Chumash View II

View northwest to the Ventura Mountains from the Chumash Trail.

View northwest to the Ventura Mountains from the Chumash Trail. The highest peak on the skyline is Hines Peak (6716′), about 28 miles distant. Here’s a larger version of the 16:9 format image. Note the hawk soaring high above the terrain.

I run the Chumash Trail frequently, but had not seen the bulldozed track on the steep slope near the start of the trail. The trail hasn’t been re-routed. Apparently on the 13th a 4WD truck that was part of a fire department response to a cycling accident got stuck, and a bulldozer was called in to extricate the vehicle. I’ve been told the Park District and Mountains Conservancy are considering next steps.

Boney Mountain – Big Sycamore Canyon Circuit

The Conejo Valley from Boney Mountain.

I liked last weekend’s run so much that this morning I returned to the Wendy Drive trailhead on Potrero Road and was now chugging up the Danielson-Old Boney trail, planning to do another circuit that would eventually take me back down into Big Sycamore Canyon.

Wearing short-sleeves, and without water bottles or packs, a group of three runners passed me as I plodded up the road. I guessed they were headed for the Danielson Monument. That’s where I was going — at least to start. The previous week I had noticed a use trail continuing east from the Danielson cabin site. It was well worn, and a little research confirmed that it was a route up the north flank of Boney Mountain.

My plan was to see where the trail led. That sounds like a given, but trails like this usually have a character of their own, and can lead to interesting areas and variations that demand exploration. Last week a hiker had asked me about this route, and commented that he hoped his group would make it up this time.

It didn’t take long to reach the spur trail to the cabin and monument. I turned left and followed the gently descending trail into the canyon. Where were the other runners? About the time I was beginning to wonder if they were doing an impressively fast and light circuit through Sycamore, I heard fleet-footed voices headed my way. We passed each other at the bottom of the canyon, and I continued the tenth of a mile up to the cabin site and the beginning of my adventure.

The route up the mountain was spectacular! This was not a trail engineered on a piece of paper, but a route that went where possible, following the vagaries and whims of the terrain. A long, sweeping traverse deep in the chaparral would seek a distant ridge and then dive back into the brush before suddenly turning directly and steeply uphill. Views of the valley grew more expansive with each step, and eventually I gained the first summit, marked 2701 ft. on the topo.

From here the trail followed a dramatic ridge, ascending a series of peaklets to a high point at about 2900′, across a canyon and to the north of Tri-Peaks (3010′). My immediate goal was to cross over to Tri-Peaks. From there I would find my way to the Backbone Trail.

What had been a well trodden path, now became less distinct. From my viewpoint, a route up the north side of Tri-Peaks looked improbable. Choked with brush and trees, the peak was an amalgam of massive volcanic blocks and boulders, fused with chaparral.

Following the crest of the Boney Mountain escarpment, I dropped down to a saddle. To my right, the terrain plunged between steep cliffs to Big Sycamore Canyon, more than 2500′ below.

Unsure of the route, but endorphin energized, I followed a path up and into a maze of corridors and rooms among the towering rock formations, eventually emerging at the summit block. Working my way out of the shadows, I traversed around to the south side of the peak. From here the Tri-Peaks trail was an obvious slash in the brush and in a few minutes I was on the Backbone Trail, headed west.

The downhill running on this section of trail is among the best in the Santa Monica Mountains, with memorable views of Boney Mountain’s massive western flank. In five miles and a nearly effortless hour I was down to the Danielson multi-use area.

I stopped for water and briefly debated how far to run down Big Sycamore. Not far — I picked up the Ranch Center fireroad (unpaved) and followed it up to the Hidden Pond trail, finishing the run like last week, on the Upper Sycamore and Danielson/Old Boney trails.

Here’s a Google Earth image and KMZ file of a GPS trace of the approximately 18.5 mile route.

Related post: Big Sycamore Canyon Circuit

Return of the Afternoon Sun

Sunset from the Chumash Trail, Simi Valley, California.

Those of us in the northern hemisphere that enjoy afternoon daylight are celebrating the passing of the dank days of Autumn when sunset occurs the earliest in the day. Depending on your location, the amount of afternoon daylight may already be increasing — be it ever so modest.

According to the Astronomical Applications Dept. of the U. S. Naval Observatory, in Los Angeles that day is today, December 11, when the sunset shifts from 4:44 p.m. to 4:45 p.m.

The more northerly your latitude, the later the date. In Miami it was back on December 4, and in Seattle it will be on December 18. In Anchorage it won’t be until December 20. Barrow, Alaska won’t see a sunset (or sunrise) until January 23!

