Gary Valle's Photography on the Run

Ahmanson Ranch Moonrise

Gary Valle — Sat, 15 Nov 2008 17:23:21 GMT

From a run at Ahmanson Ranch, now Upper Las Virgenes Canyon Open Space Preserve, Wednesday evening.

Fossil Trail - Pt. Mugu State Park

Gary Valle — Wed, 12 Nov 2008 00:16:53 GMT

The Fossil Trail is a steep, approximately mile-long trail in Pt. Mugu State Park that connects the Upper Sycamore Trail, near its junction with Sycamore Canyon Road, to the Old Boney Trail. The most obvious fossils are shell impressions and remnants found in an exposed layer of sandstone about a tenth of a mile below the Old Boney Trail junction.

The shells appear to be a type of cockle (Anadara devincta) that is an indicator of Miocene-age formations. (See the Oregon Sea Grant publication "Fossils You Can Find on Oregon Beaches.") In this case, the fossil exposure appears to be in the Lower Topanga Formation, which is believed to have been formed in the middle to early Miocene, about 20 million years ago.

The shape, thickness and ribbing of this type of shell increases its strength and resistance to crushing -- improving the shell's chances of remaining intact when buried in sediment, and during subsequent geologic processes. This may be one of the reasons it is a prevalent indicator fossil.

The photograph is from Sunday's run from Wendy Drive to Serrano Valley.

Serrano Valley from Wendy Drive

Gary Valle — Mon, 10 Nov 2008 00:05:09 GMT

Scruffy clouds clung to the mountain ridges and summits, confirmation that a weak cold front was moving through the area, cooling temperatures and stirring up the wind. The forecast for the Santa Monica Mountains National Recreation Area had mentioned 25 to 35 mph winds with gusts to 60 mph. So far the weather in Pt. Mugu State Park had been nearly perfect -- breezy and little chilly, but without the impenetrable winds that can take all the joy out of running.

Earlier we had climbed the Fossil Trail, a steep mile-long trail that connects the Upper Sycamore Trail, near its junction with Sycamore Canyon Road, to the Old Boney Trail. With only a few weeks remaining to the Solstice, shadows in the canyon were long and the light wintery. I thought we might have missed the fossils, but we happened on a nice exposure about a tenth of a mile below the Old Boney Trail junction.

About 5.5 miles later, we turned off the Old Boney Trail and descended to the rolling grasslands of Serrano Valley, another "must see" area of the Santa Monica Mountains.

Located on the east side of Big Sycamore Canyon, Serrano Valley is a more rugged counterpart to La Jolla Valley, just three miles to the west. Overseen by the castle-like summits of Boney Mountain, its vistas have a roughhewn edge, reminiscent of the most wild areas of the western U.S.

Here is a Google Earth image and Google Earth KMZ file of a GPS trace of our approximately 19 mile route to Serrano Valley and back to Wendy Drive.

Sesnon Fire Recovery - First Growth

Gary Valle — Thu, 06 Nov 2008 15:57:38 GMT

Only three weeks after the area was burned in the 2008 Sesnon Fire, this yerba santa shrub on the Chumash Trail has started the process of foliage replacement. In many areas along the trail, grasses and other annuals (many invasive) were consumed, but adjacent chaparral shrubs were only scorched. Many of these shrubs look like they will be able to recover through budding of existing stems, rather than crown-sprouting.

Simi Valley from Rocky Peak

Gary Valle — Sun, 02 Nov 2008 16:39:59 GMT

A view of the eastern Simi Valley and Simi Hills from Rocky Peak.

From a run in Rocky Peak Park today.

T-storms and Trail Work

Gary Valle — Sat, 01 Nov 2008 19:50:44 GMT

When I woke to the rumble of thunder, rain pounding the roof, and wind roaring in the trees, I wondered if a planned run of the Boney Mountain Half Marathon course with John Dale was going to turn into an epic. Radar and satellite imagery showed subtropical moisture streaming in from the southwest, producing bands of showers and thunderstorms. Things don't always look as bad at the trailhead as they do on weather radar, so I grabbed my gear and headed for Wendy Drive.

The weather looked promising driving through Agoura, but the further west I drove, the more ominous the skies became. Somewhere around Lynn Road KNX announced that the NWS had issued a severe thunderstorm warning for the Santa Clarita area, with cloud to ground lightning, heavy rain, possible damaging winds and dime-sized hail. It was with that thought in mind, and a shower pelting the car, that I pulled into the parking area on Potrero Rd.

If anything, weather is fickle, and sometimes that quirkiness can work for you. There was an area of heavy rain to the west, but the activity appeared to be skirting the area, so we opted to start the run.

There were a few sprinkles as we jogged down the blacktop into Big Sycamore Canyon, and a few more as we did the first easy mile of the Hidden Pond Trail. Down in the canyon it was hard to tell what the weather was doing, but after gaining some elevation we reached a better vantage point. Just a few miles away thunderstorms were being swept northeast from the Santa Barbara Channel, across the Oxnard Plain, and into the Ventura Mountains.

