University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1982 Mode of Deglaciation of Shetucket River Basin Black, Robert F. Clebnik, Sherman M. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Black, Robert F. and Clebnik, Sherman M., "Mode of Deglaciation of Shetucket River Basin" (1982). NEIGC Trips. 313. https://scholars.unh.edu/neigc_trips/313 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]. 49 : Q3-1 MODE OF DEGLACIATION OF SHETUCKET RIVER BASIN Robert F. Black, Department of Geology & Geophysics, University of Connecticut, Storrs, CT 06268 Sherman M. Clebnik, Earth and Physical Sciences Department, Eastern Connecticut State College, Willimantic, CT 06226 INTRODUCTION For several decades the concept of stagnation-zone retreat has dominated the thinking of many geologists mapping the glacial deposits of New England. In this concept the margin of the last continental ice sheet covering New England is considered to have retreated northward in small steps wherein the outer zone, generally 1 to 3 km wide, stagnated along the boundary of actively flowing ice. In contrast, basin-by-basin stagnation was proposed recently as a mode of deglaciation in the highlands of Connecticut. In this concept ice in entire drainage basins up to tens of kilometers across stagnated simultaneously when the continental ice thinned sufficiently to cut off resupply of ice to ) the heads of basins.