Category Archives: running|adventures

Perils of Winter, Surprises of Summer

Mt. Baldy from Mt. Baden-Powell

Storm-damaged Lodgepole Pine and Mt. Baldy

I was at the turnaround point of an out and back run from Islip Saddle (6650′) to Mt. Baden-Powell (9,399′), and had descended a short distance down the south ridge of Baden-Powell to enjoy the ridge top view. It had been a good run so far. It was windier and cooler than expected, but that was a good thing. Temps in the valleys were forecast to top 100 degrees today.

I’d been surprised to find no snow on Baden-Powell. In good snow years, remnants of snow will typically last until at least the 4th of July. There was a patch here and there last year, and sizeable drifts in 2005. This year a little remained on the north face of Mt. Baldy, but that was it.



Even if no snow remained, there was evidence it had been a tough winter. It looked like an unusually severe ice storm had struck the area. Normally resistant to such damage, a stout lodgepole pine had had two of its limbs ripped from its trunk, peeling away a thick layer of bark and cambium. On the other side of the peak, near the Wally Waldron tree, an apparently healthy limber pine had collapsed.

If I had been surprised to find no snow on Baden-Powell, I was even more surprised to find no one on the summit. That wouldn’t last. A number of hikers were working their way toward the peak from Islip Saddle and Dawson Saddle, and I was sure others were on the way up from Vincent Gap.

After visiting the Wally Waldron tree, and chatting briefly with a hiker, I turned eastward on the PCT — next stop Throop Peak!

Some related posts: Islip Saddle – Mt. Baden-Powell Out & Back, Running Hot & Cold

Air Conditioning

Nearing the summit area of Mt. Pinos

Enjoyed a combination Father’s Day & July 4th visit from Brett over the weekend. Friday we did a fun run at Malibu Creek State Park and today we headed up to Mt. Pinos to get in a cooler, higher altitude run.



In addition to Mt. Pinos (8831′), there are three other peaks along the broad ridge traversed by the Vincent Tumamait Trail — Sawmill Mountain (8818′), Grouse Mountain (8582′), and Mt. Abel/Cerro Noroeste (8280+’). I’ve run past the indistinct path to Grouse Mountain numerous times on the way to Mt. Abel, always commenting “someday I have to check that out.” Finally, today we did.

On the way to Grouse we did the short detour to the top of Sawmill. Since my last visit the Chumash spirit tower on the peak had grown, no doubt from the many fine days and views enjoyed here. This morning the snow-covered mountains of the Southern Sierra could be seen above the haze of the San Joaquin Valley.



The ascent of Grouse was straightforward. Like Sawmill Mountain, it has two nearly equal height summits. We found a small granite crag northeast of the summit and climbed a short steep route on its west face. It had fun technical moves on mostly good holds, but in running shoes you had to pay attention — especially on the downclimb!

On the way back to Mt. Pinos we stopped by Sheep Camp. The short side trip to this idyllic spot is essentially compulsory. It would be easy to spend the afternoon here, listening to the wind in the pines and the gurgling of the spring; smelling the sun-warmed pine needles; and enjoying the greens, yellows, reds and blues of Summer.

I always feel a little twinge of regret when leaving Sheep Camp, but it was a great day to be on the move, and soon we were back on the trail and enjoying that as well.
 
Some related posts: Vincent Tumamait Trail, Atmospheric Dynamics

Coyote Tag

coyote that ran with me

I was deep in thought, but have no idea what those thoughts might have been. It was at that point in a run when miles, and thoughts, flow freely. The afternoon was warm and calm and the settling sun cast a golden hue on the blond, oak-studded hills. My footfalls ticked out a steady rhythm on the dirt road, and my mind was at ease.

My reverie was suddenly broken by the realization that a coyote was running with me. Not running yards in the distance, or in the brush off to the side, but five or six feet in front of me, as if restrained by an invisible lead!