You can check your city’s sunset times using the USNO Sun or Moon Rise/Set Table.

Big Sycamore Canyon Circuit

Rancho Sierra Vista/Satwiwa and the Conejo Valley with snow on the peaks of the Ventura mountains

I was about a mile from the Wendy Dr. trailhead on Potrero Rd. in Newbury Park. A cold wind ruffled the chaparral, and to the north snow could be seen on McDonald Peak (6870′) and other peaks of the Ventura mountains. I was nearing the top of a rounded ridge in Rancho Sierra Vista/Satwiwa, and in a few minutes would be descending the sun-warmed Old Boney Trail into the upper reaches of Big Sycamore Canyon.

Big Sycamore Canyon extends from the ocean to within a mile or so of Potrero Rd. It forms the main trunk of an extensive network of trails in Pt. Mugu State Park. Of the many possible trail combinations, my loosely defined plan was to link some of the trails on the XTERRA Boney Mountain Trail Run course into a longer run.

The general idea was to start on the Old Boney and Blue Canyon Trails, and return via the Hidden Pond and Upper Sycamore Canyon Trails. I was looking to do about 20 miles, and wasn’t sure how far down Big Sycamore I would run, or what other trails I would do.

The run up and over the shoulder of Boney Mountain was brisk and blustery. On the way I checked out the waterfall spur trail and the Danielson cabin site and monument. At one point, several miles into the run, the trail rounded a ridge and descended into a bowl at the head of a broad canyon. Here, the character was unmistakably that of the wilderness — isolated and wild with the chaotic western escarpment of Boney Mountain towering above.

About two hours into the run I pulled into the Danielson multi-use area in Big Sycamore Canyon. There’s a water spigot here, adjacent to a fireplace in a low-walled picnic area. While topping off my Camelbak, I noticed a runner on nearby Big Sycamore Canyon road, then another, and another. A continuous stream of runners was passing by — I had forgotten that the Lasse Viren 20K was this weekend!

Down in the canyon the weather was perfect for the race. Swept along by the wave of runners, I missed my connection with the Two Foxes trail, and it wasn’t until the aid station at Wood Canyon road that I turned off the race course. Within a couple hundred yards I happened upon the southern end of the Two Foxes trail and worked my way back up the canyon about half a mile to the bottom of the Coyote Trail.

The previous evening I had taken a look at the Tom Harrison Santa Monica Mountains West Trail Map and noted that the Coyote Trail, Hidden Pond Trail, and Upper Sycamore Trail could all be linked together in one long single track extravaganza.

I had not done these three trails and enjoyed the exploratory feel. The Coyote Trail and Hidden Pond trails were outstanding, with excellent running and highline views. The Upper Sycamore trail is classically riparian, winding its way among white-barked sycamores and stream rubble, in a stream eroded canyon to its junction with the Old Boney Trail about 1.5 miles from the Wendy Drive trailhead.

Here’s a Google Earth image of a GPS trace of the approximately 19 mile route.

Fox Mountain Frost

Hollow columnar hoarfrost deposited on leaves and twigs on Fox Mountain in the San Gabriel Mountains, near Los Angeles.

When I see crystals of hoar frost sparkle in the Winter sun it triggers a child-like awe. On Sunday’s Condor Peak Trail Run, several sections of trail glittered as we ran into a low morning sun. On the cold east face of Fox Mountain, a fine, needle-like frost coated the edges and surfaces of leaves and twigs that had collected in pockets on the steep slope.

Digitally magnifying a small section of a 10 Mp image revealed that the frost is comprised of  hollow columns, and further magnification shows that the columns are hexagonal, with lengthwise facets.

This type  of frost – hollow columnar hoarfrost – is described in STUDIES OF FROST AND ICE CRYSTALS by W.A. Bentley, in the Monthly Weather Review, Volume 35, Issue 9 (September 1907), pp. 397-403. Here is an excerpt:

“When formed in the open, they are essentially mild-weather types. They are most common to early autumn and late spring, and the hoarfrost that collects upon the plants and grasses during the so-called destructive frosts at those dates is almost invariably of this type. Hoarfrost deposits of this character form in the open during calm, clear nights when the surface air temperatures range from 56 degrees to 40 degrees at nightfall, and from 33 degrees to 25 degrees during the latter part of the night or early morning.”

Here is a graph of weather data recorded by the Mill Creek (ANF) RAWS on December 1 and December 2. The elevation of the station is 3510′ and it is about 8.5 miles from Fox Mountain (5033′). Parameters graphed are the hourly average wind speed, air temperature, fuel temperature, relative humidity, and dew point.

