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Images of 'Flows' found, 1,061

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Sailing on the Dalyan River 16

Sailing on the Dalyan River 16

SAP622293

Sailing on the Dalyan River 13

Sailing on the Dalyan River 13

SAP622294

The Turtle Beach 3

The Turtle Beach 3

SAP622036

Sailing on the Dalyan River 1

Sailing on the Dalyan River 1

SAP622048

The Cerro Aconcagua in Argentina is the highest mountain in the Americas, the highest in the Southern Hemisphere, and the highest peak outside of Asia. It is one of the Seven Summits. This member of the Andes Range is bounded by the Valle de las Vacas to the north and east and the Valle de los Horcones Inferior to the West and South. The mountain and its surroundings are part of the Aconcagua Provincial Park. The mountain has a number of glaciers, the most substantial of which are the north-eastern or Polish Glacier and the eastern or English Glacier. The Aconcagua River rises on the southern slope and flows west, meeting the Pacific Ocean 20 km north of Valparaso, Chile. Chile-Argentina. (photo)

The Cerro Aconcagua in Argentina is the highest mountain in the Americas, the highest in the Southern Hemisphere, and the highest peak outside of Asia. It is one of the Seven Summits. This member of the Andes Range is bounded by the Valle de las Vacas to the north and east and the Valle de los Horcones Inferior to the West and South. The mountain and its surroundings are part of the Aconcagua Provincial Park. The mountain has a number of glaciers, the most substantial of which are the north-eastern or Polish Glacier and the eastern or English Glacier. The Aconcagua River rises on the southern slope and flows west, meeting the Pacific Ocean 20 km north of Valparaso, Chile. Chile-Argentina. (photo)

UIG795278

The Cerro Aconcagua in Argentina is the highest mountain in the Americas, the highest in the Southern Hemisphere, and the highest peak outside of Asia. It is one of the Seven Summits. This member of the Andes Range is bounded by the Valle de las Vacas to the north and east and the Valle de los Horcones Inferior to the West and South. The mountain and its surroundings are part of the Aconcagua Provincial Park. The mountain has a number of glaciers, the most substantial of which are the north-eastern or Polish Glacier and the eastern or English Glacier. The Aconcagua River rises on the southern slope and flows west, meeting the Pacific Ocean 20 km north of Valparaso, Chile. Chile-Argentina. (photo)

The Cerro Aconcagua in Argentina is the highest mountain in the Americas, the highest in the Southern Hemisphere, and the highest peak outside of Asia. It is one of the Seven Summits. This member of the Andes Range is bounded by the Valle de las Vacas to the north and east and the Valle de los Horcones Inferior to the West and South. The mountain and its surroundings are part of the Aconcagua Provincial Park. The mountain has a number of glaciers, the most substantial of which are the north-eastern or Polish Glacier and the eastern or English Glacier. The Aconcagua River rises on the southern slope and flows west, meeting the Pacific Ocean 20 km north of Valparaso, Chile. Chile-Argentina. (photo)

UIG795279

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 ri

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 ri

PIX4659888

A deluge, c.1517-18, (chalk on paper)

A deluge, c.1517-18, (chalk on paper)

Vinci, Leonardo da (1452-1519)

ROC5617343

Aral Sea view from 1977 to 2006 - Aral sea 1977 to 2006 - The Aral Sea observed by Landsat satellites from 1977 to 2006. In 30 years, 60% of this lake has disappeared. Left, June 4, 1977, middle, September 17, 1989, right, May 27, 2006. The Aral Sea on June 4, 1977, Sept. 17, 1989, and May 27, 2006. The Aral Sea lies between Uzbekistan (to the south) and Kazakhstan (to the north). Once the fourth largest lake in the world, the Aral Sea is now less than half of its original size. The Aral Sea is a terminal, or endorheic, sea (meaning no water flows out of it). It is fed by the Syr Darya and the Amu Darya Rivers, but Soviet river diversions for irrigation made over 40 years ago have starved the Aral Sea of water. In 2001, the World Bank funded the construction of an 8 - mile dam to separate the North and South Aral, and thus save the smaller and less polluted North Aral Sea. The North Aral has been growing since completion of the Kok - Aral Dam in the summer of 2005. Repairs and updates

