The Kenyon Devore Trail and Mt. Disappointment 50K

Strayns Canyon from the Kenyon Devore Trail in Angeles National Forest

Note: The Mt. Disappointment Endurance Run is now the Angeles National Forest Trail Race.

The photograph above was taken a little more than a mile from the top of the Kenyon Devore Trail, in the San Gabriel Mountains, near Mt. Wilson. The deep canyon seen through the trees is Strayns Canyon, which the trail follows on its way from the West Fork San Gabriel River to the shoulder of Mt. Wilson.

Bright green Bigcone Douglas fir cones
Bigcone Douglas fir

Today, I’d run down the Kenyon Devore and Gabrieleno Trails to West Fork and then up the Red Box – Rincon Road to point on the map marked Camp Ah-DA-Hi. (A former Woodcraft Rangers Camp.) With hot weather forecast next Saturday for the Mt. Disappointment 50K, I’d been glad to see the small streams that had been dry during the drought were running again.

Trails have stories to tell and when I run or hike a trail I’m always curious about its history. A trail between the West Fork San Gabriel River and Mt. Wilson is shown in the 1:62500 1897 edition of the USGS 1894 Los Angeles Sheet. Like many trails of the era, it followed a ridge, in this case a ridge just east of Strayns Canyon.

Antennae on Mt. Wilson at the top of the Kenyon Devore Trail.
Antennae on Mt. Wilson at the top of the Kenyon Devore Trail.

The first USGS map to show a trail along Strayns Creek was the 1:24000 1934 Mt. Wilson Advance Sheet. The trail remained unnamed in USGS maps until the 1966 edition of the 1:24000 Mt. Wilson Quadrangle, when it was labeled the Rattlesnake Trail. The trail was renamed the Kenyon Devore Trail in the 1995 edition of the map in tribute to Forest Service patrolman, hydrographer, and Angeles National Forest volunteer, Kenyon DeVore.

The Kenyon Devore Trail is part of the Mt. Disappointment 50K course. It is one of several trails maintained by runner-volunteers under the guidance of Forest Service volunteer and Mt. Disappointment Race Director, Gary Hilliard. Today, as I was on my way back up to Mt. Wilson, I ran into Gary and two volunteers cutting logs from the trail in preparation for next Saturday’s event.

Gary Valle and Gary Hilliard on the lower Kenyon Devore Trail.
Gary and the Other Gary on the lower Kenyon Devore Trail.

The grueling 5 mile, 2650′ climb from West Fork to Mt. Wilson on the Gabrieleno & Kenyon Devore Trails comes at about mile 26.5 of the 50K and is the highlight of the run.

I have to laugh about what happened on the Kenyon Devore climb one hot year. I’d jammed my Camelbak(TM) with so much ice at the West Fork aid station that when water was added, it melded and froze into one large chunk. I didn’t discover this until about halfway up the climb, when I ran out of water. You can’t drink a chunk of ice and even at 90 degrees, the ice was melting at an agonizingly slow rate. At best I could only get a minuscule sip of water from the pack every few minutes, and it nearly imploded from my efforts.

Some related posts: Mt. Disappointment 50K Returns!, Mt. Disappointment 50K 2012 Notes

Sizzling San Jacinto

Tahquitz Meadow
Tahquitz Meadow

We were nearly to the junction of the Pacific Crest Trail and the South Ridge Trail and about a half-mile from Tahquitz Peak (8846′). It was hot. In the shade the temp was in the high 80s, but in direct sun the temperature was close to 100°F.

Tahquitz Peak from Wellman Divide
Tahquitz Peak from Wellman Divide

A few hours earlier Skye and I had grabbed the first car up on the Palm Springs Tram and done the 5 mile, 2435′ ascent of San Jacinto Peak. At 10,800’+ at 10:00 in the morning it had been 70°F — warm for one of the higher mountains of Southern California. Remarkably, a couple of small patches of snow remained on the south side of the summit.

Where we were now, 70 degrees would feel like a refrigerator. We’d given up that cooler clime and all the elevation we’d gained, and run five miles down the Wellman Divide Trail and PCT to Saddle Junction — a descent of about 2700′. The temperature had increased all the way down.

