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Immagini di 'Sedimenti' trovate, 110

Sediment travels on conveyor belt in factory. Man stands in front of piles of sediment, talking.
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Col di Vermianaz (charcoal & conte on paper)
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astrid, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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Three charts of sediment distribution, from Three charts of sediment distribution, from Reports of the Challenger cruise, 1872-76
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Limestone sediments, Haute-Savoie, France (photo)
Limestone sediments, Haute-Savoie, France (photo)
Limestone sediments, Haute-Savoie, France (photo)
Metal anchor covered with marine sediments, Roman civilization
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Exploitation of a gold deposit in alluvial sediments, 1857 (engraving)
prydz, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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wrigley, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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balleny, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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ross, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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porpoise, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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weddell, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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norvegia, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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wilkins, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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vincennes, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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amundsen, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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bellingshausen, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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leverett, 2007, (ice from the Western Antarctic Ice Sheet, sediment from Antarctica's Dry Valleys and mixed media on paper)
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ninnus, 2007, (ice from the Western Antarctic Ice Sheet, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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Fur formation, marine sediment made of diatoms and clay minerals, Palaeocene-Eocene, Fur Island, Denmark
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Long chute from docked cargo ship is positioned over ground near docks. Sediment is dumped into large piles from chute.
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Indus river running alongside steep mountain flank in eroding valley, sediment, Alchi, Ladakh, Himalayas, Jammu and Kashmir, India (photo)
Turkey, Gokava Gulf, Amphitheater Behind Cleopatra Beach, Sedir (Cedrai) Island (photo)
Sediment piles up on ground, dumped from chute above. Chute extends from piles on ground up to tall building, then from there to taller building.
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Turkey, Gokava Gulf, Behind Cleopatra Beach, Sedir (Cedrai) Island, Gulet Boat Seen From Ruins of Amphitheater (photo)
Alaskan hydraulic gold mining used jets of water to erode rock material or move sediment. The resulting water-sediment was then directed through sluice boxes to remove the gold.c. 1900-1923
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China - Yellow River Delta 1989 - China - Yellow River delta in 1989 - The Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. Image obtained by the Landsat 5 satellite in 1989. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat 5 satellite shows the Yellow River Delta at the river mouth in 1989. In 1989, the river's main channel emptied into the Bohai Sea in a southeast - bending arc
China - Yellow River Delta in 1999 - China - Yellow River delta in 1999 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 1999. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat satellite shows the Yellow River Delta at the river mouth in 1999. In 1989, the river's main channel emptied into the Bohai Sea in a southeast - bending arc. In 1996, Chinese engineers blocked the main channel and forced the river to veer northeast. By 1999, erosion and settling along the old channel caused the tip of the delta to retreat, while a new peninsula had formed to the north
China - Yellow River Delta 2009 - China - Yellow River delta in 2009 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 2009. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat satellite shows the Yellow River Delta at the river mouth in 2009. In 1989, the river's main channel emptied into the Bohai Sea in a southeast - bending arc. In 1996, Chinese engineers blocked the main channel and forced the river to veer northeast. By 1999, erosion and settling along the old channel caused the tip of the delta to retreat, while a new peninsula had formed to the north
Astronauts on Titan - Illustration - Walking a dry gully on Titan - Astronauts explore Titan's surface. Earthlings explore a dry gully on Saturn's moon Titan. In early 2005 the European Space Agency's Huygens probe revealed a surface carved by numerous drainage channels similar to river deltas on Earth. While the exact nature of these channels is not yet known, one theory proposes that Titan's surface of hydrocarbon sediments has been washed from the highlands by methane rain
