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Images of 'From A Colour Photograph' found, 22,905

 
Chuquicamata Copper Mine - Chile - Chuquicamata Mine - Chile: The Chuquicamata Mine in Chile is the largest open-air copper mine in the world. Located in the Atacama Desert in northern Chile 15 km from the city of Calama, this mine alone contains 13% of the world's copper reserves. Image taken from the International Space Station (ISS) on December 9, 2009. This open-pit copper mine is one of the largest ones in the world. Astronaut photograph was acquired on December 9 2009 from the International Space Station (ISS)

PIX4676015

Chuquicamata Copper Mine - Chile - Chuquicamata Mine - Chile: The Chuquicamata Mine in Chile is the largest open-air copper mine in the world. Located in the Atacama Desert in northern Chile 15 km from the city of Calama, this mine alone contains 13% of the world's copper reserves. Image taken from the International Space Station (ISS) on December 9, 2009. This open-pit copper mine is one of the largest ones in the world. Astronaut photograph was acquired on December 9 2009 from the International Space Station (ISS)

PIX4676015

 
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

PIX4659018

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

PIX4659018

 
Jwaneng Diamond Mine - Botswana - Jwaneng diamond mine - Botswana: The Jwaneng Mine is an open pit diamond mine located in Botswana. Production began in 1982 and is described as the largest diamond mine in the world. Image taken from the International Space Station (ISS) on 30 June 2003. The Jwaneng diamond mine is the richest diamond mine in the world and is located in south-central Botswana. Astronaut photograph was acquired on June 30, 2003 from the International Space Station (ISS)

PIX4658479

Jwaneng Diamond Mine - Botswana - Jwaneng diamond mine - Botswana: The Jwaneng Mine is an open pit diamond mine located in Botswana. Production began in 1982 and is described as the largest diamond mine in the world. Image taken from the International Space Station (ISS) on 30 June 2003. The Jwaneng diamond mine is the richest diamond mine in the world and is located in south-central Botswana. Astronaut photograph was acquired on June 30, 2003 from the International Space Station (ISS)

PIX4658479

 
Toquepala Copper Mine - Peru - Toquepala Copper Mine - Southern Peru: The Toquepala mine in southern Peru is a large open-pit copper mine. Image taken from the International Space Station (ISS) on 22 September 2003. The rugged, mineral-rich Andes supports some of the world's biggest mines (gold, silver, copper, and more). This image looks down the bull's-eye of Peru's Toquepala copper mine, a steep sided and stepped open-pit mine. At the surface the open pit is 6.5 km across and it descends more than 3000 m into the earth. Astronaut photograph was acquired on September 22 2003 from the International Space Station (ISS)

PIX4676455

Toquepala Copper Mine - Peru - Toquepala Copper Mine - Southern Peru: The Toquepala mine in southern Peru is a large open-pit copper mine. Image taken from the International Space Station (ISS) on 22 September 2003. The rugged, mineral-rich Andes supports some of the world's biggest mines (gold, silver, copper, and more). This image looks down the bull's-eye of Peru's Toquepala copper mine, a steep sided and stepped open-pit mine. At the surface the open pit is 6.5 km across and it descends more than 3000 m into the earth. Astronaut photograph was acquired on September 22 2003 from the International Space Station (ISS)

PIX4676455

 
Ol Doinyo Lengai - Volcano Ol Doinyo Lengai - Ol Doinyo Lengai Volcano is an active volcano located in Tanzania in the Great Rift Valley. Ol Doinyo Lengai is the only volcano in the world to emit carbonatite. Image obtained from the EO-1 satellite on 12 September 2009. Volcano Ol Doinyo Lengai is an active volcano located in Tanzania in the great rift valley. It is the only known volcano producing carbonatite. The lava of Ol Doinyo Lengai is extremely cool (500 - 600* C, compared to 1,160* C for typical basaltic lava) and relatively fluid. Ol Doinyo Lengai alternates between eruptions of liquid lava that form lava lakes and fountains (called effusive eruptions) and explosive eruptions that build large cinder and ash cones. The new cone and crater are clearly visible in the center of the image acquired by satellite EO-1 on September 12, 2009. The dark spot in the crater may be fresh lava erupted from a new volcanic vent. Gray ash covers the volcano and much of the surrounding landscape

