The valley oak pictured above — one of the larger oaks along Rocky Peak fire road — toppled over in the summer of 2016 following five years of drought.
Fire and drought are a natural part of the valley oak’s habitat and the trees have evolved to withstand ordinary variations in their environment. However, severe fires or extended droughts, or fire in combination with drought can overcome the tree’s defenses.
The drought may have been the culminating factor in the felling of this oak, but fire and other factors may have also played a role.
According to the Fire Effects Information System (FEIS), the heart-rot fungus Armillaria mellea is usually present in valley oaks and larger oaks tend to be hollow or rotten in the center. The toppled oak was hollow near its base and its interior appears to have been blackened by fire. The FEIS describes instances where the decaying wood in the interior of older valley oaks could ignite in a fire, but leave the exterior bark uncharred.
The Google Earth image above shows the VIIRS fire detections from the Wilson Fire. The data is from USDA Forest Service Geospatial Technology and Applications Center Active Fire Mapping Program. The square markers show the approximate location of yesterday’s detected fire activity. The markers do not indicate the areal extent of the fire. This Forest Service Briefing Map shows the completed line and uncontrolled fire line earlier today.
The fire started before dawn yesterday and according to a tweet from @Angeles_NF at 9:31 this morning was 25% contained and at 50 acres.
The yellow traces are GPS-based tracks of trails in the area. The tracks are subject to various errors and should be considered approximate.
The north side of San Gorgonio Mountain was closed in June 2015 when the Lake Fire burned approximately 31,359 acres of forest, chaparral, sage, pinyon and Joshua tree habitat at elevations ranging from about 10,700′ to 5350′. As a result of the determined efforts of firefighters, only one residence and some remote outbuildings were lost.
Of the 30,487 acres reviewed by the Burned Area Emergency Response (BAER) team 4,327 acres (14%) were categorized as Unburned; 17,100 acres (56%) as having Low soil burn severity; 8,420 acres (28%) as having Moderate soil burn severity; and 640 acres (2%)with High soil burn severity. (Note that soil burn severity isn’t necessarily synonymous with fire intensity and fire effects such as tree loss.)
I’d been keeping an eye on the Alerts & Notices section of the San Bernardino National Forest web site to see if the Lake Fire closure order would be renewed. I was curious to see the extent and impacts of the Lake Fire and how the area was recovering. Plus, the Dollar Lake – Dry Lake keyhole loop is an outstanding trail run — one of the best in Southern California. In addition to climbing San Gorgonio Mountain (11,499′), it encompasses some of the most scenic areas on the peak.
The area’s trails reopened July 20. The weekend prior to the reopening San Gorgonio Wilderness Association volunteers worked on the South Fork and Dry Lake Trails, clearing a number of large trees, removing debris and other hazards and improving the trail tread.
A week and a half after the opening I pulled into the South Fork parking lot on Jenks Lake Road, excited to get on the trail. There was a slight chance of thunderstorms in the forecast, and I hoped to be off the summit and on my way down by 10:30 or 11:00.
Most of the run is in the San Gorgonio Wilderness and a wilderness permit is required. Check a map, but the general sequence of trails is the South Fork Trail, Dollar Lake Trail, Divide Trail, Summit Trail, Sky High Trail, Dry Lake Trail and then back down the South Fork Trail to the trailhead. This Google Earth image shows the western part of the Lake Fire burn area in relation to San Gorgonio Mountain and some of the area’s trails.
On this particular run I also wanted to check out the Fish Creek Trail and the “use trail” down to Lodgepole Springs and Dry Lake, so rather than continuing down the Dry Lake Trail from Mineshaft Saddle, I turned right (east) and followed the Fish Creek Trail to Fish Creek Saddle.
There were some downed trees and a lot of fire debris on the Fish Creek Trail. Extra care was required and I probably hiked as much of it as I ran. As I worked toward Fish Creek Saddle I could not tell how much of the canyon leading down to Lodgepole Spring had burned. The slopes on the southwest side of Grinnell Mountain had burned and some areas along the Fish Creek Trail had burned as well. Whether I descended to Lodgepole Spring from Fish Creek Saddle or returned to Mineshaft Saddle would be a judgment call.
Arriving at Fish Creek Saddle I was glad to see the forest was intact. The path down to Lodgepole Spring looked promising, but had not been used in some time. As it turned out most of the trees along the path had not burned. In places, runoff from the burned slopes above had resulted in some erosion and small flows of sandy soil. There were also the usual downed trees, but other than being a little challenging to follow, the path was generally OK.
I was nearly off the trail when the “chance of thunderstorms” forecast materialized into threatening gray clouds, a few sprinkles, and a couple of rumbles of thunder.
I was glad I didn’t turn around and head back to the car. At the beginning of the run smoke from the Whittier Fire (near Lake Cachuma) covered Mt. Pinos in an ugly shroud. Fortunately, a couple of hours into the run, the wind shifted to the north, removing the smoky veil and greatly improving the visibility and air quality.
Even it was smoky, at least the weather was cool. Following the torrid conditions at the Mt. Disappointment 50K the previous Saturday, and hot weather during the week, cool was good.
Mt. Pinos is often a good choice for escaping the triple digit heat of a Los Angeles heatwave. The elevation of the Chula Vista trailhead (8350′) is higher than the highest trailhead on Angeles Crest Highway — Dawson Saddle (7909′) and about 1000′ higher than the popular Inspiration Point (7370′) trailhead on the PCT.
My usual “Pinos to Abel” run starts at the Chula Vista trailhead and follows a dirt service road to the summit of Mt. Pinos (8831′). At the nearby wildlife viewing area it picks up the Vincent Tumamait Trail and heads west, taking a short detour to Sawmill Mountain (8818′) and the Chumash spirit tower, and then continues toward Mt. Abel (Cerro Noroeste). The trail ends at Cerro Noroeste Road, but a short climb up through the pine trees leads to the summit of Mt. Abel (8280+’) and Campo Alto. On the way back I usually run down the North Fork Trail to the spring at Sheep Camp, and sometimes extend the run by descending to Lily Meadows Camp (6250′).
It’s rare to see other runners doing the Pinos to Abel run. Dan and Dameon first passed me descending from Mt. Pinos. Our paths would cross several times over the course of the morning. They were running in the Mt. Pinos area for the first time and having a great time exploring the trails.
One of those times was on the top of Mt. Abel. They were thinking about hitting Grouse Mountain (8582′) on the way back to Pinos and asked about the route. The use trail to Grouse branches off the Vincent Tumamait Trail near a saddle ENE of the peak and about 0.3 mile west of the North Fork Trail junction. It leads to the northern summit of Grouse’s twin summits in about a quarter-mile.
I didn’t do Grouse Mountain today, but did take the North Fork Trail down to Sheep Camp. Today, the plan was to just go a “little way” down the trail below Sheep Camp to see if a particular plant was flowering. Beyond Sheep Camp the North Fork Trail drops like a rock, and it turned into one of those, “I’ll just go a little farther down” kind of things. Before I came to my senses I’d lost nearly 1000′ in elevation while looking for the plant.
After chugging back up to the spring at Sheep Camp, I refilled my Camelbak(TM) and then continued up to the Vincent Tumamait Trail and headed east, retracing my steps to Mt. Pinos, and back to the trailhead.