Showing posts with label 1998. Show all posts
Showing posts with label 1998. Show all posts

March 23 (1988, 1998, 2001, 2005)
Up Close and Far Away

“3/23/88  Sunset; just returned from a delightful day with Kelly, wherein we skied to all three of the Loch Leven Lakes, above Big Bend, and made a telemark descent through wide open slopes…”

[Russell Towle's journal]


“3/23/98    […] A dreadful house has been built on Lovers Leap Road after clear-cutting the forest, a single-fingered salute to the world and all posterity. Highly visible from Casa Loma and Iron Point.

Davey Jones and Dave Lawler were up a few days ago; we are making a detailed geo map of the petrified wood area. Mystery of the missing deep gravels.”

[Russell Towle's journal]


Date: Fri, 23 Mar 2001 19:00:05 -0800
To: Karen Callahan
From: Russell TowleView
Subject: Canyon Creek flowers

X-Attachments: :Macintosh HD:371829:BRODIAEA.JPG: :Macintosh HD:371829:BUCKBRUSH2.JPG: :Macintosh HD:371829:CUCUMBER2.JPG: :Macintosh HD:371829:POPPY.JPG: :Macintosh HD:371829:SAXIFRAGE.JPG: :Macintosh HD:371829:TOMENTOSE.JPG:


Hi Karen,

Here are photos of some of the flowers we saw today. ...


Cheers,
Russell Towle


Return to East Knoll & Sugarloaf Falls
[Photos taken March 23, 2005]





January 13 (1979, 1980, 1998, 2005, 2006)
Indian Knife ~ The Wild Mouse Igloo ~ Featherfall over Canyon Creek

“1/13/79   morning? grey sky, somber tones in the canyon. a fire in the stove... yesterday [...] two golden eagles came up and circled about ~ joy.  [...] ”

Russell Towle's journal


“1/13/80 rain, rain, rain ~ over ten inches in the past four days. the storms turned warm. [...]

4.60 inches of rain in the gauge yesterday morning. [...] spent the day at iron point & casa loma with steve r. & ron. violent winds, river in flood, waterfalls everywhere, speeding fogs and hawks whirled like leaves ~ then the knife, on the bank above the road. at first, because it was shaped so much like a bowie knife blade, i assumed it was, and that it was a very corroded, old, steel blade. when I cleaned off some of the mud I saw that it was of Indian make, possibly very old, and in good condition save for a fragment missing from one corner. it is a grey slate with an incipient cleavage right down the middle of the flat edge.”


Russell Towle's journal


“1/13/98

Rain rain rain rain, but today a little sun, tonight, more rain. [...]

Dave Lawler and I are going to file claims on the BLM ground out by the petrified forest. There is a father-son team, [names], who have been filing lots of claims on BLM land around Dutch Flat and Gold Run. We want to lock up the petrified wood parcels before [one of those names] claims them. [He] is my prime suspect in the recent thefts of large pieces of petrified wood from Dutch Flat and Gold Run."

Russell Towle's journal


Visit to Canyon Creek
[North Fork Trails blogpost, January 13, 2005:
http://northforktrails.blogspot.com/2005/01/visit-to-canyon-creek_13.html ]
Happy New Year!

Sunrise, January 13, 2006
There's been a ton of snow around these parts, and scarcely an ounce of hiking. The last fair weather in December found me visiting Green Valley with friends, and packing out the last of the garbage gathered up from an old marijuana grower's camp last winter.

Then came the storms. Snow and then rain, snow and then rain. Heroics of shoveling snow. The building of igloos and arches and sculptures only to see them melt in the rain. The shoveling of hundreds of feet of driveway only to see it buried all over again. There came a final snow storm, with no rain afterward, a final igloo was built, with the visage of a wild and mighty mouse glaring from one corner (my igloos can have sharp corners, spires, windows of any shape, buttresses, and so on, including, perhaps, the hundred-times-life-size bust of a mouse).

The Wild Mouse Igloo
And then there was at last one sunny day. Wednesday. So the intrepid Catherine O'Riley and I dared to hike through the snow into Canyon Creek and wander a mile or so down the old trail.

The Diggings were only lightly frosted with snow, and dotted with crystalline icy puddles, and walking the Paleobotanist Trail, we saw many interesting ice patterns, as we crunched along. Snow almost obliterated by rain had frozen hard under the stars, Tuesday night. Reaching the Canyon Creek Trail, we soon dropped below the snow, and continued quickly down past the little bridge to the sunny side of things, where first big waterfall comes into view, The Leaper almost hidden beside it.

The Leaper needs middling high water to even exist. Water surges into a narrow polished channel which plunges over the top of a cliff. The channel leads into a shallow pothole which makes the water shoot out and up with great force. It sails across a narrow chasm and hits another cliff before falling to a deep pool at the base.

Yesterday The Leaper was in good form.

We decided to visit the Blasted Digger Overlook, and took the side trail from Waterfall View. Arriving at the spur ridge dividing Canyon Creek from the North Fork, we followed down the ridge, which narrows to a single sharp blade of rock, and suddenly one is at this ancient lightning-struck Digger Pine, and Giant Gap is in view, and the river, and in fact, one can look far upstream and far downstream.

View to the east through Giant Gap, from the “Blasted Digger Overlook” above the Canyon Creek Trail
Gazing through the Gap, two snow peaks floated like clouds above distant dark forests. These were Monumental Ridge and Quartz Mountain. Rarely are they so white.

We explored some other viewpoints, cliffy spots where the sun beat hard on bare rock and a glorious warmth and light embraced us. This is California in the winter. One day after a snowstorm, and even at 2600' elevation, one gets a tan, or looks for shadows to hide in.

A bird appeared in Giant Gap, with small white things dropping away from it. After a moment, we realized these were feathers. It took a while to grasp what was going on. The feather-dropping bird flapped vigorously east, a thousand feet above the river, and behind it five, ten, twenty, who knows, fifty little feathers sparkled downward in the sun, easily seen against the shadowed cliffs of the far canyon wall.

Gorge Point
Suddenly a second bird, much like a hawk, shot out from the side of the canyon and chased the first bird out of view, in the vicinity of Big West Spur. We realized that the first bird had been attacked just before we'd seen it, and had probably just been attacked again.

Retreating to the main trail, we walked on down in the sunshine, to the Inner Gorge and Gorge Point and the Six-Inch Trail. The rock doves or pigeons were circling about, perhaps fifteen in all, and I counted nine pure white. A couple of Brewer's Rock Cress were in bloom at Gorge Point, which is second only to The Terraces in priority of bloom.
 
Brewer's Rock Cress
(Arabis breweri)
We'd had a late start and while lazing around down there next to those wild cliffs and chasms and waterfalls, the sun slowly lowered toward Diving Board Ridge, to the west. The faintest hint of the ridge's blurred shadow-edge touched us, and that was all it took, we were on the trail immediately, slogging back up to the Diggings, and crunching across the snow and ice.

It was another great day in the North Fork.



Looking east from Moody Ridge, January 13, 2006


April 12 (1977, 1986, 1988, 1998, 2003, 2006)
Aspiring to Loaferhood, on the SHOUT
(Super-High Old Upriver Trail)

4/12/77... i heard a grosbeak sing this afternoon...

