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stages that have been documented for the Pleistocene epoch? The first question deals with long-
                  term trends in temperature on a scale of millions of years, but this second question relates to
                  much shorter-term changes.
                         Although  the  literature  of  science  contains  many  hypotheses  relating  to  the  possible
                  causes  of  glacial  periods,  probably  the  most  attractive  proposal  for  explaining  the  fact  that
                  extensive glaciations have occurred only a few times in the geologic past comes from the theory
                  of plate tectonics.
                         Because glaciers can form only on land, we know that landmasses must exist somewhere
                  in the higher latitudes before an ice age can commence. Many scientists suggest that ice ages
                  have occurred only when Earth’s shifting crustal plates have carried the continents from tropical
                  latitudes to more poleward positions.
                         Today scientists understand that the areas containing these ancient glacial features were
                  joined together as a single supercontinent (Pangaea) located at latitudes far to the south of their
                  present positions. Later this  landmass  broke apart, and  its pieces, each  moving on a different
                  plate, migrated toward their present locations. Now we know that during the geologic past, plate
                  movements accounted for many dramatic climatic changes as landmasses shifted in relation to
                  one  another  and  moved  to  different  latitudinal  positions.  Changes  in  oceanic  circulation  also
                  must have occurred, altering the transport of heat and moisture and consequently the climate too.
                  Because  the  rate  of  plate  movement  is  very  slow—a  few  centimetres  per  year—appreciable
                  changes in the positions of the continents occur only over great spans of geologic time. Thus,
                  climate changes brought about by shifting plates are extremely gradual and happen on a scale of
                  millions of years.

                         Task  2.  Look  at  Figure  8.1.  A  shows  the  supercontinent  Pangaea  with  the  area
                  covered  by  glacial  ice  about  300  million  years  ago.  B  shows  the  continents  as  they  are
                  today. The white areas indicate where evidence of the old ice sheets exists. Using the figure
                  and the information from the text talk about  the theory of plate tectonics as one of the
                  popular hypotheses relating to the possible causes of glacial periods.

                         Task 3. Build up a glossary to the most important terms used in the text.

                         Task 4. Answer the questions:
                    1. What is the name of earlier glaciations?
                    2. When were two Precambrian glacial episodes identified in the geologic record?

                         Task 5.  Give a  short  report about some other hypotheses  relating to the possible
                  causes of glacial periods, for example, variations in Earth’s orbit.

                                                          TEST YOURSELF

                         Task 1. Tell whether the sentences are true or false. Correct the false ones.
                    1. A reservoir rock is a rock that can both store and transmit fluids.
                    2. Saturation is the percent volume of the rock that is not occupied by solids.
                    3. Porosimeter is a cylinder of rock that is drilled from the well.
                    4. Porosity cutoff is a minimum porosity value.
                    5. Permeability is measured in units of darcys (D) or millidarcys.
                    6. Porosity and permeability in a single sedimentary rock layer are not related.
                    7. Oil field brine is very salty water that shared the pores with the oil.
                    8. Sandstones usually have water in the center of the pore, and oil is on the outside of the pore
                       in contact with the sand grains.
                    9. Earlier glaciations are indicated by a sedimentary rock formed when glacial till becomes
                       lithified.
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