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Cross-bedded sandstone.
Bryce Canyon National Park. Utah. USA.
Petrified wood, 20 million years old wood. Wood turned into stone
Aerial view along the rim of the Bryce Canyon and its natural amphitheater and the rock hoodoos below.
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.
Gloss mountains national park or glass mountains, Oklahoma
Red Rock Canyon State Park, California
Bryce Canyon National Park
Bryce Canyon National Park, Utah, USA. The Rim Trail. Beautiful summer mountain landscape in Utah, Beautiful red mountains scenery.
View of the Hoodoos in Bryce Canyon National Park in a foggy and cloudy day. Utah. United States of America
Aerial view of canyons in Monument Valley, Arizona, USA.
View of Bryce Canyon Amphitheater from the Rim Trail. Utah. USA.
View of the rock hoodoos in Bryce Canyon National Park. Queens Garden Trail.
Colorful summer panorama from the Bryce Point Overlook in Bryce Canyon National Park, southwest Utah.
Majestic rock formation of sandstone, Monument Valley, Utah, Arizona, USA
Paint Mines geological rock formations near Calhan and Colorado Springs, Colorado, in western USA of North America.
The scenery at Cedar Breaks National Monument in Utah.
Hoodoos in Bryce Canyon National Park, Utah
Bryce Canyon in the southwestern US state of Utah. Bryce Canyon is famous for its geological rock formations. Due to the interacting forces of freezing and thawing, the limestone and sandstone formations are slowly eroded to form the so-called hoodoos.
Late fall in Bryce Canyon National Park, Utah, USA.
scenic view to Bryce Canyon in afternoon light
Palo Duro Canyon State Park, Texas, USA: eroded cliff side - rock strata covering the Permian age, Triassic age, Miocene-Pliocene age and Quarternary age - part of the Caprock Escarpment - Texas Panhandle - photo by M.Torres
pink hoodoos and pine trees of Fairyland Point at Bryce National Park, Utah, USA
Eroded sedimentary rocks of Cedar Breaks National Monument near Bryan Head Utah
View of Fairytale canyon (Issyk-Kul, Kyrgyzstan) in winter
Bryce Canyon is a National Park in southwestern Utah. It is not a true canyon but more like a collection of natural amphitheaters. The rim at Bryce varies from 2400-2700 meters above sea level.
landscape on the bryce canyon in the united states of america
Hoodoos in Bryce Canyon National Park, Utah
Scenic overlook at Cedar Breaks National Monument in Utah
Yellow abstract background
Free Images: "bestof:Slickensides juniata.jpg Slickensides on a sample of sandstone of the Juniata Formation from an outcrop on Rt 322 northeast of State College Pennsylvania"
Map of Pennsylvania highlighting Juniata County.svg
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John J. Patterson - Brady-Handy.jpg
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Shawangunk Formation High Point SP NJ.jpg
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Fermanagh Township cut.jpg
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Juniata River hills in Watts Township.jpg
Juniata River hills in Howe Township.jpg
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Brallier Formation PA Turnpike MM138.JPG
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Pottsville Formation Worlds End.jpg
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Corriganville NewCreek pan.jpg
Weathering Limestone State College PA.jpg
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Reedsville Formation 522.jpg
Conglomerate Foreknobs Fm.jpg
Bald Eagle 522 Shade Gap.jpg
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