UT -- Zion Natl Park:
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- Specific picture descriptions: Photos above with "i" icons next to the bracketed sequence numbers (e.g. "[1] ") are described as follows:
- ZION_060607_004.JPG: Patterns in Stone: Checkerboard Mesa:
The Navajo sandstone before you also forms the spectacular cliffs within Zion. This geographically widespread formation reaches a thickness of 2,200 feet in the park and consists almost entirely of desert sand dunes. The Checkerboard Mesa, made of Navajo sandstone, has two sets of lines forming the checkerboard pattern.
The horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that builds up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Crossbedding can also be seen in many places along the Zion Mt. Carmel Highway.
The vertical lines are less common. They are actually shallow cracks that result from stress and erosion on the rock surface. These cracks are probably caused by expansion and contraction, temperature changes, wetting/drying, or a combination of these processes.
- ZION_060607_242.JPG: This is one end of the tunnel that goes through the cliffs later
- ZION_060607_372.JPG: This picture identifies the features that you'll see in a later picture of the valley.
- ZION_060607_590.JPG: [Note the hole in the mountain wall. The tunnel runs behind it.]
Impassable Barrier:
In the 1920s, this end of the canyon appeared to be a dead end, an impassable barrier to transportation. To highway engineers, the toughest challenge was the cliff above. Their solution: a one-mile tunnel behind the cliff face.
When tunnel and highway were completed in 1930, they opened the region to motor tourism, linking Zion to Bryce and the Grand Canyon's North Rim. Now the tunnel itself has become a kind of barrier, as today's RVs and tour buses are too large for two-way traffic within the tunnel. Expect short delays as oncoming traffic is held to allow oversize vehicles to pass through.
- ZION_060607_676.JPG: Zion National Park
- AAA "Gem": AAA considers this location to be a "must see" point of interest. To see pictures of other areas that AAA considers to be Gems, click here.
- Wikipedia Description: Zion National Park
From Wikipedia, the free encyclopedia
Zion National Park is a United States National Park located in the Southwestern United States, near Springdale, Utah. A prominent feature of the 229-square-mile (593 kmē) park is Zion Canyon, 15 miles (24 km) long and up to half a mile (800 m) deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, this unique geography and variety of life zones allow for unusual plant and animal diversity. A total of 289 bird species, 75 mammals (including 19 species of bat), 32 reptiles and numerous plant species inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Notable megafauna include Mountain Lions, Mule Deer and Golden Eagles, along with reintroduced California Condors and Bighorn Sheep. Common plant species include Cottonwood, Cactus, Datura, Juniper, Pine, Boxelder, Sagebrush and various willows.
Human habitation of the area started about 8,000 years ago with small family groups of Native Americans; the semi-nomadic Basketmaker Anasazi (300 CE) stem from one of these groups. In turn, the Virgin Anasazi culture (500 CE) developed as the Basketmakers settled in permanent communities. A different group, the Parowan Fremont, lived in the area as well. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. The canyon was discovered by Mormons in 1858 and was settled by that same group in the early 1860s. Mukuntuweap National Monument was established in 1909 to protect the canyon, and by 1919 the monument was expanded to become Zion National Park (Zion is an ancient Hebrew word meaning a place of refuge or sanctuary). The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the park in 1956.
The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time, warm, shallow seas, streams, ponds and lakes, vast deserts and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago.
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I still have them though. If you want me to email them to you, please send an email to guthrie.bruce@gmail.com
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