Single Yellow Line Sunlight Usa Utah Pictures, Images and Stock Photos

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The Unique Hoodoos in the Natural Amphitheatre of Bryce Canyon in late Fall Sunshine, Utah, USA A stunning series of 7 images of the geological phenomenon that is Bryce Canyon in Southern Utah, Southwest USA. The major feature of the park is a collection of giant natural amphitheatres along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, pink and white colours of the rocks provide spectacular views from the rim at Bryce which varies from 8,000 to 9,000 feet elevation. These images were all taken in mid-afternoon from around or near Sunrise Point but the late November afternoon light has brought the vibrant and luminous colours of the rocks to life, compared to many images in which they can appear washed out.

The soft Pink Cliffs of the Claron Formation were eroded to form freestanding pinnacles called hoodoos, while the more resistant White Cliffs formed monoliths. The brown, pink and red colours are from haematite; the yellows from limonite and the purples are from pyrolusite. Hoodoos are composed of soft sedimentary rock and are topped by a piece of harder, less easily eroded stone that protects the column from the elements. Bryce Canyon has one of the highest concentrations of hoodoos of any place on Earth.

This 5th image is taken form the main road on the approaches to the park and would make an excellent National Park Promo picture. The deeply contrasting cobalt blue sky and the bright "Day-Glo" orange of the rock, compliment each other perfectly. The grey-black ashphalt of the road together with its broken yellow centre line and white dashes on either side of the road invite the viewer into the depths of the park o discover more. single yellow line sunlight usa utah stock pictures, royalty-free photos & images
The Unique Hoodoos in the Natural Amphitheatre of Bryce Canyon in late Fall Sunshine, Utah, USA A stunning series of 7 images of the geological phenomenon that is Bryce Canyon in Southern Utah, Southwest USA. The major feature of the park is a collection of giant natural amphitheatres along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, pink and white colours of the rocks provide spectacular views from the rim at Bryce which varies from 8,000 to 9,000 feet elevation. These images were all taken in mid-afternoon from around or near Sunrise Point but the late November afternoon light has brought the vibrant and luminous colours of the rocks to life, compared to many images in which they can appear washed out. The soft Pink Cliffs of the Claron Formation were eroded to form freestanding pinnacles called hoodoos, while the more resistant White Cliffs formed monoliths. The brown, pink and red colours are from haematite; the yellows from limonite and the purples are from pyrolusite. Hoodoos are composed of soft sedimentary rock and are topped by a piece of harder, less easily eroded stone that protects the column from the elements. Bryce Canyon has one of the highest concentrations of hoodoos of any place on Earth. This 5th image is taken form the main road on the approaches to the park and would make an excellent National Park Promo picture. The deeply contrasting cobalt blue sky and the bright "Day-Glo" orange of the rock, compliment each other perfectly. The grey-black ashphalt of the road together with its broken yellow centre line and white dashes on either side of the road invite the viewer into the depths of the park o discover more. single yellow line sunlight usa utah stock pictures, royalty-free photos & images

A stunning series of 7 images of the geological phenomenon that is Bryce Canyon in Southern Utah, Southwest USA. The major feature of the park is a collection of giant natural amphitheatres along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rocks. The red, orange, pink and white colours of the rocks provide spectacular views from the rim at Bryce which varies from 8,000 to 9,000 feet elevation. These images were all taken in mid-afternoon from around or near Sunrise Point but the late November afternoon light has brought the vibrant and luminous colours of the rocks to life, compared to many images in which they can appear washed out. The soft Pink Cliffs of the Claron Formation were eroded to form freestanding pinnacles called hoodoos, while the more resistant White Cliffs formed monoliths. The brown, pink and red colours are from haematite; the yellows from limonite and the purples are from pyrolusite. Hoodoos are composed of soft sedimentary rock and are topped by a piece of harder, less easily eroded stone that protects the column from the elements. Bryce Canyon has one of the highest concentrations of hoodoos of any place on Earth. This 5th image is taken form the main road on the approaches to the park and would make an excellent National Park Promo picture. The deeply contrasting cobalt blue sky and the bright "Day-Glo" orange of the rock, compliment each other perfectly. The grey-black ashphalt of the road together with its broken yellow centre line and white dashes on either side of the road invite the viewer into the depths of the park o discover more.

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