University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1987 Southwest-Trending Striations in the Green Mountains, Central Vermont Ackerly, Spafford C. Larsen, Frederick D. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Ackerly, Spafford C. and Larsen, Frederick D., "Southwest-Trending Striations in the Green Mountains, Central Vermont" (1987). NEIGC Trips. 423. https://scholars.unh.edu/neigc_trips/423 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact
[email protected]. c SOUTHWEST-TRENDING STRIATIONS IN THE GREEN MOUNTAINS, CENTRAL VERMONT Spafford C. Ackerly Department of Geological Sciences, Cornell University Ithaca, New York 14853 Frederick D. Larsen Department of Earth Sciences, Norwich University Northfield, Vermont 05663 "That the highest points of land should have been scored by abrasions passing over them seemed to the older geologists better explained by floating than by glacial ice; for no one had then made clear how ice could move up hill to altitudes of thousands of feet. The ice of living glaciers moves down slopes: how then could the ancient ice have passed over the tops of the mountains unless the land itself had been so low that icebergs could have floated over them? The geologists had the credit of believing many strange stories, but even they hesitated to accept the doctrine that land ice could have been pushed over New England from the St.