It must have come from the tall grass along the margin of the road, but from my daydream-warped perspective had just suddenly appeared. I’m surprised I didn’t stumble or start. But there was no hint of aggression or malice — just a mischievous glance backward to see how I was going to react.

I didn’t. I’ve had numerous encounters with coyotes, but this went so far beyond my other experiences, I didn’t know how to react.

For more than 50 yards the coyote ran with me, keeping pace in lead along the deserted dirt road.

At some point I started to try and retrieve my camera from the small pack on my waist. The out of synch movement disturbed the delicate balance of this improbable scene, and I could see the change in the animal’s demeanor.

Before disappearing into the cover, the coyote looked back a final time, and in so many words seemed to be saying “gotcha, you’re it!”

(From a run Tuesday at Ahmanson Ranch, now Upper Las Virgenes Canyon Open Space Preserve.)

Some related posts:
Trickster
Coyote Tag II

Atmospheric Dynamics

Complex of mountain wave clouds to the north-northeast of Mt. Pinos

These unusual clouds are a complex of lenticular clouds to the north-northeast of Mt. Pinos, photographed this morning from near Mt. Abel. They were produced by strong south-southwesterly winds blowing across the east-west oriented Emigdio and Tehachapi mountain ranges, north of Los Angeles. Here’s another view of these clouds from near the summit of Mt. Pinos.



The winds were associated with the circulation of an unseasonably strong low pressure system off the California coast. The storm system has resulted in measurable rain as far south as Santa Barbara County, and new rainfall records for the date were set in San Francisco, Paso Robles and Santa Maria.



The photographs were taken during a blustery out and back trail run from Mt. Pinos to Mt. Abel on the Vincent Tumamait Trail in the Chumash Wilderness. At the start of the run, the temperature at the Chula Vista trailhead (8400′) on Mt. Pinos was a chilly 39°F. In exposed areas the wind speed was 20-25 mph with gusts to around 50 mph.

Other than the potential for deadfall, the wind wasn’t too bad in the trees. The Vincent Tumamait Trail was in the best condition I’ve seen in years.

Update June 6, 2011. The low that was off the Central California coast Saturday and most of Sunday and an associated cold front set a new rainfall record for June 5 at Santa Barbara Airport, and produced a few sprinkles and showers in the Los Angeles area.

Some related posts: Mountain Weather, Lenticular Wave Clouds, Mt. Pinos – Mt. Abel Out & Back

After the Station Fire: Three Points – Mt. Waterman Loop

Scorched Jeffrey Pines on the South Side of Waterman Mountain

Scorched Jeffrey Pines on the South Side of Waterman Mountain

It was very odd to run up the Mt. Waterman Trail on the Sunday of a 3-day Memorial Day weekend, and see no one. And hear nothing, except the wind in the trees, the distant call of a jay, and the periodic drone of a contractor’s truck working on the highway. That’s because — surprise, surprise — Angeles Crest Highway was closed a little east of Three Points and on to Islip Saddle. CalTrans Road Conditions had only listed the Winter closure from Islip Saddle to Vincent Gap. Based on the number of cars parked at the closure, not many people knew about it.



I hadn’t known about it until I saw the Ranger’s truck and closed gate from the Pacific Crest Trail. I was doing a loop from Three Points up the PCT to the Burkhart Trail, then up to Buckhorn, over Mt. Waterman, and back down to Three Points. Part of this loop — from Mt. Waterman to Three Points on Trail 10W04 — had just reopened, and like last weekend I wanted to see how recovery from the 2009 Station Fire was progressing.



The conditions were much better on this loop, than last week’s. Although within the initial Station Fire Closure area, and closed for eight months, 11 of the first 13.5 miles of the loop were not burned in the Station Fire. This mostly unburned stretch opened in late May 2010 and is described in the post Three Points to Waterman Mountain, the Long Way.



