Grove Gilbert is well known for his concept
of graded streams. This concept maintained that streams
always make channels and slopes for themselves either by
cutting down their beds or by building them up with sediment
so that over a period of time these channels will transport
exactly the load delivered into them from above. Gilbert
also explained the structure of the Great Basin as a result of
extension, that is, individual “basin ranges” are the eroded
upper parts of tilted blocks, which were displaced along
faults as “comparatively rigid bodies of strata.” After 1862,
Gilbert received a number of awards and worked with
numerous geologists on several geological surveys. When he
studied the Henry Mountains (1875–76) he was the first to
establish the fact that intrusive bodies are capable of deforming
the host rock. He insisted that the Earth’s crust is “as
plastic in great masses as wax is in small.” Unfortunately he
exaggerated the fluidity of magma. Gilbert was conscientious
in giving credit to those who deserved it but did not pay
attention when it was given to him. From 1889 to 1892, he
was the chief geologist of the U.S. Geological Survey.
glacial system See GLACIER.
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