As I ran out the Main Drag at Ahmanson Ranch I was trying to decide where — and how far — to run.
Saturday I was planning to do a hilly 25K race and didn’t want to overdo it. But it was one of those unique late afternoons after the change from Daylight Savings Time — the running was excellent and the opportunity for a good photograph promising.
So where to run? Yesterday I’d run down the Main Drag and up the “Beast” to Lasky Mesa. The moon had been rising and I’d been intrigued by a composition involving a hay shed, alpenglow and the moon. Hmmm, if the high clouds did not get too thick, the moon would be rising a little later, and there might be another photo opportunity up on Lasky Mesa.
On the other hand, the high clouds had a look that reminded me of an exceptional sunset here a few years before. That could also be interesting IF the sunset happened, and IF I was in a place where I could get a good shot. But being in the right place at the right time was going to involve a run that was a little longer than I’d planned.
I took a chance and did the longer run. On the way back, the moon had risen over the hills to east, and within the veil of striated high clouds it looked spectacular. There was still no color from the sunset and it was getting dark. Oh well, maybe I should have just done the loop on Lasky Mesa.
Then as I started to run down a short hill, I glanced back and saw a slight tinge of pink developing on the fringe of some of the clouds. I turned around and headed back to the west. The lighting was changing fast, but it didn’t take long to find a decent spot and get the photograph I’d visualized.
What a difference a week makes! Last week an unseasonably deep upper level low, unusually strong 170+ kt Pacific jet, and associated cold front combined to produce record-setting rainfall and cool temperatures in Southern California. This week high pressure and a weak offshore flow produced triple digit temperatures in some areas and set new high temperature records Wednesday in Downtown Los Angeles, Long Beach and Santa Barbara.
Which pattern is more likely this rain season? Will Southern California tend to be drier like this week, or wetter like last week and last year? Despite last year’s wet rain season, wet La Nina Winters are not the norm. Generally, La Nina conditions result in drier than normal rain seasons in Southern California, and El Nino wetter.
Following a Summer respite La Nina conditions have reemerged in the equatorial Pacific, and appear to be consolidating. Equatorial SST anomalies have continued to decrease and now range from -1.5°C at 100°W to -0.5°C at 170°E. Equatorial Pacific temperature cross sections show substantial subsurface cooling from July 11 to September 11. The Multivariate ENSO Index (MEI) has dropped from -0.5 for July/August to -0.8 for the August/September season. This drops the MEI from a rank of 16th for July/August to 13th for August/September since 1950. This is well within La Nina territory but weaker than last year’s rank of 1st for August/September.
A precipitation composite for seven years* since 1950 in which La Nina conditions persisted or reemerged in the year following a first year La Nina indicates that “on average” the coastal Southern California climate division recorded about 5 to 6 inches less precipitation than normal for the period November through March. The percent of normal water year rainfall recorded at Downtown Los Angeles (USC) ranged from a low of 47% (1971, 7.17″), to a high of 106% (1955, 16.00″). The average rainfall for these years was 70.5%, or 10.7″.
We’ll get the official NOAA/CPC outlooks next week around October 20, when CPC’s Three-Month Precipitation Outlooks and NOAA Winter Outlook are expected to be released.
*The years included in the selection were 1950-51, 1955-56, 1962-63, 1971-72, 1974-75, 1999-2000 and 2008-09. The base period was 1971-2000. The selection was based on the MEI.
We’d just arrived in Calistoga for Amanda & Brett’s wedding, and I was looking through the “where’s the ice machine” info provided by the B & B. A couple pages down, past the wineries and restaurants was a list of local hiking trails. What better way to work off the torpor of I-5 than to do a trail run?
The trailhead for the Oat Hill Mine Trail was just a half-mile away and in a few minutes I was jogging north on Hwy 29 toward Silverado Trail road. I had about two hours before I needed to be back. The sun would be setting in a couple of hours anyway, so I could run up the trail about 75 minutes before turning around.
Other than the brief description in the B & B info, I had not researched the trail. It looked like it worked up the east side of a ridge through oak, pine and fir toward some volcanic outcrops. On a hot day the trail would be brutal. This afternoon the temperature was around eighty, and in the long shadows of the ridge, it was relatively cool and shady.
