Grand Staircase National Monument
Location:
South/Central Utah
Elevation:
8.600 feet
ABOUT GRAND STAIRCASE NATIONAL MONUMENT
Grand Staircase National Monument is made up of geological formations spanning three steps or provinces: the Chocolate Cliffs, Vermilion Cliffs and White Cliffs. The Chocolate Cliff Province consists primarily of dark-colored (hence the name) Jurassic Navajo Sandstone, formed during a period when ancient dunes were preserved in an area with little vegetation. The Vermilion Cliffs cover the second tier and are composed of sedimentary rock, such as limestone and shale deposited by rivers during the Cretaceous period. Here one can find evidence of ancient sea organisms that lived millions of years ago. Finally, on top of all this sits the White Cliffs Province, also known as the Kaiparowits Plateau. This block of land is composed of Cretaceous-age sandstone, mudstone, and shale that have been partially eroded away by wind and water over time to form spectacular canyons and other geological features. The Kaiparowits Plateau also contains some remarkable fossils from the Late Cretaceous period, including dinosaur bones and large marine reptiles. Grand Staircase National Monument is an awe-inspiring geologic wonder, a must-see for any nature lover and one of the top places to visit in Zion.
GRAND STAIRCASE NATIONAL MONUMENT GEOLOGY
the Chocolate Cliffs
Located at the base of Grand Staircase National Monument, the Chocolate Cliffs are composed of dark-colored Jurassic Navajo Sandstone that was formed during a period when ancient dunes were preserved in an area with little vegetation. These sandstone buttes have been partially eroded away over time to create spectacular views and canyons.
the Vermilion Cliffs
Located between the Chocolate Cliff and White Cliff Provinces, the Vermilion Cliffs are composed of sedimentary rock such as limestone and shale that were deposited by rivers during the Cretaceous period. Here one can find evidence of ancient sea organisms that lived millions of years ago.
the white Cliffs
The White Cliffs Province is the most visible formation of Grand Staircase National Monument, located at its highest elevation. At over 8,000 feet above sea level, this area consists of white sandstone and mudstone that have been partially eroded away by wind and water over time to form spectacular canyons, buttes, hoodoos, and other geological features.
the grey cliffs
The Grey Cliffs are the third tier of Grand Staircase National Monument, located between the Chocolate and White Cliff Provinces. Here visitors can find gray-colored sandstone that has been partially eroded away by wind and water over time to form spectacular views and canyons.
the pink cliffs
The Pink Cliffs are composed of pink-colored sandstone that was formed during a period when ancient dunes were preserved in an area with little vegetation. These soft sandstone buttes have been partially eroded away over time to create stunning views and canyons. Hikers looking for a leisurely stroll should check out the Pink Cliffs Trail, which is perfect for a scenic afternoon walk or a picnic with friends and family.
The Paunsaugunt and Aquarius Plateaus
The Paunsaugunt Plateau was created approximately 10-20 million years ago by a tectonic uplift on the Colorado Plateau (which is the highest plateau in North America). The Paunsaugunt and Aquarius Plateaus are located at the western end of Grand Staircase National Monument. Here visitors can find fossilized marine life, petrified wood, and other geological features that provide insight into the ancient history of the region.
Nearby Guided activities
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15 East State Street, Orderville, Utah, 84758
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PLACES TO STAY NEAR ZION NATIONAL PARK AND GRAND STAIRCASE
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Twin Knolls Rd, Orderville, UT 84758