Showing posts with label 2008. Show all posts
Showing posts with label 2008. Show all posts

January 3 (1981, 1989, 2000, 2001, 2003, 2008)
Big Valley Bluff ~ More on the “Blasted Trail”

January 3, 2021

Several holes, dug through the duff by one of the resident critters... was it fungi or insects it was after? Is this why I am not finding mushrooms in this area? Yep, probably.


1/3/81   Way before dawn... went to the Bluff* yesterday and hiked down to the edge of the canyon. McClungs, anxious about heights, stayed above. I got hungry for quartz crystals and climbed down the cliff in search of quartz veins; I found many veins but few crystals. Clouds came in while we were there. We left after an hour or so.

It sprinkled lightly last night, the first precipitation in weeks. Incredible weather most of December—sunny, over 70° in the day, above 40° at night.”

[Russell Towle's journal]


*The "Bluff" is Big Valley Bluff, a point on the north rim of the North Fork canyon west of Snow Mountain. It is quite unusual to have been able to visit that spot on January 2nd, since the access road would normally be long blocked with snow by this mid-winter date, being over 6000' elevation. The warm, sunny December he describes in the second paragraph explains how it could be.

View to the east from the Bluff
(Click to enlarge)

View to the west from the Bluff
(Click to enlarge)

View south across to Tadpole Canyon
Straight down over "Falcon Perch" high above the river
Taken August 2, 2008, after the "American Fire" finally died out, from the Iowa Hill Ditch trail near the head of Tadpole Canyon, looking north across the North Fork to Big Valley Bluffthe highest point on the right.
(Click to enlarge)


January the 3rd, 1989

[...]

I cried while skiing up the meadow and out from my cabin today. It really seemed like good-bye. The water line is frozen, pipes are broken inside the bathroom wall, it is all a mess and a clutter and a thousand memories of so many many prayers for someone to share that incredible beauty with. So many unanswered prayers. And there comes a point when it is just too much, it has gone entirely too far, and yet the sun lights it all up as always and I cry to think of so much loneliness. It is so less than fair. Then for my father to move out there. It's over. I'm gone; if I am seen around here now, it is only my ghost. I'm out of here.

Or so I say.

The sun sets, after another clear day, so blessed after too many storms.

[...]

[Russell Towle's journal]


Date: Fri, 3 Jan 2003 08:39:41-0800
To: North_Fork_Trails
From: Russell Towle
Subject: Blasted Trail? Uhhh ... No!!!!

Hi all,

Terry Davis of the Sierra Club wrote, of Supervisor Rex Bloomfield's proposed Capitol-to-Capitol Trail,
"Bill & Russell & others, I've been horrified by Rex's trail concept ever since he started talking about it a couple of years ago. Wide, even grade, close to the river. He refused to even talk about using existing trails. He seemed to have in mind a mini super-highway, off limits only to motorized vehicles. I think that the Sierra Club, PARC, CNPS, Audubon all need to make it clear that we will not support the trail he has in mind—can you imagine blasting through the Giant Gap and the Royal Gorge? I wouldn't be so sure it's an impossible dream. Once the EIS/EIR is approved by the agencies, the grants will just roll in. We need to strategize on stopping, or modifying, this atrocity. I hate to wait until the environmental docs are out. We need to make this controversial now. Terry"
Now, others on this list have made some inquiries, and been assured by people involved in the actual planning of the trail, that:

1. It will not go through the Royal Gorge.
2. Its actual course has yet to be determined.

Hmmm. Then why did the map in the Bee article show it going right up the river?

I agree with Terry, we need to figure out how to stop this trail.

One thing we can do right now is let District Five Supervisor Rex Bloomfield know we are opposed. Perhaps the simplest message would be, "no new trail in the North Fork American canyon." That is least open to misinterpretation. His email address is:

Rex Bloomfield [no longer relevant]

He gets all these "North Fork Trails" email list messages anyway.

Cheers,

Russell Towle


Date: Fri, 3 Jan 2003 11:20:12 -0800
To: Deane_Swickard
From: Russell Towle
Subject: Re: Blasted Trail? Uhhh ... No!!!!
Cc: North_Fork_Trails


Hi Deane (Deane Swickard, Area Manager, Folsom Area, BLM),

Thanks for your reply, in which you wrote,
>
>Relax, there is no way a trail is going to be blasted up the North Fork
>American.
>
> First, it will never pass muster on environmental grounds.  It's
>inconsistent with wild river management.  There will be no blasting a trail
>along BLM or Forest Service land in the wild river corridor.  Since most of
>the river is publically owned from 1000ft above the Iowa Hill Bridge
>eastward, a trail within a quarter mile of the river doesn't have a prayer.
Yes, this seems only what good sense would imply.
>Rex has good intentions.  Trails are very popular and there is need for new
>trails throughout the state.  In this case, he seems limited a bit by his
>knowledge of the geography, the protections afforded wild rivers and the
>difficulty and cost of trail building in steep terrain.
Yes, Rex has good intentions. But the Road to Hell should by no means proceed up the North Fork of the American River!

Although it seems to me that no new trail would be allowed to be constructed within the North Fork American Wild & Scenic River corridor, nor, for that matter, within the canyon at large, this idea has been kicking around for a few years now, has not gone away, and in fact, has attracted a grant of $1.5 million from the CA Resources Agency, and a grant of $400,000 from the Placer Legacy.

It could be that Tahoe National Forest District Ranger Rich Johnson, of the Foresthill Ranger District, has provided encouragement to Rex Bloomfield, about the prospects for building a new trail, suitable for horses and mountain bikes, up the river, within Tahoe National Forest. For, Rich Johnson has said to me personally that he envisions opening up a trail from Mumford Bar, downstream to Italian Bar. Such a trail, I believe, existed in the 19th century, since I seem to recall that, in his diary, I.T. Coffin records going from Italian Bar up to Mumford Bar in 1863, along the river, which would be quite a strenuous exercise without some kind of trail to follow.

So, in this one reach of the river, it could be maintained that a trail already exists.

Similarly for the reach from Euchre Bar, upstream to Italian Bar.

I have been scouting out some of these old trails, now abandoned, but hesitate to bring them to the attention of Tahoe National Forest, lest they become mountain bike trails. I have about had it with mountain bikes in the North Fork American, especially within the Wild & Scenic River corridor.

Thanks again for your remarks, which tend to quiet my extreme terror.

All the best,

Russell Towle


March 25 (1981, 2001, 2003, 2008)
Flower Gallery. NFARA is Launched

3/25/81 rain, rain, rain… And snow up above. Fire crackles.”

[Russell Towle's journal]


Date: Sunday, 25 March 2001
To: North_Fork_Trails
From: Russell Towle
Subject: Flowers

Hi All,

I put up some pictures of flowers in Canyon Creek, this year. More to come as more comes into bloom.

Flowers and Ferns
of Canyon Creek

Winter and Spring, 2001


~ Special thanks to Karen Callahan ~

Photography by Russell Towle


The upper trail is crowded with Rue anemone right now, and larkspur is coming on strong down by Gorge Point. Also some poppies have appeared, violets, and others.

Cheers,

Russell Towle
[The page Russell was referencing is now archived on Ron Gould's North Fork Trails website, here:
http://www.northforktrails.com/RussellTowle/NorthFork/Wildflowers/Flower_Gallery.html ]


Porch worms, after heavy rains, 3/25/2001

Date: Tuesday, 25 March 2003
To: North_Fork_Trails
From: Russell Towle
Subject: Meeting Report

Hi all,

Some of those interested in forming a non-profit organization devoted to advocacy of environmental issues in and around the North Fork American, met at the Dutch Flat Community Club on Monday evening. Thanks to some diligent telephone tag on the part of Catherine O'Riley, we expected seven people to attend, but were pleasantly surprised when fourteen people arrived.

Jim Ricker of Dutch Flat ably presided over the meeting. He astounded me by bringing along a folder containing his notes of the meeting we held in March of 2000, at Bob & Judy Suter's house, in which we discussed forming a non-profit organization. Susan Prince of Dutch Flat used an amazing little folding keyboard attached to a Palm minicomputer to take notes.