[Russell Towle's journal]


April 12, 1986: A cold and blustery morning, after days of sun, wearing cut-offs. prospecting a little with and without Alex ...

To bed early, and early to rise, this morning up before six, off to the meadow to gather pine cones for kindling, the meadow where of late a few deerbrush stumps have been burnt. ...

Looked up from face-fitting [assembling the faces of a geometrical model] to see a powerful lot of sleet falling, so went out and tried to get the Toyota up to the meadow before it was too late, but, it was too late. So gave up and fitted another face.

[Russell Towle's journal]


4/12/88 Morning, sunny, cooler, but balmy, hazy, dogwoods nearing full bloom, ferns sprouting skyward, a third cup of coffee in the making.

[Russell Towle's journal]


April 12, 1998

A snowy morning. This spring has been a stormy one, as was the winter, although these spring storms have been quite mild affairs, cold, often snow, but very light amounts. However, they are spaced close enough together that a sunny day is a rarity. Neil and I have been planning a Canyon Creek hike for over a month now, and have been rained out every Wednesday (his day off).

My big pool project at the gully below the middle spring has also provided lots of work. I have dug out tons and tons of soil, exposing a bank of rhyolite ash about twenty feet long and ten feet high. It is tempting to extend the bank laterally a few feet to either end but more tons of soil would be involved, and I am sick of digging. The basic idea is to build a dam and impound a small pond about sixteen feet across, and roughly circular, and about six to eight feet deep. A lot of masonry work. Also, the idea is to carve away the weak volcanic ash at the base of the bank to make for a vertical, not sloping face.

[Russell Towle's journal]


Date: Sat, 12 Apr 2003 10:18:14 -0800
To: NFT
From: Russell Towle
Subject: Bear on the SHOUT

Hi all,

Tom McGuire tells me that Thoreau wrote, "If a man walks in the woods for love of them half of each day, he is in danger of being regarded as a loafer. But if he spends his days as a speculator, shearing off those woods and making the earth bald before her time, he is deemed an industrious and enterprising citizen."

Aspiring to loaferhood, Ron Gould and I essayed a reconnaissance of the SHOUT (the Super-High Old Upriver Trail) on Friday. We met at the Dutch Flat exit on I-80, snuck into the Gold Run Diggings, and hied on down the Canyon Creek Trail with scarcely a pause to admire the wondrous array of flowers. The day was cloudy and cool, tho a strip of bright sky to the west suggested that a clearing would soon approach.


Striking east on the HOUT, we at last reached the Realm of Uncertainty. Here the HOUT splits into multiple trail threads, and as one follows any one, some other thread may be glimpsed above or below, and one worries, which is the "right" trail? The thread which drops to the river just west of Big West Spur is least obstructed by brush, and most used by people over recent decades, but Ron and I were interested in holding a higher line, since there is every reason to believe that the SHOUT is really the continuation of the HOUT. We chose a trail-thread which soon enough split into smaller threads, and Ron stayed on the high road, while I took the lower. With the very loud roar of the river below, we were soon out of voice contact, but struck Big West Gully about the same time, and regrouped on the east side of the gully, on the steep slopes of Big West Spur.


The clouds had lowered, and the canyon rim, two thousand feet above us, was hidden in fog. After a short rest which brought on a chill to our sweaty bodies, we contoured along, and soon spotted a trail just above. Climbing to it, I was sure it was the SHOUT, the part I had failed to find on Wednesday. We followed it back towards Big West Gully and were pleased to find that it matched up well with Ron's higher line. Then we turned back and made for the heart of Giant Gap.

The secret of the SHOUT is well-protected. Anyone with sufficient determination can find it, but to follow it along the west side of Big West Spur is difficult. We passed a nice bear bed, set into the center of a cluster of Canyon Live Oak trunks, right on the trail, and marked in the usual way bears mark their beds, with large piles of poop a few feet away. Other such piles were along the line of the SHOUT, so we saw that this fine old trail is no secret to the bears.

At a couple places the SHOUT disappears beneath an active talus slide, or is as well as obliterated by some mass of gnarled bushes and poison oak. We were always able to regain it easily enough, and were impressed with its width and integrity, after perhaps 140 years of disuse. Many are the places where dry-laid stone walls bolster the SHOUT and allow it to hold an almost level course, there on the west side of Big West Spur.

Turning the corner around the first main sub-spur of Big West Spur, Lovers Leap and the Pinnacle Ridge were suddenly in view, tho shrouded with fog along their summits. A hint of rain fell from time to time. The light was flat and scattered and worked to soften and disguise the intricate architectures of Giant Gap's cliffs.

Looking east up the canyon, the lavender line shows the easternmost part of the SHOUT I reached,
where it switched back and started a steep climb to pass more cliffs. The white arrow points to
Lovers Leap Ravine's thread of white water. The Lovers Leap cliffs base is in the background;
the base of the opposite Pinnacles Ridge descends to the river on the right.
Soon enough we reached the most eastern part of the SHOUT I had explored, and began scouting for its continuation. Again, Ron took the high road, and again Ron was right. After a time I was forced to leave my lower line and climb steep cliffs to reach his level, where, lo and behold, broad and rock-walled, the SHOUT continued east. For a time, we could look right through Giant Gap into Green Valley, and see the oldest intact patch of Pleistocene glacial outwash sediments, near the Hayden Hill Mine, with its tell-tale grove of Kellogg's Black Oak. We could also see a part of the Sawtooth Ridge, east of Euchre Bar.

It is true that here the SHOUT begins to compromise more freely with the incredibly steep and cliffy terrain; at one point we had to make a short descent, of perhaps eight or ten feet, over nearly vertical rock, to hold the line of the SHOUT. Soon we reached and crossed Lovers Leap Ravine, to another of the fine, fine viewpoints along the SHOUT.

Resting here for a good long while, we were pleased when a glimmer of sunshine spread across the cliffs of Giant Gap. It is really quite remarkable to be able to enter the very heart of Giant Gap at this time of year, without having to use a kayak or raft, and without having to do much real rock-climbing. We were directly opposite the very base and axis of the Pinnacle Ridge. No eagles were seen, but a Redtail Hawk made a visit.
So far as an eastward continuation of the SHOUT, we could see nothing; however, since if it does exist, it simply must follow a certain sequence of Canyon Live Oak groves along the cliffs, where it would be hidden from our gaze, we could by no means rule out its continuation.

During our retreat west, we were able to clear up several uncertainties as to the exact course of the SHOUT. We were eager to connect the SHOUT from the Bear Bed, across Big West Gully, to the HOUT, but, although at first we met with success, soon enough we were confronted again with multiple alternatives, and, I think, lost the true line of the high trail.

Looking down the canyon from that easternmost part of the SHOUT (Super-High Old Upriver Trail) that we reached; the lavender line shows our route.
It is a long hike out the HOUT and then up the steep steep Canyon Creek Trail. We reached Ron's truck at 6:30, and were very well pleased with the day's explorations, tho also very tired and sore.

Cheers,

Russell Towle


A rendering of the N. Fk. American watershed landscape, viewed S to N, created
from digital
elevation map data using the 3D rendering software POVray.

April 12, 2006, by Russell Towle. Click to enlarge.

