GEO5 V18 - MB
419 Geobiology Geology is the study of the deep time of the Earth and its component parts. Geology encompasses not only thegeologic past and present of the surface and mantle, but also the sub-surface past and present of the crust, lithosphere,asthenosphere, and convecting mantle. Geology also incorporates the study of the subsurface processes within which all geologicprocesses occur. The result of these geologic processes are the surface structures and materials that may be encountered byhumans. Geology as a field of science was developed during the late 17th and 18th century by several independent investigators
and, by the late 19th century, geology was incorporated as a distinct but still interdisciplinary scientific field of study within thebroader discipline of Geography. In the 1960s, geologists became more aware of the varied and often subtle ways in which
different components of geology interact with one another. Now, the early 20th century emphasis on the roles of energy in thedetermination of surface features has been superseded by a growing awareness that a host of different geological events, such asplate tectonics, the circulation of oceanic water and the accumulation of sediment, can and do have a profound effect on thesurface and subsurface features. In the last few decades it has become increasingly clear that the formation and distribution of
surface and subsurface features can have far-reaching geophysical, climatic, and anthropogenic effects. Now we know muchabout the way the lithosphere, the surface of which is slowly moving, is formed and differentiated as a result of spreading rifts
and the melting of the lithosphere. The lithosphere is in turn modulated by the solid mantle, into which the lithosphere isactively being converted as a result of subduction. This activity can be inferred by seismology, oceanography and geochemistry.
Geology is the study of the deep time of the Earth and its component parts. Geology encompasses not only the geologic past andpresent of the surface and mantle, but also the sub-surface past and present of the crust, lithosphere, asthenosphere, andconvecting mantle. Geology also incorporates the study of the subsurface processes within which all geologic processes occur.
The result of these geologic processes are the surface structures and materials that may be encountered by humans. Geology as afield of science was developed during the late 17th and 18th century by several independent investigators and,

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GEO5 V18 MB