Handbook for Field Geologists
Handbook for Field Geologists
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In our eReader you can find the full English version of the book. Read Handbook for Field Geologists Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Handbook for Field Geologists
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To quickly assess the difficulty of the text, read a short excerpt:
Note the character of the secondary minerals when possible and illus- trate by specimens.
Decomposition. The destruction of an igneous rock is usually accomplished by deep-seated chemical action or by the domi- nantly mechanical processes of weathering near or at the surface. In the former case the special characters of a given rock may be changed by the work of circulating waters. Certain com- ponents may be removed and others brought in. Thus rocks of different primary character may be brough...t to resemble each other and even the distinctive properties of an igneous mass may disappear, as in extreme silicification or kaolinization. Such alteration is usually so localized that the geologist may IGNEOUS ROCKS 93 observe various stages, even perhaps to the fresh rock, and by obtaining suitable specimens afford means for an interesting study. Consider especially the relation of such decomposition to ore deposition.
Study the surface decay of rocks with relation to the process of weathering, the formation of soil, the mechanical destruction of the exposed mass, and the deposition of detritus.
What to read after Handbook for Field Geologists?
You can find similar books in the "Read Also" column, or choose other free books by C W Charles Willard Hayes to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Note the character of the secondary minerals when possible and illus- trate by specimens.
Decomposition. The destruction of an igneous rock is usually accomplished by deep-seated chemical action or by the domi- nantly mechanical processes of weathering near or at the surface. In the former case the special characters of a given rock may be changed by the work of circulating waters. Certain com- ponents may be removed and others brought in. Thus rocks of different primary character may be brough...t to resemble each other and even the distinctive properties of an igneous mass may disappear, as in extreme silicification or kaolinization. Such alteration is usually so localized that the geologist may IGNEOUS ROCKS 93 observe various stages, even perhaps to the fresh rock, and by obtaining suitable specimens afford means for an interesting study. Consider especially the relation of such decomposition to ore deposition.
Study the surface decay of rocks with relation to the process of weathering, the formation of soil, the mechanical destruction of the exposed mass, and the deposition of detritus.
What to read after Handbook for Field Geologists?
You can find similar books in the "Read Also" column, or choose other free books by C W Charles Willard Hayes to read onlineMoreLess
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