View allAll Photos Tagged Lowest
The lowest point in North America is in Death Valley at Badwater Basin. The salt flats here are truly out of this world.
Workshops and Prints
»it is so often surprising, who rescues you at your
lowest moments.«
_aimee bender
...
no big glittery icons or invitations , please !
Frederiksborg Castle was completed by creating gardens around the large building complex. Christian IV had his own garden, but in 1720 J. Krieger was asked to create a new castle garden.
Typically, at the time, gardens had to be symmetrically structured with corded hedges.
The baroque garden fell into disrepair from the end of the 18th century and was only recreated in the 1990s. The lowest plateaus in the garden contain the royal monograms for Frederik 4th, Frederik 5th, Christian 6th and Margrethe 2nd formed in closely trimmed hedges surrounded by cone-shaped boxwood.
These are the four monarchs under whom the facility has existed.
Lowest tide of the year reveals hidden treasures. My annual return to the source. Weston Beach, Pt Lobos State Reserve.
This view was taken from the high point of Beinn Alligan, Rhuac Stac Mhor and looks over the lowest of the Horns of Alligan.
The lowest temperature ever recorded in the Northern Hemisphere was recorded in Greenland, near the topographic summit of the Greenland Ice Sheet, on 22 December 1991, when the temperature reached −69.6 °C
Leopard cub wants to climb up a nearby tree and feed on a well-hidden wildebeest carcass. It was actually hungry; it's not a made-up cute caption. The cub was licking its chops all the time while looking at its mother. Right after I made this image they trotted to the tree and the cub scooted way up to the carcass, while the mum settled down on the lowest big branch. See other images in this sequence.
The Ford Popular was made between 1953 & 1962 in England, it was at it's launch Britain's lowest priced car
Photo © Jez
Phil Varney Photography || Facebook || 500px
Zabriskie Point is probably the most iconic photographic destination in Death Valley National Park; show up on any given Saturday morning, and you're likely to share the overlook with several dozen photographers. Such a designation is well-deserved. The alluvial deposits that form the silty rock catch the morning light, giving the entire area a neat glow. And once the sun rises behind the vantage point, Manly Beacon and the other badland formations catch the bright light and display their best colors and contrast.
I waited until my last morning in DV before trying to photograph Zabriskie Point at sunrise. After several days spent at the Racetrack, Eureka Dunes, and Panamint Springs, the crowds of other photographers were definitely a change. We arrived over an hour before sunrise to stake out a location, and shortly thereafter the hordes of other tripods began setting up around us. The clouds didn't disappoint, catching an awesome pink glow before the sun finally rose.
If you look to the left side of the mountains, Telescope peak is visible towering over the valley. Its 11,000 ft. elevation gives it a ridiculous prominence over the lowest valley in the western hemisphere, and yet is still put to shame by the Sierra mountains visible from the western side of the park. If you followed the stream bed down hill from here, you would eventually exit into Death Valley via Golden Canyon. I wanted to do the Zabriskie Point to Golden Canyon trailhead hike, but there just wasn't enough time in the week! I guess I'll have to plan another trip out here!
Craig Goch, the highest upstream of the series of dams in the Elan Valley, is often referred to as the 'top dam'. It is located at a height of 1040 feet (317m) above sea level. As with all the dams, work started with the arrival of the railway line at the site. In the case of the top dam the line had the farthest to go and a rocky outcrop had to be blasted and dug through on the route to the site. Work on excavating the foundations for a secure base for the structure started in July 1897, some three years after the start of work on the lowest dam at Caban Coch.
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Jordan - Hashemite Arab Kingdom of Jordan -Dead Sea - The Lowest Point on Earth - Spectacular Natural & Spiritual Landscape - Sea of Salt
I wanted to have this kind of photo from the Dead Sea for quite some time and although I have made multiple visits to this amazing place through the time, it never came close to this result. Luckily this particular visit finally delivered kind of results I was hoping for.
Camera Model: Canon EOS 5D Mark III; Lens: EF17-40mm f/4L USM; Focal length: 22.00 mm; Aperture: 22; Exposure time: 1/5 s; ISO: 100
All rights reserved - Copyright © Lucie Debelkova www.luciedebelkova.com
All images are exclusive property and may not be copied, downloaded, reproduced, transmitted, manipulated or used in any way without expressed, written permission of the photographer.
Badwater Basin is 282 ft (86 m) below sea level.
