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Type # for projects,to access projects, > for users, and ? for help.

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Bilder zu 'Klippen' gefunden, 3,801

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Wall with Still Life, by unknown artist, 62-79, 1st Century A.D., ripped fresco, 298 x 447 cm

Wall with Still Life, by unknown artist, 62-79, 1st Century A.D., ripped fresco, 298 x 447 cm

MEB1191347

Wall with Still Life, by unknown artist, 62-79, 1st Century A.D., ripped fresco, 298 x 447 cm

Wall with Still Life, by unknown artist, 62-79, 1st Century A.D., ripped fresco, 298 x 447 cm

MEB1191308

Mih-Tutta-Hangkusch. A Mandan village

Mih-Tutta-Hangkusch. A Mandan village

Bodmer, Karl (1809-93)

NBY3673626

The 'Habitation' at Quebec was primarily a warehouse for the French traders of the Compagnie des Marchands. Built in 1608, the Habitation was an assemblage of buildings built on the river front below the cliffs of the upper city. The image key describes the various quarters: A. The Warehouse. B. Pigeon-loft. C. Detached Buildings where we keep our arms and for Lodging our Workmen. D. Detached Building for the Workmen. E. Sun-dial. F. Detached Building where the Smithy and Workmen are Lodged. G. Galleries all around the Lodgings. H. The Sieur de Champlain's Lodgings. I. The door of the Settlement with a Draw-bridge. L. Promenade around the Settlement ten feet in width to the edge of the Moat. M. Moat the whole way around the Settlement. O. The Sieur de Champlain's Garden. P. The Kitchen. Q. Space in front of the Settlement on the Shore of the River. R. The great River St. Lawrence

The 'Habitation' at Quebec was primarily a warehouse for the French traders of the Compagnie des Marchands. Built in 1608, the Habitation was an assemblage of buildings built on the river front below the cliffs of the upper city. The image key describes the various quarters: A. The Warehouse. B. Pigeon-loft. C. Detached Buildings where we keep our arms and for Lodging our Workmen. D. Detached Building for the Workmen. E. Sun-dial. F. Detached Building where the Smithy and Workmen are Lodged. G. Galleries all around the Lodgings. H. The Sieur de Champlain's Lodgings. I. The door of the Settlement with a Draw-bridge. L. Promenade around the Settlement ten feet in width to the edge of the Moat. M. Moat the whole way around the Settlement. O. The Sieur de Champlain's Garden. P. The Kitchen. Q. Space in front of the Settlement on the Shore of the River. R. The great River St. Lawrence

EVB7069138

Ireland seen by satellite Terra - Ireland satellite view - Image obtained on 4 January 2003. True - color Moderate Resolution Imaging Spectroradiometer (MODIS) image of Ireland taken from Terra satellite on January 4, 2003. The rugged cliffs that mark the island's west coast are showing their red - brown rocky surface, but the low - lying interior region is still wearing the island's signature green. The highest elevation in Ireland is Carrantuohill, located in the rugged terrain of the southwest tip. The bowl - like shape creates the network of lakes scattered across the island, and over time has produced peat bogs, which provide a source of fuel on the island, which is covered mostly by pasture and meadows. Ireland's largest city, Dublin, makes a purplish - gray patch peeking out from the clouds about halfway down the east coast. Belfast is more clearly visible on the coast in the northeast, due east of large Lake Neagh. One Ireland's few other large cities, Cork, is located at the m

Ireland seen by satellite Terra - Ireland satellite view - Image obtained on 4 January 2003. True - color Moderate Resolution Imaging Spectroradiometer (MODIS) image of Ireland taken from Terra satellite on January 4, 2003. The rugged cliffs that mark the island's west coast are showing their red - brown rocky surface, but the low - lying interior region is still wearing the island's signature green. The highest elevation in Ireland is Carrantuohill, located in the rugged terrain of the southwest tip. The bowl - like shape creates the network of lakes scattered across the island, and over time has produced peat bogs, which provide a source of fuel on the island, which is covered mostly by pasture and meadows. Ireland's largest city, Dublin, makes a purplish - gray patch peeking out from the clouds about halfway down the east coast. Belfast is more clearly visible on the coast in the northeast, due east of large Lake Neagh. One Ireland's few other large cities, Cork, is located at the m

