UPPER BIG QUILCENE TRAIL Length 6.7 mi/10.8 km Access FS Road 2750 USGS Maps Mount Townsend; Mount Deception Agency Olympic National Forest This route traverses the Buckhorn Wilderness. The trailhead (2500 ft/ 762 m) is located on FS Road 2750 just beyond Ten Mile Shelter (4.6 mi/7.4 km), near where the road crosses the Big Quilcene River. The shelter stands on a bench above the road, next to Wet Weather Creek; but, as the name implies, it was 10 miles up the trail before the road was built. The trail, which is well maintained by a number of volunteer groups, climbs gradually through stands of old-growth fir, cedar, and hemlock, primarily the latter. Rhododendrons are abundant and in early summer brighten the forest with masses of pink flowers. Many big, moss covered boulders lie scattered about, and ferns grow among the rocks. The trail comes out onto the banks of the Big Quilcene, then switchbacks upward through silver fir and western hemlock, leaving the river far below rushing wildly through the forest. The trail then returns to the river and a side trail leads, left, to Shelter Rock Camp (2.6 mi/4.2 km; 3650 ft/1113 m), located in a stand of tall hemlock beside the Big Quilcene, which at this point is scarcely 10 feet wide. Why the camp received its name is puzzling. The only large boulders nearby are two modest-sized ones. Beyond this camp the trail once again climbs up and away from the river, but parallels a small stream, the last source of water until one approaches Camp Mystery. As it traverses a steep, sun-baked mountainside, the path crosses a large boulder field where, during the winter and spring months, avalanches sweep down from Iron Mountain and Buckhorn Mountain. The river's canyon is to the left, and one can look up toward Marmot Pass. The trail then crosses scree slopes of another avalanche zone. Buckhorn Mountain stands to the north, the slope above the trail culminating in pinnacles of basalt. Across the narrow valley rise steep ridges and Peak 6852, with Mount Constance beyond. Camp Mystery (4.6 mi/7.4 km; 5400 ft/1646 m) is located in a stand of sub-alpine fir beside a stream. A cragged ridge rises to the north, and rugged peaks are visible to the south. This is a good place to make a base camp because running water is available, and the place is sheltered from the wind. The trail now climbs steadily toward Marmot Pass. The trees are much smaller and the stands thinner. The route goes through an area of large boulders interspersed with meadows and groves of subalpine fir, where a little stream tumbles down from the heights above. This is the last source of water. People who have cut across the switchbacks have done at this point considerable damage to the trail. The trail zigzags up the slope beneath outcrops of basalt, and one can look down the Big Quilcene Valley and see Puget Sound-and, beyond it, Glacier Peak topping the Cascades. The trail then breaks out into large meadows, through which it climbs to a junction with the Tubal Cain Trail at Marmot Pass (5.3 mi/ 8.5 km; 6000 ft/1829 m). Upon reaching the pass, one is inclined to linger and savor the panorama that extends across the upper Dungeness. The view includes some of the highest peaks in the Olympics, including Fricaba, Deception, The Needles, and Graywolf Ridge. The pass is merely the low point in the Constance Range, the ridge that extends north from Mount Constance to the headwaters of Copper Creek. Here the wind seldom, if ever, stops blowing, howling fiercely as it whips across the notch, whistling in the subalpine firs that cling to the nearby ridge, while the grasses and wild-flowers wave wildly. Occasionally, however, the wind is toned down to a subdued susurration, and when this occurs the pass is a pleasant place to be. One cannot help but wonder, however, what it must be like here during a winter storm. . Double-peaked Buckhorn Mountain (6988 ft/2130 m; 6956 ft/2120m), which rises about a mile northeast of the pass, offers still better views of the northeastern Olympics. The ascent of the mountain, which owes its name to a fancied resemblance of the peak to deer antlers, is non-technical, via a prominent boot path visible from the pass. The much-used route is generally snow-free by mid-July. Hikers should stay on the boot-beaten path to avoid trampling the heather. Beyond the pass the trail crosses a rock slide, then makes "the grand traverse"- alternately going through groves of subalpine fir and across meadowland brightened by bluebells, lupine, and yarrow in late summer, with splendid views of the Dungeness Valley and the rugged peaks. The trail then descends, crossing rockslides and meadows dotted with subalpine firs, and lodgepole and white bark pines. This is one of the few places where white bark pine grows in the Olympics, but about half the trees are dead. The trail then skirts a field of big, rough boulders at the foot of a talus slope, where water is available. This is the first stream since just beyond Camp Mystery. The trail enters a dense stand of subalpine fir as it drops down to a junction with the Constance Pass Trail and the Upper Dungeness Trail near Boulder Shelter (6.7 mi/ 10.8 kin; 4950 ft/1509 m).