Field Guides

Grand Canyon NP – North Rim

North Rim – Grand Canyon National Park The North Rim of Grand Canyon National Park provides elevated views into one of the most recognizable canyon systems in the world. The canyon was formed by long-term erosion of uplifted sedimentary rock layers by the Colorado River, exposing geological strata that record hundreds of millions of years […]

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Grand Staircase Escalante NM – Heart of the Cockscomb

Heart of the Cockscomb – Grand Staircase–Escalante National Monument The Cockscomb formation represents a dramatic geologic feature created by compressional forces that tilted sedimentary rock layers into a steep monocline. The Heart of the Cockscomb lies within this folded landscape and illustrates the structural deformation that shaped portions of the Colorado Plateau. The tilted rock […]

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Grand Staircase Escalante NM – Cottonwood Narrows

Cottonwood Narrows – Grand Staircase–Escalante National Monument Cottonwood Narrows preserves a narrow slot canyon environment formed through erosion acting upon sandstone layers within Grand Staircase–Escalante National Monument. The canyon’s confined passage illustrates how seasonal water flow gradually carved through relatively soft rock, creating smooth walls and winding corridors. The resulting formation demonstrates the influence of […]

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Bryce NP – Rainbow Point Trail

Rainbow Point Trail – Bryce Canyon National Park Rainbow Point Trail provides access to high elevation viewpoints overlooking the amphitheater formations of Bryce Canyon National Park. The landscape is defined by densely clustered hoodoos formed through differential erosion of sedimentary rock layers. Freeze-thaw cycles contribute to the gradual shaping of these vertical rock forms, producing […]

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Cedar Breaks NM

Cedar Breaks National Monument Cedar Breaks National Monument preserves a natural amphitheater carved into the western edge of the Markagunt Plateau in southern Utah. The formation exposes layers of limestone and sandstone shaped by erosion acting upon uplifted sedimentary rock. The resulting amphitheater reveals a landscape filled with colorful rock formations that illustrate long-term geological […]

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Great Basin NP – Wheeler Peak

Wheeler Peak – Great Basin National Park Wheeler Peak rises above the surrounding mountain landscape as one of the defining landmarks of Great Basin National Park. The peak is the second-highest summit in Nevada and anchors the park’s high-elevation environment of alpine slopes, exposed ridges, and glacially shaped terrain. Its prominence gives the park a […]

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Great Basin NP – Bristlecone Pines

Bristlecone Pines – Great Basin National Park The bristlecone pine groves of Great Basin National Park preserve one of the most remarkable high-elevation landscapes in the American West. Growing just below treeline on exposed limestone ridges, these ancient trees have adapted to severe conditions including freezing temperatures, high winds, and a very short growing season. […]

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Arches NP – The Windows

The Windows – Arches National Park The Windows section of Arches National Park preserves a concentration of large natural sandstone arches formed through erosion acting upon fractured rock layers. The arches developed as weathering gradually removed softer material beneath more resistant sandstone, leaving freestanding openings within the rock. The formations illustrate the structural processes responsible […]

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Canyonlands NP – Islands in the Sky

Island in the Sky – Canyonlands National Park Island in the Sky is a high mesa within Canyonlands National Park that provides sweeping views of canyon systems carved by the Colorado and Green Rivers. The elevated plateau is bounded by steep cliffs formed through erosion acting upon uplifted sedimentary rock layers. The landscape illustrates the […]

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Canyonlands NP – Horseshoe Canyon

Horseshoe Canyon – Canyonlands National Park Horseshoe Canyon preserves a remote canyon environment within Canyonlands National Park known for significant rock art panels associated with early Indigenous cultural traditions. The canyon’s curved shape reflects long-term erosion by seasonal water flow acting upon uplifted sedimentary rock layers. The landscape demonstrates the interaction between geological formation and […]

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