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The uplift of the Adirondack region primarily occurred during the Late Proterozoic to Early Paleozoic eras, roughly between 1.1 billion and 500 million years ago. This geological activity was part of the Grenville Orogeny, a significant mountain-building event caused by tectonic forces. Subsequent erosion has shaped the region into its current form, characterized by its rugged terrain and numerous lakes.

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2w ago

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