Image:Mars glacial-like lobe deposit.jpg

From Wikipedia, the free encyclopedia

Wikimedia Commons logo This is a file from the Wikimedia Commons. The description on its description page there is shown below.
Commons is a freely licensed media file repository. You can help.

[edit] Summary

Description

Perspective view of a 5-km-wide, glacial-like lobe deposit sloping up into a box canyon along the crustal dichotomy boundary on Mars. The up-slope geometry of these deposits implies a past thickness of ice on the order of ~920 m at this location. Cessation of glacial conditions caused lowering of the debris-covered glacier surface to the confi guration seen today. See “Late Amazonian glaciation at the dichotomy boundary on Mars: Evidence for glacial thickness maxima and multiple glacial phases,” by Dickson et al. (2008), doi:10.1130/G24382A.1

Source

Geological Society of America

Date

c. 2008

Author

NASA/JPL/MSSS

Permission
(Reusing this image)

see below


[edit] Licensing

Public domain
This file is in the public domain because it was created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (NASA copyright policy page or JPL Image Use Policy).

Deutsch | English | Español | Français | Nederlands | Português | Русский | ‪中文(简体)‬ | ‪中文(繁體)‬ | +/-

Warning sign
Warnings:

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeDimensionsUserComment
current11:21, 28 April 2008550×474 (64 KB)Bender235 ({{Information |Description=Perspective view of a 5-km-wide, glacial-like lobe deposit sloping up into a box canyon along the crustal dichotomy boundary on Mars. The up-slope geometry of these deposits implies a past thickness of ice on the order of ~920 m)
The following pages on the English Wikipedia link to this file (pages on other projects are not listed):