High Sand Fluxes and Abrasion Rates on Mars Determined from HiRISE Images

The volumetric transport rate of sand, or flux, is a fundamental parameter that controls the rate of landscape modification. This process is responsible for the movement of ripples and dunes, as well as the abrasion of rocks and landforms. Measuring sand flux on Mars was previously not possible beca...

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Bibliographic Details
Main Authors: Bridges, N. T., Ayoub, F., Avouac, J.-P., Leprince, S., Lucas, A., Mattson, S.
Format: Conference Object
Language:unknown
Published: 2012
Subjects:
Online Access:https://authors.library.caltech.edu/65496/
https://authors.library.caltech.edu/65496/1/high_sand.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20160318-162107096