~195-185 million years ago
The Kayenta Formation consists of layers of reddish-brown and pink sandstone, and varicolored mudstone and siltstone deposited in streams and rivers within an arid environment.
Similar to the environment of the underlying Moenave Formation, the Kayenta is dominated by mudstones left behind on river floodplains and in small lakes, with thin layers of sandstone that represent actual stream channels. Similar dinosaur tracks are found within both layers as well.
Learn more about dinosaur tracks found in the Kayenta and Moenave Formations
The Kayenta Formation is visible in lower Zion Canyon and Kolob Canyons as the steep reddish-brown slopes below the giant cliffs.
The Springdale Sandstone is considered to be a sub-unit or member of the Kayenta Formation, and was deposited by a main river channel associated with the same river system responsible for the deposition of the Moenave and Kayenta formations. The Springdale Sandstone is visible in lower Zion Canyon as the prominent reddish cliff band above the canyon floor, separating the lower Moenave layer from the rest of the Kayenta Formation.
The Springdale Sandstone layer provides some of the most dramatic examples of the ongoing erosion occurring at Zion National Park, as the crumbly layers of the underlying Moenave Formation erode and undercut the Springdale Sandstone cliff. Boulders break off of the Springdale with some regularity, and some have even damaged buildings and roads in Zion.
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Last updated: July 6, 2015