und Lebensmitteltransporte von Wengen zum Eigergletscher im Einsatz. Das Rudel galt als das meistfotografierte Motiv auf dem Jungfraujoch.
Für Ornithologen ist die Hochgebirgsregion interessant, da verschiedene Vogelarten zum Teil auch überwintern. Der Schneefink beispielsweise nistet und schläft in den schroffen Felswänden und findet bei den Behausungen der Forscher Futter.
(Wikipedia)
Der Grosse Aletschgletscher ist der flächenmässig grösste und längste Gletscher der Alpen. Er befindet sich auf der Südabdachung der Berner Alpen im Schweizer Kanton Wallis. Die Länge des Gletschers beträgt 22,6 km, die Fläche wird mit 78,49 km² angegeben. Der Aletschgletscher entwässert über die Massa in die Rhone. Die Fläche des gesamten Einzugsgebiets der Massa beträgt 195 km², wovon 1973 etwa zwei Drittel vergletschert waren. Oft werden bei der Flächenangabe der Ober- und Mittelaletschgletscher einbezogen, da diese früher mit dem Grossen Aletschgletscher verbunden waren. Die gesamte vergletscherte Fläche einschliesslich dieser Gletscher betrug 1973 etwa 128 km², für das Jahr 1863 wird eine Fläche von 163 km² angenommen.
Ursprung am Konkordiaplatz
Der Ursprung des Grossen Aletschgletschers liegt in der rund 3800 m hoch gelegenen Jungfrau-Region. Am Konkordiaplatz (♁645905 / 150101), einer 6 km² grossen und nur wenig geneigten Eisfläche, fliessen drei mächtige Firnströme zusammen:
Von Westen mündet der Grosse Aletschfirn, der entlang dem Nordfuss von Aletschhorn und Dreieckhorn fliesst. Der Grosse Aletschfirn wird von Norden her durch drei weitere bedeutende Firne gespeist, nämlich durch den Ebnefluhfirn, den Gletscherhornfirn und den Kranzbergfirn. Alle diese Firne nehmen ihren Ausgangspunkt auf rund 3800 m ü. M. Einschliesslich des Ebnefluhfirns hat der Grosse Aletschfirn bis zum Konkordiaplatz eine Länge von 9 km und ist durchschnittlich fast 1,5 km breit. Gegen Westen ist der Grosse Aletschfirn über den 3173 m ü. M. hohen Gletscherpass der Lötschenlücke mit dem Langgletscher verbunden, der ins Lötschental abfliesst.
Von Nordwesten mündet der Jungfraufirn, der zwar die gerade Fortsetzung des Aletschgletschers darstellt, jedoch der kürzeste der drei Tributärgletscher ist. Er hat seinen Ursprung an der Südflanke des Mönchs, am Jungfraujoch und an der Ostflanke der Jungfrau. Bis zum Konkordiaplatz legt der Jungfraufirn eine Wegstrecke von knapp 7 km zurück und wird dabei im Westen vom Kranzberg, im Osten vom Trugberg flankiert. Er ist in seinem oberen Teil 2 km, weiter unten noch gut 1 km breit.
Von Norden mündet das Ewigschneefeld, das seinen Ausgangspunkt an der Ostflanke des Mönchs nimmt und in einem Bogen, flankiert vom Trugberg im Westen sowie dem Gross Fiescherhorn und dem Grünhorn im Osten, zum Konkordiaplatz fliesst. Bis hierher ist es ungefähr 8 km lang und durchschnittlich 1,2 km breit. Die Mündung in den Konkordiaplatz erfolgt über einen Steilhang mit einem Gefälle von 25 bis 30 %; der Gletscher ist hier stark zerklüftet. Gegen Norden ist das Ewigschneefeld über den firnbedeckten Pass des Unteren Mönchsjochs (3529 m ü. M.) mit dem Einzugsgebiet des Unteren Grindelwaldgletschers verbunden. Durch das Obere Mönchsjoch (3627 m ü. M.) zwischen dem Mönch und dem Trugberg besteht eine Verbindung zum Jungfraufirn. Ferner mündet am Konkordiaplatz von Osten noch der wesentlich kleinere Grüneggfirn (3 km lang und durchschnittlich 600 m breit). Dieser ist nach Osten über den Gletscherpass der Grünhornlücke (3280 m ü. M.) mit dem Fieschergletscher verbunden.
Weiterer Verlauf
Vom Konkordiaplatz aus bewegt sich der Eisstrom mit einer Breite von ungefähr 1,5 km und mit einer Geschwindigkeit von bis zu 180 Metern pro Jahr nach Südosten in Richtung Rhonetal, gesäumt vom Dreieckhorn im Westen und dem Gross Wannenhorn im Osten. Er zeichnet dann eine grosse Rechtskurve und biegt immer mehr nach Südwesten ab, nun durch den Grat des Eggishorns und Bettmerhorns vom Rhonetal getrennt. Der unterste Teil des Grossen Aletschgletschers ist weitgehend durch das Geschiebematerial von Seiten- und Mittelmoränen bedeckt. Die Gletscherzunge liegt derzeit auf rund 1'560 Meter Höhe, weit unterhalb der lokalen Waldgrenze. Aus ihr entspringt der Bach Massa, welcher nach der Massaschlucht und einer Nutzung in einem Wasserkraftwerk, in Bitsch, oberhalb von Naters, in die Rhone (Rotten) fliesst.
Der Grosse Aletschgletscher weist beachtliche Eisdicken auf. Am Konkordiaplatz hat der Gletscher eine Eisdicke von mehr als 900 Metern, gegen Süden nimmt die Mächtigkeit des Eises allmählich auf rund 150 m ab. Charakteristisch sind die beiden dunklen, fast in der Mitte des Aletschgletschers gelegenen Moränenspuren, welche sich ab dem Konkordiaplatz auf der gesamten Länge bis in den Zungenbereich hinziehen. Es sind die Mittelmoränen, die das Eis der drei Hauptfirne voneinander trennen. Die westliche Mittelmoräne wird auch Kranzbergmoräne genannt, die östliche trägt den Namen Trugbergmoräne.
Gletscherschwankungen
In seinem Hochstadium während der Kleinen Eiszeit um die Mitte des 19. Jahrhunderts erstreckte sich der Grosse Aletschgletscher noch rund 2,5 km weiter talabwärts. Aufgrund der allgemeinen Erwärmung seit etwa 1870 hat er besonders unterhalb des Konkordiaplatzes massiv an Volumen eingebüsst und sowohl an den Seiten als auch im Zungenbereich Flächen von mehreren Quadratkilometern freigegeben. Der einstmalige, in der Neuzeit höchste Gletscherstand kann gut an den noch fast vegetationslosen Seitenmoränen abgeschätzt werden. Seit 1850 hat die Eisdicke um teilweise über 100 m abgenommen. Früher waren auch die Eisströme des Oberaletschgletschers und des Mittelaletschgletschers direkt mit dem Grossen Aletschgletscher verbunden.
In der Senke zwischen dem Strahlhorn und dem Eggishorn liegt der Märjelensee, der im 19. Jahrhundert beim Gletscherhochstand zu einem Gletscherrandsee aufgestaut wurde. Seine wiederholten plötzlichen Ausbrüche durch Gletscherspalten verursachten immer wieder starke Schadenshochwasser der Massa hin zum Rhonetal.
Gegen kurzfristige Klimaschwankungen ist der Gletscher aufgrund seiner grossen Masse relativ immun. Während viele andere Gletscher Ende der 1970er Jahre bis Anfang der 1980er Jahre vorstiessen, reagierte der Aletschgletscher auf die vorübergehende Abkühlung kaum – ebenso wenig wie auf die warmen Jahre seit 1983. Aufgrund der zunehmend extremen Hitze der letzten Jahre zieht er sich aber nun doch – wie alle übrigen Alpengletscher – deutlich verstärkt zurück.
Die relative Trägheit in seinen Reaktionen auf Klimaschwankungen macht den Aletschgletscher auch zu einem idealen Untersuchungsobjekt zur Erforschung der Klimaentwicklung im Alpenraum. Die Längenschwankungen des Aletschgletschers in der Vergangenheit dürften sogar eine Rekonstruktion aller grösseren Klimaveränderungen der letzten 3200 Jahre erlauben. Die Bestimmung der verschiedenen Längenstadien des Aletschgletschers in der Vergangenheit erfolgt durch die Radiokohlenstoffdatierung fossiler Baumstämme, die der Gletscher bei einem früheren Vorstoss einmal überfahren haben muss und nun während seines aktuellen Rückzuges wieder freigibt. Der Befund fossiler Böden und von Wurzelwerk garantiert dabei, dass es sich bei dem Fundort auch um den Wuchsstandort des fossilen Baumes handelt. Durch Zählung der Jahresringe der geborgenen Stämme kann sogar der Zeitraum bestimmt werden, während dessen der Aletschgletscher den Fundort nicht erreicht hat. Mit dieser Methode wurde festgestellt, dass der Aletschgletscher bis etwa 1200 v. Chr. um einiges kleiner gewesen sein muss als gegen Ende des 20. Jahrhunderts. Für die Jahre etwa von 1200 bis 1110 v. Chr., 850 bis 750 v. Chr. und 350 bis 250 v. Chr. sind Vorstösse festgestellt worden. Dabei ist der Aletschgletscher von 900 bis 400 v. Chr. jedoch kleiner gewesen als am Ende des 20. Jahrhunderts, genauso wie von etwa 100 v. Chr. bis ins Jahr 250. Um das Jahr 300 ist eine Gletscherlänge vergleichbar der des Höchststandes im 19. Jahrhundert festzustellen.
