Curiosity rover, NASA’s trailblazer on Mars, has just shared stunning close-up photos of large, web-like formations resembling giant spiderwebs. These formations, called “boxwork,” are intriguing because they might provide clues about Mars’ history, especially regarding water and the potential for life.
So, what exactly are these Martian ‘spiderwebs’? The boxwork formations stretch across an area of up to 12 miles (20 kilometers) and are made up of intersecting mineral-rich ridges that create a fascinating criss-cross pattern. Positioned on the slopes of Mount Sharp within Gale Crater, where Curiosity has been exploring since 2012, these features originated from ancient groundwater that left behind mineral deposits over time. Until now, researchers only observed them remotely through satellites. Now, Curiosity’s close-up views promise to unlock secrets about Mars’ geological past.
Curiosity’s team thinks these boxwork ridges formed when groundwater seeped through cracks in the rock, depositing minerals that eventually hardened. Over millions of years, Martian winds eroded softer rock around these structures, leaving the ridges intact. Interestingly, similar smaller formations can be found on Earth in cave systems, providing insight into our planet’s environmental history. This parallel gives scientists hope that studying Mars could reveal its watery past and whether it was ever suitable for life.
Among Curiosity’s recent findings is the discovery of veins of calcium sulfate near the boxwork formations. This salty mineral, usually a sign of groundwater activity, is a surprising find at such a high elevation on Mount Sharp. “This mineral hasn’t been seen so far up Mount Sharp before, so its discovery here is really surprising,” noted Abigail Fraeman, a deputy project scientist at NASA’s Jet Propulsion Laboratory. This adds more weight to the idea that liquid water once flowed in this area, possibly making it a habitable environment in Mars’ distant past.
Scientists are particularly keen on these boxwork features as they may help answer crucial questions about Mars’ capacity to support life. The minerals encased in these formations likely crystallized underground, a place where conditions could have been warmer and where salty liquid water might have existed.
This scenario bears a resemblance to early Earth, where life thrived even in extreme conditions. Kirsten Siebach, a mission scientist at Rice University, commented, “Early Earth microbes could have survived in a similar environment. That makes this place exciting to explore.” By examining the boxwork formations and their minerals, researchers hope to gain deeper insights into whether Mars could have once been alive or may still hold microbial life today.
For the time being, the focus remains on these fascinating geological features as scientists work to uncover more about Mars’ history and its intriguing potential to support life.