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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
Diverse sedimentary rocks and clay washed out by water. Petrified Forest National Park, USA,  Arizona
Summer scenery at Theodore Roosevelt National Park, North Dakota, USA
Rock wall at lake Powell
Ankara, Turkey-October 15, 2011: Clay Hills View in Nallihan. They Are Hills Created By The Wear Of Clay Layers With Different Resistance. Nallihan is a district of Ankara Province.
Gorges Du Daluis Regional Nature Reserve, Var river, Alpes-Maritimes, Provence-Alpes-Cote d'Azur, France
Ancient round  petroglyph.
Fremont Indian State Park
Various rock formations of basalt, sandstone, dross and others in layers in an abandoned quarry
Paisaje de Hoces del júcar.
Summer scenery at Theodore Roosevelt National Park, North Dakota, USA
Hell's Half Acre
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 \
Wide View of Cedar Breaks National Monument in Utah in United States, Utah, Cedar City
Very crumbly sandstone cliff in Wadi Bani Awf, Oman. Nice for background.
Newspaper rock is a protected wall with ancient Anasazi Indian petroglyphs
Guadalupe Mountains National Park, Texas
Sima de San Pedro is located in Spain, within the autonomous community of Aragon, a region characterized by aridity and extreme temperatures. It is a chasm of karst origin, with a mouth of about 100 meters in diameter and a depth of 108, It is considered unique in Europe thanks to its complex and rich geological structure. Right at the bottom of the pit lies a lake that is 22 meters deep and contains 560,000 cubic meters of water. The Sima de San Pedro, or the Voragine di Saint Peter, is located near Oliete, a small town\n\nThis natural beauty is known as one of the most unique and important ecosystems in the region. Its interior is formed by an exceptional example of a microclimate that hosts over 25 species of vertebrates, including amphibians, reptiles, birds and mammals, as well as important colonies of bats.The photo is taken from the edge of a deep sinkhole in the karst scenery of the Aragon area of Spain. The view looks directly to the edge and cliff face of the chasm but also shows some of the land above it. The sky is blue.\n\nThe sinkhole is called Sima de San Pedro is located in Aragon, Spain. It is a chasm of karst origin, with a mouth of about 100 meters in diameter and a depth of 108, It is considered unique in Europe thanks to its complex and rich geological structure. Right at the bottom of the pit lies a lake that is 22 meters deep and contains 560,000 cubic meters of water.\n\nIt is a unique and important ecosystems in the region. Its interior contains a microclimate that hosts over 25 species of vertebrates, including amphibians, reptiles, birds and mammals, as well as important colonies of bats. The Sima de San Pedro, or the Voragine di Saint Peter, is located near Oliete, a small town
Rock formation on the coast at Ap Lei Pai island, Hong Kong
Scenic view of the awe-inspiring Sipapu Bridge, a natural rock formation located in Utah's Natural Bridges National Monument - USA
John Day Fossil Beds National Monument, Oregon
China, Xinjiang, Aksu, Tianshan Tuoermu Grand Canyon
Abandoned open pit mine
Sandstone headland with a dike running through
Summer scenery at Theodore Roosevelt National Park, North Dakota, USA
Ichnites or fossilized footprints of dinosaur. El Portillo, Munilla, La Rioja, Spain.
Paint Mines geological rock formations near in El Paso county, Calhan and Colorado Springs, Colorado, in western USA of North America. Named for the colorful clays that were collected by American Indians to make paint. Brightly colored bands, caused by oxidized iron compounds throughout the many different layers of clay.
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
Unshaped stone wall pattern,wall made of rocks
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