czwartek, 19 października 2017
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Ziemia/Zjawiska natury (591)

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! EN_90257495_0001 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY False-colour, three-dimensional map of part of the East Pacific Rise, showing the Clipperton transform fault. The East Pacific Rise (EPR) is a mid ocean ridge lying to the west of Central America. It marks the boundary between the Pacific and Cocos tectonic plates and is a constructive plate boundary or spreading centre where basalt magmas rise to the surface, forming new igneous rock and pushing the older crust away on either side. The Clipperton transform fault offsets the EPR by 85km, separating two ridge segments with contrasting properties; the northern segment is relatively cool & starved of magma, whereas the southern segment is robust & swollen with magma. For more information see Nature, Vol 335, p217-
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! EN_90257597_0001 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY False-colour, three-dimensional map of part of the East Pacific Rise, showing a discontinuity called an overlapping spreading centre (OSC). The East Pacific Rise (EPR) is a mid ocean ridge lying to the west of Central America. It marks the boundary between the Pacific and Cocos tectonic plates and is a constructive plate boundary or spreading centre where basalt magmas rise to the surface, forming new igneous rock and pushing the older crust away on either side. The OSC comprises two ridge segments, offset by 8km and overlapping by 25km, separated by a 600 metre deep overlap basin. Abandoned ridges and fossil overlap basins surround the OSC. The area shown is 140 x 130 km. For more information see Nature, Vol 335, p217-
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! EN_90257644_0001 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY False-colour, three-dimensional map of part of the East Pacific Rise, showing a discontinuity called an overlapping spreading centre (OSC). The East Pacific Rise (EPR) is a mid ocean ridge lying to the west of Central America. It marks the boundary between the Pacific and Cocos tectonic plates and is a constructive plate boundary or spreading centre where basalt magmas rise to the surface, forming new igneous rock and pushing the older crust away on either side. The OSC comprises two ridge segments, offset by 8km and overlapping by 25km, separated by a 600 metre deep overlap basin. Abandoned ridges and fossil overlap basins surround the OSC. The area shown is 140 x 130 km. For more information see Nature, Vol 335, p217-
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! EN_90256240_0001 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Map of the whole earth on a blue grid.
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! EN_90256187_0140 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Abstract computer graphics composite illustration of a projection map of Earth, enveloped in a multi-coloured grid and set against a background of space which is dominated by two bright orange stars.
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! EN_90269121_0001 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Mosaic image of global weather systems produced by the experimental Tiros 9 satellite on February 13th, 1965. This was the first complete view of Earth's weather systems.
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! EN_90253135_0003 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Computer graphic representation of continental drift, showing the continents as they are today. Spherical projection.
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! EN_90253139_0001 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Computer graphic representation of continental drift, showing the continents as they were 200 million years ago. Spherical projection.
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! EN_90253139_0002 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Computer graphic representation of continental drift, showing the continents as they were 150 million years ago. Spherical projection.
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! EN_90253139_0003 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Computer graphic representation of continental drift, showing the continents as they were 100 million years ago. Spherical projection.
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! EN_90253139_0004 SCI
PHOTO: EAST NEWS/SCIENCE PHOTO LIBRARY Computer graphic representation of continental drift, showing the continents as they were 50 million years ago. Spherical projection.
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