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Zion National Park is a national park of the United States located in southwestern Utah near the town of Springdale. Located at the junction of the Colorado Plateau , Great Basin , and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity.
It is a well-known rock formation in the park, named for its distinct shape. One side is a sheer face while the other three sides are smooth and round, making it appear like a dome cut in half. It stands at nearly 8,800 feet above sea level and is composed of quartz monzonite, an igneous rock that solidified several thousand feet within the Earth.
The Grand Staircase is an immense sequence of sedimentary rock layers that stretch south from Bryce Canyon National Park through Zion National Park and into the Grand Canyon. Within this sequence, the oldest exposed formation in the Zion and Kolob canyons area is the youngest exposed formation in the Grand Canyon—the Kaibab limestone. [2]
There is one hotel inside the park, Zion National Park Lodge, which is operated by a third-party concessionaire and open year-round. There are also three campgrounds : Watchman, South and Lava Point.
Angels Landing, known previously as the Temple of Aeolus, is a 1,488-foot (454 m) tall rock formation [2] in Zion National Park in southwestern Utah, United States.A renowned trail cut into solid rock in 1926 leads to the top of Angels Landing and provides panoramic views of Zion Canyon.
Geology showing the basal layer (Kaibab Formation) of Zion National Park, southern Utah. The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast California. It is also known as the Kaibab Formation in
Clockwise from upper left: Sedona, Grand Canyon National Park, Barringer Crater, Petrified Forest National Park The geology of Arizona began to form in the Precambrian . Igneous and metamorphic crystalline basement rock may have been much older, but was overwritten during the Yavapai and Mazatzal orogenies in the Proterozoic .
Half Dome, a quartz monzonite monolith in Yosemite National Park and part of the Sierra Nevada Batholith. A batholith (from Ancient Greek bathos 'depth' and lithos 'rock') is a large mass of intrusive igneous rock (also called plutonic rock), larger than 100 km 2 (40 sq mi) in area, [1] that forms from cooled magma deep in the Earth's crust.