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Images of 'Drift' found, 601

Evening Snow at Kambara, No.16 from 'The 53 Stations of the Tokaido', pub. by Hoeido, 1833, (oban size, yoko-e - horizontal format, colour woodblock print)
Candide and his Valet, Cacambo, Drift in a Small Boat Towards the Land of Eldorado
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Smoke Drift, Autumn
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The Spanish Armada, 1588 (gouache on paper)
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midnight drift, 2017 (oil on canvas)
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Drift, 2009  (oil on canvas)
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Earth 200 million years ago - Artist's view - Early Jurassic Earth - Earth seen at the beginning of the Jurassic, about 200 million years ago. The western hemisphere is representative, the north is up. The Pangee has just split, forming Laurasia to the north and Gondwana to the south. This is how the western hemisphere of the Earth may have appeared 200 million years ago during the Early Jurassic period. North is at the top. During this period continental drift, driven by the massive forces of plate tectonics, had just begun to break the supercontinent of Pangea into Laurasia in the north and Gondwana in the south. In this image the nascent North American continent has just broken away from North Africa while South America and the rest of Africa remain joined as Gondwana. To the west in the global Panthalassa ocean are strips of land corresponding to the Wrangellia Terrane which later merged with western North America
The Drift Posts, 1923 (oil on canvas)
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Earth at the end of Permian - Ring arcs over the Permian Earth - A ring of rocks and dust is orbiting the Earth. The massive continent below is Pangee and the ocean to the west is Panthalassa. This is what Earth was supposed to look like at the end of Permian, about 260 million years ago, before the first dinosaurs appeared. This ring around the Earth was of earthly origin, constitutes debris thrown into orbit by collision with a meteorite or comet. Over time, these debris have either fallen or fallen back to Earth in a meteorite rain. A dusty ring arc orbits four thousand miles above Earth's equator. The massive continent below is Pangea and the ocean to the west is Panthalassa. This is how the Earth may have appeared during the end of the Permian period, a time just prior to the appearance of the dinosaurs, when continental drift was pulling Pangea apart into the seven continents we know today. 260 million years ago the Earth may have been host to ring arcs similar to the incomplete rings that currently circumscribe the planet Neptune. Unlike Neptune's rings, the ring arcs around the Earth were of terrestrial origin, debris thrown into orbit by a collision with a large meteorite or comet. The debris consisted of tiny pebbles that were once molten droplets of ejecta, long since cooled in the vacuum of space. The orbit of the ring arc would eventually decay, returning the debris back to Earth as a shower of meteorites. This debris is found on Earth's surface today in the form of dark, glassy objects known as tektites
Drift of Summer (oil on canvas)
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Sand Drift II
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drift ice ship (painting)
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A ring of rocks and dust is orbiting the Earth. The massive continent below is Pangee and the ocean to the west is Panthalassa. This is what Earth was supposed to look like at the end of Permian, about 260 million years ago, before the first dinosaurs appeared. This ring around the Earth was of earthly origin, constitutes debris thrown into orbit by collision with a meteorite or comet. Over time, these debris have fallen or fallen to Earth in a meteorite rain - A dusty ring arc orbits four thousand miles above Earth's equator. The massive continent below is Pangea and the ocean to the west is Panthalassa. This is how the Earth may have appeared during the end of the Permian period, a time just prior to the appearance of the dinosaurs, when continental drift was pulling Pangea apart into the seven continents we know today - 260 million years ago the Earth may have been host to ring arcs similar to the incomplete rings that currently circumscribe the planet Neptune . Unlike Neptune's rings, the ring arcs around the Earth were of terrestrial origin, debris thrown into orbit by a collision with a large meteorite or comet. The debris consisted of tiny pebbles that were once molten droplets of ejecta, long since cooled in the vacuum of space. The orbit of the ring arc would eventually decay, returning the debris back to Earth as a shower of meteorites. This debris is found on Earth's surface today in the form of dark, glassy objects known as tektites.: La Terre à la fin du Permien - Ring arcs over the Permian Earth
The Earth 650 million years ago - Artist's view - Snowball Earth - The Earth seen in a period of glaciation (Varanger glaciation), about 650 to 630 million years ago. This is how the Earth may have appeared about 650 million years ago during a period when snow and ice may have covered most, if not all, of the Earth's surface and oceans. This image suggests the Earth's appearance during the Marinoan glaciation from 650 to 630 million years ago. The southern and eastern hemispheres are dominated by glacier - covered land masses while the opposing hemisphere is frozen ocean save for a few areas of exposed liquid water, AKA refugia for the Earth's surviving soft - bodied multicellular organisms. In addition to the Marinoan glaciation there may have been at least two, and possibly three previous Proterozoic glacial periods going back to two billion years ago. The causes of these snowball periods are unknown but may have been due to massive volcanic eruptions, massive meteoritic impacts (both resulting in global sun - reflecting ash clouds), or variance's in the Earth's orbit
The Earth 600 million years ago - Artist's view - Ediacaran Earth - The Earth seen about 600 million years ago after an important period of glaciation. This is how the Earth may have appeared 600 million years ago following the Cryogenian “” Snowball Earth”” period. The worldwide glaciers have melted and the ocean is largely liquid again. During this, the Ediacaran period, it is hypothesized that all of the Earth's landmasses had merged into a single supercontinent known as Pannotia, also known as the Vendian supercontinent. Surrounding this massive landmass is the vast Panthalassic Ocean, also known as Panthalassa. While the ocean was home to a variety of evolving multicellular life forms including the ubiquitous Dickinsonia costata, it is not believed that life had moved to dry land with possible exception of bacteria and other microbial colonies
Slipping Sand, 1999 (oil on canvas)