Tahquitz Rock from the Wellman Divide Trail
Tahquitz Rock from the Wellman Divide Trail

We might as well have been in a drying oven. The combination of the hot weather, a high sun, low humidity and higher altitude had desiccated me. At the turn-off off from the PCT to Tahquitz Peak I lifted my pack and squeezed the reservoir — again. In the few minutes since I last checked, no water had magically found its way into my pack. There was less than 20 ounces remaining and that wasn’t going to be enough.

Descending from Tahquitz Peak
Descending from Tahquitz Peak

After running over to Tahquitz Peak and visiting the lookout, there was still the minor detail of getting back to the Tram. The Mountain Fire closure was still in effect, which meant we could not use the Willow Springs Trail and would have to retrace our steps and climb all the way back up to Wellman Divide.

During the drought I would bring extra water when doing this route, and stash it along the trail. With this year’s good snowpack it seemed we should be able to find water if we needed it.

Wellman Cienaga from the Wellman Divide Trail
Wellman Cienaga from the Wellman Divide Trail

Prior to the Mountain Fire I’d used Willow Creek as a water source, but since the Willow Springs Trail was closed, that was out. The seep at Wellman Cienaga was too far up and the flow was low. Skunk Cabbage Meadow and Tahquitz Valley were a possibility. Originally included in the Mountain Fire closure area, they had reopened. I recalled a water source in Skunk Cabbage Meadow, but didn’t remember much about it.

When we got to Tahquitz Peak we asked Joe, the volunteer Ranger at the Tahquitz Peak Lookout, what he thought would be a good water source. He suggested Tahquitz Creek in Tahquitz Valley. I hadn’t been to Tahquitz Valley, so this was a great time to check it out.

Corn lilies and ferns along the Wellman Divide Trail.
Corn lilies and ferns along the Wellman Divide Trail.

Although small in its upper reaches, Tahquitz Creek had plenty of water. Using a UV Pen, we refilled our packs and drank until we couldn’t drink any more. Continuing, we found there was also water available at Skunk Cabbage Meadow. At least for now. I wouldn’t hazard a guess how long these water sources will last.

Ah water, wonderful water. With water the hike and run back to Wellman Divide was just a sweaty, strenuous and scenic climb, and not the hellish ascent it might have been.

Some related posts: San Jacinto Peak and Tahquitz Peak Trail Run, Room With a View, Mountain Weather

Along the Crest

Trees and clouds along the crest of the San Gabriel Mountains. Photography by Gary Valle.

I rounded the corner, driving from deep shade into the golden glare of the rising sun. There was almost no traffic on Angeles Crest Highway. Up ahead, in the shade of some trees, there was something in the road. Was it a rock or a pine cone? Driving into the sun it was hard to tell. At this time of the morning — before the CalTrans truck has swept the road — one small rock can ruin your whole day. Getting to the trailhead unscathed is always the first challenge of the day.

Middle Hawkins from the Pacific Crest Trail. Photography by Gary Valle.
Middle Hawkins from the Pacific Crest Trail.

Today, Craig and I were planning to do a point to point run from Inspiration Point to Islip Saddle — one of the best stretches of trail in the San Gabriel Mountains.

PCTA volunteer Ray Drasher often takes care of clearing the trees from this section of the Pacific Crest Trail. It’s quite an undertaking to get the required stock and equipment to the trailhead and then cut trees spread over several miles of trail. Because of conflicting reports, Ray wasn’t sure whether there were trees still on the trail or not. We’d let him know after the run.

On the drive up you could see it was going to be a spectacular day in the Angeles high country. A low pressure trough moving through central California had pulled in the marine layer and a tumultuous ocean of cloud reached from the south-facing canyons far out over the Pacific.

Trail runner descending the PCT near Mt. Burnham.
Craig descending the PCT near Mt. Burnham.

I drove through the double tunnels at Mt. Williamson and then around a left-hand curve. Up ahead I could see the northwest ridge of Mt. Islip dropping down to Islip Saddle. What the heck? Orange cones? The gate is closed? The HIGHWAY is closed? That didn’t make sense; the Winter closure had ended weeks before.

