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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.

Palo Duro Canyon State Park, Texas, USA: second largest canyon in the USA Texas, formed by the Prairie Dog Town Fork of the Red River, part of the Caprock Escarpment - Texas Panhandle - photo by M.Torres

Abelisaurus was a theropod dinosaur that lived in Argentina during the Cretaceous Period.

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

Computer generated 3D illustration with the dinosaur Omeisaurus in a landscape

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

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

Stob pyramids in Bulgaria in Rila mountain Natural phenomenon and travel destination Selective focus

The McKittrick Ridge as seen from the summit of 7830ft Lost Peak of the Guadalupe Mountains National Park in Texas.

landscape on the bryce canyon in the united states of america

Amazing landscape created by river Zrmanja in Croatia. Large canyon with green colored river in rugged karst landscape. Aerial view

Mountain range in the remote desert of western Utah.

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.

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.

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

Split rock was a navigation aid to pioneers headed west in early America in Wyoming of North America. In Wild west times it was stage stop and pony express stop.

Red sandstone, shale and siltstone, petrified wood and caprocks form brilliant, layered monuments in the massive canyon. Hoodoos speckle the mountainsides, along with juniper and cedar, caves and arroyos.

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

Upheaval Dome, Canyolands National Park, Utah - United States

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

Landscape of Vashlovani national park of caucasus mountains in Georgia. Semi-desert panoramic view of dry grasslands with mud mountains and shrubs

$Panorama of the \$

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

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

Sant Jeroni Montserrat Mountain peak . Standing on the mountain top

Textures and cracks of naturally weathered seaside rocks

Free Images: "bestof:EdwardsDisconformity.jpg en Disconformity in which the Edwards Formation Lower Cretaceous lies upon a Lower Permian limestone in Texas The hiatus is"

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