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The Grand Staircase is an immense sequence of sedimentary rock layers that stretches south from Bryce Canyon National Park and Grand Staircase–Escalante National Monument, through Zion National Park, and into Grand Canyon National Park.
The Grand Staircase–Escalante National Monument (GSENM) is a United States national monument protecting the Grand Staircase, the Kaiparowits Plateau, and the Canyons of the Escalante (Escalante River) in southern Utah.
The Wahweap Formation of the Grand Staircase–Escalante National Monument is a geological formation in southern Utah and northern Arizona, around the Lake Powell region, whose strata date back to the Late Cretaceous (Campanian stage). Dinosaur remains are among the fossils that have been recovered from the formation. [1]
'Diving down the grand staircase.' WHOI Titanic footage nominated for two Webbies. Gannett. Heather McCarron, Cape Cod Times. April 15, 2024 at 4:58 AM.
The Grand Staircase is a sequence of sedimentary rock layers, first defined in the 1870s, that stretch south for 100 miles (160 km) from Bryce Canyon National Park through Zion National Park and into the Grand Canyon. [1] Bryce Canyon is located within the Pink Cliffs, the highest and youngest rise within the Grand Staircase. [2] [3]
The Kaiparowits Formation is a muddy bed that was deposited between about 77.3 to 72.8 million years ago, [2] [3] in the area where the Grand Staircase–Escalante National Monument of Utah is today. It is extremely fossil rich, with thousands of plants and animal fossils being preserved in amongst its sandstone and mudstone deposits.
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