This is an image of Venus.
Click on image for full size
NASA/JPL
The Earliest History of Venus
The terrestrial planets formed in two ways, either:
- very warm, separated into layers, with lots of water on the surface, with volcanic activity, as well as continental drift.
- cold and rocky, needing to be warmed from the inside before activity is seen on the surface. The planet never separates into layers, and the planet never forms a core.
With Venus, the first case is probably the most likely.
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...moreAlpha Regio is the home of Eve Mons, a volcano.
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...moreBeta Regio is an example of a volcanic rise, and is more like an island than a continent. Volcanic rises such as Beta Regio sometimes contain deep troughs. The troughs may be evidence of a surface inmotion.
...moreIshtar Terra is one of the two main continents of Venus, and is found near the north pole. Ishtar Terra is about the size of the United States. Ishtar Terra contains the four main mountain ranges of Venus.
...moreThis image clearly shows a bed where something once flowed. Without proper measurements, scientists can only guess what sort of liquid may have flowed through this channel. On Earth, such channels might
...moreThe feature of Venus' geography called a "Corona" is a deep, curving, trench surrounding an elevated plain. Coronae is the name for more than one corona. This is an image of Artemis Corona which is found
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