Garfield County Utah Pictures, Images and Stock Photos

View of Cassidy Arch at Capitol Reef National Park

Counties map of Utah state of United States of America

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken at Grand Staircase Escalante National Monument, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Sunset Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from the Queen's Garden Trail in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from the Navajo Loop Trail in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Sunset Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Sunset Point in Bryce Canyon National Park, Utah, USA.

Sunrise, with a Utah Juniper, Juniperus Osteosperma, in the foreground in the arid high desert just outside Escalante in Utah, USA

Bryce Canyon City, Utah, USA - May 11, 2011: Rustic storefronts in Bryce Canyon City depict old west history.

View of Cassidy Arch at Capitol Reef National Park

The Uinta Chipmunk (Tamias umbrinus) is endemic to the United States. This chipmunk was eating by the Queen's Garden Trail in Bryce Canyon National Park, Utah, USA.

Highly detailed downloadable and printable county map of Utah state of United States of America for web banner, mobile, smartphone, iPhone, iPad applications and educational use. The map is accurately prepared by a map expert.

Glenwood Springs, USA - June 29, 2019: Glenwood Canyon on highway through Colorado towns with cliffs and road

Desert Highway at Bryce Canyon, Utah, USA. The road passes through a natural arch.

The Pronghorn (Antilocapra americana) is a species of artiodactyl (even-toed, hoofed) mammal native to interior western and central North America. Although it is commonly thought of and called an antelope it is not a true antelope. The pronghorn is the only surviving member of the Antilocapridae family and has been in North America for over a million years. The pronghorn has a similar body shape to a deer but stockier and shorter legged. Both males and females grow horns but the male horns are larger. The horns are shed each year as the new horns grow from underneath. The pronghorn weighs between 90 and 120 pounds and stands about 3 1/2 feet tall at the shoulder. It has a tan to reddish brown body with white markings throughout. The pronghorn is the fastest land mammal in the Western Hemisphere. Its great speed enables the pronghorn to outrun most predators. Pronghorns are migratory herd animals. Their migration routes have been threatened by fencing and fragmentation of their habitat. Pronghorns cannot jump over traditional barb wire fences like deer and elk can. They try to pass underneath and sometimes get caught in the fencing. Newer types of fencing have plastic pipe under the bottom strands which allows the animals to pass through. Pronghorns are quite numerous and in some areas like Wyoming and northern Colorado the pronghorn population at times has exceeded the human population. This pronghorn was photographed at Bryce Point Turnoff in Bryce Canyon National Park, Utah, USA.

Rifle, USA - July 22, 2019: Sign closeup for Visitor center info and rest area next right exit in Colorado during summer

Glenwood Springs, USA - July 10, 2019: Historic street sidewalk in Colorado on Grand Avenue and Bullocks sign for clothing store

Glenwood Springs, USA - July 10, 2019: High angle view of famous Colorado natural hot springs pool in downtown with water and people swimming

Aerial shot of the dramatic landscape near Henrieville in Garfield County, Utah, close to Bryce Canyon National Park.

Trail sign along the Cassidy Arch Trail at Capitol Reef National Park

Spectacular View over one of the many steep curves of Highway 12, were it winds through the Grand Staircase-Escalante National Monument, Utah, USA, a section known as the Million Dollar Road. The million dollar road refers to the highway connecting the towns of Boulder and Escalante. It was built in 1983 and took five years to complete. The nickname comes from the difficult terrain and large amount of dynamite used in its construction.

Gypsum, USA - June 29, 2019: Freeway highway through Colorado towns with cars in traffic and view of snow on rocky mountains

View of Cassidy Arch at Capitol Reef National Park

A Dramatic, golden Sunrise in the Southwest, photographed just outside Escalante, Utah, USA

View of Cassidy Arch at Capitol Reef National Park

The colorful, sandstone walls of the Dryfork Slot canyon, in the Grand Staircase-Escalante National Monument, Utah, USA, aglow in the light from the noon sun entering it from above. This is the northernmost branch of Coyote Gulch, where occasional flash floods have carved a deep narrow groove into the Navajo Sandstone.

Highly detailed downloadable and printable counties map of Utah state of United States of America for web banner, mobile, smartphone, iPhone, iPad applications and educational use. The map is accurately prepared by a map expert.

