File:FacectxF23 044929 2199 XI 39N010W.jpg - Revision history

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2020-03-21T13:57:54Z

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Suitupandshowup: Landforms near Face. Mesa, ridges, and possible cirques are present. A '''cirque''' (French, from the Latin word ''circus'') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are '''corrie''' (from Scottish Gaelic coire, meaning a pot or cauldron) and '''cwm''' (Welsh "valley"). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped secti...

2020-03-21T13:53:02Z

Landforms near Face. Mesa, ridges, and possible cirques are present. A '''cirque''' (French, from the Latin word ''circus'') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are '''corrie''' (from Scottish Gaelic coire, meaning a pot or cauldron) and '''cwm''' (Welsh "valley"). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped secti...

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== Summary ==
Landforms near Face. Mesa, ridges, and possible cirques are present. A '''cirque''' (French, from the Latin word ''circus'') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are '''corrie''' (from Scottish Gaelic coire, meaning a pot or cauldron) and '''cwm''' (Welsh "valley"). A cirque may also be a similarly shaped landform arising from fluvial erosion.

The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens: hence it experiences somewhat greater erosion forces, and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a [[Tarn (lake)|tarn]] (small lake) behind a dam which marks the downstream limit of the glacial overdeepening: the dam itself can be composed of [[moraine]], [[glacial till]], or a lip of the underlying bedrock.<ref name=Knight2009 />
Source: http://viewer.mars.asu.edu/planetview/inst/ctx/F23_044929_2199_XI_39N010W#P=F23_044929_2199_XI_39N010W&T=2

Location: 39.94 N and 350.02 E

Image Credit: NASA/MSSS/Secosky

== Licensing ==
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 Landforms near Face.  Mesa, ridges, and possible cirques are present.  A '''cirque''' (French, from the Latin word ''circus'') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are '''corrie''' (from Scottish Gaelic coire, meaning a pot  or cauldron) and '''cwm''' (Welsh "valley"). A cirque may also be a similarly shaped landform arising from fluvial erosion.
-The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens: hence it experiences somewhat greater erosion forces, and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a [[Tarn (lake)|tarn]] (small lake) behind a dam which marks the downstream limit of the glacial overdeepening: the dam itself can be composed of [[moraine]], [[glacial till]], or a lip of the underlying bedrock.<ref name=Knight2009 />
+The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens: hence it experiences somewhat greater erosion forces, and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a [[Tarn (lake)|tarn]] (small lake) behind a dam which marks the downstream limit of the glacial overdeepening: the dam itself can be composed of [[moraine]], [[glacial till]], or a lip of the underlying bedrock.<ref>Knight | first = Peter G. | title = Encyclopedia of Earth Sciences Series: Encyclopedia of Paleoclimatology and Ancient Environments | publisher = [[Springer-Verlag| ]] | series = Cirques | volume = 1358  | edition =   | location = Springer Netherlands | year = 2009  | pages = 155–56  | doi = 10.1007/978-1-4020-4411-3_37  | isbn =  978-1-4020-4551-6|</ref>
 Source:  http://viewer.mars.asu.edu/planetview/inst/ctx/F23_044929_2199_XI_39N010W#P=F23_044929_2199_XI_39N010W&T=2