“Chumash Rock” is prominent rock formation seen from the Chumash Trail in the eastern Simi Valley.
As I discovered in a January 2006 adventure, it is not an easy rock formation to reach.
The title photo was taken in mid-November while doing the Chumash – Las Llajas Loop. The clouds over the Ventura County foothills and mountains from the Las Llajas Canyon – Rocky Peak Road connector were just as beautiful.
I was beginning to wonder if I would get a chance to do the Three Points Loop around Mt. Waterman this year. Angeles Crest Highway had been closed from Red Box to Vincent Gap for many months, and CalTrans projected it might not open until Thanksgiving.
That’s why Friday (November 3) I was excited to hear Angeles Crest Highway had reopened between Upper Big Tujunga Rd. and Islip Saddle.
At dawn, a couple days later, I pulled into the Three Points parking lot, put on some sunscreen, grabbed my pack, and set out to see what was happening on the Three Points loop around Mt. Waterman.
I’d done the loop many times and in many situations — clockwise, counterclockwise, after the Station Fire closure, after the Bobcat Fire closure, with snow at the higher elevations, in hot weather and in cold. When the trails are in good shape and the weather isn’t too hot, the 20-mile loop is an outstanding trail run. Today, it was a challenge just to complete the loop.
In many areas of Southern California, a wet 2022-2023 rainy season and Tropical Storm Hilary’s rain produced two seasons of Spring-like growth. One of the effects of the rain was the growth of wildflowers usually seen in the Spring, including seep monkeyflower, golden yarrow, gilia, grape soda lupine, and little paintbrush. It was strange to see a bumblebee buzzing from flower to flower of a Grinnell’s penstemon at 7250′ on Mt. Waterman in November.
At lower elevation, sections of Three Points – Mt. Waterman Trail (10W04) were overgrown with mountain whitethorn — requiring several “grin and bear it” passages. Higher, long stretches of the little-used path were covered with a second season of grass. This made route-finding difficult, particularly where the trail descends to the Twin Peaks Trail junction.
It was an intriguing puzzle to solve, and eventually I made it to the junction of the summit trail and the trail down to Angeles Crest Highway, near Buckhorn (10W05). The trail down to Buckhorn sees much more use than the trail from Three Points and is much better defined. Besides a couple of downed trees, the run down was one of the more enjoyable parts of the loop. The trail is usually very busy, but I didn’t encounter anyone coming up the trail.
As expected, Buckhorn Campground was closed and no water was available. It was a warm day — around 75 degrees — but with the November sun low in the sky, not as warm as 75 degrees in July. If I needed more water, there were several places I could refill.
The Burkhart Trail (below Buckhorn) was the only place I encountered a few hikers. They were returning from Cooper Canyon Falls. When I got down to the PCT and saw how much water was in the creek, I did the short side trip to the falls and took this video snapshot. It’s unusual for the falls to be flowing this time of year.
After checking out the falls, I resumed my westward journey on the PCT. Within feet of the creek crossing, an ugly tangle of fallen trees completely blocked the trail. This was just the first of several problems on the PCT between the Burkhart Trail junction and Cooper Canyon Camp. There were the usual downed trees, but there were also several sections of badly overgrown trail. These green thickets were generally adjacent to the creek, where the trail had been (or still was) wet.
Needing water, and to empty the debris from my shoes, I stopped for a few minutes at Cooper Canyon Trail Camp. Several campsites are nestled in a pleasant area along the creek. With Angeles Crest Highway open, I thought I might see someone here, but like Buckhorn Campground, it was empty.
After reaching Cloudburst Summit, the remainder of the run was more or less usual for the loop. There was some Poodle-dog bush and a small rockslide along the PCT on the way to Camp Glenwood, but neither were an issue. The run was more challenging than usual — and a bit slower — but it had been (mostly) fun and fascinating to work through it.
Here are a few photos taken along the way.
