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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.

Anasazi Granary in Rock Alcove Sandstone Cliffs Kaiparowits Plateau Utah

$Backlight on the eroded moraines, jagged by runoff water with a few pinaceae which decorate these gray sediments.\nPhoto taken on the website of the “Salle de Bal des demoiselles coiffées”$

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

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

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.

Aerial shot, drone point of view from above old abandoned mines of Mazarron in Murcia on blue sky background during sunny summer day. Mineral extraction industry, history concept. Spain

Enchanted Rock State Natural Area is close to Fredericksburg, Texas

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.

The Berca Mud Volcanoes are a geological and botanical reservation located in Buzau County, Romania. The main features consist of small volcano-shaped structures created by overflowing cold mud pushed by gases erupting as bubbles from 3000 meters deep through underground layers of clay and water.

Rugged terrain in the Garden of the Gods in Colorado Springs, Colorado, western USA of North America

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.

Textures and cracks of naturally weathered seaside rocks

Gingerbread horse rock and bizarre rocks in Dead city. Khoba-Tele Ridge of Karadag Reserve in early spring. Crimea

Calanchi (Badlands), in Montalbano Jonico, Basilicata, Italy

Upheaval Dome, Canyolands National Park, Utah - United States

During the late Jurassic Period about 150 million years ago, dinosaurs congregated along the shores of a vast freshwater lake in what is now southeastern Colorado. They left behind large trackways in the mud which shows up today eroded by river waters as over 1300 dinosaur footprints in limestone along the Purgatoire River. Most of these tracks are by made by herding Apatosaurus or sauropod dinosaurs. Part of the Picket Wire Canyonlands, the tracksite is the largest dinosaur tracksite in North America.

steep terrain in the south of Spain, it is an arid area, there are bushes, it is a mountainous area, the sky has clouds

details lichen on strange rock in forest

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.

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

Winter mountain landscape view without people

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