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Frommer's Las Vegas 2004

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RED ROCK CANYON 287<br />

believed were weapons of the wolf god Shinarav, can be viewed in the Chinle Formation<br />

at the base of the Red Rock Cliffs. About 100 million years ago, massive<br />

fault action began dramatically shifting the rock landscape here, forming spectacular<br />

limestone and sandstone cliffs and rugged canyons punctuated by waterfalls,<br />

shallow streams, and serene oasis pools. Especially notable is the Keystone Thrust<br />

Fault, dating back about 65 million years when two of the earth’s crustal plates<br />

collided, forcing older limestone and dolomite plates from the ancient seas over<br />

younger red and white sandstones. Over the years, water and wind have been evercreative<br />

sculptors, continuing to redefine this strikingly beautiful landscape.<br />

Red Rock’s valley is home to more than 45 species of mammals, about 100<br />

species of birds, 30 reptiles and amphibians, and an abundance of plant life.<br />

Ascending the slopes from the valley, you’ll see cactus and creosote bushes, aromatic<br />

purple sage, yellow-flowering blackbrush, yucca and Joshua trees, and, at<br />

higher elevations, clusters of forest-green piñon, juniper, and ponderosa pines.<br />

In spring, the desert blooms with extraordinary wildflowers.<br />

Archaeological studies of Red Rock have turned up pottery fragments, stone<br />

tools, pictographs (rock drawings), and petroglyphs (rock etchings), along with<br />

other ancient artifacts. They show that humans have been in this region since<br />

about 3000 B.C. (some experts say as early as 10,000 B.C.). You can still see<br />

remains of early inhabitants on hiking expeditions in the park. (As for habitation<br />

of Red Rock, the same Anasazi-to-Paiutes-to-white-settlers progression<br />

related in the Valley of Fire section above occurred here.)<br />

In the latter part of the 19th century, Red Rock was a mining site and later a<br />

sandstone quarry that provided materials for many buildings in Los Angeles, San<br />

Francisco, and early <strong>Las</strong> <strong>Vegas</strong>. By the end of World War II, as <strong>Las</strong> <strong>Vegas</strong> developed,<br />

many people became aware of the importance of preserving the canyon.<br />

In 1967 the Secretary of the Interior designated 62,000 acres as Red Rock<br />

Canyon Recreation Lands under the auspices of the Bureau of Land Management,<br />

and later legislation banned all development except hiking trails and limited<br />

recreational facilities. In 1990, Red Rock Canyon became a National<br />

Conservation Area, further elevating its protected status. Its current acreage is<br />

197,000.<br />

WHAT TO SEE & DO<br />

Begin with a stop at the visitor center; not only is there a $5 per-vehicle fee to<br />

pay, but you can pick up a variety of helpful literature: history, guides, hiking<br />

trail maps, and lists of local flora and fauna. You can also view exhibits that tell<br />

the history of the canyon and depict its plant and animal life. You’ll see a fascinating<br />

video here about Nevada’s thousands of wild horses and burros, protected<br />

by an act of Congress since 1971. Furthermore, you can obtain permits for hiking<br />

and backpacking. Call ahead to find out about ranger-guided tours as well<br />

as informative guided hikes offered by groups like the Sierra Club and the<br />

Audubon Society. And, if you’re traveling with children, ask about the free<br />

Junior Ranger Discovery Book filled with fun family activities. Books and videotapes<br />

are on sale here, including a guidebook identifying more than 100 toprated<br />

climbing sites.<br />

The easiest thing to do is to drive the 13-mile scenic loop . It really is a<br />

loop and it only goes one way, so once you start you are committed to driving<br />

the whole thing. You can stop the car to admire any number of fabulous views<br />

and sights along the way, or have a picnic, or take a walk or hike. As you drive,<br />

observe how dramatically the milky-white limestone alternates with iron-rich

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