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台南空軍基地 - 幻象2000-5 / 藍天裡的鐵三角 - 超音速最高2.2馬赫
Tainan Air Base - Mirage 2000-5 / The iron triangle in the Blue sky - Highest supersonic Mach 2.2
Tainan Air Base - Mirage 2000-5 / El triángulo de hierro en el cielo azul - Mayor supersónico Mach 2,2
台南の空軍基地 - 幻影の2000-5 / 青空の中のオーディオテクニカ - 超音速の最高な2.2マッハ
Tainan Air Base - Mirage 2000-5 / Die Eisen-Dreieck in der Blue sky - Höchster Überschallmachzahlen 2.2
Tainan Air Base - Mirage 2000-5 / Le triangle de fer dans le ciel bleu - Plus haut supersonique de Mach 2.2
Tainan Taiwan / Tainan Taiwán / 台灣台南
管樂小集 夏日時光 2013/08/02 赤嵌樓 Chihkan Tower performances
{View large size on fluidr / 觀看大圖}
{My Blog / 管樂小集精彩演出-觸動你的心}
{My Blog / Great Music The splendid performance touches your heart}
{My Blog / 管楽小集すばらしい公演-はあなたの心を心を打ちます}
{Mi blog / La gran música el funcionamiento espléndido toca su corazón}
{Mein Blog / Große Musik die herrliche Leistung berührt Ihr Herz}
{Mon blog / La grande musique l'exécution splendide touche votre coeur}
家住安南鹽溪邊
The family lives in nearby the Annan salt river
隔壁就是聽雨軒
The next door listens to the rain porch
一旦落日照大員
The sunset Shineing to the Taiwan at once
左岸青龍飛九天
The left bank white dragon flying in the sky
Captain Andy's Na Pali Coast Dinner and Sunset tour was a special highlight of our trip. This Dinner cruise got the highest ratings on TripAdvisor and the reviewers raved about the food.
We thought it was a "cruise". It was a thrilling speedboat catamaran plunging through the waves and getting everyone wet while we hung "white knuckled" to the railings.
They did slow down to a cruise for us to eat our dinner.
www.beautifulworld.com/north-america/united-states/na-pal...
The Hawaiian Islands were formed by the dramatic geological collision of tectonic plates resulting in huge volcanic eruptions and subsequent formation of this rugged rocky landscape. The subsequent erosion by wind and water has allowed nature to work as a sculptor, constantly shaping these islands into spectacular works of art. Those visiting the islands for the first time find the experience simply awe-inspiring and often wonder how islands which look so small on a world map can be so immense. This is a place of extremes with incredibly high mountains, the deepest of valleys and the steepest of cliffs. Nowhere is this more apparent than along the north-west coast of the north-western island of Kauai where a seventeen mile stretch of coastline, the NaPali Coast, has enthralled visitors for many years with its primeval splendour. It has been described as being “Shangri-La” or “Heaven on Earth” but its sheer architectural immensity endows it with a spiritual aura which seems to call for for reverence much more than any cathedral.
The name NaPali literally translates as “The Cliffs” but this must be one of the greatest understatements of all times. The cliffs of NaPali soar up from the shoreline up to a height of up to 4,000 feet and appear to be almost vertical in places. This is one of the greatest natural barriers to be found anywhere on earth. This section of the island’s coastline is virtually inaccessible by land meaning that anyone wishing to visit the cliffs or any of the small coves and pools is best advised to arrive by sea and sightseeing trips are available by boats which operate from Port Allen. Many other visitors rely on kayaks or jet-skis for a really close-up NaPali experience. For many, the only way to truly appreciate this magnificent terrain is from the air and regular chartered helicopter flights are available offering a bird’s eye view of not only the cliffs but also the deep valleys, gorges and cascading waterfalls. The cliffs of Na Pali can be seen from Ke’e Beach but the view is at its most awesome when the approach is made from the sea. The towering walls of rock seem like something from an earlier geological period and would certainly not look out of place as the home of King Kong. This wonderfully wild backdrop has not escaped the attention of the world’s film makers and many Hollywood blockbusters have featured the Na Pali Coast including the aforementioned King Kong, Jurassic Park and South Pacific.