Some related posts:
– After the Bobcat and Station Fires: Three Points Loop Around Mt. Waterman (Slideshow, 3D Terrain Maps)
– Cool Weather, Old Trees, Grape Soda Lupine and a Restored Trail
– Lemon Lilies, Tree Rings and More Heat Training on the Three Points Loop
– Three Points Loop Adventure – July 2020
The blue of the woolly bluecurls was just stunning. The plant was along the Ken Burton Trail, in the San Gabriel Mountains, near Los Angeles.
Woolly bluecurls normally flowers in the Spring, but rain from Tropical Storm Hilary, combined with Spring-like conditions caused it to bloom this Fall. Such blooms are usually not widespread and the flowers are often less robust than their Spring counterparts. Other Spring flowers that were blooming included Ceanothus, bush poppy, and golden yarrow.
The Ken Burton Trail connects the Gabrielino Trail, near Oakwilde, to a saddle at the top of Brown Mountain Road. Today, I was doing a longish out and back trail run to Wella’s Peak from Clear Creek via Switzers and the Gabrielino and Ken Burton Trails. Wella’s Peak is a bump on the west side of the saddle. Brown Mountain towers above the east side of the saddle.
Explore the scenery and terrain on the out and back trail run to Wella’s Peak from Clear Creek using our high resolution, interactive, 3D viewer. The imagery is so detailed, it’s almost like being there! To change the view, use the control on the upper right side of the screen, the CTRL key and your mouse, or touch gestures. Track and placename locations are approximate and subject to errors. Snow, ice, poor weather, and other conditions may make this route unsuitable for this activity.
Related post: Red Box – Bear Canyon Loop Plus Brown Mountain
Had they not dislodged some rocks, I doubt I would have seen the three bighorn sheep in the photo above. They are easier to see in this zoomed-in photo of the sheep descending the rocky slopes just below Windy Gap (7,588′) in the San Gabriel Mountains. They crossed a brush-covered rib and disappeared from view.
A few minutes after seeing the sheep, I reached Windy Gap and stopped to put my arm sleeves away. It had been cool at the trailhead — about 40 degrees — but the temperature had warmed as I worked up the trail. As its name suggests, the wind can be fierce at Windy Gap, but this morning there was almost no wind, foretelling nearly ideal weather for today’s adventure.
Windy Gap was still in shade, and the sun was just peeking over the ridge to the east. You couldn’t tell, but the eclipse had already begun. The eclipse would be nearly total in parts of Oregon, Nevada, Utah, New Mexico, and Texas. In the Los Angeles area, the moon would obscure more than 70% of the sun’s disc.
From Windy Gap, I headed east on the Pacific Crest Trail toward Mt. Hawkins. From time to time, I would stop and check the progress of the eclipse using eclipse sunglasses. In sunny areas, I looked for lensed images of the sun in the shadows of trees but didn’t see any. Having needles instead of leaves, conifers don’t produce the myriad images of the eclipsed sun seen under trees with leaves.
A few minutes before the eclipse reached maximum, I took this photo of the eclipse with my iPhone, using eclipse glasses as a filter.
With nearly three-quarters of the sun obscured, the light from the sun had become enfeebled. The feeling was more than that of a cloud passing in front of the sun. I stopped and listened… to nothing. It was eerily quiet. No birds called or sang, and only chill zephyrs of wind wafted about the area. Somehow, the sun was broken.
As the eclipse slowly waned, I continued east in the corrupt light, past Mt. Hawkins and Throop Peak, to the PCT’s junction with the Dawson Saddle Trail. In what seemed fitting for the day, instead of continuing to Baden-Powell, I turned left and headed down the trail toward Angeles Crest Highway (Highway 2).