Aral Sea view from 1977 to 2006 - Aral sea 1977 to 2006 - The Aral Sea observed by Landsat satellites from 1977 to 2006. In 30 years, 60% of this lake has disappeared. Left, June 4, 1977, middle, September 17, 1989, right, May 27, 2006. The Aral Sea on June 4, 1977, Sept. 17, 1989, and May 27, 2006. The Aral Sea lies between Uzbekistan (to the south) and Kazakhstan (to the north). Once the fourth largest lake in the world, the Aral Sea is now less than half of its original size. The Aral Sea is a terminal, or endorheic, sea (meaning no water flows out of it). It is fed by the Syr Darya and the Amu Darya Rivers, but Soviet river diversions for irrigation made over 40 years ago have starved the Aral Sea of water. In 2001, the World Bank funded the construction of an 8 - mile dam to separate the North and South Aral, and thus save the smaller and less polluted North Aral Sea. The North Aral has been growing since completion of the Kok - Aral Dam in the summer of 2005. Repairs and updates

PIX4661026

China: Shanghai actress Hu Die, also known as 'Butterfly Hu' (1907-1989), Shanghai, 1946

China: Shanghai actress Hu Die, also known as 'Butterfly Hu' (1907-1989), Shanghai, 1946

PFH1774572

Comparison between Earth and Venus - Earth and Venus compared - Comparison at the scale of the sizes of Earth and Venus, seen here without their atmosphere. The size of the Venus planet is roughly the same as that of the Earth. This to-scale image suggests how the Earth and Venus might appear without their atmospheres. Venus' diameter is 86% that of the Earth's. It has 82% the mass. If you weigh 180 pounds on the Earth, you would weigh 163 pounds on Venus. Venus is about three-quarters the Earth's distance from the Sun. While Venus is roughly the same size and density as the Earth, it is otherwise a very different world. Earth's surface is a varied one, with liquid water covering three quarters of its surface. Those areas not under water have been highly modified by plate tectonics, weather, and life itself. Venus on the other hand is far too hot to host liquid water. Volcanoes, massive lava flows and the occasional impact crater characterize its surface. Latest observations suggest th

Comparison between Earth and Venus - Earth and Venus compared - Comparison at the scale of the sizes of Earth and Venus, seen here without their atmosphere. The size of the Venus planet is roughly the same as that of the Earth. This to-scale image suggests how the Earth and Venus might appear without their atmospheres. Venus' diameter is 86% that of the Earth's. It has 82% the mass. If you weigh 180 pounds on the Earth, you would weigh 163 pounds on Venus. Venus is about three-quarters the Earth's distance from the Sun. While Venus is roughly the same size and density as the Earth, it is otherwise a very different world. Earth's surface is a varied one, with liquid water covering three quarters of its surface. Those areas not under water have been highly modified by plate tectonics, weather, and life itself. Venus on the other hand is far too hot to host liquid water. Volcanoes, massive lava flows and the occasional impact crater characterize its surface. Latest observations suggest th

Walter B Myers

PIX4629857

Lusi mud volcano on Java Island - Lusi mud flow seen from space - The Lusi mud volcano (Sidoarjo) erupted in May 2006 and its flows continue to expand. Comparison of two satellite photos taken on August 24, 2004, on the left, and on November 11, 2008, on the right. On these false-coloured images obtained by the Terra satellite, the vegetation appears in red, the mud of the volcano in grey. On May 29, 2006, a mud volcano began erupting in a densely populated area in eastern Java, Indonesia. In the months that followed, the Sidoarjo mud flow (also known as the Lapindo mud flow, or Lusi) showed no signs of slowing, and mitigation efforts such as dropping chains of concrete balls down the crater proved ineffective. By June 2008, the massive mud lake spawned by this eruption had smothered a dozen villages and displaced some 30,000 residents. The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on Nasa's Terra satellite acquired these images on November 11, 2008, (right

