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Mercury |
 | | Mariner observed a world similar in general respects to the Moon: heavily cratered but with regions of relatively smooth plains, some of which may be the result of ancient volcanic activity, others due to the deposition of ejecta from cratering impacts. |
 | | Its most distinctive features is the Caloris Basin, a colossal, multiringed basin about about 1,350 km (840 miles) in diameter, whose inner floor contains mostly smooth plains, known as Caloris Planitia, but also many ridges and fractures, some of them radial and others arranged in two or three concentric rings. |
 | | There are also great escarpments, up to 1,500 km long and 3 km high, some of which slice through the rings of craters and other features in a way that shows they were formed by compression of the crust when Mercury's interior cooled and shrank. |
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