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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“That we can come here today and in the presence of thousands and tens of thousands of the survivors of the gallant army of Northern Virginia and their descendants, establish such an enduring monument by their hospitable welcome and acclaim, is conclusive proof of the uniting of the sections, and a universal confession that all that was done was well done, that the battle had to be fought, that the sections had to be tried, but that in the end, the result has inured to the common benefit of all.”
—William Howard Taft (1857–1930)
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—Henry David Thoreau (1817–1862)
“Such were the first rude beginnings of a town. They spoke of the practicability of a winter road to the Moosehead Carry, which would not cost much, and would connect them with steam and staging and all the busy world. I almost doubted if the lake would be there,—the self-same lake,—preserve its form and identity, when the shores should be cleared and settled; as if these lakes and streams which explorers report never awaited the advent of the citizen.”
—Henry David Thoreau (1817–1862)
“Most works of art, like most wines, ought to be consumed in the district of their fabrication.”
—Rebecca West (1892–1983)