PIX4666158

Hamlet and the Ghost, 1901 (oil on canvas)

Hamlet and the Ghost, 1901 (oil on canvas)

Shields, Frederic James (1833-1911)

MAN5642831

A little man with a great appetite sitting down to dinner, published by I. Hays, c.1806 (colour litho)

A little man with a great appetite sitting down to dinner, published by I. Hays, c.1806 (colour litho)

English School, (19th century)

BMC2975340

Debut de l'aviation : John Moisant effectue le premier transport de passagers au dessus de la Manche en emportant son mecanicien dans son avion Bleriot biplace le 17 aout 1910

Debut de l'aviation : John Moisant effectue le premier transport de passagers au dessus de la Manche en emportant son mecanicien dans son avion Bleriot biplace le 17 aout 1910

UIS5067260

Sheringham Beach

Sheringham Beach

Catton, Charles, II (1756-1819)

USB1163011

The wreck of the 'Halsewell', Indiaman, c.1786 (oil on canvas)

The wreck of the 'Halsewell', Indiaman, c.1786 (oil on canvas)

Stothard, Thomas (1755-1834)

MMM7340072

Burning British tank landing vessel and damaged tank, Dieppe, August 1942 (b/w photo)

Burning British tank landing vessel and damaged tank, Dieppe, August 1942 (b/w photo)

Unknown photographer, (20th century)

NAM5920401

Lord Hastings' flotilla on the river, with many pinnace budgerows, 1814-15 (w/c on paper)

Lord Hastings' flotilla on the river, with many pinnace budgerows, 1814-15 (w/c on paper)

Sita Ram (fl.c.1814-23)

BL5973730

Where the Anzacs dug themselves in on the shelterless slopes of barren hills exposed to enemy fire, 1915 (b/w photo)

Where the Anzacs dug themselves in on the shelterless slopes of barren hills exposed to enemy fire, 1915 (b/w photo)

Unknown photographer, (20th century)

NAM5923026

Trip From Dover To Ruen, France

Trip From Dover To Ruen, France

LTT7239369

Wounded being brought on board a destroyer off Dieppe, August 1942 (b/w photo)

Wounded being brought on board a destroyer off Dieppe, August 1942 (b/w photo)

Unknown photographer, (20th century)

NAM5928231

FROM THE RHINE TO GREECE BY TRAIN, 1966

FROM THE RHINE TO GREECE BY TRAIN, 1966

AYF7261465

Tethys, Saturn satellite, seen by the Cassini probe - Saturn's moon Tethys seen by Cassini spacecraft - The Tethys satellite photographed by the Cassini probe on August 30, 2007 at a distance of 97,000 km. Tethys is about 1070 km in diameter. At the top left of the picture is the gigantic impact crater Odysseus, which measures 450 km in diameter. The vast expanse of the crater Odysseus spreads out below Cassini in this mosaic view of Saturn's moon Tethys. The crater (450 kilometers or 280 miles across) is a remarkably well - preserved example of an ancient multi - ringed impact basin: the outer ring is defined by steep, cliff - like walls that descend to generally broad internal terraces. The inner ring is formed by a prominent, crown - shaped, 140 - kilometer (88 - mile) diameter circular band of icy mountains. Multi - ring basins are seen on rocky bodies as well as icy ones. The complex internal structure and multi - ringed nature of these very large basins are believed to arise from

Tethys, Saturn satellite, seen by the Cassini probe - Saturn's moon Tethys seen by Cassini spacecraft - The Tethys satellite photographed by the Cassini probe on August 30, 2007 at a distance of 97,000 km. Tethys is about 1070 km in diameter. At the top left of the picture is the gigantic impact crater Odysseus, which measures 450 km in diameter. The vast expanse of the crater Odysseus spreads out below Cassini in this mosaic view of Saturn's moon Tethys. The crater (450 kilometers or 280 miles across) is a remarkably well - preserved example of an ancient multi - ringed impact basin: the outer ring is defined by steep, cliff - like walls that descend to generally broad internal terraces. The inner ring is formed by a prominent, crown - shaped, 140 - kilometer (88 - mile) diameter circular band of icy mountains. Multi - ring basins are seen on rocky bodies as well as icy ones. The complex internal structure and multi - ringed nature of these very large basins are believed to arise from

