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Buru babirusa or Moluccan babirusa, Babyrousa babyrussa. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Buru babirusa or Moluccan babirusa, Babyrousa babyrussa. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660220: Buru babirusa or Moluccan babirusa, Babyrousa babyrussa. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Alpaca, Vicugna pacos. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Alpaca, Vicugna pacos. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660228: Alpaca, Vicugna pacos. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Javan rhinoceros, Rhinoceros ondaicus. Critically endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Javan rhinoceros, Rhinoceros ondaicus. Critically endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660235: Javan rhinoceros, Rhinoceros ondaicus. Critically endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

India and Sri Lanka seen by Gemini - 11 09/1966 - India and Sri Lanka observed by Gemini - 11 on 14/09/1966
India and Sri Lanka seen by Gemini - 11 09/1966 - India and Sri Lanka observed by Gemini - 11 on 14/09/1966

PIX4660240: India and Sri Lanka seen by Gemini - 11 09/1966 - India and Sri Lanka observed by Gemini - 11 on 14/09/1966 / Bridgeman Images

Arabian oryx or white oryx, Oryx leucoryx, and Javan rusa deer or Sunda sambar. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Arabian oryx or white oryx, Oryx leucoryx, and Javan rusa deer or Sunda sambar. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660270: Arabian oryx or white oryx, Oryx leucoryx, and Javan rusa deer or Sunda sambar. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Addax or screwhorn antelope, Addax nasomaculatus. Critically endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Addax or screwhorn antelope, Addax nasomaculatus. Critically endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660291: Addax or screwhorn antelope, Addax nasomaculatus. Critically endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Narwhal, Monodon monoceros, goose-beaked whale, Ziphius cavirostris, and northern bottlenose whale, Hyperoodon ampullatus. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Narwhal, Monodon monoceros, goose-beaked whale, Ziphius cavirostris, and northern bottlenose whale, Hyperoodon ampullatus. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660312: Narwhal, Monodon monoceros, goose-beaked whale, Ziphius cavirostris, and northern bottlenose whale, Hyperoodon ampullatus. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Southern right whale dolphin, Lissodelphis peronii, and pantropical spotted dolphin. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Southern right whale dolphin, Lissodelphis peronii, and pantropical spotted dolphin. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660321: Southern right whale dolphin, Lissodelphis peronii, and pantropical spotted dolphin. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Long-finned pilot whale, Globicephala melas, and Risso's dolphin, Grampus griseus. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Long-finned pilot whale, Globicephala melas, and Risso's dolphin, Grampus griseus. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660334: Long-finned pilot whale, Globicephala melas, and Risso's dolphin, Grampus griseus. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Sei whale, Balaenoptera borealis. Endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.
Sei whale, Balaenoptera borealis. Endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838.

FLO4660353: Sei whale, Balaenoptera borealis. Endangered. Handcoloured copperplate engraving from Rene Primevere Lesson's Complements de Buffon, Pourrat Freres, Paris, 1838. / Bridgeman Images

Merchant de plaisir - Biscuit or cookie seller, Paris, early 19th century, in white bodice and bonnet, over blue petticoat and scarlet apron - Handcoloured copperplate engraving by Gatine after an illustration by Louis-Marie Lante from “” Ouvrieres de Paris” (Tradeswomen of Paris), Paris, 1823
Merchant de plaisir - Biscuit or cookie seller, Paris, early 19th century, in white bodice and bonnet, over blue petticoat and scarlet apron - Handcoloured copperplate engraving by Gatine after an illustration by Louis-Marie Lante from “” Ouvrieres de Paris” (Tradeswomen of Paris), Paris, 1823

FLO4658449: Merchant de plaisir - Biscuit or cookie seller, Paris, early 19th century, in white bodice and bonnet, over blue petticoat and scarlet apron - Handcoloured copperplate engraving by Gatine after an illustration by Louis-Marie Lante from “” Ouvrieres de Paris” (Tradeswomen of Paris), Paris, 1823 / Bridgeman Images

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
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

PIX4658455: 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 / Bridgeman Images

