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Lower Calf Creek Falls, Escalante Canyon

Escalante Canyons

Lower Calf Creek Falls, Escalante Canyon   |  Matcha

The Escalante Canyons refers to the erosional landforms shaped by the Escalante River and its tributaries. The backcountry hiking trails in this region boast attractions such as active waterfalls, arches, narrow canyons, riparian oases and sculpted slickrock.

Highlights of Escalante Canyons include Calf Creek Falls and the Dry Fork trailhead 26.2 miles down the Hole-in-the-Rock Road, which accesses the popular and short slot canyons Peek-a-boo and Spooky Gulch, ideal for canyoneering trips.

Location

The canyons are in south-central Utah, north and west of the Glen Canyon National Recreation Area and Lake Powell. Accessed from Escalante or Boulder, Escalante Canyons is in the northeastern section of the Grand Staircase area.

Geography and Geology

The Escalante Canyons in the northern reaches of the monument begin as modest draws draining the flanks of Boulder Mountain. This lofty volcanic tableland bounds the river basin to the north and northwest. Drainages begin on the broad terrace traversed by Hole-in-the-Rock Road, gradually approaching the Escalante River. Once these drainages carve routes into the resistant Navajo Sandstone, they quickly develop into a network of slickrock gorges that are the myriad veins feeding the main artery of the river. Particularly in the upper Escalante Canyons, just below Boulder Mountain, the slickrock gorges emerge so suddenly and with such profound dimensions that it is an unrivaled scene of visual inspiration on the Colorado Plateau.

Navajo Sandstone is the predominant rock formation in the Escalante Canyons. Erosion has exhumed these ancient dunes and sculpted the resistant cross-bedded slickrock into a vast landscape of domes incised with innumerable serpentine canyons. This chiseled land is a true work of natural art and an unforgettable sight.

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