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Anybody who refuses to leave a mudslide evacuation area needs to watch this video:

It’s a live recording of the slide that killed ten people in LaConchita, California, on January 10, 2005. We know people who knew people who were killed in that slide. The story of the Wallet family is especially tragic. Jimmy Wallet was walking back from a corner store with some ice cream for his family when the mudslide in the video above destroyed his house before his eyes, burying his wife and three little daughters. Only he and his teenage daughter, who was out with friends, lived. Six others also died.

And this wasn’t  an especially big slide — or the first to strike that little community. Here’s one from five years earlier. That killed people too.

I’ve been listening to KNX, which has been reporting on the heavy weather in Southern California, and I’m amazed to hear that a large percentage (40%, I think the reporter said) of evacuees are waiting it out.

Here’s the deal, folks: mudslides are inevitable. If you live below a steep hill or mountain slope in a part of Southern California that’s getting heavy rain, and you’re under an evacuation order, get out. Right now (5:45pm Pacific), Acton. La Crescenta, La Cañada-Flintridge, Glendale, Tujunga Foothill and Sierra Madre all have a total of nearly 2000 homes under evacuation order. (So says the official speaking at a news conference on KNX right now.)

Yesterday I shared some of what John McPhee wrote in The Control of Nature about a mudslide (in Glendale — in the same area under evacuation orders now. Here is the whole passage, courtesy of  this page on Los Angeles provided by United States Geological Survey:

In Los Angeles versus the San Gabriel Mountains, it is not always clear which side is losing. For example, the Genofiles, Bob and Jackie, can claim to have lost and won. They live on an acre of ground so high that they look across their pool and past the trunks of big pines at an aerial view over Glendale and across Los Angeles to the Pacific bays. The setting, in cool dry air, is serene and Mediterranean. It has not been everlastingly serene.

On a February night some years ago, the Genofiles were awakened by a crash of thunder — lightning striking the mountain front. Ordinarily, in their quiet neighborhood, only the creek beside them was likely to make much sound, dropping steeply out of Shields Canyon on its way to the Los Angeles River. The creek, like every component of all the river systems across the city from mountains to ocean, had not been left to nature. Its banks were concrete. Its bed was concrete. When boulders were running there, they sounded like a rolling freight. On a night like this, the boulders should have been running. The creek should have been a torrent. its unnatural sound was unnaturally absent. There was, and had been, a lot of rain.

The Genofiles had two teen-age children, whose rooms were on the uphill side of the one-story house. The window in Scott’s room looked straight up Pine Cone Road, a cul-de-sac, which, with hundreds like it, defined the northern limit of the city, the confrontation of the urban and the wild. Los Angeles is overmatched on one side by the Pacific Ocean and on the other by very high mountains. With respect to these principal boundaries, Los Angeles is done sprawling. The San Gabriels, in their state of tectonic youth, are rising as rapidly as any range on Earth. Their loose inimical slopes flout the tolerance of the angle of repose. Rising straight up out of the megalopolis, they stand ten thousand feet above the nearby sea, and they are not kidding with this city. Shedding, spalling, self-destructing, they are disintegrating at a rate that is also among the fastest in the world. The phalanxed communities of Los Angeles have pushed themselves hard against these mountains, an aggression that requires a deep defense budget to contend with the results. Kimberlee Genofile called to her mother, who joined her in Scott’s room as they looked up the street. From its high turnaround, Pine Cone Road plunges downhill like a ski run, bending left and then right and then left and then right in steep christiania turns for half a mile above a three-hundred-foot straight-away that aims directly at the Genofiles’ house. Not far below the turnaround, Shields Creek passes under the street, and there a kink in its concrete profile had been plugged by a six-foot boulder. Hence the silence of the creek. The water was not spreading over the street. It descended in heavy sheets. As the young Genofiles and their mother glimpsed it in the all but total darkness, the scene was suddenly illuminated by a blue electrical flash. In the blue light they saw a massive blackness, moving. It was not a landslide, not a mudslide, not a rock avalanche; nor by any means was it the front of a conventional flood. In Jackie’s words, “It was just one big black thing coming at us, rolling, rolling with a lot of water in front of it, pushing the water, this big black thing. It was just one big black hill coming toward us.”

In geology, it would be known as a debris flow. Debris flows amass in stream valleys and more or less resemble fresh concrete. They consist of water mixed with a good deal of solid material, most of which is above sand size. Some of it is Chevrolet size. Boulders bigger than cars ride long distances in debris flows. Boulders grouped like fish eggs pour downhill in debris flows. The dark material coming toward the Genofiles was not only full of boulders; it was so full of automobiles it was like bread dough mixed with raisins. On its way down Pine Cone Road, it plucked up cars from driveways and the street. When it crashed into the Genofiles’ house, the shattering of safety glass made terrific explosive sounds. A door burst open. Mud and boulders poured into the hall. We’re going to go, Jackie thought. Oh, my God, what a hell of a way for the four of us to die together.

