Everything about The Grenville Orogeny totally explained
The
Grenville orogeny was an episode of mountain-building (
orogeny) associated with the assembly of the ancient
supercontinent Rodinia. The Grenville orogeny occurred in the late
Proterozoic eon, 1300-1000 million years ago (mya), as numerous
continental plates collided around the edges of
North America, forming folded mountains.
In a narrow sense, the Grenville orogeny refers to the mountain ranges formed in western Europe and eastern North America, from
Scotland southwest to
Newfoundland and extending to northern Georgia, 1100-1000 mya.
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