Yosemite Nature Notes · Volume 16, Number 9
September 1937
Vol. XVI September 1937 No. 9
THE PUBLICATION OF THE YOSEMITE NATURALIST DEPARTMENT AND THE YOSEMITE NATURAL HISTORY ASSOCIATION
Published Monthly Volume xvi September 1937 Number 9 Interesting Notes from the Whitney Guide Book By ELIZABETH FOOTE Field School, 1936 The Yosemite Valley is a unique "Cleft or Gorge in the Granite Peak of the Sierra Nevada Mountain,—known as the Yosemite Valley" and wonderful locality; it is an exceptional creation, and as such has been exceptionally provided for jointly by the Nation and the State, which had been set aside by signature of President Lincoln June 30, 1864, and accepted by California in 1866 to be held for public use, resort and recreation." —it has been made a National public park and placed under the charge of the State of California. Tremendously impressed by the natural features of the area, the group was shocked to find that a bill had been passed by the State Legislature deeding 320 acres of the Valley floor as indemnity to James Lamon and J. M. Hutchings, two early settlers—hence, our first paragraph.
"Let Californians beware how they make the name of their State a byword and reproach for all time, by trying to throw off and repudiate a noble task which they undertook to perform,—that of holding the Yosemite Valley as a place of public use, resort, and recreation, inalienable for all time."
Fortunately for future generations, Congress side-tracked confirmation of this action. The State later voted $60,000 to pay off the claims of the two home-steaders.
So, in righteous indignation, wrote a party of the Geological Survey of California sent out in the late 1860's to write a guide book to the Yosemite region. The party, under the leadership of J. D. Whitney, first State Geologist, spent the summers of 1866 and 1867 exploring and mapping the little known and inaccessible region. The Yosemite Guide Book published in 1870, was the result of the findings of the party made up of Messrs. Whitney, King, Bolander, Gardner, and Brinley, and concerned itself primarily with descriptions of the region, designed to aid and encourage the early tourist.
Politics threatened to invade Yosemite, and the group was particularly fearful that this virgin area might again pass into private ownership.
Travel facilities in 1870 appear primitive to moderns. Travelers who had already made the steamer trip from San Francisco to Stockton took their choice from the routes appearing in the mileage chart given in the Guide Book.
On wheels, Big Oak Flat 63, Coulterville 71, Mariposa 101½; Horseback, Big Oak Flat 44 1/4, Coulterville 48½, Mariposa 37 1/4; Total, Big Oak Flat 107 1/4, Coulterville 119 1/2, Mariposa 138 7/8.
A "round trip" was recommended, the tourist coming into the Valley by way of the Coulterville Trail and leaving by way of the Mariposa Trail. No road came closer to Yosemite than Mariposa. Ten days was the minimum a traveler should allow for the journey from San Francisco, and of this three days could be spent in the Valley, one in the Big Trees, the remaining six being spent in transit. Reassuring is the comment that "there is nothing in the trip which need excite alarm in even the most timid person, as the trails are nowhere dangerous, and it is always easy to dismount where the slope is too steep for riding with comfort to man or beast."
Victorian women were apparently far more adventurous than most literature of the period would have us believe, for the Guide Book bears several injunctions for the benefit of their sex. In discussing the "Mist Trail" the authors write : "The path up the side of the canon near the fall winds around and along a steeply sloping mountain-side, always wet with the spray, and consequently rather slippery in places. Ladies, however, find no great difficulty in passing, with the aid of friendly arms, and protected by stout boots and India-rubber clothing bought from the hotel." A note of warning is found here : "Persons who are not accustomed to climbing, and especially ladies, are strongly advised to ride out of the Valley on the regular trails, rather than risk getting over-fatigued in performing acrobatic feats, which are not at all necessary to enable one to see and enjoy the whole region."
Members of the party not only mapped Yosemite Valley, but by way of the Mono Trail, near the present Tioga Pass Road, made their way to Tuolumne Meadows, thence to Hetch Hetchy, to Little Yosemite, and finally to Glacier Point. Mainly for purposes of identifying peaks in their topographical study, they named several mountains, and reported that "the names thus given by us will be adopted by the civilized and scientific world abroad, however much our disinclination to bestow on prominent points the names of great politicians and
editors may be criticized in California." "We have selected for this purpose the names of explorers, surveyors, geographers, geologists, and engineers, and especially of such as have worked or lived in the region in which the point to be named was situated" and also the names of very eminent geographers, geologists, or physicists, who have labored successfully in general science, and whose results have thus become the property of the world." Mount Dana, Mount Lyell, and Mount Ritter are among the peaks thus named by the State Geological Survey. Many mountains in this area were climbed by the party, but their considered opinion of Half Dome was that it was "perfectly inaccessible, being probably the only one of all the prominent points about the Yosemite which never has been, and never will be, trod by human foot."
The Guide Book then discusses them in turn. First, the foothills growth, characterized by the Digger Pine (Pinus sabiniana), California Buckeye (Aesculus californica), and varieties of California Lilac (Ceanothus). From this, what is now called the Upper Sonoran Zone, the authors go on to accurately describe, although naturally not by these names, the Transition, Canadian, and Hudsonian Zones. Plant markers are given to identify each zone, and many of these are the ones recognized as most trustworthy today.