Laut der letzten Studie der Universität Erlangen-Nürnberg (Juni 2020) schmolz die Oberfläche des Grossen Aletschgletscher zwischen den Jahren 2001 und 2014 um mehr als fünf Meter pro Jahr in den unteren Lagen.
Tourismus
Der Aletschgletscher galt schon früh als besondere Sehenswürdigkeit für Reisende und als willkommenes Untersuchungsobjekt für Forschende. Forschungsstationen gibt es seit 1937 auf dem Jungfraujoch und seit 1976 auf der Riederfurka oberhalb der Riederalp. Durch zahlreiche Luftseilbahnen besonders gut erschlossen ist der Berggrat zwischen dem Riederhorn und dem Eggishorn, der sehr schöne Einblicke in den Zungenbereich und den unteren Teil des Gletschers gewährt. Mit dem Bau der Jungfraubahn auf das Jungfraujoch (auf der Sphinx 3571 m ü. M.) wurde 1912 auch für nicht berggewohnte Leute ein Blick in den oberen Teil des Gletschers ermöglicht.
Am Felshang des Faulbergs östlich des Konkordiaplatzes stehen auf 2850 m ü. M. die Konkordiahütten des Schweizer Alpen-Clubs SAC. Sie dienen als wichtiger Etappenort auf der hochalpinen Gletscherroute vom Jungfraujoch oder vom Lötschental in das Gebiet des Grimselpasses.
UNESCO-Weltnaturerbe
Das Gebiet des Grossen Aletschgletschers ist zusammen mit dem einzigartigen Aletschwald und den umliegenden Regionen seit dem 13. Dezember 2001 Bestandteil des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.
(Wikipedia)
Aunque lo espectacular de este mirador, al que se llega desde el puerto the San Glorio es la vista de los picos que desde él se contempla, las nubes crearon otro punto de atención / Although the view of Picos de Europa mountain range is what makes this viewpoint, accessible form San Glorio mountain pass, spectacular, the clouds created another point of attention.
Desert View Amphitheater site covered with tarps prior to installation of stone steps and walkways with the goal of making the site accessible. NPS photo/A. Rehkopf
Image: a small white tractor with a large stone block suspended by chains from the bucket, is positioning the block, as three employees are working in the background, along the rim of the canyon. NPS Photo/Dan Pawlak
Desert View, a place that was initially created to introduce visitors to the Southwest’s diverse and rich cultural heritage, is transforming into a place very much in keeping with its origins. The site is becoming an “Inter-tribal Cultural Heritage Site”—the first in the National Park Service.
The site will provide provides opportunities for first-voice cultural interpretation from associated Native American Tribes - including cultural demonstrations - to enhance visitor orientation to both the cultural significance of the site and greater park, as well as information about tourism opportunities on surrounding tribal lands.
at the Jefferson Park transit center in Chicago
Nikon FM, Nikkor 105mm f/2.5 AI, Ektachrome E100. DSLR-scanned.
Accessible from the Pilatusbahn funicular railway, Mount Pilatus towers above Lucerne, covered in a light dusting of snow the day I visited, with the mountaintops rising above the thick clouds and drizzle of rain below
Sous le pape Hilaire (Ve siècle) ont été ajoutée les trois chapelles dédiées à Saint-Jean-Baptiste, Sainte-Croix et Saint-Jean l’Évangéliste (au septième siècle, fut ajoutée au sud-est la chapelle de San Venancio, avec des mosaïques à fond doré). Des trois chapelles, seulement celle située à l'est, accessible par des portes en bronze et dédiée à Saint- Jean l'Evangéliste, conserve sa forme originale de croix grecque, avec une voûte en mosaïque datant du règne du pape Sixte III. Sur un fond d'or, l'Agnus Dei est accompagné d'animaux et de plantes, symbolisme évident de l'Eucharistie. Les cinq fresques intérieures reproduisant des épisodes de la vie de Constantin dont celle de la bataille du pont Milvius (312), au plafond, remportée sur Maxence où se fit l'apparition de la Sainte Croix, avec la promesse in hoc signo vinces (Par ce signe tu vaincras), remontent au pape Urbain VIII (première moitié du XVIIe siècle) dont le blason avec les abeilles sur le sol.
La cuve circulaire où les chrétiens étaient baptisés jadis par immersion est au centre, entourée de huit belles colonnes en porphyre rouge aux chapiteaux ioniques et corinthiens, qui soutiennent un entablement de 8 colonnes de marbre blanc (le chiffre huit signifie l’accomplissement des temps dans la vie éternelle). Un déambulatoire entoure le bassin. Sur ces colonnes repose une architrave, avec des vers en latin, attribués au pape Saint Sixte II (432-440) et qui résument admirablement bien la doctrine chrétienne sur le Baptême :
C'est ici que jaillit ce peuple de noble lignée, voué au Ciel
Que l'Esprit engendre en ces eaux fécondées.
C'est dans l'eau que Notre Mère l'Église, dans un accouchement virginal,
met au monde ceux qu'elle a conçus par l'oeuvre de l'Esprit divin.
Vous qui êtes nés à cette source, vivez dans l'espérance du royaume des cieux.
Il faut renaître pour avoir la vie éternelle.
Voici la source de vie qui lave toute la terre,
et prend sa source aux plaies du Christ.
O pécheur, viens te plonger dans ce flot sacré et purificateur
Dont les ondes rajeuniront tout vieil homme qui s'y plonge.
Si, sous le poids du péché hérité ou de ton péché personnel,
tu tiens à l'innocence, lave-toi dans ces eaux.
Plus rien ne sépare ceux qui y sont renés. Ils sont devenus un,
Grâce à une seule source baptismale, à un seul Esprit, à une seule Foi.
Que personne ne craigne le nombre et la gravité de ses péchés :
Celui qui est rené de cette eau vive deviendra saint.
Après une période d'abandon dû à la résidence du pape à Avignon, puis au Vatican, des restaurations commencèrent au XVIe siècle, avec notamment une nouvelle porte d'entrée sur la Piazza San Giovanni réaménagée, se substituant à la chapelle nord (Sainte Croix). Le décor intérieur fut renouvelé au XVIIe siècle.
Avec le mausolée de Santa Costanza et celui du Saint-Sépulcre de Jérusalem, c'est l'un des premiers exemples d'une architecture chrétienne de ce genre, et fut l'archétype des baptistères construits dans la chrétienté au moyen-âge. Pendant les six premiers siècles, seul l’évêque, successeur des apôtres, faisait entrer dans l’église le catéchumène au cours de la liturgie pascale.
Under Pope Hilaire (5th century) were added the three chapels dedicated to Saint-Jean-Baptiste, Saint-Croix and Saint-Jean the Evangelist (in the seventh century, was added to the south-east the chapel of San Venancio, with mosaics with a golden background). Of the three chapels, only that located to the east, accessible by bronze doors and dedicated to St. John the Evangelist, retains its original Greek cross form, with a mosaic vault dating from the reign of Pope Sixtus III. On a gold background, the Agnus Dei is accompanied by animals and plants, an obvious symbolism of the Eucharist. The five interior frescoes reproducing episodes of the life of Constantine, including the battle of the Milvius Bridge (312), on the ceiling, won over Maxentius where appeared the Holy Cross, with the promise in hoc signo vinces (Par this sign you conquer), go back to Pope Urban VIII (first half of the 17th century) whose coat of arms with the bees on the ground.
The circular bowl where Christians were formerly baptized by immersion is in the center, surrounded by eight beautiful red porphyry columns with Ionic and Corinthian capitals, which support an entablature of 8 columns of white marble (the figure eight means the fulfillment of the times in eternal life). An ambulatory surrounds the basin. On these columns rests an architrave, with verses in Latin, attributed to Pope Saint Sixtus II (432-440) and which sum up admirably the Christian doctrine on Baptism:
It is here that springs this people of noble lineage, dedicated to Heaven
That the Spirit begets in these fertilized waters.
It is in the water that Our Mother Church, in a virgin birth,
give birth to those whom she has conceived by the work of the Divine Spirit.
You who are born at this source, live in the hope of the kingdom of heaven.
We must be reborn to have eternal life.
Here is the source of life that is washing the whole earth,
and takes its source in the wounds of Christ.
O sinner, come immerse yourself in this sacred flow and purifier
Whose waves will rejuvenate any old man who dives there.
If, under the weight of inherited sin or your personal sin,
you want innocence, wash in these waters.
Nothing separates those who are reborn. They became one,
Through one baptismal source, one Spirit, one Faith.
Let no one fear the number and the gravity of his sins:
He who is reborn from this living water will become holy.
