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A cross section of a sandy soil loam, with grass growing on the top.

Isometric Soil Layers diagram, Cross section of green grass and underground soil layers beneath, stratum of organic, minerals, sand, clay, Isometric soil layers isolated on white

$The Dead Sea and its predecessor lakes exhibit spectacular deformation patterns caused by earthquakes along the Dead Sea Fault. The photos exhibit various geological phenomena, including seasonal laminae layering (varves), folds, faults, fractures, dikes, soft sediment deformation, desert landscapes.$

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.

Underground soil layer of cross-section earth with grass on the top with hills view background

Beautiful landscape of harsh terrain in Moab valley, Utah, USA.

Entrance to Santa Elena Canyon, Big Bend National Park,Texas

$sedimentary rock, rock formed at or near Earth’s surface by the accumulation and lithification of sediment (detrital rock) or by the precipitation from solution at normal surface temperatures (chemical rock). Sedimentary rocks are produced by the weathering of preexisting rocks and the subsequent transportation and deposition of the weathering products.\nLocation: Çiftlik, Niğde, Turkey$

The Ochre Pits in the West MacDonnell Ranges used for traditional and sacred painting by indigenous Australians

Panoramic view of large piles of sand tower alongside railroad tracks in a rural setting of Colorado. The industrial scene contrasts with the natural landscape of grassy fields and blue skies dotted with wispy clouds in rustic Lamar, Colorado. In the distance, grain silos and other structures are visible, hinting at agricultural activity in the area. The sand mounds suggest mining or construction operations nearby.

A cut of soil with different layers visible

Deep sandstone canyon of red and white near Garden of the Gods and the Pikes Peak forest in Colorado Springs of western USA in North America.

Soil under the asphalt surface of the road, which was severely eroded

Strunjan cliff: .An 80 meters high cliff along 200 meters of the coast, a natural reserve and is the highest flysch cliff in the east part of the Adriatic.

Colorful layered rock formations in Quebrada de Cafayate valley, Argentina. National park Quebrada de las Conchas.

Santa Elena Canyon, Big Bend National Park, Texas.

Colorful mountains of Quebrada de las Conchas near Cafayate, Salta Province, Argentina

$Photo Taken At Big Bend National Park\n\nBig Bend National Park is an American national park located in West Texas, bordering Mexico. The park has national significance as the largest protected area of Chihuahuan Desert topography and ecology in the United States, and was named after a large bend in the Rio Grande/Río Bravo. The park protects more than 1,200 species of plants, more than 450 species of birds, 56 species of reptiles, and 75 species of mammals. Additional park activities include scenic drives, programs led by Big Bend park rangers, and stargazing.$

Abiquiu, NM: Sunlit red-orange mountain cliffs in Abiquiu, 50 miles north of Santa Fe, a local painted by Georgia O’Keeffe. Copy space in the vibrant blue sky.

Geology exploration to collect rock sample

Palo Duro Canyon State Park, Texas, USA: Capitol Peak - rock strata cover the Permian age, Triassic age, Miocene-Pliocene age and Quarternary age - part of the Caprock Escarpment - Texas Panhandle - photo by M.Torres

$Cathedral Valley\nCapitol Reef National Park, Utah$

Geological granite stone rock wall in Pedernales Falls State Park as part of the Texas Hill Country

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.

Lava boulders on eroded softer slopes. Big Bend National Park, Texas.

Boquillas Canyon on the border between Texas and Mexico in Big Bend National Park

An impressive mountain range crumbles in the Sonoma desert in Arizona on a Clear day

Free Images: "bestof:Texas Passive Continental Margin.JPG en Texas Passive Continental Margin own Josh214847 2010-01-10 Geological cross sections of the United States Diagrams in"

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