IMG_0606 acd
Highest position: #425 on Thursday, July 12, 2007
من دونكـ انا ماقدر اعيـش
فديـت قلبـه ., الله يـخليه لـي
ههههههههههههههـ
so cute walla .,
= )
Galdhøpiggen (2469 moh.), the highest mountain top of Norway and also the highest mountain top in North Europe.
There are two – the most popular – routs to get to the top.
The "big" route from a mountain cottage called Spiterstulen, people have to climb more or less for five six hours, mostly done in the summertime.
The other one – the "easy" route; – driving up about up to 1800 m on a curvy and hopless narrow road, to a mountain cottage called Juvasshytta. From there one can "walk up" the 400-500 m, lined up in ropes, over a big glacier and "climbed up" the rest to the top.
This picture was taken in the middle of July, – in bright sunshine from a blue sky and 20 cm new clean white snow.
© All rights reserved
The Swiss have just set two world records: they have built the longest rail tunnel, and above it they have erected the highest lighthouse. Our coach didn't stop and just drove by this world highest lighthouse, I shot this image with no hesitation as it was the lighthouse that I've even seen not close to the sea..........Happy New Year 2016 to YOU all !
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is at the Yellowstone Hotspot Volcano in northwestern Wyoming, USA.
“Elusive Geyser” is a nickname given to an otherwise-unnamed geyser in the northwestern Fountain Group of Yellowstone’s Lower Geyser Basin. The vent is located 41.2 meters north-northwest of New Bellefontaine Geyser & 58.0 meters west-southwest of Sub Geyser (= 44° 33’ 06.11” North latitude, 110° 48’ 34.85” West longitude). Elusive Geyser is the northernmost vent in a fracture-aligned group of features called the Gore Springs. The name “Gore Springs” has been applied to different Fountain Group features by different researchers. The “true” Gore Springs appears to be a north-northwest to south-southeast trending set of geysers that include Fitful Geyser, New Bellefontaine Geyser, an unnamed geyser (often mis-referred to as “Stalactite Geyser”), an unnamed vent, and the unnamed geyser shown here - “Elusive Geyser”.
Eruptions of Elusive Geyser are visible from tourist boardwalks and viewing platforms, but the vent area is not. Based on satellite imagery, the vent area is relatively small. Eruption runoff water drains to the northwest and west and joins a wide runoff apron representing drainage from Clepsydra Geyser and LFGNN012 (a.k.a. LNN012; a.k.a. “Gore Spring” of Marler, 1973).
Clips 1-4 - Elusive Geyser erupting in the mid-afternoon of 14 May 2015.
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Fast food at the Kawaguchiko fifth station.
Mount Fuji
Mount Fuji (富士山 Fuji-san) is the highest mountain in Japan located on Honshu Island at 3,776.24 m (12,389 ft). An active stratovolcano that last erupted in 1707–08, Mount Fuji lies about 100 kilometres (62 mi) south-west of Tokyo, and can be seen from there on a clear day. Mount Fuji's exceptionally symmetrical cone, which is snow-capped several months a year, is a well-known symbol of Japan and it is frequently depicted in art and photographs, as well as visited by sightseers and climbers. It is one of Japan's "Three Holy Mountains" (三霊山 Sanreizan) along with Mount Tate and Mount Haku.
Approximately 300,000 people climbed Mount Fuji in 2009. Buses to the fifth station start running on 1 July. Most Japanese climb the mountain at night in order to be in a position at or near the summit when the sun rises. The morning sunshine is called 御来光 "Goraikō" which means "honourable arrival of light".
Lindis Pass (elevation 971 m) is located in the South Island of New Zealand.
It lies between the towns of Cromwell in Central Otago and Omarama in North Otago, on the main inland route to the Mackenzie Basin in the Canterbury Region.
The pass lies between the valleys of the Lindis and Ahuriri Rivers.
