TRANSCENDENTAL GEOLOGY: HENRY DAVID THOREAU ON THE MOUNTAINS, ROCKS, AND WATERS OF NEW ENGLAND
Thoreau spent the greater part of his life within walking distance of his birthplace in Concord, MA, and established his place in American literary history with a two-year sojourn on the shores of Walden Pond, a large glacial kettle pond near the southeastern border of the town. He accurately surveyed and sounded this bottomless pond in 1846. In sauntering and boating about Concord and the surrounding country, he described many geologic features, including the Fairhaven Cliffs, Brister's Spring, the Deep Cut with its sand foliage, and the limestone quarry and kiln in the swampy Estabrook Woods.
Though Concord was a constant source of inspiration, Thoreau also took many excursions throughout New England. Among those chronicled in his writings were a week-long boat trip on the Concord and Merrimack Rivers (culminating with an ascent of Mt. Washington) and later trips to Cape Cod, Mt. Wachusett, Mt. Greylock, Mt. Monadnock, the White Mountains, and the Maine Woods. His classic Cape Cod abounds in observations on beach processes and shoreline erosion. Mountains stimulated some of Thoreau's best geological work. He described what we now recognize as glacial striations and roches moutinees on Mt. Monadnock; noted the lithologic character of the rhyolite (hornstone) on Mt. Kineo; and elaborated on the physiography of Mts. Greylock, Kineo, Katahdin, and Washington.
Thoreau was well acquainted with the geological literature of his day, frequently referring to the reports of Edward Hitchcock and Charles T. Jackson. Though he early on read Charles Lyell's Principles of Geology and absorbed its uniformitarianism, he inexplicably ignored the ideas of Louis Agassiz on continental glaciation. Science was secondaryeven somewhat suspectto Thoreau. His greatest intellectual achievement was his recognition of the physical and spiritual relationships inherent in all natural phenomena.