Since it follows an old mine cart road, the grade of the trail is generally not too steep and is very runnable. It’s rough and rocky in places, but most trails I run are rough and rocky in places. Heads up – the trail appears to be multi-use. Judging from the bear scat there are some bears (and other animal life) in the area as well.
I could have pushed it a little further up the trail, but the natural spot to turn around was the top of Bald Hill. A short use trail leads to the top from the saddle northeast of the hill. Oddly shaped fingers and pinnacles of weathered volcanic rock (andesite) form its summit.
The volcanic bluffs known as the Palisades encompass much of the view to the North. To the northwest is Mt. St. Helena, abutting the west end of the Table Rock-Palisades escarpment. To the west is Napa Valley, and in the distance, the coast near Bodega Bay.
The Oat Hill Mine Trail page of the Napa County Regional Park and Open Space District web site has more info about the trail, including a PDF brochure, trail map and a self-guided tour of the geology along the trail. The round-trip length of the run from near Brannan & Lincoln in Calistoga was a little under eight miles, with an elevation gain loss of about 1500′. From the trailhead it’s about a mile less.
With a car shuttle, the approximately 11 mile route linking the Table Rock, Palisades, and Oat Hill Mine trails looks like it would be an outstanding trail run. The Table Rock trailhead is about 8 miles north of Calistoga on Hwy 29. Next time!
A run or hike doesn’t have to be long or difficult to be enjoyable! It had been a while since I’d done San Gabriel Peak, Mt. Markham, and Mt. Lowe; and although I’d run within a quarter-mile of the summit of Mt. Disappointment several times, I’d never done the last bit up to the peak. All four of these peaks can be done in a (round trip) run/hike of less than ten miles, with a cumulative elevation gain/loss of around 3000′.
Depending on where you prefer to park, the run/hike can start at the San Gabriel Peak Trail trailhead, which is about one-third of a mile up the Mt. Wilson Road, or at Red Box on Angeles Crest Highway. Parking at Red Box requires running/hiking on Mt. Wilson Road to the trailhead.
The San Gabriel Peak/Mt. Disappointment trail climbs up through a forest of chaparral, canyon live oak, and Bigcone Douglas-fir about 1 1/2 miles to the Mt. Disappointment road, just below the antennae-infested summit of the peak. Along the way there are great views of the canyon of the West Fork San Gabriel River and San Gabriel Peak. The paved road is followed south (left) to a sharp switchback and then a short distance up to the top of Mt. Disappointment (~ Mile 2.1).
In Trails of the Angeles, John Robinson describes how government surveyors lugged their equipment to the top of Mt. Disappointment in 1875, only to discover that another peak to the southeast was higher. That peak was San Gabriel Peak. Except for Strawberry Peak (6164′), San Gabriel Peak (6161′) is the highest of the front range peaks. It is the most prominent peak on the eastern skyline when viewed from the San Fernando Valley, and is sometimes mistaken for Mt. Wilson.
I imagine it was a bit easier for me to get over to San Gabriel Peak than for the surveyors when they did the peak’s first ascent. All I had to do was run a third of a mile down a paved road and pick up the San Gabriel Peak Trail on the southeast corner of the switchback. The trail up to San Gabriel Peak forks to the left off the trail to Markham Saddle about a tenth of a mile from the switchback.
The divide extending from Mt. Disappointment to Mt. Wilson was the approximate boundary of the Station Fire in this area. Although the summit of San Gabriel Peak burned, much of the northeast side of San Gabriel Peak and Mt. Disappointment did not. From what I can determine, the northeast side of these peaks last burned in the 1898 “Mt. Lowe” fire. There’s a nice section of trail just below the summit of San Gabriel Peak that passes through a corner of Bigcone Douglas-fir forest that was not consumed by the Station Fire.
After enjoying the panoramic view from the top of San Gabriel Peak (~ Mile 2.9), I retraced my steps back down to the “main” trail and continued to descend to Markham Saddle and the Mt. Lowe fire road. At this point another trail begins on the Mt. Markham side of the road. This trail leads southwest to a saddle between Mt. Markham and Mt. Lowe. Mt. Lowe Road is closed between Markham Saddle and Eaton Saddle because an active rock slide destroyed the road just west of Mueller Tunnel.
