Rays of sunshine burst through breaks in the clouds over the Los Angeles Basin and Century City.
From a recent run on the Backbone Trail to Temescal Peak and down Rogers Ridge.
Rays of sunshine burst through breaks in the clouds over the Los Angeles Basin and Century City.
From a recent run on the Backbone Trail to Temescal Peak and down Rogers Ridge.
It’s been nine years since the Station Fire burned 160,577 acres in Angeles National Forest. The Red Box – Bear Canyon – Gabrielino loop is a long time favorite adventure run that I’ve enjoyed doing many years before and after that 2009 fire.
The loop was the first I did when the area reopened in May 2011. The trails were in poor shape — overgrown and damaged from flash floods. The notorious fire-follower Poodle-dog bush had flourished in the wake of the fire and was particularly bad along the Gabrielino Trail between Switzer’s and Red Box. Thinking I was “immune” to the plant, I brazenly plowed through it, and as a result spent several inflamed nights trying to sleep in a reclining chair.
Each year Bear Canyon and upper Arroyo Seco recover a little more. Poodle-dog bush is in decline and in many areas nearing the end of its life-cycle. The chaparral, bay trees and oaks are all recovering; and the bigcone Douglas-firs that survived the fire have become more fully-foliaged.
This year Bear Canyon was a little drier than last. The creek was a trickle, disappearing in the sand in some areas and creating small pools in others. The path in the upper part of the canyon, above Bear Canyon Camp, was better defined, but still tricky to follow in some spots.
With the dry conditions, most of the poison oak had already turned red. It was easy to spot, but difficult to avoid. The “stinging nettle” creek crossing higher in the canyon wasn’t as overgrown as last year, but I still managed to brush against a plant or two.
Bear Canyon ends at Arroyo Seco, downstream of Switzer Falls. After turning upstream on the Bear Canyon Trail, I hadn’t run far when I encountered a couple of mountain bikers. They asked me, “is this the trail to JPL?”
This wasn’t the first time that I’d encountered misplaced riders or hikers on this section of trail. Some get misplaced looking for the falls and others mistakenly follow the Bear Canyon Trail down into Arroyo Seco instead of continuing high in the canyon on the Gabrielino Trail. Because of the completion of the restoration of the Gabrielino Trail there were a few more riders on the trail than usual.
Here are a few photos taken along the way.
Some related posts: Bear Canyon Loop: If the Poison Oak Doesn’t Get You, the Stinging Nettle Will; After the Station Fire: Red Box – Bear Canyon – Gabrieleno Loop; After the Station Fire: Contact Dermatitis from Turricula parryi – Poodle-dog Bush
The smoke in the Owens Valley was as thick as PCH fog, and I wondered if it would extend into the higher elevations of the Sierra.
From Whitney Portal Road I couldn’t see any of the ridges on Lone Pine Peak and the visibility at the bottom of Horseshoe Meadow Road wasn’t much better. Gradually, as I drove up one long switchback and then another, the smoke thinned. At Horseshoe Meadow the sky in the direction of the crest was a decent Sierra blue, but smoke still spoiled the views down the canyons and over the valley.
As usual, I parked at the equestrian and overflow parking area for the New Army Pass Trail. From here, the start of the Cottonwood Pass Trail is a 5 minute walk SSW through the trees and downhill. I prefer to do the loop clockwise, going over Cottonwood Pass first, and then New Army Pass later in the run. Late season, I’ve also done the loop using (old) Army Pass, but that is more of a mountaineer’s route and is often blocked by snow and ice.
New Army Pass is fairly high — 12,300′ — and the east side is quite steep near the top. Depending on the year, snow and ice can be an issue, even in mid-summer. When doing the loop clockwise, confirm in advance that New Army Pass will be passable with your level of experience and the equipment you’ll be carrying.
For more details see the related posts below.
Here are a few photos from the run.
Some related posts: Cottonwood Pass – New Army Pass Loop 2013, Cottonwood – Army Pass Loop, Cottonwood Pass – New Army Pass Loop 2011
Yellows, reds and greens marked its location, but the seep above Sheep Camp was dry. As I approached the camp, the uppermost campsite was empty and I wondered if the spring at the camp was also going to be dry. If it was, I was going to have to revise my running plan.
So far the run had gone well. From the Chula Vista parking area (8350′), I’d run the service road up to Mt. Pinos (8831′), then followed the Tumamait Trail west to Mt. Abel Road. Along the way Sawmill Mountain (8818′)and Grouse Mountain (8582′) had been short side trips; and from the end of the trail, the summit of Mt. Abel (8280′) was a short hike up through the pines.
Compared to the triple-digit temperatures in the parched West Valley — as high as 117 °F this July — the temps on the Tumamait Trail had been wonderfully cool. The hotter than average weather seems to have become the new norm, and also — unfortunately — the resulting wildfires.
On a run here Last July, smoke from a fire near Lake Cachuma had nearly enveloped Mt. Pinos. Today several fires were burning in California, and once again smoke could be seen in the valleys and canyons to the north of the mountain.
