NASA finds out the secret of Venus!
How does the Earth lose its heat? NASA explained that the Earth's hot core heats the mantle which then transports the heat to the lithosphere, the outermost solid layer of rock. The heat is subsequently released into space, cooling the uppermost portion of the mantle. This circulation of the mantle, known as mantle convection, is responsible for driving tectonic processes on the surface and keeping the plates in motion. But the heat flow mechanism of Venus has been a mystery so far. The absence of tectonic plates on Venus has resulted in persistent questions in planetary science regarding how the planet loses its heat and what processes shape its surface.
A recent study has analyzed archival NASA data and suggests that Venus might be releasing heat due to geologic activity in areas known as coronae, which is similar to the early tectonic activity on Earth. The research has used three-decade-old data from NASA's Magellan mission with a new perspective. Here's what the study says about Venus.
While using the observations of the Magellan spacecraft made in the early 1990s of quasi-circular geological features coronae on Venus, the researchers figured out that “coronae tend to be located where the planet's lithosphere is at its thinnest and most active.”
So far, scientists used to believe that the lithosphere of Venus is stagnant and thick. NASA further explained that similar to how a thin sheet releases more body heat than a thick one, a thin lithosphere permits more heat to exit the planet's interior through buoyant plumes of molten rock. Usually, elevated heat flow results in amplified volcanic activity beneath the surface. Therefore, coronae possibly expose sites where active geology is currently influencing the surface of
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