Geology

Drive the long stretches of highway that cut through the Colorado Plateau to Glen Canyon National Recreation Area (NRA) and it will be hard to miss the colorful bluffs, mesas, buttes, and canyons that dominate the landscape. Glen Canyon NRA lies in the middle of the Colorado Plateau, which spans 130,000 square miles of Utah, Arizona, Colorado, and New Mexico, an area that can be characterized by its high elevation and arid to semi-arid climate. Take some time to explore this vast landscape, and you will find cryptobiotic soil crusts, lush hanging gardens, and traces of dinosaurs that roamed this area millions of years ago during the Mesozoic Era.
 
A natural feature called Cathedral in the Desert. Swoopy sanstone cliffs with a natural waterfall in the center. Sandy beach at the bottom.
Cathedral in the desert

NPS/John Spence

The environmental processes such as climate change, fire regime, weather, and geological processes that shaped the Colorado Plateau are recorded in rock formations, which are the storytellers of the region’s history. Canyons carved out by the Colorado River and its tributaries expose rock layers deposited on top of each other over time; the youngest rocks at the top and the oldest at the bottom. These rock layers reveal fossils and traces of past life forms, principally from the Mesozoic Era, 248 to 65 million years ago. Fossils preserved in the rocks of Glen Canyon NRA are evidence of the life and changes that occurred during the Mesozoic Era and add to our understanding of biodiversity and evolutionary history. Natural erosion, flash floods which accelerate erosion, illegal collection, and vandalism threaten the paleontological resources of this region.

The geologic formations of the Colorado Plateau also affect vegetation communities by forming different soils and constraining water flow. Lush hanging gardens cling to vertical cliff walls and are fed by springs which flow down through porous rocks and cracks, until the water reaches a less permeable layer of rock when it begins to move sideways. The water may eventually reach the walls of a canyon where it seeps out of the rock and flows down, allowing plants to grow directly on the cliff face and on the ground around the seep. Though hanging gardens cover less than 0.1% of Glen Canyon’s 1.2 million acres, they are especially biologically diverse and support at least 10 endemic species, which are unique to the Glen Canyon area. The types and abundance of plants and animals in deserts are directly related to water. With limited water sources, many plant species, associated terrestrial invertebrates, aquatic invertebrates, birds, mammals, and amphibians use hanging gardens. Erosion caused by human and livestock foot traffic can increase the risk of invasion by nonnative species. Changes in regional precipitation patterns caused by global climate change could also threaten hanging gardens.

 
The bow of a boat looks at a muddy temporary waterfall off the side of a cliff into Lake Powell.
Temporary waterfalls in Glen Canyon National Recreation Area

NPS/Mark Anderson

Look closely at the ground as you explore the desert of the Colorado Plateau and you may notice a bumpy or spongy crust covering the floor. Cryptobiotic soil crusts are an important part of arid and semi-arid ecosystems throughout the world, including those in Glen Canyon NRA. These soil crusts are formed by very small organisms and their by-products, which create a crust of soil particles held together by organic materials. It is becoming increasingly clear that the older and better developed crusts support important levels of cryptogamic plant biodiversity. Watch your step: cryptobiotic soil crusts are fragile. Tires and foot traffic by humans and livestock can break through the crust, increasing the risk of soil erosion and nutrient loss. Once compacted, cryptobiotic soils can take anywhere from a few years to several decades or longer to recover. Research suggests that recovery of some of the algal and lichen components, as well as functions, may take much longer, and could take several hundred years in very dry environments.
 
Hazy still morning aerial view of Lake Powell with cliffs rising from the water.
Lake Powell morning

NPS

Though the waters of Lake Powell, created by the completion of the Glen Canyon Dam in 1963, covered fossils and drowned hanging gardens and other vegetation and animal communities, these unique natural features can be found elsewhere in Glen Canyon NRA. The continued protection and preservation of these unique resources will contribute to the changing diversity of the ecosystem and biological communities of the Colorado Plateau and Glen Canyon NRA. The 1.2 million acres of the Colorado Plateau protected by Glen Canyon NRA provide abundant scientific research opportunities that contribute to our understanding of these unique resources.

Published 8/07

 

Fossils

Learn about the puzzle pieces of paleontology

Soils

Get in depth information on cryptobiotic crusts

 

More Geology in Glen Canyon

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    Last updated: March 5, 2024

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