|
|
|
|
Grenville orogeny
|
| |
|
| |
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, 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 million years ago.

Discussion
Ask a question about 'Grenville orogeny'
Start a new discussion about 'Grenville orogeny'
Answer questions from other users
|
Encyclopedia
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, 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 million years ago.
See also
|
| |
|
|