After a period of abandonment due to the residence of the Pope in Avignon, then in the Vatican, restorations began in the 16th century, including a new gateway to Piazza San Giovanni
Near Wajurda Point, Nelson's Beach, Mimosa Rocks National Park, NSW AUS. This beach is accessible by dirt road and popular with surfers.
Hunter Valley Gardens is a privately owned gardens in the heart of Hunter Valley wine country, located in Pokolbin, NSW, Australia. It opened in 2003 and is now open every day of the year except Christmas Day. The gardens span across 14 hectares of land, containing 10 differently themed gardens, accommodation, a shopping village, rides/events and dining. The gardens are a popular venue in the Hunter Valley for weddings and events. Hunter Valley Gardens is the largest display garden in the Southern Hemisphere. Hunter valley gardens was developed and created by the Roche Group, when founder Bill Roche retired he decided that he would finally make his lifelong ambition a reality, building a garden that would be enjoyed for generations to come. Starting construction in 1999, the team of 40–50 landscape gardeners, engineers and architects completed the gardens and it was opened in October 2003 by the premier of New South Wales.
The gardens are composed of ten individually themed gardens, influenced by different locations around the world, containing both native and exotic flora . The display gardens are divided by eight kilometres of wheelchair accessible walking paths. There are over six thousand trees, six hundred thousand shrubs and one million ground-covers populating the gardens.
Fremont Avenue
Sunnyvale, California
I was being deliberately selective when I composed what I hoped would be an incongruous image. The accessible parking spot is for disabled patrons of a restaurant and other businesses that are out of the shot, to the left.
Freedom to travel and explore the world around us. With today's technology, the world is truly a smaller place making far off lands accessible to experience and soak in their cultures!
Horseshoe Bend is the name for a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona. The bend is locally known as "King Bend." It is located 5 miles (8 km) downstream from the Glen Canyon Dam and Lake Powell within Glen Canyon National Recreation Area, about 4 miles (6.4 km) southwest of Page. Accessible via a ½-mile (0.8 km) hike from U.S. Route 89, it can be viewed from the steep cliff above. According to Google terrain maps, the overlook is 4,200 feet (1,300 m) above sea level and the Colorado River is at 3,200 feet (980 m) above sea level, making it a 1,000 foot (300 m) drop.
I took this image because I wanted to get a better shot of it than I had made a few years ago. Unfortunately, October is just not the best time to photograph the bend, since there is a large shadow due to the angle of the sun this time of year. This was taken early in the morning of our visit.
This is an HDR shot which I have worked with quite a bit to even out the shadows...
Everyone has a right to access our public lands, but few of Glacier's trails were created with accessibility in mind.
A first step to addressing limits to accessibility is to identify them.
Glacier and the National Park Service are using tools—like the orange, one-wheeled device pictured here alongside two rangers and a measuring tape—to evaluate trails in the park using the High Efficiency Trail Assessment Process (HETAP).
HETAP identifies trail variables: grade, cross-slope, trail width, surface material, and more.
This data allows park managers to prioritize future trail improvements, and allow visitors in the future to make more informed decisions.
Everyone has a right to access our public lands, but few of Glacier's trails were created with accessibility in mind.
A first step to addressing limits to accessibility is to identify them.
Glacier and the National Park Service are using tools—like the orange, one-wheeled device a ranger is pictured here using—to evaluate trails in the park using the High Efficiency Trail Assessment Process (HETAP).
HETAP identifies trail variables: grade, cross-slope, trail width, surface material, and more.
This data allows park managers to prioritize future trail improvements, and allow visitors in the future to make more informed decisions.
One interesting thing to note is that Big Lots added these doors with the remodel as the restrooms were previously only accessible through the furniture alcove.
Big Lots FINALLY reopened its Olean store after a nearly 6-month long remodel....
The store actually shrunk a bit a bit and honestly left me a little disappointed with their new product selection. The store cut back many departments back to move furniture from its prior alcove space into the store itself. Furniture has been expanded to cover at least 1/3 of the sales floor.
Big Lots stupidly cut toys back from 4-5 aisles before to 1 and 1/2 now. Electronics (taking an aisle) is now just the basic headphone and cellphone accessories. I don't recall seeing any movies or video games. Home Office (previously two aisles) supplies looked to have either been cut entirely or share space with the electronics in that one aisle by offering basic pens and pencils.
This location previously sold at least an aisle's worth of hosiery and at least a 1/2 aisle for diy and auto care products. Those departments looked to have been removed entirely.
Olean, NY. November 2018.
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I presented my creations during 3 days (May 13-15) at the Accessible Art Fair in the Conrad Hotel (Brussels, Belgium). A selection of international artists exhibited their works and the event gathered several thousands of visitors and art lovers. It was the second time I participated in this fair (with many new prints in limited numbers). This edition of the fair was a huge success and a great moment for me. Meeting people and hearing their opinion about my images was priceless and very important (if you wish, you can also view some photos of the November 2010 edition).
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For more information about my art: info@benheine.com
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GOVERNOR TOMBLIN WELCOMES ELK TO WEST VIRGINIA
Twenty elk released at Tomblin Wildlife Management Area
CHARLESTON, W.Va. (December 19, 2016) - Governor Earl Ray Tomblin today joined representatives from the West Virginia Division of Natural Resources, the Rocky Mountain Elk Foundation and The Conservation Fund to welcome elk from Kentucky to West Virginia. Today's welcoming ceremony, held at the Tomblin Wildlife Management Area, included the arrival of 20 elk to Southern West Virginia.
"Today, I was proud to join both state and federal partners to celebrate a historic conservation effort in the Mountain State," Gov. Tomblin said. "Today's reintroduction is the beginning of a wonderful success story, one that has received overwhelming support from sportsmen and women across West Virginia. I look forward to the increased recreational wildlife opportunities and the economic impact this project will have on our state now and for decades to come."
Elk were native to West Virginia more than 140 years ago. Legislation in 2015 authorized the Division of Natural Resources to begin an active elk restoration plan, starting with finding enough suitable land for the elk management area to sustain an elk population.
Through a partnership with The Conservation Fund, more than 32,000 acres of publicly accessible land has been acquired for wildlife management and wildlife recreation. The DNR also recently acquired an additional 10,000 acres under lease agreements. In total, the DNR now manages more than 42,000 acres of land within an 11-mile radius of the initial elk release site.
"The reintroduction of a once-native wildlife species to sustainable populations is part of the mission of the Division of Natural Resources, and all of our staff are proud to be part of this effort to bring elk back to our state," said DNR Director Bob Fala. "With many thanks to one key partner, The Conservation Fund, we have added the largest single land parcel in state history to provide for both our fledgling elk restoration program and for other wildlife as well. We also are deeply appreciative of all the support provided by the Rocky Mountain Elk Foundation, which has provided assistance from the beginning and continues to do so as this project will expand in coming years."
"The Rocky Mountain Elk Foundation applauds Gov. Tomblin, Director Fala and all who have a role in bringing back elk to the Mountain State. It's a tremendous payday for RMEF's volunteers and members in West Virginia and the surrounding area," said Blake Henning, RMEF chief conservation officer. "We are proud to be part of such a successful collaborative partnership that made this happen in a relatively short time but with great leadership shown by the folks in West Virginia state government."
The restoration of elk into West Virginia is a major conservation initiative, involving a number of partners, including: U.S. Forest Service, Land Between the Lakes National Recreation Area; U.S. Fish and Wildlife Service; The Conservation Fund; Rocky Mountain Elk Foundation; West Virginia Department of Agriculture; West Virginia Department of Environmental Protection - Division of Mining and Reclamation; Kentucky Department of Fish and Wildlife Resources; Virginia Department of Game and Inland Fisheries; National Fish and Wildlife Foundation - Walmart Acres for America Program; Knobloch Family Foundation; Richard King Mellon Foundation; Ecosystem Investment Partners; Ark Land Company; Alpha Natural Resources; Arch Coal; West Virginia State Chapter of the National Wild Turkey Federation; West Virginia Bowhunters Association; West Virginia Trophy Hunters Association; the Outdoor Heritage Conservation Fund; and numerous volunteers.
SUPPORTING QUOTES:
Joe Manchin, U.S. Senator, West Virginia
"As a lifelong sportsman I am thrilled to see elk successfully reintroduced into West Virginia. The reintroduction of elk will bring new economic opportunities to southern West Virginia by showcasing our wild and wonderful outdoor heritage. I wish to applaud all those involved with the successful reintroduction of elk into the Mountain State."
Shelley Moore Capito, U.S. Senator, West Virginia
"It has been over 100 years since wild elk freely roamed our state, and I am thrilled the Division of Natural Resources is reintroducing this species to a place they previously called home. I was a strong advocate for this project, signing a letter of support that enabled funding to bring this idea to fruition. This is exciting news for our state, and I hope all West Virginians will have the opportunity to see and appreciate these magnificent animals."
Evan Jenkins, U.S. Representative, West Virginia's 3rd District
"Thanks to public and private efforts to protect elk habitat, we are now able to successfully reintroduce elk to West Virginia. Wild elk have not lived in West Virginia since 1865, but decades of work have paid off as these majestic creatures make their home again in our great state. I congratulate everyone involved in making this ambitious project a reality."
