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Canyonlands National Park, in southeastern Utah, encompasses deeply<br />

eroded canyons peppered with sheer-sided mesas and a variety of<br />

spires, arches and unusual rock formations. The Green and Colorado<br />

rivers meet and continue in a series of powerful rapids through the<br />

multicolored recesses of Cataract Canyon. The park has numerous<br />

opportunities for back country hiking and travel by four-wheel-drive<br />

vehicle, mountain bike, horse, canoe, kayak, or white-water raft.<br />

Capitol Reef National Park, Utah<br />

Named for reef-like cliffs capped by white sandstone formations resembling<br />

the U.S. Capitol, the park contains a sensational section of the<br />

Waterpocket Fold. The fold stretches approximately 100 miles southeastward<br />

from Thousand Lake Mountain to Lake Powell and graphically<br />

illustrates the way the Earth’s surface was built, folded and eroded.<br />

Numerous eroded basins or “pockets” that can hold thousands of<br />

gallons of rainwater are held in this uprising. Near the visitor center,<br />

brightly tinted tiered cliffs-called sleeping rainbows by the Navajosrise<br />

1,000 feet above the Fremont River. Pre-Columbian Indian petroglyphs<br />

can be seen on the encompassing canyon walls. In the midst of<br />

Capitol Reef’s red rock are orchards where fruit may be harvested in<br />

season.<br />

Carlsbad Caverns National Park, New Mexico<br />

Carlsbad Caverns National Park lies at the rugged base of the<br />

Guadalupe Mountains. Located its 73 square miles is Carlsbad Cavern, a<br />

series of enormous rooms that form one of the world’s largest caves.<br />

The cavern was created in a limestone reef by percolating ground<br />

water, thought to have begun some 3 to 5 million years ago.<br />

Attractive effects range from small, delicate growths resembling plants<br />

to massive stalagmites, stalactites and columns. Many are dyed by iron<br />

and other minerals in the limestone. A marvel occurs each evening at<br />

dusk from approximately May through October, when bats emerge from<br />

the uppermost chamber of the cavern. Winding through the entrance,<br />

they pour southward over the rim, later to disperse in search of food.<br />

The flight outward may last up to an hour, the mass of bats return<br />

near dawn. The number of bats changes with the availability of nightflying<br />

insects upon which they feed. When insects are abundant nearly<br />

a million bats may be present. During the day they hang head down<br />

from the walls and ceilings in a portion of the cavern closed to visitors.<br />

Crater Lake National Park, Oregon<br />

On the crest of the Cascade Range, Crater Lake National Park is known<br />

for its natural beauty. The most extraordinary feature is Crater Lake,<br />

outstanding for its deep, brilliant blue color. The lake is 6 miles long,<br />

4 ½ miles wide and 1,932 feet deep. Its 20 mile shoreline is encircled<br />

by lava cliffs that rise 500 to 2,000 feet over the lake. Many years<br />

ago, Mount Mazama, a 12,000-foot volcano, occupied the site of Crater<br />

Lake. Vicious eruptions emptied the magma chamber beneath the<br />

mountain and caused the mountain top to collapse, creating the<br />

caldera which now contains the lake. Including three zones of vegetation,<br />

the park has more than 570 species of plants and a variety of<br />

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