State Highway 8 transverses the pass on its route from the Mackenzie Basin to Central Otago. The pass is the highest point on the South Island's state highway network, and the second highest point on the New Zealand state highway network, after the Desert Road (SH 1) in the Central North Island. Despite this, it is not considered one of the alpine passes as it located in the dry interior of the South Island.
EXPLORED highest position #277 ctually surrounded by many green parks like the one shown above. I love to take a walk in the local park and watch people doing exercises, Taichi and relaxin in the city.
The garden shown in picture is situated behind the Taipei Museum. The garden is actually a fusion of Japanese and Chinese (Taiwan was a territory of Japan in early 1900's).
3 exposures (-1,0,+1ev) taken handheld. Tonemapped in photomatix. Added a curve to increased contrast in image in photoshop. I tried not to overdo adjustments in photoshop to retain its natural state of beauty.
All comments and critiques are welcome.
Villoslada de Cameros, La Rioja, España.
Villoslada de Cameros es un municipio y localidad española de la comunidad autónoma de La Rioja. El término municipal, ubicado en la comarca de Cameros, tiene una población de 348 habitantes (INE 2023).
Está integrado en la comarca de Cameros, concretamente en la subcomarca de Camero Nuevo, situándose a 50 km de Logroño por la carretera N-111, que atraviesa el término municipal en el kilómetro 286.
El extenso término municipal ocupa buena parte de la cara norte de la Sierra Cebollera, que incluye el parque natural del mismo nombre. El río Iregua, que nace en el territorio, forma un profundo valle en su descenso de sur a norte, recibiendo el aporte de los numerosos arroyos de la zona y del río Mayor. Por el oeste, las sierras de Frihuela y Castejón, integradas en el Sistema Ibérico, hacen de límite, junto con la Sierra Cebollera al sur, con la provincia de Soria. En Villoslada hay un centro de interpretación del parque natural de la Sierra de Cebollera.
El techo del municipio es una enorme planicie llamada La Mesa (2168 m) que comparte con Lumbreras de Cameros. El segundo punto más elevado, que da nombre a la sierra, es el pico Cebollera (2141 m), compartido con los municipios de El Royo y Sotillo del Rincón. El núcleo urbano se alza a 1072 m sobre el nivel del mar.
Villoslada de Cameros is a municipality and town in the autonomous community of La Rioja, Spain. The municipality, located in the region of Cameros, has a population of 348 inhabitants (INE 2023).
It is part of the region of Cameros, specifically in the sub-region of Camero Nuevo, located 50 km from Logroño on the N-111 road, which crosses the municipal area at kilometre 286.
The extensive municipal area occupies a good part of the northern face of the Sierra Cebollera, which includes the natural park of the same name. The Iregua River, which rises in the territory, forms a deep valley in its descent from south to north, receiving the contribution of the numerous streams in the area and the Mayor River. To the west, the Frihuela and Castejón mountain ranges, integrated into the Iberian System, form a limit, together with the Sierra Cebollera to the south, with the province of Soria. In Villoslada there is an interpretation centre for the Sierra de Cebollera natural park.
The highest point of the municipality is a huge plain called La Mesa (2168 m) which it shares with Lumbreras de Cameros. The second highest point, which gives its name to the mountain range, is the Cebollera peak (2141 m), shared with the municipalities of El Royo and Sotillo del Rincón. The town centre is 1072 m above sea level.mar.
Me at the observation platform of Ocean Tower View Point, the highest place in Boracay.
Our vacation at: Boracay, Philippines
Highest quality prints available, contact me to request your favourite picture.
paul@pauloimages.co.uk
Highest quality prints available, contact me to request your favourite picture.
paul@pauloimages.co.uk
The highest 'wedge' possible - a full 20cm heel on these 'ballet' wedge boots. I can walk in them - for a short distance only. Size 40 so snug on my feet, which helps to support my ankles.
Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah. More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations. The park contains the highest density of natural arches in the world.
