Cooling of this magma would be expected to result in a nearly homogeneous solid moon, covered with the same crust everywhere. This is not always the case. The hemisphere always facing us, called the ...
Around 4.5 billion years ago, the Moon was covered by a global magma ocean. The solidification of the Moon is expected to produce a plagioclase-rich crust. This only appears in the farside of the Moon ...
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