Mono Lake Tufas — Stock Photo, Image

Mono Lake Tufas — Photo

Tufa tower rock formations in Mono Lake are calcium-carbonate spires and knobs formed by interaction of freshwater springs and alkaline lake water.

 — Photo by sprokop

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Tufa tower rock formations in Mono Lake are calcium-carbonate spires and knobs formed by interaction of freshwater springs and alkaline lake water.
Mono Lake Tufas — Stock Photo, Image
Tufa tower rock formations in Mono Lake are calcium-carbonate spires and knobs formed by interaction of freshwater springs and alkaline lake water.
Mono Lake Tufas — Stock Photo, Image
Alabama Hills are a hills and rock formations near the eastern slope of the Sierra Nevada Mountains west of Lone Pine, California
Rugged Landscape of the Alabama Hills — Stock Photo, Image
Alabama Hills are a hills and rock formations near the eastern slope of the Sierra Nevada Mountains west of Lone Pine, California
Rugged Landscape of the Alabama Hills — Stock Photo, Image
Tufa tower rock formations in Mono Lake are calcium-carbonate spires and knobs formed by interaction of freshwater springs and alkaline lake water.
Mono Lake Tufas — Stock Photo, Image
Tufa tower rock formations in Mono Lake are calcium-carbonate spires and knobs formed by interaction of freshwater springs and alkaline lake water.
Mono Lake Tufas — Stock Photo, Image
Bryce Canyon National Park is located in southwestern Utah in the United States and is distinctive due to its geological structures, called hoodoos, formed from
Bryce Canyon National Park — Stock Photo, Image
Alabama Hills are a hills and rock formations near the eastern slope of the Sierra Nevada Mountains west of Lone Pine, California
Landscape of Alabama Hills — Stock Photo, Image
Queen Victoria formation at Bryce Canyon National Park.
Queen Victoria formation at Bryce Canyon National Park — Stock Photo, Image
Tufa tower rock formations in Mono Lake are calcium-carbonate spires and knobs formed by interaction of freshwater springs and alkaline lake water.
Mono Lake Tufas — Stock Photo, Image
While hoodoos are scattered throughout these areas, nowhere in the world are they as abundant as in the northern section of Bryce Canyon National Park.
Hoodoos of Bryce Canyon National Park — Stock Photo, Image
Tufa tower rock formations in Mono Lake are calcium-carbonate spires and knobs formed by interaction of freshwater springs and alkaline lake water.
Mono Lake Tufas — Stock Photo, Image
Red Rock Coulee is located in south-eastern Alberta, Canada The main feature of this natural landscape is the huge red boulders of sandstone concretions.
Red Rock Coulee Natural Area — Stock Photo, Image
Red Rock Coulee is located in south-eastern Alberta, Canada The main feature of this natural landscape is the huge red boulders of sandstone concretions.
Red Rock Coulee Natural Area — Stock Photo, Image
Bryce Canyon National Park is located in southwestern Utah in the United States and is distinctive due to its geological structures, called hoodoos, formed from
Balanced Rock — Stock Photo, Image
Bryce Canyon National Park located in Utah, USA and is distinctive due to geological structures called hoodoos, formed by wind, water and ice erosion.
Winter in Bryce Canyon National Park — Stock Photo, Image

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You can use this royalty-free photo "Mono Lake Tufas" for personal and commercial purposes according to the Standard or Extended License. The Standard License covers most use cases, including advertising, UI designs, and product packaging, and allows up to 500,000 print copies. The Extended License permits all use cases under the Standard License with unlimited print rights and allows you to use the downloaded stock images for merchandise, product resale, or free distribution.

You can buy this stock photo and download it in high resolution up to 5108x3405. Upload Date: Aug 26, 2012