Backpacking
Zion National Park
March 31, 1988UTAH: Washington & Kane Counties Backpacking the eastern side of Zion National Park |
At 2:00 PM I begin walking north from the East Entrance Trailhead. It's very windy, partly cloudy and the temperature is 64°. APRIL 16:30 AM. Camped at Stave Spring, at an elevation of about 7000 feet. With very little wind the sky is clear and the temperature is 22°. Between 7:00 and l0:00 AM I walk from Stave Spring to Deertrap Mountain Overlook. Here are the birds I see, in the order in which they appear:
At l0:00 AM as I descend a steep slope a Least Chipmunk, Eutamias minimus, postures atop a large sandstone boulder. The Least is similar to the Eastern chipmunk, but smaller, without so much rusty coloration, and the two white lines on its face are more conspicuous. This individual lets me come so close that I suspect it of a history of panhandling nuts and trail mix from backpackers. At 11:35 four Western Bluebirds fly by. At 3:00 PM, passing from one mesa top to another, a thousand feet above the canyon floor a male Northern Harrier, or Marsh Hawk, has a hard time with the wind. I'm used to seeing this bird sailing calmly and low over marshes and grasslands. Its presence here is hard for my Eastern headset to adjust to. APRIL 2Having camped overnight at Cable Mountain Overlook (elevation 6496 feet), with my tent pegged right at the edge of the cliff overlooking the stomach-churning abyss known as Zion Canyon, now let me tell you about the trees found within twenty feet ponderosaof my tent.
APRIL 3Today I walk from Cable Mountain back to Henry; let me better describe the topography I've been walking through. A few million years ago the topography here was fairly level but at the end of the late Tertiary Period, about ten million years ago, the entire Zion region was uplifted from near sea level to about 10,000 feet above sea level. This uplifting imparted to the region's streams immense potential energy for erosion. The Virgin River and its tributaries became moving ribbons of sandpaper that scoured out deep canyons for themselves. This erosional process has proceeded so fast that the land between the water courses simply hasn't had time to erode into a typical rolling landscape. Thus the flatish mesa-tops I've been walking over are perched remnants of a flatish, ancient landscape. Sometimes the mesa-tops' junipers and pines yield to broad fields dominated by Sagebrush. Sagebrush seen in Nevada seldom grew over knee high but here sometimes it's ten feet tall, with gnarled, gray trunks, reminding me of gigantic Japanese bonsai. These features are especially surprising when it's remembered that Sagebrush is a member of the Composite or Daisy Family. In the East, at least, this family is almost entirely represented by non-woody, herbaceous species such as asters, goldenrods and dandelions. Sagebrush is very closely related (same genus) to wormwood, the super-odoriferous, yarrow-leaved weed that grows in rich soil around barns. It seems that in the Great Basin Desert Sagebrush takes the place of Creosote-bush as the most ubiquitous species of desert habitats. During our entire trip Creosote-bush has been such a constant companion that leaving it behind now seems almost unthinkable. However, if Creosote-bush must be replaced by something, Sagebrush is a worthy candidate. |
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