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.
Arroyo Seco below Royal Gorge at Gabrielino Trail crossing.
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.
Bighorn sheep blend into the rocky terrain near Windy Gap
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.
The partially-eclipsed sun crests a ridge east of Windy Gap.
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.
Partially eclipsed sun.
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.
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.
The south ridge of Mt. Lewis can be accessed from the CalTrans shed at Dawson Saddle.
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.
Angeles Crest Highway from the shoulder of Mt. Lewis.
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.
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.
Bigcone Douglas-fir cones, dripping with protective resin.
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.
Wash crossed by the Manzanita Trail, about a mile below Vincent Gap.
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.
Manzanita Trail obstacle course.
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!
Gooseberries along the Manzanita Trail.
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?
Damaged section of the Manzanita Trail.
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.
Tree on the Manzanita Trail that was struck by lightning.
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.
Dorr Canyon wash.
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.
Blue Ridge and Pine Mountain from the PCT on Mt. Baden-Powell.
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.
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.
San Gorgonio Mountain, and Pine Mountain from Mt. Baden-Powell.
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!
Strawberry Peak from the Strawberry Trail, near Lawlor Saddle.
Last weekend I’d considered doing a run from Red Box, but finally decided to go to higher elevation and do a combination run and climb.
Blazing star.
The puzzle to solve this weekend was to find a run that was closer to home, higher than the Santa Monica Mountains, and had a “decent amount” of elevation gain. The solution put me right back at Red Box, doing two of the most popular peaks in the Front Range — Strawberry Peak (6164′) and San Gabriel Peak (6161′).
The main difference is that the 2018 run/hike was on a cool day in March, rather than a hot day in August. In 2018, I did San Gabriel Peak first, then Strawberry. The order didn’t matter. The temperature on both peaks that day was mostly in the 40s.
Mt. Disappointment (left) and Strawberry Peak from the San Gabriel Peak Trail.
Today, it was essential to do Strawberry first, and get started early. The use trail between Lawlor Saddle and Strawberry’s summit faces south and east, and has very little shade. It’s steep and strenuous an no fun at all in the hot sun.
I left the Red Box parking lot at about 6:00 a.m. On the way up, the temperature ranged from the mid-50s to the mid-70s. On the way down, in some places it was already in the 90s. While it was hot in the sun on the upper part of the mountain on the descent, the traverse around Mt. Lawlor on the Strawberry Trail was still mostly in the shade and a relatively cool 75 to 80 degrees.
San Gabriel Peak isn’t the solar oven that Strawberry is. Much of the Bill Riley/Mt. Disappointment Trail faces north and a scrub oak forest provides some shade. Continuing up San Gabriel Peak after doing Strawberry, the temps were generally in the low to mid-80s.
Angeles Crest Highway was still closed between Red Box and Vincent Gap, and the heatwave continued. I was trying to decide where to run.
I briefly considered the Circuit Around Strawberry Peak, but yesterday at 10:00 a.m., the “in-the-shade” temperature at Clear Creek was already 92°F, and the “in-the-sun” fuel temperature 109°F. By 1:00 p.m., the fuel temp reached a scorching 122°F!
Although trailheads such as Three Points and Islip Saddle couldn’t be accessed using Angeles Crest Highway, the highway was open from Wrightwood to Inspiration Point and Vincent Gap. After seeing the temps at Clear Creek, it took about two seconds to make the decision to head to the San Gabriels’ high country.
sulfur flower-lined section of the PCT east of Inspiration Point
From Inspiration Point (7,365′), I ran east on the PCT about 7 miles to the North Backbone Trailhead on Mt. Baldy. Over most of that stretch, the temperature was a blissful 60-something degrees. Other times, I’ve driven to this trailhead — which requires a high-clearance vehicle — or run to the trailhead from Wrightwood. But the run along Blue Ridge is a favorite. It is especially scenic, with fantastic views of Mt. Baden-Powell, Iron Mountain, Pine Mountain, and Mt. Baldy.
Crossing the top of a chute on Mt. Baldy’s North Backbone.
Following a short descent, I resumed climbing the steep, somewhat loose ridge. After about ten minutes, I scrambled onto the crest of the ridge and crossed the top of a prominent, rocky chute. More than a thousand feet below, avalanche-hardened snow gleamed white in the sun at the base of the chute.
Another 10 minutes of climbing and I reached the Pine Mountain Juniper. Straddling the rocky crest at an elevation of about 9000′, this stalwart tree is estimated to be 800 – 1000 years old. It is a remarkable tree in a remarkable location. Except for one short, steep, eroded section, the remainder of the trail to the top of Pine Mountain (9648′) was relatively straightforward.
