Clouds, sun and shadow accentuate the rugged topography of the northwest rim of the San Fernando Valley.
Castle Peak is the rock-capped summit on the left of the photo. Chatsworth Peak (2314′) is in shadow and behind Castle Peak. The prominent rock bands are Chatsworth Formation sandstone formed more than 65 million years ago. Oat Mountain (3747′) is the sunlit peak in the distance.
Following a December with twice normal rainfall, Downtown Los Angeles (USC) experienced the fourth driest January-February on record. Now it seems the spigot has been turned back on, and March rainfall for L.A. might very well be above normal.
As of 3:00 p.m. today, March 13, Downtown Los Angeles (USC) has recorded 2.05 inches of rain this March, boosting the rain year total (since July 1) to 9.40 inches. This is about 75% of normal for the date.
More rain is forecast over the next week or so, but the major weather models differ on the projected amounts. To make up for the January-February rainfall deficit and finish the rain year close to 100% of normal, Los Angeles needs another 5.5 inches of rain by June 30.
Not impossible, given some of the forecasts, but that would be a lot of rain for this time of year. Well see!
Update July 6, 2020. Remarkably, Downtown Los Angeles (USC) ended the rain year, July 1 to June 30, within 0.07 inch of normal rainfall. It was a tumultuous rain season that saw copious rainfall in December, and then almost none in January and February — usually the wettest months of the year. Just when we started to think “drought,” the wet weather returned. Combined, Match and April precipitation was 221% of normal. That and a little rain in May brought the Los Angeles rain year total up to 14.86 inches, just short of the normal of 14.93 inches.
Update April 12, 2020. Over six consecutive days, from April 5 to April 10, Downtown Los Angeles (USC) recorded 2.96 inches of rain. This is about 325% of the normal amount for the whole month. The precipitation totals of 14.66 inches for the rain year and 14.63 inches for the water year are now above normal for the date and within about one-third of an inch of the normal annual rainfall for Downtown Los Angeles.
Update April 10, 2020. April rainfall picked up right where March left off. As of April 9, Downtown Los Angeles (USC) has recorded 2.80 inches of rain this month. This is more than three times the normal amount of rain for the entire month of April. This brings the rain year and water year totals to 14.50 and 14.47 inches, respectively. For the first time since February 1 the rainfall totals for Los Angeles are above normal for the date. Los Angeles is now within a few tenths of an inch of normal rainfall for the year, and it is still raining today.
Update March 24, 2020. On March 22, Downtown Los Angeles (USC) set a new rainfall record for the date of 1.51 inches. As of March 24, Downtown Los Angeles has recorded 4.35 inches of rain this month. This is 179% of the normal amount of rain in March. The current rain year/water year total of 11.70/11.67 inches is about 88%/90% of normal for the date. The magic number for 100% of normal rainfall is 14.93 inches — either by June 30 (Rain Year) or September 30 (Water Year).
Update March 17, 2020. As of March 16, Downtown Los Angeles (USC) has recorded 2.80 inches of rain this month. This already exceeds the normal amount of rainfall for the entire month of March, which is 2.43 inches. The current rain year/water year total of 10.15/10.12 inches is about 79%/81% of normal for the date.
Tuesday is usually a “short run day” for me. On Tuesdays, I usually run a mile or so west on East Las Virgenes Canyon fire road, and then fork left onto another dirt road that descends a short distance, and then climbs steeply up to Lasky Mesa. Once on Lasky Mesa, I check what’s blooming, crawling or flying in the area.
Today, as I was leaving Lasky Mesa, I scanned a grove of valley oaks for a pair of northern harriers I’ve been seeing on the mesa. I didn’t see the harriers, but another pair of much smaller raptors caught my eye.
The male and female American kestrels were perched at the top of a valley oak tree, about 25 yards away. At that distance, they were difficult to positively ID, and nearly beyond the reach of my compact camera.
Usually a kestrel will fly from a perch as soon as it spots me, but this time the pair cooperated. I stopped running, grabbed the camera from my pack, and took a couple of photos. The female kestrel is perched above the male.
Along with Sandstone Peak, Tri Peaks, and Exchange Peak, Boney Peak is an officially named peak that is part of the Boney Mountain massif. The peak is located about 0.5 mile southwest of Sandstone Peak and is easily accessed from the Backbone Trail.
I’d climbed the other peaks in the area, and run past Boney Peak many times, but never scrambled to its summit. Getting to Boney Peak from the Wendy Drive trailhead was pretty much the same as doing Sandstone Peak. I took the “escalator” up the Western Ridge of Boney Mountain to Peak 2935 and then ran over to Tri Peaks. From there, I followed the Tri Peaks Trail to the Backbone Trail, near the Mishe Mokwa Trail junction.
The use trail to the top of Boney Peak leaves the Backbone Trail about a mile from the Tri Peaks/Mishe Mokwa Trail junctions. Other than a little brush, it’s fairly easy to get to the peak’s boulder-strewn summit. There was a red register can stashed in the rocks. (The title photo of Boney Peak was taken where the use trail begins.)
The actual high point of the peak is atop, a large, exposed summit block. Various trip reports describe the easiest route up the summit block as class 3. That seems about right. Although relatively straightforward, the use of handholds is necessary, and a fall would ruin your whole day. Like many such boulders, it is easier to climb up than to climb down, and someone without rock climbing experience could easily find themselves unable or unwilling to climb down.