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken at Grand Staircase Escalante National Monument, Utah, USA.

The White-Breasted Nuthatch (Sitta carolinensis) is a small songbird that is common across much of temperate North America. It is a thickset bird, with a large head, short tail and long pointed bill. It has a white body with a black cap, white face and blue-gray upperparts. Like other nuthatches it forages for insects on trunks and branches while moving head-first down a tree. Seeds, hickory nuts and acorns form a substantial part of its diet. The nuthatch breeds in old-growth woodland and makes its nest is in a tree cavity. This white-breasted nuthatch was photographed in a tree at Queen's Garden in Bryce Canyon National Park, Utah, USA.

An isolated Sandstone hoodoo, against the clear blue late afternoon sky in the Devils Garden, Escalante, Utah, USA. These strange formations consist of orange and yellow colored Entrada Sandstone situated on top of the beige colored Navajo sandstone and were shaped by erosion and weathering. This area is located on the Hole-in-the-Rock Road in the Escalante-Grand Staircase National Monument

The Bizarre, weathered rock formations of the Devil"u2019s Garden, Escalante, Utah, USA, in Black and white. This area, located on the Hole-in-the-Rock Road, consist of various hoodoos, natural arches, and other sandstone formations. These strange formations consist of orange and yellow colored Entrada Sandstone situated on top of the beige colored Navajo sandstone and were shaped by erosion and weathering.

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken near Paria River in Grand Staircase Escalante National Monument, Utah, USA.

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken near Paria River in Grand Staircase Escalante National Monument, Utah, USA.

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken near Paria River in Grand Staircase Escalante National Monument, Utah, USA.

Devil"u2019s garden, an area filled with sandstone hoodoos, in Escalante, Utah, USA, in Black and White in the last sun of the afternoon. This area is located on the Hole-in-the-Rock Road in the Escalante-Grand Staircase National Monument.

A photographer, taking a photo of the Metate Arch, a thin delicate stone arch in the Devils Garden, Escalante, Utah, USA, in the late afternoon. This area, located on the Hole-in-the-Rock Road, consist of various hoodoos, natural arches, and other sandstone formations, formed by wind erosion of the orange and yellow colored Entrada Sandstone.

A sandstone formations, weathered to form almost a face, in the Devil's Garden in Escalante-Grand Staircase National Monument, Utah, USA. This is an area, located on the Hole-in-the-Rock Road, just outside Escalante, consisting of various hoodoos, natural arches and other sandstone formations. These strange formations consists of orange and yellow colored Entrada Sandstone situated on top of the beige colored Navajo sandstone and were shaped by erosion and weathering.

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken near Paria River in Grand Staircase Escalante National Monument, Utah, USA.

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken at Grand Staircase Escalante National Monument, Utah, USA.

Most of the Mojave Desert is located in southeastern California and southern Nevada, with smaller portions in Utah and Arizona. The Mojave Desert is situated between the Great Basin Desert to the north and the Sonoran Desert to the south and is considered to be the smallest and driest desert in the United States. The Mojave Desert is in rain-shadow defined by a combination of latitude, elevation, geology, and indicator plants. This picture of the desert was taken near Paria River in Grand Staircase Escalante National Monument, Utah, USA.

Mano Arch, a small stone arch in the Devils Garden, Escalante, Utah, USA, in the vibrant colors of the late afternoon light. This area, located on the Hole-in-the-Rock Road, consist of various hoodoos, natural arches, and other sandstone formations, formed by wind erosion of the orange and yellow colored Entrada Sandstone.

Raven and red rocks above the Colorado River, Utah.

The Bryce Canyon area is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Red Canyon in Dixie National Forest, Utah, USA.

The Bryce Canyon area is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Red Canyon in Dixie National Forest, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from the Queen's Garden Trail in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from the Navajo Loop Trail in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Paria View in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Paria View in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Paria View in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Bryce Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Paria View in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its tall thin spires of rock known as hoodoos. Hoodoos start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the weather. Hoodoos generally form within sedimentary rock such as sandstone. These hoodoos were photographed from Paria View in Bryce Canyon National Park, Utah, USA.