Why? Angeles Crest Highway was closed from Red Box to Vincent Gap, transforming Dawson Saddle into one of the more isolated areas of the Angeles National Forest. I hadn’t been on the Dawson Saddle Trail in years, and with Highway 2 closed, it would be a quirky way to climb Mt. Lewis. Instead of having one of the shortest approaches in the San Gabriels — a few feet from the CalTrans shed at Dawson Saddle — it would involve a trail run of nearly eight miles just to get to the base of the peak.
The eclipse was nearly over when I reached the bottom of the Dawson Saddle Trail on Highway 2. From the trailhead, I ran up an empty Angeles Crest Highway a short distance to Dawson Saddle. Mt. Lewis’ south ridge was accessed from here.
Only about a half-mile long, the south ridge isn’t technical, but the first third is steep and rocky. The elevation gain from the saddle to the summit is about 500′. Offset from the crest of the San Gabriels, the flat summit of Mt. Lewis has unique views of the crest extending from Mt. Baden-Powell to Mt. Islip and beyond.
After a few minutes enjoying the summit, I turned southward and began working my way back down to Angeles Crest Highway, up to the PCT, over to Windy Gap, and back down to the trailhead in the Crystal Lake Recreational Area.
Here are a few photos taken along the way.
Some related posts:
Solar Eclipses, Saros Cycles and Chumash Rock Art
Boney Mountain Eclipse Run
It’s Mid-July And There Is Still Snow in Los Angeles County!
Update September 14, 2023. Mustard is sprouting along Ahmanson’s fire roads, and more surprising — a few mushrooms.
Update September 8, 2023. The new grass from T.S. Hilary’s rain is coming in nicely at Upper Las Virgenes Canyon Open Space Preserve (Ahmanson Ranch).
Tropical storms are a different kind of weather beast than usually seen in Southern California. The warmer air associated with such storms can carry much more water and produce unusually high amounts of precipitation.
The rain resulting from Tropical Storm Hilary shattered many daily and monthly records. Over decades of record keeping, most stations in the greater Los Angeles area had previously measured only a trace of rain on August 20 or 21, or at best, a few hundredths of an inch. Some stations had never recorded any rain on these days.
This Google Earth image with precipitation data from the California-Nevada River Forecast Center (CNRFC) shows the remarkable rainfall totals across Southern California for the 24-hour period ending at 5:00 a.m. on Monday, August 21, 2023.
The highest rainfall amounts occurred where the precipitation was enhanced by mountainous terrain. The northeast-facing slopes of the eastern San Gabriel Mountains, near Wrightwood, were ideally positioned in Hilary’s circulation to enhance rainfall. The Big Pine RAWS recorded over 6 inches of rain for the storm, Lewis Ranch slightly over 7 inches, and Lytle Creek nearly 10 inches.
Detailed observation and impact reports for Hilary are available from NWS Los Angeles/Oxnard, NWS San Diego and the Center for Western Weather and Water Extremes.
Curious to see some of the local impacts of the storm, I ran at Ahmanson Ranch on August 22 and then a few days later at Malibu Creek State Park.
My West Hills weather station, about three miles from Ahmanson Ranch’s Victory Trailhead, recorded 3.86 inches of rain for the storm. After an initial technical hiccup, the Cheeseboro RAWS, overlooking Las Virgenes Canyon, recorded 3.52 inches of rain. This and other data suggest rainfall amounts in the Ahmanson area of at least 3.5 – 4.5 inches.
My Ahmanson run started at the Victory trailhead, went out East Las Virgenes Canyon, through part of Las Virgenes Canyon, and then up to Lasky Mesa. With that much rain, I was sure I would be wallowing in the mud and wading the creek crossings. But my shoes didn’t even get muddy!
There was certainly some mud, puddles, and a little erosion, but the impact of Hilary on Ahmanson was surprisingly minor. The ground must have been desiccated because Las Virgenes Creek had almost no increase in flow. The creek crossings near the pipeline station and south of the station were essentially the same as before Hilary. Even more surprising, there was no water at the crossing a little north of the Las Virgenes Trailhead.
