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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.
Fremont Indian State Park
Early in the spring, badlands. Drumheller Alberta, Canada.
Eroding distinct layers of sandstone.
Photo taken late in the afternoon, near Bivacco Salvasera 2596m, towards the southwest slope of the Gan Gorgia summit
red rock wall, the detail of the Kings Canyon  rock, Outback, Australia
Sand Tufa at Navy Beach in Mono Lake. Mono Lake Tufa State Reserve; Mono Basin National Scenic Area; Mono Basin; Mono Basin National Forest Scenic Area;
Pictures Sicily region of Italy scala dei turchi agrigento beach
Anasazi Granary in Rock Alcove Sandstone Cliffs Kaiparowits Plateau Utah
nature sceneries inside the Aliano badlands park during a springtime sunny day, Matera province
View of Bryce Canyon Amphitheater from the Rim Trail. Utah. 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.
Tunelboca cemented beach in Biskay, Spain. Sample of the anthropocene age, with a 7 m layer of industrial sediment deposits in the coast, formed by the wastes of the former Altos Hornos de Vizcaya steel mill
Red Rock Canyon State Park, California
Beautiful Iceland Landscape.
Scenery at Black Canyon of the Gunnison National Park, Colorado, USA
A folded sandstone cliff in Morocco
A close look at the Tre Cime di Lavaredo, also known as \
Basalt organs under the village of Chilhac, Haute-Loire
Aerial view of canyons in Monument Valley, Arizona, USA.
Bromo Tengger National Park in Indonesia. Semeru mountain and volcanic landscape view in fog
Fault in New Zealand cliff face showing movement along fault plane
The Symphony of Stones or also known as the Basalt Organ  in the Garni Gorge province in Kotayk, Armenia
Purple cays eroded in the field, near Pedraforca Mountains. Lacustrine deposits, Garumnian.
Surreal shapes of the famous Piramidi di terra (Earth Pyramids) rock formations eroded by wind in fog, Puster Valley, South Tyrol, Italy
Belas, Luanda Province, Angola: Miradouro da Lua, located along the coastal road between Luanda and Barra do Kwanza is Angola's answer to Bryce Canyon, a striking natural viewpoint known for its dramatic lunar-like landscape. The name, which translates to \
Route of Los Calderones-Hoces del Turia. Chulilla Valencia
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.
Devils Tower National Monument
Free Images: "bestof:FOLDED HORIZONTAL STRATA IN THE BROOKS RANGE ON THE EAST SIDE OF THE ATIGUN VALLEY - NARA - 550423.tif Scope and content General notes 550423 Local identifier"
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