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Images of 'Sediment' found, 143

astrid, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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Puddingstone
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The Basque Corniche - The Basque Corniche - The cliffs of the Basque Corniche, between Socoa and Hendaye, consist of an alternation of hard layers of limestone and soft layers of clay, depositing the sea at the bottom during the tertiary era. It was in the Quaternary (2 million years ago) that this rocky thousand leaves was straightened following tectonic movements, thus forming the cliffs we observe today. Cliffs of the Basque Corniche between Socoa and Hendaye, Pyrenees - Atlantiques, France
Mississippi River Delta, Louisiana, Usa, True Colour Satellite Image
Mississippi River Delta, Louisiana, USA in 1976 and 2001 (photo)
Ripple marks
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Landsat 8 scene, 2003
Sedimentary depots on Mars seen by Curiosity 02/2013 - Martian surface seen from the rover Curiosity 02/2013 - Sedimentary depots in the crater Gale sur Mars. Mosaic of images obtained by the rover Curiosity is his Mastcam camera on February 14, 2013. This mosaic of images from the Mast Camera (Mastcam) instrument on Nasa's Curiosity Mars rover shows a series of sedimentary deposits in the Glenelg area of Gale Crater, from a perspective in Yellowknife Bay looking toward west - northwest. Mastcam took the images for this mosaic during the 188th Martian day, or sol, of Curiosity's work on Mars (Feb. 14, 2013). The image has been white - balanced to show what the rocks would look like if ther were on Earth
A brittle star (Opheiolepis elegans)
Mars: Sedimentary layers in Becquerel crater - Mars: Periodic Layering in Becquerel Crater - Detail on sedimentary layers in Becquerel crater (Arabia Terra region), obtained on June 10, 2007 by the HIRISE camera on board the Mars Reconnaissance orbiter probe. This image in false colors shows sedimentary rocks in pink, sand in blue. The study of these sedimentary depot strata suggests that the climate of Mars is linked to the inclination of the axis of rotation of the planet. Rhythmic bedding in sedimentary bedrock within Becquerel crater on Mars is suggested by the patterns in this image from the High Resolution Imaging Science Experiment (HiRise) camera on Nasa's Mars Reconnaissance Orbiter. Three dimensional analysis based on stereo pairs of images confirmed the regularity of repetition in the thickness of the beds. In the top half of this image, some of the rhythm is apparent as a series of bundles of about 10 individual layers per bundle. By corresponding to a known 10 - to - one pattern in changes in the tilt of Mars' rotation axis, this pattern suggests the periodicity in the rock layers results from cyclical changes in the planet's tilt. Individual layers in the scence average 3.6 meters (12 feet) thick. The view is presented in enhanced color emphasizing the differing compositions of surface material. Sand trapped in relative low points in the terrain appears blue. Sedimentary rocks appear pink. This image was taken on June 10, 2007. The location of the imaged area is at 22 degrees north latitude, 352 degrees east longitude, within the Arabia Terra region
Proterozoic ocean floor
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norvegia, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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weddell, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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wilkins, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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Fossil Diagram (colour litho)
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porpoise, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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ross, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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The Basque Corniche - The Basque Corniche - The cliffs of the Basque Corniche, between Socoa and Hendaye, consist of an alternation of hard layers of limestone and soft layers of clay, depositing the sea at the bottom during the tertiary era. It was in the Quaternary (2 million years ago) that this rocky thousand leaves was straightened following tectonic movements, thus forming the cliffs we observe today. Cliffs of the Basque Corniche between Socoa and Hendaye, Pyrenees - Atlantiques, France
amundsen, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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vincennes, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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The Basque Corniche - The Basque Corniche - The cliffs of the Basque Corniche, between Socoa and Hendaye, consist of an alternation of hard layers of limestone and soft layers of clay, depositing the sea at the bottom during the tertiary era. It was in the Quaternary (2 million years ago) that this rocky thousand leaves was straightened following tectonic movements, thus forming the cliffs we observe today. Cliffs of the Basque Corniche between Socoa and Hendaye, Pyrenees - Atlantiques, France
Solidified Lava, San Salvador Island, Galapagos Islands (photo)
bellingshausen, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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prydz, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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balleny, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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wrigley, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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The Basque Corniche - The Basque Corniche - The cliffs of the Basque Corniche, between Socoa and Hendaye, consist of an alternation of hard layers of limestone and soft layers of clay, depositing the sea at the bottom during the tertiary era. It was in the Quaternary (2 million years ago) that this rocky thousand leaves was straightened following tectonic movements, thus forming the cliffs we observe today. Cliffs of the Basque Corniche between Socoa and Hendaye, Pyrenees - Atlantiques, France
Fossilisation process (colour litho)
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ninnus, 2007, (ice from the Western Antarctic Ice Sheet, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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leverett, 2007, (ice from the Western Antarctic Ice Sheet, sediment from Antarctica's Dry Valleys and mixed media on paper)
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New Mexico, Bisti Badlands Wilderness
