BEDROCK GEOLOGY OF THE ORDOVICIAN CASCO BAY GROUP, HARPSWELL, MAINE
This study involves the detailed mapping of a 9 km2 area just south of Harpswell Center that was previously mapped by Arthur Hussey in his classic study of the bedrock geology of the Orrs Island 7.5’ quadrangle (Hussey, 1971). The field site lies along the western limb of the Harpswell Sound syncline where rocks of the Cushing, Cape Elizabeth, and Spring Point formations have undergone low pressure amphibolite facies metamorphism (staurolite zone). The rocks exposed here provide an excellent opportunity to explore the transition between primarily felsic volcanism in the Cushing Formation, to sedimentation in the Cape Elizabeth Formation. At this transition lies the distinctive Wilson Cove Member of the Cushing Formation – a thin Fe- and sulfide-rich unit previously interpreted to represent a mixture of hydrothermal exhalative and sediment. Finally, above the metasedimentary Cape Elizabeth Formation, a transition back to volcanism is recorded in rocks of the Spring Point Formation.
Major and trace element geochemical studies of all these rocks will provide information on the nature of the protoliths, and insight into their depositional/tectonic environments in Ordovician time. Additionally, structural and petrographic investigation will shed light on the superimposed Devonian-aged Acadian deformation and metamorphism.