Origin of longitudinal grooving in Tiu VallisMars: Isolation of responsible fluid‐types

Geophysical Research Letters

Volumn 6, Issue 9, 1979, Pages 735-738

  Thompson, David E ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0001464035     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/GL006i009p00735     Document Type: Article

References (14)

1. Paleohydrology and sedimentology of Lake Missoula flooding in eastern Washington:
2. Erosional forms and processes for the catastrophic Pleistocene Missoula floods in eastern Washington:
3. A preliminary assessment of the fluid erosional processes that shaped the martian outflow channels:
4. Morphological mapping of martian outflow channels:
5. Morphometry of streamlined forms in terrestrial and martian channels:
6. Erosion by catastrophic floods on Mars and Earth:
7. The Channeled Scabland: a guide to the geomorphology of the Columbia Basin
8. Missoula flooding in the Cheney‐Palouse scabland tract: terrestrial analogue to the channeled terrain of Mars:
9. Instability and river channels:
10. Instability of erodible beds:
11. On the origin of meandering and braiding in alluvial streams: