Jeff Goulden Bryce Canyon National Park Pictures, Images and Stock Photos

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.

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.

The pale blue male Mountain Bluebird (Sialia currucoides) is one of the most beautiful birds of the western United States. This bluebird lives in more open terrain than the other two bluebirds and may nest in holes in cliffs or dirt banks when tree hollows are not available. It often forages for insects while hovering low over open fields. Its diet also includes berries, especially during the winter. During the winter, Mountain Bluebirds often gather in large flocks. This bluebird was photographed in an open meadow near Bryce Point Turnoff in Bryce Canyon National Park, Utah, USA.

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.

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.

Cumulus clouds appear in a blue sky over Sunset Point in Bryce Canyon National Park, Utah, USA.

Cumulus clouds appear in a blue sky over 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 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.

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.

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.

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.

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.

The Golden-Mantled Ground Squirrel (Callospermophilus lateralis) is a type of squirrel found in the mountainous areas of western North America. Because of its stripes and cheek pouches the Golden-Mantled Ground Squirrel is often thought of as a chipmunk. It is considerably larger than the chipmunk and lacks facial stripes. This squirrel was photographed on the Navajo Loop Trail in Bryce Canyon National Park, Utah, USA.

Bryce Canyon National Park, Utah, USA - May 12, 2011: Hikers pass through the hoodoo rock formations on their way to the Queen's Garden.

The Golden-Mantled Ground Squirrel (Callospermophilus lateralis) is a type of squirrel found in the mountainous areas of western North America. Because of its stripes and cheek pouches the Golden-Mantled Ground Squirrel is often thought of as a chipmunk. It is considerably larger than the chipmunk and lacks facial stripes. This squirrel was photographed on 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 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 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 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 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 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 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 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 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 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 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 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 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 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 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 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 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 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 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 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 Sunrise 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.

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.

The Pondersosa Pines (Pinus Ponderosa) of the Colorado Plateau thrive in a region of very little precipitation that primarily falls in the winter as snow and as rain during the summer monsoon season. This lone Ponderosa Pine was photographed at 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.

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 Sunrise 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 Ponderosa Canyon Overlook 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 Sunrise 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 Natural Bridge Overlook 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 Sunrise 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 Sunrise 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 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 Rainbow 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 Rainbow 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 Yovimpa Point in Bryce Canyon National Park, Utah, USA.

Bryce Canyon is famous for its colorful rock formations. These formations start with an initial deposition of rock. Then over time the rock is uplifted then eroded and weathered. Typically these form from sedimentary rock such as sandstone. These rock formations were photographed from Rainbow 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 Rainbow 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 Rainbow 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.

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 Sunrise Point in Bryce Canyon National Park, Utah, USA.