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QUATERNARY PERIOD                          sea level rose 17 cm (6.7 in.) in the last
                                 PLEISTOCENE           HOLOCENE            ANTHROPOCENE ?    century and will likely rise by much more
                                                                                             in this century (pp. 516–519). Moreover,
                          Meters per million years  300                                      acidifies ocean water
                            400
                                 Erosion rate
                                                                                             increasing atmospheric carbon dioxide
                                                                                             (pp. 446–447, 506), which kills off coral
                            200
                                                                                             reefs (and will even likely dissolve some
                            100
                                                                                             of the geologic strata being formed).
                                                                                                 All these changes—along with the
                              0
                            500  Atmospheric                                                 pollution and habitat disturbance we are
                                                                                             inflicting on Earth’s biotic  communities—
                          Parts per million  300                                             are causing extinctions of animals and
                                 carbon dioxide
                            400
                                                                                             plants (pp. 299–301). If we step back to
                                                                                             view our impacts in deep geologic time,
                            200
                                                                                             motion a rapid new mass extinction event.
                            100                                                              it becomes clear that we are setting in
                              8  Human                                                           Finally, our recent explosion in popu-
                                 population                                                  lation has intensified our impact—changes
                              6                                                              are happening in the blink of an eye,
                          Billions  4                                                        geologically speaking. The entire period
                                                                                             of our society’s existence so far could end
                              2                                                              up represented in as little as a millimeter of
                              0                                                              rock in the future, so the changes we are
                                 15 14 13 12 11 10 9  8  7  6  5  4  3  2  1  0              bringing about now would appear sudden
                                          Thousands of years before present                  to a geologist of the far future.
                                                                                                 Many scientists resist the idea of
                        Figure 1 global soil erosion rates (top) and atmospheric carbon dioxide concentrations
                        (middle) have increased sharply in just the last few hundred years, along with human   renaming our current epoch because they
                        population (bottom). These patterns have persuaded some geologists that we should   question whether the proposal holds true
                        recognize a new epoch in Earth history and call it the Anthropocene. Adapted from Zalasiewicz,   to the tradition of defining time periods   CHAPTER 2 •  E ART h’s Physi CAL
                        J., et al., 2008. Are we now living in the Anthropocene? GSA Today 18(2), 4–8, Figure 1.  based on changes actually seen in the
                                                                                             geologic record. But supporters of the
                            As greenhouse gas concentra-   century (p. 514). Rising temperatures are   idea maintain that today’s changes will be
                        tions rise, so does temperature. Earth’s   melting polar ice. The influx of meltwater   readily visible in future stratigraphy and
                        temperature has risen 0.7 °C (1.3 °F) in   into the oceans,  combined with the fact   that we should recognize this unprece-
                        the past century and is predicted to rise   that warmed water expands in volume,   dented time of rapid change in Earth’s his-
                        by 1.8–4.0 °C (3.2–7.2 °F) in the current   means that sea level is rising. Global   tory by designating it the Anthropocene.



                          FAQ        Technically speaking, is coal a rock?


                          Coal is a geologic resource of great importance in environ-  Geologic and Natural Hazards
                          mental science, but many people are unsure of what coal is or                                           s ys TE m s:  mATTER , E NER gy,  AN d
                          where it comes from. Coal is hard and is found underground,   Plate tectonics gives rise to creative forces that shape our
                          like many types of rocks, so some people would classify it as   planet—yet some of the consequences of tectonic movement
                          a rock. Others, however, argue coal is not a rock because   can  also  pose  hazards  to  us.  Earthquakes  and  volcanoes  are
                          it is the modified remains of organic material, mostly woody   examples of geologic hazards. We can see how such hazards
                          plants, from hundreds of millions of years ago.    relate to tectonic processes by examining a map of the cir-
                              According to geologists, coal is a rock because it is a   cum-Pacific belt, or “ring of fire” (Figure 2.20). Nine out of 10
                          solid aggregation of minerals, particularly carbon. Carbon   earthquakes and over half the world’s volcanoes occur along
                          is classified as a mineral because it is a naturally occurring   this 40,000-km (25,000-mi) arc of subduction zones and fault   gE o L ogy
                          solid element with a crystalline structure. Other rocks, such as   systems. Like many locations along the circum-Pacific belt,
                          some types of limestone, also contain the remains of ancient   Japan has experienced earthquakes and volcanism frequently
                          organisms (such as the shells of marine organisms) and are   in its past. As a result, it had put  precautions in place for such
                          categorized with coal as organic sedimentary rocks.  dangers.                                           57







           M02_WITH7428_05_SE_C02.indd   57                                                                                     12/12/14   2:53 PM
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