Kayenta Formation

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Kayenta Formation, Geological formation in southern Utah and northern Arizona, United States.

The Kayenta Formation is a geological layer of red and brown sandstone that stretches across Utah, Arizona, Colorado, and Nevada. It sits between the older Wingate Sandstone below and the younger Navajo Sandstone above, creating distinct visible bands when you walk through canyons and national parks.

This layer formed during the Early Jurassic period roughly 200 million years ago in a shallow lake and river landscape. In 1936, geologist A.A. Baker systematically named this formation after studying the Monument Valley and Navajo Mountain region.

Research teams from universities across North America regularly visit the formation to study dinosaur tracks and Early Jurassic period fossils.

You can observe it best in Zion, Capitol Reef, and Canyonlands, where the layers are clearly visible on canyon walls. Visiting is possible year-round, but spring and fall offer the most comfortable hiking conditions.

The layer holds fossilized footprints of early dinosaurs and remains of freshwater creatures like mussels and snails. These discoveries reveal that the region once teemed with ancient water systems where life thrived.

Location: Nevada

Location: Arizona

Location: Colorado

Location: Utah

GPS coordinates: 37.80000,-110.60000

Latest update: December 7, 2025 19:32

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« Kayenta Formation - Geological formation in southern Utah and northern Arizona, United States » is provided by Around Us (aroundus.com). Images and texts are derived from Wikimedia project under a Creative Commons license. You are allowed to copy, distribute, and modify copies of this page, under the conditions set by the license, as long as this note is clearly visible.

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