Joe Hankins, West Virginia Director, The Conservation Fund
The Conservation Fund is helping the State conserve 32,396 acres of working forestland in southern West Virginia-the largest single conservation acquisition in State history-to create a large, protected block of prime habitat for elk restoration.
"The Conservation Fund is proud to partner with the West Virginia Division of Natural Resources in establishing a vast protected landscape of sustainably managed land for the new elk population. This historic effort is creating new opportunities on land that once supported the state through it resources, and it is redefining conservation in West Virginia to provide multiple tangible economic and environmental benefits to local communities. We thank Governor Tomblin for his leadership, the DNR for seeing this vision through, and U.S. Senators Manchin and Capito and U.S. Representative Jenkins for their continued support of this project and important conservation programs like the Pittman-Robertson Wildlife Restoration Program."
Jeff Trandahl, Executive Director and CEO, National Fish and Wildlife Foundation
A grant from the Acres for America program, established by Walmart and the National Fish and Wildlife Foundation, supported the transfer of 10,922 acres from The Conservation Fund to the WV DNR in 2016.
"The return of any species to its native range is a reason for celebration. Bringing such a magnificent species as the elk back to the hills of West Virginia is one of the most significant reintroductions in recent years. The National Fish and Wildlife Foundation applauds the work of the State of West Virginia and we are proud to help support this effort."
John Clark, Vice President of Store Planning, Walmart
"Walmart is proud to support the longstanding efforts to bring elk back to West Virginia today. We know they will both thrive and help to inspire future generations of West Virginians to take care of and appreciate the state's incredible wildlife and natural resources."
Photos available for media use. All photos should be attributed “Photo courtesy of Office of the Governor.”
Photo of the Southernmost portion of the Lost Coast and Hardy Creek, draining into the Pacific, captured via Minolta MD W.Rokkor-X 24mm F/2.8 Lens and the bracketing method of photography alongside California Highway 1, the Shoreline Highway, before sharply turning inland, avoiding the Lost Coast and 20+ miles later terminating at Junction U.S. 101, the Redwood Highway, in the census-designated place of Rockport. King Range, a sub-region of the Coast Range. Lost Coast Region of the North Coast. Mendocino County, Northern California. Early July 2016.
Exposure Time: 1/250 sec. * ISO Speed: ISO-100 * Aperture: F/11 * Bracketing: +1 / -1
Accessible, Quiet, Elegant
Maximum of Luxury at Minimum of Cost
Rooms, $1.50 with Bath, $2.00 Family Suites. $4.00 and Up. European Plan.
Most Artistic Grill Rooms & Restaurant In The City
Roof Garden, Music Send for Colored Map of New York
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CAPA-061211
Accessible Ramp and Footbridge in Autumn at Multnomah Falls on the Columbia River Gorge National Scenic Area.
The underground tour of the White Scar Caves complex takes about 1h 20mins and is a walk of about one kilometre from the entrance to the end of the publicly accessible part of the cave complex. Parts of it are narrow and others have very low headroom but its well worth the bent knees and dripping cold water to experience the marvelous rock formations deep under the Pennine Hills. My good lady wife is seen negotiating the part of the route known as "The Squeeze" where the passageway is being narrowed by a large flowstone. All the time the noise of running water is beneath your feet as the path is elevated above an underground stream which cascades over an underground waterfall.
Schweiz / Wallis - Aletschgletscher
The Aletsch Glacier (German: Aletschgletscher, German pronunciation: [ˈalɛtʃˌɡlɛtʃɐ]) or Great Aletsch Glacier (Grosser Aletschgletscher) is the largest glacier in the Alps. It has a length of about 23 km (14 mi) (2014), has about a volume of 15.4 km3 (3.7 cu mi) (2011), and covers about 81.7 km2 (31.5 square miles) (2011) in the eastern Bernese Alps in the Swiss canton of Valais. The Aletsch Glacier is composed of four smaller glaciers converging at Konkordiaplatz, where its thickness was measured by the ETH to be still near 1 km (3,300 ft). It then continues towards the Rhône valley before giving birth to the Massa. The Aletsch Glacier is – like most glaciers in the world today – a retreating glacier. As of 2016, since 1980 it lost 1.3 kilometres (0.81 mi) of its length, since 1870 3.2 kilometres (2.0 mi), and lost also more than 300 metres (980 ft) of its thickness.
The whole area, including other glaciers is part of the Jungfrau-Aletsch Protected Area, which was declared a UNESCO World Heritage Site in 2001.
Geography
The Aletsch Glacier is one of the many glaciers located between the cantons of Bern and Valais on the Bernese Alps located east of the Gemmi Pass. The whole area is considered to be the largest glaciated area in western Eurasia. The Fiescher and Aar Glaciers lying on the east have similar extensions.
Except the Finsteraarhorn, all the highest summits of the Bernese Alps are located within the drainage basin of the glacier. The Jungfrau and Mönch constitute the northern boundary; the Gross Fiescherhorn and Gross Wannenhorn lie on its east side; finally the culminating point, the Aletschhorn (4,193 m (13,757 ft)) is located on the west side.
Before reaching the maximum flow, four smaller glaciers converge at Konkordiaplatz:
From the western mouth flows the Grosser Aletschfirn, which runs along the northern foot of the Aletschhorn and Dreieckhorn. The Grosser Aletschfirn is supplied from the north by three notable firns: the Äbeni Flue-Firn, the Gletscherhornfirn, and the Kranzbergfirn. All of these firns have their starting points at around 3,800 m (12,500 ft). From the Äbeni Flue-Firn to the Konkordiaplatz, the Grosser Aletschfirn is 9 km (5.6 mi) long and is on average about 1.5 km (0.93 mi) wide. On the west, the Grosser Aletschfirn connects with the Langgletscher over the 3,158 m (10,361 ft) high glacier pass, the Lötschenlücke, into the Lötschental.
From the northwestern mouth flows the Jungfraufirn. This firn in fact represents the straight continuation of the Aletsch Glacier, yet is the shortest of the four tributary glaciers. It has its origin on the southern flank of the Mönch and at the eastern flank of the Jungfrau with the Jungfraujoch in-between. Up to the Konkordiaplatz, the Jungfraufirn is a scarce 7 km (4.3 mi) long, and returns to flank the Kranzberg in the west and the Trugberg in the east. At its highest point, it is 2 km (1.2 mi) wide, and further down it is still a good 1 km (0.62 mi) wide.
From the northern mouth flows the Ewigschneefäld ("Eternal snow field"), where its starting point takes the east flank of the Mönch. In an elbow, it flanks from Trugberg in the west and the Gross Fiescherhorn and Grünhorn in the east, flowing on to the Konkordiaplatz. Up to here, it is about 8 km (5.0 mi) long and averages about 1.2 km (0.75 mi) wide.
The mouth at the Konkordiaplatz it follows over a rise with a descent from 25 to 30 percent; here, the glacier is sharply split. Against the north is the Ewigschneefäld over the snow-covered pass of the Unners Mönchsjoch (3,518 m (11,542 ft)), connected with the catchment area of the Ischmeer (Wallis German for "Ice Sea"). Through the Obere Mönchsjoch (3,624 m (11,890 ft)) between the Mönch and the Trugberg stands a connection to the Jungfraufirn.
From the east, the smallest firn arrives at the Konkordiaplatz: the Grüneggfirn. Its northern arm begins below the Grünegghorn (3,860 m (12,660 ft)). The southern arm collects its snow and ice in the pot flanked by the Wyssnollen, Fiescher Gabelhorn (3,866 m (12,684 ft)), and the Chamm. Between the peaks Wyssnollen and Grünhörnli another glacier pass, the Grünhornlücke (3,279 m (10,758 ft)), connects to the Fieschergletscher. The Grüneggfirn enters the Konkordiaplatz in a gap between the mountainsides Grünegg to the north and the Fülberg to the south. On the western side of the Fülberg the Konkordia hut (mountain hut) overlooks the whole Konkordiaplatz at an altitude of 2,850 m (9,350 ft).
South of Konkordiaplatz, the glacier runs towards the valley of the Oberwallis (Upper Valais); on the east side, near Bettmeralp, lies a small glacier lake, Märjelensee (2,301 m (7,549 feet)); from the western side used to enter the Mittelaletschgletscher, but since the end of the 20th century the connection with the Aletsch Glacier has been lost. Further down, until about 1880, the Oberaletschgletscher did also enter the Aletsch Glacier at its mouth. But since then both glaciers have been retreating so far that they do not connect anymore (the Upper Aletsch Glacier did retreat about 1.3 km (0.81 mi) from its connecting point with the Aletsch Glacier), but both serve now only as the source of the river Massa. The river flows through the Lake Gibidum (a reservoir, and coincidentally representing the glacier's mouth region in the 19th century, which is a retreat of more than 4 km (2.5 mi)) and a gorge of the same name before reaching the Rhône near Brig.