As Hilary moved northward in California, the counterclockwise circulation of the storm increased the rainfall in the Santa Monica Mountains. Automated RAWS stations in Topanga, the Malibu Hills, and in Malibu Canyon recorded 4.0 to 4.5 inches of rain during the storm. CNRFC gridded precipitation data indicated higher amounts in some parts of the range.
On August 27, I ran the Bulldog Loop in Malibu Creek State Park. The run started at a small parking area at the junction of Malibu Canyon & Piuma Roads. As I was running up the Tapia Spur Trail, I wondered if State Parks had — as a precaution — removed the seasonal bridge across Malibu Creek on the Crags Road Trail. On August 19, the day before Hilary drenched the area, the bridge had been in place for the Bulldog Ultra. If it wasn’t removed, did Malibu Creek get high enough to damage it?
Once again, I need not have worried. The bridge was just fine, and the reeds in the water near the bridge suggested only a modest increase in streamflow.
It looked like Malibu Creek State Park received more rain than Ahmanson Ranch. There was slightly more erosion on the dirt roads and some small sluffs/slides, including one tree that slid onto Mesa Peak Mtwy fire road. A tree had also fallen near the beginning of the Forest Trail.
Back at Ahmanson on August 31, things were drying out, but it was beginning to look like Spring. Grass was sprouting all over Ahmanson Ranch. It will be interesting to see if the grass survives the inevitable heat and grows enough to turn the hills green. The little bit of rain and cooler weather over Labor Day weekend will help. Some out-of-season wildflowers could also result from a false Spring.
Yesterday, I did a run in Topanga State Park, and the story was much the same. There was some minor erosion on the fire roads, but none of the larger sluffs and slides seen during the rainy season. There was no new damage to the Musch or Garapito Trails. It did look like the flow had increased on Garapito Creek with Hilary’s rain, and there was a still little water in the mainstem of the creek.
Update September 3, 2023, 1:15 p.m. Caltrans Quickmap is showing Angeles Crest Highway (Hwy 2) is now open between Grassy Hollow and Vincent Gap. Caltrans Road Conditions says the closure is “5 mi west of Big Pines.” Google Maps and Waze still show the section between Grassy Hollow and Vincent Gap as closed.
Update August 23, 2023. The Big Pines RAWS recorded 6.26 inches of rain, and Lewis Ranch RAWS 7.04 inches from T.S. Hilary. The heavy rain on the north-facing slopes of the eastern San Gabriels may have produced debris flows in the washes crossed by the Manzanita Trail. Excessive runoff may have done more damage to stabilized sections of the Manzanita Trail where it crosses steep slides above Paradise Springs. According to CalTrans, the previously open section of Angeles Crest Highway (Hwy 2) between Grassy Hollow and Vincent Gap is currently closed.
I’d been thinking about doing the South Fork Loop, a challenging loop that I usually start at Islip Saddle. The route descends the South Fork Trail to South Fork Campground (4,565′) and then climbs all the way to the top of Mt. Baden-Powell (9,399′), using the Manzanita Trail and PCT. From the top of Baden-Powell, the PCT is followed back to Islip Saddle.
But there were a couple of problems with this idea. First, the road to Islip Saddle — Angeles Crest Highway — was closed. More importantly, parts of the South Fork Trail were burned in the Bobcat Fire, and heavy snow and rain may have damaged the South Fork Trail or Manzanita Trail.
The road closure would be easy to work around — the loop could be started at Vincent Gap. But I definitely needed to check the condition of the South Fork and Manzanita Trails. The loop is difficult, even when the trails are in good shape.
I decided to check the Manzanita Trail first. If that trail had issues, then the condition of the South Fork Trail didn’t matter.
So that is what I was doing today. The plan was to run the Manzanita Trail from Vincent Gap down to South Fork Campground, then turn around and — just like on the South Fork Loop — take the Manzanita Trail and PCT to the top of Mt. Baden-Powell.
