Back to Search Start Over

The Curiosity Rover's Exploration of Glen Torridon, Gale Crater, Mars: An Overview of the Campaign and Scientific Results.

Authors :
Bennett KA
Fox VK
Bryk A
Dietrich W
Fedo C
Edgar L
Thorpe MT
Williams AJ
Wong GM
Dehouck E
McAdam A
Sutter B
Millan M
Banham SG
Bedford CC
Bristow T
Fraeman A
Vasavada AR
Grotzinger J
Thompson L
O'Connell-Cooper C
Gasda P
Rudolph A
Sullivan R
Arvidson R
Cousin A
Horgan B
Stack KM
Treiman A
Eigenbrode J
Caravaca G
Source :
Journal of geophysical research. Planets [J Geophys Res Planets] 2023 Jan; Vol. 128 (1), pp. e2022JE007185. Date of Electronic Publication: 2022 Dec 30.
Publication Year :
2023

Abstract

The Mars Science Laboratory rover, Curiosity , explored the clay mineral-bearing Glen Torridon region for 1 Martian year between January 2019 and January 2021, including a short campaign onto the Greenheugh pediment. The Glen Torridon campaign sought to characterize the geology of the area, seek evidence of habitable environments, and document the onset of a potentially global climatic transition during the Hesperian era. Curiosity roved 5 km in total throughout Glen Torridon, from the Vera Rubin ridge to the northern margin of the Greenheugh pediment. Curiosity acquired samples from 11 drill holes during this campaign and conducted the first Martian thermochemolytic-based organics detection experiment with the Sample Analysis at Mars instrument suite. The lowest elevations within Glen Torridon represent a continuation of lacustrine Murray formation deposits, but overlying widespread cross bedded sandstones indicate an interval of more energetic fluvial environments and prompted the definition of a new stratigraphic formation in the Mount Sharp group called the Carolyn Shoemaker formation. Glen Torridon hosts abundant phyllosilicates yet remains compositionally and mineralogically comparable to the rest of the Mount Sharp group. Glen Torridon samples have a great diversity and abundance of sulfur-bearing organic molecules, which are consistent with the presence of ancient refractory organic matter. The Glen Torridon region experienced heterogeneous diagenesis, with the most striking alteration occurring just below the Siccar Point unconformity at the Greenheugh pediment. Results from the pediment campaign show that the capping sandstone formed within the Stimson Hesperian aeolian sand sea that experienced seasonal variations in wind direction.<br /> (© 2022 The Authors. California Institute of Technology. Government sponsorship acknowledged. This article has been contributed to by U.S. Government employees and their work is in the public domain in the USA.)

Details

Language :
English
ISSN :
2169-9097
Volume :
128
Issue :
1
Database :
MEDLINE
Journal :
Journal of geophysical research. Planets
Publication Type :
Academic Journal
Accession number :
37034460
Full Text :
https://doi.org/10.1029/2022JE007185