Tourism
The area of the Aletsch Glacier and some surrounding valleys is on the UNESCO World Heritage list, thus it is protected and the facilities are mostly restricted to the external zones. The region between Belalp, Riederalp and Bettmeralp (which is called Aletsch Region) in Valais gives access to the lower part of the glacier. The Bettmerhorn and Eggishorn are popular view points and are accessible by cable car. The Massa river can be crossed since 2008 by a suspension bridge, thus allowing hikes between the left and the right part of the glacier.
The Jungfraujoch railway station (3,450 m) gives a direct access to the upper Aletsch Glacier as well as the normal route to the Jungfrau. It can be reached only from Interlaken in the canton Bern. Hiking paths pass the Konkordia Hut or the Hollandia Hut, eventually reaching other glaciers in the massif.
On the Riederfurka, at 2,065 metres between Riederalp and the glacier, is located the historic Villa Cassel, former summer residence of many famous and influential guests from the worlds of politics and finance. The house is now one of the centers of the environmental organization Pro Natura, which hosts a permanent exhibition about the site.
Panorama
Also at the mouth of the Konkordiaplatz from the east is the small but important Grüneggfirn (3 km long and averaging 600 m wide). This firn is connected in the over the glacier pass Grünhornlücke (3280 m high) to the Fiescher Glacier in the east.
From the Konkordiaplatz, the Aletsch Glacier has a width of approximately 1.5 km and moves at a rate of 180 m per year to the southeast on course with the Rhône valley, bordering the Dreieckhorn in the west and the great Wannenhorn in the east. It then takes a great right turn and bends ever closer to the southwest, running through the edge of the Eggishorn and Bettmerhorn of the Rhône valley. The lowest part of the great Aletsch Glacier is largely covered with detritus of the lateral and medial moraines. The glacier's toe currently lies about 1560 m high, far beneath the local tree line. From it springs the Massa stream, which flows through the Massa Canyon and is used to generate hydroelectric power. It continues through the upper half of the Brig, eventually entering into the Rhône.
The great Aletsch Glacier shows considerable ice cover. At the Konkordiaplatz, it has an ice cover of more than 900 m, but as it moves to the south, the greater part of the ice melts, gradually decreasing the cover to around 150 m.
The characteristically dark medial moraine, situated almost in the middle of the glacier, runs protracted in two bands from the Konkordiaplatz along the whole length to the glacier's toe-zone. This medial moraine is collected from the ice of three large ice fields, which all run together. The westernmost medial moraine has been named the Kranzbergmoräne, and the easternmost carries the name Trugbergmoräne.
Formation and evolution
The Aletsch Glacier resulted from the accumulation and compaction of snow. Glaciers generally form where snow and ice accumulation exceed snow and ice melt. As the snow and ice thicken it reaches a point where it begins to move due to a combination of gravity and pressure of the overlying snow and ice.
During the last glacial periods, the Aletsch Glacier was much larger than now. 18,000 years ago the lower part of the ridge, between Riederalp and the glacier, was completely covered by ice. Only the summits of the Bettmerhorn, Eggishorn and the Fusshörner were above the glacier. After an important retreat, the glacier again advanced 11,000 years ago during the last glacial period. The glacier reached the Rhône valley, and its ice the Riederfurka. Remaining moraines are still visible in the Aletsch Forest.
Since the last glaciation, the glacier generally retreated. However slight climatic changes happened and, in 1860, the glacier was 3 km longer and the ice level 200 m higher.
As for many other glaciers, records show a major longer-term retreat trend. The Aletsch Glacier receded by 3.2 km (2.0 mi) since 1870, including 1.3 km (0.81 mi) since 1980.[6] A record retreat of 114.6 metres (376 ft) happened in 2006 alone.
Since the end of the Little Ice Age in 1850 the glacier has lost 20 percent of its ice mass, considerably less than other glaciers in Switzerland, which have lost up to 50 percent. This is explained with the large size of the Aletsch Glacier, which reacts much slower to climate change than smaller glaciers. It is however estimated that, by 2100, the glacier will have only one tenth of its 2018 ice mass.
Photo opportunity
On August 18, 2007, photographer Spencer Tunick used hundreds of naked people in a "living sculpture" on the Aletsch Glacier in a photo shoot which he said was intended to draw attention to global warming and the shrinking of the world's glaciers. The temperature was about 10 °C (50 °F) at the time of the photo shoot. The 600 participants on the shrinking glacier said that they had volunteered for Tunick (a collaboration with Greenpeace) to let the world know about the effects of global warming on the melting Swiss glaciers.
(Wikipedia)
Der Grosse Aletschgletscher ist der flächenmässig grösste und längste Gletscher der Alpen. Er befindet sich auf der Südabdachung der Berner Alpen im Schweizer Kanton Wallis. Die Länge des Gletschers beträgt 22,6 km, die Fläche wird mit 78,49 km² angegeben. Der Aletschgletscher entwässert über die Massa in die Rhone. Die Fläche des gesamten Einzugsgebiets der Massa beträgt 195 km², wovon 1973 etwa zwei Drittel vergletschert waren. Oft werden bei der Flächenangabe der Ober- und Mittelaletschgletscher einbezogen, da diese früher mit dem Grossen Aletschgletscher verbunden waren. Die gesamte vergletscherte Fläche einschliesslich dieser Gletscher betrug 1973 etwa 128 km², für das Jahr 1863 wird eine Fläche von 163 km² angenommen.
Ursprung am Konkordiaplatz
Der Ursprung des Grossen Aletschgletschers liegt in der rund 3800 m hoch gelegenen Jungfrau-Region. Am Konkordiaplatz (♁645905 / 150101), einer 6 km² grossen und nur wenig geneigten Eisfläche, fliessen drei mächtige Firnströme zusammen:
Von Westen mündet der Grosse Aletschfirn, der entlang dem Nordfuss von Aletschhorn und Dreieckhorn fliesst. Der Grosse Aletschfirn wird von Norden her durch drei weitere bedeutende Firne gespeist, nämlich durch den Ebnefluhfirn, den Gletscherhornfirn und den Kranzbergfirn. Alle diese Firne nehmen ihren Ausgangspunkt auf rund 3800 m ü. M. Einschliesslich des Ebnefluhfirns hat der Grosse Aletschfirn bis zum Konkordiaplatz eine Länge von 9 km und ist durchschnittlich fast 1,5 km breit. Gegen Westen ist der Grosse Aletschfirn über den 3173 m ü. M. hohen Gletscherpass der Lötschenlücke mit dem Langgletscher verbunden, der ins Lötschental abfliesst.
Von Nordwesten mündet der Jungfraufirn, der zwar die gerade Fortsetzung des Aletschgletschers darstellt, jedoch der kürzeste der drei Tributärgletscher ist. Er hat seinen Ursprung an der Südflanke des Mönchs, am Jungfraujoch und an der Ostflanke der Jungfrau. Bis zum Konkordiaplatz legt der Jungfraufirn eine Wegstrecke von knapp 7 km zurück und wird dabei im Westen vom Kranzberg, im Osten vom Trugberg flankiert. Er ist in seinem oberen Teil 2 km, weiter unten noch gut 1 km breit.
Von Norden mündet das Ewigschneefeld, das seinen Ausgangspunkt an der Ostflanke des Mönchs nimmt und in einem Bogen, flankiert vom Trugberg im Westen sowie dem Gross Fiescherhorn und dem Grünhorn im Osten, zum Konkordiaplatz fliesst. Bis hierher ist es ungefähr 8 km lang und durchschnittlich 1,2 km breit. Die Mündung in den Konkordiaplatz erfolgt über einen Steilhang mit einem Gefälle von 25 bis 30 %; der Gletscher ist hier stark zerklüftet. Gegen Norden ist das Ewigschneefeld über den firnbedeckten Pass des Unteren Mönchsjochs (3529 m ü. M.) mit dem Einzugsgebiet des Unteren Grindelwaldgletschers verbunden. Durch das Obere Mönchsjoch (3627 m ü. M.) zwischen dem Mönch und dem Trugberg besteht eine Verbindung zum Jungfraufirn. Ferner mündet am Konkordiaplatz von Osten noch der wesentlich kleinere Grüneggfirn (3 km lang und durchschnittlich 600 m breit). Dieser ist nach Osten über den Gletscherpass der Grünhornlücke (3280 m ü. M.) mit dem Fieschergletscher verbunden.
Weiterer Verlauf
Vom Konkordiaplatz aus bewegt sich der Eisstrom mit einer Breite von ungefähr 1,5 km und mit einer Geschwindigkeit von bis zu 180 Metern pro Jahr nach Südosten in Richtung Rhonetal, gesäumt vom Dreieckhorn im Westen und dem Gross Wannenhorn im Osten. Er zeichnet dann eine grosse Rechtskurve und biegt immer mehr nach Südwesten ab, nun durch den Grat des Eggishorns und Bettmerhorns vom Rhonetal getrennt. Der unterste Teil des Grossen Aletschgletschers ist weitgehend durch das Geschiebematerial von Seiten- und Mittelmoränen bedeckt. Die Gletscherzunge liegt derzeit auf rund 1'560 Meter Höhe, weit unterhalb der lokalen Waldgrenze. Aus ihr entspringt der Bach Massa, welcher nach der Massaschlucht und einer Nutzung in einem Wasserkraftwerk, in Bitsch, oberhalb von Naters, in die Rhone (Rotten) fliesst.