NOTE: Any provided GPS is usually only a rough estimate, and not intended to be the exact point where the photo was taken.
Thank you so much for any comments! I really appreciate it!
October Milky Way over Temple of the Moon, Cathedral Valley, Capitol Reef National Park, Utah - with low-level stationary light painting. This natural monument is 270 feet (82 m.) high, or about 27 stories.
I used 2 F&V Z96 LED panel lights filtered to 3200ºK. They were left on during the entire exposure time. The left light was placed about 600 feet away and set at full power. The right (fill) light was placed about 500 feet away and set at 1/3 power. With some foreground features, you can dim the lights to the lowest setting (about 1/16 power), and this is usually enough LLL (Low Level Landscape Lighting) for objects up to 100 feet away. 600 feet requires full power, and is the maximum effective distance for these lights.
Zion National Park is an American national park located in southwestern Utah near the city of Springdale. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. Human habitation of the area started about 8,000 years ago with small family groups of Native Americans, one of which was the semi-nomadic Basketmaker Anasazi (c. 300). Subsequently, the Virgin Anasazi culture (c. 500) and the Parowan Fremont group developed as the Basketmakers settled in permanent communities. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s. In 1909, President William Howard Taft named the area Mukuntuweap National Monument in order to protect the canyon. In 1918, the acting director of the newly created National Park Service, Horace Albright, drafted a proposal to enlarge the existing monument and change the park's name to Zion National Monument, Zion being a term used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." On November 20, 1919, Congress redesignated the monument as Zion National Park, and the act was signed by President Woodrow Wilson. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the national park in 1956. The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateau lifted the region 10,000 feet (3,000 m) starting 13 million years ago. The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateau, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40. The 8,726-foot (2,660 m) summit of Horse Ranch Mountain is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m). Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)—one of the steepest stream gradients in North America. The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava, which is named for the coyote god of the Paiute Indians. The canyon becomes more narrow near the Temple and a hiking trail continues to the mouth of The Narrows, a gorge only 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round. The east side of the park is served by Zion-Mount Carmel Highway (SR-9), which passes through the Zion–Mount Carmel Tunnel and ends at Mount Carmel. On the east side of the park, notable park features include Checkerboard Mesa and the East Temple. The Kolob Terrace area, northwest of Zion Canyon, features a slot canyon called The Subway, and a panoramic view of the entire area from Lava Point. The Kolob Canyons section, further to the northwest near Cedar City, features one of the world's longest natural arches, Kolob Arch. Other notable geographic features of the park include the Virgin River Narrows, Emerald Pools, Angels Landing, The Great White Throne, and Court of the Patriarchs. Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March. Source: en.wikipedia.org/wiki/Zion_National_Park
Zion National Park is an American national park located in southwestern Utah near the city of Springdale. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. Human habitation of the area started about 8,000 years ago with small family groups of Native Americans, one of which was the semi-nomadic Basketmaker Anasazi (c. 300). Subsequently, the Virgin Anasazi culture (c. 500) and the Parowan Fremont group developed as the Basketmakers settled in permanent communities. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s. In 1909, President William Howard Taft named the area Mukuntuweap National Monument in order to protect the canyon. In 1918, the acting director of the newly created National Park Service, Horace Albright, drafted a proposal to enlarge the existing monument and change the park's name to Zion National Monument, Zion being a term used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." On November 20, 1919, Congress redesignated the monument as Zion National Park, and the act was signed by President Woodrow Wilson. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the national park in 1956. The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateau lifted the region 10,000 feet (3,000 m) starting 13 million years ago. The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateau, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40. The 8,726-foot (2,660 m) summit of Horse Ranch Mountain is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m). Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)—one of the steepest stream gradients in North America. The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava, which is named for the coyote god of the Paiute Indians. The canyon becomes more narrow near the Temple and a hiking trail continues to the mouth of The Narrows, a gorge only 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round. The east side of the park is served by Zion-Mount Carmel Highway (SR-9), which passes through the Zion–Mount Carmel Tunnel and ends at Mount Carmel. On the east side of the park, notable park features include Checkerboard Mesa and the East Temple. The Kolob Terrace area, northwest of Zion Canyon, features a slot canyon called The Subway, and a panoramic view of the entire area from Lava Point. The Kolob Canyons section, further to the northwest near Cedar City, features one of the world's longest natural arches, Kolob Arch. Other notable geographic features of the park include the Virgin River Narrows, Emerald Pools, Angels Landing, The Great White Throne, and Court of the Patriarchs. Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March. Source: en.wikipedia.org/wiki/Zion_National_Park
Landscape of Tibet
Tibet is the highest country on earth with an average elevation of over 4000m. The lowest regions of Tibet are still over 2000m above sea level with Jomo Langma (Everest,Sagarmatha) ཇོ་མོ་གླང་མ being the highest point at 8848m. Tibet is covered in grasslands, mountains and valleys.