PIX4659350

Ol Doinyo Lengai - Volcano Ol Doinyo Lengai - Ol Doinyo Lengai Volcano is an active volcano located in Tanzania in the Great Rift Valley. Ol Doinyo Lengai is the only volcano in the world to emit carbonatite. Image obtained from the EO-1 satellite on 12 September 2009. Volcano Ol Doinyo Lengai is an active volcano located in Tanzania in the great rift valley. It is the only known volcano producing carbonatite. The lava of Ol Doinyo Lengai is extremely cool (500 - 600* C, compared to 1,160* C for typical basaltic lava) and relatively fluid. Ol Doinyo Lengai alternates between eruptions of liquid lava that form lava lakes and fountains (called effusive eruptions) and explosive eruptions that build large cinder and ash cones. The new cone and crater are clearly visible in the center of the image acquired by satellite EO-1 on September 12, 2009. The dark spot in the crater may be fresh lava erupted from a new volcanic vent. Gray ash covers the volcano and much of the surrounding landscape

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Eruption of Rabaul volcano in Papua New Guinea, New Guinea - Rabaul eruption in Papua New Guinea - View from space shuttle Discovery of the smoke plume from Rabaul volcano, 19/09/1994. This volcano is located in New Britain, the island of the Bismarck Archipelago in Papua, off New Guinee. View of the Rabaul eruption, located east end of New Britain (island of Bismarck archipelago off the northeastern coast of New Guinea) from the STS - 64 Space Shuttle Discovery on September 19 1994

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Eruption of Rabaul volcano in Papua New Guinea, New Guinea - Rabaul eruption in Papua New Guinea - View from space shuttle Discovery of the smoke plume from Rabaul volcano, 19/09/1994. This volcano is located in New Britain, the island of the Bismarck Archipelago in Papua, off New Guinee. View of the Rabaul eruption, located east end of New Britain (island of Bismarck archipelago off the northeastern coast of New Guinea) from the STS - 64 Space Shuttle Discovery on September 19 1994

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Atafu Atoll - Tokelau Islands, South Pacific - Atafu Atoll, Tokelau, Southern Pacific Ocean - Atafu is a small atoll belonging to the Tokelau Archipelago, in the South Pacific Ocean. With an elevation of two metres above the water, this coral reef is still vulnerable to cyclones and to the rise of water due to global warming. At roughly eight kilometers wide, Atafu Atoll is the smallest of three atolls and one island (Nukunonu and Fakaofo Atoll to the southeast and Swains Island to the south are not shown) comprising the Tokelau Islands group located in the southern Pacific Ocean. The primary settlement on Atafu is a village located at the northwestern corner of the atoll - - indicated by an area of light gray dots in this astronaut photograph. The typical ring shape of the atoll is the result of coral reefs building up around a former volcanic island. Over geologic time, the central volcano has subsided beneath the water surface, leaving the fringing reefs and a central lagoon that co

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Atafu Atoll - Tokelau Islands, South Pacific - Atafu Atoll, Tokelau, Southern Pacific Ocean - Atafu is a small atoll belonging to the Tokelau Archipelago, in the South Pacific Ocean. With an elevation of two metres above the water, this coral reef is still vulnerable to cyclones and to the rise of water due to global warming. At roughly eight kilometers wide, Atafu Atoll is the smallest of three atolls and one island (Nukunonu and Fakaofo Atoll to the southeast and Swains Island to the south are not shown) comprising the Tokelau Islands group located in the southern Pacific Ocean. The primary settlement on Atafu is a village located at the northwestern corner of the atoll - - indicated by an area of light gray dots in this astronaut photograph. The typical ring shape of the atoll is the result of coral reefs building up around a former volcanic island. Over geologic time, the central volcano has subsided beneath the water surface, leaving the fringing reefs and a central lagoon that co

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Richat Structure - Mauritania - Richat structure seen from space - Richat structure, geological formation of volcanic origin, in Mauritania, observed by Space Shuttle Columbia in October 1995. The so-called Richat Structure is a geological formation in the Maur Adrar Desert in the African country of Mauritania. Although it resemble an impact crater, the Richat Structure formed when a volcanic dome hardened and gradually eroded, exposing the onion - like layers of rock. Image taken from the space shuttle Columbia in October 1995

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Richat Structure - Mauritania - Richat structure seen from space - Richat structure, geological formation of volcanic origin, in Mauritania, observed by Space Shuttle Columbia in October 1995. The so-called Richat Structure is a geological formation in the Maur Adrar Desert in the African country of Mauritania. Although it resemble an impact crater, the Richat Structure formed when a volcanic dome hardened and gradually eroded, exposing the onion - like layers of rock. Image taken from the space shuttle Columbia in October 1995

