Erosional Free Stock Images

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Red Wave

Vast Desert & Sand Dunes

Beautiful desert scene with golden sand dunes in the distance at Death Valley National Park, California. Beautiful desert scene with golden sand dunes in the distance at Death Valley National Park, California

South Rim View, Grand Canyon National Park, Arizona

Erosional landscape

Erosional landscape

Zabriskie Point Ridges

Zabriskie Point Ridges

Erosional landscape

Erosional landscape

Red Mountain Trail No. 159

Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, October 2010. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website. Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, October 2010. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website.

Red Mountain Trail No. 159

Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website. Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website.

Haleakala Volcano, Maui

Haleakala Volcano, Maui

Erosional Forms

Erosional Forms

Geological layering of a former riverbed

Geological layering of a former riverbed, boulders fixed by a sand matrix

The Colorado River As It Runs Through Marble Canyon In Northern Arizona, USA

View of the erosional landscape in Zabriskie Point - Death Valley, California

View of the erosional landscape in Zabriskie Point - Death Valley, California

Erosional view of Ruginoasa Pit from Apuseni mountains

Erosional view of Ruginoasa Pit from Apuseni mountains

Erosional view of Ruginoasa Pit from Apuseni mountains

Erosional view of Ruginoasa Pit from Apuseni mountains

Salt mounds in Death valley near Furnace Creek

Zabriskie Point Ridges

Erosional Ridges At Zabriskie Point, Death Valley National Park, California, Artistic Effects. Erosional Ridges At Zabriskie Point, Death Valley National Park, California, Artistic Effects

Iconic Shiprock, Farmington, New Mexico

Iconic Shiprock, Farmington, New Mexico

Zabriskie Point

Zabriskie Point

Classic image of Badlands near Drumheller, Alberta, Canada. Classic image of Badlands near Drumheller, Alberta, Canada

Red Mountain Trail No. 159

Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website. Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website.

Delicate Arch, Arches National Park, Moab Utah

Red Mountain Trail No. 159

Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website. Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website.

Erosional landscape

Erosional landscape in Groapa Ruginoasa, Apuseni mountains, Romania

Hoodoos in Bryce Canyon, UT.

Lookout viewpoint for tourists with binoculars

Marble Canyon Trail, Death Valley National Park, California

Red Waves

Swirling Sandstone Rock

Swirling Sandstone Rock

Death Valley National Park

Sand Dunes Amid Mountain Peaks, Death Valley National Park, California

Red Mountain Trail No. 159

Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website. Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, February 2015. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website.

Rock formation in Death valley near Furnace Creek

Overview of The Wave

Overview of The Wave

Red Mountain Trail No. 159

Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, October 2010. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website. Red Mountain is a volcanic cinder cone that rises 1,000 feet above the surrounding landscape. It is unusual in having the shape of a "U," and in lacking the symmetrical shape of most cinder cones. In addition, a large natural amphitheater cuts into the cone's northeast flank. Erosional pillars called "hoodoos" decorate the amphitheater, and many dark mineral crystals erode out of its walls. Studies by U.S. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain formed in eruptions about 740,000 years ago. The trailhead is located on U.S. Highway 180, 25 miles northwest of Flagstaff, Arizona. The trail is an easy 1.5 miles through open terrain with fantastic views of the San Francisco Peaks and surrounding San Francisco Volcanic Field. There is a short (approximately 6 feet) ladder climb required just before entering the natural amphitheater of the cinder cone. Photo by Deborah Lee Soltesz, October 2010. Credit: U.S. Forest Service, Coconino National Forest. For more information about this trail, see the Red Mountain Trail #159 trail description on the Coconino National Forest website.

East Rim Sunset

Plateau And Cliff In Silhouette At Sunset, Panoramic View, Grand Canyon National Park, Arizona, East Rim View, USA. Plateau And Cliff In Silhouette At Sunset, Panoramic View, Grand Canyon National Park, Arizona, East Rim View, USA

Zabriskie point desert sunset

Zabriskie point desert sunset, Death valley, California

Boulders Along Artists Drive; Death Valley National Park

Bad land details - ideal for background

Red Sandstone Waves

Red Sandstone Waves

Zabriskie Point, Death Valley

Zabriskie Point, Death Valley National Park, California

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