Tumalo Falls, Oregon

A recent photo of Tumalo Falls near Bend, Oregon, relayed back to the Lazy J by a lady friend living in the area.

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Stapelia Bloom

The miniature Stapelia variegata (aka carrion or starfish flower) growing in my backyard is throwing off flowers. It’s a relatively common succulent plant and flowers freely and so it’s not a rare phenomenon to see it bloom, but it’s exotic looking, and smelly. These flowers are much smaller than those of the plate-sized Stapelia gigantea and are only about two inches in diameter. But they seem to have a stronger scent than the gigantea, both of which reek of rotting flesh and attract flies.

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Haddock Peak Descent to Sespe Creek via Potrero John Creek

Pacific marine layer filling Matilija Creek watershed at sunrise, as seen on the drive to the trailhead. (Sunset marine layer view from same location 2010)

A rough outline of the route hiked down the Potrero John Creek watershed from Haddock Mountain.

There is no trail and we had no knowledge of other people having done it. We had no idea what to expect. Is it possible to descend Haddock Mountain into the Potrero John Creek watershed and make it to Sespe Creek with a only a pair of boots and trekking poles, no ropes, harnesses or other such mountaineering gear?

Stillman thought it worth a try (DavidStillman.blogspot.com). I agreed. Sometimes strolling along the well-beaten path of local trails becomes too routine and of too little consequence. It amounts more to glorified walking rather than hiking. This venture, on the other hand, promised to bring us to the borderline separating hiking and canyoneering.

Stillman en route to Haddock Peak crossing through the long shadows of early morning.

Mountaintop view prior to the descent.

Reaching the west end of Haddock Mountain, we left the official U.S. Forest Service trail, walked up a few yards across the bare soil of the ridgeline and dropped into the canyon. We began the slow and deliberate switchback zigzaggery necessary to avoid slipping off our feet while descending the steep slope covered in loose rocks.

Picking our way through the talus, Stillman leading, while I tried to avoid kicking boulders on his head, we quickly reached a section requiring a few minutes of thoughtful analysis to determine the most effective route.

Stillman disappeared around a small protrusion of weathered, gritty bedrock and, emerging on its east side, advised me on a route between a wiry manzanita bush growing up against the sandstone mass he was working his way around from below. I trust it looked far better from his perspective, because from my view above I wanted nothing to do with it. I found a way down a few yards to the east. We continued down through the stone rubble field, and were soon funneled into a bedrock throat between towering formations covered in neon green lichen, which can be seen thousands of feet below from Highway 33.

This upper section wasn’t hairy, but I’m not sure that the photos accurately convey the steepness of the slope. I would sum it up as enough to raise my heartbeat in at least one place, for sure, perhaps more, but good fun nonetheless. If you’re an experienced climber or mountaineer then it rates as easy.

Stillman making simple work of an easy section along our initial descent.

Getting steeper and rockier, but still relatively easy going.

Looking back up through the throat-like break between the bedrock outcrops.

The characteristic green lichen covered crags of Haddock Peak.

At a certain place a point is crossed and there is no going back. Or at the very least you really, really hope you aren’t forced to attempt a return due to unfavorable geography which makes continuing impossible. It’s a point at which commitment to the end goal, the bottom of the canyon thousands of feet below, is resolutely affirmed and accepted once and for all as unalterable fact, because the difficulty of returning up slope is unthinkable.

And so you slip, slide and scramble your way down the barren mountain and over the weathered sandstone outcrops clinging precariously to tree stumps and branches and what little stability there exists on the side of a crumbly, ragged and highly eroded 7400′ mountain.

The body is burdened with the physical strain of resisting gravity when lowering oneself down walls of bedrock and trying to maintain traction while walking down steep slopes covered in loose rocks and sand. The mind is burdened with the intense concentration necessary to cross sketchy sections that threaten great bodily harm or death, and when that wanes, it’s nagged with a lingering thought: Will we be able to make it to the bottom where the car is parked or will we come up on a sheer rock face that is impassible? And if so then what? Will we have to bushwhack up steep sun-blasted hillsides of dense chaparral and if so for how long? Or will be forced to return the way we came and some how pull ourselves up out of the notch of the canyon and claw our way up the unstable crumbly slope for several thousand feet?

