Mars, often called the Red Planet, may have been much wetter in its past than we thought. A recent study reveals more than 15,000 kilometers of ancient riverbeds in Mars’ Noachis Terra region. This suggests that flowing water, likely from rainfall, once covered a vast section of the planet.
Led by PhD student Adam Losekoot from the Open University, this research uncovered a network of fluvial sinuous ridges, or inverted channels, throughout Noachis Terra. These ridges formed when river sediment hardened and later became exposed as surrounding material eroded. The sheer size of these riverbeds points to a Mars that was once rich in water.
This finding changes the narrative about Mars’ history. Previously, many scientists thought the planet had been mostly cold and dry. But these ridges indicate a stable presence of surface water over a long period. This directly challenges older assumptions.
Historically, evidence of ancient water on Mars has often focused on valley networks. However, Noachis Terra hasn’t received as much attention. Researchers believed it had fewer valley networks, directing their focus to the sinuous ridges instead, which provide a compelling alternative for understanding Mars’ wet past.
The research team suggests that these conditions likely stabilized during the Noachian-Hesperian transition, a significant geological period around 3.7 billion years ago. This era marked a turning point in Mars’ climate and landscape, hinting that the region could have experienced prolonged wet periods crucial to shaping the planet.
A recent tweet from @cosmoknowledge highlighted these findings, emphasizing the ancient river system’s impact on our understanding of Mars. The analysis utilized high-resolution satellite data to reveal persistent water flow affecting the Martian landscape over extended times.
To gather this data, the researchers employed three advanced orbital tools: the Context Camera (CTX), the Mars Orbiter Laser Altimeter (MOLA), and the High-Resolution Imaging Science Experiment (HiRISE). These instruments allowed them to meticulously map the ridges across Noachis Terra, revealing many segments that rise tens of meters above the terrain.
The shapes and locations of these ridges indicate long periods of stable surface conditions. Water must have flowed across Mars longer than previously believed, suggesting a once-active environment.
This discovery contradicts the long-held view of Mars as largely cold and dry, hinting instead at sustained warm and wet conditions in its past. Losekoot expressed his excitement about studying Noachis Terra, noting it’s like uncovering a time capsule that has remained unchanged for billions of years.
These findings align with recent trends in space exploration and astronomy. With growing interest and funding in Mars research, scientists continually uncover more about the planet’s potential for ancient life and its climate history. As we gather more data, our understanding of Mars will undoubtedly continue to evolve.
For more in-depth information, you can read about the discovery on NASA’s official site here.