From the Markham-Lowe saddle a path follows the southwest ridge of Mt. Markham about a half-mile to its summit. The route up the ridge is relatively straightforward, but a steeper section requires a little scrambling over fractured, loose rock. The high point on Mt. Markham’s elongated summit ridge appeared to be a pile of rocks covered with Turricula. A little further out on the ridge was a clearing with a rusty can that may have been a summit register (~ Mile 5.1).
Returning to the Markham-Lowe saddle, less than a half-mile of moderate uphill led to the summit of Mt. Lowe (~ Mile 6.0). There’s a bench here, along with locating tubes pointed at various landmarks. As explained by the interpretive sign on the peak, Professor Thaddeus Lowe had planned to build a large hotel on the summit, serviced by the Mt. Lowe Railway. In his grand vision, a suspended cable car would have continued to San Gabriel Peak, where an observatory was to be built. Here’s a map of Mt. Lowe area trails and landmarks created by The Scenic Mt. Lowe Railway Historical Committee.
Turricula was present virtually everywhere along the route that had been burned, and could not entirely be avoided. It was especially prevalent on the path to summit of Mt. Markham from the Markham-Lowe Saddle.
I’ve been exposed to Turricula now on a number of runs, and except for the first time, when I literally waded through unbroken stands of the sticky young plants, it hasn’t been a problem — even wearing running shorts and short-sleeves. I’ve had a little irritation on my ankles, or sometimes along my waistband, or a random spot here or there, but it’s been no big deal. Certainly nothing like the widespread inflammation, swelling and blisters the first time!
Of course now I at least make an attempt to avoid the plants. And I also wash off my arms and legs at the earliest opportunity after being exposed to Turricula.
It also seems the older plants don’t have as much of the “exudate” on them, since my legs and arms haven’t become sticky from brushing up against the plants. Anecdotal evidence suggests that in the older plants irritation results from the almost microscopic hairs on the plant. It is thought these irritating hairs are more easily broken and shed as the plant ages.
Originally posted November 25, 2006. Updated November 11, 2020.
Nature isn’t necessarily nice. Behavior and interactions among animals are often violent. So it is with mountain lions. But the mountain lions of the Santa Monica Mountains also have to cope with the additional problems of living on an island of lion habitat in the middle of an ocean of urban sprawl.
The mountain lion tracks above were photographed on a run at Sage Ranch Park in late January 2000. They might have been made by a young male mountain lion designated P3, whose territory encompassed this area. There is also a possibility there were from an older female lion, P4 that frequented the Rocky Peak area. Unfortunately, both these animals were killed in late 2004 by eating prey (coyote) that had eaten rodents that had consumed anticoagulant-based poisons. These poisons are used by parks, schools, golf courses, and housing developments for rodent control.
The P3 and P4 pumas were tracked as part of an ongoing study started by the National Park Service in 2002 to learn more about mountain lions in the Santa Monica Mountains National Recreation Area. As of May 2012, twenty-six mountain lions, P1 to P26, have been tracked, and their history has been quite a saga.
The patriarch of the lions in the study is P1. He was the first lion captured and collared in 2002, and at that time was estimated to be 5-6 years old. In his prime, P1 was a large, 140+ lb. male whose territory was essentially all of the Santa Monica Mountains. In August of 2004, P1 and P2 – the only female lion known to be in P1’s range – produced a litter of four cubs — two males (P5 and P8) and two females (P6 and P7).
Despite high hopes for the lions and their new litter, things turned ugly in August of 2005, when P1 killed his mate P2. A few months later, in June of 2006, P1 also killed one of the 22-month-old females from the litter, P7. According to biologists these were not the actions of a lion run amuck but were most likely related to conflicts over kills, or in the case of P2, a mother protecting her offspring.
As might be expected, the young males from the litter, P5 and P8, headed for opposite ends of P1’s territory. However, urbanization and limited linkages essentially prevented their escape to other wildland areas.
In early September 2006, P5 was likely killed by P1, and in a development that surprised researchers, P8 appeared to have been killed by an unknown lion, probably male, inside of P1’s territory. The “unknown lion” was the male P9, who was killed by a vehicle on Las Virgenes road in July 2007.
One other female lion was collared and designated P13. DNA testing indicated that P13 was a daughter of P6. At that time P6 was the only surviving lion from P1 and P2’s 2004 litter.