To get in a bit more mileage and elevation gain the next part of my run was supposed to be an out and back to the sun-baked environs of Lily Meadows (6600′). That wasn’t going to happen if the spring was dry.
When I stopped at the wildflower-accented spring I could see that there was the barest thread of water trickling from the pipe. It didn’t look like much, but it filled my 18 oz. cut-off water bottle in about three minutes. I gulped down most of the first bottle and it took a couple more to fill my Camelbak. In about 10 minutes I was headed downhill.
The North Fork Trail is far less used than the Tumamait Trail. That’s part of the fun. Thunderstorms had not only wiped away any previous tracks, but had severely eroded some sections of the trail as well.
With the loss of elevation came an increase in temperature. By the time I reached Lily Meadows Camp the temp was in the 90s. This time of year there were no lilies or meadows at the campsite, but there was a nice grove of Jeffrey pines and a new camp table!
I didn’t spend much time down there. There was a hill to climb and the cool temps along the crest were only about an hour away.
Some related posts: Pinos to Abel Plus, Thunderstorm, Vincent Tumamait Trail
There seems to have been some carryover from the wet rainy season we had in 2016-17 to this year. The 2017-18 rain season was very dry — the third driest on record at Downtown Los Angeles — but seeps at Waterman Meadow, along the Burkhart Trail below Buckhorn were still wet. In general plant growth along trails has been more than I expected in such a dry year.
Wet and dry periods can be seen in the growth rings of the large Jeffrey pine along the Three Points – Mt. Waterman Trail just west of the Twin Peaks Trail junction. A more careful count of its rings totaled about 500. No matter how careful the count, because of the various anomalies that occur with tree rings, some form of crossdating is usually required to confidently assess the age of a tree. Even so, it is clear this was an old tree.
The first few miles of the loop were gloriously cool, but by the time I reached Cooper Canyon and was working up to Cloudburst Summit on the PCT, the sun beat down on me in a familiar refrain.
Here are a few photos taken on the loop.
Related post: Cool Weather, Old Trees, Grape Soda Lupine and a Restored Trail
It was “déjà vu all over again” for the 12th running of the Angeles National Forest Trail Race on Saturday. When the sun rose over Mt. Wilson Saturday morning, the temperature was already in the 80s and monsoon clouds were scattered across the eastern sky. We all knew it was going to be a hot day. The only question was how hot?
Following weeks of seasonable — and often cool — weather, temps began to ramp up Thursday. On Friday many daily and some all-time record high temps were set around the Los Angeles area. Van Nuys set an all-time record high of 115°F. Downtown Los Angeles set a new daily record of 108°F and Woodland Hills set a new daily record of 117°F.
The record-breaking heatwave continued race day with temps on the ANFTR course surpassing the torrid temps of 2017. The Clear Creek RAWS recorded hourly temperatures as high as 100°F and hourly fuel temps as high as 123°F. The highest temperature measured at Clear Creek was 105°F — five degrees higher than last year’s race.
Once again, despite the heat, there were some AMAZING performances. In the 60K, first and second place in both the Mens and Womens division finished only a couple minutes apart. Mario Martinez’s 6:41:25 just edged Rupert Romero’s 6:43:27, and Katie Asmuth’s 7:29:11 was just ahead of Teresa Kaiser’s 7:32:21. Chase Coffey ran the 50K in 4:25:26, which I believe is the fastest time for the normal 50K course. (In 2009 we ran all the way to Red Box on Mt. Wilson road.) Ana Suchey was the top woman in the 50K with a time of 6:04:30. In the 25K Victor Martinez bested the record he set last year, running the course in 2:07:27. Jennifer Sunahara was first among the women, with a time of 2:58:29. Not all the great performances were from the fastest runners. Sa Il Hong, age 80, completed the 50K in fine form.
Many thanks to Gary and Pam Hilliard and all the ANFTR staff and volunteers! It wasn’t just hot for the runners! And those setting up the event and marking the course had to endure Friday’s record-setting temps, spend a warm night on the mountain, and then work in the heat again on Saturday!
See the ANFTR web site, Facebook page and Facebook group for more info. The Angeles National Forest Trail Race is the new name for the Mt. Disappointment Endurance Run. Only the name changed. All the results for the ANFTR/Mt. Disappointment races since 2005 can be found on Ultrasignup.com.
Note: The temperature in a commercial weather station is measured inside a white, ventilated instrument housing, several feet off the ground. Mid-day temperatures in the sun, in the summer, with a cloudless sky will be much warmer than this. Some stations, such as Clear Creek, also measure the fuel temperature — the temperature of a pine dowel in direct sun about a foot off the ground. According to the NWS (and common sense) exposure to full sunshine can increase heat index values by up to 15°F. In my experience the fuel temp gives a better indication of the actual temperature a runner can experience in the sun, especially on exposed mountain slopes facing the sun.
Related post: Record Heat for the 2017 Mt. Disappointment 50K & 25K