The parents’ bedroom was on the far side of the house. Bob Genofile was in there kicking through white satin draperies at the paneled glass, smashing it to provide an outlet for water, when the three others ran in to join him. The walls of the house neither moved nor shook. As a general contractor, Bob had built dams, department stores, hospitals, six schools, seven churches, and this house. It was made of concrete block with steel reinforcement, 16 inches on center. His wife had said it was stronger than any dam in California. His crew had called it “the fort.” In those days, 20 years before, the Genofiles’ acre was close by the edge of the mountain brush, but a developer had come along since then and knocked down thousands of trees and put Pine Cone Road up the slope. Now Bob Genofile was thinking, I hope the roof holds. I hope the roof is strong enough to hold. Debris was flowing over it. He told Scott to shut the bedroom door. No sooner was the door closed that it was battered down and fell into the room. Mud, rock, water poured in. It pushed everybody against the far wall. “Jump on the bed,” Bob said. The bed began to rise. Kneeling on it — on a gold velvet spread — they could soon press their palms against the ceiling. The bed also moved toward the glass wall. The two teen-agers got off, to try to control the motion, and were pinned between the bed’s brass railing and the wall. Boulders went up against the railing, pressed it into their legs, and held them fast. Bob dived into the muck to try to move the boulders, but he failed. The debris flow, entering through windows as well as doors, continued to rise. Escape was still possible for the parents but not for the children. The parents looked at each other and did not stir. Each reached for and held one of the children. Their mother felt suddenly resigned, sure that her son and daughter would die and she and her husband would quickly follow. The house became buried to the eaves. Boulders sat on the roof. Thirteen automobiles were packed around the building, including five in the pool. A din of rocks kept banging against them. The stuck horn of a buried car was blaring. The family in the darkness in their fixed tableau watched one another by the light of a directional signal, endlessly blinking. The house had filled up in six minutes, and the mud stopped rising near the children’s chins.”

Note that these flows don’t happen only when it’s still raining. Here’s one that happened along the Hayward Fault, in Fremont, that I remember watching from across the South Bay when we lived in Emerald Hills, California, in the late Nineties. It moved slowly and didn’t take out any houses; but it almost did, and was dramatic to watch. It wasn’t raining at the time. The mountainside was saturated with water from earlier rains, and chose its own time to give.

In terms of Geology, California is new. If you were to run a short video of the last few hundred thousand years in Southern California, you’d see a riot of mountains forming, sliding sideways and collapsing. If you were to do the same for the mountains of Arkansas or North Carolina, you’d see almost nothing happening.

Living anywhere is a game of russian roulette with nature: a bet that grand geologic or weather events will not occur within our brief lifespans. In communities like La Conchita, and others placed below dirt sure to move, there are many more bullets in the chambers.

But denial is a powerful force. When I first moved to Santa Barbara, and drove past La Conchita on Highway 1, I was astounded that anybody would chance to build there, because big landslides had obviously happened already, and more were sure to come. Since the mudslide of 2005, many people continue to live in La Conchita, and insist that the county “fix” the mountain above them — even though geologists have studied the region closely and said this:

The 1995 and 2005 landslides in the 200-m high sea cliff above the community of La Conchita, California, are known to be part of a reactivated Holocene prehistoric landslide. We propose that the prehistoric Holocene slide is part of a much larger, several hundred million cubic meter late Pleistocene slide complex composed of upper slumps and lower flows, informally termed as the Rincon Mountain megaslide.

On the positive side, rain on SoCal’s low elevations in winter means snow on the high peaks. If the air clears, Los Angeles will be flanked by white alps. I guarantee great skiing on Mt. Baldy when this thing is over. Provided there isn’t a debris flow blocking the road going up there.

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On not skiing

Shows here in EdHat that there’s snow on Mount Baldy. That means there’s skiing in Los Angeles. Or close enough. Mt. Baldy is the highest point in the San Gabriel Mountains, which overlook Los Angeles from the North. Imagine a 10,064 mountain on Staten Island and you get the picture.

Skiing on Mt. Baldy is a trip. Mainly, a short one. Ignoring traffic (which you can do if you leave early enough), you can be there in under an hour from most of the L.A. basin. On a clear day you can see it from nearly anywhere there too. Its the big snow-capped one.

Here’s a photo set that gathers a few of my shots of Baldy, both from the ground and from airplanes.

And here’s a post I put up after a day of not-very-good skiing there. The snow wasn’t too bad, considering. The main problem was rookie snowboarders who crashed into the kid and I when they weren’t sitting on their butts like a bunch of traffic cones. From that post…

Rules for snowboarding on Mt. Baldy:

1. Fall on your ass.
2. Sit on your ass, for as long as possible.
3. Wait for your friends to come and fall on their asses next to your ass.
4. Sit on your ass with your friends on their asses, for as long as possilbe.
5. Do all this in the middle of a trail. The narrower the trail, the better.
6. If possible, fall on your ass in the path of somebody else.
7. Have no skills. Other than falling on your ass.
8. When actually snowboarding, run into people.
9. When running into people, fall on your ass again.
10. Bonus: get the people you run into to fall on their asses too.

Anyway, the kid is skiing this weekend in the Sierras somewhere, while I work in Atlanta. That’ll be fun too, but not quite the same.

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