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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.

Track and field sprinter on starting point at cinder track in sp

Track and field sprinter on starting point at cinder track in sp

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.

Close-up of a red en white cinder track

Running track with sky and clouds

red running track with sky and clouds

Ashes of burnt grass

Ashes of burnt grass on the field

Lava Butte Lava Field

Lava Butte Lava Field

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.

USA, Arizona: Sunset Crater - Cinder Hills

USA, Arizona: Sunset Crater - Cinder Hills

Artificial Turf Field

Artificial Turf Field

Sunset Crater Volcano Cinder Cone

Sunset Crater Volcano Cinder Cone

Track and field cinder path with curve

Track and field cinder path with curve

Close-up of a red en white cinder track

Lava Butte

Cinder path in the field

Cinder path in the field

Building materials, a pile of bricks, cement, sand, cinder blocks, stones on white background.

Building materials, a pile of bricks, cement, sand, cinder blocks, stones on white background.

The brown background for runing

Ashes of burnt grass

Ashes of burnt grass on the field

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.

Artificial Turf Field

Artificial Turf Field

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.

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.

Close-up of a red en white cinder track

Close-up of a red en white cinder track

Lava Butte

Burning straw after a fire in the field

Feather grass in wind against a blue sky

Track and field sprinter on starting point at cinder track in sp

Track and field sprinter on starting point at cinder track in sp

Close-up of a red en white cinder track

Lone Tree at Sunset Crater National Park.

Desolate landscape image of Sunset Crater National Park in Arizona. Desolate landscape image of Sunset Crater National Park in Arizona.

Volcanic Landscape - Bartolome - Galapagos Islands

Volcanic Landscape - Bartolome - Galapagos Islands

Volcanic landscape - Bartolome - Galapagos Islands

Volcanic landscape - Bartolome - Galapagos Islands

USA, Arizona/Sunset Crater: Cinder Slope with Pines

USA, Arizona/Sunset Crater: Cinder Slope with Pines

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