Sandy Cay - Bahamas - Seabed currents and sandbanks on Sandy Cay and Long Island, Bahamas. Image obtained on 27 November 2010 from the International Space Station (ISS). This astronaut photograph, taken from the International space station on November 27, 2010, provides a view of tidal flats and channels near Sandy Cay, on the western side of Long Island and along the eastern margin of the Great Bahama Bank (North is top). The continuously exposed parts of the island are brown, a result of soil formation and vegetation growth. To the north of Sandy Cay, an off - white tidal flat composed of carbonate sediments is visible; light blue - green regions indicate shallow water on the tidal flat. The tidal flow of seawater is concentrated through gaps in the land surface, leading to the formation of relatively deep channels that cut into the sediments. The channels and areas to the south of the island have a vivid blue color that indicates deeper water
French advertisement for filter against sediment, may 1944
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Thick gooey sediment created by the spilling of burnt fuel and other toxic chemicals from the ships, felling of thousands of trees for land and vapours and fumes from burning materials made the coastal areas along the ship breaking yards at Sitakunda, Chittagong a highly polluted area. The industry started its operation in 1960 and flourished in a very short period of time due to lower labour costs and less stringent environmental regulations. Chittagong, Bangladesh. October 31, 2009.  (photo)
Archean stromatolites - Illustration showing the shores of an ancient sea 3 billion years ago. In the foreground, stromatolites, aggregation of sediments and cyanobacteries. Stromatoliths have undoubtedly contributed to our dioxygen-rich atmosphere and the ozone layer that allowed the development of a more complex terrestrial and oceanic life. Dome - shaped stromatolites, averaging three feet high and four feet wide, populate the shallow shore of an ancient sea 3 billion years ago. The Moon looms near the horizon, much closer to the Earth than it is now and therefore appearing considerably larger, but otherwise looking much like the moon we know today. 3 billion years ago the first macro evidence of life on Earth may have appeared in the form of large aggregations of microorganisms and associated sediments known as stromatolites. Cyanobacteria (AKA blue - green algae) were likely one of the primary contributors to these aggregations. During the Archean Eon the Earth's atmosphere contained very little oxygen. Cyanobacteria would have thrived during this time as they employ photosynthesis to combine water, carbon dioxide, and sunlight to create their food, while the byproducts of this process are oxygen and calcium carbonate. Billions of years of photosynthetic processes by cyanobacteria other living organisms are likely the primary source of the oxygen we breathe. They also provided the oxygen that forms the protective ozone layer, filtering the shorter wavelengths of ultraviolet light from the Sun that are harmful to most forms of life. Varieties of stromatolites still flourish to this day with well - known formations in parts of Australia, Brazil, and the Bahamas
Aegean Sea from the shuttle Atlantis - 09/2000 - Aegean Sea from the space shuttle Atlantis 09/2000 - The Aegean Sea, with Greece and Turkey, seen by the shuttle Atlantis on 09/09/2000. Crete (foreground), the Cyclades Islands, Greece and Turkey lie along the margin of the Eurasian and African tectonic plates; Africa is moving northward and being driven down beneath Eurasia. As a result volcanic islands, such as Santorini, develop and fault - bounded basin such, as the Gulf of Corinth, are formed. In addition, lavas and sediments that were originally deposited on the Mediterranean seafloor are uplifted and deformed
Aegean Sea from Space - Aegean Sea from Space - The Aegean Sea, with Greece, Cyclades, Crete and Turkey, seen from the International Space Station (ISS) in March 2010. Crete (foreground), the Cyclades Islands, Greece and Turkey lie along the margin of the Eurasian and African tectonic plates; Africa is moving northward and being driven down beneath Eurasia. As a result volcanic islands, such as Santorini, develop and fault - bounded basin such, as the Gulf of Corinth, are formed. In addition, lavas and sediments that were originally deposited on the Mediterranean seafloor are uplifted and deformed. Image taken from the International Space Station (ISS) in March 2010
March: Hebes Chasma - Mars: Hebes Chasma - Hebes Chasma is a basin of almost 8000 m deep located in the northern part of Valles Marineris, the great Martian canyon. At the centre of this depression is a stratified plateau that constitutes sedimentary deposits. Image obtained by the Mars Express probe in 2005. View of Hebes Chasma obtained by the High Resolution Stereo Camera (HRSC) on ESA's Mars Express spacecraft. Hebes Chasma is an enclosed trough, almost 8000 m deep, in Valles Marineris, the Grand Canyon of Mars. A mesa - like mountain is located in the center of Hebes Chasma. It reaches 8000 meters above the graben floor and extends almost to the top of the surrounding plain. The mountain is made up by numerous stacked rock layers. The layering may consists of remnants of the older plateau, lake sediments, wind blown sediments or volcanic rock. The rock layers were exposed by erosional processes. Newest data acquired by the OMEGA spectrometer on - board Mars Express revealed hydratized (water - bearing) minerals like gypsum in some areas of Hebes Chasma. What ever kind of processes led to the formation of the Interior Layered Deposits: at least some water once existed in Hebes Chasma. Hebes Chasma is located at approximately 1* south and 282* east. The HRSC obtained image data on 16 September 2005 with a ground resolution of approximately 15 m/pixel
