Mars has a long and complex geological history. Geological activity, such as volcanic eruptions, tectonics, and crustal movements, played a significant role in shaping the planet. In the past, Mars was a much more dynamic planet, with active volcanoes and possibly liquid water flowing on its surface.
Today, Mars appears to be geologically inactive for the most part. The northern hemisphere, home to expansive volcanic plateaus and ancient lava plains, along with formations like Valles Marineris, suggests a history of significant geological events.
Key features of Martian geology include:
- Volcanism, especially around the Tharsis and Elysium regions
- Different ages in surface features across the planet
- A lack of plate tectonics
Recent research hints at the possibility of minor tectonic activity or "marsquakes," but nothing has confirmed widespread geological activity as seen in Earth's past.
If contemporary volcanic activity were discovered, particularly in unexpected regions like the southern highlands, it would revolutionize our understanding of Mars. It might suggest internal heat sources or processes at work that we have yet to discover or understand.