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Source: GEOTECHNICAL ENGINEERING
               2                Igneous Rocks, Ultimate Sources for Soils
























                2.1   GEOLOGY AND THE GEOLOGICAL CYCLE


                                    2.1.1   Knowing the Materials
                                    Regardless of the field of specialization, an engineer should know and
                                    understand the materials with which he or she will be working. Naturally
                                    occurring soils and rocks are complex, and an appreciation of their particular
                                    properties can be critical to the success of a project. Formal course work in
                                    geology therefore is a prerequisite to the study of geotechnical engineering. The
                                    purpose of these introductory chapters is to serve as a reminder and to add
                                    emphasis to points that are most relevant in engineering. Students also are
                                    urged to re-read their basic text in physical geology. Large or complicated
                                    projects usually utilize the services of one or more professional engineering
                                    geologists.

                                    2.1.2   Igneous Rocks as Primordial Sources for Soils

                                    As shown in Fig. 2.1, the originating sources for soils are igneous rocks, that is,
                                    rocks that have solidified from molten material, or magma. Although most
                                    igneous activity occurred in past geological eras, active volcanoes are evidence
                                    that such activity continues, being concentrated along weaker zones of the
                                    Earth’s crust at plate margins.


                                    2.1.3   Weathering, Saprolite, and Residual Soils
                                    The conversion of rock to soil involves physical and chemical processes of
                                    weathering. Generally, the farther a rock is removed from its nascent envi-
                                    ronment, the more vulnerable it is to changes in the environment. Thus, a rock
                                    that has formed under extremes of heat and pressure will be relatively immune


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