Condensation trains seen from ISS. - Contrails over Rhone valley seen from ISS. - Condensation trains caused by air traffic. Upstairs, Leman Lake. Image obtained from the International Space Station on May 15, 2002. This digital photograph taken through the windows of the International Space Station on May 15, 2002, shows condensation trails over the Rhone Valley. Condensation trails - - or contrails - - are straight lines of ice crystals that form in the wake of jet liners where air temperatures at altitude are lower than about - 40* C. Newer contrails are thin whereas older trails have widened with time as a result of light winds. Because of this tendency for thin contrails to cover greater areas with time, it is estimated that these artificial clouds”” cover 0.1% of the planet's surface. Percentages are far higher in some places such as southern California, the Ohio River Valley and parts of Europe, as illustrated here.
Condensation trains seen from ISS. - Contrails over Rhone valley seen from ISS. - Condensation trains caused by air traffic. Upstairs, Leman Lake. Image obtained from the International Space Station on May 15, 2002. This digital photograph taken through the windows of the International Space Station on May 15, 2002, shows condensation trails over the Rhone Valley. Condensation trails - - or contrails - - are straight lines of ice crystals that form in the wake of jet liners where air temperatures at altitude are lower than about - 40* C. Newer contrails are thin whereas older trails have widened with time as a result of light winds. Because of this tendency for thin contrails to cover greater areas with time, it is estimated that these artificial clouds”” cover 0.1% of the planet's surface. Percentages are far higher in some places such as southern California, the Ohio River Valley and parts of Europe, as illustrated here.

PIX4672384: Condensation trains seen from ISS. - Contrails over Rhone valley seen from ISS. - Condensation trains caused by air traffic. Upstairs, Leman Lake. Image obtained from the International Space Station on May 15, 2002. This digital photograph taken through the windows of the International Space Station on May 15, 2002, shows condensation trails over the Rhone Valley. Condensation trails - - or contrails - - are straight lines of ice crystals that form in the wake of jet liners where air temperatures at altitude are lower than about - 40* C. Newer contrails are thin whereas older trails have widened with time as a result of light winds. Because of this tendency for thin contrails to cover greater areas with time, it is estimated that these artificial clouds”” cover 0.1% of the planet's surface. Percentages are far higher in some places such as southern California, the Ohio River Valley and parts of Europe, as illustrated here. / Bridgeman Images

Condensation Trains - Contrails - Aircraft Condensation Trainees whose shadow is projected on the lower cirrus sail
Condensation Trains - Contrails - Aircraft Condensation Trainees whose shadow is projected on the lower cirrus sail

PIX4672388: Condensation Trains - Contrails - Aircraft Condensation Trainees whose shadow is projected on the lower cirrus sail / Bridgeman Images

Glacier Malaspina, Alaska - The Malaspina Glacier in Alaska - Le Glacier Malaspina, Alaska, from perspective. This image is the result of joint observations made by the Landsat-7 satellite in August 2000 in visible and infrared, combined with elevation radar data obtained by the SRTM (Shuttle Radar Topography Mission) in February 2000. This glacier extends over 3000 km2. Natural colours have been applied to this image: light blue, ice, white, snow, green vegetation, grey rock and blue for the ocean. Malaspina Glacier in southeastern Alaska is considered the classic example of a piedmont glacier. Piedmont glaciers occur where valley glaciers exit a mountain range onto broad lowlands, are no longer laterally confined, and spread to become wide lobes. Malaspina Glacier is actually a compound glacier, formed by the merger of several valley glaciers, the most prominent of which seen here are Agassiz Glacier (left) and Seward Glacier (right). In total, Malaspina Glacier is up to 65 kilometers (40 miles) wide and extends up to 45 kilometers (28 miles) from the mountain front nearly to the sea. This perspective view was created from a Landsat satellite image and an elevation model generated by the Shuttle Radar Topography Mission (SRTM). Landsat views both visible and infrared light, which have been combined here into a color composite that generally shows glacial ice in light blue, snow in white, vegetation in green, bare rock in grays and tans, and the ocean (foreground) in dark blue. The back (northern) edge of the data set forms a false horizon that meets a false sky. Glaciers are sensitive indicators of climatic change
Glacier Malaspina, Alaska - The Malaspina Glacier in Alaska - Le Glacier Malaspina, Alaska, from perspective. This image is the result of joint observations made by the Landsat-7 satellite in August 2000 in visible and infrared, combined with elevation radar data obtained by the SRTM (Shuttle Radar Topography Mission) in February 2000. This glacier extends over 3000 km2. Natural colours have been applied to this image: light blue, ice, white, snow, green vegetation, grey rock and blue for the ocean. Malaspina Glacier in southeastern Alaska is considered the classic example of a piedmont glacier. Piedmont glaciers occur where valley glaciers exit a mountain range onto broad lowlands, are no longer laterally confined, and spread to become wide lobes. Malaspina Glacier is actually a compound glacier, formed by the merger of several valley glaciers, the most prominent of which seen here are Agassiz Glacier (left) and Seward Glacier (right). In total, Malaspina Glacier is up to 65 kilometers (40 miles) wide and extends up to 45 kilometers (28 miles) from the mountain front nearly to the sea. This perspective view was created from a Landsat satellite image and an elevation model generated by the Shuttle Radar Topography Mission (SRTM). Landsat views both visible and infrared light, which have been combined here into a color composite that generally shows glacial ice in light blue, snow in white, vegetation in green, bare rock in grays and tans, and the ocean (foreground) in dark blue. The back (northern) edge of the data set forms a false horizon that meets a false sky. Glaciers are sensitive indicators of climatic change