Foxholm, and Mike Case's Letter
[North Fork Trails blogpost, April 12, 2006:
http://northforktrails.blogspot.com/2006/04/foxholm-and-mike-cases-letter.html ]
Yesterday, scouting for sound, dead maple trunks to cut for firewood (the tight grain of the Bigleaf Maple keeps the wood amazingly dry, even after constant storms), on a steep hillside in the rain (it has rained or snowed continuously since March 1st, and my family has consumed a ton or five of firewood more than usual), I was staggering along beneath an ancient Kellogg's Black Oak, five feet in diameter but only twenty feet tall, broken down in storms decades ago, and almost, almost, but not quite, dead. I have often admired this recondite monster, with its giant burls. I noticed, yesterday, that a bear had been by recently, and clawed loose bark away from one of the burls. Climbing around and above the tree, I was passing it on a faint game trail when a plump grey fox suddenly jumped down from about ten feet above ground level and raced away. I suppose it has its den inside the monstrous oak, although I could not see the entrance. For an instant, while the fox was in mid-air, it was less than six feet from me. Foxholm of the Ancient Oak.

Those who have been on this email list for a few years will recall Mike Case's interesting accounts of trips down the North Fork with his son, Jason, from Euchre Bar to Mineral Bar.

What makes their trips exceptional is that they would spend a week or ten days or more making this distance, of maybe fifteen river miles. Hence they had time to really appreciate the great canyon and the river and the strange magic and mystery which seems to overtake one, there. Well do I recall Mike's stories of the ghostly Chinese music.

Also interesting is that Mike lives in Alaska and knows wilderness like few others. He flies into the back country and hunts and fishes and camps.

Yet he loves the North Fork American River like he was born and raised here.

Here is a letter Mike wrote to Mr. Ferenback of Friends of the River:
Dear Mr. Ferenback:

My name is Michael Case and I'm writing you from Alaska. I have a great concern about the deteriorating ascetic quality of the North Fork of the American River. I will try to keep it short. Above Green Valley there are a growing number of "mansions", or homes that rich people are building right on the canyon rim. Everyone who utilizes this portion of the river cannot escape the sight of these homes perched on the rim, overlooking everything wilderness minded people do on the river. I have been down this portion of the river several times and cringe when entering this section of river now. Using field glasses one can see the people up there sitting on their fancy decks with telescopes looking down upon us, watching our every move. These houses litter the landscape of the valley, and GREATLY detract from the "Wild and Scenic" quality of the river, and the wilderness experience.

My question is, why are these people being allowed to build on the canyon rim, within plain sight of everyone using the river, when this is a "Wild and Scenic" river? I thought the reason we had Wild and Scenic rivers was so people could get away from civilization and back to pristine nature. Are people going to continue to be allowed building and trashing the view from the river? I can just imagine the conditions 30 years from now if this dreaded building isn't stopped in its tracks now - there will be literally hundreds of homes lining the canyon rim, and the river will no longer have any "Wild or Scenic" value. If this sort of thing is going to be allowed, why not open the river back up to gold dredgers, motor cycles, atv's, etc. The Wild and Scenic quality of the river is being lost anyway. I find it very infuriating that this is being allowed.

Thank you for your time.

Sincerely,

Mike Case
Thanks for that letter, Mike. I don't know what FOR can do, but they ought to do something about the vulture houses which try to impose themselves upon the great canyon, and upon all of us who love it.


October 24 (1975, 1985, 1988, 1998, 2000)
Clunk.

“10/24/75 [...] yesterday went out to canyonland and broke the chain right off the bat. i went ahead and worked on the trail, since the road is very nearly as long as it can be already—within twenty yards, anyway. a beautiful day, clear, cool, fresh snow on the peaks. not much accomplished but returned tired and sore, went to sleep early in the evening. i am tired of fighting brush.

saw porcupine damage to a young pine yesterday. large area of bark gnawed away. came upon some interesting rocks in elderberry meadow. should be nothing but volcanic mudflow boulders up there, but these were some kind of micaceous schist, probably Paleozoic in age. might have been picked up and carried along by the mudflow when it coursed down the valley of the tertiary Yuba. the bedrock beneath elderberry meadow is serpentine, probably fifty to a hundred feet down.”

[Russell Towle's journal]


“October 24, 1985

[...]  today, I was burning out deerbrush stumps, as I have for several days. This, in 1985 terms, involves digging the duff and several inches of soil away from the basal burl and however much of the root can be exposed. If the root proves too large for cutting—as most did today—then it is a "burner" and flammable materials are cleared for a foot or so on all sides. Then, boulders are carried in, and assorted rocks, to make a circle, close in to the basal burl of the ceanothus, which serves to make the fire burn hotter—it does not lose heat so readily by radiation and air mixing from the sides if confined by warm boulders. One of the boulders today exploded repeatedly, spalling off exfoliation shells from the andesite bomb. I burned about ten stumps today. I recalled that it has been ten years since I began work on Moody Ridge. Drank the rest of my zinfandel in celebration. [...] It's been a great ten years.

[...]

I climbed an oak tree in the lower meadow today that I've always wanted to climb. Snapped off many dead branches, went up perhaps forty of its seventy feet height. A good climbing tree.

Yesterday [...] rolled big boulders down a slide area below the railroad tracks. They went about a thousand feet down a steep slope, perhaps five hundred feet vertical; some were in the thousand-pound range; some exploded into a dozen pieces on the way down. It was very satisfying. There was an acute finality about the way these heavy boulders reached their resting places; after leaping and bouncing all that way, they'd reach the zone of accumulation of heavy boulders and clunk into their niche. After all that lively leaping: clunk.”

[Russell Towle's journal]


“10/24/88   Morning. [...]

A canyon wren pecks and scratches around the cabin as has been the case for weeks of this Indian Summer.

[Russell Towle's journal]


“October 24, 1998

Today I showed Frank, Michael and Luc the Sugarpine Flat area. We were rained on and snowed on and got pretty soaked and wet, but built a bonfire in the rain for a lunch break, and had a pretty good time.

I have been out to Sugarpine Flat many times this summer, with Neil Gerjuoy, Bill Newsom and Ed Stadum. And so on; and also, hiked down the Little Granite Creek trail with Dave Lawler, a couple of weeks ago, a debacle, I mean, the canyon was wonderful, we went down to Big Valley creek, checked out the little inner gorge, came back up the American River trail, and had plenty of time as we began the climb out, but Dave's legs began cramping, we had to stop for him to rest frequently and we ended up hiking out through unfamiliar terrain in the dark.”

[Russell Towle's journal]


Date: Tue, 24 Oct 2000 20:03:03 -0800
To: [...]@emigranttrailswest.org
From: Russell Towle
Subject: Truckee Trail


Hi,

I visited your website about emigrant trails, and wish to add one further branch from what you call the Truckee Trail, but which is locally, in this part of the Sierra, known as the Donner Trail. You mentioned the Nevada City and Henness Pass and Beckwourth branches. There is another; it forked from the Donner Trail at Emigrant Gap (avoiding the descent to Bear Valley, and keeping to the ridge), was used beginning in 1849, and followed the divide between the North Fork American and Bear River down through what would in later years be the towns of Alta, Dutch Flat, Gold Run, Colfax, Auburn, terminating in Sacramento. This road is called The Old Emigrant Road in newspapers of the 19th century. Dutch Flat's Main and Sacramento streets are portions of the old road. Few people know about it. It appears on one or more of the ca. 1866 GLO maps of this area, marked as Old Emigrant Road.