The remaining six miles of the loop, which winds in and out of the shallow canyons on the south side of Mt. Waterman, was in the burn area. Conditions along the trail appeared to generally correspond to BAER burn severity maps and images. At the higher elevations, fingers of the fire had run up the steep slopes, burning understory and scattered Jeffrey pines and incense cedars, while leaving other areas untouched.



At lower elevation, particularly in the chaparral and pine at the head of the north branch of Devils Canyon, the fire effects were more severe. The chaparral is recovering, but numerous Coulter and Jeffrey pines appeared to have been killed, and their replacement will be a slower process. This area is traversed by the last two miles of Trail 10W04, leading to Three Points.

There was very little, if any, damage from runoff and the trail was generally in good shape. The trail was slightly overgrown in spots, particularly at lower elevation, but was nothing like the Gabrielino Trail between Switzer and Red Box. There was some Turricula (Poodle-dog bush) at lower elevation, but for the most part it was fairly easy to avoid. Some pine needle covered sections of trail were indistinct, but it was like that before the fire.



From a trail running perspective, it is still a very “runnable” course with varied terrain and much to see and enjoy. Cooper Canyon Falls is very short side trip from the PCT’s junction with the Burkhart Trail. The side trip to the summit of Mt. Waterman (8038′) adds about two miles to the loop.

Some related posts: Three Points – Mt. Waterman Loop, Three Points Loop Plus Mt. Waterman

After the Station Fire: Red Box – Bear Canyon – Gabrielino Loop

Recovering chaparral and bigcone Douglas-fir in Bear Canyon 19 months after the Station Fire

Recovering Chaparral and Bigcone Douglas-fir in Bear Canyon

Most Southern Californians have direct experience with wildfire and its effects. Wildfires are often described as being a “natural part of the ecosystem,” but in Southern California wildfire is anything but natural. Urbanization, land management policies and firefighting practices shape fire frequency, behavior, intensity and effects — often with unexpected and tragic consequences.



According to InciWeb, the Station Fire started on Wednesday August 26th, 2009 at approximately 03:30 p.m. and was fully contained at 7:00 p.m. on Friday, October 16, 2009. Two firefighters were killed in the arson caused blaze, numerous homes and structures were lost, and 160,577 acres burned. The fire was the largest recorded in Angeles National Forest since it was established in 1892 and the 10th largest fire in California since 1933.

In January 2011 the Station Fire Closure was updated and extended to January 2012. At that point, it looked like it might be a long time before any substantial part of the closure area would be opened to the public. But with increasing public pressure to open more of the Forest, Angeles National Forest reopened about half of the Station Fire Closure area earlier this week. Today I did a run/hike in the newly opened area to see first-hand how recovery from the fire, and subsequent debris flows and flash floods, is progressing 19 months after the fire was contained.

The first areas I wanted to check were Bear Canyon, and upper Arroyo Seco from Switzer Falls to Red Box. I’d done loops through these areas in April 2009, a few months before the Station Fire, as well as in March 2007 and November 2005. Because Mueller Tunnel was closed, I couldn’t do the same loop as in 2009, but I could bypass the tunnel using the Mt. Disappointment Trail, and then drop down into Bear Canyon from the Mt. Lowe Truck Trail. From there the loop could be completed by following the Gabrielino Trail from near Switzer Falls, back to Red Box. After checking with the Forest Service that all of the trails were open, the loop was a go!



I’d done all the sections of the loop on previous runs, and was familiar with the trails and terrain. My intent was to follow the routes of pre-existing trails as closely as possible. Just in case, I took a paper map; and as a backup and source of extra info, I loaded my GPS with the track points of the trails. It turned out the GPS did help a couple of times to follow missing or overgrown sections of trail, but there was also more than one instance when blindly following the GPS would have led me in the wrong direction.



