Category Archives: running|adventures

Mt. Wilson Area Peaks From Twin Peaks

Mt. Wilson, Occidental Peak, Mt. Markham, San Gabriel Peak, Mt. Disappointment, and Mt. Deception from the summit of Twin Peaks, in the San Gabriel Mountains, near Los Angeles.

Mt. Wilson, Occidental Peak, Mt. Markham, San Gabriel Peak, Mt. Disappointment, and Mt. Deception from the summit of Twin Peaks, in the San Gabriel Mountains.

Mt. Markham (5742′) is the craggy peak along the skyline, just right of the centerline of the photograph. The bump to the left of Mt. Markham is Occidental Peak (5732′). To the right of Mt. Markham is the highest peak in the group, San Gabriel Peak (6161′). To the right of San Gabriel Peak are Mt. Disappointment (5960′), and Mt. Deception (5796′). The indistinct summit of Mt. Wilson (5710′), and the observatory, are on the left.

Guardian of the rugged San Gabriel Wilderness, Twin Peaks (7761′) has an isolated, high mountain feel. Its flanks drop more than 5000 feet to Devils Canyon on the southwest, and Bear Canyon on the southeast.

We climbed Twin Peaks while doing a point to point run from Buckhorn to Three Points. Including the peak, the run/hike was about 13 miles, with an elevation gain of about 3200′. Here’s a Google Earth image and Google Earth KMZ file of a GPS trace of the route.

Related posts: Manzanita Morning, Three Points – Mt. Waterman Loop

Mt. Langley in a Day from L.A.

Cirque Peak from Cottonwood Lakes Basin.
Cirque Peak from Cottonwood Lakes Basin

The sky was brightening in the east, and sunrise was approaching when I met Miklos and Krisztina at the Denny’s in Sylmar. We were already wasting light. The plan was to drive from near sea level up to Horseshoe Meadows, at about 10,000′ on the Sierra east side. The hike/run we had in mind was a keyhole loop from the Cottonwood Lakes Trailhead up (old) Army Pass and then down New Army Pass. If we felt OK at the top of Army Pass, we would also do Mt. Langley (14,026′).

The weather forecast looked good. There was a chance of some gusty southwest winds in the afternoon, but temps were warm and there was virtually no chance of T-storms. With a record low Southern Sierra snowpack, there was almost no chance that an ice axe would be required on Army Pass. I was familiar with the route on Langley and down from New Army Pass, and expected to be back to the car well before sunset. But, just in case, the moon was about half full.

Low snow year on Army Pass. June 23, 2007.
Low snow year on Army Pass. June 23, 2007.

In fact, there had been very little snow on Army Pass, or anywhere else. We reached the pass relatively quickly, and decided to continue to Langley. Now, after another hour of hiking, we were above a prominent rock band that extends across Langley’s south face, and making good progress.

I’ve been convinced for some time that pursed-lip breathing helps me at higher altitudes, particularly when I’m not well acclimated. There’s a skill to it. There seems to me an optimum blend of heart rate, respiratory rate, and the amount of resistance created on exhalation. When all these factors are in balance, the breathing technique is almost automatic and effortless, and it really does seem to help. It certainly seemed to be helping me now.

I topped out a few hundred yards west of the summit, and ambled over to the high point of the peak. On a scale of 1 to 10, I felt pretty good — maybe a 7. Making an effort to stay hydrated, consume plenty of calories, and not push the pace too hard seemed to have worked — at least this time.

The view along the crest to Mt. Whitney and the peaks of the Kings-Kern Divide was telling. It was remarkable just how little snow there was at the highest elevations of the Sierra. A week before I had been paddling the Kern River. Now I could see why the flow on the upper Kern was dropping so fast.

This wide-angle photograph of Mt. Whitney and the Sierra crest from the summit of Mt. Langley is from a high resolution composite of 8 individual images. It was created using the improved photo-merge tools in Photoshop CS3.

Big horn sheep on the slopes of Mt. Langley. June 23, 2007.
Big horn sheep on the slopes of Mt. Langley. June 23, 2007.