The park consists of 310.31 square kilometres (76,680 acres; 119.81 sq mi; 31,031 ha) of high desert located on the Colorado Plateau. The highest elevation in the park is 5,653 feet (1,723 m) at Elephant Butte, and the lowest elevation is 4,085 feet (1,245 m) at the visitor center. The park receives an average of less than 10 inches (250 mm) of rain annually.
Administered by the National Park Service, the area was originally named a national monument on April 12, 1929, and was re designated as a national park on November 12, 1971. The park received more than 1.6 million visitors in 2018.
As stated in the foundation document in U.S. National Park Service website:
The purpose of Arches National Park is to protect extraordinary examples of geologic features including arches, natural bridges, windows, spires, and balanced rocks, as well as other features of geologic, historic, and scientific interest, and to provide opportunities to experience these resources and their associated values in their majestic natural settings.
The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago (Mya) when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 200 Mya), desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Mya), was deposited on top of the Navajo. Over 5,000 feet (1,500 m) of younger sediments were deposited and have been mostly eroded. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.
The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual "salt anticlines" or linear regions of uplift. Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center.
As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer-cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches.
Although the park's terrain may appear rugged and durable, it is extremely fragile. More than 1 million visitors each year threaten the fragile high-desert ecosystem. The problem lies within the soil's crust, which is composed of cyanobacteria, algae, fungi, and lichens that grow in the dusty parts of the park. Factors that make Arches National Park sensitive to visitor damage include being a semiarid region, the scarce, unpredictable rainfall, lack of deep freezing, and lack of plant litter, which results in soils that have both a low resistance to and slow recovery from, compressional forces such as foot traffic. Methods of indicating effects on the soil are cytophobic soil crust index, measuring of water infiltration, and t-tests that are used to compare the values from the undisturbed and disturbed areas.
Geological processes that occurred over 300 million years ago caused a salt bed to be deposited, which today lies beneath the landscape of Arches National Park.[ Over time, the salt bed was covered with sediments that eventually compressed into rock layers that have since been named Entrada Standstone. Rock layers surrounding the edge of the salt bed continued to erode and shift into vertical sandstone walls called fins. Sand collected between vertical walls of the fins, then slightly acidic rain combined with carbon dioxide in the air allowed for the chemical formation of carbonic acid within the trapped sand. Over time, the carbonic acid dissolved the calcium carbonate that held the sandstone together. Many of the rock formations have weaker layers of rock on bottom that are holding stronger layers on top. The weaker layers would dissolve first, creating openings in the rock. Gravity caused pieces of the stronger rock layer to fall piece by piece into an arch shape. Arches form within rock fins at points of intense fracturing localization, or weak points in the rock's formation, caused by horizontal and vertical discontinuities. Lastly, water, wind, and time continued this erosion process and ultimately created the arches of Arches National Park. All of the arches in the park are made of Entrada Sandstone, however, there are slight differences in how each arch was developed. This allows the Entrada Sandstone to be categories into 3 groups including Slick rock members, Dewey rock members, and Moab members. Vertical arches can be developed from Slick rock members, a combination of Slick rock members and Moab members, or Slick rock members resting above Dewey rock members. Horizontal arches (also called potholes) are formed when a vertical pothole formation meets a horizontal cave, causing a union into a long arch structure. The erosion process within Arches National Park will continue as time continues to pass. Continued erosion combined with vertical and horizontal stress will eventually cause arches to collapse, but still, new arches will continue to form for thousands of years.
Humans have occupied the region since the last ice age 10,000 years ago. Fremont people and Ancestral Puebloans lived in the area until about 700 years ago. Spanish missionaries encountered Ute and Paiute tribes in the area when they first came through in 1775, but the first European-Americans to attempt settlement in the area were the Mormon Elk Mountain Mission in 1855, who soon abandoned the area. Ranchers, farmers, and prospectors later settled Moab in the neighboring Riverine Valley in the late 1870s. Word of the beauty of the surrounding rock formations spread beyond the settlement as a possible tourist destination.