I had envisioned reading aloud the text of six emails received from people interested in forming a non-profit, but unable to attend the meeting, but the opportunity never seemed to arise. Thanks nevertheless to those who offered support and suggestions, notably Michael McCormack, Tim Lasko, Tom McDonnell, Michael Joyce, Bill Newsom, and Evan Jones. Catherine and Jim did take the time to read these emails, at any rate.

Having established that those present were all in favor of forming an organization, and moreover a non-profit organization, we moved on to the initial issues of, first, what should the name be, and second, what should the "mission statement" of the organization be. We did little more than chalk up some possibilities on the old blackboard (the DF Community Club is the old DF school, which dates to 1898).

We scheduled another meeting for early May, on Monday the 6th, I believe.

Suggestions as to a name are welcome. Since we intend to defend the wildness and beauty of the North Fork of the American river, the name should reference that. Immediately we have quite a mouthful of words and syllables. Hence a name which lends itself to a good acronym is desired; much as the group "Protect the American River Canyons" has the acronym "PARC" which of course sounds like "park."

Incidentally, from an historic viewpoint, the phrase "American River Canyon" was taken to apply only to the North Fork canyon, not to any other branch of the American river. However, this point has been muddled over the course of time, and nowadays one often finds other forks of the American denoted as *the* American River Canyon. All this is only to say that a name which includes the phrase "American River Canyon" is susceptible to misinterpretation on the one hand, and confusion with PARC on the other.

The meeting went very well. Thanks to all who attended, and all who sent emails.

Cheers,

Russell Towle


March 25, 2008

“Playhouse Oak,” Moody Ridge

[Russ discovered this tree near the pond, along the line of an old narrow gauge railroad bed, in a thickly-forested area where he was doing some clearing and burning for the property owner.]


March 11 (1978, 1988, 2001, 2003, 2008)
Royal Depths, Royal Heights

“3/11/78   morning, on this fog-embraced mountain… i went out walking yesterday afternoon, took the old trail past the springs up beside the twin giant ponderosas to the rim of the canyon near the pond. then along the ridge to red ridge, where i descended to the cliffs. the clouds were thicker and the patches of light fewer. i was feeling good, delighting in the views of giant gap, finding some plants in bloom ~ some of the manzanita is in full bloom, and a certain purple crucifer and the umbellifer of yellow flowers (biscuit root?) ~ found a chipping station where indian men flaked stone, at a fine outcrop with many natural chairs and a great view of the pinnacles.

on impulse i decided to traverse the canyon wall from red ridge to lover's leap. sometimes scrambling through brush and small trees, sometimes out-and-out rock climbing, i slowly approached lover's leap, staying a few hundred feet below the rim of the canyon. finally the cliffs became too steep to traverse safely so I started climbing up, encountering some fine broad ledges, and some easy escalades spiced by dizzy five-hundred foot exposures. i pulled myself up one last ledge and found myself 20 feet from the leap. i sat down and watched the sunset colors on the high clouds that occasionally could be glimpsed through holes in the lower layers. an ethereal milky blue light filled the canyon below giant gap, while beyond to the west the entire cloud mass seemed to glow in the same pastel hues of blue and gray ~ a blue sunset. caƱon wrens called out from various points on the cliffs. the patch of purple flowers in their tiny nook on the brink of the leap were in total bloom… clouds lowered and lowered as the light faded and it began to sprinkle lightly… i walked slowly back, savoring the beauty of the whole day, stopping to listen to the frogs at the pond for a while, and walking down my trail as it finally began to rain in earnest. a few flashes of lightning to the west with vague rolling thunder sounds lent a sense of drama and magic to the day's end ~ i am a fool for thunder and lightning and beautiful women.”

[Russell Towle's journal]


“3/11/88   […]

Today, Eric Peach and I will be skiing out to Snow Mountain.

Later; 10:30 PM; having utterly thrashed myself, by skiing to Snow Mountain, I am now at home and at rest, muscles sore, heels blistered, face sunburned, my back, that of an ancient who'd carried hundredweight sacks of wheat for a living all his working life: but it was worth it. Fifteen or so miles, three thousand or so feet of elevation gain, the snow, monolithic ice, the sun bright, the wind fresh and cold, the three golden eagles rambunctious and eerily transcendent (what? were they butting heads together? impetuously charging? Let it only be known that they playfully soared and explored, that they rose with ghostly ease from royal depths to royal heights), and the view of course wide and wonderful, encompassing much dear diary, of the same ol' same ol' — but including, to my surprise, not only Mt. Lassen but Mt. Shasta!

Now I am home and now I drink tea and replenish my self, my fluids.”

[Russell Towle's journal]


Date: Sun, 11 Mar 2001 22:11:43 -0800
To: North_Fork_Trails
From: Russell Towle
Subject: Sunday's work party

Hi all,

Evan Jones, Tom Molloy, and I headed in to Canyon Creek Sunday morning, to work on the rockslide part of the trail near Gorge Point. The cloudy morning quickly turned sunny. At the rockslide, we were able to identify the original line of the trail. In many places the original retaining walls had been torn away by the rockslide. We focused our efforts on the uppermost section and for an hour or so dug with shovel and mattock and heaved big slabs of rock around. Although even this section cannot be said to be finished, it is better than it was.

The sun was hot and we took lunch at the base of the Big Waterfall before continuing down to the river. The North Fork is running medium high and clear. After enjoying the scene we took saw and loppers, jumped the creek above the last waterfall, and headed west on the trail to Indian Ravine/Pickering Bar. We cleared the brush off the trail and spent a while exploring around near Indiana Ravine. Some small patches of Quaternary gravels there had been worked pretty intensively, long ago.

On the way back out we visited the fine overlook on the ridge dividing Canyon Creek from the main canyon. You can see Lovers Leap and the Pinnacle Ridge flanking Giant Gap, and beyond, Sawtooth Ridge, with snowy Black Mountain and Quartz Mountain in the distance. The river itself can be seen far below. There is also a nice view to the southwest, down the canyon, from there.

It was a good day and some progress was made on the trails.


Date: Tue, 11 Mar 2003 11:09:03 -0800
To: North_Fork_Trails
From: Russell Towle
Subject: Lost Camp

Hi all,

Recently I have heard from Dave Sutton of the Trust for Public Land, about possible BLM acquisition of lands in the Gold Run area. I hope that much if not all of the 800 acres currently for sale in the Gold Run Diggings can be acquired. A 40-acres parcel in the west part of Green Valley, north of the river, is also of prime importance.

A fellow named Mike Powell contacted me with remembrances of adventures with Gene Markley years ago. I hope he will write up some of them for this list. He did write as follows:
>I will try to recall this trip from my faded brain cells...this was done in my early twenties and was one of many, many canyon trips throughout the region to include a number of trips into the "tea cup" area of the N. of the N. Fork American above where Fulda creek dumps in. I remember a small group of us scrambling and repelling down falls on Fulda one afternoon just for grins into the pool on the N. of the North, swimming the pool down stream and climbing out on the old China Bar trail. That was back in the days where you could haul ass out to the old Bar in Blue Canyon and have a cold beer while shooting the breeze with Joe while he told stories of catching big rainbow and browns...
I usually call this the Lost Camp Trail, because I have nothing in the historical record to support the name "China Bar Trail." Whatever it is called, it is one of our more important trails, and, unfortunately, heads up on private property near the ghost town of Lost Camp. I have advocated that Tahoe National Forest try to acquire these lands at Lost Camp, but so far, without even a response, not to mention a positive response.

The "tea cup area" is in the inner gorge of the North Fork of the North Fork, a remarkable confluence of gorges, with many, many waterfalls, and, wow, not at all easy to get into and see. An awesome, awesome place! The easiest way in is upstream from the Lost Camp Trail, swimming the Pool of Cold Fire ... and then on.

Cheers,

Russell Towle


March 11, 2008
[Excerpt from North Fork Trails blogpost:
http://northforktrails.blogspot.com/2008/03/odds-ends-new-old-trail.html ]
Over recent weeks I have been clearing a beautiful little patch of forest up on Moody Ridge, and burning tons of dead wood in the snow. I walk half a mile or so to the job site, and while walking, I have seen many a mountain lion track, likely all from one and the same lion. I have had a chance to see what tracks look like in soft snow, in hard snow, what they look like after one day, or after four days, and so on.

