Northern Highland Lake District
The Northern Highland Lake District consists of an array of lakes. "This geological province is characterized by primarily Precambrian bedrock capped by a thin layer of sedimentary rocks left by the Paleozoic seas. On top of this are glacial deposits left by the Woodfordian and Valderan substages of the Wisconsin glaciers. The soils are infertile glacial outwash with reduced cation exchange capacity, leaving them susceptible to acidification and bog formation. As the Valderian glaciation (ca. 12,000 years ago) receded, the kettle basins of Paul, Peter, and Tuesday Lakes arose from the melting of blocks of ice in the glacial drift."
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