The lay of the land is deceptively flat looking in this photo, which shows the same craggy peaks from a distance as are shown closer up in the previous image.

Pertinacity

We sat for a few minutes resting in the cool, shady creek bed listening to the sound of trickling spring water and discussing the nature of the route we had thus far taken. My head heated from the effort, a slight headache coming on, I swept chilly creek water over my face, forehead and hair. I swallowed some Advil with plenty of water and got some food down, and felt refreshed and ready to ramble.

It had been, for the most part, relatively easy going. Steep? Yes. Requiring decent physical effort? Certainly. A few sections where a slip or fall could have meant possibly serious consequences? Absolutely. But, based on the nature of the mountain, it was nothing too bad. I was feeling very good about it all. And we made mention of it; how smoothly the day was playing out.

Then within probably like fifty yards or less after resuming our hike, as if the mountain was mocking us in response to our discussion a few minutes before, we came across the first real obstacle. It was precisely what I had been concerned about; a substantial waterfall impossible to descend and with no apparent route around it upon first glance. This sucker was tall and hemmed in by steep rocky cliffs and crags on either side. And at this point we were deep into our hike. Returning back to the top of the peak would have been ass-kickingly miserable! We had to locate a route by which to continue down canyon.

Stillman peeking over the precipice of the waterfall.

Stillman decided to chart a course to the east, to his left in the above photo, through some pine trees and up a very steep slope of exposed knobby bedrock. I didn’t like this one bit. It was pushing my limits, which I made known when asked, but still, I reasoned and felt mentally, very much doable for me. My heart beat picked up and beads of sweat began percolating above my brow. But after a few minutes I felt calmer as I acclimated to the situation. At one point I asked myself why I drag my body into these situations, rather than staying in town in perfect safety lounging around on the sofa surrounded by the comfort and convenience of home.

Unlike Stillman, I’m not a rock climber, and have no mountaineering experience. I was really hoping not to be the weak link in this situation, as we picked our way up the bedrock blanketed with pockets of pine needles and sandy dirt, kicking loose small boulders along the way, which bounced down the crag and plummeted over the edge of the cliff. The loose rocks slammed into the stone lined canyon out of sight far below us. The hammering sound resonated through the high mountain air with an unsettling emphasis that made it plainly evident, should one of us slip and fall, we’d be lucky to end up in the hospital, but perhaps more likely to end up in the morgue.

Stillman removed his pack and set his trekking poles aside and proceeded to climb up a pine tree jutting out of the rock, and then, trying another course, began a scramble up a flat slope of stone. I sat in nervous amusement watching him make it look carefree and easy. After starting to look at a third option, he called it off.

We hiked a short distance back up the creek and then found an open route up a slope of deep gravel. Leaving the slope of loose rocks we penetrated through a section of heavy brush, our only bushwhacking of the day, and popped out atop a ridgeline overlooking a huge section of scree.

After the previous aborted attempt up the sketchy rock section the steep pebbly slope looked inviting. But rather than being covered in a thick layer of gravel into which we could sink our feet and gain traction, it was essentially a sheet of rock covered in ball bearings. We slid slowly down it on our butts digging our heals into what little loose rock existed and in some places skidding the soles of our boots on bare rock, while bracing against out trekking poles, and trying as best we could to not break into an unstoppable free slide. It wasn’t easy to keep from breaking free. By about halfway down I was wondering just how far up my rear my pants were going to be shoved.

I busted the top off one of my poles and ripped one pocket off the butt of my nylon pants and Stillman scratched up his leg pretty good. There were two trees on the slope, the second one rooted just above a short ledge of a few feet and we both used it to break our slide. Stillman broke loose several yards above and to the side of tree and skillfully snatched its trunk with one hand as he slid by. I was a little more squarely line up to the tree, and as I came sliding toward it a bit faster than planned, I was able to stop myself by jamming my foot straight against the trunk. From that point we were able to walk-slide down the remainder of the slope which had a far deeper coverage of gravel.

First try at the scree section. We next walked along the top of it beside the bushes above and entered higher up and to the far side of the photo.

The entry.

Butt sliding down the slope.

