rift geology - Axtarish в Google
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics . Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side.
In geology, a rift is caused by tectonic plates in the Earth's lithosphere moving apart. Rifts are usually accompanied by orogeny (mountain building), volcanoes ...
Rifting is defined as the splitting apart of a single tectonic plate into two or more tectonic plates separated by divergent plate boundaries. The rifting of a ...
Modern models of rifting events are based on a wide diversity of information, from geophysical, to evidence of modern events, to evidence of ancient events.
4 янв. 2024 г. · A rift valley is a lowland region that forms where Earth's tectonic plates move apart, or rift. Rift valleys are found on land and at the bottom of the ocean.
A rift is a linear zone where the Earth's lithosphere is being pulled apart, leading to the formation of a divergent boundary between tectonic plates.
Продолжительность: 3:29
Опубликовано: 19 нояб. 2023 г.
11 февр. 2020 г. · The continental crust breaks along faults, forming long mountain ranges separated by rift valleys. diagram of continental rift showing earth's ...
16 окт. 2023 г. · In geology, a rift is caused by tectonic plates in the Earth's lithosphere moving apart. Rifts are usually accompanied by orogeny (mountain ...
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