P1 appears to have been injured in a battle for dominance in March 2009. A bloody radio collar and tufts of hair were found in a tree in Hidden Valley, near Thousand Oaks. P1’s opponent was suspected to be P12, a lion collared in December 2008, and the first lion to be tracked crossing the 101 Freeway. Scat found three weeks after the fight was genotyped, and found to be P1’s.
In May 2010 P13 had a litter of three kittens — P17 (female), P18 (male), and P19 (female). The father was P12. Since P12 originated from an area other than the Santa Monica Mountains, this increased the genetic diversity of the mountain lion population in the study. P18 was killed August 30, 2011, attempting to cross the 405 freeway.
It is unclear how many male lions now inhabit P1’s original territory. P12’s collar is no longer functioning. P18 was killed August 30, 2011, attempting to cross the 405 freeway. P15 was found deceased on September 11, 2011. Reportedly another male lion has been photographed in the area.
In May 2010 a male lion living in the Santa Susana Mountains west of I-5 was collared and given the designation P16. This is the first lion to be followed in the Santa Susana Mountains since P3 and P4 died in 2004, after eating contaminated prey. P21, an adult male, is also being tracked in the Santa Susana Mountains. Both P16 and P21 have made excursions into Angeles National Forest, and P16 remains there.
Johanna Turner of CougarMagic.com has captured breathtaking stills and videos of the area’s mountain lions and other wildlife.
Following are some previous updates to this post, with links to additional articles and information.
Update October 24, 2012. The remains of P-25, an approximately one-year-old female mountain lion were discovered by hikers in Point Mugu State Park on Sunday. P-25 and P-26 (male) are the offspring of P-12 (male) and P-13. The death did not appear to be the result of a conflict with another lion. A necropsy is pending.
Update October 18, 2012. This summer NPS biologists discovered two mountain lion kittens, P-23 (female) & P-24 (male), east of Circle X Ranch in the Santa Monica Mountains. They are the offspring of P-12 (male) and P-19, a daughter of P-12. The kittens were outfitted with tracking devices.
Update June 18, 2012. Analysis of the DNA of the mountain lion killed by authorities in downtown Santa Monica on May 22 revealed it is related to lions that reside north of the 101 Freeway. One possibility is that the approximately three-year-old lion was the offspring of mountain lion P-12. P-12 has been documented crossing the 101 Freeway in Agoura and is the only lion known to have done so.
Update May 26, 2012. Earlier this Spring biologists from Santa Monica Mountains National Recreation Area (SMMNRA) captured an adult male mountain lion in the Griffith Park area. Designated P-22, the approximately three-year-old lion is the first to have been photographed east of Cahuenga Pass and within the Santa Monica Mountains eco-region. The lion was fitted with a GPS collar and released where it was captured. According to Kate Kuykendall, Public Affairs Officer for the SMMNRA, preliminary genetic analysis by UCLA indicates that P22 is likely from the Santa Monica Mountains, which would mean he crossed both the 405 and the 101 Freeways.
Update November 21, 2011. On October 4, 2011, the National Park Service announced that male mountain lion P-15 has been killed. It was the first documented intentional human-caused death of a mountain lion in the Santa Monica Mountains. P-15’s collar stopped transmitting on August 25, 2011. P-15 was discovered on September 11, 2011, following a report of a dead mountain lion. The California Department of Fish and Game and the National Park Service are seeking information related to the death of P-15 and the parties responsible. With the addition of $5000 from the City of Malibu, the reward being offered for information leading to the arrest and conviction of the poachers currently stands at $16,700. The DFG Cal Tip Hotline is 1-888-334-2258.
Update August 7, 2009. According to Where the Mountain Lions Live in the Santa Monica Mountains in laist.com, P1 may have survived the fight with another mountain lion back in March. DNA from scat collected about two weeks after the fight matched P1!
Update March 28, 2009. There was sad news earlier this month. According to an article in the Daily News, mountain lion P1, the long-standing patriarch of the Santa Monica Mountains, appears to have lost a battle for dominance with another mountain lion. A bloody radio collar and tufts of hair were found in a tree in Hidden Valley, near Thousand Oaks. P1’s opponent is suspected to have been P12, a lion collared in December, and the first lion to be tracked crossing the 101 Freeway.