Lusi mud volcano on Java Island - Lusi mud flow seen from space - The Lusi mud volcano (Sidoarjo) erupted in May 2006 and its flows continue to expand. Comparison of two satellite photos taken on August 24, 2004, on the left, and on November 11, 2008, on the right. On these false-coloured images obtained by the Terra satellite, the vegetation appears in red, the mud of the volcano in grey. On May 29, 2006, a mud volcano began erupting in a densely populated area in eastern Java, Indonesia. In the months that followed, the Sidoarjo mud flow (also known as the Lapindo mud flow, or Lusi) showed no signs of slowing, and mitigation efforts such as dropping chains of concrete balls down the crater proved ineffective. By June 2008, the massive mud lake spawned by this eruption had smothered a dozen villages and displaced some 30,000 residents. The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on Nasa's Terra satellite acquired these images on November 11, 2008, (right

PIX4660901

Martian dunes in Spring - March: Spring view of Dunes - Detail on sand dunes near the north pole of Mars. These dunes are covered with carbon dioxide gel during the Martian winter. In spring, dark streaks appear, sand flows caused by the degel. Image obtained by the HIRISE camera of the Mars Reconnaissance probe orbiter on April 7, 2008. HIRISE is a 50 cm telescope that observes visible and near infrared. Falling Material Kicks Up Cloud of Dust on Dunes. There is a vast region of sand dunes at high northern latitudes on Mars. In the winter, a layer of carbon dioxide ice covers the dunes, and in the spring as the sun warms the ice it evaporates. This is a very active process, and sand dislodged from the crests of the dunes cascades down, forming dark streaks. In thid image falling material has kicked up a small cloud of dust. The color of the ice surrounding adjacent streaks of material suggests that dust has settled on the ice at the bottom after similar events. Also discernible in thi

Martian dunes in Spring - March: Spring view of Dunes - Detail on sand dunes near the north pole of Mars. These dunes are covered with carbon dioxide gel during the Martian winter. In spring, dark streaks appear, sand flows caused by the degel. Image obtained by the HIRISE camera of the Mars Reconnaissance probe orbiter on April 7, 2008. HIRISE is a 50 cm telescope that observes visible and near infrared. Falling Material Kicks Up Cloud of Dust on Dunes. There is a vast region of sand dunes at high northern latitudes on Mars. In the winter, a layer of carbon dioxide ice covers the dunes, and in the spring as the sun warms the ice it evaporates. This is a very active process, and sand dislodged from the crests of the dunes cascades down, forming dark streaks. In thid image falling material has kicked up a small cloud of dust. The color of the ice surrounding adjacent streaks of material suggests that dust has settled on the ice at the bottom after similar events. Also discernible in thi

PIX4616482

A sunset. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arunchal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

A sunset. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arunchal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG798770

Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG798771

The Vesuve seen at Radar - 15/04/1994 Mt. Vesuvius, one of the best known volcanoes in the world primarily for the eruption that buried the Roman city of Pompeii, is shown in the center of this radar image. The central cone of Vesuvius is the dark purple feature in the center of the volcano. This cone is surrounded on the northern and eastern sides by the old crater rim, called Mt. Somma. Recent lava flows are the pale yellow areas on the southern and western sides of the cone. Vesuvius is part of a large volcanic zone which includes the Phalagrean Fields, the cluster of craters seen along the left side of the image. The Bay of Naples, on the left side of the image, is separated from the Gulf of Salerno, in the lower left, by the Sorrento Peninsula. Dense urban settlement can be seen around the volcano. The city of Naples is above and to the left of Vesuvius; the seaport of the city can be seen in the top of the bay. Pompeii is located just below the volcano on this image. The rapid er