The Arches area was first brought to the attention of the National Park Service by Frank A. Wadleigh, passenger traffic manager of the Denver and Rio Grande Western Railroad. Wadleigh, accompanied by railroad photographer George L. Beam, visited the area in September 1923 at the invitation of Alexander Ringhoffer, a Hungarian-born prospector living in Salt Valley. Ringhoffer had written to the railroad to interest them in the tourist potential of a scenic area he had discovered the previous year with his two sons and a son-in-law, which he called the Devils Garden (known today as the Klondike Bluffs). Wadleigh was impressed by what Ringhoffer showed him, and suggested to Park Service director Stephen T. Mather that the area be made a national monument.
The following year, additional support for the monument idea came from Laurence Gould, a University of Michigan graduate student (and future polar explorer) studying the geology of the nearby La Sal Mountains, who was shown the scenic area by local physician Dr. J. W. "Doc" Williams.
A succession of government investigators examined the area, in part due to confusion as to the precise location. In the process, the name Devils Garden was transposed to an area on the opposite side of Salt Valley that includes Landscape Arch, the longest arch in the park. Ringhoffer's original discovery was omitted, while another area nearby, known locally as the Windows, was included. Designation of the area as a national monument was supported by the Park Service in 1926 but was resisted by President Calvin Coolidge's Interior Secretary, Hubert Work. Finally, in April 1929, shortly after his inauguration, President Herbert Hoover signed a presidential proclamation creating the Arches National Monument, consisting of two comparatively small, disconnected sections. The purpose of the reservation under the 1906 Antiquities Act was to protect the arches, spires, balanced rocks, and other sandstone formations for their scientific and educational value. The name Arches was suggested by Frank Pinkely, superintendent of the Park Service's southwestern national monuments, following a visit to the Windows section in 1925.
In late 1938, President Franklin D. Roosevelt signed a proclamation that enlarged the Arches to protect additional scenic features and permit the development of facilities to promote tourism. A small adjustment was made by President Dwight Eisenhower in 1960 to accommodate a new road alignment.
In early 1969, just before leaving office, President Lyndon B. Johnson signed a proclamation substantially enlarging the Arches. Two years later, President Richard Nixon signed legislation enacted by Congress, which significantly reduced the total area enclosed, but changed its status. Arches National Park was formally dedicated in May 1972.
In 1980, vandals attempted to use an abrasive kitchen cleanser to deface ancient petroglyphs in the park, prompting park officials to recruit physicist John F. Asmus, who specialized in using lasers to restore works of art, to use his technology to repair the damage. Asmus "zapped the panel with intense light pulses and succeeded in removing most of the cleanser".
Climbing Balanced Rock or any named or unnamed arch in Arches National Park with an opening larger than 3 ft (0.9 m) is banned by park regulations. Climbing on other features in the park is allowed but regulated; in addition, slacklining and BASE jumping are banned parkwide.
Climbing on named arches within the park had long been banned by park regulations, but following Dean Potter's successful free climb on Delicate Arch in May 2006, the wording of the regulations was deemed unenforceable by the park attorney. In response, the park revised its regulations later that month, eventually imposing the current ban on arch climbing in 2014.
Approved recreational activities include auto touring, hiking, bicycling, camping at the Devils Garden campground, backpacking, canyoneering, and rock climbing, with permits required for the last three activities. Guided commercial tours and ranger programs are also available.
Astronomy is also popular in the park due to its dark skies, despite the increasing light pollution from towns such as Moab.
Delicate Arch is the subject of the third 2014 quarter of the U.S. Mint's America the Beautiful Quarters program commemorating national parks and historic sites. The Arches quarter had the highest production of the five 2014 national park quarters, with more than 465 million minted.
American writer Edward Abbey was a park ranger at Arches National Monument in 1956 and 1957, where he kept journals that became his book Desert Solitaire. The success of Abbey's book, as well as interest in adventure travel, has drawn many hikers, mountain bikers, and off-pavement driving enthusiasts to the area. Permitted activities within the park include camping, hiking along designated trails, backpacking, canyoneering, rock climbing, bicycling, and driving along existing roads, both paved and unpaved. The Hayduke Trail, an 812 mi (1,307 km) backpacking route named after one of Edward Abbey's characters, begins in the park.
