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Checkerboard Mesa is an iconic 6,520+ ft (1,990+ m) elevation Navajo Sandstone summit located in Zion National Park, in Kane County of southwest Utah, United States. [3] Checkerboard Mesa is situated immediately southwest of the park's east entrance, towering 900 feet (270 meters) above the Zion – Mount Carmel Highway .
The geology of the Zion and Kolob canyons area includes nine known exposed formations, ... The crosshatched appearance of Checkerboard Mesa is a good example .
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.
The geology of the Zion and Kolob canyons area includes 9 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.
View from Utah Highway 12 of Grand Staircase–Escalante National Monument The Cockscomb at right runs along Cottonwood Canyon Road. The Grand Staircase is an immense sequence of sedimentary rock layers that stretch south from Bryce Canyon National Park and Grand Staircase–Escalante National Monument, through Zion National Park, and into Grand Canyon National Park.
Navajo Sandstone. The Navajo Sandstone is a geological formation in the Glen Canyon Group that is spread across the U.S. states of southern Nevada, northern Arizona, northwest Colorado, and Utah as part of the Colorado Plateau province of the United States. [2]
In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original depositional layering is tilted, such tilting not being the result of post-depositional deformation.
Geology of the Canyonlands area. Shafer Canyon Overlook, Canyonlands. The geology of the park is the consequence of deposition, uplift and erosion. Island in the Sky is a mesa overlooking the Green River (Colorado River tributary) to the west and the Colorado River to the east, and separated from the Colorado Plateau by the "the neck".