Utah: A Geologic History

Today Utah is a land of great diversity and scenery. Many factors have determined the changes the state has undergone through time. In a sense it could be said that Utah has had many different faces.

At times in the past Utah has been covered by oceans and inland seas, and at times it has been dry land. The elevation of the land surface had changes as well, ranging from sea level to over two miles above sea level. There have been periods where the topography has been relatively flat and times of mountain building and valley formation.

Utah has not always had the moderate climate that it has today. There have been wet tropical periods, dry dusty desert environments, and cold times that caused glaciers.

The geographic position of Utah has changed through time as well. Although these images represent Utah in its present orientation, the state has not always been so. Due to plate tectonics the state has move from a position on the equator to its present location and in doing so has rotated nearly 90 degrees from an east-west orientation to its present north-south position.

These images begin with the Paleozoic, which began about 540 million years ago at the expansion of complex life forms, and give a conceptual idea of what the State of Utah may have looked like in its geologic past. However, Utah had a history before that time that covered 3 billion years or more.

We don’t know as much about the first 3 billion years as we know about the 540 million years that followed, but rocks of this vast age range are exposed in the Raft River Range, Uinta Mountains, and parts of the Wasatch Range, as well as several other smaller areas of the state. These rocks give clues to the formation of the continent (including Utah), metamorphism and igneous intrusion, erosion of several miles of sediment, and a variety of environments, including oceans, tidal flats, rivers, streams, lakes, and continental glaciers.

Paleozoic

The Early Years: Paleozoic. During this era Utah was at the western edge of North America.  The eastern portion of the state was a low plain with little relief at about sea level.  What little sediment did reach the ocean was well washed quartz sand.  Coral reefs, now exposed as thick limestones in the Wasatch Mountains, marked shallow seas that led to deep oceans in the west.

Early Jurassic

Wind Deposited Sands: Early Jurassic. Cut off from moisture-laden ocean winds by rising mountains to the west, desert sands were blown into Utah from the north and northwest.  These blowing sands formed dunes which eventually turned into rock and are preserved in what is now called the Navajo Sandstone.  These ancient dunes are well exposed at Checkerboard Mesa in Zion National Park and on the San Rafael Swell.

Late Jurassic

Famous Dinosaurs: Late Jurassic. At this time Utah was a hot, swampy lowland with mountains and volcanoes to the west and northwest.  Meandering rivers and lakes abounded, while dinosaurs roamed the land.  Their fossilized bones are preserved and can be seen at famous sites such as the Cleveland-Lloyd Dinosaur Quarry and Dinosaur National Monument.

Late Cretaceous

Coal Formations: Late Cretaceous. Pressure from continental collisions with the Pacific Plate to the west produced high mountains in western Utah.  The eastern portion of the state was covered by an inland sea that stretched from the Gulf of Mexico to the Arctic.  The costal plain between these two areas advanced and retreated as sediment filled the sea and the basin sank.  Coal swamps formed behind barrier islands while dinosaurs continued to rule.

Paleocene

Utah Starts to Come Up in the World: Paleocene. Erosion wore down the mountains to the west and sediments filled the inland sea to the east.  Continued pressure from the Pacific Plate caused both the Uinta Mountains and the Colorado Plateau to uplift.  The Colorado Plateau warped as it rose, making the beginning of predominate swells and depressions now found in Utah (such as the San Rafael Swell).  A large freshwater body, called Lake Flagstaff, occupied a depression in what is now central Utah.

Eocene

Oil Shale and Fossil Fish: Eocene. After spending nearly 500 million years near sea level, Utah continued its rise to nearly a mile high in elevation.  Continued warping of the Colorado Plateau produced basins for lakes such as Lake Uinta.  Organic-rich accumulations in the bottom sediments include well-preserved fish fossils and oil shales.  The western mountains were reduced to relics.

Oligocene

Uplift and Volcanics: Oligocene. On the Colorado Plateau the lake basins were filled in and broad plains separated mountain uplifts.  The beginning of modern rivers ran across these plains.  The continental divide passed through northeastern Utah so the Green River in Wyoming drained to the Mississippi River.  With the beginning of extension in western Utah, which would eventually lead to the Basin and Range, extensive volcanic activity started to occur.

Miocene

Precious Metals Emplaced: Miocene. Whereas previous compression had moved the site of San Francisco closer to Salt Lake City, extension was now moving the two apart.  This extension separated uplifted mountain blocks from down-dropped basins forming the Basin and Range.  Volcanic activity continued forming three great metallic mineral belts.  From north to south they are:  Park City-Oquirrh, Deer Creek-Tintic, and Wah Wah-Tushar.  The Colorado Plateau continued to rise and tilt northeastward.

Pleistocene

Water and Ice: Pleistocene. The geography of Utah was very close to what it is now.  Mountains, canyons, and rivers were all well in place.  The climate at this time was wetter and colder and as a result glacial activity took place.  Canyons were carved and expanded in the Uinta Mountains as well as in several other mountain ranges throughout the state.  A giant fresh-water body called Lake Bonneville also formed, stretching from the Wasatch Mountains to Nevada and from the Utah-Idaho border nearly down to Cedar City in southern Utah.

Present

These are the Places: Present. The geologic history of Utah has left an indelible mark on the state.  It explains why the rocks to the east are brightly colorful while those to the west have somber colors, why there are spectacularly massive canyons on the Colorado Plateau while much of the Basin and Range has no external drainage, and why a high mountain chain, the Wasatch, runs down the middle of the state.  This history determines the location of settlements, industry, and recreation sites.