Update October 6, 2008. The Ventura County Star reported that a young male lion was found dead on October 2 on the 118 freeway, just west of Rocky Peak Road. A wildlife passageway crosses under the freeway nearby and has been used by at least one other lion. On July 18 a mountain lion was reported in the area of the Chumash Trail.
Update May 1, 2008. NPS wildlife biologists are currently aware of 4 lions in the Santa Monica Mountains — 2 recently radio-collared young males designated P10 and P11, and P1 and P6. There is probably at least one more female, the mother of P10 and P11. A remote camera picture has also been taken of a lion in the Simi Hills.
Update January 25, 2008. An article in the Simi Valley Acorn reported that on January 13, 2008, a mountain lion was discovered in an abandoned building near Chatsworth Reservoir. Two days later there was another mountain lion sighting in the nearby Simi Hills by employees at the Santa Susana Field Laboratory.
Update August 7, 2007. According to an article in the Malibu Times, on July 31 a five or six-year-old mountain lion was hit by a car near the tunnel on Malibu Canyon Road and died shortly thereafter. The mountain lion, designated P9, was recently collared, and along with P1 and P6 was one of three mountain lions being tracked by the NPS. There is speculation that P9 may have been the unknown lion that killed P8.
No matter if you run at the front, middle, or back of the pack, there’s the race you plan, and the race you run.
Based on the course info, it looked like the 7th edition of the Mt. Disappointment 50K was going to be more difficult than in 2009 and 2010, adding both mileage and elevation gain. Because of the closure of Mueller Tunnel and the damage done by the Station Fire and subsequent floods, we still wouldn’t be running up and over the shoulder of Mt. Disappointment, or down to Clear Creek and around Strawberry Peak, but the 2011 course would make up for that with its own very memorable sections.
To try and cope with the difficulties of the course, I’d put in extra miles and done more back to back Saturday-Sunday runs. But in one of those uh-oh moments a couple of miles into the race, I could feel in my legs that I was probably going to need to adjust my expectations. I wasn’t injured. I wasn’t getting over a cold or flu. My stomach wasn’t upset. I felt pretty good. But there was this nagging bit of fatigue in my legs…
At the bottom of the Valley Forge we turned onto the Gabrielino Trail, and started up the canyon of the West Fork toward Red Box-Rincon Road. The change in grade from level to uphill confirmed it. I stepped aside so two running friends could pass. Maybe it was a tapering or over-training issue, or maybe it was just “one of those days.” Whatever, the legs were just not cooperating.
The irony is, this was probably a good thing. The day turned out to be the hottest of any Mt. Disappointment race to date. The lurking leg fatigue forced me to not push the pace, which made dealing with the temperature easier.
And hot it was! The forecast had looked decent just two days before the race, but Friday temperatures exploded in the mountains, jumping 10-12 degrees in 24 hours. The hot temps on Friday carried over into Saturday, making race day just that much warmer.
Here are the race day temperatures at Clear Creek and Chilao for 2005-2011, and Mt. Wilson for 2009-2011. And these temps are the temperature off the ground and in the shade! A better indication of the temperature in the sun is the “fuel temperature.” This is the temperature of a ponderosa pine dowel in direct sun. Here are plots of the race day fuel temperature at Clear Creek and Chilao for 2005-2011.
Because I wasn’t pushing the pace I didn’t hesitate to take a little extra time at aid stations. I can still feel that ice cold sponge on the back of my neck, and the cold water running down my back. This year there were numerous small stream crossings, and I think there was at least one small stream between every aid station. This was “free” cooling, and I paused a dozen times to dump water over my head. Thanks to the West Fork San Gabriel River, I was soaked from head to toe for the first steep, sun-baked section of Edison Road. This was also the case on the Silver Moccasin Trail in Shortcut Canyon and on part of Kenyon Devore.
Hot day or not there were some remarkable performances. Heather Fuhr was not only was the first place woman, she was fourth overall and set a new women’s course record of 5:07:11. Perennial favorite Jorge Pacheco sped through the tough Mt. Disappointment course in 4:46:29, winning the overall and setting a new course record in the Men’s 40-49 Division.
Once again the event was superbly organized by race director Gary Hilliard and the Mt. Disappointment 50K Staff, with the help of an extraordinary group of volunteers, runners, SAR personnel and sponsors. Thank you!