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Stunning rock formations in Capital Reef National Park, Utah, USA. Lots of unique shapes made out of red, orange and grey stones.
Maras, Peru
Abandoned open pit mine of Rio Tinto in Southern Spain
Bentonite Hills of Cathadral Valley in Capitol Reef National Park, Utah. The Bentolinte Hills are the Brushy Basin shale member of the Morrison Formation. Formed by mud, silt, fine sand and volcanic ash laid down in swanps and lakes about 140 million years ago durintg Jurassic times. The Painted Desert on the Hartnet Road.
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.
Berkeley Pit Mine in Butte, Montana, USA.
Scenery at Theodore Roosevelt National Park, North Dakota, USA
Spinazzola bauxite quarry in alta Murgia Park (Puglia, Italy)
La Cienaga area on Tumbaya, near Purmamarca on the colourful valley of Quebrada de Humahuaca in Jujuy Province, northern Argentina.
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.
A long view of the Amphiter area of hoodoo formations in Bryce Canyon National Park.
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.
Scenic overlook at Cedar Breaks National Monument in Utah
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.
Indonesia, kaliwungu - October 25, 2020. a place of mining of soil and rocks, accidentally forming a beautiful natural landscape and bright blue sky
Summer scenery at Theodore Roosevelt National Park, North Dakota, USA
Views of colorful mountains from Tilcara, Jujuy province, Argentina
Vilamala Hills a cloudy day.
Aerial view of Ankara, Nallıhan Bird Paradise.
Checkerboard Mesa in Zion National Park in Utah, USA
Beautiful and colorful landscape of the Painted Hills in Eastern Oregon, near John Day.
Panorama of the \
Hill Detail at Painted Hills Overlook in John Day Fossil Beds National Monument
Scenery at Painted Hills Unit, John Day Fossil Beds National Monument, Oregon, USA
Peru. Salt mine.
Volcanic Landscape at Nallihan Bird Sanctuary (Nallıhan Kuş Cenneti) in Turkiye's Ankara. Taken via drone.
Upheaval Dome, Canyolands National Park, Utah - United States
Winter mountain landscape view without people
John Day Fossil Beds National Monument
View from the top of the gondola in autumn in Vail
Free Images: "bestof:Tellurium with Quartz - Native Element Moctezuma Mine Sonoma Mexico.jpg These mineral images are free to use how you wish Own 2007-04-15 Dave Dyet http //www"
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