|
-->
* [[havza]]<!--
* 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">{{citeCite web | url = http://www.geotech.org/survey/geotech/dictiona.html#sectB | başlık = Dictionary of Geologic Terms - B | erişimtarihi = 2006-08-25 | yayımcı = geotech.org }}</ref>
| url = http://www.geotech.org/survey/geotech/dictiona.html#sectB
| title = Dictionary of Geologic Terms - B
| accessdate = 2006-08-25
| publisher = 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">{{citeCite web | url = http://www.geotech.org/survey/geotech/dictiona.html#sectK | başlık = Dictionary of Geologic Terms - K | erişimtarihi = 2006-08-26 | yayımcı = geotech.org }}</ref>
| url = http://www.geotech.org/survey/geotech/dictiona.html#sectK
| title = Dictionary of Geologic Terms - K
| accessdate = 2006-08-26
| publisher = geotech.org
}}</ref>
-->
<!--
* 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">{{citeCite web | 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.
| url = http://www.geotech.org/survey/geotech/dictiona.html#sectC
| title = Dictionary of Geologic Terms - C
| accessdate = 2006-08-25
| publisher = geotech.org
}}</ref> or [[maar]]s in volcanic areas.
-->
<!--
* [[: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]].-->
<!--
* 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">{{citeCite web | 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">{{Cite web | 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>
| url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm#peripheral
| title = Glossary of Important Terms in Glacial Geology - Peripheral Depression
| accessdate = 2006-08-25
| year = 1999
| publisher = Montana State University
}} 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">{{cite web
| url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm#forebulge
| title = Glossary of Important Terms in Glacial Geology - Forebulge
| accessdate = 2006-08-25
| year = 1999
| publisher = Montana State University
}} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).</ref>
-->
* [[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.
-->
== Referanslar ==
* {{Cite web | url = http://www.geotech.org/survey/geotech/dictiona.html | başlık = Dictionary of Geologic Terms | erişimtarihi = 2006-08-25 | yayımcı = geotech.org }}
* {{cite web
* {{Cite web | 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).
| url = http://www.geotech.org/survey/geotech/dictiona.html
| title = Dictionary of Geologic Terms
| accessdate = 2006-08-25
| publisher = geotech.org
}}
* {{cite web
| url = http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm
| title = Glossary of Important Terms in Glacial Geology
| accessdate = 2006-08-25
| year = 1999
| publisher = Montana State University
}} Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).
=== Citations ===
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