Page 68 - The Restless Earth Fossils
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Finding and excavating Fossils  67


                          Suddenly, the appearance of shells from an ancient sea or giant
                          bones may jolt the finder out of his or her present to contemplate
                          a long and mysterious past. Still, while luck plays a role, finding
                          fossils with regularity and confidence requires a more systematic
                          approach.
                             Geologists  create  color-coded  maps  that  show  exposed  rock
                          layers along with information about rivers, roads, and the topogra-
                          phy, or “lay of the land.” Fossil hunters can find these geological
                          maps produced by the U. S. Geological Survey through the USGS
                          Web site or at local stores catering to hunters, hikers, and climb-
                          ers.  (Maps  are  also  available  through  state  geological  surveys.)
                          In  all  cases,  the  ages  of  rocks  are  color-coded,  so,  for  example,
                          areas with Mesozoic rocks are shown in various shades of green,
                          Cenozoic rocks are yellow, and Paleozoic rocks are purples, blues,
                          and oranges. Curving contour lines give the height of the land
                          above sea level. When the lines are drawn close together, it means
                          the elevation changes quickly, which may indicate ridges and val-
                          leys where erosion may have exposed fossils. Geological maps also
                          contain information about rock orientation, as well as regional
                          gravitational and magnetic forces that might be helpful in plan-
                          ning roads, railroads, and finding important mineral deposits.
                             Learning to read maps, use compasses, and search for pos-
                          sible fossil-bearing sites can be more fun when done as a group
                          project. Many larger communities host rock or geology clubs or
                          amateur paleontology groups. National organizations include the
                          American  Federation  of  Mineralogical  Societies  (AFMS),  which
                          has various regional subgroups. Visiting their Web site will lead
                          you to more local organizations. Some of the paleontology groups
                          open to amateur participation often partner with museums. The
                          Western Interior Paleontological Association (WIPS) works with
                          scientists from the Denver Museum of Nature and Science, for
                          example, and the Paleontological Research Institution (PRI) can
                          be reached through the Museum of the Earth, which is based in
                          Ithaca, New York.
                             Members of local clubs often lead field trips to road cuts,
                          quarries,  mines,  riverbeds,  seashores,  and  other  areas  where








        RE_Fossils2print.indd   67                                                             3/17/09   9:00:10 AM
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