Interactive Continental Maps
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Interactive Continental Maps
Continental plates and the breakup of Pangea (credit: Wikicommons) The Earth's crust consists of multiple, rocky sections (plates) that move up, over, and under each other while being carried on portions of the Earth's interior mantle. Imperceptible over human time scales but dramatic over eons Continental Drift is one of the most fundamental ...
Aug 5, 2022
Continental Crust Formation
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
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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Continental Drift: founding block of the Plate Tectonics Theory – Geology 101 for Lehman College (CUNY)
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