Many of Asia’s largest rivers have their headwaters in Tibet such as the Ma chu རྨ་ཆུ་ ( Yellow River), Dri chu འབྲི་ཆུ་ (Yangtze), Nag chu ནག་ཆུ་ - རྒྱ་མོ་རྔུལ་ཆུ (Salween), Yarlung Tsangpo ཡར་ཀླུངས་གཙང་པོ་ (Brahmaputra) and Dza chu རྫ་ཆུ་ (Mekong). Western Tibet (Ngari) is a high, arid region with few people, while southeast Tibet (Kham) is forested and suitable for farming. Northern Tibet (Amdo) is covered in vast grasslands filled with yaks and sheep and central Tibet (U-Tsang) is the most densely populated area of Tibet lying along the fertile Yarlung Valley.
Zion National Park is an American national park located in southwestern Utah near the city of Springdale. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. Human habitation of the area started about 8,000 years ago with small family groups of Native Americans, one of which was the semi-nomadic Basketmaker Anasazi (c. 300). Subsequently, the Virgin Anasazi culture (c. 500) and the Parowan Fremont group developed as the Basketmakers settled in permanent communities. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s. In 1909, President William Howard Taft named the area Mukuntuweap National Monument in order to protect the canyon. In 1918, the acting director of the newly created National Park Service, Horace Albright, drafted a proposal to enlarge the existing monument and change the park's name to Zion National Monument, Zion being a term used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." On November 20, 1919, Congress redesignated the monument as Zion National Park, and the act was signed by President Woodrow Wilson. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the national park in 1956. The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateau lifted the region 10,000 feet (3,000 m) starting 13 million years ago. The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateau, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40. The 8,726-foot (2,660 m) summit of Horse Ranch Mountain is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m). Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)—one of the steepest stream gradients in North America. The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava, which is named for the coyote god of the Paiute Indians. The canyon becomes more narrow near the Temple and a hiking trail continues to the mouth of The Narrows, a gorge only 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round. The east side of the park is served by Zion-Mount Carmel Highway (SR-9), which passes through the Zion–Mount Carmel Tunnel and ends at Mount Carmel. On the east side of the park, notable park features include Checkerboard Mesa and the East Temple. The Kolob Terrace area, northwest of Zion Canyon, features a slot canyon called The Subway, and a panoramic view of the entire area from Lava Point. The Kolob Canyons section, further to the northwest near Cedar City, features one of the world's longest natural arches, Kolob Arch. Other notable geographic features of the park include the Virgin River Narrows, Emerald Pools, Angels Landing, The Great White Throne, and Court of the Patriarchs. Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March. Source: en.wikipedia.org/wiki/Zion_National_Park
Hottest. Driest. Lowest. This is how Death Valley is thought of by most people – a dry, hot, and desolate place. Well, on this morning in November, Badwater Basin was still the lowest place in North America (-282 feet) but it was not the driest or the hottest! Flooding rains in October left an ephemeral lake in the basin which was at this point just a few inches deep. The rain also flattened the salt polygons, leaving all kinds of interesting formations behind. After many treks out to this spot, we finally lucked out with a colorful sunrise one morning.
This spring could be phenomenal for wildflowers in Death Valley, as large patches of yellow flowers are already blooming in the southern part of the park. If you are visiting Death Valley this spring, you might be interested in our ebook on the park, Desert Paradise: The Landscape Photographer's Guide to Death Valley National Park (www.naturephotoguides.com/ebooks).
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en.wikipedia.org/wiki/Sulphur_Mountain_(Alberta)
ELEVATION 2281 m 7486 ft
Sulphur Mountain (Nakoda: Mînî Rhuwîn) is a mountain in Banff National Park in the Canadian Rocky Mountains overlooking the town of Banff, Alberta, Canada.
The mountain was named in 1916 for the hot springs on its lower slopes. George Dawson had referred to this landform as Terrace Mountain on his 1886 map of the area. Sanson's Peak was named in 1948 for Norman Bethune Sanson who diligently attended the observatory recording equipment atop Sulphur Mountain for nearly 30 years.