PIX4672430: Glacier Malaspina, Alaska - The Malaspina Glacier in Alaska - Le Glacier Malaspina, Alaska, from perspective. This image is the result of joint observations made by the Landsat-7 satellite in August 2000 in visible and infrared, combined with elevation radar data obtained by the SRTM (Shuttle Radar Topography Mission) in February 2000. This glacier extends over 3000 km2. Natural colours have been applied to this image: light blue, ice, white, snow, green vegetation, grey rock and blue for the ocean. Malaspina Glacier in southeastern Alaska is considered the classic example of a piedmont glacier. Piedmont glaciers occur where valley glaciers exit a mountain range onto broad lowlands, are no longer laterally confined, and spread to become wide lobes. Malaspina Glacier is actually a compound glacier, formed by the merger of several valley glaciers, the most prominent of which seen here are Agassiz Glacier (left) and Seward Glacier (right). In total, Malaspina Glacier is up to 65 kilometers (40 miles) wide and extends up to 45 kilometers (28 miles) from the mountain front nearly to the sea. This perspective view was created from a Landsat satellite image and an elevation model generated by the Shuttle Radar Topography Mission (SRTM). Landsat views both visible and infrared light, which have been combined here into a color composite that generally shows glacial ice in light blue, snow in white, vegetation in green, bare rock in grays and tans, and the ocean (foreground) in dark blue. The back (northern) edge of the data set forms a false horizon that meets a false sky. Glaciers are sensitive indicators of climatic change / Bridgeman Images

Clouds - Alaska - seen by Landsat 7 06/2000 - Cloud formation over the Aleutian Islands in Alaska. Color variations are explained by the difference in temperature and the size of the water droplets that make up these clouds. Image obtained by satellite Landsat - 7 on 16 June 2000
Clouds - Alaska - seen by Landsat 7 06/2000 - Cloud formation over the Aleutian Islands in Alaska. Color variations are explained by the difference in temperature and the size of the water droplets that make up these clouds. Image obtained by satellite Landsat - 7 on 16 June 2000

PIX4672450: Clouds - Alaska - seen by Landsat 7 06/2000 - Cloud formation over the Aleutian Islands in Alaska. Color variations are explained by the difference in temperature and the size of the water droplets that make up these clouds. Image obtained by satellite Landsat - 7 on 16 June 2000 / Bridgeman Images

Nervous system of the back. Lithograph of Corbie, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.
Nervous system of the back. Lithograph of Corbie, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.