Dawson Peak and Mt. Baldy from Pine Mountain’s south summit.
Pine is the second-highest peak in the San Gabriels and has excellent views of the surrounding terrain. It is higher than Mt. Baden-Powell (9399′) and Dawson Peak (9575′) but a few hundred feet lower than Mt. Baldy (10,064′).
From Pine Mountain, the North Backbone trail continues over Dawson Peak another 2.5 miles to Mt. Baldy. There was still a long ribbon of snow along the east side of the upper North Backbone, but it looked like the trail might avoid it. I would have liked to confirm that, but today the top of Pine was my planned turnaround point. As it was, with the warm weather, I thought I might run short on water on the return to Inspiration Point.
Leaving Pine behind, I started back down — jogging when it made sense — but trying not to do anything stoopid. On the way down, I kept reaching behind me and squeezing the bladder in my hydration pack. I guess I was hoping that it would magically be more full than the last time I checked. It never was.
San Gabriel beardtongue along the PCT on Blue Ridge.
Back at the North Backbone Trailhead, and definitely low on water, I decided it was a good time to run the dirt road back to the top of the Acorn Trail and see how much shorter it was than the PCT. The answer was not much — only about a tenth of a mile.
I’d been willing to push the water envelope because it had been a heavy snow year. I expected the spring near Guffy Camp would probably be running. I’d passed the side trail to the spring a bunch of times but never ventured down the steep slope. My impression was that the spring was often low or nearly dry. This time when I reached the side trail, I headed down.
Pumphouse at Guffy Spring, surrounded by giant larkspur.
And down and down… It sure seemed like a long way to the spring, but when I checked the track, it was less than a quarter-mile with an elevation loss of about 200′.
Back on the PCT, the temperature was generally in the mid-eighties but was warmer on south-facing slopes. At about 1:00 p.m., the in-the-sun fuel temperature at the Big Pines RAWS was 109°F. I was very happy to have the extra water.
Snow in the lee of the West Ridge of Mt. Baden-Powell.
You might not see it from the Los Angeles side of the mountains, but there is still some snow on the higher, north-facing slopes of the San Gabriel Mountains.
During and after storms, snow-laden southerly winds dump their load on the backside of the crest, creating deep drifts, cornices, and compacted slabs of snow. This snow is often the last to melt, not only because it doesn’t face the sun, but because there is more of it.
Mt. Burnham, Peak 9086, and Mt. Baden-Powell from near Throop Peak.
This morning, I was doing an out-and-back from the Windy Gap Trailhead in the Crystal Lake Recreation Area to Mt. Baden-Powell. The Windy Gap Trail climbs 1730′ in 2.6 miles, joining the PCT at Windy Gap. From there the trail follows the spine of the San Gabriels past Mt. Hawkins, Throop Peak, and Mt. Burnham to Mt. Baden-Powell.
I usually do this run from Islip Saddle, but with Angeles Crest Highway (Highway 2) closed between Red Box and Vincent Gap, the Islip Saddle trailhead isn’t accessible.
Snow at about 9100′ on the west side of Mt. Baden-Powell.
Whether you start at Crystal Lake or Islip Saddle, the length of the run is about the same — a bit over 16 miles. The main difference is that the Windy Gap Trailhead is about 800′ lower in elevation. On the plus side, the Windy Gap Trail is very scenic; on the minus side, it faces south and can bake in the midday sun.
On today’s run, I encountered the first snowbanks at an elevation of 8870′, near the Dawson Saddle Trail junction. Out of curiosity, I tried to follow the trail and soon realized that was a mistake. I was more or less forced to skirt the downhill side of a lengthy and deep drift — it being too steep and icy to cross directly.
Mt. Baldy from the summit of Mt. Baden-Powell. July 9, 2023.
For the remainder of the run, I switched to the early season tactic of staying on the crest when the trail deviated onto shaded, north-facing slopes. These areas might have significant snow on the trail. This only happens in a few places, such as when the PCT works around Mt. Burnham. There is a use trail that ascends the west ridge of Mt. Burnham, and then returns to the PCT.
The conditions today are reminiscent of those found here in early July 2005. July 3rd of that year there was still snow on the summit of Baden-Powell, and there was deeper snow in the areas where there was snow today. We had a lot of storms this rain season, but in Rain Year 2004-2005 Downtown Los Angeles (USC) recorded about 9 inches more rain than during the 2022-2023 rain year!