PIX4625574

Mars: dunes and ice in Chasma Boreale - Mars: dunes and ice in Chasma Boreale - Chasma Boreale is a huge canyon located in the northern polar cap of Mars. This image, obtained by the Mars Express probe, shows Tenuis Cavus, the end of this canyon, where layers of water ice mix with Mars dust. At the bottom of the bowl there are numerous sand dunes. Chasma Boreale is a huge canyon in the northern polar cap. The images taken by Mars Express spacecraft show sharp detail of a series of scarps at the head of Chasma Boreale, a giant trough that almost divides the north polar ice cap in two. The trough is about 318 kilometers long and has cliffs that are almost two kilometers high. The images show layers of water ice and dust possibly for the first time in perspective view. Chasma Boreale is cut into the layered material that lies beneath the water ice of the polar cap. For decades, these layered materials were assumed to consist of a mixture of ice and dust. Recent observations could mean tha

Mars: dunes and ice in Chasma Boreale - Mars: dunes and ice in Chasma Boreale - Chasma Boreale is a huge canyon located in the northern polar cap of Mars. This image, obtained by the Mars Express probe, shows Tenuis Cavus, the end of this canyon, where layers of water ice mix with Mars dust. At the bottom of the bowl there are numerous sand dunes. Chasma Boreale is a huge canyon in the northern polar cap. The images taken by Mars Express spacecraft show sharp detail of a series of scarps at the head of Chasma Boreale, a giant trough that almost divides the north polar ice cap in two. The trough is about 318 kilometers long and has cliffs that are almost two kilometers high. The images show layers of water ice and dust possibly for the first time in perspective view. Chasma Boreale is cut into the layered material that lies beneath the water ice of the polar cap. For decades, these layered materials were assumed to consist of a mixture of ice and dust. Recent observations could mean tha

PIX4615964

Richat structure - Mauritania - satellite view - Richat structure, Mauritania, seen by satellite - Richat structure is a geological formation of volcanic origin in Mauritania. This “eye” measures 50 km in diameter. This image is a combination of an image obtained by the Landsat satellite in 1987 and a radar image obtained from the Space Shuttle (SRTM) in 2000. The relief is exaggerated by about 6 times. The picture covers an area of 68 km by 112 km. This prominent circular feature, known as the Richat Structure, in the Sahara desert of Mauritania is often noted by astronauts because it forms a conspicuous 50 - kilometer - wide (30 - mile - wide) bull's - eye on the otherwise rather featureless expanse of the desert. Initially mistaken for a possible impact crater, it is now known to be an eroded circular anticline (structural dome) of layered sedimentary rocks. Extensive sand dunes occur in this region and the interaction of bedrock topography, wind, and moving sand is evident in this

Richat structure - Mauritania - satellite view - Richat structure, Mauritania, seen by satellite - Richat structure is a geological formation of volcanic origin in Mauritania. This “eye” measures 50 km in diameter. This image is a combination of an image obtained by the Landsat satellite in 1987 and a radar image obtained from the Space Shuttle (SRTM) in 2000. The relief is exaggerated by about 6 times. The picture covers an area of 68 km by 112 km. This prominent circular feature, known as the Richat Structure, in the Sahara desert of Mauritania is often noted by astronauts because it forms a conspicuous 50 - kilometer - wide (30 - mile - wide) bull's - eye on the otherwise rather featureless expanse of the desert. Initially mistaken for a possible impact crater, it is now known to be an eroded circular anticline (structural dome) of layered sedimentary rocks. Extensive sand dunes occur in this region and the interaction of bedrock topography, wind, and moving sand is evident in this

PIX4659064

Woman Dancing in Traditional Costume next to the Ulu Watu Temple, Pura Luhur, Bali (photo)

Woman Dancing in Traditional Costume next to the Ulu Watu Temple, Pura Luhur, Bali (photo)

Sergi Reboredo

SRB1202582

The Escape of the Young Pretender (engraving) (b&w photo)

The Escape of the Young Pretender (engraving) (b&w photo)

English School, (19th century)

XJF107400

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