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- CRISM: Compact Reconnaissance Imaging Spectrometer for Mars
- CTX: Context Camera
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- SHARAD: Shallow Radar
- THEMIS: Thermal Emission Imaging System
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Tag Archives: sediments
HiRISE: Ridge in Coprates Chasma
A ridge in Coprates Chasma. Beautiful Mars series.
Posted in Reports
Tagged Beautiful Mars, Coprates Chasma, High Resolution Imaging Science Experiment, HiRISE, Mars Reconnaissance Orbiter, mass wasting, MRO, NASA, sediments, University of Arizona, Valles Marineris
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HiRISE: Choose your hiking trail
Choose your hiking trail. Beautiful Mars series.
Posted in Reports
Tagged Beautiful Mars, High Resolution Imaging Science Experiment, HiRISE, layers, Mars Reconnaissance Orbiter, MRO, NASA, sand dunes, sediments, University of Arizona
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HiRISE: Out and about in a Nili Fossae crater
Out and about in a crater in northern Nili Fossae. Beautiful Mars series.
Posted in Reports
Tagged Beautiful Mars, double craters, High Resolution Imaging Science Experiment, HiRISE, layers, Mars Reconnaissance Orbiter, MRO, NASA, Nili Fossae, sediments, University of Arizona
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HiRISE: Ancient lake sediments
This image shows some interesting fractured materials on the floor of an impact crater in Arabia Terra. There is a channel entering the crater and exiting it (see CTX image). This channel, along with an unusual deposit on the lowest … Continue reading
Posted in Reports
Tagged Arabia Terra, channels, crater lakes, High Resolution Imaging Science Experiment, HiRISE, Mars Reconnaissance Orbiter, MRO, NASA, sediments, University of Arizona
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HiRISE image: Bright sediments in Ladon Basin
This image shows some bright layered deposits exposed within a linear trough along the floor of the Ladon Basin. There is a large channel system that flows into the basin, called Ladon Valles, and scientists think that the basin may … Continue reading
Posted in Reports
Tagged channels, High Resolution Imaging Science Experiment, HiRISE, Ladon Basin, Ladon Valles, layers, Mars Reconnaissance Orbiter, MRO, NASA, sediments, University of Arizona
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Polar gullies erode from carbon dioxide flows
Gullies on Martian slopes form by flowing water, most probably trickles of snowmelt or groundwater. But what about the gullies found in places such as the high latitudes and polar regions where temperatures never rise above the freezing point for … Continue reading