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* A basin may be any large sediment filled depression. In [[tectonics]], it may refer specifically to a circular, [[syncline]]-like depression: a [[Basin (geology)|geologic basin]]; while in [[sedimentology]], it may refer to an area thickly filled with sediment: [[sedimentary basin]].<ref name="GTb">{{Web kaynağı| url = http://www.geotech.org/survey/geotech/dictiona.html#sectB | başlık = Dictionary of Geologic Terms - B | erişimtarihi = 2006-08-25 | yayımcı = geotech.org }}</ref>
* A basin may be any large sediment filled depression. In [[tectonics]], it may refer specifically to a circular, [[syncline]]-like depression: a [[Basin (geology)|geologic basin]]; while in [[sedimentology]], it may refer to an area thickly filled with sediment: [[sedimentary basin]].<ref name="GTb">{{Web kaynağı | url = http://www.geotech.org/survey/geotech/dictiona.html#sectB | başlık = Dictionary of Geologic Terms - B | erişimtarihi = 2006-08-25 | yayımcı = geotech.org | arşivurl = http://web.archive.org/web/20121116065716/http://www.geotech.org:80/survey/geotech/dictiona.html | arşivtarihi = 16 Kasım 2012}}</ref>
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* A [[Kettle (geology)|kettle]] is left behind when a piece of ice left behind in [[Glacier|glacial]] deposits melts.<ref name="GTk">{{Web kaynağı| url = http://www.geotech.org/survey/geotech/dictiona.html#sectK | başlık = Dictionary of Geologic Terms - K | erişimtarihi = 2006-08-26 | yayımcı = geotech.org }}</ref>
* A [[Kettle (geology)|kettle]] is left behind when a piece of ice left behind in [[Glacier|glacial]] deposits melts.<ref name="GTk">{{Web kaynağı | url = http://www.geotech.org/survey/geotech/dictiona.html#sectK | başlık = Dictionary of Geologic Terms - K | erişimtarihi = 2006-08-26 | yayımcı = geotech.org | arşivurl = http://web.archive.org/web/20121116065716/http://www.geotech.org:80/survey/geotech/dictiona.html | arşivtarihi = 16 Kasım 2012}}</ref>
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* A depression may be an area of [[subsidence]] caused by the collapse of an underlying structure. Examples include [[sinkhole]]s above caves in [[karst topography]], or [[caldera]]s.<ref name="GTc">{{Web kaynağı| url = http://www.geotech.org/survey/geotech/dictiona.html#sectC | başlık = Dictionary of Geologic Terms - C | erişimtarihi = 2006-08-25 | yayımcı = geotech.org }}</ref> or [[maar]]s in volcanic areas.
* A depression may be an area of [[subsidence]] caused by the collapse of an underlying structure. Examples include [[sinkhole]]s above caves in [[karst topography]], or [[caldera]]s.<ref name="GTc">{{Web kaynağı | url = http://www.geotech.org/survey/geotech/dictiona.html#sectC | başlık = Dictionary of Geologic Terms - C | erişimtarihi = 2006-08-25 | yayımcı = geotech.org | arşivurl = http://web.archive.org/web/20121116065716/http://www.geotech.org:80/survey/geotech/dictiona.html | arşivtarihi = 16 Kasım 2012}}</ref> or [[maar]]s in volcanic areas.
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* [[:Kategori:Okyanus çukurları|okyanus çukuru]]<!--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]].-->
* [[:Kategori:Okyanus çukurları|okyanus çukuru]]<!--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">{{Web kaynağı| url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm#peripheral | başlık = Glossary of Important Terms in Glacial Geology - Peripheral Depression | erişimtarihi = 2006-08-25 | yayımcı = Montana State University | yıl = 1999 }} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).</ref> Further from the ice, a forebulge may form, which is curved slightly upward.<ref name="MSUforebulge">{{Web kaynağı| url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm#forebulge | başlık = Glossary of Important Terms in Glacial Geology - Forebulge | erişimtarihi = 2006-08-25 | yayımcı = Montana State University | yıl = 1999 }} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).</ref>
* 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">{{Web kaynağı | url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm#peripheral | başlık = Glossary of Important Terms in Glacial Geology - Peripheral Depression | erişimtarihi = 2006-08-25 | yayımcı = Montana State University | yıl = 1999 | arşivurl = http://web.archive.org/web/20110817031149/http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm | arşivtarihi = 17 Ağustos 2011}} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).</ref> Further from the ice, a forebulge may form, which is curved slightly upward.<ref name="MSUforebulge">{{Web kaynağı | url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm#forebulge | başlık = Glossary of Important Terms in Glacial Geology - Forebulge | erişimtarihi = 2006-08-25 | yayımcı = Montana State University | yıl = 1999 | arşivurl = http://web.archive.org/web/20110817031149/http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm | arşivtarihi = 17 Ağustos 2011}} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).</ref>
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* [[yol çukuru]]<!--A depression may be a [[pothole]] - either a simple roadway depression or a [[fluvial]] erosional depression in a [[river]] [[streambed]], or area affected by coastal water currents.
* [[yol çukuru]]<!--A depression may be a [[pothole]] - either a simple roadway depression or a [[fluvial]] erosional depression in a [[river]] [[streambed]], or area affected by coastal water currents.
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== Referanslar ==
== Referanslar ==
* {{Web kaynağı| url = http://www.geotech.org/survey/geotech/dictiona.html | başlık = Dictionary of Geologic Terms | erişimtarihi = 2006-08-25 | yayımcı = geotech.org }}
* {{Web kaynağı | url = http://www.geotech.org/survey/geotech/dictiona.html | başlık = Dictionary of Geologic Terms | erişimtarihi = 2006-08-25 | yayımcı = geotech.org | arşivurl = http://web.archive.org/web/20121116065716/http://www.geotech.org:80/survey/geotech/dictiona.html | arşivtarihi = 16 Kasım 2012}}
* {{Web kaynağı| url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm | başlık = Glossary of Important Terms in Glacial Geology | erişimtarihi = 2006-08-25 | yayımcı = Montana State University | yıl = 1999 }} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).
* {{Web kaynağı | url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm | başlık = Glossary of Important Terms in Glacial Geology | erişimtarihi = 2006-08-25 | yayımcı = Montana State University | yıl = 1999 | arşivurl = http://web.archive.org/web/20110817031149/http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm | arşivtarihi = 17 Ağustos 2011}} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).


{{jeoloji-taslak}}
{{jeoloji-taslak}}

Sayfanın 13.24, 19 Aralık 2015 tarihindeki hâli

Jeolojide depresyon çevresine göre çökmüş bir yeryüzü şeklini tanımlamak için kullanılır. Depresyonun oluşmasında çok değişik mekanizmalar rol alabilir ve depresyon çok değişik terimlerle açıklanabilir.

Bu terimlerden bazıları; Graben, vadi, okyanus çukuru vb.

Referanslar