Yesterday afternoon I was walking home and thought to take a shortcut to avoid some deep snow. I got myself into a real tangle of young conifers and brush and broke through into a small opening. Lion tracks dotted the snow, extremely fresh, retaining every detail. Hours old at best. I quickly scanned the trees above me: no lion. Then I looked down at the snow again and was puzzled to see that the lion had walked in circles. All the tracks looked very fresh. I looked again, up, and all around; nothing, but the forest is so overgrown I couldn't see far in any case. So I blundered along my supposed shortcut. In another few yards a disgusting smell wafted my way, and at first I thought of the gamy smell a bear can have, which I have only smelled a few times in my life. I walked another few paces, the smell ever stronger, and suddenly realized it was the smell of Death. The lion had left its kill somewhere very near, possibly up in a tree. I hastened away.



February 10 (1982, 2003, 2008)
Snow Flakes in the Sun ~ CCT Photos and a River Scramble into Giant Gap ~ Thrusting Shoo Fly

2/10/82   Soon after dawn. Skis stand in the sun, awaiting the re-mounting of the heel locators with sanded bottoms and epoxy in the screw holes.

Dave Nelson and I went skiing yesterday, up to Rowton and the meadows in the headwaters of Onion Creek. He did quite well. We were blessed by a beautiful day, with two inches of fresh powder on a firm base. Partly cloudy skies dropped finely shaped snowflakes on us while the sun shone.

I saw a bird dive into a hole in the snow up on top of the ridge near Dave's place. It had been dancing.”

[Russell Towle's journal]


Date: Mon, 10 Feb 2003
To: NorthForkTrails
From: Russell Towle
Subject: Giant Gap by way of Canyon Creek

Hi all,

I met Larry Hillberg, who has been gradually cleaning up the mess out on the Stevens Trail, at ten in the morning, and we snuck into the Gold Run Diggings and drove to the head of the Canyon Creek Trail in Potato Ravine. Larry says that there are probably twenty more loads to be carried out from the Stevens Trail site.

This was Larry's first visit to Canyon Creek. We stopped to admire the great tunnel of the Gold Run Ditch & Mining Co. (1873), crossed the bridge, saved the side trail to the Blasted Digger for later, noted Brewer's Rock Cress and Biscuit Root in bloom at Gorge Point, skipped the Six-Inch Trail to the Inner Gorge, but took High Terraces Trail and then the spur up to the Big Waterfall. We saw many California Milkmaids and some Rue Anemone in bloom. The white racing pigeons were not in evidence.

I remember a friend of mine, Ron LaLande, brought a passel of racing pigeons up here in the mid-1970s, and all but one of them were killed by falcons and bird hawks in fairly short order. The one survivor, a female named Jethro, used to fly beside Ron as he rode his little motorcycle miles in to Dutch Flat. Perhaps these pigeons of the Big Waterfall have been discovered by hawks or falcons.

Returning down the spur trail, we dropped down to the Terraces, where the miners who tended the sluice boxes in Canyon Creek in the 1870s had their principal camp, to find a young man camping there. His name is Peter Fortune, and his camp was neat, and a civil engineering textbook has open beside him on the lawn-like terrace. We chatted with him for a while. It developed that he had discovered Canyon Creek on my web site. I mentioned that only that morning I had thought about taking down the Canyon Creek page, since too many people seem to be discovering it. However, young Peter Fortune is just the kind of person I like to see in there. He is a friend of Gene Markley, the famous gorge-scrambler and master of obscure mining trails in the American River basin, and Peter and his friends consult with Gene and then explore accordingly. He has done the Royal Gorge, Giant Gap, the gorge between Euchre Bar and Green Valley, and other parts of the North Fork. In fact, it was Peter who did the trail work Catherine and Ron Gould and I observed in the east end of Green Valley, a few weeks ago.

Peter mentioned what I had also recently heard from Ron, that the side trail to Green Valley from the Euchre Bar Trail has been flagged in red; Peter adds that the flagging extends to the summit of East Knoll. This worries me, as a private parcel extends to the top of East Knoll from the river, and I have heard the inquiries were made to Tahoe National Forest by someone owning property in Green Valley, who wished to bulldoze a road down there. TNF made some efforts a few years ago to purchase the private inholdings in Green Valley but failed.

Larry and I left Peter to his studies, and took Lower Terraces Trail back to the main trail and quickly reached the river. The day was surpassingly sunny and clear. After a short break, we decided to explore the upriver trail. This trail passes a rather nasty cliff only a couple hundred yards east of Canyon Creek. From this first part of the upriver trail one can see, alternately, the Pinnacles on the right, and Lovers Leap on the left, as one looks up into Giant Gap.


The trail climbs and then plunges up and down in an annoying fashion, passing rocky spurs and dipping in and out of gullies. We saw a pair of kayakers ahead, scouting some rapids. The trail drops slowly back to near river level and then climbs slightly to level out through a grove of Canyon Live Oaks, around half a mile upstream from Canyon Creek. At the east end of the grove the trail becomes faint and an old miner's camping terrace is seen, with garbage strewn all over the slopes by squatters, perhaps ten years ago.

Here one reaches a gully and a problematic part of the upriver trail. East of the gully is a difficult patch of brush with much thorny Buckbrush. At the lower level, around one hundred feet above the river, where we hit the gully, there is no clearly-defined continuation of the trail. At higher and then still higher levels, there are two trails leading out of the gully to the east, but both enter the brush-patch, which is nearly impassable. Larry and I just stayed low until past the brush and then switched back and forth up grassy slopes between rock crags until we reached the upriver trail again, here around three or four hundred feet above the river.

This trail probably dates back to the Gold Rush, and then likely was used by Chinese miners working the river in the later 1850s and 1860s. Wherever the canyon narrows into a gorge it is forced to follow a higher line. It was very open and sunny and we saw Houndstongue in full bloom.

Now nearly a mile upstream from Canyon Creek, and so high above the river, we enjoyed very fine views of the remarkable cliffs and pinnacles of Giant Gap. In places we lost the trail, but always rediscovered it, and finally it descended back to river level, at a sharp bend in the river.

An unnamed spur from Moody Ridge forces the river into an even sharper bend just upstream. One rambles along over boulders near river level, and then climbs up a short distance to regain the upriver trail, as it runs along the base of the spur ridge. As it approaches the sharper bend, another old camping terrace, with another mess of squatter's garbage, is passed. Then, in a welter of poison oak, one can climb to some rocky cliff-tops with a view up the river east of the spur ridge. Although the canyon has been fairly gorge-like in the two miles upstream from Canyon Creek, here it becomes so extremely cliffy that whatever slender thread of trail which may have once existed, would have followed a very high line above river level.

The sun was lowering as we began our retreat back down the trail. When we reached the Brush Patch near the gully, we did some crawling and found the higher of the two trail lines into the gully. Since we were fully 400 feet above the river, and since we agreed that elevation is a precious thing, we decided to angle up and to the west and strike the ridge dividing Canyon Creek from the North Fork at the Blasted Digger Overlook. This turned out to be somewhat harder than we had imagined, but it was interesting to be on such wild cliffy slopes. There are a couple of gullies which contain great fields of angular talus.

As we slowly zigged and zagged up and to the west past crag and shrub a falcon zoomed by, heading west. It had a lot of white on its head, and I am not sure what species it was.

Finally we gained the ridge, only a hundred yards from the Blasted Digger. I had hoped to stop and rest there and enjoy the fine view, but the sun had set for that point, though still gilding the high cliffs across the canyon, and a chill was in the air. We took the trail back to Canyon Creek and arrived at Potato Ravine in another fifteen or twenty minutes, very tired and scratched, but pleased to have visited such an inaccessible and beautiful part of the canyon.

Such was a day on the North Fork American.

