Chumash Rock


Rock formation northwest of the Chumash Trail.
Rock Formation Northwest of the Chumash Trail


Practically any objective can make a good excuse for an adventure. Each time up or down the Chumash Trail, I pondered the prominent rock formation northwest of the trail, and wondered what I might find there.


My first thought was to find a direct route across the deep canyon that parallels the Chumash Trail. Recons from a couple of points on the trail revealed that the this was a bad idea. Sections of the canyon that looked passable from above were incised, with crumbling, near-vertical walls. A Plan B was required.


A look at a topo map suggested it might be possible to access the ridge on which the formation was located from Las Llajas Canyon. An advantage of this approach was that, if it worked, it would be part of a loop. A cool January morning, I decided to give it a go.


From Las Llajas Canyon, an old overgrown roadbed led up a side canyon to a point where there was no obvious route. The canyon bottom did not look promising, and steep slopes bounded both sides of the canyon. After scrambling several hundred feet up a south-facing slope, I found a deer trail that seemed headed in the general direction I wanted to go. This game trail was the key. Its route reflected the cumulative experience of deer in dealing with the terrain issues I faced. It turned out to be remarkably efficient, and appeared to represent the path of least energy needed to reach the main ridge. That is, if you’re a deer. At one point I was forced to backtrack and climb above the trail when it crossed a steep, exposed slope better suited to those with four legs and cervid hooves.


Once up on the main ridge, it didn’t take long to reach the rock formation. According to the Dibblee geological map of the area, the formation is positioned on the south branch of the Simi Fault. The steeply inclined beds of river cobble seen in this photo might have been deposited as part of a fan delta some 60 million years ago. This Paleocene age cobble is also encountered at several places along the Chumash Trail.


Near the summit of the formation some chiseled inscriptions  were found. They were very weathered. The most prominent might be either a “93” or “33” over the top of a “W,” and another is perhaps a “DH.” It’s hard to tell.


Of the three high points comprising the formation, I scrambled to the top of two. The eastern-most summit (on the far right when viewed from the Chumash Trail) is wholly comprised of cobble and looked like an accident waiting to happen. Here’s a photo from near the summit of the formation, looking back down the ridge.


As I climbed down from the summit to a saddle northeast of the rock formation, I spooked a deer and it bounded into a brush filled gully. Continuing up the ridge, it eventually intersected Rocky Peak Rd. at its high point near some bivalve fossil beds. According to the Dibblee map, these are much younger than the rock formation’s river cobble, and may have been deposited in shallow marine conditions or lagoons a couple million years ago.


At Rocky Peak Rd. I had the option of returning via Las Llajas Canyon, but opted to complete the approximately 8 mile route via the Chumash Trail. This Google Earth image  shows most of the route. (Photographs from hike & run on January 29, 2006.)

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Owl’s Clover


Owl's Clover, in this case Castilleja exserta, is a fairly common California native.


A close view of Owl’s Clover reveals the probable reason for the name — fat little purplish-pink owls, crowned with a tinge of yellow, perched amid the purplish-pink of this unusual blossom. Here’s an even closer view of one of the individual flowers, showing its remarkable structure.


Owl’s Clover, in this case Castilleja exserta, is a fairly common California native that seems to prefer the margins of dirt roads and other disturbed areas at lower elevations. It’s in bloom now in the Santa Monica Mountains and Simi Hills. I noticed some on the Bulldog loop while running the Malibu Creek Challenge on Saturday, and also while doing a short run out a Sage Ranch Sunday.


This photograph is from a run at Sage Ranch on May 2, 2005.

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Olancha Peak Sierra Panorama

Part of the Panorama from Olancha Peak.

Part of the Panorama from Olancha Peak

Olancha Peak (12,123 ft.) is the prominent, pyramidal peak seen on the Sierra crest from Hwy 395, south of Olancha. Its rocky summit is above tree line, and in some years snow can persist in the east-facing summit gullies and other sun-protected areas into late June, or early July.

There are better choices for a run in the Sierra, but early in the summer when the passes on other routes are blocked by snow, Olancha may be passable. Views from the summit of Olancha Peak are expansive, and the running on the PCT was enjoyable. Round trip, the distance is an arduous 20 miles, with over 6300 ft. of elevation gain and loss.

