8.4: Sedimentary Products of Rifting in the Basin and Range
8.4: Sedimentary Products of Rifting in the Basin and Range
Jun 30, 2023
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The style and rate of rifting varies along the East African Rift System. Rift zones form during extension of the lithosphere. In the south, rifting is in an early stage and advances to intermediate and mature rifting in the north. 🎥 http://ow.ly/HzfN50KRV0j | EarthScope Consortium
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The style and rate of rifting varies along the East African Rift System…
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SEDIMENTARY BASIN A sedimentary basin is a low area in the Earth’s crust, of tectonic origin, where sediments accumulate over a long period of time. These sediments are deposited by water, wind, or ice, and later become compacted and lithified into sedimentary rocks. FORMATION OF SEDIMENTARY BASINS Sedimentary basins form due to subsidence (sinking of the crust) caused by tectonic processes such as: ° Crustal stretching (rifting) ° Crustal loading (mountain building or volcanic loading) ° Therma
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