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Their forms, structures and inter-relationships (Structural Geology); the geological processes or machinery of the earth, by means of which changes of all kinds are brought about (Physical Geology); and finally the succession of these changes in time, or the history of the earth (Historical Geology). (Holmes, 1944: 5; 1965: 9–10) Comp. 1 Holmes’ Figure 1 from his Principles of Physical Geology (1945: 4; 1965: 9). Within physical geology, the central subject of his book, he included geomorphology, oceanography, meteorology, and climatology.

A theory or solution also encounters internal theoretical difficulties if it embodies an inconsistency. Here is an example. Fixists raised such a difficulty with Wegener’s explanation of mountain building, arguing that it was not only inconsistent with itself but also with other solutions that he offered in his overall theory. Wegener claimed that continents plow through seafloor, sima (rock rich in silicon (Si) and magnesium (Mg) identified as the general constituent of ocean floors) being weaker than sial (rock rich in silicon and aluminum (Al) identified as the general constituent of continents).

Paleontologists specializing in Cenozoic studies of the distribution of mammals tended to be fixists.

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What is Global Warming? by Hayanon


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