Der Grosse Aletschgletscher weist beachtliche Eisdicken auf. Am Konkordiaplatz hat der Gletscher eine Eisdicke von mehr als 900 Metern, gegen Süden nimmt die Mächtigkeit des Eises allmählich auf rund 150 m ab. Charakteristisch sind die beiden dunklen, fast in der Mitte des Aletschgletschers gelegenen Moränenspuren, welche sich ab dem Konkordiaplatz auf der gesamten Länge bis in den Zungenbereich hinziehen. Es sind die Mittelmoränen, die das Eis der drei Hauptfirne voneinander trennen. Die westliche Mittelmoräne wird auch Kranzbergmoräne genannt, die östliche trägt den Namen Trugbergmoräne.
Gletscherschwankungen
In seinem Hochstadium während der Kleinen Eiszeit um die Mitte des 19. Jahrhunderts erstreckte sich der Grosse Aletschgletscher noch rund 2,5 km weiter talabwärts. Aufgrund der allgemeinen Erwärmung seit etwa 1870 hat er besonders unterhalb des Konkordiaplatzes massiv an Volumen eingebüsst und sowohl an den Seiten als auch im Zungenbereich Flächen von mehreren Quadratkilometern freigegeben. Der einstmalige, in der Neuzeit höchste Gletscherstand kann gut an den noch fast vegetationslosen Seitenmoränen abgeschätzt werden. Seit 1850 hat die Eisdicke um teilweise über 100 m abgenommen. Früher waren auch die Eisströme des Oberaletschgletschers und des Mittelaletschgletschers direkt mit dem Grossen Aletschgletscher verbunden.
In der Senke zwischen dem Strahlhorn und dem Eggishorn liegt der Märjelensee, der im 19. Jahrhundert beim Gletscherhochstand zu einem Gletscherrandsee aufgestaut wurde. Seine wiederholten plötzlichen Ausbrüche durch Gletscherspalten verursachten immer wieder starke Schadenshochwasser der Massa hin zum Rhonetal.
Gegen kurzfristige Klimaschwankungen ist der Gletscher aufgrund seiner grossen Masse relativ immun. Während viele andere Gletscher Ende der 1970er Jahre bis Anfang der 1980er Jahre vorstiessen, reagierte der Aletschgletscher auf die vorübergehende Abkühlung kaum – ebenso wenig wie auf die warmen Jahre seit 1983. Aufgrund der zunehmend extremen Hitze der letzten Jahre zieht er sich aber nun doch – wie alle übrigen Alpengletscher – deutlich verstärkt zurück.
Die relative Trägheit in seinen Reaktionen auf Klimaschwankungen macht den Aletschgletscher auch zu einem idealen Untersuchungsobjekt zur Erforschung der Klimaentwicklung im Alpenraum. Die Längenschwankungen des Aletschgletschers in der Vergangenheit dürften sogar eine Rekonstruktion aller grösseren Klimaveränderungen der letzten 3200 Jahre erlauben. Die Bestimmung der verschiedenen Längenstadien des Aletschgletschers in der Vergangenheit erfolgt durch die Radiokohlenstoffdatierung fossiler Baumstämme, die der Gletscher bei einem früheren Vorstoss einmal überfahren haben muss und nun während seines aktuellen Rückzuges wieder freigibt. Der Befund fossiler Böden und von Wurzelwerk garantiert dabei, dass es sich bei dem Fundort auch um den Wuchsstandort des fossilen Baumes handelt. Durch Zählung der Jahresringe der geborgenen Stämme kann sogar der Zeitraum bestimmt werden, während dessen der Aletschgletscher den Fundort nicht erreicht hat. Mit dieser Methode wurde festgestellt, dass der Aletschgletscher bis etwa 1200 v. Chr. um einiges kleiner gewesen sein muss als gegen Ende des 20. Jahrhunderts. Für die Jahre etwa von 1200 bis 1110 v. Chr., 850 bis 750 v. Chr. und 350 bis 250 v. Chr. sind Vorstösse festgestellt worden. Dabei ist der Aletschgletscher von 900 bis 400 v. Chr. jedoch kleiner gewesen als am Ende des 20. Jahrhunderts, genauso wie von etwa 100 v. Chr. bis ins Jahr 250. Um das Jahr 300 ist eine Gletscherlänge vergleichbar der des Höchststandes im 19. Jahrhundert festzustellen.
Laut der letzten Studie der Universität Erlangen-Nürnberg (Juni 2020) schmolz die Oberfläche des Grossen Aletschgletscher zwischen den Jahren 2001 und 2014 um mehr als fünf Meter pro Jahr in den unteren Lagen.
Tourismus
Der Aletschgletscher galt schon früh als besondere Sehenswürdigkeit für Reisende und als willkommenes Untersuchungsobjekt für Forschende. Forschungsstationen gibt es seit 1937 auf dem Jungfraujoch und seit 1976 auf der Riederfurka oberhalb der Riederalp. Durch zahlreiche Luftseilbahnen besonders gut erschlossen ist der Berggrat zwischen dem Riederhorn und dem Eggishorn, der sehr schöne Einblicke in den Zungenbereich und den unteren Teil des Gletschers gewährt. Mit dem Bau der Jungfraubahn auf das Jungfraujoch (auf der Sphinx 3571 m ü. M.) wurde 1912 auch für nicht berggewohnte Leute ein Blick in den oberen Teil des Gletschers ermöglicht.
Am Felshang des Faulbergs östlich des Konkordiaplatzes stehen auf 2850 m ü. M. die Konkordiahütten des Schweizer Alpen-Clubs SAC. Sie dienen als wichtiger Etappenort auf der hochalpinen Gletscherroute vom Jungfraujoch oder vom Lötschental in das Gebiet des Grimselpasses.
UNESCO-Weltnaturerbe
Das Gebiet des Grossen Aletschgletschers ist zusammen mit dem einzigartigen Aletschwald und den umliegenden Regionen seit dem 13. Dezember 2001 Bestandteil des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.
(Wikipedia)
We had a short day-visit to Red Rock Canyon National Conservation Area, which was only 15 kms away from my sister-in-law’s house. Far from the strip and the grandeur, this house was always a peaceful and prefered place for me to stay for a couple of weeks. The magnificent hills and the red rocks could be easily visible from the balcony. I spent hours looking at the wonderful sunsets on the canyon hills from this balcony on one side, and magnificent illuminations of the strip like a huge diamond necklace on the other side.
Description:
The Red Rock Canyon National Conservation Area in Clark County, Nevada, is an area managed by the Bureau of Land Management as part of its National Landscape Conservation System, and protected as a National Conservation Area. It is about 24 km west of Las Vegas, and is easily seen from the Las Vegas Strip. This is one of the finest places I have ever visited. More than two million people visit the area each year.
The conservation area showcases a set of large red rock formations- a set of sandstone peaks and walls called the Keystone Thrust. The walls are up to 3,000 feet high, making them a popular hiking and rock climbing destination. The highest point is La Madre Mountain, at 8,154 feet.
A one-way loop road, 21 km long, provides vehicle access to many of the features in the area. Several side roads and parking areas allow access to many of the area trails. A visitor center is at the start of the loop road. The loop road is also popular for bicycle touring; it begins with a moderate climb, then is mostly downhill or flat.
Red Rock Canyon is a side-canyon accessible only by an unmaintained primitive road from the scenic loop which mostly only off-road or high clearance vehicles can access. State Route 159 cuts through an unnamed but often-visited valley; it is commonly, but mistakenly, referred to as Red Rock Canyon.
Toward the southern end of the National Conservation Area are Spring Mountain Ranch State Park; Bonnie Springs Ranch, which includes a replica of a western ghost town; and the village of Blue Diamond.
Ancient Past:
The first humans were attracted to the Red Rock area due to its resources of water, plant, and animal life that could not be easily found in the surrounding desert. Hunters and gatherers such as the historical Southern Paiute and the much older Archaic, or Desert Culture Native Americans, have successively occupied this area. As many as six different Native American cultures may have been present at Red Rock over the millennia.
Source: Wikipedia
Near the Massa Martana train station, in a place remained unchanged and easily accessible on foot, is a completely intact Roman bridge built with perfectly squared massive blocks of travertine in a single arch. It granted passage on the ancient Via Flaminia over the Fonnaia river. The Fonnaia bridge hasn’t changed since the restoration of the Augustan period (27 AD), is 15 m long, 8 m high, with a single circular arch of 3.5, has a lower slanting surface so that the road above can maintain its geometric axis. On the inner surface of the arch the blocks are disposed in even rows, and marked by letters and numbers that indicate the quarry.
Accessible PowerScape 3D play system with shade structures, adaptive whirl and swings, musical instruments, motion activities and much more.
Accessible from the Pilatusbahn funicular railway, Mount Pilatus towers above Lucerne, covered in a light dusting of snow the day I visited, with the mountaintops rising above the thick clouds and drizzle of rain below
Explore more photos or shop prints, canvas, etc. at andrewwebbcurtis.com
The location of Big Ed Hurley from the TV series Twin Peaks, in Preston, Washington, USA.
