Scratches and grooves on the Martian surface look like a huge 'fingernail' was gouging out regolith on the Red Planet, but there's a volcanic origin to these features.
Specifically, scientists believe that these faults, dubbed Tantalus Fossae, were created by the volcano Alba Mons, which is located to the west of the terrain visible in the striking new views. The images are based on data gathered by the European Space Agency's (ESA) Mars Express mission, which has been orbiting Mars since 2003.
Those intriguing gouges around the flanks of Alba Mons are known as grabens, which formed as the mountain grew, ESA officials wrote in a statement about the images. As volcanic activity pulled at the Martian surface, parallel fault lines opened up circling the peak; the rock between them dropped into the empty space this created, agency officials explained — like geologic stretch marks
The grabens stretch in an "incomplete ring" around Alba Mons, ESA noted, for a total length of 620 miles (1,000 kilometers). In some places, the grabens are as deep as 1,150 feet (350 meters), more than three times the height of the Statue of Liberty.
According to ESA, the faults on display in the new images likely formed one by one over a long period of geological activity, not simultaneously.
Scientists in part generate that timeline by comparing the grabens with other features in the region. For example, a large crater that forming the centerpiece of one image has grabens on top of it — which shows the crater must have been there first. Also, smaller "branching" valleys cutting through the grabens are assumed to be older.
Alba Mons is roughly 22,000 feet (6.8 km) tall. Compared to its neighbor, the gigantic Olympus Mons, Alba Mons has gentler slopes and a much lower elevation. That said, Alba Mons is comparable in height to Earth's Mount Everest, which stands at nearly 29,000 feet (8.8 km.)
Mars Express has been examining Mars since 2003 and acquired the new imagery using its High Resolution Stereo Camera. According to ESA, the mission has charted odd features on the Red Planet's surface, such as tectonic faults and river channels, throughout its mission in a long-standing investigation to chronicle Martian history.
A 2006 Journal of Geophysical Research paper — which uses an alternate name for the volcano, Alba Patera, that emphasizes the collapsed summit — suggests its volcanic deposits date to the Amazonian period. That period of slow-scale change, according to ESA, started roughly 2.9 billion years ago and continues to today.
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Elizabeth Howell (she/her), Ph.D., is a staff writer in the spaceflight channel since 2022 covering diversity, education and gaming as well. She was contributing writer for Space.com for 10 years before joining full-time. Elizabeth's reporting includes multiple exclusives with the White House and Office of the Vice-President of the United States, an exclusive conversation with aspiring space tourist (and NSYNC bassist) Lance Bass, speaking several times with the International Space Station, witnessing five human spaceflight launches on two continents, flying parabolic, working inside a spacesuit, and participating in a simulated Mars mission. Her latest book, "Why Am I Taller?", is co-written with astronaut Dave Williams. Elizabeth holds a Ph.D. and M.Sc. in Space Studies from the University of North Dakota, a Bachelor of Journalism from Canada's Carleton University and a Bachelor of History from Canada's Athabasca University. Elizabeth is also a post-secondary instructor in communications and science at several institutions since 2015; her experience includes developing and teaching an astronomy course at Canada's Algonquin College (with Indigenous content as well) to more than 1,000 students since 2020. Elizabeth first got interested in space after watching the movie Apollo 13 in 1996, and still wants to be an astronaut someday. Mastodon: https://qoto.org/@howellspace