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
Where a stream has all the load of a given degree of comminution which
it is capable of carrying, the entire energy of the descending water and
load is consumed in the translation of the water and load and there is
none applied to corrasion. If it has an excess of load its velocity is
thereby diminished so as to lessen its competence and a portion is
dropped. If it has less than a full load it is in condition to receive
more and it corrades its bottom.
A fully loaded stream is on the verge between corrasion and deposition.
As will be explained in another place, it may wear the walls of its
channel, but its wear of one wall will be accompanied by an addition to
the opposite wall.
The work of transportation may thus monopolize a stream to the exclusion
of corrasion, or the two works may be carried forward at the same time.
_Corrasion and Declivity._
The rapidity of mechanical corrasion depends on the hardness, size, and
number of the transient fragments, on the hardness of the rock-bed, and
on the velocity of the stream. The blows which the moving fragments deal
upon the stream bed are hard in proportion as the fragments are large
and the current is swift. They are most effective when the fragments are
hard and the bed-rock is soft. They are more numerous and harder upon
the bottom of the channel than upon the sides because of the constant
tendency of the particles to sink in water. Their number is increased up
to a certain limit by the increase of the load of the stream; but when
the fragments become greatly crowded at the bottom of a stream their
force is partially spent among themselves, and the bed-rock is in the
same degree protected. For this reason, and because increase of load
causes retardation of current, it is probable that the maximum work of
corrasion is performed when the load is far within the transporting
capacity.
The element of velocity is of double importance since it determines not
only the speed, but to a great extent the size of the pestles which
grind the rocks. The coefficients upon which it in turn depends, namely,
declivity and quantity of water, have the same importance in corrasion
that they have in transportation.
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