An abundance of wildlife occurs in Arches National Park, including spadefoot toads, antelope squirrels, scrub jays, peregrine falcons, many kinds of sparrows, red foxes, desert bighorn sheep, kangaroo rats, mule deers, cougars, midget faded rattlesnakes, yucca moths, western rattlesnakes, and collared lizards.
A number of plant species are common in the park, including prickly pear cactus, Indian ricegrass, bunch grasses, cheatgrass, moss, liverworts, Utah juniper, Mormon tea, blackbrush, cliffrose, four-winged saltbrush, pinyon pine, evening primrose, sand verbena, yucca, and sacred datura.
Biological soil crust consisting of cyanobacteria, lichen, mosses, green algae, and microfungi is found throughout southeastern Utah. The fibrous growths help keep soil particles together, creating a layer that is more resistant to erosion. The living soil layer readily absorbs and stores water, allowing more complex forms of plant life to grow in places with low precipitation levels.
Among the notable features of the park are the following:
Balanced Rock – a large balancing rock, the size of three school buses
Courthouse Towers – a collection of tall stone columns
Dark Angel – a free-standing 150 ft-tall (46 m) sandstone pillar at the end of the Devils Garden Trail
Delicate Arch – a lone-standing arch that has become a symbol of Utah and the most recognized arch in the park
Devils Garden – many arches and columns scattered along a ridge
Double Arch – two arches that share a common end
Fiery Furnace – an area of maze-like narrow passages and tall rock columns (see biblical reference, Book of Daniel, chapter 3)
Landscape Arch – a very thin and long arch in the Devils Garden with a span of 290 ft (88 m) (the longest arch in the park)
Petrified Dunes – petrified remnants of dunes blown from the ancient lakes that covered the area
The Phallus – a rock spire that resembles a phallus
Wall Arch – located along the popular Devils Garden Trail; collapsed sometime on August 4/5, 2008
The Three Gossips –a mid-sized sandstone tower located in the Courthouse Towers area.
Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.
Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.
People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.
Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.
The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.
Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.
The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:
use of the bow and arrow while hunting,
building pithouse shelters,
growing maize and probably beans and squash,
building above ground granaries of adobe or stone,
creating and decorating low-fired pottery ware,
producing art, including jewelry and rock art such as petroglyphs and pictographs.
The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.
These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.
In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.
In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.
Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.
At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.
The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.
A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.
Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.
Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.
Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.
Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.
Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.
The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.
Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.
Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.
In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.
The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.
Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.
After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.
As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.
Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.
Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.
Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.
Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.
On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.
Main article: Latter Day Saint polygamy in the late-19th century
During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.
The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.
Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:
William Torrington in Carson City (then a part of Utah territory), 1859
Thomas Coleman (Black man) in Salt Lake City, 1866
3 unidentified men at Wahsatch, winter of 1868
A Black man in Uintah, 1869
Charles A. Benson in Logan, 1873
Ah Sing (Chinese man) in Corinne, 1874
Thomas Forrest in St. George, 1880
William Harvey (Black man) in Salt Lake City, 1883
John Murphy in Park City, 1883
George Segal (Japanese man) in Ogden, 1884
Joseph Fisher in Eureka, 1886
Robert Marshall (Black man) in Castle Gate, 1925
Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).
Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.
Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.
During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.
In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.
Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.
Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.
As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.
One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.
It is estimated that 1,450 soldiers from Utah were killed in the war.
Explored- Highest Position May 8th 2010 # 173.
Dandelions are mostly a hated pest in the spring. For this image I thought they brought a nice splach of yellow on such a gloomy day.
This was taken the same day as my last lone tree image. Even with the ominous clouds the forground lighting was very nice. The greens were popping and the yellow dandelions were screaming for me to capture them :)
The winds were blowing pretty fierce this day. Instead of trying to stop all the motion, I let the dandelions sway a bit to capture the scene as it was.