Maldives: An inland freshwater lake surrounded by mangroves (in the distance waves break on the coral reef out to sea), Fen Muli Island, Addu Atoll (Seenu Atoll)
Maldives: An inland freshwater lake surrounded by mangroves (in the distance waves break on the coral reef out to sea), Fen Muli Island, Addu Atoll (Seenu Atoll)
Maldives: An inland freshwater lake surrounded by mangroves (in the distance waves break on the coral reef out to sea), Fen Muli Island, Addu Atoll (Seenu Atoll)
Maldives: A heron sits in the mangroves (mangroves help to protect the islands from all but the biggest waves), Fen Muli Island, Addu Atoll (Seenu Atoll)
Ploughboat, 1993 (photo)
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Mississippi River Delta, Louisiana, USA in 1976 and 2001 (photo)
Landsat 8 scene, 2003
Dunes near the north pole on Mars - Dunes at North Polar Cap on Mars: Image obtained on March 26, 2014 by the HIRISE camera on board the Mars Reconnaissance orbiter probe. HIRISE is a 50 cm telescope that observes visible and near infrared. Formative down-slope winds descending on Mars' North Polar ice cap likely play an important role in transporting sediment from the base of the ice cap into the dune fields that sit beyond the ice cap. The deep chasm that formed on the polar cap edge is identified as an area of strong down-slope winds and has a clear connection to Mars' largest dune field, Olympia Undae. Repeat HiRise images from this chasm that specifically targets the dunes, provides the basis to evaluate the sand fluxes which are associated with the dune and ripple movement in this area
Betsiboka River Delta - Madagascar - - Betsiboka estuary, Madagascar, seen from space - Betsiboka River Delta seen from space shuttle Atlantis in July 2001. During the 20th Century Madagascar, the world's fourth largest island, experienced a tremendous reversal in the quantity of vegetative cover throughout the entire island. From an estimated 80 to 90 percent vegetation cover in 1900 to less than an estimated 10 percent by the year 2000, the rate of deforestation has been dramatic. This image, along with many other space - acquired images, documents the massive annual soil losses that have occurred during the last 30 years. Note the orange - brown sediment that is almost always being transported by the Betsiboka River and being deposited in the delta region. The sequence of images astronauts have taken over time, shows the sediment accumulating and forming islands in the estuary mouth
Garzweiler open pit mine, 1995 (photo)
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Tide Pool, Oregon, 1974 (silver gelatin print)
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Mississippi River Delta, Louisiana, Usa, True Colour Satellite Image
Banks of the Bahamas seen from space - Great Bahamas Bank: Image obtained on 5 February 2014 by the Landsat-8 satellite. Underwater structures of the Great Bahamas Bank are pictured in this image from the Landsat-8 satellite on 5 February 2014. Sitting north of Cuba, the bank is made of limestone - mainly from the skeletal fragments of marine organisms - that has been accumulating for over 100 million years. Currents sculpted these underwater sediments into the wavy pattern we see along the bottom of the image, just a few meters deep. We can clearly see where the shallow waters drop off into the deep, dark water of an area known as the Tongue of the Ocean. With depths of up to about 4000 m, this trench surrounded by islands, reefs and shoals has an opening to the Atlantic Ocean at its northern end (not pictured). Over the deep Tongue we can see a few sparse clouds
Sedimentary layer of rock
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View from the Mastcam on NASA's Curiosity Mars rover looks southward at the Kimberley waypoint
March: chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles and Sacra Fossae. To the north, the large impact crater is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The image shows an old 35 km - diameter impact crater in the north. The crater's southwestern rim is eroded strongly, mostly by flowing water. The source of the water was located in Etus Chasma, which lies about 850 km to the southwest. The crater floor and the northwestern part are remarkably flat, formed by sediments and basaltic lava flows from the Tharsis volcanic region
Bombetoka Bay, Madagascar, from space, c 2005
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Lake Amadeus, Australia, True Colour Satellite Image
