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High Dome Trail fern covered meadow overlooks Patrick Creek. Smith River National Recreation Area, Redwood Highway 199, Crescent City, northwest California Klamath Mountain coast

  High Dome Trail overlooking Smith River National Recreation Area, northwest California

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High Dome Trail, California
Smith River National Recreation Area

High Dome Trail, Smith River National Recreation Area, Patrick Creek, CaliforniaThe 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

High Dome Trail, Smith River National Recreation Area, Redwood Highway 199, Crescent City, northwest California Klamath Mountain coastThe 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 overlooking Cold Springs Mountain. Smith River National Recreation Area, Redwood Highway 199, Crescent City, northwest California Klamath Mountain coast
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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