Skies darkened and the shower intensity increased as we ran down Ranch Center Fire Road. The wind was blowing in the fitful gusts that precede a thunderstorm, and it felt as if the sky might fall at any moment. With a slight shift in the track of the thunderstorms we might be running in a deluge, dodging lightning strikes.

But it didn't shift. Following the shower, the sun broke through the clouds just long enough to add glints to the raindrops dripping from the leaves of sycamores and oaks in Blue Canyon. Under overcast skies, we climbed up the Old Boney Trail and into the Boney Mountain Wilderness.

We had not seen a hiker, runner, or rider since turning onto the Hidden Pond Trail early in the run. So it was a bit of a surprise when we rounded a corner and ran into Ed Reid and several other volunteers with the Santa Monica Mountains Trails Council doing trail maintenance on a section of the Old Boney Trail.

Just about any weekend of the year, dedicated members of the SMMTC will be somewhere in the Santa Monica Mountains, working on a trail. To get a better idea of the amount of work done and the number of trails involved, take a look at this list of recently maintained trails! How many of these have you hiked, run or ridden?

There are several ways to help support SMMTC:

Volunteer to do trail maintenance.
Join the SMMTC.
Make your REI purchases using the REI link on the SMMTC web site. REI will donate a percentage of the purchase to SMMTC.

See the Santa Monica Mountains Trails Council web site for more info.

Some related posts: Boney Mountain Half Marathon, Return to Hidden Pond

Southern California 2008-2009 Winter Precipitation Outlook

Gary Valle — Fri, 31 Oct 2008 16:16:04 GMT

Downtown Los Angeles (USC) happened to be under the right cloud yesterday, and recorded 0.02 inch of rain. There's a continuing chance of showers in Southern California through the weekend. The area could use some rain. The last storm to produce more than a couple tenths of inch of rain at Downtown Los Angeles was back on February 24, 2008 -- more than eight months ago.

Last year, California's rain season might have been scripted by Dr. Jekyll and Mr. Hyde. Lowland rain totals and the Sierra snowpack were well above normal through the end of February, and then the spigot was turned off. The storm track shifted north, and California had its driest March to May on record. (The March 29, 2008 post in Ed Berry's Atmospheric Insights blog describes the events that may have led to and maintained this shift.)

Which rain season personality will surface this Winter? Earlier this year the equatorial Pacific tried to transition to El Nino, but the atmosphere didn't cooperate. As measured by the Multivariate ENSO Index (MEI), the ENSO state has returned to the weak La Nina threshold. And as measured by the Global Wind Oscillation (GWO), an uncooperative atmosphere has continued to cycle through a La Nina base state.

This suggests a winter precipitation outlook with a La Nina flavor -- similar to last year. This precipitation map, generated by the ESRL-PSD Composite ENSO plots page, shows the mean November-March precipitation for the U.S. during 9 La Niña events from 1948 to the present. The average La Niña rainfall indicated for coastal Southern California is in the 7.0-10.5 inch range. Last season's November-March rainfall in Downtown Los Angeles was about 12 inches.

Here's the current Nov-Dec-Jan precipitation outlook issued October 16 by the Climate Prediction Center. The "EC" means an equal chance of below normal, near normal, or above normal precipitation. The IRI Multi Model Seasonal Forecast for Nov-Dec-Jan is similar. We'll see what we get!

Rocky Peak After the Sesnon Fire

Gary Valle — Sun, 26 Oct 2008 14:28:15 GMT

My run to "Fossil Point" on Rocky Peak road, and side trip to Rocky Peak, was not the appalling experience I've come to expect when investigating a wildland area that has been overrun by a Southern California brush fire. Much of the chaparral along the fire road was not burned. Here are a few photos:

View southeast toward Porter Ranch from the summit of Rocky Peak (larger image).

View north toward Rocky Peak where the trail levels out, about 1.4 miles from the trailhead.

Burned area near viewpoint of Simi Valley about 2.3 miles from the trailhead.

View north from the summit of Rocky Peak. Rocky Peak fire road is on the far left, and the Johnson trail is on the right.

Unburned area along Rocky Peak fire road about 2.8 miles from the trailhead. Rocky Peak is the peak on the left.

False color image of slopes on the southwest side of Blind Canyon. The image has been modified to emphasize burned and unburned areas.

Chumash Trail - Sesnon & Simi Fires

Gary Valle — Fri, 24 Oct 2008 23:43:48 GMT

This weather worn sandstone boulder is a familiar landmark to those who do the Chumash Trail. It's a little less than a mile up the trail, and is at the point where the trail turns east and continues its climb along a cobble strewn divide. The chaparral here and elsewhere along the Chumash Trail was burned last week by the western flank of the Sesnon fire.

In the areas bordering the Chumash Trail, the Sesnon Fire appears to have been much less intense than the 2003 Simi Fire. In the case of the Simi Fire, it had been about 15 years since the area was burned, the fuel load was moderately high, and the fire intensity was such that nearly all plant materials were consumed down to the mineral earth.

Recovery from the Simi Fire has been primarily through the slow processes of basal-sprouting and seed germination. Just prior to the Sesnon Fire, common chaparral plants such as chamise, yerba santa, toyon and holly-leaved cherry had recovered about 70% to 90% of their 2003 size.