Two hot springs have been commercially developed. The lowest is the Cave and Basin National Historic Site and the highest is the Banff Upper Hot Springs.
A gondola on the eastern slope goes to the summit ridge which has an upper terminal containing three restaurants, a gift shop, and multiple observation decks. The summit ridge provides views both westward up and east down the Bow Valley. A boardwalk can be followed on the north side to the top of Sanson's Peak (2,256 m or 7,402 ft).
The original, and more scenic, summit access is along an old fire road (Sanson Road) on the Southwest face of the mountain with a distance of 5.8 km from the Banff Sundance Canyon trail system near the Bow River. Another 5.4 km switchback trail route exists under the gondola with trailhead access from the Banff Hot Springs parking lot near the gondola terminal.
The mountain has been the site of two research facilities. In 1903, a meteorological observatory building was completed atop Sanson Peak. This building still exists and visitors can look through a window to see its interior complete with rustic furnishings. In the winter of 1956-57, the National Research Council built a small laboratory on Sanson's Peak in order to study cosmic rays as part of Canada's contribution to the International Geophysical Year (IGY). The Sulphur Mountain Cosmic Ray Station remained in operation until 1978 and the building was removed in 1981. A plaque now marks the site's location.
The hot springs at the base of Sulphur Mountain are home to the endangered Banff Springs snail and the now-extinct Banff longnose dace.
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African Fish Eagle Haliaeetus vocifer
During the month of August the Chobe River reaches its lowest level. This not only creates good fishing opprtunities for the fish-eating bird species, but also allows them to launch their attacks from the many islands that appear in the river at this time.
This in turn allows the photographer to capture low-level in-flight images of these birds -- a rare opportunity to get up close to these magnificent Fish Eagles.
This image was processed in Lightroom and then passed to Nik Silver Efex Pro 2 for black and white conversion and partial re-colorization.
This image was captured on the Chobe River, near Kasane, northern Botswana, Southern Africa while on photo safari with CNP Safaris. www.cnpsafaris.com
©2015 Duncan Blackburn
Jostedal Glacier National Park is a national park in Norway that encompasses the largest glacier on the European mainland, Jostedalsbreen. Jostedalsbreen covers 487 km², and lies in the municipalities of Luster, Balestrand, Jølster and Stryn (in the county of Sogn og Fjordane). The highest peak in the area is Lodalskåpa at 2,083 meters. The glacier's highest point, Brenibba, lies 2,018 meters above sea level while its lowest point is 350 meters above sea level.
Norgesguidane offers blue ice climbing on the glacier.
Het Jostedalsbreen nationaal park is een nationaal park in Noorwegen. Het natuurgebied, in de provincie Sogn og Fjordane, omvat de grootste gletsjer van het Europese continent, de Jostedalsbreen. Het nationaal park is 1310 km2 groot, en bijna de helft hiervan wordt door de Jostedalsbreen bedekt. Het gebied omvat ook andere gletsjers. Het hoogste punt van het park is de top van de berg Lodalskåpade, op 2083 meter. Het park heeft een breed scala aan vegetatie, van het beboste laagland tot de alpiene vegetatie in het hooggebergte.
The bottom fall at Deckers Creek in Morgantown,WV. Hard to get down to but worth the knee and elbow scrapes.
CSX 5, the lowest numbered active CW44AC on the CSX roster, idles away on the point of CSX M573 as they wait for M574 to clear Memphis Junction in order to start their work.
