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Scenic overlook at Cedar Breaks National Monument in Utah

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.

The Berkeley Pit, a former open pit copper mine located in Butte, Montana, is currently one of the largest Superfund sites that is filled with water that is heavily acidic.

Desert valley. Grand Staircase-Escalante National Monument, Utah.

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

Scenic photo of rock formations in dixie national forest.

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.

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

Bryce Canyon National Park, Utah, United States

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.

Kapadokya is an area in Central Anatolia in Turkey best known for its unique moon-like landscape, underground cities, cave churches and houses carved in the rocks.

Scenery at Theodore Roosevelt National Park, North Dakota, USA

View inside the Ubehebe crater in the Death Valley National Park. Marvel at the vibrant colors adorning the crater walls and geological formations, creating a mesmerizing nature's artistry

Sunset View Overlook at Cedar Breaks National Monument in Utah_6947

Medium shot of red rock formation in Tien Shan mountains (Jeti Oguz, Kyrgyzstan)

Forêt Toufliht, Morocco rural mountain range scenery

Beautiful and colorful landscape of the Painted Hills in Eastern Oregon, near John Day.

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

Barren landscape of the Badlands of Drumheller, Alberta, Canada

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

The Blue Basin Valley in the Sheep Head Unit of John Day Fossil Beds National Monument is in the forefront of the photograph with the large mountain range surrounding it.

Eroded sedimentary rocks of Cedar Breaks National Monument near Bryan Head Utah

Bryce Canyon from Lower Inspiration Point in Bryce Canyon National Park, Utah

Rhyolite is a type of extrusive igneous rock characterised by its light color, high silica content, and fine-grained texture. It forms from the rapid cooling of magma on the Earth's surface and is often associated with volcanic eruptions. Rhyolite is rich in silica (SiO₂), typically containing more than 70% silica. It is composed mainly of quartz and feldspar, with minerals like biotite, hornblende, and pumice often present.

Deep sandstone canyon of red and white near Garden of the Gods and the Pikes Peak forest in Colorado Springs of western USA in North America.

$East exit of Zion National Park / past the Canyon overlook Trail -near and around Checkerboard Mesa : This famous formation was originally named so by Preston P. Patrow, the 3rd superintendent of Zion. Standing at 6,670 feet, it was named for its checkerboard appearance caused by th horizontal cross-bedding of ancient sand dunes and vertical cracking due to expansion and contraction of the sandstone during winter. The unusual crack pattern in the sandstone hills resemble a grid much like you would see on a checkerboard. \nDesert Bighorn, perfectly adapted to survive in severe desert climate are seen between Zion-Mt. Carmel Tunnel & East Entrance.$

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

Free Images: "bestof:Butte Geology.PNG en Butte Geology 1990-01-01 USGS Bulletin 1857-E Gold in Porphyry Copper Systems Gold in the Butte District Montana Edwin W Tooker other"

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