Space Science
Curiosity Blog, Sols 4845-4851: Bye-Bye Boxwork, Bye-Bye
Apr 13, 2026, 7:37 PM
出典: NASA News
Written by Lucy Thompson, APXS Strategic Planner and Planetary Geologist at the University of New Brunswick, Canada Earth planning date: Friday, March 27, 2026 Last weekend’s drive took us just over the southernmost contact of the boxwork terrain with the surrounding layered sulfate unit. This was our third time crossing this contact, providing an excellent […]
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Curiosity Blog, Sols 4845-4851: Bye-Bye Boxwork, Bye-Bye
NASA’s Mars rover Curiosity acquired this image, showing the polygonal sulfate unit currently being investigated by the rover after leaving the boxwork terrain. Curiosity captured the image using its Left Navigation Camera on March 27, 2026 — Sol 4848, or Martian day 4,848 of the Mars Science Laboratory mission — at 10:43:16 UTC.
NASA/JPL-Caltech
Written by Lucy Thompson, APXS Strategic Planner and Planetary Geologist at the University of New Brunswick, Canada
Earth planning date: Friday, March 27, 2026
Last weekend’s drive took us just over the southernmost contact of the boxwork terrain with the surrounding layered sulfate unit. This was our third time crossing this contact, providing an excellent opportunity to look for any changes across it. We have acquired multiple observations (chemistry and imaging for textures) of the boxwork-bearing bedrock close to the contact. We are also interested in determining whether the layered sulfate unit to the south of the boxwork terrain has the same depositional setting as that encountered to the north. Is the composition the same as the typical layered sulfate unit we encountered prior to the boxwork, or could there be a change associated with a different depositional environment, source sediment, or potential alteration along the contact with the boxwork?
Unfortunately, although the weekend drive was successful, Curiosity was not on stable enough ground coming into planning Monday to brush the dusty bedrock, although we were able to get MAHLI imaging of a block within the workspace. The rover engineers repositioned the rover so that we could safely unstow the arm, brush, image with MAHLI, and analyze with APXS the layered sulfate unit bedrock just across the contact (“Santa Rosa”) in Wednesday’s plan. We also looked at a concentration of granules with APXS and MAHLI (“Piedra Colgada”). They appear to be a collection of fine nodules that eroded from the bedrock, thereby allowing us to obtain chemical and textural data on these nodules.
The drive planned on Wednesday took us another 50 meters (about 164 feet) away from the boxwork, to a stunning sulfate unit workspace. The bedrock contained abundant resistant ridges forming a polygonal pattern. We wanted to compare these current exposures with polygonal textures observed previously, for example, within the boxwork, the sulfate unit before the boxwork, and the clay-sulfate transition. We are brushing two spots on the bedrock in front of us (“Ocharaza” and “Nevado Tres Cruces”) and analyzing them both with APXS and MAHLI for chemistry and texture.
Across the three plans, Mastcam imaging was acquired of the boxwork terrain behind, the sulfate unit ahead, and the rocks immediately in front of us. In particular, this weekend’s plan was jam-packed full of mosaics to capture the amazing polygonal textures surrounding the rover. The planned 30-meter drive (about 98 feet) should keep us in this same terrain.
The environmental group has also been busy planning multiple observations to monitor atmospheric opacity, optical depth and aerosol scattering properties, clouds, wind direction, and potential dust-devil activity. Navcam and Mastcam are utilized to make these observations. As usual, our plans this week included the standard DAN, REMS and RAD activities.
NASA’s Curiosity rover at the base of Mount Sharp
NASA/JPL-Caltech/MSSS
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Apr 13, 2026
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Mars rovers are robotic vehicles designed to explore the surface of Mars. They are equipped with scientific instruments to analyze soil, rocks, and atmosphere, providing valuable data about the planet's geology and potential for past life.
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Sulfate Minerals
Sulfate minerals are a group of minerals that contain the sulfate ion (SO4) and are formed through various geological processes. They are significant in understanding the chemical composition of planetary bodies, including Mars, as they can indicate past water activity and environmental conditions.