A Report on Washington TerritoryRuffner, William Henry
History
A Report on Washington Territory
Ruffner, William Henry
Washington (State)
The undulating country north and east of Puget Sound is in many places
deeply covered with drift material which shows the effect of both ice
and water. Blocks of partially rounded granite several feet in diameter
are found on the hills around Seattle. This gravel deposit is not often
found on high points, but there is a ridge in the Cascade Mountains,
near Salal Prairie, which is thickly bestrewed at an elevation of 1,000
feet. This, however, was quite exceptional, and may be the lateral
moraine of a local glacier. The deposit around Seattle is not only easy
to cultivate (its soil being a light blue loam), but seems fertile. The
bottom lands are free from gravel.
So much for the general geology.
ECONOMIC GEOLOGY.
NOTE.--The location of the coal-fields and collieries mentioned in
the following pages may be seen on an accompanying map.
Under the head of Economic Geology, I shall describe with more detail
the mineral beds which have a commercial value, and in the following
order:--I. Coal; II. Iron Ore; III. Granite, Limestone, and Marble; IV.
Precious and Base Metals.
[Sidenote: Thickness of the Coal Measures.]
I. COAL.--The thickness of the Coal Measures of the Puget Sound basin is
estimated by Bailey Willis at something like 14,000 feet, though he
admits the obvious possibility of error in the calculation by reason of
undiscovered faults. We may fairly expect them, however, to be thicker
than the same group in the Rocky Mountains, which measure about 9,000
feet. As heretofore remarked, the sediments become thinner from west to
east. Of course, the maximum thickness is not to be expected in every
locality. Mr. Willis's estimate was made in the Wilkeson and Green River
fields, and really did not reach the limit of the coal-bearing rocks.
The coal rocks of the Cedar River and Snoqualmie basin have never, so
far as I know, been estimated, but probably this group is equal in
thickness to that of any other part of the field. The difficulty of
measurement arises from the numerous fractures and changes of strike
which exist.
[Sidenote: Fifteen workable seams.]
The number of distinct workable seams of coal of three feet and upwards,
belonging to the measures, may safely be put down at not less than
fifteen.
[Sidenote: Different kinds of coal described.]
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