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THE M A G A Z I N E - Desert Magazine of the Southwest

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lue limestone underlain by white quartzite. The blue limestone<br />

has wea<strong>the</strong>red to form huge pinnacles. Above this wall<br />

<strong>of</strong> limestone, what might be called <strong>the</strong> Upper Hidden Forest<br />

canyon extends several miles, ending at <strong>the</strong> foot <strong>of</strong> Hayford<br />

peak at a point nor<strong>the</strong>ast <strong>of</strong> <strong>the</strong> o<strong>the</strong>r canyon. Hayford, known<br />

to <strong>the</strong> old-timers as Niggerhead peak, is <strong>the</strong> highest mountain<br />

in <strong>the</strong> Sheep range, having an elevation <strong>of</strong> 9,730 feet.<br />

<strong>Southwest</strong> <strong>of</strong> Hidden Forest canyon, Sheep peak towers to an<br />

elevation <strong>of</strong> 9,706 feet.<br />

On <strong>the</strong> north wall <strong>of</strong> <strong>the</strong> canyon great outcroppings <strong>of</strong> limestone<br />

and conglomerate occur. The tops <strong>of</strong> <strong>the</strong> peaks are mainly<br />

<strong>of</strong> badly jointed and wea<strong>the</strong>red blue limestone, although a<br />

few are <strong>of</strong> sandstone. Between Sheep peak and Hayford peak<br />

<strong>the</strong> country is badly faulted. Some <strong>of</strong> <strong>the</strong> strata are tilted to<br />

nearly vertical position while o<strong>the</strong>rs are practically horizontal.<br />

The vertical outcroppings are found high on <strong>the</strong> west bank <strong>of</strong> a<br />

canyon leading <strong>of</strong>f to <strong>the</strong> northwest <strong>of</strong> <strong>the</strong> Hidden Forest<br />

canyon. Higher on this same bank, <strong>the</strong> limestone takes on <strong>the</strong><br />

shape <strong>of</strong> a huge wall, on which <strong>the</strong> corners have been<br />

wea<strong>the</strong>red round and many caves have been developed. In<br />

one place a natural bridge has been formed. Under <strong>the</strong> north<br />

end <strong>of</strong> <strong>the</strong> bridge is a large cave with stalactites hanging from<br />

<strong>the</strong> ceiling and stalagmites on <strong>the</strong> floor. The bridge was<br />

formed by <strong>the</strong> collapsing ro<strong>of</strong> <strong>of</strong> a limestone cave, leaving a<br />

portion still standing to form <strong>the</strong> arch. To <strong>the</strong> south and west<br />

is an outcropping <strong>of</strong> conglomerate <strong>of</strong> sandstone, quartzite, and<br />

blue limestone. Below this to <strong>the</strong> south is ano<strong>the</strong>r outcropping<br />

<strong>of</strong> limestone with a number <strong>of</strong> caves, in front <strong>of</strong> which are<br />

<strong>the</strong> remains <strong>of</strong> crude shelters evidently built by <strong>the</strong> Indians<br />

who inhabited this region hundreds <strong>of</strong> years ago. Inside <strong>the</strong><br />

caves we found charred wood.<br />

Quest for Indian Sun Temple<br />

Following our discovery <strong>of</strong> <strong>the</strong> evidence <strong>of</strong> prehistoric cave<br />

dwellers, <strong>the</strong> mystery <strong>of</strong> <strong>the</strong> so-called Indian Sun Temple<br />

again became uppermost in our minds. A short distance northwest<br />

<strong>of</strong> <strong>the</strong> Indian caves we came upon a natural amphi<strong>the</strong>ater<br />

carved out <strong>of</strong> <strong>the</strong> rocks. The formation is high above <strong>the</strong> canyon<br />

floor and is in <strong>the</strong> shape <strong>of</strong> a large crescent with vertical<br />

7 5-foot walls. Inside <strong>of</strong> <strong>the</strong> crescent and extending down to<br />

<strong>the</strong> floor <strong>of</strong> <strong>the</strong> canyon, great quantities <strong>of</strong> broken rocks cover<br />

<strong>the</strong> mountain sides. This amphi<strong>the</strong>ater was formed by<br />

<strong>the</strong> breaking <strong>of</strong>f <strong>of</strong> portions <strong>of</strong> <strong>the</strong> wall, leaving <strong>the</strong> crescentshaped<br />

structure <strong>of</strong> red, yellow and white sandstone. One<br />

might imagine this to have been a natural temple <strong>of</strong> sun worship.<br />

There is no evidence that <strong>the</strong> place was ever frequented<br />

by <strong>the</strong> Indians, however.<br />

Although snow can be found in <strong>the</strong> sheltered places nearly<br />

all year, <strong>the</strong>re is no running water in Hidden Forest. A small<br />

spring is located about a hundred yards northwest <strong>of</strong> <strong>the</strong> end<br />

<strong>of</strong> <strong>the</strong> road where <strong>the</strong> canyon divides. Motorists going into<br />

this area should carry plenty <strong>of</strong> water and should also be<br />

equipped with shovel and axe. Fire precautions are especially<br />

important here. This area is too fine to be despoiled by careless<br />

humans.<br />

As Jim and I stood on <strong>the</strong> jagged ridge midway between<br />

Hayford peak and Sheep peak, we could see below us <strong>the</strong> full<br />

extent <strong>of</strong> <strong>the</strong> Hidden Forest canyon with its many varieties <strong>of</strong><br />

trees. In <strong>the</strong> late afternoon <strong>the</strong> outcropping pinnacles <strong>of</strong> rock<br />

cast queerly shaped shadows across <strong>the</strong> canyon walls. The deep<br />

silence is broken only by <strong>the</strong> calls <strong>of</strong> <strong>the</strong> birds and <strong>the</strong> whisper<br />

<strong>of</strong> wind in <strong>the</strong> pines. There is peace and mystery in <strong>the</strong> solitude<br />

<strong>of</strong> this remote forest-oasis in <strong>the</strong> Nevada mountains.<br />

NOVEMBER, 1938 15

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