The Vesuve seen at Radar - 15/04/1994 Mt. Vesuvius, one of the best known volcanoes in the world primarily for the eruption that buried the Roman city of Pompeii, is shown in the center of this radar image. The central cone of Vesuvius is the dark purple feature in the center of the volcano. This cone is surrounded on the northern and eastern sides by the old crater rim, called Mt. Somma. Recent lava flows are the pale yellow areas on the southern and western sides of the cone. Vesuvius is part of a large volcanic zone which includes the Phalagrean Fields, the cluster of craters seen along the left side of the image. The Bay of Naples, on the left side of the image, is separated from the Gulf of Salerno, in the lower left, by the Sorrento Peninsula. Dense urban settlement can be seen around the volcano. The city of Naples is above and to the left of Vesuvius; the seaport of the city can be seen in the top of the bay. Pompeii is located just below the volcano on this image. The rapid er

PIX4666416

Vietnam: A Chinese merchant family in Cholon, Saigon, 1872

Vietnam: A Chinese merchant family in Cholon, Saigon, 1872

PFH1773706

Inside a Kopeka Bird Cave, Atiu Island, Cook Island, Polynesia, South Pacific Ocean (photo)

Inside a Kopeka Bird Cave, Atiu Island, Cook Island, Polynesia, South Pacific Ocean (photo)

Sergi Reboredo

SRB1202898

Vietnam: Chinese style gate ( paifang ), Cholon, Saigon (early 20th century)

Vietnam: Chinese style gate ( paifang ), Cholon, Saigon (early 20th century)

Unknown photographer, (20th century)

PFH2561742

Vietnam: Street market in Cholon, Saigon (early 20th century)

Vietnam: Street market in Cholon, Saigon (early 20th century)

Unknown photographer, (20th century)

PFH2561743

Vietnam: Rich Chinese couple in Cholon, Saigon, 1872

Vietnam: Rich Chinese couple in Cholon, Saigon, 1872

PFH1773707

Vietnam: Chinese temple, Cholon, 1827

Vietnam: Chinese temple, Cholon, 1827

PFH1774558

Ganges, Gangotri, India (photo)

Ganges, Gangotri, India (photo)

Sergi Reboredo

SRB3036600

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.

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.

PIX4659907

Fishing boats, on the Brahmaputra river, in Gauhati, Assam, Northeast India. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers fall into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

Fishing boats, on the Brahmaputra river, in Gauhati, Assam, Northeast India. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers fall into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG799741

Spree River from atop the Berlin Cathedral or Berliner Dom, Berlin, Germany2018 (photo)

Spree River from atop the Berlin Cathedral or Berliner Dom, Berlin, Germany2018 (photo)

Sergi Reboredo

SRB5058766

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 developmen

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 developmen

PIX4659895

Ganges, Rishikesh, India (photo)

Ganges, Rishikesh, India (photo)

Sergi Reboredo

SRB3036543

March: Promethei Planum - Mars: Promethei Planum - Promethei Planum is a region located near the southern pole of Mars. This region is seasonally covered with a thick layer of ice up to 3500 metres thick. On this image obtained by the Mars Express probe on September 22, 2005, an impact crater about 100 km wide and 800 metres deep is visible to the right (north). It is partially covered with ice. In the center of the image, structures formed by lava flows; on the left of the image, ice, which is an extension of the southern polar cap. Promethei Planum, an area seasonally covered with layer of ice more than 3500 m thick layer of ice in the martian south polar region, was the subject of the High Resolution Stereo Camera's focus on 22 September 2005 as Mars Express was in orbit above the Red Planet. Promethei Planum lies at approximately 76* south and 105* east. An approximately 100 km - large and 800 m - deep impact crater is visible in the northern part of the image. The crater's interio

