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Special Problems with Sedimentary Rocks
                58   Geotechnical Engineering

                 Figure 3.9
                 The Black Hills
                 area of South
                 Dakota is a
                 classic dome
                 that illustrates
                 many geological
                 relationships
                 including
                 hogbacks,
                 metamorphic rock
                 close to a granite
                 intrusion, and
                 escalation of
                 erosion from uplift.
                 The width of the
                 dome is about
                 70 km (45 miles).
                 (USGS
                 Guidebook 25, Int.
                 Geol. Congress,
                 1933.)



                                    Further Reading
                                    Jackson, Donald D. (1982). Underground Worlds. Time-Life Books, Alexandria, Va.
                                    Jackson, Julia A., ed. (1997). Glossary of Geology, 4th ed. American Geological Institute,
                                        Alexandria, Va.
                                    Kehew, Alan E. (1995). Geology for Engineers and Environmental Scientists, 2nd ed.
                                        Prentice-Hall, Englewood Cliffs, N.J.
                                    Martinez, J. D., Johnson, K. S., and Neal, J. T. ( 1997). ‘‘Sinkholes in Evaporite Rocks.’’
                                        American Scientist, 86(1), 38–51.
                                    Miller, Russell (1983). Continents in Collision. Time-Life Books, Alexandria, Va.
                                    Way, Douglas S., and Everett, John R. (1997). Ch. 3, ‘‘Landforms and Geology,’’ in
                                        Manual of Photographic Interpretation, 2nd ed. American Society for Photogrammetry
                                        and Remote Sensing, Bethesda, Md.
















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