Its route foreshadows the later construction of the CPRR and Dutch Flat Donner Lake wagon road.

Part of its exact route was taken over by the Pacific Turnpike, a toll road from Dutch Flat to Virginia City by way of Henness Pass.


Date: Tue, 24 Oct 2000 20:23:40 -0800
To: [...]@aol.com
From: Russell Towle
Subject: Donner


Hi,

On your Donner web site you describe the snowshoe party of which Mr. Stanton was a member, and their progress west towards Sacramento. But I believe you must be mistaken about their route. I have no problem with it until they reach Emigrant Gap. But at that point you have them descending into the North Fork of the North Fork, then following Sawtooth Ridge, then descending into the bottom of the canyon, then following it down to Giant Gap, thence to Iowa Hill and on down.

It is extremely unlikely that they would have descended to and followed any portion of the North Fork of the north Fork, still less the main North Fork American. My opinion is based upon decades of hiking in the Sierra, often purposedly avoiding trails, and going cross country, and decades of exploration of the North Fork American canyon and that of the North Fork of the North Fork. To follow these streams is very very difficult. To follow them in snow is unthinkable. Especially if there were any in the party who had even a particle of good sense or woodsmanship about them. Say, an Indian. No Indian would be so utterly foolish as to use the lower (unglaciated) reaches of a Sierran canyon as a route to gain the Sacramento Valley. One would always stay on the ridgetops. Always.

It is instead very likely that the party, at Emigrant Gap, used an existing Indian trail which followed the ridgetop to the southwest through the vicinity of the Blue Canyon exit, and then on down through the vicinity of Dutch Flat. They might well have been forced off the ridgetop down into Canyon Creek—a shady little canyon where the snow lies deep—but it is so very unlikely that they would have been forced down to the main North Fork. If they followed Canyon Creek, at various points, near Alta and Gold Run, they would have been able to regain the ridgetops easily even in snow, and have obtained views down to the Sacramento Valley.

This route down the ridge from Emigrant Gap evolved into an emigrant road in its own right in 1849.

I am no expert on the Donners, but a descent to the North Fork American seems unthinkable (since the implication is that they followed along the river, a difficulty even in summer, a misery and even near impossible in the winter).

Cheers,

Russell Towle



August 24 (1976, 1998, 2003)
Big Granite Trail

“8/24/76 time flies and I don't get any richer. money worries, yuk. well. early morning in wren shack. went out to the ridge with jim rife day-before-yesterday. we carried a bunch of lumber down to the site, pulled some brush up from the road, and then went over to neil's to see about moving my piano over to raun and kathy's place. raun was at neil's, coincidentally, and after a couple of numbers it was loaded (we were loaded too) and a while later after a slow drive out to casa loma tract, it was installed in the living room of the big stone cabin. we stayed for supper and i played the piano for hours [...]

yesterday morning stopped at rick and susan's to borrow the chain, which works so well for pulling out brush. the new method is better all the way, with a short cable from truck to old tire casing, and the chain from the tire to the bush. shock absorber. hank bradley [of Coastways Ranch, Año Nuevo] turned me onto that idea.”

[Russell Towle's journal]


August 24, 1998

Monday. Yesterday Gay & Janet & Greg & I joined Frank Olrich, Michel Onewing, Luc, and Kelley, for a hike from Lost Camp down to the North Fork of the North Fork American. Luc and I continued upstream to Burnett Canyon, and visited a nice 100-foot waterfall a little ways up Burnett. Also a double waterfall on the North Fork of the North Fork itself, a little ways up from the confluence with the East Fork. Very nice. The kids did well. Janet spotted a rattlesnake in a spot we all had to cross, good eyes.

Last week we went camping up by Robinsons Flat, and hiked down to Sailor Meadow, truly wonderful first-growth forest. Also visited the X-ray mine in Sailor Canyon.

[...]

Received Green Valley photographs of Bernie & Harriet Denton, preparing to scan some of them in to Dutch Flat digital archive. Also, spoke with William Dunckhorst, whose family still has property in Green Valley.

[Russell Towle's journal]



Date: Sun, 24 Aug 2003 17:29:49 -0800
To: North Fork Trails
From: Russell Towle
Subject: The Big Granite Trail
Cc: Richard A Johnson, Gus Wiseman

Hi all,

Friday dawned amid thunder, lightning, and much rain, and the exploration of the Big Granite Trail Catherine O'Riley and I had planned seemed much in doubt. However, the weather people all agreed that this storm would pass quickly, with clear skies Friday night and warming temperatures on Saturday. So with a bit of our usual devil-may-care spirit urging us along, Catherine swung by the little cabins near Dutch Flat around eleven, and off we went. Gus Wiseman and Greg Towle rounded out the party. We hoped to find Tom and Mary McGuire at the confluence of the North Fork with Big Granite Creek. They had hiked in Wednesday from the Sailor Flat Trail.

Through masses of fog and occasional sprinkles we wound our way in from the Yuba Gap exit, past Huysink Lake and the Salmon Lake trailhead, to a pass on the crest of the ridge dividing Big Valley on the west from Little Granite Creek on the east. A TNF sign there showed Pelham Flat ahead, Huysink Lake behind, and we parked in a log landing beside the road.

The Big Granite Trail seems to have once stemmed from Cisco, on the railroad, and by way of Huysink Lake crossed that very pass where we parked, before descending to Four Horse Flat and Little Granite Creek. It crossed the North Fork at a ford and climbed Sailor Canyon to the La Trinidad Mine and Sailor Flat, up on the Foresthill Divide. So at some point, perhaps the crossing of the North Fork, its name should change to "Sailor Flat Trail."

Gradually roads penetrated this lovely part of the Placer County high country—I have a 1900-era map showing a road from Cisco up to Huysink, for instance—and then in a sustained frenzy of timber harvests and road-building many of the old trails on the area were obliterated, such as the Sugar Pine Point Trail and the Big Valley Trail. Much of this occurred about twenty years ago. There is the usual "checkerboard" pattern of even-numbered TNF sections interspersed with the odd-numbered "railroad" sections, with a few local variations.

Most all if not all of these old railroad sections had been purchased by lumber companies, most notably, Sierra Pacific Industries (SPI). This alone caused an increase in timber harvests in the area.

As Rich Johnson of the Foresthill Ranger District recounted to us the other night, at the NFARA meeting, quite a few of the old railroad sections have been purchased by TNF in recent years. I would like to see these land acquisitions continue. For instance, considering only T16N, R13E, sections 7, 17, and 9 would stand at the top of my list. And of these, how much could be said about section 9.

