New Text book of Geology Designed for Schools And Academies
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In our eReader you can find the full English version of the book. Read New Text book of Geology Designed for Schools And Academies 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 New Text book of Geology Designed for Schools And Academies
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Means of degradation. The principal means of degrada- tion are the following: 1. Erosion by moving waters, either those of the sea or land (pages 90, 107); 2. Erosion by ice, either that of glaciers, icebergs, or ordinary snow and ice FORMATION OF SEDIMENTARY ROCKS. 123 (page 120); 3. Pressure of the water descending into fissures; 4. Forming of substances, for example oxide of iron, in cracks, this tending to open and deepen the cracks ; 5. Growth of rootlets, roots, and trunks of trees, in cr...evices, resulting in opening and tearing apart rocks, and often producing exten- sive destruction of rocks, especially when they are jointed ; 6. Freezing of water in fissures (pa. Ge 115); 7. Chemical decomposition of one or more of the ingredients of a rock, in the course of which process the rock becomes crumbled or reduced to earth ; 8. Kemoval by solution, as of limestones by carbonated waters ; 9. Undermining of rocks by any method ; 10. Expansion and contraction by heat (page 128. ) 3. Formation of deposits The principal methods by which deposits have been formed are the following : 1.
What to read after New Text book of Geology Designed for Schools And Academies?
You can find similar books in the "Read Also" column, or choose other free books by James Dwight Dana to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Means of degradation. The principal means of degrada- tion are the following: 1. Erosion by moving waters, either those of the sea or land (pages 90, 107); 2. Erosion by ice, either that of glaciers, icebergs, or ordinary snow and ice FORMATION OF SEDIMENTARY ROCKS. 123 (page 120); 3. Pressure of the water descending into fissures; 4. Forming of substances, for example oxide of iron, in cracks, this tending to open and deepen the cracks ; 5. Growth of rootlets, roots, and trunks of trees, in cr...evices, resulting in opening and tearing apart rocks, and often producing exten- sive destruction of rocks, especially when they are jointed ; 6. Freezing of water in fissures (pa. Ge 115); 7. Chemical decomposition of one or more of the ingredients of a rock, in the course of which process the rock becomes crumbled or reduced to earth ; 8. Kemoval by solution, as of limestones by carbonated waters ; 9. Undermining of rocks by any method ; 10. Expansion and contraction by heat (page 128. ) 3. Formation of deposits The principal methods by which deposits have been formed are the following : 1.
What to read after New Text book of Geology Designed for Schools And Academies?
You can find similar books in the "Read Also" column, or choose other free books by James Dwight Dana to read onlineMoreLess
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