NASA’s Curiosity Mars rover captured this panorama of
boxwork formations — the low ridges seen here with hollows in between them —
using its Mastcam on Sept. 26, 2025.
NASA/JPL-Caltech/MSSS
For about six months, NASA’s Curiosity
Mars rover has been exploring a region full of geologic formations called
boxwork, low ridges standing roughly 3 to 6 feet (1 to 2 meters) tall with
sandy hollows in between. Crisscrossing the surface for miles, the formations
suggest ancient groundwater flowed on this part of the Red Planet later than
scientists expected. This possibility raises new questions about how long
microbial life could have survived on Mars billions of years ago, before rivers
and lakes dried up and left a freezing desert world behind.
The boxwork formations look like giant spiderwebs when viewed
from space. To explain the shapes, scientists have proposed that groundwater
once flowed through large fractures in the bedrock, leaving behind minerals.
Those minerals then strengthened the areas that became ridges while other
portions without mineral reinforcement were eventually hollowed out by wind.
These bumpy nodules were formed by minerals left
behind as groundwater was drying out on Mars billions of years ago. NASA’s
Curiosity rover captured images of these pea-size features while exploring
geologic formations called boxwork on Aug. 21, 2025.
NASA/JPL-Caltech/MSSS
Until Curiosity arrived at this region, however, no one could be sure what
these formations looked like up close, and there were even more questions about
how they were made.
Unpacking boxwork
Although Earth also has boxwork
ridges, they’re rarely taller than a few centimeters and are usually found in
caves or in dry, sandy environments. The Curiosity team wanted to get a close
look at the Martian formations and gather more data. This posed a real
challenge for rover drivers: They needed to send instructions to Curiosity, an
SUV-size vehicle that weighs nearly a ton (899 kilograms), so that it could
roll across the tops of ridges not much wider than the rover itself.
“It almost feels like a highway we
can drive on. But then we have to go down into the hollows, where you need to
be mindful of Curiosity’s wheels slipping or having trouble turning in the
sand,” said operations systems engineer Ashley Stroupe of NASA’s Jet Propulsion
Laboratory in Southern California, which built Curiosity and leads the mission.
“There’s always a solution. It just takes trying different paths.”
For scientists, the challenge is
piecing together how such a vast network of boxwork could exist on Mount Sharp,
the 3-mile-tall (5-kilometer-tall) mountain the rover has been ascending. Each
layer of the mountain formed in a different era of Mars’ ancient, changing
climate. The higher Curiosity goes, the more the landscape bears signs that
water was drying out over time, with occasional wet periods that saw the return
of rivers and lakes.
“Seeing boxwork this far up the
mountain suggests the groundwater table had to be pretty high,” said Tina
Seeger of Rice University in Houston, one of the mission scientists leading the
boxwork investigation. “And that means the water needed for sustaining life
could have lasted much longer than we thought looking from orbit.”
Previous orbital imagery included
one crucial piece of evidence: dark lines running across the “spiderwebs.” In
2014, it was proposed that these lines might be what are known as central
fractures, where groundwater seeped through rock cracks and allowed minerals to
concentrate. Investigating the ridges up close, Curiosity found that these
lines are in fact fractures, lending weight to that hypothesis.
The rover also discovered bumpy
textures called nodules, an obvious sign of past groundwater that has been
spotted many times by Curiosity and other Mars missions. Unexpectedly, these
nodules were not found near the central fractures, but along a ridge’s walls
and the hollows between them.
“We can’t quite explain yet why the
nodules appear where they do,” Seeger said. “Maybe the ridges were cemented by
minerals first, and later episodes of groundwater left nodules around them.”
Roving laboratory
A major part of Curiosity’s science
centers on rock samples collected by the rock-pulverizing drill on the end of
the rover’s robotic arm. The resulting powder can be trickled into complex
science instruments in the vehicle’s body for analysis.
Last year, three samples from the
boxwork region — one from a ridgetop, one from bedrock within a hollow, and one
from a transitional area before Curiosity reached the ridges — were collected
by the drill and analyzed with X-rays and a high-temperature oven. The X-ray
analyses found clay minerals in the ridge and carbonate minerals in the hollow,
providing additional clues to help understand how these features formed.
The mission recently collected
a fourth sample, which was analyzed with a special technique reserved for the most
intriguing science targets: After the pulverized rock went into the rover’s
high-temperature oven, chemical reagents reacted with the sample to conduct
what is called wet chemistry. The resulting reactions make it easier to detect certain organic
compounds, carbon-based molecules important to the formation of life.
Sometime in March, Curiosity will
leave the boxwork formations behind. The whole region is part of a layer on Mount Sharp enriched in salty minerals called sulfates,
which formed as water was drying out on Mars. Curiosity’s team plans to
continue exploring this sulfate layer for many miles in the coming year,
learning more about how the ancient Red Planet’s climate changed billions of
years ago.
More about Curiosity
Curiosity was built by NASA’s Jet
Propulsion Laboratory, which is managed by Caltech in Pasadena, California. JPL
leads the mission on behalf of NASA’s Science Mission Directorate in Washington
as part of NASA’s Mars Exploration Program portfolio.
To learn more about Curiosity, visit: science.nasa.gov/mission/msl-curiosity
Source: NASA’s Curiosity Rover Sees Martian ‘Spiderwebs’ Up Close - NASA


