Forest River – Field Trip
The landscape of the North Shore is the product of differential weathering and erosion of a brittly deformed igneous terrain followed by glacial scouring and deposition. Irregular basins and straight valleys, developed along faults and fracture zones. Knobby highlands and ridges are of rock less fractured. Forest River Park is characterized by this knock-and-lochan topography, a galic term ... ................
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