By Robert N. Oldale1, James V. O'connor2, Brian B. Tormey3, And
A GEOLOGIC OVERVIEW OF CAPE COD AND A GEOLOGIC TRANSECT OF WELLFLEET FROM THE ATLANTIC OCEAN TO CAPE COD BAY by Robert N. oldale1, James V. O'Connor2, Brian B. Tormey3 , and Richard 8. Williams, Jr. 1 U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 93-618 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature Hj.S. Geological Survey, Woods Hole, MA 02543 2University of the District of Columbia, Washington, D.C. 20008 Pennsylvania State University, Altoona, PA 16601 A GEOLOGIC OVERVIEW OF CAPE COD AND A GEOLOGIC TRANSECT OF WELLFLEET FROM THE ATLANTIC OCEAN TO CAPE COD BAY by Robert N. Oldale, James V. O 1 Connor, Brian B. Tormey, and Richard S. Williams, Jr. INTRODUCTION This field trip guide is for the October 30, 1993 NAGT field trip EVOLUTION OF CAPE LANDSCAPES: MARINE AND GLACIAL FIELD TECHNIQUES APPLIED TO CAPE COD to be conducted in association with the Geological Society of America 1993 Annual Meeting at Boston, Massachusetts. The guide is based, in part, on two previous Cape Cod field trip guides (Oldale, 1988; Oldale, 1992a). Although the complete geologic history of Cape Cod spans more than 600 million years, the Cape Cod we will view today has a much shorter history. This history encompasses the last glacial stage of the ice age, the Wisconsin, and the present interglacial stage, the Holocene. The Cape was initially shaped by the Laurentide ice sheet, which formed in Canada about 75,000 years ago. For much of its existence, the ice sheet remained north of New England.
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