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Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.
Wikipedia article traffic statistics – a tool for charting how many hits any given article gets, great for comparing different kinds of articles at different times, e.g., Genetics (in the school year) vs. (in the summer), or YouTube (with weekend spikes) and Simpsons (with spikes when new episodes come out). Students can also use it to see ...
Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction. [citation needed]
An example of the note method is Joseph Bird's 1861 Vocal Music Reader and Benjamin Jepson's three-book series using "note" methodology. The Elementary Music Reader was published in 1871 [1] by the Barnes Company, one year after Luther Mason's The National Music Course. Benjamin Jepson was a military man turned music teacher in New Haven after ...
Indo-Australian plate – Major tectonic plate formed by the fusion of the Indian and Australian plates (sometimes considered to be two separate tectonic plates) – 58,900,000 km 2 (22,700,000 sq mi) Australian plate – Major tectonic plate separated from Indo-Australian plate about 3 million years ago – 47,000,000 km 2 (18,000,000 sq mi)
The plate tectonics rock cycle is an evolutionary process. Magma generation, both in the spreading ridge environment and within the wedge above a subduction zone, favors the eruption of the more silicic and volatile rich fraction of the crustal or upper mantle material. [ 9 ]
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