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
Let us begin with the simplest case. The drainage system of Mount
Ellsworth is more purely consequent than any other with which I am
acquainted. In the accompanying chart the point _c_ marks the crest of
the Ellsworth dome; the inner circle represents the line of maximum dip
of the arching strata and the outer circle the limit of the disturbance.
It will be seen that all the waterways radiate from the crest and follow
closely the directions in which the strata incline. At _a_ the Ellsworth
arch touches that of Mount Holmes and at _b_ that of Mount Hillers; and
the effect of the compound inclination is to modify the directions of a
few of the waterways.
[Illustration:
FIG. 71.—Drainage system of the Ellsworth Arch.
]
Turning now to Mount Holmes, we find that its two domes are not equally
respected by the drainage lines. The crest of the Greater arch (see
Figure 72) is the center of a radiating system, but the crest of the
Lesser arch is not; and waterways arising on the Greater traverse the
Lesser from side to side. More than this, a waterway after following the
margin of the Lesser arch turns toward it and penetrates the flank of
the arch for some distance. In a word, the drainage of the Greater arch
is consequent on the structure, while the drainage of the Lesser arch is
inconsequent.
[Illustration:
FIG. 72.—Drainage system of the Holmes Arches.
]
There are at least two ways in which this state of affairs may have
arisen.
First, the Greater arch may have been lifted so long before the Lesser
that its waterways were carved too deeply to be diverted by the gentle
flexure of the latter. The drainage of the Lesser would in that case be
classed as antecedent. If the Lesser arch were first formed and carved,
the lifting of the Greater might throw a stream across its summit; but
it could not initiate the waterways which skirt the slopes of the
Lesser, especially if those slopes were already furrowed by streams
which descended them. If the establishment of the drainage system
depended on the order of uplift, the Greater arch is surely the older.
Public-domain text, read in full here on John Shaqi.
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