At Mill Creek the fuel temperature dropped below the frost point at 10:00 p.m Saturday, and did not exceed the frost point again until 8:00 a.m Sunday. For a 5 hour period from 2:00 a.m. to 7:00 a.m. the mean air temperature was 30°F-31°F and the fuel temperature was 22°F-23°F — suggesting strong radiative cooling. Similar conditions probably produced the frost on Fox Mountain.

Condor Peak Trail Run

Trail runner on the Condor Peak Trail as it nears Condor Peak.

The temp was in the 30’s and it took a couple of minutes for my car’s engine to warm enough to thaw the coating of ice on the windshield. I was headed for a run in the San Gabriel Mountains and was wondering how cold it might be.

In a November in which 29 days had been bone dry, it had rained on the 30th, and temps had cooled dramatically. That was day before yesterday. This morning the sky was still a storm-cleansed blue, and except for a few passing high clouds, promised to stay that way. If the winds were not too brisk, it could be one of those invigoratingly crisp late Autumn days — cold in the shadows, but warm and pleasant in the sun.

About an hour later Miklos and I were working our way up the Condor Peak Trail (13W05), not far from the trailhead on Big Tujunga Canyon Road. At the parking area I had shed some extra layers and was now running in shorts and a light long-sleeve top. In the pack were an ultralight shell, gloves, and a headband.

About a 1/4 mile from the parking area we caught up to some hikers and their dogs. They asked us if we were headed “to the top.” I replied that we were doing Fox Mountain and Condor Peak, and would continue on to the Trail Canyon Trail.

“Do you have a car at the Trail Canyon trailhead?”

“Yep…”

“You know it’s 17 miles, right?”

“Yep…”

Twenty minutes into the run, we reached the point where the old trail jumps up from Big T and joins the main trail. From here we turned north, away from the highway, and began a long, winding, uphill course that would eventually reach the divide between Fox Mountain (5033′) and Condor Peak (5440’+). This meandering approach resulted in a very runnable section of trail that gains about 2500′ in 5.5 miles — an average 8.6% grade.

As the trail wound in and out of canyons, and from shadowed to sunny slopes, the temperature contrasts were startling. Within a few feet, we would stride from balmy, solar heated granite alcoves into frosty, refrigerated nooks near freezing. We estimated the difference in temperature to be 30-40 degrees.

Gradually we gained elevation, and in about an hour and a half we crested the broad divide at the base of Fox Mountain. From this point a short — but steep — path leads directly to Fox’s summit. 

Deep in morning shadow, the east side of the peak was cold! The ground was frozen, and heavy frost covered fallen leaves of chaparral. A few strenuous minutes and we were atop the peak, relishing the warmth of the sun and the panoramic view. Mt. Lukens, Josephine Peak, Strawberry Peak and Mt. Wilson loomed nearby. Further to the east, beyond Mt. Waterman and Twin Peaks, Mt. Baldy glistened white with a new coat of snow. Dressed for running, and damp from the climb, chill breezes hurried us from the summit.

Peak to peak the distance from Fox to Condor is over two miles. That’s what the map says, but on the ground Condor looks deceptively close. Several false summits amplify the deception, and many a hiker has been deceived. Even having viewed the route from Fox and climbed the peak before, I still did not fully appreciate the distance.

The scramble up Condor was a little longer than the hike up Fox. The peak has twin summits at very nearly the same elevation. We were curious which summit would have the register and found it on the more westerly summit. To do both Fox and Condor only added about an hour to our run.

Once down from Condor Peak it took about twenty minutes to hoof it over to the Trail Canyon Trail (13W03) junction. From here the trail drops about 3110 ft. in six miles. The grade of the trail is steeper than the Condor Peak trail, and a little more rocky and technical. Where the Condor Peak trail seeks the high lines, the Trail Canyon trail follows a creek and plunges into a deep riparian canyon.

Back at the car we marveled at what an enjoyable run it had been. The perfect weather and nearly ideal grade of the trails seemed to make the run almost effortless. It isn’t always that way.

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

Note: Although the Trail Canyon drainage is relatively small, it appears to have generated some sizable flash floods and debris flows. The canyon forms a huge southwest facing “rain catcher.” During Winter storms, the canyon wrings water from moisture laden wind as it is funneled into and up its slopes.

Photography and inspiration from running and other adventures in the Open Space and Wilderness areas of California, and beyond. No ads. All content, including photography, is Copyright © 2006-2024 Gary Valle. All Rights Reserved.