FLO4672457: Nervous system of the back. Lithograph of Corbie, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864. / Bridgeman Images

Bering Glacier, Alaska - Bering Glacier in Alaska - The Bering Glacier is the largest glacier in North America. Since 1900, the glacier front has receded 12 km. Image obtained by Landsat-7 satellite on 29 September 2002. Bering Glacier currently terminates in Vitus Lake south of Alaska's Wrangell - St. Elias National Park, about 10 km from the Gulf of Alaska. Combined with the Bagley Icefield, where the snow that feeds the glacier accumulates, the Bering is the largest glacier in North America. Warmer temperatures and changes in precipitation over the past century have thinned the Bering Glacier by several hundred meters. Since 1900 the terminus has retreated as much as 12 km. Most of the glaciers along the Alaskan coast are retreating along with the Bering Glacier. This true - color image of the Bering Glacier terminus was acquired on September 29, 2002, by the Enhanced Thematic Mapper plus (ETM +) instrument aboard the USGS/NASA Landsat - 7 satellite
Bering Glacier, Alaska - Bering Glacier in Alaska - The Bering Glacier is the largest glacier in North America. Since 1900, the glacier front has receded 12 km. Image obtained by Landsat-7 satellite on 29 September 2002. Bering Glacier currently terminates in Vitus Lake south of Alaska's Wrangell - St. Elias National Park, about 10 km from the Gulf of Alaska. Combined with the Bagley Icefield, where the snow that feeds the glacier accumulates, the Bering is the largest glacier in North America. Warmer temperatures and changes in precipitation over the past century have thinned the Bering Glacier by several hundred meters. Since 1900 the terminus has retreated as much as 12 km. Most of the glaciers along the Alaskan coast are retreating along with the Bering Glacier. This true - color image of the Bering Glacier terminus was acquired on September 29, 2002, by the Enhanced Thematic Mapper plus (ETM +) instrument aboard the USGS/NASA Landsat - 7 satellite

PIX4672475: Bering Glacier, Alaska - Bering Glacier in Alaska - The Bering Glacier is the largest glacier in North America. Since 1900, the glacier front has receded 12 km. Image obtained by Landsat-7 satellite on 29 September 2002. Bering Glacier currently terminates in Vitus Lake south of Alaska's Wrangell - St. Elias National Park, about 10 km from the Gulf of Alaska. Combined with the Bagley Icefield, where the snow that feeds the glacier accumulates, the Bering is the largest glacier in North America. Warmer temperatures and changes in precipitation over the past century have thinned the Bering Glacier by several hundred meters. Since 1900 the terminus has retreated as much as 12 km. Most of the glaciers along the Alaskan coast are retreating along with the Bering Glacier. This true - color image of the Bering Glacier terminus was acquired on September 29, 2002, by the Enhanced Thematic Mapper plus (ETM +) instrument aboard the USGS/NASA Landsat - 7 satellite / Bridgeman Images

Hubbard Glacier - Alaska - Wide view of Hubbard Glacier - Alaska - The Hubbard Glacier is the longest glacier in North America leading to the sea. Hubbard Glacier, the largest tidewater glacier in the world. The Hubbard and Turner/Haenke Glaciers extend out into Disenchantment Bay (discovered and named by Captain Alejandro Malaspina in 1791, who was disappointed to find the inlet was a dead end). The face of Hubbard Glacier extends 6 1/2 miles in length. The towering ice peaks making up the face of the glacier are 400 to 500 feet high! To give some perspective the Wrangell - St. Elias mountain peaks in the background are all between 14,000 and 18,000 feet in elevation, the tallest coastal mountains in the world
Hubbard Glacier - Alaska - Wide view of Hubbard Glacier - Alaska - The Hubbard Glacier is the longest glacier in North America leading to the sea. Hubbard Glacier, the largest tidewater glacier in the world. The Hubbard and Turner/Haenke Glaciers extend out into Disenchantment Bay (discovered and named by Captain Alejandro Malaspina in 1791, who was disappointed to find the inlet was a dead end). The face of Hubbard Glacier extends 6 1/2 miles in length. The towering ice peaks making up the face of the glacier are 400 to 500 feet high! To give some perspective the Wrangell - St. Elias mountain peaks in the background are all between 14,000 and 18,000 feet in elevation, the tallest coastal mountains in the world

PIX4672493: Hubbard Glacier - Alaska - Wide view of Hubbard Glacier - Alaska - The Hubbard Glacier is the longest glacier in North America leading to the sea. Hubbard Glacier, the largest tidewater glacier in the world. The Hubbard and Turner/Haenke Glaciers extend out into Disenchantment Bay (discovered and named by Captain Alejandro Malaspina in 1791, who was disappointed to find the inlet was a dead end). The face of Hubbard Glacier extends 6 1/2 miles in length. The towering ice peaks making up the face of the glacier are 400 to 500 feet high! To give some perspective the Wrangell - St. Elias mountain peaks in the background are all between 14,000 and 18,000 feet in elevation, the tallest coastal mountains in the world / Bridgeman Images

Glossopharyngeal nerve. Lithograph by Davesne, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.
Glossopharyngeal nerve. Lithograph by Davesne, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.

