mathematics & science center go to website then click on virginia physiography

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Page 1: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

MATHEMATICS & SCIENCE CENTERMATHEMATICS & SCIENCE CENTER

Page 2: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Go to website

http://arcims.mathsciencecenter.infoThen click on Virginia Physiography

Page 3: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 4: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 5: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 6: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 7: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Virginia Division of Mineral Resources

Page 8: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 9: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of USGS

Page 10: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

THE COASTAL PLAIN

• A region of sedimentary strata consisting of sands, muds, and gravels

• Tidal waters occupy not only the Chesapeake Bay, but also lower portions of the James, York, Rappahannock and Potomac rivers

• Extends inland for more than 100 miles and is monotonously flat

Page 11: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 12: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 13: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 14: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 15: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Virginia Division of Mineral Resources

Page 16: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 17: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Carroll Ellis, Physical Geology, 2003

Page 18: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Carroll Ellis, Physical Geology, 2003

Page 19: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 20: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 21: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 22: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 23: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 24: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 25: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

THE PIEDMONT

• Largest province extending from the Fall Line westward to the Blue Ridge Mountains

• Comprised of a complex of metamorphic and igneous rocks, overlain in a few places by Triassic-age sedimentary beds

• Important rocks and minerals include pegmatites, slate, kyanite, gold and pyrite

Page 26: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 27: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 28: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Virginia Division of Mineral Resources

Page 29: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 30: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 31: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

1998 Geology Summer Field School – Radford University

Page 32: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 33: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

The Blue Ridge Mountain

• A long narrow, northeast-southwest trending mountain chain

• Consists of old Precambrian-age sedimentary and volcanic rocks

• Old Rag Granite is the oldest rock unit dated in Virginia at 1.2 billion years

• The two highest mountains in the state, Mt Rogers (elevation 5,719 ft.) and White Top (elevation 5,520 ft.) are both in the southern Blue Ridge

Page 34: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 35: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 36: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Virginia Division of Mineral Resources

Page 37: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

http://www.goodearthgraphics.com

Page 38: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 39: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 40: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

The Valley and Ridge

• Composed of folded and faulted 550 to 300 million-year-old sedimentary rocks

• Most ridges are held up by resistant sandstone, and most valleys are underlain by less resistant shale, limestone, and dolostone

• Karst features, such as caves and sinkholes are common throughout this province

Page 41: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 42: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Virginia Division of Mineral Resources

Page 43: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography
Page 44: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

Courtesy of Virginia Division of Mineral Resources

Page 45: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography

The Appalachian Plateau

• Contains deep narrow valleys and steep, rugged mountain sides caused by downcutting by streams

• Consists of 320 to 280 million-year-old sandstone and shale with coalbeds

• Most of the rock layers are relatively flat-lying• Coal is Virginia’s most important mineral

resource

Page 46: MATHEMATICS & SCIENCE CENTER Go to website  Then click on Virginia Physiography