Named after railway official William T. Preston, it is a historic mill town on the northeast edge of the large Tiger Mountain State Forest and is located within commuting distance of Seattle and Bellevue.
The local Raging River feeds into the Snoqualmie River at Fall City and offers recreational activities like fly-fishing and swimming. Eastside Fire & Rescue has an all-volunteer fire station, Station 74, staffed by residents of Preston and nearby communities, which serves the Preston area.
The Preston Community Club is a volunteer organization that was created to unite and protect the historic Preston community by organizing town events and acting as liaisons to local and state government.
Several small stores have popped up as the area has grown, such as the Preston General store, Indoor Garden & Lighting, Coffee Too!, Subway, and the Preston Post Office. Several larger companies have taken advantage of Preston's accessibility, such as bottled water company Talking Rain, SanMar, and Platt.
Information Sources:
en.wikipedia.org/wiki/Preston,_Washington
www.twinpeaksblog.com/2018/05/15/setting-the-stage-big-ed...
www.cntraveler.com/galleries/2015-03-16/10-real-life-twin...
This rural retreat is a fisherman's delight, set on the banks of a coarse fishing lake in 15 acres of landscaped heaven! It's a beautiful setting and York with its many attractions, pubs and restaurants is easily accessible by car.
As well as fishing for all ages and abilities, there's lots to do in the Vale of York. Just a few miles away, Allerthorpe Park Watersports offers sailing, kayaking, windsurfing and canoeing - or you could swing from the high wires 40 feet up at Go Ape in Thornton le Dale.
If you're looking for a luxurious lodge with an outdoor hot tub, try Paradise Wood View VIP. It sleeps six people and is tastefully furnished with a verandah and garden furniture. Or if there's a party of you, Kingfisher House sleeps up to ten and has a balcony overlooking the lake plus its own cinema and games room; it's perfect for a big family celebration or special event!
York has much to offer visitors, from the Minster and the racecourse to the dungeons, but a little further afield, you can go rock climbing and bowling at Xscape in Castleford or head to Scunthorpe for some retail therapy.
Storwood is a hamlet and former civil parish, now in the parish of Cottingwith, East Riding of Yorkshire, England. It is situated approximately 6 miles (9.7 km) south-west of Pocklington and lies to the south of the B1228 road on the south bank of the Pocklington Canal. In 1931 the civil parish had a population of 63. Storwood was formerly a township in the parish of Thornton, in 1866 Storwood became a civil parish, on 1 April 1935 the civil parish was merged with East Cottingwith to create Cottingwith.[
The East Riding of Yorkshire, often abbreviated to the East Riding or East Yorkshire, is a ceremonial county in the Yorkshire and the Humber region of England. It borders North Yorkshire to the north and west, South Yorkshire to the south-west, and Lincolnshire to the south across the Humber Estuary. The city of Kingston upon Hull is the largest settlement.
The county has an area of 2,479 km2 (957 sq mi) and a population of 600,259. Kingston upon Hull is by far the largest settlement, with population of 267,014, and is a major port and the county's economic and transport centre. The rest of the county is largely rural, and the next largest towns are the seaside resort of Bridlington (35,369) and the historic town of Beverley (30,351). The county is governed by two unitary authorities, East Riding of Yorkshire Council and Hull City Council. It takes its name from the East Riding, a historic subdivision of Yorkshire.
In the east of the county the low-lying plain of Holderness is enclosed by a crescent of low chalk hills, the Yorkshire Wolds. The Wolds meet the sea at Flamborough Head, a chalk headland, while the Holderness coast to the south is characterised by clay cliffs. The west of the county is part of the Vale of York, the wide plain of the River Ure/Ouse; the south-west is part of the Humberhead Levels.
The East Riding of Yorkshire is a local government district with unitary authority status, and is a ceremonial county of England. It is named after the historic East Riding of Yorkshire which was one of three ridings alongside the North Riding and West Riding, which were constituent parts a Yorkshire ceremonial and administrative county until 1974. From 1974 to 1996 the area of the modern East Riding of Yorkshire constituted the northern part of Humberside.
As a ceremonial county, the East Riding of Yorkshire borders North Yorkshire, South Yorkshire and Lincolnshire, and includes the city of Kingston upon Hull, which is a separate unitary authority. As a district it borders North East Lincolnshire (over the Humber estuary), North Lincolnshire (over the Humber and on land), Hull, Doncaster, Selby, York, Ryedale and Scarborough.
The East Riding originated in antiquity. Unlike most counties in Great Britain, which were divided anciently into hundreds, Yorkshire was divided first into three ridings and then into numerous wapentakes within each riding. The ancient wapentake system is not used in the modern day, though it is an important part of Yorkshire's cultural heritage. Within the East Riding of Yorkshire there were seven wapentakes (including Hull), two of these were further sub-divided into divisions, thus;
1. Ouse and Derwent
2. Buckrose
3. Harthill – Wilton Beacon Division
4. Harthill – Holme Beacon Division
5. Howdenshire
6. Harthill – Hunsley Beacon Division
7. Harthill – Bainton Beacon Division
8. Dickering
9. Holderness – North Division
10. Kingston upon Hull (county corporate)
11. Holderness – Middle Division
12. Holderness – South Division
The separate Lieutenancy for the riding was established after the Restoration, and the ridings each had separate Quarter Sessions.
For statistical purposes in the 19th century an East Riding of Yorkshire registration county was designated, consisting of the entirety of the poor law unions of Beverley, Bridlington, Driffield, Howden, Hull, Patrington, Pocklington, Sculcoates, Skirlaugh and York, thus excluding parts of the historic riding around Norton and Sherburn (which are also excluded from the modern district), but also including the city of York and environs (more usually associated with the West Riding). These poor law unions formed the basis of rural sanitary districts in 1875.
A county council for the East Riding of Yorkshire was set up in 1889, covering an administrative county which did not cover the county borough of Hull, but otherwise had the same boundaries as the historic riding. Apart from Hull the East Riding contained two municipal boroughs, Beverley and Hedon.
Under the Local Government Act 1894 the rest of the administrative county was divided into rural districts and urban districts. The rural districts were based on the rural sanitary districts, with Beverley Rural District, Bridlington Rural District, Driffield Rural District, Howden Rural District, Patrington Rural District, Pocklington Rural District, Riccal Rural District, Sculcoates Rural District and Skirlaugh Rural District being formed as-is.
Several other rural districts were formed by divisions of rural sanitary districts to conform to the administrative county borders : Sherburn Rural District and Norton Rural District came from Scarborough and Malton RSDs respectively (otherwise in North Riding); Riccal Rural District from Selby RSD (otherwise in the West Riding); and Escrick Rural District which was previously part of York RSD (which covered all three ridings). Urban districts were Cottingham, Great Driffield, Filey, Hessle (from 1899), Hornsea, Norton, Pocklington and Withernsea (from 1898).
The East Riding's only large town is Hull, a major port. Hull's population of which rose rapidly in the late 19th century : quadrupling from about 60,000 in 1851 to 240,000 in 1901. Other towns in the riding did not have similar growth and remain small: Bridlington's permanent population remained largely static in the same period, increasing from 6,000 to around 7,000. By 1971 the riding had a population of slightly over 500,000. In comparison, the West Riding (including county boroughs) saw extensive urbanisation and the formation of several conurbations, and had a population of nearly 4,000,000 in 1971, and the North Riding a population of about 700,000. Beverley was once a town of some importance, with St. John's College and Beverley Minster. The college was suppressed along with the monastery in the 16th century (see Dissolution of the Monasteries) and the town entered a decline in relative importance, although gaining a charter of incorporation in 1573, having previously been under the Archbishop of York. Beverley benefited somewhat from the proximity of Hull during the Industrial Revolution, and became the county town for the East Riding administrative county in 1892.
Bridlington obtained municipal borough status in 1899, having become a resort town (as had Hornsea and Withernsea), although not matching the population growth of Scarborough further up the coast in the North Riding.
The county districts underwent a major reorganisation in 1935 :Derwent Rural District formed from most of Escrick RD, Riccal RD and part of Howden RD (which continued in existence)
Holderness Rural District formed from Patrington RD and Skirlaugh RD
Sherburn RD abolished, split between Bridlington RD, Norton RD and part to Filey UD
Sculcoates RD abolished, mostly to Beverley RD
Great Driffield urban district made smaller and renamed Driffield, the rural part going to Nafferton parish in Driffield
Rural District
an urban district of Haltemprice formed to cover the urbanised area west of Hull, from Cottingham and Hessle urban districts, and parts of Sculcoates Rural District (including Haltemprice, West Ella and parts of other parishes)
Pocklington urban district abolished and added to Pocklington RD
Both the administrative county and the historic Lieutenancy were abolished under the Local Government Act 1972, on 1 April 1974, with most of the riding going to form the northern part of Humberside. Some parts became part of North Yorkshire, with the borough of Scarborough taking in Filey UD and part of the Bridlington Rural District, the district of Ryedale taking in Norton and the former Norton Rural District, and the district of Selby taking in the former Derwent Rural District. Humberside also included northern Lincolnshire, and Goole and the former Goole Rural District, which are in the historic West Riding.