The recency of the Simi fire appears to have reduced the fuel load available to the Sesnon Fire. In many cases grasses and other annuals (many invasive) were consumed, but adjacent chaparral shrubs were only scorched. Many of these shrubs look like they will probably be able to recover through foliage replacement, rather than crown-sprouting. One exception might be laurel sumac, which appears to have been less fire tolerant.

In addition to reducing the fire danger, a little light rain would help jump start the recovery process. Computer weather models have been hinting at a change in the weather around November 1, and now seem to be converging on the possibility of a shower in Southern California around Halloween, followed by a front and some rain later in the weekend. That's still a week away, so we'll have to see!

Here's a Google Earth image and Google Earth KMZ file of the perimeters of the Sesnon and Simi Fires, as well as GPS traces of some of the trails in the area.

Manzanita Red

Gary Valle — Sat, 18 Oct 2008 23:08:34 GMT

From the Boney Mountain loop a couple of weeks ago.

La Jolla Valley & Mugu Peak from Wendy Drive

Gary Valle — Sun, 12 Oct 2008 21:20:16 GMT

The scat appeared to be a day or two old, and was much bigger than a coyote's. It was full of fur and could only be from one animal -- a mountain lion. The spot had been used before, and it probably wasn't a coincidence that this was one of the few points along the trail with a good view and nearby cover. I looked into the brush and wondered if unseen eyes looked back.

The sun was well above the horizon, but the first gusts of a developing Santa Ana wind kept the morning cool. No one was on the trail ahead or behind me, and the best I could tell, I was the only two-legged creature within sight.

Walking slowly from the spot, I surveyed the secluded valley. Perched on the edge of the coastal mountains, La Jolla Valley is extraordinary. Surrounded by wind-sculpted peaks, it is situated above and to the west of Big Sycamore Canyon. Its bottom is carpeted with areas of native and non-native grass. Only a tiny percentage of California's native perennial grasslands remain, and like the big trees, they are relics of the past. Preservation of this native grassland is probably due to the valley's proximity to the ocean, and its unique microclimate.

Here, trails have been run and peaks climbed for thousands of years. (Charcoal at an archaeological site in the valley has been dated to a maximum age of 7000 B.P.) Above me a raven calls, and Spirit-like, a gust of wind rustles through the grass. Respectfully, I continue running in the direction of Mugu Peak.

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The run from Wendy Dr. was more moderate than expected. The first 3 miles of Sycamore Canyon Fire Road are paved, and whether on the fire road, or the single track trails that parallel the road at times, a fast pace can be maintained down to the junction with Wood Canyon Fire Road.

The Wood Canyon Vista Trail/Backbone Trail takes off right (west) from Sycamore Canyon Fire Road a short distance past the Wood Canyon Fire Road junction. It is moderately graded and very runnable. At it's top a short zig right (north) on the Overlook Fire Road leads to the La Jolla Valley Fire Road, which can be followed left (west) down into La Jolla Valley.

Many, many variations of this course are possible. Here's a trail map from the La Jolla Valley Natural Preserve web page. Depending on whether you want the beta, a little time in Google Earth should help clarify the options. This particular course worked out to about 21 miles, with about 2200 ft. of elevation gain/loss. Here's a Google Earth image and Google Earth KMZ file of a GPS trace of my route.

Boney Mountain - Big Sycamore Canyon Circuit - Coyote Trail Variation

Gary Valle — Sun, 05 Oct 2008 15:44:39 GMT

It's fun to link together several trails into a loop, and it's even more fun when the trails are single-track, or at least have a single-track flavor. The Boney Mountain - Big Sycamore Canyon circuit links together segments of more than ten trails and roads in Rancho Sierra Vista/Satwiwa and Pt. Mugu State Park. The route is characterized by airy ridges, steep climbs, wide-ranging views, towering rock formations, and one of the best downhill running segments in the Santa Monica Mountains. Today's run expanded the loop, adding even more single-track trail -- and elevation gain.

This route also climbs over Boney Mountain and descends the Chamberlain Trail segment of the Backbone Trail. However, at the Old Boney Trail junction, instead of descending to the Danielson multi-use area on the Old Boney Trail (northbound) and Blue Canyon Trail, this route follows the Old Boney Trail (westbound) to Sycamore Canyon Fire Road.

From the junction of the Old Boney Trail with the Sycamore Canyon Fire Road the goal is to hook up with the Coyote Trail, which can be seen switchbacking steeply up a slope on the other side of the canyon. We did this by continuing about 0.5 mile down Sycamore Canyon Fire Road, and then turning right on Wood Canyon Fire Road. The Two Foxes Trail starts a short distance up the fire road, and in about 0.4 mile leads to the start of the Coyote Trail. Once on the Coyote Trail it is about 2.3 tough -- and often hot -- miles to the start of the Hidden Pond Trail at Ranch Center Road. The rest of the route is the same as in the Boney Mountain - Big Sycamore Canyon circuit.

All in all the course is about 21 miles long, with 4000 ft. of elevation gain/loss. Here's a Google Earth image and Google Earth KMZ file of a GPS trace of the route.