Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image

width 220 m; Right: parallel streaks and effect of local topography at lower left; image width 260 m. Slope is 20-300, top to bottom. Slope streaks in the Antarctic Dry Valleys: Characteristics, candidate formation mechanisms, and implications for slope streak formation in the Martian environment

Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.753
http://people.bu.edu/marchant/Dave_Conference Abstracts/Other/Head_ISAES_2007_177.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.456.753 2023-05-15T13:35:23+02:00 Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.753 http://people.bu.edu/marchant/Dave_Conference Abstracts/Other/Head_ISAES_2007_177.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.753 http://people.bu.edu/marchant/Dave_Conference Abstracts/Other/Head_ISAES_2007_177.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://people.bu.edu/marchant/Dave_Conference Abstracts/Other/Head_ISAES_2007_177.pdf 2007 Slope streaks in the Antarctic Dry Valleys Characteristics candidate formation text ftciteseerx 2016-01-08T06:14:54Z width 220 m; Right: parallel streaks and effect of local topography at lower left; image width 260 m. Slope is 20-300, top to bottom. Slope streaks in the Antarctic Dry Valleys: Characteristics, candidate formation mechanisms, and implications for slope streak formation in the Martian environment Text Antarc* Antarctic Unknown Antarctic The Antarctic
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic 2007
Slope streaks in the Antarctic Dry Valleys
Characteristics
candidate formation
spellingShingle 2007
Slope streaks in the Antarctic Dry Valleys
Characteristics
candidate formation
Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image
topic_facet 2007
Slope streaks in the Antarctic Dry Valleys
Characteristics
candidate formation
description width 220 m; Right: parallel streaks and effect of local topography at lower left; image width 260 m. Slope is 20-300, top to bottom. Slope streaks in the Antarctic Dry Valleys: Characteristics, candidate formation mechanisms, and implications for slope streak formation in the Martian environment
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image
title_short Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image
title_full Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image
title_fullStr Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image
title_full_unstemmed Figure 1. Mars slope streaks. MOC M00/02117. Figure 2. Slope Streaks in the ADV; Left: digitate streaks, image
title_sort figure 1. mars slope streaks. moc m00/02117. figure 2. slope streaks in the adv; left: digitate streaks, image
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.753
http://people.bu.edu/marchant/Dave_Conference Abstracts/Other/Head_ISAES_2007_177.pdf
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source http://people.bu.edu/marchant/Dave_Conference Abstracts/Other/Head_ISAES_2007_177.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.753
http://people.bu.edu/marchant/Dave_Conference Abstracts/Other/Head_ISAES_2007_177.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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