The posts Boney Mountain - Big Sycamore Canyon Circuit and Boney Mountain Western Ridge & Loop describe two routes that ascend the north side of Boney Mountain -- a circuitous eastern ridge route, and a more difficult western ridge.

These two routes can be combined into an adventurous loop that starts and ends at the junction of Danielson Road and the Old Boney Trail. The loop, with no side trips, works out to about 4 miles. Add in the 2.5 mile approach from the Wendy Drive trailhead, and the total distance for the course is about 9 miles, with an elevation gain of a bit over 2000 ft.

I did the loop counterclockwise -- up the western ridge and then down the eastern. The New Year's weather could not have been better. Dense fog clung to the coast, but a brisk offshore breeze kept inland views crystal-clear. On the way up the western ridge I couldn't resist doing a short detour to climb one of the crag's appealing summits.

At the top of the western ridge, I briefly debated doing Tri-Peaks and Big Dome, but was hoping to make it home by noon, so skipped those side trips.

With gravity on my side, the run down the eastern ridge was not nearly as gnarly as I thought it might be. I was running in Inov-8 Roclite 305s -- nimble shoes with a fell running heritage. Mine weigh only 21.1 oz./pair (US 9.0) and were particularly well-suited to the rough terrain.

This climb and adventure run was a great way to start the New Year -- and I did make it home in time for lunch with my wife!

Here's a Google Earth image of a GPS trace of my route.

Two routes are commonly used to climb the rugged north side of Boney Mountain. One route ascends a ridge to the east of the Danielson cabin site, and the other a rocky ridge to the west of the site. Today, I was planning to do the western ridge, and then continue up and over Tri-Peaks to the Chamberlain segment of the Backbone Trail.

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. Some of the shell impressions are palm-sized and larger.

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.

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.

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.

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.

Some related posts: Chumash Trail - Sesnon & Simi Fires, San Fernando Valley from Rocky Peak

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.

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.

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.

Fall color is not as widespread in chaparral as in some other plant communities. This vividly colored poison oak is along the Garapito Trail in Topanga State Park.

From a run of the Trippet Ranch Loop from Marvin Braude Mulholland Gateway Park at the southern end of Reseda Blvd., in the San Fernando Valley.

Related post: Poison Oak, Ferns Along the Garapito Trail

Following are brief descriptions, Google Earth images, and a Google Earth KMZ file of several trail runs at Ahmanson Ranch -- now Upper Las Virgenes Canyon Open Space Preserve. These are shorter courses, generally on dirt roads, that extend as far west as Las Virgenes Canyon. Some longer runs in this area are listed in the Santa Monica Mountain Conservancy Open Space section of my Google Earth KMZ Files of Trail Runs page.

Sometimes growing as large as a supermarket cherry, the sweetish, thin-pulped fruit of hollyleaf cherry (Prunus ilicifolia) is a favorite snack of coyotes.

These are on the Chumash Trail in Rocky Peak Park. This is the first year since the 2003 Simi Fire that there has been a sizable hollyleaf cherry crop along the trail.

It is commonly reported that an "acid treatment" in the digestive tract of a coyote or bird is required for germination. However, according to the University of Texas Native Plant Information Network Native Plant Database, fresh seeds require no treatment.

Related post: Holly-leaved Cherry