Cheers,

Russell Towle


Thrusting Shoo Fly
[North Fork Trails blogpost, February 10, 2008:
http://northforktrails.blogspot.com/2008/02/thrusting-shoo-fly.html ]
On YouTube, at
http://www.youtube.com/watch?v=J3KryrAGkBo

is an animation of a flight up the American River Canyon, using the USGS Digital Elevation Model 30-meter data set, and merging a couple dozen DEM quadrangles to build a landscape spanning Colfax on the west, the Sierra Crest on the east, the San Juan Ridge and Grouse Ridge to the north, and the Middle Fork of the American on the south. The virtual camera follows an almost due east heading from west of Rollins Lake, crossing over Lovers Leap and Green Valley, and flying on up the canyon into the Royal Gorge. The animation finishes with the virtual camera making an orbit of 360 degrees around Snow Mountain.

Thrusting Shoo Fly: on my iMac I can set the screensaver to loop through any folder of images in my iPhoto library. It so happens that right now it loops through a folder of some of my favorite photographs in the North Fork. Here is Giant Gap, from the west, and now from the east; or the 500-foot waterfall in New York Canyon, or Big Valley Bluff at dawn, as seen from the North Fork, a couple miles up the canyon.

And so on. It's not hard to take beautiful photographs in such a beautiful place.

It happens that one of these special photographs shows what I call Bluff Camp, an old mining camp immediately adjacent to the river, set on a cliff-bounded strath terrace bearing a fine grove of Canyon Live Oaks. From the North Fork American River Trail, connecting Sailor Canyon to Mumford Bar, a side trail leads one down a hundred yards, or so, to Bluff Camp. I have camped there many a time. It is half a mile or so east of Tadpole Canyon, and directly below Big Valley Bluff, rising in ragged cliffs all of 3500', across the river to the north.

And the photograph was taken from a point upstream from Bluff Camp; so one sees a part of the encircling cliffs, and a flat area—the strath terrace—perhaps thirty feet above river level. (A "strath terrace" is a glacio-fluvial landform associated with glacial outwash sediments which once occupied the terrace itself; and it was these very sediments which planed down the bedrock, to make the terrace).

It caught my eye, the other day, the Bluff Camp photo, as it filled the screen; I could see an abrupt change in the bedrock, right at the upstream end of the strath terrace. Slowly, dimly, I realized I was seeing a thrust fault. Two disparate bodies of rock had been juxtaposed by faulting.

The bedrock for miles up and down the canyon is composed of metasediments of the early-Paleozoic "Shoo Fly Complex," the oldest rocks in all the Sierra. I have a wonderfully precise geologic map of this part of the North Fork canyon, made by David S. Harwood et. al. of the USGS, in the early 1990s. Harwood shows many thrust faults in the Shoo Fly Complex near Big Valley Bluff, Sugar Pine Point, and New York Canyon. The faults sometimes bring big blocks of chert, hundreds of yards in extent, or more, into contact with slates and other types of rock in the Shoo Fly Complex.

By the way, it is called a "Complex" because it is composed of many distinct formations, spanning many millions of years in time, but all very old. Harwood describes and names four such formations in this particular area. His map does not show the Bluff Camp Thrust, which is probably a sensible choice, for it is likely not very long or large as thrust faults go, and if he were to put every such minor thrust fault on his map, well, there would be room for precious little else.

It has long been considered that the great mashing-together, the epochal juxtaposition of the disparate Sierran metamorphic rocks alongside one another, took place around 145 million years ago, in what was named the "Nevadan Orogeny" (an "orogeny" is a mountain-building). It was this Nevadan Orogeny which acted to rotate all these disparate bodies of metamorphic rock almost 90 degrees to the east, so that what were once flat-lying beds are now almost vertical, or even slightly overturned. And it is considered that the "penetrative fabric" of these disparate metamorphic rocks is mainly due to the Nevadan Orogeny. The compressive and shearing forces which imparted the fabric were fairly well parallel with the current, almost-vertical orientation of the beds. Very likely it all had to do with continental accretion, at a time when Pacific ocean floor was being actively subducted beneath the continental margin, moving from west to east, but also plunging steeply down.

However, in many of these different metamorphic rock formations, whether they be down by Auburn or up at Big Valley Bluff, an experienced eye can detect at least two different episodes of deformation, each leaving its footprint, or imposing its fabric, upon the rocks. There is the later Nevadan Orogeny; and at Bluff Camp, there is a thrust fault vastly older than the Nevadan Orogeny. That is to say, the Shoo Fly was already well-deformed, well-sliced and diced by thrust faults, long before the Nevadan Orogeny.

And Harwood discusses all this in the twelve-page essay which accompanies his map. There are a couple of typographical errors in this essay which play the very devil in understanding the thing.

It is not at all easy to learn to recognize these different rock types. That this is chert, and that is quartzite, may not be discernible except under a microscope. To develop a simple portrait of the bedrock geology, one can read what was written about it a century and more ago. At that time the focus was upon the broad outlines, not the higgley-piggley details. And for a time, the following usage had currency, for instance, in the articles by C.J. Brown of Dutch Flat, published in the Mining & Scientific Press, in 1875.

Brown divides the metamorphic rocks as follows: the Western Slate, the Middle Slate, and the Eastern Slate. Between the Middle Slate and the Eastern Slate, he identifies the long narrow serpentine belt we now name for its associated Melones Fault Zone.

Hence his Eastern Slate corresponds to the Shoo Fly Complex, and those other Paleozoic and Mesozoic rocks which lie on top of the Shoo Fly, and therefore, to the east (the whole shebang, be it remembered, rotating 90 degrees to the east during the Nevadan Orogeny).

Brown's Middle Slate corresponds to the Calaveras Complex, another complex of formations, but late-Paleozoic in age, and he correctly identifies the rock of Giant Gap as metavolcanic—in fact, Brown declares it to be metabasalt; and his Western Slate corresponds to all those metamorphic rocks west of Cape Horn, in which there are several distinct formations, often dominated by metavolcanic rock, but containing some metasediments, too.

So, if we wish to blur our focus and appreciate the broader outlines of local bedrock geology, we might give C.J. Brown's Western/Middle/Serpentine/Eastern model a try.



January 22 (1978, 2002, 2008)
Harpies, Daemons, and Nefarious People

1/22/78   Well, here I sit in my cabin. A weak storm front that moved through during the night has left the North Fork canyon a witch's cauldron of fog—here, billowing up in mountains edged with gold in the morning light, there, exploded into puffs and patches and tendrils that drift about with shadows in tow, fleet shadows that make the sunny north wall of the canyon into a rippling tapestry, sometimes, however, coalescing into a dull, somber aspect that seems akin to the medieval man's image of mountains ~ fearful landscapes beplagued with harpies, daemons of all sorts and kinds, certain disaster for those unwary enough to stray therein...

yes, a magnificent day. [...] well, outside is the place for me.”

[Russell Towle's journal]

Green Valley, glimpsed through the shifting mists

Date: Tue, 22 Jan 2002 14:04:12 -0800
To: North_Fork_Trails
From: Russell Towle
Subject: Gold Run/Canyon Creek


Hi all,

With two weeks of dry weather, the latter week with cold nights, Canyon Creek has subsided to low to moderate flows. It is interesting that, despite all the wet weather we have had, the ground water has not yet recharged to a "normal" winter surplus, and the hundreds of springs issuing from the volcanic strata in the upper basin of Canyon Creek continue at low, more summer-like flows.

Over this past fall and winter I have worked a bit on the uppermost section of the Canyon Creek Trail, from Potato Ravine Pass east to the Indiana Hill Ditch and a little ways along that ditch. This portion of the trail was partly buried and disrupted in various ways by salvage logging following a wildfire ca. 1960, and then again by bulldozer activity on a nearby road, in the 1980s. Ed Stadum and Catherine O'Riley helped a lot. Most recently, I restored the original line of the trail along the ditch, where logging skid trails had left huge piles of dirt. I have made no attempt to restore the full original width of the trail, merely making the narrowest of bench cuts and minor fills along the original trail line.