Zion National Park is an American national park located in southwestern Utah near the city of Springdale. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. Human habitation of the area started about 8,000 years ago with small family groups of Native Americans, one of which was the semi-nomadic Basketmaker Anasazi (c. 300). Subsequently, the Virgin Anasazi culture (c. 500) and the Parowan Fremont group developed as the Basketmakers settled in permanent communities. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s. In 1909, President William Howard Taft named the area Mukuntuweap National Monument in order to protect the canyon. In 1918, the acting director of the newly created National Park Service, Horace Albright, drafted a proposal to enlarge the existing monument and change the park's name to Zion National Monument, Zion being a term used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." On November 20, 1919, Congress redesignated the monument as Zion National Park, and the act was signed by President Woodrow Wilson. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the national park in 1956. The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateau lifted the region 10,000 feet (3,000 m) starting 13 million years ago. The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateau, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40. The 8,726-foot (2,660 m) summit of Horse Ranch Mountain is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m). Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)—one of the steepest stream gradients in North America. The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava, which is named for the coyote god of the Paiute Indians. The canyon becomes more narrow near the Temple and a hiking trail continues to the mouth of The Narrows, a gorge only 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round. The east side of the park is served by Zion-Mount Carmel Highway (SR-9), which passes through the Zion–Mount Carmel Tunnel and ends at Mount Carmel. On the east side of the park, notable park features include Checkerboard Mesa and the East Temple. The Kolob Terrace area, northwest of Zion Canyon, features a slot canyon called The Subway, and a panoramic view of the entire area from Lava Point. The Kolob Canyons section, further to the northwest near Cedar City, features one of the world's longest natural arches, Kolob Arch. Other notable geographic features of the park include the Virgin River Narrows, Emerald Pools, Angels Landing, The Great White Throne, and Court of the Patriarchs. Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March. Source: en.wikipedia.org/wiki/Zion_National_Park
Lowest elevation in North America, 282 feet below sea level, Badwater, Death Valley, Inyo County, California 1985
Death Valley National Park is an American national park that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eureka Valley and most of Saline Valley.
The park occupies an interface zone between the arid Great Basin and Mojave deserts, protecting the northwest corner of the Mojave Desert and its diverse environment of salt-flats, sand dunes, badlands, valleys, canyons and mountains.
Death Valley is the largest national park in the contiguous United States, as well as the hottest, driest and lowest of all the national parks in the United States. It contains Badwater Basin, the second-lowest point in the Western Hemisphere and lowest in North America at 282 feet below sea level. More than 93% of the park is a designated wilderness area.
The park is home to many species of plants and animals which have adapted to the harsh desert environment including creosote bush, Joshua tree, bighorn sheep, coyote, and the endangered Death Valley pupfish, a survivor from much wetter times. UNESCO included Death Valley as the principal feature of its Mojave and Colorado Deserts Biosphere Reserve in 1984.
A series of Native American groups inhabited the area from as early as 7000 BC, most recently the Timbisha around 1000 AD who migrated between winter camps in the valleys and summer grounds in the mountains. A group of European-Americans, lost in the valley in 1849 while looking for a shortcut to the gold fields of California, gave this valley its grim name, even though only one of their group died there.
Several short-lived boom towns sprang up during the late 19th and early 20th centuries to mine gold and silver. The only long-term profitable ore to be mined was borax, which was transported out of the valley with twenty-mule teams. The valley later became the subject of books, radio programs, television series, and movies. Tourism expanded in the 1920s when resorts were built around Stovepipe Wells and Furnace Creek. Death Valley National Monument was declared in 1933 and the park was substantially expanded and became a national park in 1994.
The natural environment of the area has been shaped largely by its geology. The valley is actually a graben with the oldest rocks being extensively metamorphosed and at least 1.7 billion years old. Ancient, warm, shallow seas deposited marine sediments until rifting opened the Pacific Ocean. Additional sedimentation occurred until a subduction zone formed off the coast. The subduction uplifted the region out of the sea and created a line of volcanoes. Later the crust started to pull apart, creating the current Basin and Range landform. Valleys filled with sediment and, during the wet times of glacial periods, with lakes, such as Lake Manly.
Death Valley is the fifth-largest American national park and the largest in the contiguous United States. It is also larger than the states of Rhode Island and Delaware combined, and nearly as large as Puerto Rico. In 2013, Death Valley National Park was designated as a dark sky park by the International Dark-Sky Association.
At 190.4 meters, Turning Torso is the third tallest residential building in Europe, after the 264-meter skyscraper Triumph Palace in Moscow and the 212-meter skyscraper Sky Tower in Wrocław.
The construction is based on nine cubes with five floors in each cube. Including the intermediate floors, there will be a total of 54 floors. Each floor is about 400 m². The total office space comprises approx. 4,200 m² and is located in the two lowest cubes. Cube three to cube nine comprise a total of 147 apartments. The top two floors (53 and 54) are the Turning Torso Meetings conference facility. Each floor basically consists of a square part around the core and a triangular part, which is partly supported by an external steel support structure. The entire structure turns a quarter of a turn on its way up.
Notice on a map of the US that the coast of Georgia is indented relative to the Florida and Carolinas. This Georgia Bight causes the ocean water to be funneled toward the coast creating tides that can exceed seven feet. The result is a tremendous lateral sweep of water on the gently sloping beaches and marshes.
