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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.

Maras, Peru

Unbelievable Views from the top of Mt Charleston Nevada USA

Devils Tower in Devils Tower National Monument, Wyoming, USA. The monolith is an igneous intrusion with columnar (hexagonal) jointing of the granite rising through the surrounding sedimentary rock.

rock in the mountains of Cyprus as a background 7

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

Aerial drone view, high altitudes, open air. Extreme mountainous region. Season is autumn. Yellowing meadows. Yellowing trees.

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.

Yellow rock sur coton road

Maras, Peru

Mountain range in the remote desert of western Utah.

Nature photography during hiking and climbing activities

A grand view from top of Kitt Peak near Tucson,Arizona. Several observatories look out over the Sonoran desert valley below.

Detailed histology image of the layers of the small intestine at 40x magnification, displaying the intricate structure and cellular composition of the organ.

Lion Geyser Group hot springs in Yellowstone National Park

Massive white Morrison period sandstone formations in the Garden of the Gods in Colorado Springs, Colorado, western USA of North America

A panoramic view on the plain on top of a mountain in Hochschwab region in Austrian Alps. The flora overgrowing the slopes is turning golden. Autumn vibes. Sharp and steep mountain chain. Wilderness

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.

Shot of mammoth hot springs in yellowstone national park in america, usa

Cloudy mountain Antalya Kemer Turkey

White wall of limestone in Pamukkale, Turkey. Carbonate formation.

Gastric mucosa intestinal metaplasia under microscopy

Landscapes of Turkey in high quality

Mount Rushmore shot in late September with a tilt shift lens.

Marble mining plant at the east of the island. White stone in blocks and gravel. Seaside of the Thracian sea. Porto Vathy, island Thassos (Thasos), Greece.

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.

snowy mountains, snow patterns and amazing spring beauties

Central footpath entry to the Garden of the Gods in Colorado Springs, Colorado, USA, North America.

Granite cliff formations in the Laramie Range of Wyoming.

Rhyolite is a type of extrusive igneous rock characterised by its light color, high silica content, and fine-grained texture. It forms from the rapid cooling of magma on the Earth's surface and is often associated with volcanic eruptions. Rhyolite is rich in silica (SiO₂), typically containing more than 70% silica. It is composed mainly of quartz and feldspar, with minerals like biotite, hornblende, and pumice often present.

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