The creation of a cross-Humber authority was unpopular, despite the promise of the Humber Bridge (which ultimately opened in 1981), and identification with Yorkshire and the East Riding remained strong (for example, North Wolds District Council change its name to East Yorkshire Borough Council in the early 1980s, with Beverley also taking the name 'East Yorkshire Borough of Beverley'). This culminated with the local government review in the 1990s, which saw Humberside abolished and the northern part form two unitary authorities.
The East Riding district was formed on 1 April 1996 from the former districts of East Yorkshire, Beverley and Holderness, along with the northern part of the Boothferry district, including the Goole area which forms part of the historic West Riding (attaching it to the districts of Selby or Doncaster were proposed but rejected). The ceremonial county, the area in which the Lord Lieutenant of the East Riding of Yorkshire represents the Crown, was re-established the same day, covering Hull as well as the district.
The East Riding has two quite distinctive and contrasting archaeological areas, the Yorkshire Wolds and the Humber Wetlands. The Yorkshire Wolds form an upland arc of chalk hills stretching from Flamborough head on the coast to the Humber Estuary at its southern end. The Humber Wetlands consist of all the land in the Humber basin that lies below 10 metres above sea level which encompasses a large part of Holderness and the valleys of the Rivers Hull and Derwent and the lower part of the River Ouse valley.
The Arctic conditions associated with the last ice age started to improve and the climate gradually became warmer about 10,000 BC. This warming-up process suffered several temporary setbacks as short, cool spells occurred which disrupted the overall momentum. By about 9,000 BC the vegetation had changed from tundra to a closed woodland, of pine and birch.
Evidence from Gransmoor, to the east of Driffield, in Holderness indicates that Late Palaeolithic people were present in East Yorkshire during the climatic transition. In 1992, a small barbed antler harpoon point was found lodged in a preserved log, thought to be either birch or rowan. This find has been dated to around 9,500 BC.
Between 8,300 and 4,000 BC, Mesolithic communities occupied the area. In the GreatWold Valley, at Willow Garth, to the west of Boynton, pollen samples of Mesolithic date, indicate that the forest cover in this area was being altered by man, and that open grasslands were being made to create grazing areas to which animals would be attracted thus making hunting easier.
In the Yorkshire Wolds there are thousands of Iron Age square barrows and hundreds of farmsteads and settlements, droveways, tracks and field systems. There is a profusion of Neolithic, Bronze Age, Iron Age and Romano-British sites extending across the entire Wolds area. Some Mesolithic sites are known on the chalklands of the Yorkshire Wolds, at Craike Hill (Eastburn Warren), Garton Slack, Huggate Dykes, Huggate Wold, and Octon Wold. The Yorkshire Wolds has a wide range of favourable natural resources and so became a major focus for human settlement during the Neolithic period. Two of the most recently excavated earthen long barrows in the region are to be found at Fordon, on Willerby Wold, and at Kilham, both of which have provided radiocarbon dates of around 3,700 BC. An extensive Neolithic ritual complex, the principal elements of which are four large cursus monuments and a henge, is situated near the eastern end of the Great Wold Valley. More than 1,400 Bronze Age round barrows, are known to exist on the Yorkshire Wolds, occurring either in isolation or, more usually, grouped together to form cemeteries. In the Iron Age the distinctive local tradition known as the Arras Culture emerged and was named after the type-site, found near Market Weighton, and excavated in 1815–17. Romano British villa sites are known on the Wolds at Rudston, Harpham, Brantingham, Welton, and Wharram-le-Street. Anglo-Saxon cemeteries are known from East Yorkshire.
The Humber Wetlands Project which took place between 1992 and 2001 identified numerous prehistoric wetland sites in Holderness, the Hull Valley, the Humberhead Levels and the Vale of York. A boat found at North Ferriby, near Kingston upon Hull, has been dated as 2030 BC, which makes it the oldest of its kind in western Europe. New scientific research carried out on the remains shows it is at least 4,000 years old. The boat was one of three discovered by amateur archaeologist Ted Wright on the banks of the Humber. Historians knew that the boats were old, but only now do they know how old. New scientific techniques suggest the boat Mr Wright found in 1963 is 500 years older than everyone thought. That means it date backs more than 4,000 years to the early Bronze Age. The Ferriby site was an ideal point of departure for east/west travel along the Humber or as a crossing-point to the south bank. The Ferriby Boats were a means by which ideas, such as the decorative design of pottery, and goods such as Baltic amber and metals could arrive on the Humber shore. It has also been suggested that it may have been used to carry stones to Stonehenge.
The Battle of Stamford Bridge took place at the village of Stamford Bridge, East Riding of Yorkshire on 25 September 1066. In the battle the majority of the invading Norwegian forces were killed by the forces of King Harold Godwinson of England. It was the final fall of the Vikings in England. A fortnight after the battle, on 14 October 1066, after having marched his forces to the south coast of England, Harold was defeated and killed by Norman forces under William the Conqueror at the Battle of Hastings. This began the Norman Conquest of England.
In Holderness the extensive Lordship was granted by King William I of England to Drogo de la Beuvirere, a Flemish follower. Drogo built a castle at Skipsea before 1087 but he was disgraced and his estates were confiscated by the king. The area was then given to Odo, Count of Champagne, but was taken from him when he rebelled against King William II of England in 1095. It was returned to Odo's son Stephen of Aumale in 1102. Large estates in Holderness were held by the Bishop of Durham and the Archbishop of York. Other large landowners in the area included the abbeys of Meaux and Thornton and the priories of Swine, Nunkeeling and Bridlington. These ecclesiastical estates were confiscated and became crown property when King Henry VIII of England dissolved the monasteries in the 16th century. The Yorkshire Wolds is rich in medieval sites, and is particularly well known for its deserted villages, like those at Wharram Percy and Cottam. Settlement on the Wolds during the medieval period was concentrated on the most suitable agricultural soils. The two major settlement zones are, the Great Wold Valley villages, such as Helperthorpe, Weaverthorpe, Butterwick, Foxholes, Burton Flemming and Rudston, and the east-facing slope of the Wolds including villages such as Carnaby, Haisthorpe, Thornholme, Burton Agnes, and Nafferton, all of which are sited so as to take advantage of a ration of both heavier and lighter agricultural soils.
One of the well loved landmarks of Plymouth somewhat hidden from view now but, the area around it has had a bit of a revamp when the Theatre Royal was having it's make over.
It was built in 1862 when a local businessman William Derry( who later became Mayor)donated money towards building the clock.Unfortunately the corporation was unable to help pay towards it but could pay for a fountain,which it did.Although known as the clock it is officially a fountain although never linked to the water supply.
It is one of the few buildings to have survived the blitz.
A plaza now surround the clock which does make the whole area a little more accessible though.
Thanks you for viewing and any comments
Forest path, wheel chair accessible, in western Norway. Also of note: the path was constructed by volunteers.
Paved, accessible trail in the Lava Lands Trail of Molten Lands in Newberry Volcano National Monument
Destruction Island Lighthouse is a decommissioned lighthouse on Destruction Island, a rocky island that is part of the Quillayute Needles National Wildlife Refuge lying about 3 miles (4.8 km) off the coast of Jefferson County, Washington, in the northwest of the United States.
Construction of the Destruction Island Lighthouse began in 1890. The island was proposed as a site for a lighthouse years earlier, but a shortage of funds and shifting priorities delayed the project. After the 94-foot (29 m) conical tower was complete, it was wrapped in a skin of iron to protect it from the elements. The fog signal was placed in operation November 1, 1891, and the five concentric wicks of the lamp were set afire on January 1, 1892. The tower's first order Fresnel lens stood 147 feet (45 m) above sea level and was visible for 24 miles (39 km). The Coast Guard assumed responsibility for the lighthouse in 1939; it was automated in November 1968. In 1963, the Coast Guard's attempt to turn off the beacon for good was scuttled by the protests of local boaters.
The Fresnel lens was removed in 1995 and is on exhibit at the Westport Maritime Museum in Westport, Washington. It was replaced with a Vega Rotating Beacon (VRB-25). At that time the use of the underwater power cable was retired to solar panels. The Coast Guard gutted the original fog signal building and developed it into temporary housing just in case weather prevented maintenance crews from leaving the island. The two keepers' dwellings are no longer standing. The only remaining companions to the lighthouse are two oil houses, the fog signal building and original water tower.
The Coast Guard shut off the light for good in April 2008. The structure is now under the management of U.S Fish & Wildlife, Quillayute Needles National Wildlife Refuge, and is closed to the public. The lighthouse is visible in the distance from U.S. Route 101 at Ruby Beach about 5 miles (8.0 km) north of Kalaloch.
en.wikipedia.org/wiki/Destruction_Island_Light
Photo of Destruction Island and Destruction Island Lighthouse captured via Minolta MD Rokkor-X 50mm F/1.7 lens and the bracketing method of photography. Olympic National Park. Coast Range. Olympic Peninsula. Jefferson County, Washington. Late May 2016.
Exposure Time: 1/250 sec. * ISO Speed: ISO-100 * Aperture: F/8 * Bracketing: +1 / -1