From our parking place in the pass, at 6600' elevation, a steep jeep trail drops to the east, bears south into section 9, and in a few hundred yards ends at a hunters' camp, where there is enough room to turn around. The only time I had ever hiked this part of the Big Granite Trail was in pitch darkness—some six years ago, perhaps—feeling my way with my feet, for the trail itself was firm and compacted, while the rich forest floor was soft. Dave Lawler and I had taken a "short cut" to the trail from Sugar Pine Point, hitting it a couple miles down. We explored the lower part of Big Granite Creek and then ventured a mile or so down the North Fork all the way to the inner gorge below Big Valley Bluff. Then, on our way back up from the river, leg cramps struck, and our pace slowed until finally the fullness of night embraced our little world of gurgling brooks and dense stands of mountain alder and occasional meadows and gigantic ancient trees. With rare and unusual luck, we found the critical fork in the trail by feel alone, and had climbed out of Four Horse Flat, to the hunters' camp, and on up the jeep trail to the road above.

Catherine, Greg, Gus and I were glad to find the foot trail itself and plunged down into a very remarkable grove of huge old Incense Cedar. A fairly light "selective harvest" had been executed, perhaps ten or fifteen years ago, but the stumps were few, and the forest giants, everywhere, running up to five and six feet in diameter, some flaring out to near ten feet in diameter at ground level. The trail actually goes through the fire-hollowed center of one ancient cedar.

As Four Horse Flat is neared the trail suddenly merges with a logging road, often clothed in brush, various species of Ceanothus and Prunus being prominent. Here and there log landings held stacks of Incense Cedar sawlogs, left behind because they were too "pecky"—for a fungus will invade the heartwood of this species, and riddle it with little patches of "rot." Then the loggers come, and one can never tell from the outside just how "pecky" any one ancient Incense Cedar will be. So, you just cut it down, and look and see. It is very very irritating to me that this area was ever logged, and then, to see this—to see that a tree likely all of 500 years old is felled just on the chance the wood is sound—it is just infuriating.

Nevertheless, for all the roads, log landings, and stacks of cull logs, the harvest here had been rather light. We have an opportunity, right now, to lobby TNF to acquire this Section 9, T16N R13E, and other sections close by. Both the Big Granite and Cherry Point trails traverse this Section 9. For an area which has been logged, this is as close to true old-growth forest as one will usually ever see. With some concerted volunteer work the cull logs and stumps could be burned, the roads maintained as trails or closed altogether, and in as little as a decade one could hike through on the Big Granite Trail and scarcely realize that any logging had ever occurred.

And this would be a good thing. A very very good thing, for, there is something quite special, quite exceptional about this trail. Or many special things. For just one, the descent, of 3,600 feet, to the North Fork, is like going from Canada to Mexico in four or five miles! You start out up in the Lodgepole Pines and Red Fir of the high montane forest, and end up among sun-blasted manzanita and Canyon Live Oaks at the river. And there are many delicate shades of changing vegetation, of ecotones and microclimates, along the old trail.

Four Horse Flat is just below 6000' and has many grassy, ferny, flowery meadows, and wet meadows all clogged with Mountain Alder. The Cherry Point Trail merges with the Big Granite Trail in this area. The logging, I guess, has forced a new intersection of the two trails, and moreover, the main trail now in use, as one continues south towards the North Fork, is on the east side of Little Granite Creek, while the true Big Granite Trail holds the west bank for half a mile before it crosses to the east side, at about 5200'.

The forest is rich with huge old trees, White Fir rather than Red Fir, some Douglas Fir, and quite a notable incidence of Incense Cedar. Where the east- and west-side trails merge, Kelloggs Black Oak begins to intermix. This is an area of sudden transition, from the shady groves of ancient conifers, to a mixed oak and coniferous forest on the steep slopes of the canyon of Little Granite Creek.

Little Granite Creek, in this area, flows through metamorphic bedrock, but one might never guess, since a million granite boulders were dragged down here by the ice from the Loch Leven Lakes area and stranded, 12,000 years ago. The creek flows over and around these giant white eggs of granite, and more eggs are embedded everywhere on the steep slopes. The underlying metamorphic rock is almost entirely masked by these glacial deposits.

Below about 5,000 feet, the forest thins and one begins to gain good views of the surrounding terrain. A particularly monstrous cliff over on Sugar Pine Point is seen again and again as one descends. Then the trail bends east towards Big Granite Creek and steepens drastically, with many switchbacks, and passes a very notable and rare old grove of monstrous Canyon Live Oaks. I doubt I've ever seen so many giant oaks in one area. One had several large trunks, and two of these trunks, each near three feet in diameter, were connected about twenty feet above the ground by an arch of living wood. I called it the Monstrosi-Tree.

Having already made a descent of over 2000 feet, these steep switchbacks began to really take their toll, with toes crammed forward in our shoes, and despite the otherwordly fog and mist which swirled throughout the canyons and cliffs around us, we were sweating. At last the trail levels and bears east to the crossing of Big Granite Creek.

We took a long rest, and I explored downstream about a quarter-mile to the confluence of Little Granite Creek, in search of some fossiliferous Triassic limestone. I found some isolated masses of limestone, delicately fluted by solution-type erosion, with myriad little ridges and channels and hollows, but no discernible fossils. Later, upon re-examining my map, I saw that I should have gone much higher into Little Granite Creek. Another time, then.

The bed of Big Granite Creek just like that of Little Granite Creek had been, at the crossing: giant rounded granite boulders everywhere. We shouldered our packs and continued down the trail towards the river. It follows a roughly level line for a time, on a southerly bearing, and soon one breaks free of the forest into glaciated barrens of metamorphic rock. Far below, within what looks to be the impassible inner gorge of Big Granite Creek—and here flowing directly over the bedrock, without any granite eggs—we could see waterfalls and deep deep pools.

Crossing the Big Southwest Spur of Snow Mountain, the North Fork itself finally was in view, and after a few switchbacks we found our side trail leading west to the confluence of Big Granite Creek. Right at the fork there is an ancient TNF sign reading "Ford" and "Sailor Flat Trail" (and possibly "Robinson Flat") with an arrow pointing left. The post stands but the sign has split and lies on the rocks. We hustled on down to the river. Tom and Mary were not in camp, but we spotted them picking their way down cliffy areas beside the waterfalls just upstream. They looked a little shocked that strangers would arrive at their camp. However, Greg zoomed up there and identified our party, and soon we were lazing around the camp and chatting. Tom and Mary were there in the depths of the great rock-bound canyon during the several thunderstorms and were almost but not quite driven into a headlong retreat.

The fog was lifting, the clouds thinning, and we struck up a cozy little fire using more or less sodden wood. Supper was a matter of roasting vegetarian hot dogs and other delicacies. We turned in around ten under starry skies. Mars so bright had risen just above the forested ridges near New York Canyon to the southeast.

I rose before dawn and built a new fire and heated water for coffee. Tom joined me and then Greg and Gus and what with coffee and cocoa and a modest little breakfast of Grape Nuts etc. hours passed. The sun struck the canyon rim and the slowly entered the canyon depths. Yet Catherine O'Riley remained snugly wrapped in her one-man tent. I took off downriver with my loppers and worked on the fine old trail, which never appears on maps. By the time I returned the sun was about blazing and everyone was stirring.

We explored west on the trail, which stays high for a quarter-mile before dropping to river level at a large gravel bar with a lovely deep pool. Here a few of us swam, the others strangely indulging in fears of how very cold the water might be. The water was cool but not bitingly cold. Some rocks rose in tiny cliffs along one side and allowed easy jumps and dives from about ten feet up.