Recently I learned of the California Heritage Fund grant program, which is directed at acquisition of properties with historical significance, and which seems an awfully good match for the 800 acres now for sale in the Gold Run Diggings. I contacted Supervisor Rex Bloomfield and Placer Legacy chief Loren Clark about the grant program, which is administered by the State Office of Historic Preservation. I also contacted a person in that office, Cheri Stanton, who sent me a PDF file containing the grant application form. There are two deadlines for the current funding cycle, in March and August of 2002. Cheri informs me that the grant application is also available for viewing and downloading at the Office of Historic Preservation (OHP) web site:
http://www.ohp.parks.ca.gov

Perhaps the BLM and Placer County could collaborate to acquire the entire 800 acres now for sale. This land includes much of the length of the Canyon Creek Trail. Currently the BLM lands in the southern part of the Diggings are open to OHV use and also are open to "mineral entry," i.e., mining claims. This, despite the fact that these same lands are within the special Gold Run Extension of the North Fork American Wild & Scenic River zone. I would like to see these existing BLM lands, along with any acquisitions which may be made, closed to OHV use and to mineral entry, with every effort made to quiet existing claims.

All this is only to say that if, by some miracle, the 800 acres were acquired, the BLM and Placer County would be faced with the question, what do we do with it? How will it be managed, for what purposes, etc. etc.? And so it behooves those of us who like the Diggings and the Canyon Creek Trail to give some thought about the future of this area.

Cheers,

Russell Towle


The Secret Trails of Green Valley
["North Fork Trails" blog post, January 22, 2008:
http://northforktrails.blogspot.com/2008/01/secret-trails-of-green-valley.html ]
I was surprised to hear from someone, in response to my "Visit to Green Valley," that she wishes the trails of Green Valley kept a secret. She objects to my mention of hiking on old mining ditches or on this or that old trail; there are, it seems, Nefarious People on this North Fork Trails email list, who, though my malfeasance, now know about the mining ditches and old trails in Green Valley.

Never mind that I have often written about precisely these ditches and trails before.

The Nefarious People, she writes, will tie plastic flagging all along the ditches, all along the trails, spray-painting a boulder now and then for good measure, with artful messages like "Green Valley Blue Gravel Mine Ditch, .25."

Perhaps one spray-painted boulder would warn of rattlesnakes. Another might read, "Euchre Bar, 1 mile, If You Like Jumping on Cliffs and Fording Raging Rivers."

Well, I'm sorry, but it is my philosophy that the old trails of the North Fork need to be known, not unknown. The North Fork of the American River—its wildness, its beautiful scenery, its historic trails and mining ditches and prehistoric sites—deserves every kind of protection and preservation. But this protection and preservation is hardly possible if no one knows the great canyon, and its great old trails.

This email list is all about making this wildness, this beauty, these old trails and ditches, known. In Green Valley, a number of private parcels exist, old patented mining claims, any one of which could on any given day sprout "No Trespassing" signs, or even a cabin. The purchase of these private parcels, and the transfer of the titles to Tahoe National Forest, or to the Bureau of Land Management, depending upon the location of the parcel— the purchase of these parcels is critical to the future of Green Valley.

So, don't forget, the High Ditch is quite near the 2080' contour, in Green Valley, north of the river. Hike it, and let me know if you like it; it makes for a nearly level walk of a mile or so, from one end of Green Valley to the other. It crosses the East Trail about three hundred yards above Joe Steiner's grave, with another ditch, at that point, closely paralleling it, just above. The Still-Higher Ditch, as it were. But the High Ditch itself is the ticket.

Below, a map of Green Valley, showing some of its trails and ditches—which are also trails.

Trails in Green Valley
North is up. This map doesn't show the parking area that was established on county land to serve users of the Green Valley Trail. It is on Moody Ridge Rd., about 100 yards west of the Aquila Rd. intersection, on the left. There is a shortcut trail from that parking area over to the trailhead.



June 1 (1977, 1979, 1986, 1996, 2002, 2008)
Ants' Hunting Camp ~ Passion for Trails

6/1/77 ~ just after dawn in the canyon. as i listened to a grosbeak singing, a train enters the canyon… the upper pinnacles of giant gap are sunlit.

grosbeaks sing in such sweet phrases. river roars in its distance. mosquitoes whine. mice dash about from ridge pole to plate to floor. a colony of carnivorous ants have a hunting camp established on the sill of the big window. about a hundred of them rear up on their hind legs and wave their arms about in the most atavistic manner, waiting for some careless fly or wasp, engaged in buzzing against the glass, to lurch down within reach. Then one of the ants will chomp onto a foot and hang on like a bulldog. soon nearby ants will notice the capture and assist, until the fly is held securely by half a dozen or so. eventually the whirring wings are caught and held, the squirming abdomen restrained, the wiggling head captured as well. soon the wings are torn off and discarded (there were quite a number of them on the floor beneath that corner of the window when i arrived yesterday) and somehow the coup de grace is administered (i haven't been patient enough to observe it yet); then the fly nearly disappears in a swarm of ants as they tug and pull, never entirely in concert, the corpse on the long road out of the cabin. at any given point during the day the hunting camp is usually engaged in three or four kills.”

[Russell Towle's journal]


6/1/79 wind roars in the trees as it has every day recently. deerbrush at its peak now.”

[Russell Towle's journal]


June 1, 1986 […]
Called Newsom last Friday [about the] tax deductible status for his donation towards the full-page ad which ran today in the Auburn Journal concerning the TNF Plan. He asked me to look into a situation in Truckee, wherein logging has begun recently on a timber sale made in 1982; much of the job involves clearcutting, and I'll enclose for future reference a draft of the first page of the report I wrote for Newsom, in the Archives. [...]

Kevin Clark from BLM had to call off the meeting we planned for last Friday; I need to get back to him. Will Carroll will be coming up on Tuesday to examine the Big Oak. Rebecca Siren will be coming up on Thursday to look at the garbag at Bogus Point; she's from Placer County Environmental Health.”

[Russell Towle's journal]


June 1, 1996

Saturday afternoon, the kids in the hot tub, which is slowly filling with warm water, made by burning manzanita branches I had to cut from the path of my newest trail. Yes, dear diary, trails have become one of my passions around here, over the past several years. I first improved the Old Trail out to the springs and beyond, then added a long extension over to Rick and Aki’s place, making more than a half mile altogether. I made a High Trail which makes a return to the Meadow from the Rick & Aki Trail (as we call it), but it is in poor condition, and rarely used. I made a Low Trail out to a point on the Rick & Aki Trail, from the Fourth Spring down to the ridge to the west, where an old mule trail descends to Green Valley, thence up the mule trail to the top of the ridge.

I made a Maple Grove Trail out to the northeast corner of my property, with a return to the upper Meadow. But it is rarely used, and partially blocked with fallen branches.

Also, a Lower Cliff Trail out to The Cliffs.

Most recently, I made a trail which descends the cliffs and winds back into the gully where the old mine tunnel is. There I made a pool, using volcanic mudflow (andesite) boulders for the dam, where water from the springs falls down a mossy rock face. So we call this the Pool Trail. Along the way a branch leads to the Sun Spot, a protected hollow in the cliffs opening to the south. A good place in winter, when clear weather returns after storms, but strong north winds make the Cliffs themselves a little too cool.

And then finally, the New Trail, connecting to the old Green Valley Trail to the east, where I have restored in part the old mule trail which switches back and forth in descent, long ago cut by hikers who avoided the switchbacks and made a steeper more direct route, and overgrown by manzanita, which I cut away. This trail was a piece of work. It is cut into a steep hillside, and makes a smooth descent to join the Green Valley Trail. It still needs a lot of work. [...]

So, Janet and Greg and I dragged a few manzanita branches up here, and I kindled the fire beneath the old metal tank, and a hose leads the hot water into the old wooden hot tub Bill Newsom gave me seven years ago. We had to drain the water out and bail the residue, full of little wiggly worms and water beetles and mosquito larvae and so on. We couldn’t clean the algae out properly, so now the new fresh water is a little green and murky from the get-go.”

[Russell Towle's journal]


Date: Sat, 1 Jun 2002 14:05:31 -0800
To: North_Fork_Trails
From: Russell Towle
Subject: Lion search

Hi all,

Harvest Brodiaea
(Brodiaea elegans)
At 7:00 a.m. Friday morning I drove out to Gold Run, then south on Garrett Road, parked in the pine forest, and hiked across the Diggings on the Paleobotanist Trail to the Canyon Creek Trail. I made an early start to beat the heat. At the Canyon Creek trailhead I shouldered one of the three 2X6's John Krogsrud bought for the little bridge, and carried it on down. As I approached the big tunnel on the old wagon road section of the trail, I was surprised to see, through a tiny gap in the Canyon Live Oaks, the Blasted Digger Pine, well to the south on the ridge dividing Canyon Creek from the North Fork. I had no idea it was visible from this high on the trail.

