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Geology 101 Notes

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Geology 101 Notes
Geology 101

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Examples of Time & Geology * Sphinx
Precambrian Era: (4.5 billion) * Ended 542 million years ago * Started with no life and evolved bacteria & algae
Paleozoic Era: (542 – 251 MYBP) * Fish, amphibians, etc. were early years * Ended with the Greatest Extinction of all time
Mesozoic Era: (251 – 65 MYBP * Dinosaurs ruled and small animals developed in end * Ended with asteroid in Yucatan
Cenozoic Era: (65 – now MYBP) * Rise of mammals and Great Glaciations * Holocene = Rise of Man (last 15k years) Natural Resources * Most resources are: limited in quantity and non-renewable
Earth’s Systems * Atmosphere * Hydrosphere * Biosphere * Geosphere
Earth’s Heat Engines * External * Energy form the sun * Internal * Energy from radioactive decay
Earth’s Interior * Crust * Thin outer rocky shell (solid) * Variable thickness * Mantle * Hot solid * Special “plastic” zone * Fe, Mg, and Si rich minerals * Core * Outer Core * Liquid, mostly iron * Inner Core * Solid, mostly iron
Rock vs. Minerals * A mineral is a crystalline solid and is formed by natural geological processes * Has a specific chemical composition * Has consistent physical and chemical properties * A crystal is a mineral with shape properties * A rock is a composite of one or more minerals
Atoms and Elements * Elements * Substances not divided by chemical reactions * “Periodic Table” listing * Atoms * Smallest unit with properties of element * Composed of 3 types of subatomic particles: protons, neutrons, and electrons * Molecules * Combination of atom’s Atomic structure * Nucleus * Most of the atom’s mass * Electrons * Tiny fraction of atom’s mass * Chemical vs. Nuclear reactions *

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    Bantam Dell Publishing Group, Inc. New York.<br><li>Magaritz, M., Bar, R., Baud, A. and Holser, W.T., 1988, The carbon-isotope shift at the Permian/Triassic boundary in the southern Alps is gradual, Nature, 331 (6154): 337-339.<br><li>Maxwell W. Desmond., 1989, The End Permian Mass Extinction, New York, Columbia University Press. 182-170 p.<br><li>Maxwell, W.D. and Benton, M.J., 1987, Mass extinctions and data bases: changes in the interpretation of tetrapod mass extinction over the past 20 years. In P.J. Currie and E.H. Koster (eds), 4th Symposium on Mesozoic Terrestrial Ecosystems, Occasional Paper of the Tyrrell Museum of Palaeontology, Alberta, 3: 156-160.<br><li>Monastersky, R. 1993. Sudden death decimated ancient oceans. Science News, vol 146. p.38<br><li>Monastersky, R. 1997. Life 's closest call: what caused the spectacular extinctions at the end of the Permian period? Science News, vol. 151. p.74-75.<br><li>McKinney, M.L., 1987, Taxonomic selectivity and continuos variation in mass and background extinctions of marine taxa, Nature, 325 (6100):143-145.<br><li>Newell, N.D., 1963, Crises in the history of life, Scientific American, 208 (2): 76-92.<br><li>Schopf, T.J.M., 1974, Permo-Triassic extinction: relation to sea-floor spreading, Journal of Geology. 82 (2): 129-143.<br><li>Raup, D.M., 1979, Size of the Permo-Triassic bottleneck and its evolutionary implications, Science, 206 (4415): 217-218.<br><li>Renne, Paul., Zichao, Zhang., Richards, Mark., Black, Michael., and Basu, Asish. 1995. Synchrony and Causal Relations Between Permian-triassic Boundary Crises and Siberian Flood Volcanism. Science, vole 269. p. 1413-1416.<br><li>Stepkoski, J.J., Jr. 1986, Phanerozoic overview of mass extinctions. In D.M. Raup and D. Jabloknski (eds), Patters and processes in the history of life, Springer-Verlag, Berlin: 277-95.<br><li>Sweet, W.C., 1992. A conodont-based high resolution biostratigraphy for the Permo-Triassic boundary interval.…

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