FLO4672515: Glossopharyngeal nerve. Lithograph by Davesne, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864. / Bridgeman Images

Sympathic nervous system in the cardiac plexus. Lithograph by Davesne, based on a drawing by Leveille, in Petiure Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.
Sympathic nervous system in the cardiac plexus. Lithograph by Davesne, based on a drawing by Leveille, in Petiure Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.

FLO4672521: Sympathic nervous system in the cardiac plexus. Lithograph by Davesne, based on a drawing by Leveille, in Petiure Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864. / Bridgeman Images

Spinal bone, ribs and sternum. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.
Spinal bone, ribs and sternum. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.

FLO4672534: Spinal bone, ribs and sternum. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864. / Bridgeman Images

North America at night - 2012 - North America by night - 2012 - North America at night by satellite. Composite image obtained by the Suomi NPP satellite in April and October 2012. This image of the United States of America at night is a composite assembled from data acquired by the Suomi NPP satellite in April and October 2012
North America at night - 2012 - North America by night - 2012 - North America at night by satellite. Composite image obtained by the Suomi NPP satellite in April and October 2012. This image of the United States of America at night is a composite assembled from data acquired by the Suomi NPP satellite in April and October 2012

PIX4672537: North America at night - 2012 - North America by night - 2012 - North America at night by satellite. Composite image obtained by the Suomi NPP satellite in April and October 2012. This image of the United States of America at night is a composite assembled from data acquired by the Suomi NPP satellite in April and October 2012 / Bridgeman Images

Pelvic bone, front and back views. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.
Pelvic bone, front and back views. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.

FLO4672563: Pelvic bone, front and back views. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864. / Bridgeman Images

Baghdad - Copper Mine in Arizona - USA - Baghdad Copper Mine - Arizona: Baghdad is a copper mining community located in the western state of Arizona in the United States. It is one of the only two labourers that still exist in Arizona. Image taken from the International Space Station (ISS) on 1 March 2007. The Baghdad Mine is a large copper mine located in Arizona, in the southwestern part of the United States. Baghdad represents one of the largest copper reserves in the United States and in the world. The town of Baghdad, Arizona was built as a company town to house mine workers. Astronaut photograph was acquired on March 1, 2007 from the International Space Station (ISS)
Baghdad - Copper Mine in Arizona - USA - Baghdad Copper Mine - Arizona: Baghdad is a copper mining community located in the western state of Arizona in the United States. It is one of the only two labourers that still exist in Arizona. Image taken from the International Space Station (ISS) on 1 March 2007. The Baghdad Mine is a large copper mine located in Arizona, in the southwestern part of the United States. Baghdad represents one of the largest copper reserves in the United States and in the world. The town of Baghdad, Arizona was built as a company town to house mine workers. Astronaut photograph was acquired on March 1, 2007 from the International Space Station (ISS)

PIX4672576: Baghdad - Copper Mine in Arizona - USA - Baghdad Copper Mine - Arizona: Baghdad is a copper mining community located in the western state of Arizona in the United States. It is one of the only two labourers that still exist in Arizona. Image taken from the International Space Station (ISS) on 1 March 2007. The Baghdad Mine is a large copper mine located in Arizona, in the southwestern part of the United States. Baghdad represents one of the largest copper reserves in the United States and in the world. The town of Baghdad, Arizona was built as a company town to house mine workers. Astronaut photograph was acquired on March 1, 2007 from the International Space Station (ISS) / Bridgeman Images

North America seen from space - North America seen from space - North America seen from space. Composite satellite photos. Composite of satellite photographs
North America seen from space - North America seen from space - North America seen from space. Composite satellite photos. Composite of satellite photographs

PIX4672587: North America seen from space - North America seen from space - North America seen from space. Composite satellite photos. Composite of satellite photographs / Bridgeman Images

Ankle and foot bone. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.
Ankle and foot bone. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.