Scotland view by satellite - United Kingdom seen from space: United Kingdom seen by satellite Sentinel-3A on 9 May 2016 - The recently launched Sentinel-3A satellite takes us over the United Kingdom, in this false-colour image acquired on 9 May 2016 - Made up of England, Scotland, Wales and Northern Ireland, the UK is an island nation in northwestern Europe - At the top centre of the image, we can see aircraft contrails - water vapour condenses around the small particles in the aircraft exhaust to form ice crystals - The result is the formation of an elongated cloud-like condensation trail in the sky, unmistakable in the centre of the image - At top right, some snow cover in southern Norway is still evident. At bottom right, part of the Netherlands with the unmistakable 700 sq km Lake Markermeer is clearly visible - In the southern North Sea/English Channel, an algal bloom is distinguishable in shades of light blue and green. Meanwhile, closer to the coast we can see brown sediments where rivers and streams run into the sea - The Scottish Highlands at the tip of the United Kingdom appear light brown, representing bare soil and rock formations, with some vegetation. The rest of the island, as well as the visible part of Ireland, are very green, representing dense vegetation
Christchurch and the Peninsula of Banks (New Zealand) from space - Christchurch and Banks Peninsula, New Zealand - The Peninsula of Banks and the City of Christchurch seen from the International Space Station (ISS) on August 15, 2006. The Banks Peninsula is an ancient erode volcano forming a peninsula on the east coast of the South Island. Oblique view (the photograph was taken from a side angle) of the city of Christchurch, New Zealand. Snow highlights the peaks of the Banks Peninsula to the southeast of the city. The peninsula has a radically different landscape compared to the adjoining, flat Canterbury Plains, where Christchurch (gray patch to the north) is located. The Banks Peninsula is formed from the overlapping cones of the extinct Lyttelton and Akaroa volcanoes. Subsequent erosion of the cones formed the heavily dissected terrain visible in the image, and sea level rise led to the creation of several harbors around the Peninsula. Erosion continues unabated today, as evidenced by the apron of greenish blue, sediment - laden waters surrounding the Banks Peninsula. Other interesting features in the image include the braided Waimakariri River to the north - northwest of the city, and the greenish brown waters of Lake Ellesmere at image left. The coloration of the water is due both to its shallow depth (1.4 meters on average) and its high concentrations of nitrogen and phosphorus, which fertilizes the growth of large amounts of green algae
STYROFOAM DEAD FISH FLOAT IN ARGENTINA'S MOST POLLUTED RIVER., 2000-11-28 (photo)
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Dust Tempete on Dubai - 02/2009 - Dust storm on Dubai - 02/2009 - Dust Tempete on Dubai seen by Terra satellite on February 28, 2009. The coasts of the Emirates of Dubai with the three palm islands of Jebel and the World, an archipelago of 250 to 300 private islands, are hardly discernible. Heat and dust storms plagued the United Arab Emirates at the end of February 2009. Temperatures soared to 37 degrees Celsius (98.6 degrees Fahrenheit), the highest February temperatures since record keeping began in 1974. Pushed by winds gusting to 35 knots (65 kilometers per hour), dust storms reduced visibility throughout the region. Parallel plumes of dust blow off the coast of the United Arab Emirates and over the Persian Gulf in this image acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA's Terra satellite on February 28, 2009. In this true - color image, the beige plumes of dust partially obscure the satellite's view of the ocean water. In some places, the dust appears to form wave patterns that run perpendicular to the dust plumes. Neither the capital city of Abu Zabi (also known as Abu Zaby or Abu Dhabi) nor the human - engineered Palm Island Resorts escape the plumes. Part of the Arabian Peninsula's Empty Quarter, or Rub 'al Khali, the United Arab Emirates is covered by sand seas and dry salt lakes. The sand and fine sediments provide ample material for dust storms
The banded iron formations exposed in this sedimentary rock, originated more than 2..., 2000 (photo)
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Mississippi Delta, Louisiana, seen by satellite - Mississippi River Delta. Louisiana - Mississpi Delta, Louisiana, USA, seen by Landsat-7 satellite, November 27, 1999. The Mississippi River drains the heart of the North American continent, carrying vast quantities of sediment and depositing it along the shore of Louisiana and into the Gulf of Mexico. The sediment is composed of topsoil, sand, dead and decaying plants, and anything else washed away by a strong rainstorm far upstream. Many of these effluents are nutrients that act as fertilizer for the microscopic plants (phytoplankton) living near the surface of the Gulf waters. Each summer the phytoplankton population explodes. As the phytoplankton age, die, and decompose, bacteria absorb oxygen dissolved in the water, creating a dead zone”” along the shore at the ocean bottom. The oxygen - poor water is deadly to animals, from the microscopic zooplankton that graze on phytoplankton to crustaceans, molluscs, and fish. Once infrequent, the Gulf of Mexico dead zone is now an annual event, triggered by phosphorus and nitrogen in fertilizers used on farms throughout the central United States and as far away as Saskatchewan, Canada. In the fall, strong winds from seasonal storms stir the water, mixing the oxygen - poor deep water with oxygen - rich surface water, bringing a reprieve until the next spring. The true - color image above was acquired on November 27, 1999, by the Enhanced Thematic Mapper plus (ETM +) aboard Nasa's Landsat 7 satellite.