March: Promethei Planum - Mars: Promethei Planum - Promethei Planum is a region located near the southern pole of Mars. This region is seasonally covered with a thick layer of ice up to 3500 metres thick. On this image obtained by the Mars Express probe on September 22, 2005, an impact crater about 100 km wide and 800 metres deep is visible to the right (north). It is partially covered with ice. In the center of the image, structures formed by lava flows; on the left of the image, ice, which is an extension of the southern polar cap. Promethei Planum, an area seasonally covered with layer of ice more than 3500 m thick layer of ice in the martian south polar region, was the subject of the High Resolution Stereo Camera's focus on 22 September 2005 as Mars Express was in orbit above the Red Planet. Promethei Planum lies at approximately 76* south and 105* east. An approximately 100 km - large and 800 m - deep impact crater is visible in the northern part of the image. The crater's interio

PIX4616118

March: Promethei Planum - Mars: Promethei Planum - Promethei Planum is a region located near the southern pole of Mars. This region is seasonally covered with a thick layer of ice up to 3500 metres thick. On this perspective image obtained by the Mars Express probe on September 22, 2005, an impact crater about 100 km wide and 800 metres deep is visible at the bottom of the image. It is partially covered with ice. On top, structures formed by lava flows; at the top of the picture, ice, which is an extension of the southern polar cap. Promethei Planum, an area seasonally covered with layer of ice more than 3500 m thick layer of ice in the martian south polar region, was the subject of the High Resolution Stereo Camera's focus on 22 September 2005 as Mars Express was in orbit above the Red Planet. Promethei Planum lies at approximately 76* south and 105* east. An approximately 100 km - large and 800 m - deep impact crater is visible in the bottom of the image. The crater's interior is par

March: Promethei Planum - Mars: Promethei Planum - Promethei Planum is a region located near the southern pole of Mars. This region is seasonally covered with a thick layer of ice up to 3500 metres thick. On this perspective image obtained by the Mars Express probe on September 22, 2005, an impact crater about 100 km wide and 800 metres deep is visible at the bottom of the image. It is partially covered with ice. On top, structures formed by lava flows; at the top of the picture, ice, which is an extension of the southern polar cap. Promethei Planum, an area seasonally covered with layer of ice more than 3500 m thick layer of ice in the martian south polar region, was the subject of the High Resolution Stereo Camera's focus on 22 September 2005 as Mars Express was in orbit above the Red Planet. Promethei Planum lies at approximately 76* south and 105* east. An approximately 100 km - large and 800 m - deep impact crater is visible in the bottom of the image. The crater's interior is par

PIX4616138

Florida seen by Envisat - Florida seen from space - This image taken by Envisat shows Florida Detroit through which the Loop Current “” flows eastward out of the Gulf of Mexico before joining the “Gulf Stream” which passes off the western coast of the United States and Newfoundland (not visible here). Scientists are monitoring this near area because they are concerned about the possibility that the winds may push the Black Marea of the Gulf of Mexico (visible west of Florida) south into the Loop Current “or that the current may extend northward to reach the oil slick. If oil from this slick were to penetrate into the Loop Current, it could be drained towards the Florida Keys archipelago (this set of circular islands associated with coral reefs off the tip of Florida) and further east to the Gulf Stream. By combining sea surface state and current circulation information with Envisat Advanced Synthetic Aperture Radar (ASAR) data on black maree, analysts are able to determine in which dir

Florida seen by Envisat - Florida seen from space - This image taken by Envisat shows Florida Detroit through which the Loop Current “” flows eastward out of the Gulf of Mexico before joining the “Gulf Stream” which passes off the western coast of the United States and Newfoundland (not visible here). Scientists are monitoring this near area because they are concerned about the possibility that the winds may push the Black Marea of the Gulf of Mexico (visible west of Florida) south into the Loop Current “or that the current may extend northward to reach the oil slick. If oil from this slick were to penetrate into the Loop Current, it could be drained towards the Florida Keys archipelago (this set of circular islands associated with coral reefs off the tip of Florida) and further east to the Gulf Stream. By combining sea surface state and current circulation information with Envisat Advanced Synthetic Aperture Radar (ASAR) data on black maree, analysts are able to determine in which dir

