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Scenic overlook at Cedar Breaks National Monument in Utah

Maras, Peru

Summer scenery at Theodore Roosevelt National Park, North Dakota, USA

Rainbow Mountain, Peru. Also known as Cerro Colorado near to Cusco. Aerial view. South America

Palo Duro Canyon State Park, Texas, USA: eroded cliff side - Geologic time periods marked by major changes in the fossil record - rock strata covering the Permian age, Triassic age, Miocene-Pliocene age and at the top the Quaternary age - this cliff includes the Permian-Triassic (P-T) extinction boundary, colloquially known as the Great Dying, that took place about 248 million years ago. The extinction was caused by climate change. The main cause of extinction was the vast amount of carbon dioxide emitted by volcanic eruptions that created the Siberian Traps, which elevated global temperatures and acidified the oceans. Geological time scale, part of the Caprock Escarpment - Texas Panhandle.

Beautiful Iceland Landscape.

Gorges Du Daluis Regional Nature Reserve, Var river, Alpes-Maritimes, Provence-Alpes-Cote d'Azur, France

Aerial view of canyons in Monument Valley, Arizona, USA.

Stone quarry for the production of crushed stone and gravel for use in construction.

Rock formation and sea water at a rocky beach in Norwegian fjord in summer (July). Shot with a full frame camera with a fast lens at low ISO resulting in a large clean file. Shallow depth-of-field.

Gloss mountains national park or glass mountains, Oklahoma

Summer landscape in Badlands National Park, South Dakota, USA

Sandy soil cross section

South Ural Mountains with a unique landscape, vegetation and diversity of nature in spring.

Top view of a huge crater of a stone crushed stone quarry in Russia, Chelyabinsk region, Miass city

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.

Red Deer River Canyon of Alberta in Canada

Panorama from Homestead Overlook, Badlands National Park, South Dakota, USA showing the badlands transitioning into mixed grass prairie.

Stunning rock formations in Capital Reef National Park, Utah, USA. Lots of unique shapes made out of red, orange and grey stones.

Scenery at Painted Hills Unit, John Day Fossil Beds National Monument, Oregon, USA

Early in the spring, badlands. Drumheller Alberta, Canada.

Palo Duro Canyon State Park, Texas, USA: eroded cliff side - rock strata covering the Permian age, Triassic age, Miocene-Pliocene age and Quarternary age - part of the Caprock Escarpment - Texas Panhandle - photo by M.Torres

Horsetooth Reservoir and Lory State Park near Fort Collins

Checkerboard Mesa in Zion National Park in Utah, USA

White wall of limestone in Pamukkale, Turkey. Carbonate formation.

Vilamala Hills a cloudy day.

Badland, red lands without vegetation of the Fardes River Valley.

Summer scenery at Theodore Roosevelt National Park, North Dakota, USA

The scenery at Cedar Breaks National Monument in Utah.

High angle view of mountain ridge in summer

Free Images: "bestof:Cuyuna Iron Range general geology.PNG en Minnesota's Cuyuna Iron Range's general geology Minnesota Geologic Survey url http //www geo umn edu/mgs/cuyuna/fig2"

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