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Scenic overlook at Cedar Breaks National Monument in Utah

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

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

Stone wall and cloudy sky(the from below view against the blue sky)

Dry Waterfall and Painted Mountains on Artist Palettes Drive, Death Valley National Park, California, USA

Late fall in Bryce Canyon National Park, Utah, USA.

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.

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.

South of Bardenas Reales, bardeak 8-9 walking path, Navarra, Spain 24 april 2024

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.

Aliaga is a little town in teruel spain

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.

Panorama of the quarry for ore extraction. Pit of the Stoilensky Mining and Processing Plant

Scenery at Theodore Roosevelt National Park, North Dakota, USA

Amazing canyon. Mountain landscape. Green pine-trees on rock slopes. Hell's Backbone Road in the wilderness area located in south-central Utah, United States.

A glacier moraine on the italian side of Monte Rosa. Pennine Alps. Anzasca Valley. Macugnaga Municipality. Piedmont. Italy.

steep rock quarry

Henrieville is a town in Garfield County, Utah, United States.

Parco naturale nell'Utah

Looking across Farrell Canyon with the Chilcotin River running through it . The Hoodoos and sand dunes are on the fare bank of Farrell Canyon.

Aerial top view for breathtaking white cliff near green valley on beautiful, cloudy sky background. White, high rock cliff near the field with green grass.

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

Drumheller, Alberta, Canada, Badlands

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

A glacier moraine on the italian side of Monte Rosa. Pennine Alps. Anzasca Valley. Macugnaga Municipality. Piedmont. Italy.

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.

Wide view of Miradouro da Lua, Angola

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.

Aerial view of the Mountains in Leung Tin Au,Tuen Mun,Hong Kong

Aerial view of marble quarry in Burdur, Turkey. Taken via drone.

Free Images: "bestof:Ely Geology Part 1.PNG en Ely Geology Part 1 1990-01-01 USGS Bulletin 1857-E Gold in Porphyry Copper Systems Gold in the Ely Robinson Copper District White Pine"

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