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Frederick Delius' score for Sea- Drift
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drift ice ship, 2017 (painting)
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Western Inner Seaway - Artist's View - The Western Interior Seaway - The Western Interior Seaway (or North American Inner Sea) seen about 75 million years ago. This sea divided the North American continent into two continents, Laramidia in the west and Appalachia in the east. This is how the Western Interior Seaway may have appeared 75 million years ago from Earth orbit. This large inland sea once divided the North American continent into two landmasses, Laramidia to the west and Appalachia to the east. Branching toward the northeast is the Hudson Seaway and to the north on the horizon are the liquid polar waters of the Labrador Seaway. At less than one - fifth the size of present day North America, the island continent of Laramidia extended from present - day Mexico to Alaska and was home to tyrannosaurs, dromaeosaurids, troodontids, hadrosaurs, ceratopsians, pachycephalosaurs, and titanosaur sauropods. The dinosaurs of Appalachia are less - understood as much of the fossil evidence was destroyed by the glaciers that alternately descended from the north and retreated starting 2.5 million years ago
Atmospheres - Drift, 2018 (mixed media on paper)
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The Defence of Rorke's Drift, 1880 (oil on canvas)
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India 70 million years ago - Artist's view - Late Cretaceous India - India seen in the upper cretace about 70 million years ago. The north is upstairs. To the west, Madagascar separates from India. This is how the Indian subcontinent may have appeared 70 million years ago during the Late Cretaceous period. Looking north, immediately to India's west is the island continent of Madagascar and further west is the eastern coast of southern Africa. In the distant past India and Madagascar formed a single continent, however India was part of a separate tectonic plate that subsequently began to drift northward. This northward motion (covering about 8 inches per year making it among the fastest on the Earth's lithosphere) split India from Madagascar and carried it north across the Tethys Ocean until it collided with Eurasia about 50 to 35 million years ago. This collision between the Indian and Eurasian plates joined India to South Asia and created the Tibetan Plateau and the Himalaya Mountains, a process which is still evolving to this day
Drift stump, North Coast, 1939 (gelatin silver print)
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Rain or Snow, 1943 (oil & wax emulsion on canvas)
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Trees in the Snow, c.1865
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Continental drift diagrams
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A drift on an iceberg, 1933 (print)
Drift, 2014 (oil on canvas)
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Snow Drift, Clear Sky, 1974 (oil on canvas)
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Snow Drift, Clear Sky, 1974 (oil on canvas)
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Snow Drift, Clear Sky, 1974 (oil on canvas)
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Earth 90 million years ago - Artist's view - Late Cretaceous Earth - Earth seen in the upper cretace, about 90 million years ago. This is how the western hemisphere of the Earth may have appeared 90 million years ago during the Late Cretaceous period. During this period continental drift, driven by the massive forces of plate tectonics, had broken the supercontinent of Pangea into Laurasia in the north and Gondwana in the south. With a climate much warmer than today's there were no frozen polar caps and the resulting high ocean levels submerged a third of today's landmasses under warm shallow seas creating numerous waterways and “” island””” continents. In this image much of the incipient North American continent is divided by the Western Interior Seaway, the Isthmus of Panama is submerged by the Proto - Caribbean Sea, and the Pacific Ocean is making an incursion into South America
Snow Drift, Clear Sky,  1974 (oil on canvas)
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Drift, detail, 2020 (oil on linen mounted on board)
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Continental drift, volcanoes and oceanic ridge. Artwork by Mike Saunders
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Snow drift over winter sea ice, August 1980 (photo)
A derive airship in Rochefort, France 19/02/1922 (print)
Nansen's Fram expedition
African gold miners developing a drift, a tunnel following a vein of ore, in the Crown Mine, in the greatest gold bearing region of the world, near Johannesburg, South Afric. 1935
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Usuyuki, 1977-78 (encaustic & collage on canvas)
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Black hole collision in NGC 6240 - Black holes colliding in NGC 6240 - The galaxy NGC 6240, is located about 400 million light years away from Earth in the constellation Ophiuchus. This system consists of two colliding galaxies each with a central black hole; in several millions of years, they will form only one galaxy. A composite X-ray image (red, orange and yellow) and visible from the space telescopes Chandra and Hubble. This image of NGC 6240 contains X - ray data from Chandra (shown in red, orange, and yellow) that has been combined with an optical image from the Hubble Space Telescope. In 2002, the discovery of two merging black holes was announced based on Chandra data in this galaxy. The two black holes are a mere 3,000 light years apart and are seen as the bright point - like sources in the middle of the image. Scientists think these black holes are in such close proximity because they are in the midst of spiraling toward each other - a process that began about 30 million years ago. It is estimated that the two black holes will eventually drift together and merge into a larger black hole some tens or hundreds of millions of years from now. NGC 6240 is a peculiar, butterfly - or lobster - shaped galaxy consisting of two smaller merging galaxies. It lies in the constellation of Ophiuchus, the Serpent Holder, some 400 million light - years away
Car Buried In Snow (b/w photo)
Dunkleosteus and Cladoselache - Dunkleosteus and Cladoselache - A Dunkleosteus approaches a Cladoselache, the ancestor of sharks. Dunkleosteus, formerly called Dinichthys, is a large fossil placoderm. He lived in the Upper Devonian, between 415 and 360 million years. The largest representatives of the genus were approximately 8-10 m long and weighed around 5 tonnes. These fish were probably the greatest marine predators of their time. In a Devonian lagoon, the giant placoderm fish, Dunkleosteus, drifts towards the early shark, Cladoselache
Drift ice