GREENPEACE ACTIVIST SHOWS SAMPLES OF WATER ALLEGEDLY CONTAMINATED
BY AN OIL COMPANY., 2000-12-18 (photo)
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San Francisco Bay area view from space - San Francisco Bay area seen from space - San Francisco Bay area seen from space on April 17, 1998 from space shuttle Columbia. San Francisco Bay Area, California April 17, 1998. Considered one of the best natural harbors in the world, San Francisco Bay, with its various sediment patterns, can be seen in this unique near - vertical view. Surrounded by the San Francisco Metropolitan area to the west and southwest, the Berkeley and Oakland Metropolitan area to the east, and the San Jose Metropolitan (not visible on the image) to the southeast, San Francisco Bay is 50 miles (80 km) long and from 3 to 13 miles (5 to 21 km) wide. Waters of the Pacific Ocean (bottom of image) enter the bay through Golden Gate, a strait between two peninsulas. The world famous Golden Gate Bridge is discernible on the image connecting the two peninsulas. The bay is as deep as 100 feet (30 meters) in spots, with a channel 50 feet (15 meters) deep maintained through the sand bar off Golden Gate. The major transportation routes in all metropolitan areas are visible on this image. Also discernible is the San Mateo Bridge near the right center of the image. Just to the left of the center of the image is Treasure Island, an artificial island covering 400 acres (162 hectares). It was constructed as a site of the Golden Gate International Exposition (1939 - 1940) and became a United States Naval Base in 1941. The small white objects in the bay and entering the golden gate are ships
GREENPEACE ACTIVIST SHOWS SAMPLES OF WATER ALLEGEDLY CONTAMINATED
BY AN OIL COMPANY., 2000-12-18 (photo)
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Caspian sea area seen from space - Caspian sea area seen from space - Satellite photo of the Caspian Sea obtained by Aqua satellite on 30 September 2004. The borders are drawn. In the upper left portion of the image, the southwestern - most portion of Russia spreads across the broad plains north of the Caucasus Mountains. Georgia runs along the southern face of the Caucasus Mountains and part of the southeastern shore of the Black Sea. In the small valley and plains south of Russia and on the central shore of the Caspian Sea, Azerbaijan sprawls until butting up against the mountains of Armenia and northern Iran. Another small piece of Azerbaijan is tucked away on the far side of Armenia. Stretching far from the southern shores of the Black Sea into the mountains and deserts of the Middle East is eastern Turkey, while in the bottom right corner, Syria and Iraq mark the northern edges of the Syrian Desert. The Reshteh - ye Kuhha - ye Alborz Mountains curve in a bright green arc around the southern end of the Caspian Sea in northwestern Iran, while on the far side of the Caspian Sea, Kazakhstan (upper right) and Turkmenistan (lower right) sprawl across the Urstyurt Plateau. Three major lakes stand out like jewels against the mountains in the lower left portion of the image - Lake Van in eastern Turkey, Lake Sevana in Armenia, and the turquoise - hued Lake Urmia in northwestern Iran. Like the Caspian Sea, the bright colors are likely due to sediment in the waters. Image taken by satellite Aqua on September 30, 2004. NB: borders are marked
NASA MARS GLOBAL SURVEYOR VIEW OF PLANET MARS SURFACE, 2000-12-04 (photo)
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Lake Orumieh in Iran seen from space - Lake Urmia in Iran seen from space - Lake Orumieh is the largest lake in Iran. This dirty lake is a UNESCO biosphere reserve. Image obtained by Space Shuttle Challenger in October 1984. Lake Urmia is an isolated lake in Azerbaijan Province in northwest Iran. The total area of the lake is 1815 square miles (4700 square kilometers), and the north - south length is about 90 miles (145 kilometers). The maximum depth of the shallow, saline lake is approximately 50 feet (15 meters). Climatically, the lake region is located in a semiarid, almost desert environment, with general precipitation averaging 12 inches (30 centimeters) per year. Topographically, the entire region is either plateau or mountain. The surface of the lake is approximately 4100 feet (1250 meters) above sea level with several of the individual volcanic