PIX4673019

The Omega nebula (M17) seen in infrared - M17 nebula in infrared - The Omega nebula (M17) seen in infrared by the Spitzer space telescope. M17 is a star-forming region about 6000 light years ago in the constellation Sagittarius. In the center of the nebula is a group of massive stars. The dust appears in red, the hot gas in green, the regions or this gas and the dust mixes in white. Nasa's Spitzer Space Telescope has captured an infrared view of the star - making cloud called M17, or the Swan nebula. The cloud, located about 6,000 light - years away in the constellation Sagittarius, is dominated by a central group of massive stars - - the most massive stars in the region. These central stars give off intense flows of expanding gas, which rush like rivers against dense piles of material, carving out the deep pocket at center of the picture. Winds from the region's other massive stars push back against these oncoming rivers, creating bow shocks like those that pile up in front of speedin

The Omega nebula (M17) seen in infrared - M17 nebula in infrared - The Omega nebula (M17) seen in infrared by the Spitzer space telescope. M17 is a star-forming region about 6000 light years ago in the constellation Sagittarius. In the center of the nebula is a group of massive stars. The dust appears in red, the hot gas in green, the regions or this gas and the dust mixes in white. Nasa's Spitzer Space Telescope has captured an infrared view of the star - making cloud called M17, or the Swan nebula. The cloud, located about 6,000 light - years away in the constellation Sagittarius, is dominated by a central group of massive stars - - the most massive stars in the region. These central stars give off intense flows of expanding gas, which rush like rivers against dense piles of material, carving out the deep pocket at center of the picture. Winds from the region's other massive stars push back against these oncoming rivers, creating bow shocks like those that pile up in front of speedin

PIX4620190

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

French School, (12th century)

PHL434225

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

French School, (12th century)

PHL434223

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

French School, (12th century)

PHL434226

Auckland Region (New Zealand) satellite view - Auckland, New Zealand - Auckland Region, the largest urban area in New Zealand, in the North Island, viewed by Landsat satellite - 7 August 27, 2002. Auckland, New Zealand's largest city, is located on the country's North Island. Nearly a third of New Zealand's population lives in Auckland - - more than three million people. This natural - color (photo - like) image of Auckland was acquired on August 27, 2002, by Nasa's Landsat 7 satellite. The most densely developed areas appear white and gray, while suburban areas appear grayish green - - a mixture of houses, streets, and lawns. The city spreads out across various peninsulas surrounding Tamaki Strait and other bays and inlets. The city has been built up around the Auckland Volcanic Field; within a 20 - kilometer (12.4 - mile) radius of the heart of the city, there are 49 volcanoes, most of them small cones less than 150 meters (492 feet) high. Many of them have been protected as parks or

Auckland Region (New Zealand) satellite view - Auckland, New Zealand - Auckland Region, the largest urban area in New Zealand, in the North Island, viewed by Landsat satellite - 7 August 27, 2002. Auckland, New Zealand's largest city, is located on the country's North Island. Nearly a third of New Zealand's population lives in Auckland - - more than three million people. This natural - color (photo - like) image of Auckland was acquired on August 27, 2002, by Nasa's Landsat 7 satellite. The most densely developed areas appear white and gray, while suburban areas appear grayish green - - a mixture of houses, streets, and lawns. The city spreads out across various peninsulas surrounding Tamaki Strait and other bays and inlets. The city has been built up around the Auckland Volcanic Field; within a 20 - kilometer (12.4 - mile) radius of the heart of the city, there are 49 volcanoes, most of them small cones less than 150 meters (492 feet) high. Many of them have been protected as parks or

PIX4675653

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

Fountain from the Monastery of Saint-Michel-de-Cuxa, Roussillon, France, 1125-50 (marble)

French School, (12th century)

