The Mineralogical Variability of Aram Chaos
NASA/JPL-Caltech/UArizona
The Mineralogical Variability of Aram Chaos
ESP_085467_1840  Science Theme: 
Aram Chaos is located within a confined 280-kilometer diameter Noachian-aged crater that at some time filled with water. Much of the chaos terrain within Aram is characterized by plateaus and mesas separated by valleys with varying degree of sizes.

After the chaos terrain formed, light-toned sulfates were deposited. Sulfates are a common mineral identified from both orbital and rover data of Mars and can vary in their mineralogy and hydration state. Three different types of sulfates have been identified in Aram Chaos, indicating a complex and evolving aqeuous history.

By studying the distribution and stratigraphy of the different types of sulfates, scientists can explore what most likely explains their formation, as well as how that geologic timing constrains the broader Martian climate evolution when they formed.

Written by: Cathy Weitz  (22 January 2025)


This is a stereo pair with PSP_006953_1840.
 
Acquisition date
19 October 2024

Local Mars time
14:27

Latitude (centered)
3.918°

Longitude (East)
339.501°

Spacecraft altitude
273.2 km (169.8 miles)

Original image scale range
from 28.3 cm/pixel (with 1 x 1 binning) to 56.7 cm/pixel (with 2 x 2 binning)

Map projected scale
25 cm/pixel and North is up

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Equirectangular

Emission angle
16.0°

Phase angle
22.2°

Solar incidence angle
38°, with the Sun about 52° above the horizon

Solar longitude
348.1°, Northern Winter

For non-map projected images
North azimuth:  96°
Sub-solar azimuth:  352.2°
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All of the images produced by HiRISE and accessible on this site are within the public domain: there are no restrictions on their usage by anyone in the public, including news or science organizations. We do ask for a credit line where possible:
NASA/JPL-Caltech/UArizona

POSTSCRIPT
NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, Calif., manages the Mars Reconnaissance Orbiter for NASA’s Science Mission Directorate, Washington. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona.