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The specific factors model was developed by
Isostatic Rebound
The rise of land masses that were depressed by the weight of ice sheets during glaciation, occurring as the ice melts and the land slowly returns to its original elevation.
Metamorphic Rocks
Rocks that have been transformed by heat, pressure, or chemically active fluids, altering their original composition or structure.
Plutonic Rocks
Intrusive igneous rocks that crystallize deep underground from magma, such as granite and diorite.
Continental Crust
The relatively thick part of the Earth's crust that forms the large landmasses. It is generally older, less dense, and composed mainly of granite.
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