Caterpillar Phacelia

Caterpillar Phacelia (Phacelia cicutaria)


Caterpillar Phacelia (Phacelia cicutaria) was prevalent at Sage Ranch prior to the 2005 Topanga Fire. It may be somewhat more widespread than I’ve generally seen, but this could be due in part to last year’s record rainfall and this season’s late rainfall. It doesn’t appear to be a fire follower in the same sense as Large Flowered Phacelia, Star Lily or Dicentra, whose populations have increased dramatically this year.

Facebooktwittergoogle_pluspinterestlinkedinmailFacebooktwittergoogle_pluspinterestlinkedinmailby feather

Spring Growth

New growth on a Big Cone Douglas Fir (Pseudotsuga macrocarpa) in the San Gabriel Mountains.

Bright green highlights new growth on a Big Cone Douglas Fir (Pseudotsuga macrocarpa) in the San Gabriel Mountains near Josephine Peak and Strawberry Peak.

These peaks are popular lower elevation summits, that can be snow-free in Winter, or a blast furnace in Summer. Josephine Peak (5558 ft.) was once the site of fire lookout, and a fire road leads from Clear Creek Station to its summit. From the west, via Clear Creek or Colby Canyon, Strawberry Peak (6164 ft.) is a more difficult ascent that requires careful route-finding and rudimentary rock climbing skills. Many hikers prefer to do Strawberry from the east, starting at Red Box.

The day this photograph was taken, I wasn’t climbing Strawberry Peak, but instead was running a circuit around the peak. Part of the Mt. Disappointment 50K course, the circuit is an excellent 15 mile loop with an elevation gain/loss of about 2700 ft. Here’s a Google Earth image and Google Earth KMZ file of a GPS trace of the Strawberry Peak Circuit. A longer variant of this route is described in Fall Leaves on Bear Creek and Strawberry – Bear Canyon Loop.

Facebooktwittergoogle_pluspinterestlinkedinmailFacebooktwittergoogle_pluspinterestlinkedinmailby feather

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.)

Facebooktwittergoogle_pluspinterestlinkedinmailFacebooktwittergoogle_pluspinterestlinkedinmailby feather

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.

Facebooktwittergoogle_pluspinterestlinkedinmailFacebooktwittergoogle_pluspinterestlinkedinmailby feather

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.

Facebooktwittergoogle_pluspinterestlinkedinmailFacebooktwittergoogle_pluspinterestlinkedinmailby feather

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.

Facebooktwittergoogle_pluspinterestlinkedinmailFacebooktwittergoogle_pluspinterestlinkedinmailby feather