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
4th. There is a limit to upward expansion, dependent on the fact that
the pressure due to the combined weight of the laccolite and cover
cannot exceed the pressure of the intrusive lava. Regarding the
intrusive pressure as constant, it is divisible into three parts, of
which one sustains the weight of the cover, also constant; another
sustains the weight of the fluid laccolite, and is measured by its
thickness or depth; and the third produces deformation. When the sum of
the weights of the cover and laccolite equals the total pressure of the
intrusive lava, uplift ceases, and the maximum depth or thickness is
attained. We may call this the _limital thickness_. With regard to
simple laccolites the limit is absolute, but it applies only to the
distinct layers of those which are composite; for a composite laccolite,
built by successive intrusions at wide intervals of time, may be
relieved of part of its load by the erosion of the mound which its
expansion causes at the surface of the land.
A laccolite formed beneath the bottom of a sea has a greater limital
thickness than one formed beneath a land surface; for the superjacent
water being displaced and thrust aside, is to that extent subtracted
from the load to be lifted.
5th. The laccolite in its formation is constantly solving a problem of
“least force”, and its form is the result. Below, above, and on all
sides its expansion is resisted, and where the resistance is greatest
its contour is least convex. The floor of its chamber is unyielding, and
the bottom of the laccolite is flat. The roof and walls alike yield
reluctantly to the pressure, but the weight of the lava diminishes its
pressure on the roof. Hence the top of the laccolite becomes broadly
convex, and its edges acutely. Local accidents excepted, the walls
oppose an equal resistance on every side; and the base of the laccolite
is rendered circular.
The second of the conclusions enunciated above is susceptible of test by
observation. By selecting those laccolites of which the dimensions are
known with the best degree of approximation, the following table has
been formed:
│ Formations. │Titles of Laccolites.│Diameters│Means.
│ │ │in miles.│
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