The scree slide allowing our return to the creek, the toughest part of the hike was then behind us. Boulder hoping on down the canyon, with several short detours out of the creek bed to get around waterfalls, we made swift time at a leisurely pace. We came across a long line of black half-inch irrigation tubing some boneheaded guerrilla marijuana farmer had run down the creek bed in plain sight. The irrigation line seemed to go on forever running over boulders, across open soil and drooping along the sheer bedrock faces lining the creek’s edge. For as much work was required to haul the heavy spool of plastic tubing up the far reaches of the canyon, and then unroll it back down the creek, there was no effort to conceal it. It was a pretty pathetic looking operation.

We made our way down numerous unnamed good-sized, respectable waterfalls or cascades before arriving at the largest one, Potrero John Falls. Potrero John Falls was the last obstacle to get around and once we were there I finally breathed a sigh of relief; there was no longer any question that we had made it down the canyon; there was no longer the possibility that we would walk up to a sheer rock face we couldn’t get down or around. The rest of the route then followed the frequently traveled trail down to Potrero John Camp and then the well-beaten US Forest Service trail down to Highway 33. The descent was done.

Breaking into the more open reaches of Potrero John Creek.

Stillman standing on top of Potrero John Falls.

Looking up over a smaller waterfall and at the top of Potrero John Falls barely visible below the blue sky.

Looking up at our route down Haddock Mountain as seen from lower Potrero John Creek.

A log jam in lower Potrero John Creek showing the high level of water and tremendous force that rips through the canyon during heavy winter rains. The wood was jumbled up in a dry channel, while the creek was flowing a short distance away.

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Solitude on a Busy Day, Matilija Wilderness

The canyon mouth of Upper North Fork Matilija Creek.

“I shall be telling this with a sigh
Somewhere ages and ages hence:
Two roads diverged in a wood and I—
I took the one less traveled by,
And that has made all the difference.”

—Robert Frost, The Road Not Taken

I am suspicious of consensus and despise group mentality. I don’t go with the flow, I swim upstream. The surest way not to convince me of something is to tell me that everybody else is doing it, or believes it or the like. I shy away from crowds and I dislike seeing footprints on the trail. I cringe when I pull up to a trailhead and the parking lot is full of cars. It’s not hatred of people, but preference for solitude.

That is the whole point for me in getting out into the forest, to escape the masses. To this end I prefer hiking during the week. If I go somewhere particularly popular on a weekend I usually do so on a cloudy, cold or rainy day when most people avoid the area.

And yet in early May, a weekend of all days, a blue-skied warm Sunday, I was headed into the Matilija Wilderness on a day that guaranteed a crowd and everything I prefer to avoid. I knew before getting there, by way of the exceptional weekend weather, that a mob of people had descended upon the creek. Arriving at the trailhead parking lot my presumption was confirmed. The lot was stacked with vehicles.

Coming to the fork in the trail I took the path less traveled. Less traveled because it lacks the exceptional waterfalls and swimming holes found along the other route. But that didn’t bother me. I wouldn’t enjoy hanging out at a waterfall with a noisy pack of people there anyway. If I was with friends, then yeah, I’d have fun and a crowd wouldn’t matter, but not on this day. I was out alone and after something different.

Of course, as for the two trails, “the passing there/Had worn them really about the same.” If it was less traveled my choice of paths didn’t show it. I merely figured that the vast majority of people that day had headed toward the waterfalls and swimming holes and that the other branch of the canyon, the one I was headed up, would be relatively vacant by comparison. I was not disappointed.

“Growing up [in Santa Barbara], I lived in a house that had a fairly big backyard and a creek across the street. It was when I was by myself that the environment meant most to me. … Being in nature can be a way to escape without fully leaving the world.”

—Lauren Haring, as quoted in Last Child in the Woods by Richard Louv

Related Posts:

Upper North Fork Matilija Double Waterfall

Upper North Fork Matilija Tributary Cascade

Matilija Creek Waterfalls

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Edgar B. Davison’s Cabin (circa 1900)

Edgar B. Davison’s Fir Canyon cabin, Figueroa Mountain, Santa Barbara County. (Courtesy Bryan Conant, by way of a friend.)