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Millennium Island - Millennium Island - Millennium Island, or Carolina Island, is an uninhabited atoll belonging to the Republic of Kiribati and is the most eastern island in the Pacific Ocean. In 1999, for celebrations marking the arrival of the year 2000, the island of Carolina was officially renamed the island of the Millennium, being one of the points on earth closest to the date change line. This island, whose highest point is about 6 metres, is particularly threatened by rising sea levels. Image obtained on 1 July 2009 from the International Space Station (ISS). Millennium Island is located at the southern end of the Line Islands in the South Pacific Ocean. This uninhabited island is part of the Republic of Kiribati. At a maximum height of approximately 6 meters (19.7 feet) above sea level, Millennium Island has been identified as being at great risk from sea level rise by the United Nations. Millennium Island was known as Caroline Island prior to 2000. The name was changed becau

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Millennium Island - Millennium Island - Millennium Island, or Carolina Island, is an uninhabited atoll belonging to the Republic of Kiribati and is the most eastern island in the Pacific Ocean. In 1999, for celebrations marking the arrival of the year 2000, the island of Carolina was officially renamed the island of the Millennium, being one of the points on earth closest to the date change line. This island, whose highest point is about 6 metres, is particularly threatened by rising sea levels. Image obtained on 1 July 2009 from the International Space Station (ISS). Millennium Island is located at the southern end of the Line Islands in the South Pacific Ocean. This uninhabited island is part of the Republic of Kiribati. At a maximum height of approximately 6 meters (19.7 feet) above sea level, Millennium Island has been identified as being at great risk from sea level rise by the United Nations. Millennium Island was known as Caroline Island prior to 2000. The name was changed becau

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Earth- Illustration - Earth from space. Artwork

S. Numazawa

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Earth- Illustration - Earth from space. Artwork

S. Numazawa

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Cananea Copper Mine - Mexico - Cananea Copper Mine - Sonora - Mexico: The Cananea Mine is an open pit copper and gold mine located in Mexico. Its production began in 1899. Image taken from the International Space Station (ISS) on June 27, 2016. One of the largest open-pit copper mines in the world, the Cananea mine produced over 164,000 tonnes of copper in 2006. The mine is located approximately 40 km south of the border between the USA (Arizona) and Mexico (Sonora). Copper and gold ores at Cananea are found in a porphyry copper deposit, a geological structure formed by crystal-rich magma moving upwards through pre-existing rock layers. The mine workings at Cananea are significant in the recent history of Mexico, as poor working conditions there in 1906 led to a mineral's strike that resulted in 19 deaths. This event is generally considered to a major catalyst of the Mexican Revolution of 1910, as well as the beginning of Mexico's labor movement. Current environmental and economic cond

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Cananea Copper Mine - Mexico - Cananea Copper Mine - Sonora - Mexico: The Cananea Mine is an open pit copper and gold mine located in Mexico. Its production began in 1899. Image taken from the International Space Station (ISS) on June 27, 2016. One of the largest open-pit copper mines in the world, the Cananea mine produced over 164,000 tonnes of copper in 2006. The mine is located approximately 40 km south of the border between the USA (Arizona) and Mexico (Sonora). Copper and gold ores at Cananea are found in a porphyry copper deposit, a geological structure formed by crystal-rich magma moving upwards through pre-existing rock layers. The mine workings at Cananea are significant in the recent history of Mexico, as poor working conditions there in 1906 led to a mineral's strike that resulted in 19 deaths. This event is generally considered to a major catalyst of the Mexican Revolution of 1910, as well as the beginning of Mexico's labor movement. Current environmental and economic cond

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Palabora Mine - South Africa - Phalaborwa Copper Mine - Republic South Africa - The Palabora Copper Mine in South Africa is the largest open pit mine and the largest artificial hole in the world with 2,000 metres in diameter and 762 metres deep. Image obtained from the International Space Station (ISS) in December 2009. Palabora Mining Company Limited's open cast mine is Africa's widest man-made hole at almost 2,000 meters wide. Seen from the international space station in december 2009

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Palabora Mine - South Africa - Phalaborwa Copper Mine - Republic South Africa - The Palabora Copper Mine in South Africa is the largest open pit mine and the largest artificial hole in the world with 2,000 metres in diameter and 762 metres deep. Image obtained from the International Space Station (ISS) in December 2009. Palabora Mining Company Limited's open cast mine is Africa's widest man-made hole at almost 2,000 meters wide. Seen from the international space station in december 2009