I noted a complete absence of recent Bobcat scat on the trail, and wondered whether some distemper had afflicted the local population. This happens to the foxes from time to time, they are decimated by disease. After a little exploring around on Canyon Creek downstream from the bridge, I was back up top at my truck before ten in the morning.

Last night my dog awoke me around 1:30 in the morning with one of his irksome harangues of the local wildlife. Perhaps a deer or a bear had strayed too near for his liking. As I waited for the barking to subside, I heard the hooting of an owl and opened my sleeping loft window. It was a Spotted Owl, hated by loggers, an owl I have never seen but heard often enough. They make an amazing variety of sounds. When I first moved here in 1976, I slept outside all summer, and was actually frightened by the demonic howling of the spotted owls. Moody Ridge was very wild then, in the days before it was illegally subdivided.

My daughter and I heard one the other night. It made a series of even-toned, soft barks, and then launched into some very sweet and smooth whistles, each beginning on a low note and rising fairly high. Last night the owl was again quite close. It did not sound like a tortured dog from hell but like an owl, making a series of sweet hooting barks, in gradually rising notes, with a final flourish of three finely crafted hoots. Gradually it simplified this complex series. I got up, dressed quickly, and went outside. The stars were glittering. The owl had moved west along the tops of the little cliffs near here, and had retained its simplified mode of hooting. I walked west towards the springs and answered with similar hoots, hoping to lure it back, but it slowly went farther west. When it was about a half-mile away I came back inside.

I noticed that a bank of clouds hung over the Sierra to the south. Staying up nearly another hour, I peeked outside before returning to bed, and saw the clouds had moved north and were directly overhead.

This morning dawned cool and cloudy and I decided to return to Canyon Creek and carry the last two 2X6's down to the bridge. I began to harbor a hope that I would see some wildlife; there was something about this cloudy morning, a hushed, still feeling, with some prospect of thunderstorms developing, that made me think I might get lucky; and then, I had heard the spotted owl the night before; somehow this all seemed to add up to a chance of actually seeing something.

I did notice that, as I approached the Canyon Creek Trail, in the Diggings, there were two fresh Bobcat scats on the road, where there had been none yesterday. They were quite different from one another, inches apart. Something to do with diet I suppose. At any rate. I brought a ratty little pillow along to cushion my shoulder, and heaved the two 2X6's up. They were heavy; John had warned me that they were green and heavy, and even now, after a couple of weeks to dry, they were a load; around, say, 40 to 50 pounds. I had my pack on too, with my camera and some water etc.
Orange Bush Monkeyflower
(Diplacus aurantiacus)
Well, it was kind of rough, but I did it. I had to switch from one shoulder to the other, increasingly frequently, and even though it was all pretty much downhill, I worked up quite the sweat. Finally I was there, and took a break, and admired the flowers near the bridge. The Notch-petaled Bush Monkeyflower is in full bloom at the bridge level now, and remains in full bloom at least as far down as Gorge Point. These small bushes are covered with dozens to, I should think, hundreds, of showy, large flowers, somewhat like snapdragons in appearance, salmon to cream in color, with some small yellow blotches inside the floral tube. And, there are a lot of these little bushes. I would say that I saw, oh, at least 100,000 of these flowers today.

Mystery Plant—if you can identify, post a comment.
After a rest, I crossed the bridge and walked down to the Waterfall Vista, then out to the Blasted Digger Pine, and then on down to Gorge Point and the Rockslide. There are many species of flower in bloom now, and many that were in bloom a month or so ago, but are not, now. There were the tall larkspurs, and the Tincture Plant, and thousands of daisy-like tarweeds, and real daisies, and on and on. It is, I think, a little better than average year for flowers, in Canyon Creek, anyway.

Eventually, I headed up and out. It was a quiet, rather leisurely morning in Canyon Creek. I did see some swallows and hawks and assorted other birds, but no big animals, no foxes or bobcats or bears or lions. A few alligator lizards startled me along the trail, but not even one rattlesnake made an appearance. As I hiked slowly up the trail the clouds began to part and swell into thunderstorm form, but without producing any actual storms, at least, in this area. I was back home about 1:00 p.m.

If anyone entertains thoughts of visiting Canyon Creek and seeing the fine flowers, do it now, or next weekend if possible. If you want some company, or just directions, give me a call.

Cheers,

Russell Towle


Return to Hayden Hill and the Terrace Trail
[North Fork Trails blogpost, June 1, 2008:
http://northforktrails.blogspot.com/2008/06/return-to-hayden-hill-and-terrace-trail.html ]

Russ included several pictures within the post at that link—which he rarely did (though he took scads of wonderful photos) because of the horrible slow rodent-chewed "farm-line" dialup internet connection we suffered with at the time. I will not repost everything here, but just an excerpt, and this map showing the route he and Ron took:

[...]

We reached the top of one of the huge red mining scars above the mine. These were much more visible thirty years ago; small pines and other trees have gradually populated the scars. The scars derive from hydraulic mining over a century ago. I had never been to the top of the scars before. I scanned the red surface closely; already the auriferous gravels at the Hayden Hill Mine counted as the oldest of the glacial outwash deposits left in Green Valley, as the mine is associated with an abandoned channel of the North Fork, the base of which channel is fully four hundred feet above the river, and the tops of the principal outwash terraces flanking this abandoned channel, six hundred feet above the river. I myself guess these terraces to be roughly 750,000 years old, dating from the Sherwin Glaciation. But the Red Scars rise higher yet. Could one find an absolute highest elevation where glacial outwash is preserved, in these scars?

At the top of the scars, the reddish material had the character of being a very weakly stratified deposit of angular chunks of rock, of an entirely local origin, in a matrix of silt and clay. Were it not for the weak stratification, almost invisible, one would be tempted to name it a colluvial deposit, not alluvial at all. As it is, it is about as frustrating as the trail-which-is-not-a-trail we had been following: the deposit has rocks deriving only from the slopes immediately above, and all angular: hence colluvium, hence not glacial outwash. But the deposit is weakly stratified! And it is, whatever its origin and significance, lying on top of true glacial outwash deposits, some distance below.

Well. Interesting, anyway. We followed a game trail right through the Western Red Scar basin, and entered another patch of oak forest, with more game trails, of the kind which with enough imagination might be human trails.

[...]


May 24 (1976, 1979, 1987, 1988, 2006, 2008)
Moody Ridge Ecotones ~ Pileated Woodpeckers ~ More Birds; and Helicopters

5/24/76 morning, birds singing loud… heard a fox barking around dawn. got the ‘basket’* almost all wired up yesterday before the mosquitoes got too bad. should start laying up the cement today. wish i had thought to bring a trowel. my hands will suffice for it.”

Russell Towle's journal
*Russell refers to the water storage cistern he'd begun building to hold spring water for his cabin supply.

5/24/79 ~ beautiful sunrise. two partly cloudy days cooled down the temperature, but no rain. deerbrush is blooming around my cabin.”

Russell Towle's journal


5/24/87 morning, cloudy and cool. I light a fire, cook macaroni, plan the day. Yesterday I went by Bill's in the morning, no sign, dropped off a copy of The Letter [...]

Russell Towle's journal


5/24/88 and now in print once again, yours truly, atque in perpetuum, frater, ave atque vale, hence I re-read Jaime de Angulo, and what was to have been a short essay upon the lives and times of the Dutch Flat Maidu became, within seconds of sitting down before the computer, a cry of despair at their complete and most shameful annihilation at our hands. Hence I read articles which tally infinite acreages swallowed by subdivisions, which herald more and even more growth for Sacramento, and feel even more determined to stem the tide here in the Sierra, however possible.”

Russell Towle's journal


Birds and More Birds
[North Fork Trails blogpost, May 24, 2006:
http://northforktrails.blogspot.com/2006/05/birds-and-more-birds.html ]
Often over recent weeks I have wandered the woods near my home, tending to my various paths and trails, and watching the progress of the bloom. The Old Railroad Grade(s) up on top of Moody Ridge have proved an interesting challenge; I have mapped a few of them, but they have been so often cut by more recent logging roads, that it begins to take a healthy dose of imagination to see them at all. Ah, the old railroad grades.