The trail starts at Sage Flat, at a relatively low elevation of 5800 ft. As a result, in warm weather it can be hot and dusty. In addition, the trail segment up to Olancha Pass (9200 ft.) can have a lot of pack train traffic. To lessen the chance of encountering horses or mules on the trail, I opted to follow a very steep and rough “cow driveway” that shortcuts 1.3 miles of the trail up to Olancha Pass. It’s hard to imagine driving cattle up this swath, and judging from the cow femur I saw sticking up from the rubble, the cattle don’t find it so easy either.

Beyond Olancha Pass, the aesthetics improve, and a spur trail is followed northwest along Summit Meadow to a junction with the Pacific Crest Trail. The PCT eventually leads to the west slopes of Olancha Peak, and from here the summit is a short second class scramble. Here’s a Google Earth image and Google Earth KMZ file of a GPS trace of my route.

This summit panorama is from a run on June 26, 2005. The view shows the headwaters of the N.F. and S.F. Kern River, and the high peaks of the Southern Sierra. From south (left) to north (right) are the Little Kern, the N.F. Kern near Hole in the Ground, Kern Peak, the Great Western Divide, the Kaweah Group, Junction Meadow, Mt. Whitney, and Mt. Langley.

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Collective


Lichens on Chatsworth Formation sandstone at Sage Ranch.


Lichens are composite lifeforms, usually comprised of a fungus and algae, or a fungus and cynobacterium. Generally, the fungus provides shelter and needed minerals, and the algae, using photosynthesis, provides food. This community is on Chatsworth Formation sandstone at Sage Ranch.


There is a tendency to think of living things, including ourselves, in the singular. But most life is a intertwined assemblage of cooperating organisms, from the very small to the very large, living in harmony. Circle within circle, life within life.

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Complications

This photograph was taken October 23, 2005, on one of my favorite loops in the San Gabriel Mountains. This adventurous route starts at Islip Saddle, follows the South Fork trail down to South Fork Campground, then takes the Manzanita Trail up to Vincent Gap and the Pacific Crest Trail. From here, the PCT is followed up, and with a slight detour, over Mt. Baden-Powell, and then along the crest of the San Gabriels back to Islip Saddle. It’s a very wild and scenic 23 mile run that covers a wide range of elevations. South Fork Campground is at 4,560 ft., and the summit of Baden-Powell is at 9399 ft. Total elevation gain and loss on the run is well over 5000 ft.

This year, it might make more sense to start this loop at Vincent Gap. In order to protect critical habitat of the mountain yellow-legged frog, the Forest Service has closed 1,000 acres in the upper Little Rock Creek drainage, including Williamson Rock, and the PCT between Eagle’s Roost and the Burkhart Trail. In addition, Angeles Crest Highway (SR2) is now closed at Cedar Springs, just west of Eagles Roost.

Update May 21, 2009. Angeles Crest Highway (SR2) has since been re-opened to Islip Saddle, and through to Wrightwood.

Following are links to PDF maps of the closure area and the PCT detour. For more information see the News section of the Angeles National Forest web site. For more information regarding the closure of Williamson Rock, see the Friends of Williamson Rock web site.

The post Wally Waldron Limber Pine includes links to a Google Earth image and Google Earth KMZ file of this route.

PLEASE NOTE: The condition of certain sections of the Manzanita and South Fork trails is marginal, and rock slides and washouts may block the trail.

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Snow Plant Still Life

A snow plant and other forest floor elements highlighted by a shaft of sunlight.

A snow plant and other forest floor elements highlighted by a shaft of sunlight. The photo was taken on a rambling out and back run of about 25 miles from the lower McGill trailhead to Mt. Pinos and Mt. Abel on July 24, 2005.

Here’s a Google Earth image and Google Earth KMZ file of a GPS trace of my route.

For additional snow plant photographs, see the posts Three Points – Mt. Waterman Loop and Snow Plant, and also Snow Plant on SierraPhotography.com.

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Images taken on trail runs, and other adventures, in the Open Space and Wilderness areas of California, and beyond. All content, including photography, is Copyright © 2006-2017 Gary Valle. All Rights Reserved.