peaks reaching more than 7000 feet (2134 meters) above sea level. The massive, rugged mountain range west of the lake has ridges that exceed 11,000 feet (3353 meters) above sea level. Agricultural patterns are visible in several delta areas around the lake (darker signatures). Sediment patterns can be seen along the southern end of the lake near the salt flats and the delta areas. The highly reflective area along the eastern shore of the lake appears to be either the development of salt deposits along the shoreline or the receding water level in the lake, which exposes more shoreline. The narrow linear features jutting into the lake from opposing shorelines (towards the middle of the lake) could not be identified, but appear to be manmade. Image taken from the space shuttle Challenger in october 1984
Traces of the impact crater Chicxulub - Chicxulub impact crater - Excessive relief view of the Yucatan peninsula obtained from radar altimetric data acquired by the SRTM instrument aboard the space shuttle Endeavour in 2000. An arc of circle is visible to the north-west of the peninsula, marking the outer edge of the Chicxulub impact crater whose centre is located off the Mexican coast. This meteorite impact would have caused the disappearance of dinosaurs 65 million years ago. This shaded relief image of Mexico's Yucatan Peninsula show a subtle, but unmistakable, indication of the Chicxulub impact crater. Most scientists now agree that this impact was the cause of the Cretatious - Tertiary Extinction, the event 65 million years ago that marked the sudden extinction of the dinosaurs as well as the majority of life then on Earth. Most of the peninsula is visible here, along with the island of Cozumel off the east coast. The Yucatan is a plateau composed mostly of limestone and is an area of very low relief with elevations varying by less than a few hundred meters (about 500 feet.) In this computer - enhanced image the topography has been greatly exaggerated to highlight a semicircular trough, the darker green arcing line at the upper left corner of the peninsula. This trough is only about 3 to 5 meters (10 to 15 feet) deep and is about 5 km. wide (3 miles), so subtle that if you walked across it you probably would not notice it, and is a surface expression of the crater's outer boundary. Scientists believe the impact, which was centered just off the coast in the Caribbean, altered the subsurface rocks such that the overlying limestone sediments, which formed later and erode very easily, would preferentially erode on the vicinity of the crater rim. This formed the trough as well as numerous sinkholes (called cenotes) which are visible as small circular depressions. Two visualization methods were combined to produce the image: shading a
Sand Hills, Nebraska, from space, c 2000
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II. WK, Reich Labor Service 1943 (photo)
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The Alps seen by satellite Envisat - The Alps as seen from satellite Envisat - Les Alpes seen by satellite ENVISAT on 8 December 2008. The snow - capped, crescent - shaped Alps and Italy's Apennines mountain chain are shown in this Envisat image. Snowfall in early winter - for meteorologists winter begins on the 1 December - covered the whole mountain areas with fresh snow, while the lower lands in the south and north of the mountains remained snow - free. Due to this snow cover and a relatively low illumination angle of the sun, the ranges and valleys of the mountains stand out in the image. Much of the whiteness seen in the top of the image is cloud cover, but fog is visible in the valleys such as the Rhine. The Alps - central Europe's major mountain range - extend some 1,200 km through France, Switzerland, Italy and Austria and down through Slovenia, Croatia, Bosnia and Herzegovina, Serbia and Montenegro and Albania as the Dinaric Alps. The Alps occupy an area of about 200,000 km and are inhabited by some 20 million people. On the southern side of the Alps a series of glacier carved lakes are visible in dark blue, including Lake Como, Lake Maggiore and Lake Garda. With an area of 370 km, Garda is the largest lake in Italy. The Apennines (visible mostly in brown) stretch the entire length of the Italian Peninsula. Most of Italy's rivers find their source in the Apennines, including the Tiber and Arno. Lakes visible on the Italian Peninsula include Trasimeno (green) and Bolsena (blue). All lakes of central Italy are of volcanic origin and are resting in former volcano craters, which accounts for their almost perfectly round shape. The Ligurian Sea to the west of Italy and the Adriatic Sea to Italy's east are both visible. (In this image, north is in the upper left corner.) The light green colour of the seas along the coast is caused by increased sediments carried by the rivers due to the heavy rainfalls over the last weeks. Corsica, the Mediterranean's f