I woke early on Sunday and arrived at Vincent Gap at about 6:45 a.m. With much of Angeles Crest Highway closed, I shouldn’t have been surprised that the main parking lot was already full. I nabbed the last spot in the overflow area across the highway. I could only imagine what it must be like on the trail up Baden-Powell.
But I didn’t have to worry about that — not for a while. I grabbed my pack from the back of the car and started jogging down the Manzanita Trail. On that trail, I probably wouldn’t see anyone!
As would be expected on a little-used trail after a hard Winter, the Manzanita Trail was a bit of a mess. In addition to being generally overgrown, there were fallen trees, brush deposited on the trail by runoff or avalanches, minor washouts, and other damage. These slowed the pace but weren’t too much of a problem.
On the other hand, there is a section of the Manzanita Trail that could be a serious issue. It is where the trail crosses several steep, loose, stabilized slides. This area is about 4.4 miles from Vincent Gap and 1.4 miles from South Fork Campground. This section of the trail is almost always damaged, but on past adventures, had always been passable. How bad was it going to be today?
The answer is — pretty bad. As I started across the first slide, it looked like it would go just fine, but then I looked closer. One of the abutments on the down-slope side of the trail had completely given way. The trail had collapsed, leaving only a narrow slice of crumbling dirt along the base of the up-slope barrier. I would have to use the barrier to get past, and it wasn’t in the best shape. I’m sure people have done this, but it seemed like a bad idea. I could see no straightforward way around the collapsed trail. Disappointed, I turned around and started working back up the trail toward Vincent Gap.
I’d been running for a few minutes when I came across a “lightning tree.” These are trees that have been struck by lightning and have a scar spiraling down their trunk. I’ve photographed a number of them. Some are in a location that you would expect to be struck by lightning, but just as many are along seemingly unexposed sections of trail. Once, I was running down the PCT below Mt. Hawkins, well below the crest, and a tree 50 yards down the slope was smoking from just being struck.
On the way back up to Vincent Gap, there would be a little route-finding fun. The Manzanita Trail crosses some small debris-filled washes. Over time, paths develop through the rubble but can be intermittent and indistinct. Debris flows can destroy a part of nearly all of a path.
The wash in Dorr Canyon is the largest crossed by the Manzanita Trail. Keeping in mind that Tropical Storm Hilary may have changed things, on August 13th, the path across the wash was mostly intact. One gotcha was that on the west side of the wash, the path ended short of the Manzanita Trail.
Did I mention the gnats, stinging nettle, and Poodle-dog bush? Oh, the gnats. On the way down the trail they weren’t too bad, but as the temperature warmed, they became increasingly annoying and persistent.
When doing the South Fork Loop, I usually stop for water at the stream that feeds Icy Springs. The trail was overgrown near the stream, and mixed in with the greenery was some stinging nettle. Even knowing it was there, I managed to brush against it on the way down the trail and then again coming back up.
There was also a little Poodle-dog bush on the trail about two miles down from Vincent Gap in a small area that had been burned. As long as you noticed it, it was easy to avoid.
What the heck? As I topped out at Vincent Gap, the sounds of revelry came from across the highway. It was party time in the Baden-Powell parking lot! A large group of people were gathered at the west end of the lot, near the trailhead. Were they preparing to do a mass ascent of Baden-Powell? I quickly refilled my hydration pack, grabbed some food, and headed up the PCT.
Once I escaped the craziness of the parking lot, it turned out to be one of the most pleasant ascents and descents of Baden-Powell I’ve done. Even with the machinations of the Manzanita Trail earlier in the morning and the additional vertical gain, Baden-Powell couldn’t have gone better. Very few hikers were on the trail, everyone was super-friendly, and when I reached the summit, it was empty — at noon, on a Sunday, in August!
Some related posts: Manzanita Trail Morning, South Fork Adventure, Bear Cubs on the South Fork Trail, San Gabriel Mountains Running Adventure