HiPOD: Saturday, 11 June 2022
Detecting Olivine near Noachis Terra

Detecting Olivine near Noachis Terra
This observation shows the bedrock on the floor of a crater near Noachis Terra. This crater is unique because it has been very well characterized as being olivine rich.

Olivine is a magnesium-iron silicate that is very common on Earth, particularly in the mantle. While the large scale morphology of these craters is well characterized, this is not the case with fine scale layering and fracturing. Understanding these morphologic characteristics in craters could help describe large scale crustal processes on Mars, including the genesis of magmas and the creation of regolith.

There are other regions of Mars that are also rich in olivine. Olivine turns into other minerals in the presence of water, so scientists are interested in looking for those minerals as well.

This caption is based on the original science rationale.

ID: ESP_021971_1505
date: 4 April 2011
altitude: 255 km

#Mars #science #NASA

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Black & white is less than 5 km across; enhanced color is less than 1 km. For full images including scale bars, visit the ID link.