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The Vine–Matthews–Morley hypothesis, also known as the Morley–Vine–Matthews hypothesis, was the first key scientific test of the seafloor spreading theory of continental drift and plate tectonics. Its key impact was that it allowed the rates of plate motions at mid-ocean ridges to be computed.
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The Vine–Matthews–Morley hypothesis is the first scientific test to confirm the seafloor spreading concept. Earth Sciences paradigm shift, from fix continents to plate tectonics (Wilson 1968): Magnetometer readings of sediment cores, geomagnetic reversals: ratio of cm (vertical).
Paleoclimate indicators derived from terrestrial sediments, on the other hand, are commonly influenced by local tectonic movements and paleogeographic variations. Factors governing the Earth's climate system include plate tectonics, which controls the configuration of continents, the interplay between the atmosphere and the ocean, and the Earth ...
Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') is the scientific theory that Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.
From the late 18th century until its replacement by plate tectonics in the 1960s, geosyncline theory was used to explain much mountain-building. [4] The understanding of specific landscape features in terms of the underlying tectonic processes is called tectonic geomorphology , and the study of geologically young or ongoing processes is called ...
Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis , volcanism , and erosion , while relevant climatic processes include atmospheric circulation , orographic lift , monsoon circulation and the rain shadow effect .
The Mesozoic structures underneath the North Sea can be seen as a failed rift system. [2] After initial crustal extension and the formation of rift basins during the Triassic and Jurassic periods, [1]: [70] the extension concentrated on the other side of the British Isles, which would create the northern Atlantic Ocean.