Category Archives: photography|black & white

Missing Snakes at Ahmanson Ranch

Legend has it that St. Patrick chased all the snakes from Ireland, and while there have been no reports of the 5th Century cleric being sighted at Ahmanson Ranch, I don’t recall a Spring and Summer when I’ve seen so few snakes in the 3,000 acre preserve.

I’ve run at Ahmanson Ranch — now Upper Las Virgenes Canyon Open Space Preserve — more than a decade. I generally run at Ahmanson a few times a week and have become very familiar with the area’s plants and wildlife.

So far this year I’ve seen no mature rattlesnakes and only one gopher snake at Ahmanson. I’ve seen a couple of baby rattlesnakes and a handful of tracks, but that’s it. In some years I’ve counted more than a dozen snake tracks during one 7 mile run.

The reduction in the snake population is likely related to back-to back years with low rainfall. This year Downtown Los Angeles has recorded only 2.72 inches of rain since January 1. That’s a deficit of nearly 8 inches and about 25% of the normal amount of rainfall.

The reduced rainfall not only reduces the population of rodents, reptiles and other prey animals sought by snakes, but also increases the likelihood snakes will be preyed upon by animals higher on the food chain. Snakes, including rattlesnakes, are eaten by a long list of birds and mammals, and may also be preyed upon by other snakes. Humans also kill a large number of snakes.

The title photograph is the track of a Southern Pacific rattlesnake.  The snake was moving from the upper left of the photo to the lower right.

Some related posts: Big Southern Pacific Rattlesnake at Ahmanson Ranch, Southern Pacific Rattlesnake

Split Rocks, Squeeze Chimneys and the Steck-Salathé

Split Rock Stoney Point Poster

As long as we’re talking about split rocks, the poster above was based on a photo of mine from 1971 of “Split Rock” at Stoney Point, near Los Angeles. Rock climbers of my generation will recognize the Robbins’ “blue boots” that Tom is wearing.

This type of feature is called a “chimney” and the climbing technique being employed is called “chimneying.” Chimneys vary in width from a “squeeze” chimney, in which you can barely fit your body, to chimneys so wide it’s difficult to span their width. One side of Split Rock is average width and the other is a squeeze chimney.

Perhaps the most infamous chimney in the U.S. is the Narrows on the Steck-Salathé route on Sentinel Rock in Yosemite. The chimney abruptly changes from a comfortable width that is easily climbed to an impossibly narrow slot. It’s easy enough to get the top half of your body up into the slot, but the bottom half poses a significant dilemma. How do you make upward progress with your upper body wedged and your legs and feet dangling?

I think my upward progress into the slot might have been measured in millimeters per hour. At least it felt that way. It was so narrow that I could hold myself in place by taking a deep breath! Eventually I was able to get fully into the slot and then it was just a matter of being patient and threading my way through the remainder of the claustrophobic passage. (The photos of the Narrows in Climbing the Steck-Salathé by Guillaume Dargaud illustrate the situation well.)

From the top of the Narrows Ron and I still had a few more pitches to climb, and we topped out shortly before sunset. Around us the granite glowed in a rich golden light — the kind of light that seems only to be found on mountains, rivers and other places the sharp edge of adventure dwells.

The day had been long and challenging, but we were not done — we still had to get down. By the time we reached the upper section of the descent gully it was starting to get dark. There were still patches of snow in the gully and the temperature was dropping. Rather than risk a fall on frozen snow or meltwater, we opted to bivi.

Skies were clear and the night was going to be cold. We didn’t have much in the way of warm clothes, but we did have matches and started a small fire on the granite ledge that was going to be our lodging for the night. About the time we were settling in, two headlamps came bobbing down from the direction of Sentinel. The climbers had just come off the Chouinard-Herbert route and were more than happy to call it a day. We shared our meager resources, and with the fire we all had enough to get by.

L.A. Basin Clouds & Showers

Los Angeles basin clouds and showers

According to the 1981-2010 climate normals January, February and March are the rainiest three months at Downtown Los Angeles (USC). March is normally a little wetter than December, but close enough that the four months December to March “normally” account for nearly 80% of Los Angeles’ annual rainfall total of 14.93 inches.

But normal weather years only exist on paper, and those rarely seen monthly normals are just a reference so we may make comparisons from year to year. This water year Downtown Los Angeles was only about 0.2 inch under the normal amount of rainfall for December, but as of today is about 1.5 inches under the normal January total. When you add it all up Los Angeles is at about 63% of the normal total for the water year.

Although much of Southern California has recorded well below average rainfall, that isn’t necessarily the case across the board. LAX’s water year rainfall total currently stands at 89% of normal, and Santa Barbara Airport is at 94% of normal.

There are some indications (GWO phase and forecast MJO activity) that February might just have its share of wet weather. We’ll see!

Update February 13, 2013. Despite hopeful signs at the end of January and CPC’s above average Precipitation Outlook for Southern California for the period February 5-9 and February 7-13, Downtown Los Angeles (USC) has recorded only 0.02 inch of rain so far this February. Los Angeles water year rainfall now stands at 4.42 inches, which is slightly less than half of normal. Once again it looks like there may be some opportunities for wet weather in California during the last week or so of February, but the increasingly La Nina-like character of the atmospheric circulation suggests more rain is probable in Northern and Central California than in the southern part of the state. Again, we’ll see!

The photo of clouds and showers in the Los Angeles basin is from this morning’s run in the Santa Monica Mountains.

No Snow in Sight!

View to the ocean from Eagle Rock in the Santa Monica Mountains

Well, actually you could see some snow on Mt. Baldy and the higher peaks of the San Gabriel Mountains, but that snow was 50 miles away. So far there had been a little frost in the shadows and mud in the low spots of the fire roads of Topanga State Park, but not a patch of snow in sight.

Lynn & Frank were heading back to the land of rain and snow for Christmas and there WAS snow on their local trails. More snow and bone-chilling temps were in the forecast, and a long snow-free run in the Santa Monica Mountains was a great way to celebrate the holidays!

We had taken a detour from the Backbone Trail to the top of Eagle Rock. After enjoying the view we would extend the detour down the Musch Trail and pick up the Backbone Trail at Trippet Ranch. From Trippet we would follow the Backbone Trail down into Topanga Canyon, up Hondo Canyon, over to Saddle Peak and then down to Malibu Canyon.

With a couple of short side trips the distance from the End of Reseda (Marvin Braude Mulholland Gateway Park) worked out to about 21 miles. The distance and elevation gain were about the same as last Saturday’s run — also on the Backbone Trail.

Related post: July Fourth Trail Run to Trippet Ranch, Hondo Canyon and Saddle Peak