GEOLOGY OF OLYMPIC NATIONAL PARK:
PART Il NOTES ON THE GEOLOGY
Obstruction Peak Road
STOP 11:
Collapsed pinnacle Most geologic
processes are of barely comprehensible slowness, but a few are rapid
and even catastrophic. Where the Obstruction Peak Road emerges from
the forest to balance precariously on a knife-edge saddle before the
long hill up to the base of Steeple Rock (about 1 mile from the turnoff),
look to the west to see some large blocks of dark rock among the trees
on the bumpy terrain (fig. FT 23).

Fig. FT
23. Collapsed basalt pinnacle along the Obstruction Peak Road. |
The explorer
who wanders down among these monoliths of pillow basalt will find a
fantastic jumble of rock wails, blocks, and rubble piles. The scene
resembles the ruins of some gigantic city, overgrown and partly hidden
by trees At the base of some huge mountain escarpment we would expect
to find such debris fallen from the heights, but there is no such escarpment
near here. Up the road, however, is a clue to the ruin in the form of
Steeple Rock, an erosion-resistant pinnacle of basalt standing high
above the rolling meadows of slate and sandstone. It is part of an uptilted
zone of basalt layers, the inner basalt ring, extending many miles to
the southeast (see figs. 16
and geologic map). The rocky
ruin lies along a projection of the same zone to the northwest The rubble
probably once stood as a pinnacle like Steeple Rock. From the amount
of debris, we can surmise that the pinnacle was even larger. The cause
of its collapse appears to be landsliding. Slippage of the surface layers
of rock, especially in areas of weak slate or shale, is very common
in the Olympics.

Fig. FT
24. Sketch of depression along the Obstruction Peak Road. |
Along
the Obstruction Peak Road are shallow swales paralleling the contour
of the hillside; the road follows some of these features (fig FT 24).
Similar to ridgetop depressions,
they are caused by downhill creep of surface rubble and in some places
of the bedrock itself.
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