Landscape near Hofn, Iceland
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Chile; Norte Grande region; Antofagasta; Atacama Desert; Valley of the Moon
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Fur formation, marine sediment made of diatoms and clay minerals, Palaeocene-Eocene, Fur Island, Denmark
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French advertisement for filter against sediment, may 1944
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Scene in Wealden Times, before 1935 (oil on canvas)
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Alaskan hydraulic gold mining used jets of water to erode rock material or move sediment. The resulting water-sediment was then directed through sluice boxes to remove the gold.c. 1900-1923
USA; California; Death Valley National Park; Badwater Basin depression; salt flats
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Desertscape, Namibia, Africa (photo)
USA; California; Death Valley National Park; Badwater Basin depression; salt flats
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China - Yellow River Delta in 1999 - China - Yellow River delta in 1999 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 1999. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat satellite shows the Yellow River Delta at the river mouth in 1999. In 1989, the river's main channel emptied into the Bohai Sea in a southeast - bending arc. In 1996, Chinese engineers blocked the main channel and forced the river to veer northeast. By 1999, erosion and settling along the old channel caused the tip of the delta to retreat, while a new peninsula had formed to the north
China - Yellow River Delta 2009 - China - Yellow River delta in 2009 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 2009. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat satellite shows the Yellow River Delta at the river mouth in 2009. In 1989, the river's main channel emptied into the Bohai Sea in a southeast - bending arc. In 1996, Chinese engineers blocked the main channel and forced the river to veer northeast. By 1999, erosion and settling along the old channel caused the tip of the delta to retreat, while a new peninsula had formed to the north
High angle view of a river; Landmannalaugar; Fjallabak Nature Reserve; Iceland
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Thick gooey sediment created by the spilling of burnt fuel and other toxic chemicals from the ships, felling of thousands of trees for land and vapours and fumes from burning materials made the coastal areas along the ship breaking yards at Sitakunda, Chittagong a highly polluted area. The industry started its operation in 1960 and flourished in a very short period of time due to lower labour costs and less stringent environmental regulations. Chittagong, Bangladesh. October 31, 2009.  (photo)
Belemnotheutis antiquus
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A GREENPEACE BIOLOGIST PRESENTS OILY SEDIMENT SAMPLES IN HAMBURG, 1997-08-20 (photo)
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China - Yellow River Delta 1989 - China - Yellow River delta in 1989 - The Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. Image obtained by the Landsat 5 satellite in 1989. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat 5 satellite shows the Yellow River Delta at the river mouth in 1989. In 1989, the river's main channel emptied into the Bohai Sea in a southeast - bending arc
Sea salt extraction in salt pans; Xwejni Bay; Gozo; Malta; Europe
Tufa formation, Mono Lake (photo)
Chalk
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Sting rays in the shallow waters of the Bora Bora lagoon, Moorea, French Polynesia, Society Islands, South Pacific, Cook's Bay, 2020 (photo)
Sandstone formations on the coast; sea salt extraction in salt pans; Xlendi; Gozo; Malta; Europe
Sting rays in the shallow waters of the Bora Bora lagoon, Moorea, French Polynesia, Society Islands, South Pacific, Cook's Bay, 2020 (photo)
Sting rays in the shallow waters of the Bora Bora lagoon, Moorea, French Polynesia, Society Islands, South Pacific, Cook's Bay, 2020 (photo)
Sting rays in the shallow waters of the Bora Bora lagoon, Moorea, French Polynesia, Society Islands, South Pacific, Cook's Bay, 2020 (photo)
Japan; Hokkaido; Akan National Park; Iozan Volcano; fumes over sulphur covered rocks
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Metal anchor covered with marine sediments, Roman civilization
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Xlendi Tower; coastal watchtower on a yellow sandstone cliff; sea salt extraction in salt pans; Xlendi; Gozo; Malta; Europe
Cornish rock (w/c on paper)
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Sting rays in the shallow waters of the Bora Bora lagoon, Moorea, French Polynesia, Society Islands, South Pacific. Cook's Bay, 2018 (photo)
Snorkeling excursion in the shallow waters of the Bora Bora lagoon, Moorea, French Polynesia, Society Islands, South Pacific. Cook's Bay, 2018 (photo)
Mississippi Delta, Louisiana, seen by satellite - Mississippi River Delta. Louisiana - Mississpi Delta, Louisiana, USA, seen by Landsat-7 satellite, November 27, 1999. The Mississippi River drains the heart of the North American continent, carrying vast quantities of sediment and depositing it along the shore of Louisiana and into the Gulf of Mexico. The sediment is composed of topsoil, sand, dead and decaying plants, and anything else washed away by a strong rainstorm far upstream. Many of these effluents are nutrients that act as fertilizer for the microscopic plants (phytoplankton) living near the surface of the Gulf waters. Each summer the phytoplankton population explodes. As the phytoplankton age, die, and decompose, bacteria absorb oxygen dissolved in the water, creating a dead zone”” along the shore at the ocean bottom. The oxygen - poor water is deadly to animals, from the microscopic zooplankton that graze on phytoplankton to crustaceans, molluscs, and fish. Once infrequent, the Gulf of Mexico dead zone is now an annual event, triggered by phosphorus and nitrogen in fertilizers used on farms throughout the central United States and as far away as Saskatchewan, Canada. In the fall, strong winds from seasonal storms stir the water, mixing the oxygen - poor deep water with oxygen - rich surface water, bringing a reprieve until the next spring. The true - color image above was acquired on November 27, 1999, by the Enhanced Thematic Mapper plus (ETM +) aboard Nasa's Landsat 7 satellite.
lauritzen, 2007, (sea ice from the Antarctica’s Ross Sea, sediment from Antarctica’s Dry Valleys and mixed media on paper)
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