PHL434224

Add 15296 (1) f.111r, Meanwhile, all is peaceful with the exiles in their abode on the Citrakuta mountain. Rama points out its beauties Sita - the many varieties of lovely trees and birds, the rocks coloured by gems and minerals, and the Mandakina river which rises in the mountain and flows along the bottom of the picture, with hermits praying, meditating and bathing along it. Rama decorates Sita's forehead with red arsenic and takes her protectively in his arms when a lion growls. They return to the hut, where Laksmana has killed deer and prepared food, which the two brothers eat while Sita keeps the flies away. After they have eaten, an audacious crow annoys Sita. Rama, enraged, takes aim at it with an arrow made of a reed. The crow is refused protection by all in the three worlds (heaven being represented by a pair of divine beings in a heavenly chariot, and the underworld by a snake-king and his queen). It returns to beg for mercy from Rama, who allows his arrow to pierce just the

Add 15296 (1) f.111r, Meanwhile, all is peaceful with the exiles in their abode on the Citrakuta mountain. Rama points out its beauties Sita - the many varieties of lovely trees and birds, the rocks coloured by gems and minerals, and the Mandakina river which rises in the mountain and flows along the bottom of the picture, with hermits praying, meditating and bathing along it. Rama decorates Sita's forehead with red arsenic and takes her protectively in his arms when a lion growls. They return to the hut, where Laksmana has killed deer and prepared food, which the two brothers eat while Sita keeps the flies away. After they have eaten, an audacious crow annoys Sita. Rama, enraged, takes aim at it with an arrow made of a reed. The crow is refused protection by all in the three worlds (heaven being represented by a pair of divine beings in a heavenly chariot, and the underworld by a snake-king and his queen). It returns to beg for mercy from Rama, who allows his arrow to pierce just the

Indian School, (17th century)

BL3283029

Tempete sur Saturn seen by the Cassini probe - Huge Storm on Saturn seen by Cassini spacecraft - Evolution of a huge tempete on Saturn seen by the Cassini probe from December 5, 2010 to August 12, 2011. This series of images from Nasa's Cassini spacecraft shows the development of the largest storm seen on the planet since 1990. These true - color and composite near - true - color views chronicle the storm from its start in late 2010 through mid - 2011, showing how the distinct head of the storm quickly grew large but eventually became engulfed by the storm's tail. The earliest image of the storm, taken Dec. 5, 2010, is in the top left of the panel. The storm appears only as a small, white cloud on the terminator between the day side and night side of the planet. The next view, in the top middle of the panel and taken Jan. 2, 2011, shows that the head quickly grew much larger and a tail began to trail a great distance eastward. Some of the clouds moved south and got caught up in a curre

Tempete sur Saturn seen by the Cassini probe - Huge Storm on Saturn seen by Cassini spacecraft - Evolution of a huge tempete on Saturn seen by the Cassini probe from December 5, 2010 to August 12, 2011. This series of images from Nasa's Cassini spacecraft shows the development of the largest storm seen on the planet since 1990. These true - color and composite near - true - color views chronicle the storm from its start in late 2010 through mid - 2011, showing how the distinct head of the storm quickly grew large but eventually became engulfed by the storm's tail. The earliest image of the storm, taken Dec. 5, 2010, is in the top left of the panel. The storm appears only as a small, white cloud on the terminator between the day side and night side of the planet. The next view, in the top middle of the panel and taken Jan. 2, 2011, shows that the head quickly grew much larger and a tail began to trail a great distance eastward. Some of the clouds moved south and got caught up in a curre

PIX4625230

GRANT FLOWER OF ZIMBABWE BOWLS IN NAGPUR, 2000-11-26 (photo)

GRANT FLOWER OF ZIMBABWE BOWLS IN NAGPUR, 2000-11-26 (photo)

Reuters Photographer

REU7845553

Frontispieces and illustrations from 'Dewdrops from Fairyland' by Lucy M. Scott, published 1912, 'The Secrets of Flowers' by E.M. Coker, 'The Book of the Flower Fairies' by C.M. Barker, published 1930, and 'The Pleasure Garden', published 1904

Frontispieces and illustrations from 'Dewdrops from Fairyland' by Lucy M. Scott, published 1912, 'The Secrets of Flowers' by E.M. Coker, 'The Book of the Flower Fairies' by C.M. Barker, published 1930, and 'The Pleasure Garden', published 1904

FAM203980

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