Charles G. Spencer grew up in Lee’s Summit, Missouri, and became interested in geology while walking along the railroad tracks near his home, collecting interesting rocks from the gravel ballast. He earned his geology degrees at the University of Missouri–Kansas City, the last being a PhD in Interdisciplinary Studies (Geosciences and Physics) in 1995. He currently works as a consultant, advising residential and commercial clients on environmental and engineering geology issues. He is also an Adjunct Professor of Geosciences at the University of Missouri–Kansas City. Charlie still lives in Lee’s Summit, along with his wife, Shirley, daughter Sarah, their dogs, cats, horse, various domesticated rodents, and a basement full of rocks.
Roadside Geology of Missouri
Paperback
- ISBN-13: 9780878425730
- Publisher: Mountain Press
- Publication date: 03/28/2011
- Pages: 273
- Sales rank: 151,934
- Product dimensions: 6.00(w) x 8.90(h) x 0.70(d)
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The Show-Me State has plenty of geology to show, including the biggest entry room of any cave in North America, the largest lead deposit in the United States, and the only exposures in the Midwest of a large province of 1.48-billion-year-old granite and rhyolite. Geologic history is still being made here, too. In 1811 and 1812, an unprecedented series of magnitude 7 and 8 earthquakes rocked southeast Missouri, liquefying the floodplain sediments and temporarily blocking the flow of the Mississippi River. In Roadside Geology of Missouri, author Charlie Spencer shows you around the state-from the flat, glaciated plains in the north to the knobs of rhyolite in the St. Francois Mountains in the south, and from the earthquake-formed sand boils on the Mississippi floodplain in the southeast to the layers of coal, shale, sandstone, and limestone on the Springfield Plateau and Osage Plains in the west. With this book as your guide, find out where dinosaur fossils have been found in Missouri, why caves and springs seem to pop up nearly everywhere, and which of Missouri's mysterious structures were formed by meteorite impacts.
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