An osprey flew over us twice while at the pool, and from the trees nearby a peeping was heard, which might have been a second osprey.

Regrouping and reclothing, we continued west on the trail, and another quarter mile or less brought us to a large sandy flat with a grove of oaks and some ancient wheelbarrows and a huge fire ring littered with garbage. A small cross had been erected where the trail reached the camp, and I have little doubt but that this had been the camp of the large Christian youth group party, of fifty kids and five or six adults, Ron Gould and Greg and I had seen on the Sailor Flat Trail in June. They need to do a much better job of picking up their trash and also in using basic sanitary practices, so that wads of toilet paper are not scattered through the area.

A little ways beyond the camp, the trail appears to ford the river. We followed it a short distance past the ford, where a line of boulders allows an easy crossing, and found the path not only indistinct but overgrown, so, the retreat was sounded, and we made the easy walk back east to Big Granite Creek.

After lunch we scrambled up the creek to an amazing pool and waterfall surrounded by cliffs with one just gigantic overhang. Some swam and some scrambled around on the water-polished metasediments of the Sierra Buttes Formation. The waterfall occupies a twisted little inner gorge, a gorge within a gorge, a spiraling slot in the cliff.

Finally it was time to leave. Around two p.m. we shouldered our packs and started up the side trail. Tom came along for a ways, since he had never been on the Big Granite Trail. We had the benefit of the warmest part of the day combined with the least possible shade as we switched back and forth up the almost bare rock of Snow Mountain Spur. A rather quick and brutal climb of 500 feet carries one across the spur and into the canyon of Big Granite Creek.

At the crossing we had a long rest, and Tom left us at a trot to get back to lovely Mary, who had stayed at the camp, alone. Then the long slog up and out really kicked into gear, if you can call a deadly slow trudge, punctuated by numerous stops, "in gear." That trail is a killer. That 3,600 feet is a terrible terrible thing. We did stop often and long and as a result reached the car at 7:20, with the shadows growing very long and the sun almost setting.

One curiosity of the ascent was a sign, reading "Big Granite Trail," the words nicely routed into a slab of wood and bolted to a tree, in the Four Horse Flat area. We had seen no sign the day before. And, following the logging road reach just above the sign, I saw a peculiar patch of trail which had been freshly dug out wider. And I saw that some of the branches I had lopped the day before had been neatly stowed off the trail; and yet no one in our party had been stowing the cut branches, that I was aware. Then, in a mud puddle, two bootprints were seen, leading up and out. So it all gave every indication that that very day, Saturday, someone had walked in and bolted up the sign and did a little trail work.

I will call the ranger station at Big Bend and ask Phil Sexton. Maybe he knows about the sign.

Such was a wonderful visit to the North Fork by way of the Big Granite Trail.

Cheers,

Russell Towle
Russell Towle on the Big Granite Trail


June 22 (1978, 1987, 1988, 1998, 2005)
Climb of Devils Peak ~ Green Valley Characters ~ Secret Canyon & IHC

“6/22/78 morning. now the days begin getting shorter; spring rolled by quickly. the morning light in giant gap is very nice. at this time of year the sun, the pinnacles, and the edge of giant gap ridge are all aligned early in the morning. at first only the pinnacles are lit, and the characteristic curve of giant gap ridge's profile is displayed along the base of their cliff. then other ribs of rock begin getting light, until now there are several lighted streaks, on a shadowed, dark background. on a couple of ridgelets, the tops of tall douglas firs are in light; a tracery of triangles marks their presence.”

[Russell Towle's journal]


“6/22/87 Morning; just awoke from the most bizarre dream, no doubt brought on by my cold… In the dream, of which I have only partial recall, I was traveling at night—was it at night?—and stopped at a ramshackle house, where a family of black people lived. I stayed there for a day; I got to know a fine young black man, very nice, tall and athletically built, but blind. We had long conversations. Walking outside the house (it was in the Midwest somewhere, in (oddly) mountainous terrain), I saw at sunset, a view down a valley/canyon towards a city: what had once been a beautiful canyon was now nearly covered with houses. I told the blind man of Lovers Leap and the North Fork canyon, of my Fears that the North Fork, which had made it into the 1980s in a virtual wilderness condition, by itself be overwhelmed by senseless civilization. My travels continued. I was in the city in Kansas, with the Nelson brothers; so strange, so foreign; inner-city: old tenements, whores leaning out windows: I saw three matching whores all with platinum blonde hair, leaning out the same window, gesticulating; one of the Nelsons led me on a walk through a maze of streets and corridors within warehouses, to visit an old woman they said was really neat; I found her utterly disgusting, and left peremptorily to find my way out of the warren alone; somehow reunited with the brothers, sat on a sunny bank and watched a black man practicing martial arts; he would throw hefty stones and chunks of concrete in the air and then kick them with expert vigor: how could his foot be so tough? Then he took a staff and twirled it around his body, a blur of motion, a spinning club. awoke to the squawking of bluejays, within old early 60s song going through my mind, Dionne Warwick possibly—I can remember the melody even now, but not the words, not the title.

Yesterday, drove over to Bill's, hoping to score some breakfast. I did find some coffee, but we were running late (Dave Black and Tim Fagan had stopped by just as I was getting ready to leave), as were Ed & Tina—we called them, but no answer, and figured they'd already left for Soda Springs, where we were to meet some friends of Ed's, Gary and Julia; Bill and I found Gary and Julia, but not Ed & Tina, a matter of crossed wires which it is not necessary to recount in detail; after 15 minutes or so, they rolled in, and we continued toward Cascade Lake, parked, and hiked in on the Palisades trail, which, at a certain point, one must leave and head out cross-country towards Devils Peak; typically, Ed and Tina did not trust my reckoning or ability, but eventually they gave in and off we went, without the benefit of a trail, something which seemed to astound everyone but me. At Devils Peak we traversed around the base of the columnar andesite cliffs, easy going but again, something extraordinary insofar as these city slickers were concerned; it was really a very beautiful day, with cumulus clouds in a slowly thinning deck, and strong winds; finding a sheltered nook in the cliffs, we paused for lunch, and then all of us but Julia continued towards the summit, and all succeeded in reaching the summit; Tina is really improving in her ability to handle rocks, while Ed, I see, struggles against an intense fear of heights; it was too windy on top to stay very long, but the view was tremendous, and we picked our way down over the easy rocks, easy, that is, for Gary and me, but for Bill and Tina and Ed a real challenge; soon we were tramping through the wildflowers on our way down to the big Mule Ears meadows at the base of the peak, where Julia awaited us. We all lazed around in the sun for a while before heading back, which again involved a certain amount of cross-country travel; we saw a marmot, and earlier, at the peak, an immature golden eagle; and when we got back to the cars, all were unanimous in proclaiming the hike a success. Bill had enlivened things considerably with the recitation of a variety of ribald limericks; he had us all in stitches while perched on the rocks eating lunch; he is truly wonderful. After a beer and some nachos at Tinker's Station, we went our various ways, and I rode back with Ed & Tina, had a beer and was paid for the weed-eating, along with an advance for further work.”