“Edgar was a forest ranger on Figueroa Mountain from 1898 through 1912, making $75 a month. Grace and Edgar built a cabin in remote Fir Canyon, in what is now the Los Padres National Forest, and lived there for the early years of their marriage. If they were separated, grandson Don Davison related, at sundown Edgar would signal from his lofty Figueroa perch with a mirror to Grace in Ballard, flashing an all’s well. “

William Etling, Sideways in Neverland: Life in the Santa Ynez Valley, California (2005)

Edgar B. Davison

Edgar B. Davison was active in civil society and described himself as being “proud of California, and a deep-dyed optimist as concerns her future.” He was a proactive citizen that helped build the state into what it is today. The son of pioneers, he was in many ways a pioneer himself as an early resident of Ballard in the Santa Ynez Valley.

Describing the tiny community as she first saw it in 1882 when brought there by her parents, Davison’s wife Grace wrote, “Ballard was a mere handful of houses, with a school, but as yet without a school house.”

Edgar B. Davison helped build the town church and school and worked as the first manager of Ballard’s Oak Hill Cemetery, which was founded in 1883, and within which today still grow several towering redwood trees he planted.

In 1894, concerned about a drought, Davison wrote a letter to the Los Angeles Herald asking the editor for clarification about the “possibilities of causing rain by artificial means.” His question was published in addition to a lengthy reply informing him in conclusion: “When the conditions are favorable for rain, explosives and fires may precipitate rain, but when the air is too dry no artificial means can cause rain to fall.” The editor went on to warn people of being “duped” should they “contract or subscribe to any rain making agents for the production of rain.”

Davison participated in party politics and in 1898 was elected a delegate in the Republican county congressional convention. The next year the San Francisco Call published a letter he wrote commending the newspaper for its “bold and fearless fight” against political corruption in California. In 1911, President Taft appointed him postmaster of Ballard.

Memorial plaque at Oak Hill Cemetery.

Aside from his work within the Ballard community, one of his more enduring legacies enjoyed by countless outdoor enthusiasts and hikers through the decades was the protection of a mountain reserve that eventually became part of the Los Padres National Forest, as well as the building of Davy Brown Trail.

Davison created the Davy Brown Trail between 1898 and 1899. The three mile path leads down the backside of Figueroa Mountain (4528′) to Sunset Valley and what today is Davy Brown Campground (2095′).

During the same period of time around the turn of the century, Davison was actively involved in laying the groundwork for what would become the Zaca Lake Forest Reserve, which eventually became incorporated into what today is known as the Los Padres National Forest.

On September 12, 1898, the San Francisco Call noted Davison’s leading role in the creation of the Zaca Lake portion of the Pine Mountain and Zaca Lake Forest Reserve:

“. . .Edgar B. Davison of Ballard, to whom is due, through his exponency of the idea in the newspapers, the setting apart of Pine Mountain Reservation by the government, . . .”

On September 25, 1898, the Los Angeles Herald offered readers an illustrated feature story about the new forest reserve, which praised Davison for his conservation work.

Originally Edgar B. Davison, H. H. Doyle (the present county clerk of Santa Barbara county), Henry Robinson (editor of the Santa Ynez Argus), Mrs. Flora Haines Loughead and others suggested to Congressman McLachlan that Zaca lake and a few sections adjacent be set aside as a government reservation. …

Mr. Davison’s articles in the country press had great influence in forming public opinion to be ready to support the petition. …

Edgar B. Davison, who has done as much as anyone else to procure the reserve for Californians, is a young man, a resident of Ballard, near the reserve. He is 29 years old, and has lived near or on the tract for fifteen years past. Pleasing to state is the fact that his zealous efforts to secure the state a splendid reserve have not been unrecognized at headquarters. Mr. Davison is now one of Commissioner Crawshaw’s assistants, and has his headquarters in Brown’s cabin, on the Little Manzana.

Davison became one of the first forest rangers serving in Santa Barbara County. He used the Fir Canyon cabin on Davy Brown Creek as a station for his duties, as well as using the cabin built by C.E. Munch in what today is known as Munch Canyon for his winter headquarters. Neither structure still exists. Today, along the Davy Brown Trail, a plaque notes the location of the old Davison cabin.

The Edgar B. Davison cabin site in 2012. The above shown green plaque can barely be seen in the shadows just below center frame and to the left of the thin trunk of the tree.

The “X” marks the location of the old Edgar B. Davison cabin.

Reference:

William Etling, Sideways in Neverland : Life in the Santa Ynez Valley, California (2005)

E.R. Blakley, Historical Overview of Los Padres National Forest (1985)

Grace L. Davison, Beans for Breakfast (1956)

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