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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
Bryce Canyon National Park, Utah, United States
Scenic view of deserted canyon in Kyrgyzstan at sunset
Amazing rock formations of Bryce Canyon National Park, Utah.
The Faisal's Finger Rock is a natural stand-alone rock about 200 m in height near the Jabal Tuwaiq escarpment, a geological wonder near Riyadh.
Summer scenery at Theodore Roosevelt National Park, North Dakota, USA
Falls Park quartzite stone walls and trees in Sioux Falls, South Dakota, USA
A beautiful mountain landscape, a geological wonder on the road from Ouarzazate to Merzouga. Atlas Mountains, Morocco. Bald mountain cliffs and canyons under the pouring sun.
View of Fairytale canyon (Issyk-Kul, Kyrgyzstan) in winter
Badakshan - the North Eastern part of Afghanistan
Gorges Du Daluis Regional Nature Reserve, Var river, Alpes-Maritimes, Provence-Alpes-Cote d'Azur, France
The colors of the South Dakota Badlands are enhanced by the moisture and contrast brought by an early winter snowfall.
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.
Zhangye Danxia National Geopark - Gansu Province, China. Chinese Danxia multicolor danxia landform, rainbow hills, unusual colored rocks, sandstone erosion, layers of Red, Yellow and Orange stripes.
Scenery of Bisti Northern Section, Farmington, New Mexico, USA
Tatacoa desert located near the city of Neiva
cliff made of pieces of Pumice, an Igneous rock created during a volcanic eruption at Vlyhada beach on the Greek Island of Santorini
Panoramic view of the vast arid desert between Biskra and Batna. Algeria
Aerial view along the rim of the Bryce Canyon and its natural amphitheater and the rock hoodoos below.
Upheaval Dome, Canyolands National Park, Utah - United States
beautiful panoramic scenery of danxia at Zhangye national geopark, Gansu, China.
Massive red sandstone formations in the Garden of the Gods in Colorado Springs, Colorado, western USA of North America
A mountain of quarry and river sand, in which the birds made nests. Mountain, canyon, nesting place of birds.
Medium view of Fairytale canyon (Issyk-Kul, Kyrgyzstan) in winter
Beautiful natural landscape. A dip in the Earth's crust. Beautiful ravine. Alexandrovsky graben in the Volgograd region
Bryce Canyon National Park, Utah, USA.
View of the Hoodoos in Bryce Canyon National Park in a foggy and cloudy day. Utah. United States of America
ocres in Rustrel Luberon landscape French colorado
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.
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