Miklos and Krisztina joined me on the summit, and after taking a few summit photos, we headed down. Screeing down the slopes below the rock band, we were startled when a herd of perhaps 20 big horn sheep rumbled across the slopes below us. They flowed across the rough landscape like quicksilver. Graceful and robust, they moved effortlessly between the rocks and up a small slope. In the moments it took me to react, grab my camera, and turn it on, all but two large rams trailing the group, had disappeared.

Energized by the sight of these fleet-footed animals, we continued down to the saddle at Army Pass, and then up and over New Army Pass. Before sunset we would be back to the car, and before dark, eating dinner at Lone Pine. Before midnight we would be back in L.A. Here’s a Google Earth image and Google Earth KMZ file of a GPS trace of our route.

Note: Going to higher altitudes without properly acclimating can result in very serious, life-threatening illnesses. There is much information available on the Internet regarding altitude sickness and acclimatization. As a starting point see UIAA Medical Commission – Advice and Recommendations and Wikipedia: Altitude sickness.

Related post: Cottonwood – New Army Pass Loop

Snowless San Gabriels

Ridge between Mt. Baden-Powell and Mt. Burnham in the San Gabriel Mountains. 
Ridge between Mt. Baden-Powell and Mt. Burnham

Standing on the summit of Mt. Baden-Powell (9399′), I squinted through the haze at Mt. Baldy (10,064′). Nope, no snow.

It’s not often that the highest elevations of the San Gabriel Mountains are snowless on Memorial Day weekend. If nowhere else, there will usually be a patch of white on the north side of Mt. Baldy. Two years ago there were 10-15 ft. drifts on Baden-Powell that persisted into July. Not this year.

This year, usually dependable water sources might not make it through the Summer. On the way to Baden-Powell I  stopped at Little Jimmy Springs. Descending to the spring, I didn’t hear the usual splitter-splatter of water streaming onto the rocks. For a worried moment I wondered if the spring could already dry.

It wasn’t dry, but the spring was nearly as low as it was in August 2002, following the driest water year ever recorded in Los Angeles. Whether Little Jimmy Spring will last through this Summer, after what is likely to be an even drier year, we’ll just have to see. To date, Los Angeles has received only 3.21 inches of rain since July 1, 2006, and will very likely break the record set in 2001-2002.

When on the trail between Islip Saddle and Mt. Baden-Powell, I almost always visit Little Jimmy Spring. The area surrounding the spring is lush and green, and in midsummer is accentuated with the yellows and reds of wildflowers. There are several impressive Incense Cedars nearby, and one huge tree must have enjoyed the idyllic setting and refreshing waters for at least a few centuries. The tree was threatened by the 2002 Curve Fire, but fortunately only a part of its fire-resistant trunk was burned.

At the spring, I filled my Camelbak to the brim. On the way back from Mt. Baden-Powell, I was planning to climb Mt. Burnham, Throop Peak, Mt. Hawkins and Mt. Islip. Most of these peaks are relatively easy ascents requiring short detours from the main trail. Mt. Islip requires a little more effort, and is about a mile by trail from Windy Gap.

According to my Forerunner 205, the distance from Islip Saddle to Mt. Baden-Powell is about 8.1 miles. Depending on how Islip is done, the total mileage including the five peaks is in the neighborhood of 17-18 miles, with an elevation gain and loss of about 4700′.

Note: Angeles Crest Highway (SR2) was open to Islip Saddle.

Related post: PCT Above Windy Gap.

San Joaquin Ridge

San Joaquin Ridge, near Mammoth Mountain.