But atop the ridge: In that crowded umpteenth-growth coniferous forest, often dominated by White Fir and Incense Cedar, there is quite an abundance of Rattlesnake Orchids, not in bloom yet, and not much to write home about when they are in bloom; but their patterned dark-green leaves, veined in cream, are spectacular.

Rattlesnake Orchid
(Goodyera oblongifolia)
There are some amazing ecotones in this area, dramatic contrasts in microclimate, soils, and therefore, vegetation and all that depends upon vegetation.

For instance, the uplands atop Moody Ridge, mostly a remnant of the once universal andesitic mudflow plateau which preceded incision of our canyons, these uplands receive sixty inches of rain per year, have deep soils, and support heavy coniferous forest.

But so soon as one drops onto the south-facing canyon wall, overlooking Green Valley, the forest becomes a mixture of Kellogg's Black Oak and Ponderosa Pine, with a scattering of Douglas Fir, especially as an understory, and also more riparian species like California Ginseng, White Alder, Maple, Dogwood, etc., around springs and seeps.

For, the volcanic strata capping the ridge are horizontal, some layers being quite permeable, others not, and that sixty inches of rain soaks down to impermeable layers and then slowly finds its way to the sides, emerging as springs, or maybe just wetting a generalized area, so that of a sudden there are many more maples and dogwoods than is usual.

I attribute the change from near-pure coniferous forest, into oak-pine woodland, as a function of fire. Over the long term, fires will burn hotter and more destructively on these steep slopes, than in the uplands. These fires have delicately groomed and managed the forest for thousands of years. If all fires were suppressed, this same mixed oak and pine woodland would become a Douglas Fir forest; which it is trying to do, right now. The Douglas Fir which sprouted after the last fire (ca. 1955) are now thirty to fifty feet tall, and more. They will shade out the oaks and pines, given a few centuries without fire.

The Black Oak-Ponderosa Pine woodland of the uppermost canyon walls ends at a razor-sharp boundary at the roughly horizontal contact between the young volcanics, above, and the ancient bedrock, below. This bedrock is serpentine of the Melones Fault Zone. Many plants cannot tolerate serpentine; Black Oak and Ponderosa Pines are good examples. From miles away one can see this abrupt shift in vegetation. Below, in the serpentine, is all manner of brush, and quite a lot in the way of Canyon Live Oak and Bay Laurel (tho somewhat stunted).

Now I have reached my birds.

It happens that every year, Black-Headed Grosbeaks arrive here in the Black Oak woodland, at the exact time these deciduous oaks break their buds and unfold their new leaves. These grosbeaks sing their hearts out for weeks on end, in a sweet fluty warbling which reminds me strongly of the Robin.

The grosbeaks begin singing at first light, more than an hour before dawn. That is when I usually rise and have my first cup of coffee, now as in 1976, when I first became aware of this species; I camped for months, right here in the oak woods, then.

Ah, the Black-Headed Grosbeak; the grosbeak, and young love!

Love! Love, and the Grosbeak, you say?

Oh yes. It is quite a sad story; I rescued a baby Grosbeak, fallen unfledged from its nest, and took it across Moody Ridge to the Sons of Norway camp, to My Beloved—to be saved, to be nurtured, and at last to be given freedom, once its wings were feathered. This one little bird, shivering, alone, would be the Symbol of My Beloved!

Of course, it died. Actually, one of her other boyfriends thought it was ready to fly; and who could have foreseen, that the cat was waiting? Thus may bright dreams fall into confusion, and amid the general chaos, a young bird dies.

Ah well, that was then, this is now.

The Grosbeaks arrive, and fill the forest with song, at first, all day long, and then, after a couple weeks, as they sit their nests, they quiet somewhat, and only the few hours near dawn and sunset are blessed by their incredibly sweet voices.

That is about how it is right now, at 4000 feet elevation, on a south-facing slope, in the northern Sierra.

I rarely see their nests, and assume them to be high in the Black Oaks, and hidden from human sight; later in the summer I will suddenly notice a twiggy nest here or there, and never be quite sure whose it was.

The other day, returning from the Railroad Trail, I was lopping a pesky little Canyon Live Oak beside a monstrous old Ponderosa. The little live oak was encroaching upon my trail. One side branch fell away under my attack, and then I saw the nest, at waist height, in the dense spiny foliage typical of the young Canyon Live Oak.

I was about to call my friend over, but then to my amazement I (finally!) saw that a bird was sitting her eggs, a streaky plump Grosbeak female. I walked quickly away.

This surprised me. These birds seem so closely tied to the Black Oaks, I never considered they might nest elsewhere.

A day later, I found a second Grosbeak nest directly above the same trail, eight feet above the ground, also in Canyon Live Oak, and also admitting a view directly into the nest (from the hillside above).

It begins to look as tho these Grosbeaks often nest near the ground.

This morning, watching a raft of clouds slowly light up from beneath while the sun broke free from yet other clouds to the east, I heard what I took to be an especially bold series of yelps from a Red-Shafted Flicker. From the Flicker's red feathers the Indians of Central California were wont to make headdresses, for their dances, which would trail to the ground itself, the feathers sewn crosswise into long bands.

A dark crow-sized bird alighted on an oak outside my window, and so soon as I saw its red crest I knew I had a Pileated Woodpecker at hand. I grabbed my camera and stepped cautiously to the door, just as the Pileated made a swoop to another larger oak, nearby. One picture, two, three, none good. The bird flew west and out of view and I hurried in that direction, collaring my daughter en route and whispering urgently of strange woodpeckers in the woods.

These big woodpeckers are not all that rare, but it had been ten years since I'd seen one. They chop out huge holes in rotten tree trunks and branches, with loud hammering sounds which can be heard from quite a distance. We scanned a grove of tall Ponderosa and Douglas Fir: a squirrel, but nothing else.

Then the chopping began.

It was so loud, I expected to spot the thing immediately; but it took a minute to locate him, high in a Black Oak, digging deeply into a dead branch. I took ten photographs and not one came out well.

Googling "Pileated Woodpeacker" + "Placer County" I turned up this interesting missive, apparently from the (birding magazine) the Condor, in 1919. It had been badly OCR'd and I took time to correct many errors, but likely missed some. I am not sure whether to count the "large mountain lake" mentioned as one of the Loch Levens, or Fordyce.
THE Northern Pileated Woodpecker, while not rare, is such a wary bird that its nesting habits in California are but little known. In a search through our various publications dealing with such subjects we fail to find a record of the taking of a single set of eggs of this species in the State. It seems probable that there are fewer California taken eggs of this bird in collections than even eggs of the California Condor. Barlow (CONDOR, III, 1901, p. 163) records a nest with young birds at Fyffe on June 13, 1897. Sheldon (CONDOR, XX, 1907, p. 188) records a nest with young near Big Meadows, Plumas County. The date is not given but it is assumed to be early in July. This paper embraces a partial account of our joint studies of this species over a period of five years (1914 to 1918), and the final culmination of our efforts in the taking of two sets of the eggs. The region worked lies near Cisco, Placer County, California, and it seems probable that the same pair of birds was observed during the five-year period. While working among the dead and dying trees at the upper end of a large mountain lake in June of 1914 the loud cackle of this unique bird was frequently heard. The type of country appeared to be suitable for the residence of the bird and it was then determined to pay especial attention to this species when next we should visit the lake, it then being too late in the season for eggs. Some time was spent in watching the birds feed, as they tore and pried off large slabs of dead bark in their search for various grubs and insects.

