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The
High Dome Trail is a relatively short trail about a mile in length
that takes you to a meadow of ferns overlooking Smith River National
Recreation Area and the northwest California Klamath Mountains. A
short spur trail takes you on a side trip to a high point that was
once used for a fire lookout. This description
covers only the 3/4 mile segment of trail from County Road 315 to the
meadows. It does not cover the lower part of the High Dome Trail
that goes down the mountain for about two miles and ends at County
Road 315 near the historic 1885 Gasquet Toll Road.
Directions to the High Dome trailhead
The most direct route is to drive up the gravel
surfaced Patrick Creek Road from Highway 199 near Patrick Creek
Lodge. This road begins on the north side of the Patrick Creek
Bridge, across the creek from the lodge. Follow this road for about
3.5 miles to the narrow bridge over Patrick Creek. Immediately after
the bridge, TURN RIGHT on the road to Holiday Mine (County Road
315). Follow this road for 5.5 miles and look for the trailhead on
the right. An alternative route to the trailhead is
to follow the
Patrick Creek Loop Drive. This
describes the history and geology of the region as well as points
out other hiking opportunities near High Dome. The driving distance
to go directly from Highway 199 to High Dome and return to Highway
199 is 18 miles. The total distance of the loop drive is 25 miles.
High Dome trail description
The
High Dome Trail (picture right) to the fern covered meadows is about
3/4 mile in length and is relatively level except for some sections
that climb steeply for a short distance. As you approach the meadows
a short trail goes off to the left and climbs to a ridge that was
once used as a fire lookout. After the intersection with the lookout
trail, the High Dome Trail begins to go down hill. Continue down the
trail for a short distance and look for the trail to the meadows on
the right. Walk about 300 feet through the forest to the edge of the
meadows. There is no trail beyond this point.
A word to the wise: As you walk out into the meadow,
take a look behind you and make a mental note of landmarks to help
you find the trail when you return. There is no marker to indicate
where the trail is located and all the forest around the meadow
looks the same.
At one point the trail crosses a talus of medium
sized rock. The talus creates an opening that offers a view toward
Cold Springs Mountain and the ridge that was once used by strings of
pack mules carrying supplies from cargo ships in Crescent City
harbor to southwest Oregon mining camps during the Oregon gold rush
of 1851.

High Dome Trail with Cold Springs Mountain the
high point along the ridge in the far distant center. The ridge from
Cold Springs Mountain and center-right foreground was used by pack
trains using the 1852 Cold Springs Mountain Pack Trail (now called
the Elk Camp Ridge Trail).
If
you look closely at the soil of the High Dome Meadow you will see
small particles that glint in the sun. These are mostly flakes of
mica, which is not common to most rocks in this region. The large
boulders in the meadow provides a good example of the type of rock
that this sandy, mica laced soil comes from. These rocks are made up
of a type of rock called diorite, a rock that is peppered with white
and black crystals. These rocks, like many others in the
region, were formed when molten magma worked its way up into the
surrounding rock. Over a long period of time, this molten material
slowly cooled and crystallized forming these rocks that are salt and
peppered with white and black crystals. Diorite tends to break
down into to sand and one of the minerals that is released by the
rock is mica.
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