Located near Mammoth Mountain, San Joaquin Ridge extends from Minaret Summit (9265′) north about six miles to San Joaquin Mountain (11,601′). Views from this ridge are legend, with broad vistas that include Mt. Morrison, Red Slate, Mammoth Mountain, the Minarets and Ritter & Banner, Mono Lake, and much more. In good weather it is an awe inspiring locale in which to hike, ski or run.


he Minarets, and Mts. Ritter and Banner from San Joaquin Ridge. May 21, 2007.
This day, the conditions for running the ridge are ideal. In the wake of a weak weather system, skies are mostly clear, and a cool breeze reduces the heat of the harsh sun, producing a welcome warmth. Winter snow is already receding from the ridge crest, allowing a choice of routes over, or around, remnant drifts and cornices.

Returning from a high point a few miles distant, bounding strides lengthen, and I seem to soar down the ridge, weaving among the stunted pines, glissading across bands of snow, caressing the wind and flying up or down slopes with equal ease. It has become a run that defines the root experience of trail running and the rewards of being in the mountains. There is freedom of motion — and emotion — in every stride.

Ahead of me, a pair of ravens turn and the Sun glistens from back to wing. Individual feathers ruffle as wings are adjusted to increase lift, and turns are tightened. Soon we are soaring high above the Sierra, and all things seem possible.

Three Points – Mt. Waterman Loop

Trail sign on the Mt. Waterman Trail in the San Gabriel Mountains.

Five miles of (mostly) downhill to go. Running through an old growth forest of Jeffrey Pine, Sugar Pine and Incense Cedar, I relished being on a pine needle covered trail at 7000 ft. in the San Gabriel Mountains.

In a record dry water year, I had been curious to see how the mountains were faring. Although creeks were very low and grasses dry, my impression was that groundwater resources were not quite as bad. The usual springs and seeps still muddied the trail. In 2005 the San Gabriel Mountains were deluged with rain, and in the 2006 the rainfall was nearly normal, so some carryover would be expected.

Update May 27, 2007. My impression of groundwater resources may have been overly optimistic. On a run to Mt. Baden-Powell from Islip Saddle, I stopped by Little Jimmy Spring. It was nearly as low as in late August 2002, when Los Angeles had just experienced its driest water year on record. This year will likely break the 2001-2002 record.

Even so, it was obviously much drier than normal. There were fewer wildflowers, and some young Incense Cedars looked as if they might be stressed. On the plus side, manzanita and currant were blooming in profusion, and perhaps 30-35 scarlet red stalks of snow plant were seen on the loop.

About three miles from Three Points I happened upon another Jeffrey Pine that had been struck by lightning. This strike appeared to more energetic than the bolt that struck the tree on the Baldy North Backbone Trail. The spiral scar was wider and braided at some points, and the strike ignited the tree. Where the Baldy tree was on a sharp ridge crest, this tree was several hundred feet below the main crest in an area where the trail started to work around a projecting ridge.

More about this loop and a Google Earth image of the course can be found in the post Manzanita Morning.

Strawberry – Bear Canyon Loop

Trail runner in Bear Canyon, in the San Gabriel Mountains.

The Strawberry – Bear Canyon loop trail run is a longer, more adventurous variation of the run around Strawberry Peak described in the post Strawberry Peak Circuit.

The photograph Fall Leaves On Bear Creek was taken on this loop in November 2005. As described in that post, instead of descending directly to Switzer’s from Red Box, this route descends the West Fork to Valley Forge Campground and then climbs up and over the shoulder of Mt. Wilson, and down into Bear Canyon, eventually working its way back to Switzer’s and Clear Creek.

Without any wrong turns or other route finding issues the loop works out to about 25.5 miles with an elevation gain and loss of about 5500-6000 ft. The running (and hiking) is extremely varied, including fire roads, old road beds, easy trail, technical trail, and lots of up and down. Bear Creek’s lush canyon is gorgeous, but 20 miles into the run, it’s winding course and many creek crossings can prove demanding.

I attempted to obtain a GPS trace of this route in 2005, but the steep, narrow canyons defeated my Foretrex 201. Not so with my Forerunner 205. I continue to be amazed at the 205’s performance. Here’s a Google Earth image and Google Earth KMZ file of the GPS trace of my route.

Related posts: Spring Growth, Fall Leaves On Bear Creek, Forerunner 205.