The Nakimu Caves, Glacier Dominion Park, B. C.Canada. National Parks Branch
Science
The Nakimu Caves, Glacier Dominion Park, B. C.
Canada. National Parks Branch
Nakimu Caves (B.C.)
“At the meeting of the ways above referred to, the lower or eastern one
is named ‘The Slanting Way’ from the fact that the passage is formed by
a separation of the limestone strata, and lies across their dip. The
upper passage has an arched roof and has been named ‘The Subway.’ Both
are difficult to traverse: the former on account of the broken debris
and sloping rock of which the floors are formed, and of two
uncomfortably narrow places which can be squeezed through with
difficulty; the latter on account of the close proximity of floor and
ceiling and the necessity of bending nearly double for a considerable
part of the distance while traversing it. The lower passage is the
easier of the two. The strata forming the Slanting Way are from five to
ten feet apart. The slabs of both roof and floor are water-worn and bear
spatulated erosion marks, like incipient honey-combing. On the east, or
left side, as you advance, are deep cracks in the strata, at the bottom
of whose depths Cougar creek may be heard echoing loudly through the
vaulted ways. Stones dropped into these seem to rebound for a long time
before resting. About the centre of the Slanting Way the cracks in the
strata expand and a descent may be made to the bed of Cougar creek below
the Turbine. The Turbine is reached by a rather difficult passage
requiring some skill in climbing. The end of the passage is an irregular
opening in the rock. Across a chasm, at whose bottom flows the main
stream, a number of water-spouts rush out with great force and a noise
resembling that produced by water falling into the pit of a turbine. For
an account of this section see Ayres’ report. Near the south end of the
Slanting Way is a curious pothole on the left-hand side. Directly beyond
it the floor and walls are covered by an incrustation of carbonate of
lime, varying in thickness from 2 to 6 inches. It is of a light creamy
colour, shading off in some places to a delicate salmon. The formation
has a florescent appearance and resembles, mostly, cauliflower heads set
closely together, a simile derived from W. S. Ayres’ report. Owing to
the beautiful floral decorations, this particular spot has been named
‘The Art Gallery.’
“Similar decorations are found throughout the Caves, though not so
extensively as at this and a few other places. At some, there is only a
thin veneer of the carbonate formation and, at others, rock-milk
(_agaric mineral_) is seen on the floors and boulders. The writer did
not observe any stalagmites, nor any stalactites worth speaking of. The
longest did not exceed 15 inches, and resembled, more than anything
else, a thin icicle of that length; its chief interest being that it was
clear and transparent, as though made of ice, and as brittle as glass.
Public-domain text, read in full here on John Shaqi.
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