[Russell Towle's journal]


“6/22/88 Morning. To continue, [following up on the entry of June 21, 1988] well, it was a bit strange, to spend a half-hour with Steve, drunken 36-year-old martial arts expert and recreational fist-fighter, to listen to him lurch from one topic to another, every once in a while raising a hand to his poor aching head—Ow! That was a good right cross he caught me with—he was a Marine, recon, Vietnam—I was Special Forces—I'm sorry, man, I'm drunk, schizophrenic, not making any sense—but that was a good right cross, 'cept I gave him worse than I got. That's where we fought—right on your driveway, right where you saw us—for the second time—oh, I been drinkin' too much beer. I get down to the Valley, I'll be okay. My brother's been visiting me, we been mining gold, I'll tell you, I can work like a son-of-a-bitch, you never saw anybody move boulders around like me, well, not long ago, we hit a rich pocket, heavy with gold, cleanin' it out, one day, this kid, The Kid I should say, Red, there he was right in the middle of our claim, I'm gettin' tired of his shit, one of these days, one of these days, I'm goin' to turn him inside out, he's more than got it comin' and walkin' on thin ice right now I'll tell you—

Wait a minute—I say—Red? You mean that kid with the red hair, James? He thinks he owns Green Valley—

Oh? You know who I'm talkin' about? Yeah, that's him, and he's doing too much drugs, man, hard stuff, crank, crack, all the time he brings that shit down there—I'm from the 60s, right? Hey, I don't mind passin' a joint around from time to time, but that shit!

It makes you crazy.

Damn right it does. And Red, he's walkin' thin ice, I'll tell you. He ain't—I mean, excuse my English, man, I've got five years of college, I'm just drunk, and my head hurts so bad—that was a good right cross the Marine caught me with—he's good all right, but I flattened him, he knows I'm good, heck, he's always tryin' to get me to do mercenary work—

We lean against my car and smoke in the fading twilight. The guy's tall, about six-three, lean of hip and broad of shoulder, like one of Louis l'Amour's heroes, long arms and big long muscles, a powerful man. Eagle face, lank hair dark and matted with sweat, deep tan from working in the sun.

You're A POWERFUL man, I say, you get into fights with your friends, you could really hurt somebody.

He hurt me! I'll tell you that! Oh, my head…

But how can you hit somebody like that, and not break your hand. How can you hit their jaw and not break it and a bunch of bones in your hands at the same time?

Like this, man!

He raises his hands slightly above his shoulders and slowly clenches them to fists, first one, then the other. Each one makes a series of crackling sounds—you could have heard his hands clench from 20 feet away.

Like this. They don't break if you've got them like this.

Well, I don't know about any of that, me, I'm a wimp, I don't know anything.

I used to be a wimp too! Here let me show you something. You see this? You fold your fingers down, your thumb just so, no, hold your arm up like that—now the other arm—yeah, that's it. That's The Crane. Know what you use The Crane for? Well, suppose I swing on you like this—and you just make a circle up with your hand—

Followed a little lesson on how to deflect punches to the side. The Crane. Finally I realized it was getting dark, and this guy Steve had a couple of miles of trail to cover, so we parted, Steve apologizing for about the tenth time about the gate. Invited me down for martial arts lesson. Said he taught for years—I believe it. And now? Now he lives wild and free and far from the nine-to-five, mines gold, engages in the constant round of territorial disputes which seem to characterize life on the river, comes up once in a while and gets drunk, finds his Marine and has a fist-fight or two, that's Steve Williams.”

[Russell Towle's journal]


June 22, 1998

Strange that I have not written for a long while, with so much going on. I see from my last entry that Neil and I had been planning a hike into Canyon Creek waterfalls; which we at last accomplished, on April 22nd, if I recall. We had a fine sunny day for the hike, made quickly for the Indiana Hill pit, took the Indiana Hill Ditch around the corner into Canyon Creek canyon, and then scrambled down the steep wall of the canyon to the creek, where heavy brush blocked further progress along the ditch. We joined the creek just at the old trail crossing, and were barely able to make the jump across, the creek being somewhat high. We followed the Canyon Creek Trail all the way to the river, which was itself running high and wild. As we returned up the trail (there being nothing to do at the river, it being too high to explore alongside), Neil and I checked out a few of the old lateral trails leading back into Canyon Creek itself. The entire trail and its laterals were constructed to allow access to all of Canyon Creek, which was treated as an enormous sluice box, and since it received all the tailings from the Gold Run hydraulic mines, or nearly all, a lot of gold was cleaned up there. I am unsure as to just how much of the lower portion of the creek had actual wooden sluice boxes installed in it. Higher up the creek, Colonel Moody had a 3000-foot sluice box in the creek itself.

Neil and I covered a lot of ground and as always the hike out of the North Fork canyon was quite an effort. However, when we reached the crossing, where a bridge once spanned the creek, I suggested we continue up the trail to the big old Gold Run Ditch & Mining Co. tunnel, and so we did. It was my first visit to the tunnel in over ten years, maybe fifteen years. A wagon road leads down to the tunnel from the diggings. which I had explored in 1978 but found far too overgrown with manzanita etc. to make a feasible route. We decided to venture up the wagon road and see how it looked nowadays. To our surprise, it had been cleared of the worst of the brush, perhaps five or ten years ago. We easily followed it right up to the Indiana Hill Ditch. This too showed signs of having been cleared, so we headed south towards the Indiana Hill Pit, half expecting to be blocked by massive brush tangles at some point. To my delight and amazement, the ditch was cleared to within a few feet of the point at which I have over the past couple of years always stopped, because of brush. Only a few bushes disguised the continuation of the cleared portion of the ditch.

So we had a wonderful hike, and I was tremendously inspired. Suddenly, my idea of a Giant Gap Trail, connecting Garrett Road to Lovers Leap, seemed much more easily realized. I began bringing various people in to see the new route; Steve Bush, Jim Ricker, Alex Henderson, Kelly Olrich, and more recently, Eric Smith of Dutch Flat, Bill Newsom, and Dave Lawler. Later in April I led a group of about 30 people on a Nevada County Land Trust hike into the Indiana Hill pit and then over to the Petrified Wood Preserve.

I began firing off letters and phone calls to the BLM offices, talking to Deane Swickard and Jim Eicher, to Deane Decker, and trying to get them to come see the new route into Canyon Creek, and the historic Canyon Creek Trail. While down there with Jim Ricker I noticed a faint lateral leading up towards Bogus Point, as it seemed, and I have yet to explore this, but if it goes where it seems, then the trail from Garrett Road to Lovers Leap is nearly complete already, only requiring a little brush work in the main. I have not managed to get Deane Swickard or actually anyone from the Folsom office in here to see the trail this spring. Now it is summer, the creek is diminishing, and the waterfalls are less impressive. On my latest hike in, last Saturday the 20th, with Dave Lawler, we went all the way to the river and explored some of the laterals. One leads into a 100-foot waterfall which I had seen only once or twice or so before, back in the late seventies and early eighties. A marvelous spot. The main trail itself is not much more than a mile but with the laterals another mile or so of trail figures in.

Just upstream from the big tunnel, there is a tight oxbow on the creek, with a large cut through the neck of the ridge. This I take to be the terminus of Colonel Moody’s 3000-foot sluicebox. It has an interesting three-pronged, three-channeled configuration which is seemingly repeated on Canyon Creek just above where it meets the river. Undercurrents were installed at these places I am sure, but I don’t know just how it all worked.