After parking, I talked to a hiker who said it was closed for “road work.” I assumed there must have been a rock slide in one of the problematic areas between Islip Saddle and Vincent Gap. Later I learned the problem was a “sink hole” west of the Grassy Hollow Visitor Center.

After Craig arrived we discussed route options to Mt. Baden-Powell. Either we did the South Fork loop, which I’d done a couple weeks before, or we did an out and back on the PCT. We opted for the out and back.

Weather-beaten limber pine near the summit of Mt. Baden-Powell. Photography by Gary Valle.
Weather-beaten limber pine near the summit of Mt. Baden-Powell.

The run was as spectacular as expected. The visibility above the deck of stratus was at least 100 miles. San Bernardino Peak, San Gorgonio Mountain and San Jacinto were easy marks to the east and Owens Peak and the Southern Sierra could be seen to the north. Before it was immersed in a tide of cloud, the summit of Santiago Peak (Saddleback) had been visible to the south. High clouds and a gusty westerly wind kept the temperatures moderate. Only one very small patch of snow remained on the trail.

I’d hoped to be able to tell Ray the trees had been cleared from the trail, but no — they were still there. He said the next time I ran there, they would be gone. Thanks Ray!

Say Goodbye to the Snow in the San Gabriel Mountains

Patches of snow on the PCT west of Mt. Baden-Powell

Each year around Memorial Day weekend I like to do a run that includes Mt. Baden-Powell (9399′). It’s a good time to check how much snow remains at the higher elevations of the San Gabriel Mountains. In a heavy snow season, such as 2004-2005, higher sections of trail may still be buried in snow and drifts can persist into July. In below average years, such as we experienced from 2013 to 2016, there may be little or no snow.

South Fork Trail below Islip Saddle
South Fork Trail below Islip Saddle

There are several good runs that summit Mt. Baden-Powell. If Hwy 2 is still closed between Islip Saddle and Vincent Gap, I’ll usually do an out and back from Islip Saddle to Mt. Baden-Powell. If Hwy 2 is open, then a point to point run from Inspiration Point to Islip Saddle or Eagles Roost is a good option. Today the choice was one of my favorite loops in the San Gabriels. It starts at Islip Saddle, descends to South Fork Campground, then climbs about 5000′ to the summit Mt. Baden-Powell. From Baden-Powell the route follows the Pacific Crest Trail back to Islip Saddle.

Pine Mountain, Dawson Peak and Mt. Baldy from the summit of Mt. Baden-Powell.
Pine Mountain, Dawson Peak and Mt. Baldy from the summit of Mt. Baden-Powell.

This was my third time on the PCT between Islip Saddle and Mt. Baden-Powell this Spring. The first was at the beginning of April and was more of a snow hike than a run. The micro spikes went on at 7000′, less than 0.7 mile from the Islip Saddle trailhead. The second trip was two weeks later, in mid-April. Micro spikes were still helpful in a couple of places and there was still plenty of snow on the north side of the crest. Based on other seasons with a similar amount of snow, I thought some patches of snow might last into June, or even early July. Today (May 27) only a few patches remain on Baden-Powell and along the crest, and these will soon be gone.

Manzanita Trail between South Fork Campground and Vincent Gap
Manzanita Trail between South Fork Campground and Vincent Gap

Except for being a little disappointed there wasn’t more snow, the run went well. The South Fork Trail was rocky and rough — as usual. The Manzanita Trail, which connects South Fork Campground to Vincent Gap, has seen a lot of work in recent years and is in relatively good shape. Even the gnats weren’t bad. I saw no one on the South Fork and Manzanita Trails. As might be expected on a Saturday on Memorial Day Weekend, there were “a few” hikers, thru-hikers and runners on the PCT.

The South Fork Trail is part of a long and little-used “official” PCT detour around the mountain yellow-legged frog closure at Eagles Roost. Based on the number of thru-hikers I see on Hwy 2, most opt to hike the 2.7 road miles between Eagles Roost and Buckhorn Campground and then descend the Burkhart Trail to the PCT. It’s been more than 11 years since the initial “temporary” closure of the Williamson Rock area in December 2005. Hopefully it won’t be too many more years before the proposed plan to reopen the PCT and partially reopen Williamson Rock is completed.

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