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Sols 4461-4463: Salty Salton Sea?

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Sols 4461-4463: Salty Salton Sea?

A grayscale wide-angle view of the Martian surface showing very rocky terrain in front of the Curiosity rover. Dark gray rocks — some wide and flat, others smaller and sharp-edged poking from the ground — are scattered among the dark gray soil. Some areas of the soil are wavy, as if sculpted at some point by wind or water. The rover’s robotic arm is reaching down and touching a rock with one of its instruments, in the upper-left center of the image. On the horizon, at upper right a butte rises from the ground, silhouetted by a light-colored sky. The rover’s right- and left-front wheels are also visible in the image, in the lower right and lower left corners of the image.
NASA’s Mars rover Curiosity acquired this image showing its Alpha Particle X-Ray Spectrometer (APXS), a spectrometer that measures the abundance of chemical elements in rocks and soils, on the “Chumash Trail” target in its workspace. Note the butte in the background. The rover used its Front Hazard Avoidance Camera (Front Hazcam) to capture the image on Feb. 19, 2025 — sol 4458, or Martian day 4,458 of the Mars Science Laboratory mission — at 21:03:48 UTC.
NASA/JPL-Caltech

Earth planning date: Friday, Feb. 21, 2025

Since first encountering the sulfate-bearing unit around Sol 3540, we have detected minerals and elemental concentrations consistent with the presence of various salts and a general drying out of Mars climate (read ”NASA’s Curiosity Mars Rover Reaches Long-Awaited Salty Region”). Salton Sea in California is a saline lake, meaning it has high concentrations of salty minerals formed as a result of evaporation processes dominating over input of fresh water. As such, we thought it would be a fitting name for one of our rock targets to be analyzed by the APXS and MAHLI instruments in this weekend plan. We have observed a variety of different textures and colors associated with the sulfate-bearing unit. The target “Salton Sea” is an example of one such texture — a dark-toned, relatively smooth, platy layer. Will the chemistry indicate the presence of salty minerals, some of which may be the same as those found at Salton Sea? Other rock targets to be analyzed in this busy weekend plan include “Wellman Divide,” another APXS and MAHLI target on a thicker, dark-toned, rougher textured layer, and “Goodykoontz” and “Paseo del Mar,” both ChemCam LIBS targets, on a nodule and a dark, platy layer, respectively.

We also continue to document the layers of rock exposed within several buttes and mesas around us (“Dragon Tooth” and “Texoli” buttes, and “Gould Mesa”) with CCAM RMI and Mastcam imaging. Curiosity will hopefully climb though equivalent layers as we continue our ascent of Mount Sharp, so these images can help with interpretation when we finally encounter them on the ground. Mastcam will also image a trough in the sand surrounding one of the bedrock blocks — a feature that has been observed relatively frequently lately.

The atmospheric scientists also have an action-packed plan with coordinated APXS atmospheric and ChemCam passive-sky observations to measure argon and oxygen, respectively, as well as standard activities. These observations help to track changes in seasonal atmospheric flow from equatorial to polar regions on Mars. Standard atmospheric monitoring activities included in the plan are: Navcam dust devil movies (x2), suprahorizon movies (x2), a zenith movie, line of sight observations (x2), and a cloud altitude observation, as well as Mastcam tau observations (x2).

After a planned drive of about 49 meters (about 161 feet) on the second sol of this three-sol weekend plan, the MARDI camera will take an image of the terrain beneath the rover. The plan is rounded out with standard REMS, DAN and RAD activities.

Written by Lucy Thompson, Planetary Geologist at University of New Brunswick

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