Tourist Attraction - Ouachita Mountains, Arkansas

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Tourist Attraction - Ouachita Mountains, Arkansas

description

Summary

The sandstone, shale and chert layers are part of a thick pile of sediments that were deformed and uplifted as Gondwanaland collided with the southern edge of ancient North America 280 million years ago.

date_range

Date

2019
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Source

National Parks Gallery
copyright

Copyright info

Public Domain Dedication

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plate tectonics
plate tectonics