Depresyon (jeoloji): Revizyonlar arasındaki fark
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19. satır:
* [[graben]]<!--A [[graben]] is a down dropped and typically linear depression or basin created by [[rifting]] in a region under tensional tectonic forces.
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* [[
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* A [[pit crater]] is a depression formed by a sinking, or caving in, of the ground surface lying over a void.
43. satır:
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* [[vadi]]<!--A [[valley]] is a type of depression usually carved by erosion.-->
* [[:Kategori:Okyanus çukurları|okyanus çukurları]]<!--An [[oceanic trench]] is a deep depression with steep sides located in the ocean floor. Oceanic trenches are caused by the [[subduction]] (when one tectonic plate is pushed underneath another) of [[oceanic crust]] beneath either other oceanic crust or [[continental crust]].-->▼
▲* An [[oceanic trench]] is a deep depression with steep sides located in the ocean floor. Oceanic trenches are caused by the [[subduction]] (when one tectonic plate is pushed underneath another) of [[oceanic crust]] beneath either other oceanic crust or [[continental crust]].
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* A depression may result from the weight of overlying material such as an ice sheet during continental [[glaciation]] which is subsequently removed resulting in a basin which slowly [[Post-glacial rebound|rebounds]]. The area around the ice sheet, though not covered in ice itself, may also be pulled down by the weight of the ice sheet, which is known as peripheral depression.<ref name="MSUperipheraldepression">{{cite web
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