At around 7:30 I left an empty Red Box parking lot and started running up the Mt. Wilson road. About 0.4 mile up the road I turned onto the San Gabriel Peak/Mt. Disappointment Trail and began working up toward the saddle between the two peaks. Nearly all of the trail to the saddle was unburned. The robust mix of chaparral and forest towered overhead, and a few minutes later I felt some anguish as I crossed the saddle and entered the burn area.

There was a little more debris than normal on the rocky stretch of the Mt. Disappointment Trail that crosses the west face of San Gabriel Peak, but the trail was mostly runnable, and it didn’t take long to get down to the Mt. Lowe Truck Trail fire road. At Markham Saddle a DANGER sign marked the closure of the road to Mueller Tunnel.



Turning in the opposite direction, I started running down the fire road, and after a short distance, stopped to take photos of the Bear Creek drainage. It looked to be in pretty good condition, considering. The side canyons didn’t have the runnels and debris flows I’d seen in upper Arroyo Seco on the drive up Hwy 2. I’d be getting a closer look at those channels later in the run.



At the hairpin turn west of Mt. Lowe I left the fire road and picked up the trail that leads down the ridge to Tom Sloan Saddle. It had taken about an hour and a quarter to get to this point, and I suppressed an overly optimistic thought that I might reach Red Box by noon or so.

As would be expected with little or no use, two seasons of growth, and a wet winter, sections of the trail were really overgrown. The upper part of the Bear Canyon Trail was also significantly overgrown, and in a couple of places difficult to follow. It helped that animals had used the trail, though their path through the grass was indistinct. Trails are valuable resources that can be lost through prolonged closure and disuse.



Once down to Bear Creek, the character of the canyon was much the same as before the fire. Bear Canyon is one of the more wild and isolated places in the San Gabriel Mountains that can be accessed by trail. Not far beyond the old cabin site, I paused by the creek and absorbed the sounds, smells and scenery of this special place.



The creek was incised in places, and there was other evidence of moderately high flows in the two years since I had been there. Very little remained of the use trail. The remnants of the old Tom Sloan trail are still there, but these are few and far between. There were more fallen trees, and a ton of poison oak. It was time consuming to try and dance around the poison oak, and about halfway through the canyon I gave up trying. Bear Camp appeared to be unscathed, and looked much like it did in 2009.



It took twice as long to work through Bear Canyon as in 2009, and I was happy to get to Bear Creek’s confluence with Arroyo Seco. Except for a couple of fallen trees, it was straightforward getting back to the Gabrielino Trail and to the Switzer Picnic Area. The bridge at the picnic area was littered with flood debris. The high water likely occurred during our record-setting December 2010 rain event.

It was a close call, but no doubt due to the efforts of firefighters, Switzer Picnic Area appeared to have survived almost unscathed. The Forest Service has made a number of improvements to the facilities. According to a Forest Service press release, the picnic area will remain closed until sometime in June, while construction is completed.



The first two miles of the Gabrielino Trail above Switzer really took it on the chin. The fire effects there were very pronounced, and of all the trails in the loop, that segment was the most severely affected. Flash flooding and debris flows have swept the canyon, obliterating sections of trail. The rest is very overgrown. Virtually every tributary canyon is now incised with debris flow runnels, up to several feet deep.



Once away from the canyon bottom and on the old road bed the trail was still overgrown, but was generally in better shape and easier to follow. The last mile to Red Box was nearly in the same condition as before the fire, and the last half-mile (where some trailwork had been done) even better!

In the last decade I’ve followed the recovery and studied aspects of several fires including the 2002 McNally Fire, 2002 Curve Fire, 2003 Simi Fire, 2005 Topanga Fire, 2006 Day Fire, 2007 Corral Fire and 2008 Sesnon Fire.  Even after having observed it many times, I continue to be amazed at the resilience of fire-adapted ecosystems. As long as the fire recurrence interval isn’t too short, nature seems to do a pretty good job of recovery.

Related post: Contact Dermatitis from Turricula parryi – Poodle-dog Bush