WebCLINTON - NEWBURY FAULT ZONE SOmb SOme Sap O ba Obb Obba Obba Sab Sam O b Obg Oba Obg 500 ft sea level-500 ft-1000 ft-1500 ft-2000 ft Johnsons Pond N A S H O B A T E R R A N E M E R R I M A C K B E L T Cited References Lyons, J.B., Bothner, W.A., Moench, R.H., and Thompson, J.B. Jr., 1997: Bedrock geologic map of New F i s h B r o … WebRegionally, the Clinton-Newbury fault is a terrane boundary between the Merimack belt to the west and the Nashoba block to the east (Zen, 1983). Goldsmith (1991) states that the …
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WebUniversity of New Hampshire Scholars' Repository University of New ... WebThe bedrock geology of the 7.5-minute Worcester South quadrangle, Massachusetts, consists of deformed Neoproterozoic to Paleozoic crystalline metamorphic and intrusive … honda accord bekas dijual
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WebThese features are typically not included on bedrock geologic maps but are included here because of their potential importance to groundwater. Outcrop scale faults are most numerous in outcrops near the Clinton-Newbury fault zone, and have dips either greater than 60° or less than 30°. The shallowly dipping faults (dips < The early history of Massachusetts can be traced to around 1.2 to 1.1 billion years ago in the Mesoproterozoic Era of the Precambrian with some of the oldest rocks in the state situated in the Berkshires. What is now the western edge of the state was at the time the continental margin of the proto-North American continent Laurentia. The Grenville orogeny significantly altered many rocks thro… WebMylonites along the Silver Hill-Wekepeke Fault (Robinson, 1981), bounding the western edge of the NSB, show east-side-down normal motion and west-side down normal motion along the Clinton-Newbury Fault Zone (CNFZ; Goldstein, 1994) which bounds the NSB’s southeastern margin. honda accord bekas jakarta olx