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Explore the geological history of Vermont through tectonic plate movements, continental drift, and mountain formations from the Grenville supercontinent to the present day. Witness the evolution of landscapes shaped by subduction, orogeny, and the formation of Pangea. Supported by the National Science Foundation and University of Vermont.
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Jens Hilke Landscape Change Project Perkins Geology Museum jhilke@uvm.edu www.uvm.edu/perkins/Landscape/ Index.html supported by National Science Foundation University of Vermont
Credits • "Plate tectonic maps and Continental drift animations by C. R. Scotese,PALEOMAP Project (www.scotese.com)"
Earth’s rigid crust floats on the soft mantle Mantle Crust
NY VT NH GRENVILLESUPERCONTINENT NY VT NH Grenville supercontinent breaks apart
IAPETUS OCEAN NY VT NH PROTO- AMERICA PROTO-EUROPE
IAPETUS OCEAN NY VT NH PROTO- AMERICA PROTO-EUROPE NY VT NH PROTO- AMERICA PROTO-EUROPE Plates reverse direction Subduction creates a chain of island arcs
Island Arcs slam into Proto-American Plate VT NH NY PROTO- AMERICA PROTO-EUROPE Formation of Taconic Mtns (Taconic Orogeny)
VT NH NY PROTO- AMERICA PROTO-EUROPE Acadian Orogeny Formation of the Green Mtns
VT NH NY PROTO- AMERICA PROTO-EUROPE Proto European Plate collides with Proto America • Formation of the White Mtns. (Alleghanian Orogeny) • Champlain Thrust Fault occurs as a result of • these compressional forces
Pangea begins to split apart Forms partial graben in Champlain Valley
Present 570 mya 4.6 bya Phanerozoic Precambrian Present mya 570 mya 458 mya 255 mya 514 mya 425 mya Phanerozoic "Plate tectonic maps and Continental drift animations by C. R. Scotese,PALEOMAP Project (www.scotese.com)"
VT NH NY PROTO- AMERICA PROTO-EUROPE VT NH NY PROTO- AMERICA PROTO-EUROPE