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Dried Out Soil in Yellowstone National Park

Close up of Dry cracks in dried out soil - Texture

Free Image of Dried Out Soil in Yellowstone National Park

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yellowstone national park

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Stunning natural land features

Yellowstone National Park, Park County, Wyoming, United States. In the Mammoth Hot Spring area. On a travertine hill, many hot springs deposit each day tons of water containing calcium carbonate. Their energy comes from the magmatic system that feeds other Yellowstone geothermal areas.

Maras, Peru

Boiling water bubbler Geyser. Active geyser with major eruptions. Yellowstone National Park, Wyoming, USA

Dry tree in the middle of hot springs

Water creek in Yellowstone National Park

White color landscape in the Mammoth Hot Springs in the Yellowstone National Park, Wyoming, USA

Scenery at Upper Geyser Basin, Yellowstone National Park, Wyoming, USA

Flow of sulphate from bubbling boiling mud pit natural springs in Hverir Geothermal Field, Iceland

Yellowstone River cuts a deep canyon as it moves north in the Yellowstone Ecosystem in western USA and North America. Nearest cities are Gardiner, Cooke City, Bozeman, Billings, Montana, Jackson, Wyoming, Salt Lake City, Utah and Denver, Colorado.

Fountain Paint Pot Trail, Yellowstone National Park, Teton County, Wyoming, United States. Volcanic Tableland.

Midway Geyser Basin in Yellowstone National Park.

Interesting textures and colors of Plume Geyser, a hot spring in the Upper Geyser Basin, Yellowstone National Park, Wyoming

Gobustan, Azerbaijan: mud spewing out from the earth due to compactional stress, Azerbaijan has the most mud volcanoes in the world, with around 300 of them, around a third of all mud volcanoes in the world, some thought to have medicinal qualities. Their occurrence in the area around Qobustan is closely linked to the oil and gas deposits there.

Panorama erosive multi-colored clay in Petrified Forest National Park, Arizona

Geyser and hot spring in old faithful basin in Yellowstone National Park in Wyoming

The Painted Hills are one of the three units that comprise the John Day Fossil Beds. Take time to also visit the Clarno Unit, with Mars-like pillars formed by waterfalls and volcanic sludge, and the Sheep Rock Unit, where fossils of plants and animals like saber-toothed cats are on display at the Thomas Condon Paleontology Center. The hills get their name from the delicately colored stratifications in the soil and the yellows, golds, blacks and reds of the Painted Hills are best seen in the late afternoon. Tones and hue may appear to change from one visit to another, as the claystone differ with ever-changing light and moisture levels. Once you see them for yourself, it’s pretty easy to understand why the Painted Hills are one of the 7 Wonders of Oregon.

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