From the hairpin curve in the wagon road just above the Oxbow, a trail leads away northwest to meet the Indiana Hill Ditch only a little ways south of Potato Ravine. This might eventually become the shortest or at least easiest way into the Canyon Creek Trail from the diggings, were the BLM ever to acquire some of the diggings from Gold Run Properties. It seems that the latter entity is selling off some at least of its land, which imparts urgency to my own quest, since some of the GRP parcels are along the line of the Giant Gap Trail. Who knows but that other of the private parcels along the line of the trail are being built on even as I write this. The Giant Gap Trail may remain only a dream, a good dream overtaken by the nightmare of development of property which should never have been developed.

[Russell Towle's journal]


Return to Secret Canyon and the Iowa Hill Canal
[North Fork Trails blogpost, June 22, 2005:
http://northforktrails.blogspot.com/2005/06/return-to-secret-canyon-and-iowa-hill.html ]
Winecup Fairyfan
(Clarkia purpurea)
On Tuesday morning I met Catherine O'Riley and geologist/paleontologist Dave Lawler at Weimar for a visit to Secret Canyon and the Iowa Hill Canal. We crossed the North Fork on Ponderosa Way, where a tremendous bloom of Clarkia purpurea, Purple Clarkia, or Winecup Fairyfan, is in progress along the old wagon road, as it drops into the canyon. These spectacular flowers have four pinkish or lavender petals grouped in a bowl, each with a purple spot. There is a ring of white anthers at the base of the corolla-bowl, and the four-parted stigma is a deep maroon.

We stopped to photograph these lovely flowers.

There are many species of Clarkia in California. They are in the Evening Primrose family. Recently I have been photographing another species, Clarkia arcuata, with a cream to white stigma, and dark blue anthers, near the head of the Green Valley Trail, on sunny serpentine slopes. This C. arcuata may be the flower I mistakenly identified as a Sidalcea near Giant Gap, about a month ago.

The road up the south wall of the canyon is rough and rocky. Eventually we won through and drove the twenty or so miles up the Foresthill Road to Ford Point, at about 5600' elevation. A deep blue sky was adorned with scattered fair-weather cumulus clouds, driven north by strong south winds. What would have been quite a warm day at lower elevations was markedly cool.

Click to enlarge
We took the same little road breaking east from the Ford Point road, a road marked 13-14-2 as I recall, into a logged area rich with green manzanita which scratched my little Subaru. Again the Subie managed to collect pine needles in its catalytic converter housing, and a delicate perfume of burning pine wafted about as we parked and gathered our packs. I looked beneath the car and reassured myself that nothing too significant was afoot; it would not do to set Tahoe National Forest afire.

The country rock is metasediments of the Shoo Fly Complex. The Complex is divided into four major thrust blocks, each containing various formations which have never yet been systematically mapped, except in this area, by David Harwood of the USGS. He identifies the rocks of Secret Canyon as belonging to the oldest thrust block of the Shoo Fly, the Lang sequence, and divides this Lang Sequence into formations such as the Big Valley Bluff fm., the Screwauger Breccia, etc.

At any rate, there are not very many exposures of the bedrock here, almost everything being covered by a glacial till which itself contains these same Lang sequence rocks, with few to no exotic rocks from outside the area. The till makes for rich soils which do a good job of storing the snowmelt and support much in the way of heavy timber, especially on the more northern exposures.

On a pure south slope near our parking spot, Ponderosa Pines grew. Large Sugar Pines and Douglas Fir were in the area. But across Secret Canyon to the south, on the northern exposures, these same ancient Sugar Pine and Douglas Fir are mixed with some large true fir such as White Fir and, rarely, Red Fir, with an understory of small to fairly large true fir.

We followed the road east to its end, where a short trail drops to the Secret Canyon Canal (SCC), a tributary to the Iowa Hill Canal (IHC). Suddenly all signs of logging disappeared and we all felt that this was a very special trail, almost level, winding through the forest of huge old trees. We passed the half-crushed shingled cabin and reached the "take" from Secret Canyon, where a log dam likely once diverted the creek into the SCC.

Directly across Secret Canyon and 25 feet higher is the American Hill Canal (AHC). We crossed and climbed over rocks to the old ditch, there, a wooden flume, with a surprising quantity of flume wood still visible on the ground.

It looks as though the flume, its most recent incarnation possibly dating to the 1930s, had been robbed for its lumber at some time, possibly for the cabin across the creek, and for whatever mining operations had been underway there.

At any rate, the main body of the wooden flume is gone, with parts of the floor remaining, and no signs of a fire have affected the area since the flume was built, perhaps seventy years ago.

We followed this American Hill Canal back down Secret Canyon to the west, until the first little "ditch lake" is reached, where a generous array of springs fill the old canal over a distance of over a hundred feet. We rested and ate and explored before turning back; there was only so much time, if we wished to visit the IHC.

At Beacroft we saw an SUV with a trailer and some kayaks. Soon we were at the pass, just beyond where the Beacroft Trail climbs away west, and entering a grove of White Fir, found and followed the little old road by which lumber for the giant IHC flume was hauled to the work. This part of the flume was necessary to cross the cliffy areas on both sides of Tadpole Canyon. Here, in contrast to the AHC in Secret Canyon, several wildfires had intervened since the flume's principal period of operation, in the 1870s, and only a very few fragments of almost unrecognizable flume wood remained.

However, the bench cut blasted from the cliffs makes for a very nice trail, in fact, the entire upper few miles of the IHC is shown as a trail on the 1962 TNF map of this area. It is fairly easy going and the old flume-trail offers great views into and across the North Fork canyon, here over 3000 feet deep. The big waterfall near the bottom of Big Valley Creek is still impressive.

Very much yellow-flowering Stonecrop was in bloom on the cliffs along the IHC trail, mixed with a red-purple profusion of Penstemon, possibly that species called Mountain Pride.

Tadpole Canyon creek has subsided quite a bit over recent weeks and we crossed by an easy jump and continued along on the IHC as it curved from north to east and reentered the main North Fork canyon. There the brush becomes extreme and further progress is barred. Green Manzanita, Huckleberry Oak, and Bush Chinquapin dominate. We had fine views across the North Fork to Sugar Pine Point, Cherry Point, Snow Mountain, and in the distance to the north, Castle and Basin peaks.

The Big Waterfall in Big Granite Creek is still big, and looks quite monstrous in fact. It would require quite a hike to actually visit the thing. It could be approached from above, from the Loch Leven Lakes area, but quite a bit of brush guards the entrances to Big Granite Canyon in that area.

The shadows lengthened and added considerable drama to the great and deep canyon of the North Fork American. We had a schedule to meet and had to leave a little earlier than we would have liked.

I have not seen, yet, the larger part of the Secret Canyon Canal. Maps suggest that it has been disrupted by logging and logging roads over much of its course in Little Secret Canyon. More exploration is needed. If it had been left intact, one could treat that uppermost part of the IHC, the SCC, and the AHC as one continuous trail, almost perfectly level, winding along through the main North Fork canyon, Tadpole Canyon, Little Secret Canyon, and Secret Canyon, for a distance of, say, almost ten miles.

It was a great day in and around the great canyon.