Geologically the party advanced a subsidence theory in explaining the formation of Yosemite Valley, and disposed of the glacial idea, now universally accepted, in this summary fashion. "Much less can it be supposed that the peculiar form of the Yosemite is due to the erosive action of ice. A more absurd theory was never advanced than that by which it was sought to ascribe to glaciers the sawing out of these vertical walls and the rounding of the domes. Nothing more unlike the real work of ice, as exhibited in the Alps, can be found. Besides, there is no reason to suppose, or at least no proof, that
The High Sierra excited the admiration of Whitney's group, and they went to some pains to compare it, point by point, with the Swiss Alps, commenting drily that : "There are probably ten times as many persons in California who have traveled for pleasure in Switzerland, as among these most interesting portions of the Sierra."
Scientifically, the purpose of the expedition was, of course, to make accurate maps of the area, which they did, but some time was obviously spent on the botany and geology of the region. It is well to note that here is one of the early
glaciers have ever occupied the Valley or any portion of it, so that this theory, based on entire ignorance of the whole subject, may be dropped without wasting any more time upon it."
And yet when the party visited Hetch Hetchy, which they termed "almost an exact counterpart of Yosemite" their report is that there is no doubt but what it was formed by glacial action.
It should be noted here that Clarence King, who had just joined the Whitney party as a student to earn his way, submitted a "minority" report disagreeing with his chief. He held that there were evidences of glaciation in Yosemite Valley and attributed much of the sculpturing effect to the work of ice. Clarence King later became first Director of the United States Geological Survey in 1867.
Whitney and his group also visited many of the groves of Big Trees, including the Mariposa Grove, in order to publish what they believed to be the first accurate account of the distribution, size, and age of this already widely publicized species. It was apparently largely a "debunking" mission, for many of the stories circulated about the giant Redwoods were considerably taller than the trees. Careful measurements of circumference and height were taken and published.
It is easy for us now to look at this old Guide Book, smile at what have proved to be scientific fallacies, be amused by the quaint tone and extravagant superlatives which pervade the text, and indeed be horrified by the lack of accommodations and transportation. But the men who wrote this book were among the last of our own pioneers and explorers, and not only did they serve well in this capacity, they were also men of vision. With the true spirit of Nature-lovers, they appreciated the wonders before them, and at the same time hoped and planned for the time when "hundreds, nay thousands" would come to Yosemite yearly to enjoy it without the cheapening atmosphere of the profitable amusement park. Fish Planting - An Adventure By Ranger-Naturalist Harold E. Perry Seldom does a Yosemite ranger-naturalist have the privilege of accompanying a fish planting expedition. His educational contacts with the park visitors are usually most numerous about the time that the work of planting fish is being done, so he has to get his information relative to this last and important phase of fish culture from one of the men in charge of the Yosemite Hatchery or from the ranger who supervises this work in the park.
There are exceptions to all rules, however, and my recent good fortune is an example, for I have just returned from a trip to Chowchilla Creek, some ten miles from Wawona, where I was privileged to assist Mr. Archie Thompson, Superintendent of the Yosemite Hatchery, and Mr. Ray Brewer in planting ten thousand Loch Leven trout.
These trout were hatched about four months ago from eggs which arrived March sixth from the Mt. Whitney Hatchery. This morning (July 21) they weighed approximately fifty to the ounce and one thousand trout, or twenty ounces, were weighed out for each of the ten fish transportation cans which were used in today's adventure. Each thousand trout unit was emptied into a ten gallon can containing six or seven gallons of water. Every can was covered with a burlap jacket. Ice was added to each container and before our departure, the burlap jackets were saturated with water as an additional aid in maintaining a lower water temperature within the cans, and it was noted with satisfaction that the trout were remaining at the bottoms of the cans,--proof that the water was adequately rich in oxygen. If at any time during the trip we had observed the trout rising to the surface of the water, it would have been necessary to aerate the water immediately, either by rocking the truck or by using a special, perforated can having a goose-neck pipe attached to it, by means of which it is possible to lift a quantity of water and allow it to pour back through the large perforations. No difficulty arising from lack of oxygen was encountered at any time during this trip. The baby trout were apparently very healthy and they seemed to stand the trip satisfactorily.
By eight forty we were on our way. Because of smooth road conditions between Yosemite Valley and Wawona, the fore part of the trip was made quite rapidly in an effort to reach quickly the rougher road over Chowchilla Mountain where the jerking of the truck would agitate the water sufficiently to aerate it constantly. At Wawona ice was again added to the water.
When Chowchilla Creek was reached at a point ten miles from Wawona, plantings were made in three rather widely separated areas. At each stop, the fish to be planted were emptied into a special pail which had two screen insertions on opposite sides near the top to allow surplus water to escape without loss of fish. From this special pail, the trout were emptied into other pails which could be carried conveniently to the stream's edge.
