Page 75 - Geotechnical Engineering Soil and Foundation Principles and Practice
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Soils That Are Sediments
                70   Geotechnical Engineering

                                    4.4.4   Beaches and Strandlines
                                    The extent of depression of the earth’s crust is indicated by the inclination of
                                    uplifted beaches that originally were level. Such beaches are called strandlines.
                                    Strandlines bordering Hudson Bay, the Great Lakes, and the Baltic Sea now are
                                    tilted in directions consistent with a hypothesis of crustal rebound. The directions
                                    of bedrock striations indicate that the Hudson Bay area was at the center of the
                                    Laurentide ice sheet, and measurements and dating of strandlines show that the
                                    Gulf of Bothnia in the northern part of the Baltic Sea is rising at a rate of about
                                    1 cm (0.5 in.) per year.

                                    Tilted strandlines also indicate rebound around Great Salt Lake as the lake level
                                    lowered as a result of desiccation. The ancestral lake, known as Lake Bonneville,
                                    was about 330 m (1000 ft) higher during the Pleistocene, and the land has risen
                                    about 70 m (230 ft).



                                    4.4.5   Mechanics of Glacial Sliding
                                    Rock debris concentrated in basal ice is a kind of ‘‘glacial sandpaper.’’ The
                                    drag marks, deep longitudinal gouges left in bedrock, are called striations.
                                    Nevertheless the overall frictional resistance to sliding had to be low to carry
                                    the ice for such long distances with a low slope angle, and must have been aided
                                    by pressure-melting of ice at the bottom of the glacier. This would transfer
                                    the weight to liquid water trapped between the ice and the soil, thereby creating
                                    a positive pore-water pressure sufficient to support the ice. A similar decrease
                                    in friction from positive pore-water pressures also plays an important role in
                                    landslides.



                                    4.4.6   Life in the Pleistocene
                                    The time of glaciation is referred to as the Pleistocene epoch of the Cenozoic
                                    (recent life) era, and extended from about 2.5 million to 10,000 years ago.
                                    Subarctic cold and a generous food supply led to many experimental models of
                                    cats, cave bears, sloths, mammoths, and mastodons. A few mammoths survived in
                                    miniature on islands off the northern coast of Siberia almost into historical times,
                                    5000 years ago. Mammoths found in permanently frozen ground, or permafrost,
                                    yield frozen tissues that are being studied for their DNA.

                                    The early Pleistocene saw the emergence of man, who now probably would be
                                    referred to as intellectually challenged. The stocky and large-brained Neanderthal
                                    man appeared about 100,000 years ago, and the taller and equally large-brained
                                    Cro-Magnon man first appeared about 35,000 ybp (years before present) and
                                    threw his weight around. Modern man is Cro-Magnon with shoes and a haircut.




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