Canon 50d
Sigma 10-20mm
B&W F-Pro CPL
Lee Filter Holder
Hitech 0.6 Soft Grad ND
Lee 0.6 Hard Grad ND
Single RAW exposure @ 10mm
ISO 100
f/13
1/15
Jog Falls Karnataka
Located in the state of Karnataka, Jog Falls is the highest waterfall in India. The water fall is 829 ft (253 m) high. During monsoons (July/August) the fall is intense. The Linganmakki Dam and hydro-electric power station across the river Sharavathi releases its excessive water during the monsoons making the fall even more intense.
Camera : Nikon FM10
Location: Jog Falls, Shimoga District, Karnataka, India
Ávila (Spanish pronunciation: [ˈaβila]; Latin: Abila and Obila) is a Spanish town located in the autonomous community of Castile and León, and is the capital of the Province of Ávila.
It is sometimes called the Town of Stones and Saints, and it claims that it is one of the towns with the highest number of Romanesque and Gothic churches (and bars and restaurants) per capita in Spain. (Zamora, a town of similar size, claims the greatest number of Romanesque churches in Europe.) It is notable for having complete and prominent medieval town walls, built in the Romanesque style. The town is also known as Ávila de los Caballeros, Ávila del Rey and Ávila de los Leales (Ávila of the Knights, the King and the Loyalists), each of these epithets being present in the town standard.
The writer José Martínez Ruiz (Azorín), in his seminal book El alma castellana (The Castilian Soul), described it as "perhaps the most 16th-century town in Spain", and it was declared a UNESCO World Heritage Site in 1985.
The Leadhills & Wanlockhead Railway is Britain's highest adhesion railway, reaching 1498 feet above sea level at Hillend summit, it was originally built in 1900 for the Caledonian Railway Company.
Clyde, Leadhills and Wanlockhead Locomotive No 6 was built by Hunslet Locomotives , Leeds in 1975, as locomotive number HE6347. This Locomotive has a six cylinder water cooled Perkins diesel engine producing sixty horse power to its four wheels via a torque converter and chain drive.
the highest wooden Gothic altar in the world (18,62 cm), height of Madonna 2,47 m
Late Gothic style, 1508-1517, sculptures of Madonna, St. James the Greater the Apostle and St. John the Apostle were created at the beginning of the whole work, before 1510
carved by Master Paul of Levoča and his workshop
statues in the suprastructre are dated to the 1380s
taking photos in the whole church is strictly prohibited (although churches are public spaces), but recently I had a chance to make some pictures to share with everybody, who loves old art
Highest position - #484 Thanks, everyone!
A walk on a cloudy morning revealed this little guy. They really are tiny, less than an inch. I think it was taking a drink of water off this blade of grass.
A black and white version of this shot can be found at my Facebook page
Please view in 'Lightbox'
Pico de las Nieves is the second highest peak on the island of Gran Canaria, Canary Islands, Spain. Its height is 1,949 metres above sea level. It is of volcanic origin (stratovolcano). On its slopes, Canary Islands Pine was reintroduced in the 1950s.
The name means 'peak of the snows' in Spanish and refers to the fact that several covered pits (neveras in Spanish) for holding snow were built directly into the mountainsides. The first of the neveras was constructed in 1694 by order of the Catholic Church. The snow was collected by laborers using wooden shovels and wicker baskets, making real mountains of snow. The snow was placed into the pits by the "paleros" in rows, and packed in rectangular boxes of wood or cork separated by layers of straw.
Most of the highest plateau is occupied by a military base, including a large ball-shaped radar. Civilian visitors are allowed to enter a platform somewhat below the base, from which half of the island as well as Tenerife's Pico del Teide is visible, in case of good weather. The most distinctive feature is the Roque Nublo monolith, the second highest peak of the island.
(Wikipedia)
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We did a short stop on the mountain top of Pico de las Nieves which is easily accessible by car when driving through the island's interior - some stunning views there for sure, weather-dependent...