In 1915 we reached Cisco early in June and at first opportunity searched for our birds. A hard climb took us to the top of the dividing ridge and a swift descent, to the shores of the lake. One of the first birds seen was the Pileated Woodpecker as it flew from a tree standing in deep water to the thick woods across the lake. We passed near this tree and hid in some brush near by to await the appearance of the bird. It shortly returned and made straight for the tree, alighting on the opposite side from that facing us. We watched several minutes and as the bird did not appear we approached nearer the tree and were chagrined to discover a large hole about twenty feet up, in plain view and on the side of the tree which had first been exposed to us. We clapped our hands and immediately the bird appeared at the hole and flew cackling away. The tree stood about fifteen feet from the shore of the lake and in about five feet of water. At its base the diameter was about eighteen inches, at the nest entrance about ten. The tree was a live aspen. The base was exceedingly slippery and altogether the examination of the nest presented difficulties. Floating near the shore was a long dead trunk with a projecting limb which we decided to use as a raft to approach the tree. We each made an attempt to reach the tree but on both trials the raft turned over and we each got an icy bath. Inasmuch as the hills were covered with snow and the temperature on that day was low we were not particularly pleased with the ducking. We decided the tree raft would not serve and accordingly we made a fast trip back to headquarters, covering the distance in less time than that taken in coming out.

We soon returned with some planks and a lot of spikes with which we made a good raft and succeeded in reaching the nest tree. By driving spikes in the trunk Wells reached the nest and drew out a small young fledgling. The appearance of this object, resembling a skinned Chipmunk instead of a large white egg, certainly disappointed us. The nest cavity was eighteen inches deep and six inches in diameter, while the entrance was three inches in width. The entire excavation had been made in live wood although there were plenty of large dead trees near by. After leaving the nest we watched the old birds, both of which came to the tree and were quite tame as they fed the young, which, by the way, were three in number. The old birds reminded us a great deal of a pair of Flickers in their general movements and manner.

Determining to obtain a set of eggs the following spring, a visit was made on May 19, 1916, to the same mountain lake. Conditions were found to be quite similar to those of the previous year, there being much snow on the ground. The arrival at the lake was made enjoyable by a view of the pair of Woodpeckers flying towards the woods from the same tree in which the nest was located the previous year. An examination of the old tree was made in double-quick time and resulted in finding a second hole located three feet higher up and on the opposite side of the tree. Although two weeks earlier this year than the last we were again doomed to disappointment, for the nest contained three newly hatched young and one unhatched egg. The young birds evidently remained in the nest for about thirty days as they were seen climbing about the trees on June 20. The following year (1917) the locality was visited on May 5 we being determined to get ahead of the birds this time. The season was more advanced than on the three previous years and but little snow was on the ground and the lake at this point had less than three feet of water in it. The Pileated Woodpeckers had abandoned the lake and were making their home in a tree located in the channel of a small stream which flowed into the lake and about three hundred yards from their former site. The nest was found to be about half completed. Visits were made to it on several occasions until May 26, but the birds were not seen again. Apparently they had moved out of the basin entirely, as they could not be located.

While spending the winter of 1917-1918 at Summit, Wells determined to make the most of his opportunities to study the Woodpeckers. Through several friends living at Cisco the birds were kept under observation throughout the winter. It was found that the birds seldom strayed as far as two or three miles from their lake and that only the one pair was in evidence. In 1918, the first attempt to locate the nest was made on May 2, by Wells in company with W. O. Flickinger. On nearing the lake several unfinished cavities were noted, so that the date for eggs seemed about right. There was but little snow on the ground and practically no water in the lake. A search was then made through the aspen grove which in former years had stood in its entirety in from two to seven or eight feet of water, with the result that Mr. Flickinger discovered a fresh hole forty feet up in a live aspen growing close to the lake shore. Enough chips lay at the base of the tree to indicate that the cavity must be nearly finished.

The birds were not in evidence; so the nest was examined. It was found to be completed, but contained no eggs. Allowing ten days for the birds to lay a complete set, the nest was visited again on May 12, by Wells and Flickinger. We had great confidence that on this trip we would finally get a set of this prince of woodpecker. When we reached the tree a smart rap on the trunk brought the old bird to the entrance with an anxious expression on her face and we knew this time that we would soon have the eggs. She flew a short distance away and was soon joined by her mate. We hid in the brush and waited about thirty minutes, when the female returned and entered the nest. We thus felt positive that the nest contained a full set of eggs, and Wells accordingly strapped on his irons and climbed the tree.

His exultant shout proclaimed that the eggs were there--a set of four fresh glossy eggs. The nest cavity was eighteen inches deep by about six in diameter, while the entrance was nearly four inches across. The nest was visited again on June 1 by both of us, and to our surprise we found that the birds had used the same cavity for a second set of eggs, four in number, which were three-quarters incubated. The short time intervening between the two sets shows that the birds did not lose any time after their first set was lost to them. The locality was again visited on June 30 and we found that the birds had finished another cavity about two hundred feet from the first tree and apparently the female was brooding a third set. We did not disturb the bird. and hope that she successfully raised her brood. Inasmuch as the lake contained no water at this point we made a careful search of the upper end of the basin with the result that twenty cavities in all were located in various trees in what is usually the lake or very close to its shores. Most of these cavities were in live aspens.

Apparently this pair of birds has nested here for a great many years, for although we have carefully worked the surrounding country for miles in every direction we have never discovered other birds or their cavities. Inasmuch as the food supply is abundant, and hunters rarely visit the region, it is assumed that the species is simply an extremely rare one for this portion of the Sierra Nevada. The two sets of eggs are identical in shape, size, and other characters. They are small for the bird, being but little larger than eggs of the Red-shafted Flicker. In their glossy surface, pyriform shape and hardness of shell they are distinctively eggs of the Picidae. The average measurements of the four eggs are about 1.29x0.99 inches.

Oakland, California, February 24, 1919.


Helicopters in Giant Gap
[North Fork Trails blogpost, May 24, 2008
http://northforktrails.blogspot.com/2008/05/helicopters-in-giant-gap.html ]
A year or so ago I found that it was impossible to convince the Placer County Sheriff's department that it should avoid Giant Gap with its helicopters, inasmuch as both Peregrine Falcons and Golden Eagles were actively nesting. The Sheriff's department seemed to think I was from Outer Space; what I asked was absurd.

Several times this spring the Sheriff helicopter has flown through Giant Gap.

Yesterday I received an email from Jan Cutts, District Ranger of the American River Ranger District, Tahoe National Forest (TNF), at Foresthill. Jan wrote:

"I want to let you know that in the next day or so there will be a helicopter operating in the North Fork American River drainage east of Giant Gap to remove trash from the Green Valley area. We have worked with our biologist regarding concerns with impacts to the Peregrine falcon in the Giant Gap area, and will be working with the helicopter to keep it as far away from the area as possible."

This was good news. I called Jan immediately and asked, which mess of garbage would they clean up? Were they going after all the garbage sites, or one, or what?

For years I have urged TNF to bring a helicopter in to the Euchre Bar and Green Valley areas, where huge and horrible accumulations of garbage exist, beyond, really, the capacity of hikers to simply carry up and out. I sent maps showing all these locations. My friends and I would volunteer to help pack it up for the helicopter cargo nets. However, there was never enough money in the TNF budget.

Well. Jan replied she did not know just what garbage site was being cleaned up, but that surely, any garbage taken out, whatsoever, was a good thing. I agreed, but wondered whether we could not expand the cleanup to include that especially horrid site, above Euchre Bar, on the North Fork of the North Fork of the American.

She advised me to contact Tom Madrigal of TNF, at the Foresthill office, and I immediately called, and left a message, but did not hear back.

Today, as advertised, a helicopter arrived in Green Valley. They appeared to be working on what I call Mexican Marijuana Growers' Camp #1, along the High Ditch, towards the east end of Green Valley. I could hear the thunder of the helicopter in the distance, grabbed my binoculars, and ran out to a cliff-top from which I can see much of Green Valley.

To my amazement, after spending quite a time in the east end of Green Valley, out of my view, the helicopter rose slowly westward, without any cargo net, and flew right through Giant Gap, perhaps 500 feet above the river, which is about as bad as it can get, so far as the nests of the falcons and eagles.

Needless to say, I was not pleased. I believe it was a National Guard helicopter. I would not be at all surprised if this garbage cleanup occurred under the auspices of the Drug Enforcement Agency, replete with special grants from the Bureau of Homeland Security, or whatever the blasted thing is called. For nothing happens nowadays without grants. Employees of one agency Coordinate Their Efforts with employees of some other agency, and this wonderful "coordination" could only happen thanks to a grant. It is the debacle of Hurricane Katrina, dragged out to an impossible degree, under an infinite recursion.