From Boney Peak, I returned to the Backbone Trail and headed west, down the Chamberlain Trail and on to the Danielson Multi-Use area. A few brightly-colored, yellow-orange poppies were already blooming along the trail. The rest of the run was the usual jog up Sycamore Canyon to the Upper Sycamore Trail, and then back to Satwiwa and Wendy Drive.
Here’s a 3D Cesium interactive view that shows a GPS track of my route. The view can be zoomed, tilted, rotated, and panned. Placemark and track locations are approximate and subject to errors.
In January, on my way to do a run on the Backbone Trail, I stopped for a moment along Kanan Road to see if the ridges on the east side of Ladyface peak were still accessible. I didn’t see any obvious access issues and made a mental note to get back and do the peak soon.
“Soon” turned out to be earlier this February. While the route and the climbing were about the same as the last time I did the Ladyface Loop, the mountain itself had changed dramatically.
Nearly all of the chaparral on the peak was incinerated by the Woolsey Fire. Compare the title photo above to this photo taken before the fire. Before the Woolsey Fire, the last time Ladyface was burned in a wildfire was in the October 1982 Dayton Canyon Fire — a span of 37 years.
Like other areas burned in the Woolsey Fire, Ladyface is recovering. It will just take time. December’s rains have turned the mountain green, laurel sumac and other chaparral plants are crown-sprouting, and the season’s first wildflowers are blooming along the sun-warmed ridges.
For those with appropriate skills and experience, Ladyface is a relatively straightforward and enjoyable climb. But some of the things that make it interesting are the very things that can make it sketchy.
Some climbing with the hands is necessary — and that includes going down the mountain as well as going up. The route-finding isn’t always obvious, and the rock isn’t always sound. The volcanic rock is sharp, and some sections of the trail on the east/southeast ridge are very slippery — especially if wearing smooth-soled shoes.
Below are a couple of photos of the east/southeast ridge.
The loop packs a lot of adventure into its 2.5 miles!
The range of temperatures had been remarkable. At the Secret Trail trailhead in Calabasas, where I left my car, it had been a balmy 60 degrees. Near the start of my run from the Tapia Trailhead in Malibu Canyon, it had been a very chilly 32 °F. Near the end of the run, the temp topped out at 79 °F. That’s SoCal Winter running!
On the way to Saddle Peak, I was surprised to see how wet it was on some sections of the Backbone Trail. There has been very little rain this January, but marine layer dew, the trail’s north-facing aspect, the low sun angle, the canopy of bays and oaks, and relatively cool temps have kept the trail damp. In places it looked like it had just rained yesterday.
Because there’s about 1000′ less elevation gain, I usually do this run in the opposite direction, starting on the Secret Trail and ending at Tapia. This is the route described in the venerable guidebook, 50 Trail Runs in Southern California. But I’d run it in that direction a bunch of times — so here I was, chugging up the Backbone Trail, nearing the end of a 2600′, seven-mile climb from Tapia to Saddle Peak.
The area around Saddle Peak is yet another spectacular section of the Backbone Trail. (There are so many!) Just west of the peak, the trail winds through a narrow passage with massive sandstone rocks on either side. As the trail levels out, there is a short spur trail to the peak’s antennae-infested summit.
Even if a little obstructed, views from the top extend to Catalina, Boney Mountain, Mt. Pinos, and Mt. Baldy. Sometimes San Gorgonio Mountain and San Jacinto Peak can be seen beyond Mt. Baldy. The round trip to the summit of Saddle Peak adds about 0.8 mile. The eastern summit is slightly lower, but no antennae obstruct the view.
Getting to Saddle Peak from the Tapia trailhead is relatively straightforward, if a bit strenuous. Getting to Calabasas Peak and the Secret Trail from Saddle Peak is not as simple.
The “normal” way to get from Saddle Peak to Calabasas Peak would be to run back down the Backbone Trail to the Stunt High Trail and then follow that trail to the parking area on Stunt Road. Calabasas Peak Mtwy is across the highway and slightly downhill (west) of the parking area and leads to Calabasas Peak and the Secret Trail.
If doing the regular route, note that the Stunt High Trail crosses Stunt Road twice on the way down. In each case turn right and follow the road east about 100 yards to pick up the trail on the other side of the road. There are also various side trails to avoid.
I had been planning to do the regular route, but as I was returning to the Backbone Trail from Saddle Peak, it occurred to me there was a way to avoid backtracking. Instead of turning left on the Backbone Trail and descending to the Stunt High Trail, I turned right and continued east, past the water tank, to the Lois Ewen Overlook. From there, I ran over to the Topanga Lookout and then scrambled down Topanga Lookout Ridge to Calabasas Peak Mtwy.
This option is more adventurous, but requires good route-finding skills and being comfortable clambering down a rocky ridge. This 3D Cesium interactive view shows a GPS track of my route. The yellow track is today’s route. The red track is the usual route between the Backbone Trail and Calabasas Peak Mtwy. The view can be zoomed, tilted, rotated and panned. Placemark and track locations are approximate and subject to errors.
Scrambling down the ridge put me at “The Bench,” at the junction of Calabasas Peak Mtwy and Red Rock Road. This is a little more than a mile from Calabasas Peak. Once on Calabasas Peak, it was only about 0.6 mile to the top of the Secret Trail, and from there about 1.3 miles of mostly downhill running to the trailhead.
With about 4000′ of gain over 14 miles, it was a demanding route, with challenging route-finding and a fun scramble down a rocky ridge. Here are a few photos taken along the way.