Saudi Arabia's coral reefs - Al Wadj Bank, Saudi Arabia - Approximately 260 coral species have been recorded in Al Wadj Bank coral reefs in Saudi Arabia. Image obtained from the International Space Station (ISS) in December 2007. Saudi Arabia boasts the most coral reefs of any Middle Eastern country, as it includes coastline along both the Red Sea and the Gulf of Arabia. This high - resolution astronaut photograph shows part of the Al Wadj Bank, located along the northern Red Sea coast. Despite the relatively high salinity of Red Sea water, approximately 260 species of coral have been documented in the region. Large tracts of the Saudi Arabian coastline are undeveloped, and reefs in these areas are in generally good ecological health. However, reefs located near large urban centers such as Jeddeh have suffered degradation due to land reclamation (dredging and filling), pollution, and increased sediment runoff from land. The Al Wadj Bank (a bank is an underwater hill) includes a healthy and diverse reef system, extensive seagrasses beds, and perhaps the largest population of dugong - - a marine mammal similar to the North American manatee - - in the eastern Red Sea. The portion of the Bank in this image illustrates the complex form and topography of the reef system. Several emergent islands (tan) are visible, surrounded primarily by dark green seagrasset; the largest is at top left. Only the islands are above the waterline; over the reefs, the water color ranges from light teal (shallow) to turquoise (increasing depth). The southern edge of the reef is well defined by the deep, dark blue water of the Red Sea (top). Image taken from the international space station (ISS) in december 2007
Evaporation of the Aral Sea - Evaporation of the Aral Sea - Comparison of satellite images taken on 19 August 2000 (left) and 16 August 2009 (right) by the Terra satellite. In overprint, the shore of the Aral Sea in 1960. In the first half of the 20th century, the Aral Sea was the fourth largest lake. In the 1960s, the Sovietic Union began a massive irrigation project in what is now Kazakhstan, Uzbekistan and Turkmenistan, moving water from rivers that feed the Aral Sea to irrigate agricultural land. In August 2009, virtually nothing remains of the eastern lobe of the southern Aral Sea. In 2005, Kazakhstan built the Kok-Aral dam between the northern and southern parts of the lake to successfully preserve water levels in the north. The southern part of the Aral Sea is considered irrecuperable. Comparison of satellite images taken on August 19 2000 (left) and August 16 2009 (right) by satellite Terra. Approximate shoreline in 1960 has been added. The Aral Sea, is actually a lake rather than a sea. In the 1960s, the Soviet Union began a massive irrigation project in what are now Kazakhstan, Uzbekistan, and Turkmenistan, diverting water from the rivers that feed the Aral Sea to irrigate farmland. Although the Northern Aral Sea (upper right) still appears healthy, the Southern Aral Sea consists of two isolated water bodies: an irregular oval shape directly southwest of the Northern Aral Sea, and the long, thin remainder of the Southern Aral Sea's far western lobe. Although the faintest glimmers of blue - green appear in the eastern lobe, earth tones predominate, surrounded by a ghostly film of pale beige. Lake sediments from this depleted water body have provided ample material for frequent dust storms. Much of what finally doomed the Southern Aral Sea was an attempt to save its neighbor to the north. In 2005, Kazakhstan built the Kok - Aral Dam between the lake's northern and southern p
Carlisle State Management Brewery, Bridge Street, Caldewgate, Carlisle, Carlisle, Cumbria, UK, 1954 (b/w photo)
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