The water in Chowchilla Creek was somewhat warmer than that in which the fish had been transported so before the actual planting was made at each stop, it was necessary to equalize those temperatures.
This was done by adding stream water to the pails until equalization was accomplished. Then the baby trout were liberated, a few at a time, in the quiet pools along the edge of Chowchilla Creek, a creek which we saw adorned with the showy blossoms of columbines, scarlet monkey flowers and leopard lilies and with a charming display of the delicate rein-orchis.
Almost immediately, the tiny trout began to distribute themselves along the stream. The stronger, more rugged ones felt the edge of the current and were soon seeking adventure in an upstream direction. The weaker ones were frequently caught by the moving water to be carried to pools farther down where in quieter waters they will no doubt recuperate from the effects of their long journey. All were hungry because of an enforced fast during the preceding twenty-four hours. Their desire for food will do much in assisting them to adjust themselves to their new home.
There is a story of human effort and achievement behind those baby trout, a story which began in the higher mountains of the Sierra where adult trout were trapped enroute to their spawning areas, and where they were stripped of the eggs and milt which made today's adventure possible. Another stream has been restocked with trout which will bring an abundance of satisfaction to an unknown number of patient anglers for many fishing seasons to come, and a grateful ranger-naturalist has been able to enrich his background of experience in the fascinating study of fish culture.
Water Ouzels at Home Ranger-Naturalist M. D. Bryant I left Mirror Lake on the morning of June 15 with a regular group of all-day hikers to explore the rugged beauty of Tenaya Canyon. The churning waters of Snow Creek altered our plans. The heavy snows of the past winter were melting rapidly and the water was too high for a safe crossing. Finding that we could not cross the creek we walked to the foot of the falls, enjoyed the wild scramble of the waters for a time, and then started on our way down. Shortly thereafter a slate-gray flash of a bird caught my eye. It flew upstream, scarcely a foot above the water, and suddenly disappeared in the spray. I climbed over a large boulder, balanced on a projecting rock, bent as low as I could, and was rewarded with a splendid observation of Water Ouzels at home.
I have seen nests of Water Ouzels in many situations. One was attached to the vertical surface of a boulder on the Merced River, one was above a fall on the Lyell Fork of the Merced River, one was on a shallow shelf many feet above Tenaya Creek. I have heard of the birds nesting in a spray-splashed fallen log near the base of the Lower Yosemite Fall. Although these nesting sites are in many cases unusual, I feel that the one discovered on Snow Creek merits special attention. The nest is fifty yards below the base of the falls and about twenty feet to the right of the trail leading up to the observation boulder. It is under a small overhanging ledge and is about two feet back from the margin. The water divides a short distance upstream from the ledge. A portion comes over the western half of the ledge in a miniature fall and the major part rushes past the eastern edge. The roof and walls of the nest are composed of moss and are in good condition. Bare granite forms the floor. The nest seems to have been used before and must have been constructed when the water was lower than now. Since the nest is constantly drenched by the spray blown from the tiny fall, the eggs must have been incubated and the young reared under conditions that would have spelled doom to most birds.
The parents were not at all frightened by my nearness and continued to make their hurried excursions downstream in search of food for the young. Both followed the same ritual in taking the food to the young. They would fly upstream with larvae in their bills, light on a nearby rock for a momentary survey of the surroundings, fly between the two streams of water, perch on the rock under the fall, shake the water from the feathers, pull the white nictitating
membrane over the eye a time or so, and present the food to the gaping mouths of the young birds in the nest.
The members of the hiking party also had the opportunity to take part in the study and we returned to Mirror Lake feeling that the time had been well spent even though our original plans had gone astray.
It was indeed an unusual opportunity, perhaps even a new altitude record as the highest one reported in Grinnell and Storer's Animal Life in Yosemite was on a pass, 700 feet in altitude near Ten Lakes, on October 11, 1915.
WESTERN MEADOWLARK ON HALF DOME
By F. Wallace Taber, Field School '37 Although quite common at lower elevations, it is a rare occasion when a Meadowlark is observed at elevations as high as that of Half Dome, 9,930 feet. On June 27, about 12:30 noon, Bill Richardson, Bob Waste and the writer were walking around on top of Half Dome when a Meadowlark was flushed from behind a small granite ledge. It took to the air about 20 feet in front of us, circled, and flew out of sight over the edge of the cliff to the northeast, out over the valley proper. Its characteristic fluttering flight and bright pattern easily distinguished it as a Western Meadowlark. Although the quick tailspreads were numerous, revealing the lighter outer tail feathers, the usual accompanying "chucks" were absent, and the bird went away songless. Nevertheless, its identity was certain and all the party agreed that Meadowlarks are rare in Yosemite. It is interesting to speculate upon the cause of the bird's appearance. Meadowlarks are not known to be migratory, so the bird observed could not have stopped in migration. Seeds and insects are relatively scarce so undoubtedly food was not the cause of its presence. At this time of year, Meadowlarks are beginning to form flocks, so another question arises as to why the bird was alone. All these points are of interest, but of equal interest is the fact that less than two hundred yards farther down a Sierra Nevada Rosy Finch was observed feeding.
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