This past week, a team of researchers using the now-dead Venus Express spacecraft revealed hotspots on the surface shooting up by several hundred degrees. Their best guess as to what’s happening? Lava from active volcanoes.
We all know that Venus is a hellish world that killed some Soviet landers in minutes. Its average surface temperature would easily melt lead. But even on the surface trapped in a runaway greenhouse effect, the hotspots stood out. So what do we know about volcanoes on Venus?
Recent lava flows were first reported in 2010, when data from Venus Express was compared to the older NASA Magellan spacecraft, which mapped elevations. Scientists saw compositional differences in the lava-soaked terrain compared to what was around it — specifically, minerals that are abundant in lava on Earth.
“Recent”, however, was a relative term that could mean hundreds of years ago, or millions. Here’s an example of what Venus Express saw on the volcanic peak Idunn Mons. More concrete evidence came in 2012, when scientists reported spikes in sulfur dioxide noted by Venus Express after six years of work. The gas is generated by volcanoes, so this provided even more evidence that the volcanoes are awake.
Why are volcanoes so important? One reason is they reveal what is happening on the insides of the planet. And what we know shows that Venus was or is extremely active. The planet has more than 1,600 large volcanoes or volcanic features and many smaller ones, according to Oregon State.
But here’s the rub (literally) — plate tectonics don’t appear to be involved in a big way. On Earth, colliding tectonic plates create volcanic activity. But the chains of volcanoes and rifts on our planet aren’t in evidence on Venus.
Read more at Discovery News
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