With the pounds sterling drop to lowest in history, we don't moan but work harder than before, our spirit are not dampened by it
Sometimes one
Is more depending
On the scale its in
Sometimes one
Is many things
And movements
Sometimes one
Is small and unseen
At the lowest end
Sometimes one
Is large and fills
Our sight
Sometimes one
Is you and me
Together .........
Fresh ballast being deposited on the trackbed at Elford. Curiously the train seen here, which originated last night at Toton, has the top number for a DB 66 at this end, 66207, and the lowest at the other end, 66001.
There is a quite rare phenomenon in Venice called Acqua Alta, during which parts of the city get covered in sea water for a few hours. This usually happens in winter and the first place to get underwater is the Piazza San Marco, which is the lowest part of the city. You can imagine my excitement, when I got the chance to photograph Venice in such an unusual way during my trip there this winter😎! You can also imagine how many other excited photographers there were, everyone walking through the water and ruining the reflection for the others 😁.
This picture was taken shortly after sunrise on my last day in Venice, just before heading back to the hotel and proceeding to the airport
Badwater – the lowest point in North America, the hottest point in the world. An expansive ocean of salt and mud forms cracked patterns extending hundreds of square miles across the valleys, embraced by staggering mountain ranges standing many thousands of feet above on all sides, each filled with beautiful secluded canyons just waiting to be explored.
These salt flats are covered with myriad patterns and textures of all scales from the microscopic to the expansive, white crystals inches long filling dried pools where rainwater once sat, and massive mud formations extending towards the horizon in places as far as the eye can see. Each year the formations morph to form ever more unique masterpieces of form and texture, resembling the surfaces of alien planets.
As I stood there, my jaw dropped in awe at the majesty of the spectacle that was unfolding before me. I couldn't believe I was really there, really experiencing that sunset in that incredibly vast and special place. It was about 80F, and the refreshing wind was blowing strong, as the sun dropped below the Panamint Range below Telescope Peak, the highest point in Death Valley National Park, towering 11,300 feet above me, just a few miles to the west. Of all the places I've visited, perhaps Death Valley is the place most deserving of the term, "magical."
This particular area on the salt flats is many miles in, near the back side of the playa, far, far away from the trampled tourist attractions on the edges of the playa that most people visit there. I was entirely alone for hours out there, never a soul in sight. The silence was palpable, the vastness overwhelming.
The tiles you see here are flat, white, and hard, covered in translucent white salt crystals, which reflect the blue sky above them, creating the cold bluish hues you see here. You are viewing them from about 3 feet above, looking slightly downwards. Each tile is about 3-6 feet in width, and only a hundred feet away, the patterns are entirely different.
The lowest lake in Pioneer Basin, looking across towards Third and Fourth Recess in the John Muir Wilderness. I had just arrived to this small lake on a multi-day backpacking trip late afternoon/early evening as a storm cleared. The brook trout were rising and the sun was golden, it was a wonderful display of God's creation.
Taken with a Canon Elan 7; Canon 17-40mm lens; Fuji Velvia 50 film; 81B warming filter; Galen Rowell/Singh-Ray 3-stop hard GND filter.
Welcome to the lowest point in North America at 282 feet below sea level. Badwater Basin was one of the spots we were looking forward to shoot the entire trip. I had never seen such a large salt flat before and this spot did not disappoint. Interestingly our first outing to Badwater was the previous night. We had originally intended to shoot the Mesquite Dunes under moonlight but after spending more than 4 hours trudging through the dunes we were finished with the dunes. Instead, we headed to Badwater hoping to catch some nice nightscapes.
We decided to try somewhere different than so we drove past the typical turnout a short distance and began our exploration a bit further south. Badwater Basin is so big that despite various visitors, almost no one else was within view. Scouting around for some time, I came across this impressive salt crack. It resembled a large fault line but what caught my eye the most was the squiggly and serpentine shape of it. At that moment I knew I had my spot. I shot in the opposite direction initially as the sun lit the mountains behind. After the sun had set I decided to reverse my direction and moved to the opposite end of this large crack. Despite the lack of clouds I focused on capturing the afterglow of sunset. Yet again to our disappointment, the clouds began moving in after sunset. Nonetheless I was still pleased with this wicked looking crack.
Canon 5D Mark II
EF 17-40mm f/4L
LEE 0.6 soft ND grad filter
(IMG_5612)