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Painted Wall at Dragon Point in Black Canyon of the Gunnison National Park, Colorado, USA

Landscape photo, nature, forest, Usak, Turkey

Badlands scenery of Theodore Roosevelt National Park, North Unit, North Dakota.

Badland, red lands without vegetation of the Fardes River Valley.

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.

South of Bardenas Reales, bardeak 8-9 walking path, Navarra, Spain 24 april 2024

Big Horn sheep group (herd) on a rugged Rocky mountain hill side in Waterton Canyon near Denver, Colorado in western USA.

Aerial top view for breathtaking white cliff near green valley on beautiful, cloudy sky background. White, high rock cliff near the field with green grass.

Landscape shot of Pedernales Falls State Park

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

Viewpoint of mountain valley in summer morning

Stones the structure of the nature background, gray texture. Iron mine, natural texture of volcanic stone

Scenic rock wall at Black Canyon of the Gunnison National Park, Colorado, USA

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.

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.

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

Guadalupe Mountains National Park, Texas

Terraced Fields and Severe Erosion Loess Plateau Inner Mongolia China

The gabbro quarry in the Radautal, Harz, Lower Saxony, Germany, Europe

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

Bromo Tengger National Park in Indonesia. Semeru mountain and volcanic landscape view in fog

Stamp printed in USA showing Grand Canyon, circa 1989

$São Tomé Stone is a flexible stone, does not loose splinters, is non-slip, very absorbent and does not spread heat.\$

Forêt Toufliht, Morocco rural mountain range scenery

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