The park is part of the Colorado Plateau as well as a significant transition zone in a volcanic arc that stretches from Delta Utah to Southern Colorado. This area has experienced various volcanic eruptions over the past million years and there are many volcanic sites to visit from Central to Southern Utah.
The park itself boasts the oldest volcano, the Kolob Volcano, which is approximately 1.1 million years old. Other eruptions, such as Firepit and Spendlove Knolls, took place along the Kolob Terrace Road between 220,000 to 310,000 years ago. The most recent eruption, Crater Hill, happened about 120,000 years ago near the West Temple.
Some eruptions from nearby the park itself include
St. George which experienced eruptions as recent as 41,000 and 32,000 years ago. The Cedar Breaks region saw eruptions about 1,000 years ago. The most recent eruption in Utah occurred at Ice Spring, near Fillmore, a mere 660 years ago.
The rock layers found in the park can tell a story of their own about the evolution of this beautiful place. The oldest rocks in Zion are located at the base of its cliffs. This layer of sedimentary rocks includes sandstone, limestone, and shale from ancient seas that once covered this part of Utah millions of years ago. These once submerged rocks found at the base of the cliffs are more than 200 million years old.
Above the bottom layer are two other distinct layers: the Navajo Sandstone and Kayenta formations. The Navajo Sandstone is a large deposit of sand that was dropped off by wind during the Jurassic period. This sandstone layer is responsible for the beautiful, steep cliffs of Zion. The Kayenta Formation came some 40 million years later.
The youngest rock layer is the Carmel Formation which is an important contributor to the canyons and valleys you see today. This mudstone and shale composite was created during the Cretaceous period, about 95 million years ago when a shallow sea covered the area.
Zion is found nestled along the edge of the Colorado Plateau which extends from Central Utah to Northern Arizona, encompassing parts of Colorado and New Mexico.
The Grand Staircase is one of the Colorado Plateau’s finest works of art. It is a set of colorful cliffs that have formed over the course of 2 billion years. The rock layers of iconic canyons, such as the
Grand Canyon, Zion, and
Bryce Canyon, serve as a vivid record of the region's extraordinary geological events. Spending time in the Colorado Plateau region is a trip through the work of billions of years of transformation and creation.