thrust fault oor Masedonies
thrust fault
en
(geology) A type of fault, with movement of the Earth's crust, in which a lower stratigraphic layer is pushed up and over a younger one as a result of compression forces.
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The Lunar Reconnaissance Orbiter discovered that similar small thrust faults exist on the Moon.
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As Mercury's interior cooled, it contracted and its surface began to deform, creating wrinkle ridges and lobate scarps associated with thrust faults.
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Small-scale thrust fault scarps have been found, tens of meters in height and with lengths in the range of a few km, that appear to be less than 50 million years old, indicating that compression of the interior and consequent surface geological activity continue to the present.
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3 sinne gevind in 2 ms. Hulle kom uit baie bronne en word nie nagegaan nie.