Report on the geology of the Henry Mountains — John Shaqi
Report on the geology of the Henry MountainsGilbert, Grove Karl
Science
Report on the geology of the Henry Mountains
Gilbert, Grove Karl
Geology -- Utah -- Henry Mountains; Intrusions (Geology) -- Utah -- Henry Mountains
The Henry Mountains have been visited only by the explorer. Previous to
1869 they were not placed upon any map, nor was mention made of them in
any of the published accounts of exploration or survey in the Rocky
Mountain region. In that year Professor Powell while descending the
Colorado River in boats passed near their foot, and gave to them the
name which they bear in honor of Prof. Joseph Henry, the distinguished
physicist. In 1872 Prof A. H. Thompson, engaged in the continuance of
the survey of the river, led a party across the mountains by the
Penellen Pass, and climbed some of the highest peaks. Frontiersmen in
search of farming and grazing lands or of the precious metals have since
that time paid several visits to the mountains; but no survey was made
of them until the years 1875 and 1876, when Mr. Walter H. Graves and the
writer visited them for that purpose.
They are situated in Southern Utah, and are crossed by the meridian of
110° 45′ and the thirty-eighth parallel. They stand upon the right bank
of the Colorado River of the West, and between its tributaries, the
Dirty Devil and the Escalante.
At the time of their discovery by Professor Powell the mountains were in
the center of the largest unexplored district in the territory of the
United States—a district which by its peculiar ruggedness had turned
aside all previous travelers. Up to that time the greater part of the
knowledge that had been gained of the interior of the continent had been
acquired in the search for routes for transcontinental railways; and the
cañons of the Colorado Basin, opposing more serious obstacles to travel
than the mountain ranges which were met in other latitudes, were by
common consent avoided by the engineers.
The same general causes which have rendered the region so difficult of
access and passage have made it a desert, almost without economic value.
The physical conditions of elevation and aridity which have caused it to
be so deeply carved in cañons, have prevented the streams with which it
is scantily watered from being bordered by tracts of land which can be
irrigated; and agriculture without irrigation being in that climate an
impossibility, there is nothing to attract the farmer. As will be
explained in the sequel, the mountains offer no inducements to the miner
of the precious metals. There is timber upon their flanks and there is
coal near at hand, but both are too far removed from other economic
interests to find the market which would give them value. It is only for
purposes of grazing that they can be said to have a money value, and so
distant are they at present from any market that even that value is
small.
Public-domain text, read in full here on John Shaqi.
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