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Lake Chad seen by satellite in 2007 - Lake Chad as seen by satellite in 2007 - Lake Chad seen by Envisat satellite on 19 December 2007. This Envisat image highlights Lake Chad, a freshwater lake located in central Africa at the junction of Chad, Cameroon, Nigeria and Niger. Lake Chad, once Africa's third largest inland water body, is located in West Africa's Sahel region - a transition zone between the Sahara Desert to the north and savannas and woodlands to the south. Because the lake is shallow, between 1 m in the northwest and 7 m in the south, it has always undergone seasonal fluctuations. However, it has shrunk dramatically over the last four decades due to a decrease in rainfall and an increase in the amount of water used for irrigation projects. Lake Chad's surface area was 25 000 sq km in the early 1960s, compared with 1350 sq km in 2001. Lake Chad is fed primarily by the Chari and Logone Rivers, which are both located in the southwest and flow northward into the lake, which do

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Lake Chad seen by satellite in 2007 - Lake Chad as seen by satellite in 2007 - Lake Chad seen by Envisat satellite on 19 December 2007. This Envisat image highlights Lake Chad, a freshwater lake located in central Africa at the junction of Chad, Cameroon, Nigeria and Niger. Lake Chad, once Africa's third largest inland water body, is located in West Africa's Sahel region - a transition zone between the Sahara Desert to the north and savannas and woodlands to the south. Because the lake is shallow, between 1 m in the northwest and 7 m in the south, it has always undergone seasonal fluctuations. However, it has shrunk dramatically over the last four decades due to a decrease in rainfall and an increase in the amount of water used for irrigation projects. Lake Chad's surface area was 25 000 sq km in the early 1960s, compared with 1350 sq km in 2001. Lake Chad is fed primarily by the Chari and Logone Rivers, which are both located in the southwest and flow northward into the lake, which do

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Richat Structure - Mauritania - Richat structure seen from space - Richat structure, geological formation of volcanic origin, in Mauritania, observed from the International Space Station (ISS) in February 2009. The so-called Richat Structure is a geological formation in the Maur Adrar Desert in the African country of Mauritania. Although it resemble an impact crater, the Richat Structure formed when a volcanic dome hardened and gradually eroded, exposing the onion - like layers of rock. Image taken from the International space station (ISS) in February 2009

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Richat Structure - Mauritania - Richat structure seen from space - Richat structure, geological formation of volcanic origin, in Mauritania, observed from the International Space Station (ISS) in February 2009. The so-called Richat Structure is a geological formation in the Maur Adrar Desert in the African country of Mauritania. Although it resemble an impact crater, the Richat Structure formed when a volcanic dome hardened and gradually eroded, exposing the onion - like layers of rock. Image taken from the International space station (ISS) in February 2009

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Malosmadulu Atoll (Maldives) - South Malosmadulu atolls (Maldives) seen from space - Southern part of Malosmadulu Atoll in Maldives seen from the International Space Station (ISS) in July 2001. South Malosmadulu Atoll are in the Maldives, an island republic in the northern Indian Ocean, southwest of India. The Maldives are made up of a chain of 1,192 small coral islands, which are grouped into clusters of atolls. Arguably the lowest - lying country in the world, the average elevation is just 1 meter above sea level. Image taken from the International Space Station (ISS) in july 2001

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Malosmadulu Atoll (Maldives) - South Malosmadulu atolls (Maldives) seen from space - Southern part of Malosmadulu Atoll in Maldives seen from the International Space Station (ISS) in July 2001. South Malosmadulu Atoll are in the Maldives, an island republic in the northern Indian Ocean, southwest of India. The Maldives are made up of a chain of 1,192 small coral islands, which are grouped into clusters of atolls. Arguably the lowest - lying country in the world, the average elevation is just 1 meter above sea level. Image taken from the International Space Station (ISS) in july 2001

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Richat Structure - Mauritania - Richat structure seen from space - Richat structure, geological formation of volcanic origin, in Mauritania, observed by space shuttle Atlantis in May 2000. The so-called Richat Structure is a geological formation in the Maur Adrar Desert in the African country of Mauritania. Although it resemble an impact crater, the Richat Structure formed when a volcanic dome hardened and gradually eroded, exposing the onion - like layers of rock. Image taken from the space shuttle Atlantis in May 2000

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Richat Structure - Mauritania - Richat structure seen from space - Richat structure, geological formation of volcanic origin, in Mauritania, observed by space shuttle Atlantis in May 2000. The so-called Richat Structure is a geological formation in the Maur Adrar Desert in the African country of Mauritania. Although it resemble an impact crater, the Richat Structure formed when a volcanic dome hardened and gradually eroded, exposing the onion - like layers of rock. Image taken from the space shuttle Atlantis in May 2000

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