FLO4672592: Ankle and foot bone. Lithograph of Corbie, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864. / Bridgeman Images

Back and torso muscles. Lithograph by Davesne, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.
Back and torso muscles. Lithograph by Davesne, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864.

FLO4672626: Back and torso muscles. Lithograph by Davesne, based on a drawing by Leveille, in Petity Atlas complet d'Anatomie descriptive du Corps Humain, by Dr. Joseph Nicolas Masse, published by Mequignon Marvis, Paris (France), 1864. / Bridgeman Images

Hiker inside Lower Antelope Canyon - A female hiker walks inside Lower Antelope Canyon
Hiker inside Lower Antelope Canyon - A female hiker walks inside Lower Antelope Canyon

PIX4672669: Hiker inside Lower Antelope Canyon - A female hiker walks inside Lower Antelope Canyon / Bridgeman Images

Grand Canyon, Arizona - Grand Canyon, Arizona - North Rim, Bright Angel Point
Grand Canyon, Arizona - Grand Canyon, Arizona - North Rim, Bright Angel Point

PIX4672704: Grand Canyon, Arizona - Grand Canyon, Arizona - North Rim, Bright Angel Point / Bridgeman Images

Grand Canyon, Arizona - Hiker on South Kaibab Trail in Grand Canyon - A tourist admires the Grand Canyon from Skeleton Point on the South Kaibab Trail. Skeleton Point on South Kaibab Trail in Grand Canyon National Park
Grand Canyon, Arizona - Hiker on South Kaibab Trail in Grand Canyon - A tourist admires the Grand Canyon from Skeleton Point on the South Kaibab Trail. Skeleton Point on South Kaibab Trail in Grand Canyon National Park

PIX4672749: Grand Canyon, Arizona - Hiker on South Kaibab Trail in Grand Canyon - A tourist admires the Grand Canyon from Skeleton Point on the South Kaibab Trail. Skeleton Point on South Kaibab Trail in Grand Canyon National Park / Bridgeman Images

Grand Canyon, Arizona - South Kaibab Trail in Grand Canyon - Mules on the South Kaibab Trail. Mules going up South Kaibab Trail in Grand Canyon National Park
Grand Canyon, Arizona - South Kaibab Trail in Grand Canyon - Mules on the South Kaibab Trail. Mules going up South Kaibab Trail in Grand Canyon National Park

PIX4672752: Grand Canyon, Arizona - South Kaibab Trail in Grand Canyon - Mules on the South Kaibab Trail. Mules going up South Kaibab Trail in Grand Canyon National Park / Bridgeman Images

Variety of orchid Lycaste skinneri, the white is of type Alba or Monja Blanca, purple and purple is called nigro rubra. Lithograph by Worthington G.Smith (1835-1917), published in Floral Magazine, 1872, edited by Henry Honywood Dombrain (1818-1905).
Variety of orchid Lycaste skinneri, the white is of type Alba or Monja Blanca, purple and purple is called nigro rubra. Lithograph by Worthington G.Smith (1835-1917), published in Floral Magazine, 1872, edited by Henry Honywood Dombrain (1818-1905).

FLO4671341: Variety of orchid Lycaste skinneri, the white is of type Alba or Monja Blanca, purple and purple is called nigro rubra. Lithograph by Worthington G.Smith (1835-1917), published in Floral Magazine, 1872, edited by Henry Honywood Dombrain (1818-1905). / Bridgeman Images

Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals
Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals

PIX4671358: Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals / Bridgeman Images

Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. The parhely is clearly off the halo of 22* radius when the Sun is 21* high. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals
Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. The parhely is clearly off the halo of 22* radius when the Sun is 21* high. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals

PIX4671367: Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. The parhely is clearly off the halo of 22* radius when the Sun is 21* high. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals / Bridgeman Images

Parhelia - Sundog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals
Parhelia - Sundog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals

PIX4671368: Parhelia - Sundog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals / Bridgeman Images


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