Why Are the Appalachian Mountains So High? John Cipar, PhD Weston Observatory Boston College April 16, 2014 1 Adirondacks from Mt. Marcy, NY Steep Topography (30 m at Lake Champlain) High elevation (1630 m at summit) Photo by Jef Renaud Old Rocks from deep crust (1200 Ma Anorthosite, crystallized at 15-20 depth) 2 Eastern North America Topography Canadian Shield Adirondacks Northern Appalachians Catskills Alleghany Plateau Central Appalachians Blue Ridge Southern Appalachians Coastal Plain From Geological History of Jamestown, Rhode Island web site 3 Earth’s Interior • Pressure at center is 350 Gpa (3,500,00 atmospheres) UC Berkeley Seismo Lab • Temperature at center: 5430 ⁰C (9800 ⁰F) 4 Continents v. Oceans Continental crust • Light granite: “floats” on surface • Formed by continental collision • Old (4000 My) to very young 30-50 km Oceanic crust • Heavy basalt: subducts into mantle • Formed at mid-ocean ridges • Young <185 My to right now! Rigid & elastic PhysicalGeography.net 5 Plate Tectonics • Continental Drift was first proposed by Alfred Wegner in 1912 • Strong geological evidence for drift, but no physical mechanism for moving the continents through the oceans • Modern theory of sea floor spreading /Plate Tectonics developed in 1950s 1970s US Geological Survey 6 Plate Map 2011 Tohoku, Japan earthquake Boston 2004 Sumatra earthquake Earth’s Dynamic Systems /W. Kenneth Hamblin and Eric H. Christiansen 7 Plate Boundaries 8 Hawaiian Hot Spot May 30, 2011 9 Subduction zones Earth’s Dynamic Systems /W. Kenneth Hamblin and Eric H. Christiansen 10 Wilson cycle Lynn S. Fichter/James Madison University 11 Building the Appalachians: Precambrian to Paleozoic 12 Geology of North America 13 Geologic Map of Eastern North America USGS 14 “Suspect” Terranes Hibbard et al, 2006 15 Rodinia - 700 My Laurentia Paul Hoffman, Science, v. 252, p. 1409 16 Passive Margin Early Cambrian - 550 My Laurentia (North America) Iapetus Ocean Amazonia (South America) • Maps from Ron Blakely • Cross-sections from Virginia Geology web site and USGS 17 Taconic Orogeny Ordovician - 450 My Ron Blakely and USGS Boston 18 Acadian Orogeny Devonian - 385 My Ron Blakely and USGS 19 Alleghany Orogeny Pennsylvanian & Permian - 290 My North America The Paleozoic Appalachians were probably similar to today’s Himalaya Mountains Boston Africa Ron Blakely and USGS 20 Rifting of Pangaea Triassic - 195 My North America Africa Ron Blakely and JMU 21 Triassic rifting: Opening of the Atlantic ~200 My ~185My Earth’s Dynamic Systems /W. Kenneth Hamblin and Eric H. Christiansen 22 “How many years can a mountain exist Before it's washed to the sea?” - Bob Dylan, Blowin’ in the Wind 23 The Last 200 My • Eastern North America is a “passive” margin – Sedimentation along the Atlantic coast – Far from active plate boundaries • Passage over the Great Meteor hotspot 12590 My Unsolved question is the persistence of high Appalachian topography to the present 24 Great Meteor Hotspot Track 125 My White Mountains 125-100 My 105 My 85 My McHone, 1996 Hot spot in New England 125-100 My 25 North America 115 My ago Greenland North America Great Meteor hotspot Farallon plate Atlantic Ocean Map by Ron Blakely 26 Evidence for Hotspot Uplift Devonian sediments are truncated Crough, 1981 27 Thermochronology Apatite grain w/tracks Apatite fission track (AFT) ages tell when a rock cooled through approximately 100 °C, or about 4-5 km depth. Assumed geothermal gradient converts temperature to depth 28 New England AFT ages 125-178 My ~70-125 My 125-178 My Roden-Tice and Tice, 2005 29 Offshore sediments 30 Sediment Supply to Atlantic Basins Pulse in sedimentation (& uplift?) ~15 My 31 Seismic structure of the Earth Stephen A. Nelson, Tulane University 32 S-wave velocities in New England Slow S-wave ≡ high T Li et al (2002) Remnant of Great Meteor hot spot ? 33 Structure of North American mantle constrained by simultaneous inversion of multiple‐frequency SH, SS, and Love waves Tian, Yue, Ying Zhou, Karin Sigloch, Guust Nolet, and Gabi Laske (2011) Map view Cross-section Slow S –wave velocity in NH & VT Journal of Geophysical Research: Solid Earth Volume 116, Issue B2, B02307, 15 FEB 2011 DOI: 10.1029/2010JB007704 http://onlinelibrary.wiley.com/doi/10.1029/2010JB007704/full#jgrb16621-fig-0013 Farallon plate beneath North America eastern US High S velocity = • low temp • high density 35 IRIS Earthscope TA Stations Incorporated Research Institutions in Seismology 36 The “Great” Unconformity near Alexandria Bay, NY 540 My 1100 My ~560 My Chris Murray, Thousand Islands Life web site 37 Saga of the Potsdam sandstone 38 Questions? 39 Further Reading • Mountain Press Roadside Geology Series – Fr. James Skehan, S.J.: MA and CT/RI • USGS Geology of the New York City Region – http://3dparks.wr.usgs.gov/nyc/index.html • Geological Evolution of Virginia and the Mid-Atlantic Region – Lynn S. Fichter/James Madison University – http://csmres.jmu.edu/geollab/vageol/vahist/ • Geological History of Jamestown, Rhode Island – http://www.jamestown-ri.info/northern_appalachians.htm • PhysicalGeography.net – http://www.physicalgeography.net/ • Ron Blakely Paleogeographic Maps – http://cpgeosystems.com/paleomaps.html 40 Bibliography Crough, S.T. (1979). Hotspot epeirogeny, Tectonophysics, vol. 61, pp. 321-333. Crough, S. Thomas (1981). Mesozoic hotspot epeirogeny in eastern North America, Geology, v. 9, pp. 2-6. Duncan, R. A. (1984). Age Progressive Volcanism in the New England Seamounts and the Opening of the Central Atlantic Ocean, J. Geophys. Res., 89(B12), 9980– 9990, doi:10.1029/JB089iB12p09980. Ehlers, Todd A. and Kenneth A. Farley (2003). 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