At 3720 mtrs the highest cricket ground in the world. Open for cricket only for 5 months. The rest of the year its too blustery and snow is often more than a meter thick for weeks together. In village Nako near the Indo-Tibet Border in Kinnaur District of Himachal Pradesh, India.
Sandakphu / Sandakfu (3636 m; 11929 ft) is the highest peak in the state of West Bengal, India. It is situated at the edge of the Singalila National Park in Darjeeling district on the West Bengal-Sikkim border, and is the highest point of the Singalila Ridge.
The trek along the Singalila Ridge to Sandakphu and Phalut is one of the most popular ones in the Eastern Himalayas due to the grand vistas of the Kangchenjunga range and the Everest range which can be seen from the ridge, and also for the seasonal wildflower blooms, red panda populations and birding. More: en.wikipedia.org/wiki/Sandakfu
Singalila National Park, Eastern Himalayas,
Beautiful Bengal, India
Jebel Shams Arabic: جبل شمس, is a mountain located in northeastern Oman north of Al Hamra town. It is the highest mountain of the country and part of Al Hajar Mountains range. It is a popular sightseeing area located 240 km from Muscat.
Designer unknown (佚名)
Ca. 1967
Highest instruction
Zuigao zhishi (最髙指示)
Call nr.: BG C32/477 (IISH collection)
39 Caricatures of prominent Party members, specialists, scholars and other functionaries who were under attack during the Cultural Revolution. On the two bottom rows: foreign politicians and state leaders.
Published in Shanghai.
This is the back of www.flickr.com/photos/chinesepostersnet/12176184976
More? See: chineseposters.net
Highest explore position: 404 on Tuesday, June 12, 2007.
Replaced with a de-noised version 11-11-2007.
Explore Highest position # 228 on Saturday, October 4, 2008
Orchids from our garden. To my flickr friends. Special thanks to Daylily18 for a very beautiful testimonial. Hope you have a great weekend.:)
Cattleya ชื่อกล้วยไม้หลายชนิดในสกุล Cattleya วงศ์ Orchidaceae
แคทลียาเป็นกล้วยไม้ที่ได้รับความนิยมปลูกเลี้ยงอย่างกว้างขวางในหลายประเทศ เนื่องจากแคทลียาเป็นกล้วยไม้ที่มีดอกขนาดใหญ่ที่สุดและสีสวยงามที่สุด บางชนิดมีกลิ่นหอม และถือกันว่าแคทลียาเป็น ราชินีแห่งกล้วยไม้ และเป็นสัญญลักษณ์สากลของกล้วยไม้ทั่วไป
มีถิ่นกำเนิดอยู่ในเขตร้อนแถบอเมริกากลางและอเมริกาใต้ตอนเหนือ
Exposure: 1/350 sec, Aperture: f/6.7, Focal Length: 70 mm, ISO: 100, +1EV
Nikon D80, Nikkor AF-S 24-70mm f/2.8G ED
鲜花 "الزهور " 鮮花 цветя květiny blomster bloemen bulaklak kukkien fleurs Blumen λουλούδια פרחים virágokat blóm bunga bláthanna fiori 花 꽃 blomster گل kwiaty flores цветы blommor çiçekler квіти hoa
Mason Neck State Park, Lorton, Virginia
Nikon D90, Nikkor DC 135mm f/2 AF-D, Defocus Control at Rear f/2, Heliopan 3x Magnification Filter
"As we express our gratitude, we must never forget that the highest appreciation is not to utter words, but to live by them." ~ John F. Kennedy, 451 - Proclamation 3560 - Thanksgiving Day, November 5, 1963
Yesterday, Lois and I were fortunate enough to see Mt. McKinley or Denali, the highest mountain in North America (20,320 feet) Later in the day, most of it was covered with clouds. I would have loved to have some blue sky, but it was great to be able to see the top.
We are celebrating our 25th anniversary in Alaska. May the creator of this Masterful sculpture keep us in his care and continue to bless our marriage as He has done for the past 25 years. Glory to God!