List of sandstones

Last updated

Obernkirchen Sandstone Obernkirchener-gebeilt.jpg
Obernkirchen Sandstone

This is a list of types of sandstone that have been or are used economically as natural stone for building and other commercial or artistic purposes.

Contents

Trans-regional

(across state borders)

Australia

University of Sydney built from Hawkesbury Sandstone University of Sydney Main Quadrangle.jpg
University of Sydney built from Hawkesbury Sandstone

Belgium

Canada

Czech Republic

Denmark

Estonia

Devonian Sandstone at Suur Taevaskoda, Polva County, Estonia Suur Taevaskoda 2010 01.jpg
Devonian Sandstone at Suur Taevaskoda, Põlva County, Estonia

France

Germany

Bavaria

Adams Gate at Bamberg Cathedral made of Burgpreppach Sandstone BambergDom-HeinrichKunigunde.JPG
Adams Gate at Bamberg Cathedral made of Burgpreppach Sandstone
Quarry in Worzeldorf (Nuremberg) Steinbruch Worzeldorf (01).jpg
Quarry in Worzeldorf (Nuremberg)

Baden-Württemberg

Hessen

Lower Saxony

North Rhine –Westphalia

Coat of arms of the town of Anrochte made of Anrochte Stone Anroechter wappen.jpg
Coat of arms of the town of Anröchte made of Anröchte Stone

Rheinland-Pfalz

Saarland

Saxony

Dresden's Zwinger Palace, made of Cotta Sandstone Wallpavillon33.jpg
Dresden's Zwinger Palace, made of Cotta Sandstone

Elbe sandstones:

Saxony-Anhalt

Thuringia

Hungary

India

Israel/Palestine

Italy

Lesotho

Pakistan

Poland

Spain

Sweden

Switzerland

South Africa

A piece of Table Mountain Sandstone Tafelbergsandstein.jpg
A piece of Table Mountain Sandstone
Tesinsky sandstone quarry (Goulda Sandstone) Godula (rock) 2.jpg
Těšínský sandstone quarry (Goulda Sandstone)

United Kingdom

England

Horsham Stone Horsham Stone.jpg
Horsham Stone

Scotland

Wales

United States

The Three Gossips tower in Arches National Park is Entrada Sandstone of the Colorado Plateau The Three Gossips in Arches National Park.jpg
The Three Gossips tower in Arches National Park is Entrada Sandstone of the Colorado Plateau

See also

Related Research Articles

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The Carboniferous is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period 358.9 Ma to the beginning of the Permian Period, 298.9 Ma. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian and the later Pennsylvanian.

<span class="mw-page-title-main">Grand Canyon</span> Steep-sided canyon carved by the Colorado River in Arizona, United States

The Grand Canyon is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile.

<span class="mw-page-title-main">Petroglyph</span> Images carved on a rock surface as a form of rock art

A petroglyph is an image created by removing part of a rock surface by incising, picking, carving, or abrading, as a form of rock art. Outside North America, scholars often use terms such as "carving", "engraving", or other descriptions of the technique to refer to such images. Petroglyphs, estimated to be 20,000 years old are classified as protected monuments and have been added to the tentative list of UNESCO's World Heritage Sites. Petroglyphs are found worldwide, and are often associated with prehistoric peoples. The word comes from the Greek prefix petro-, from πέτρα petra meaning "stone", and γλύφω glýphō meaning "carve", and was originally coined in French as pétroglyphe.

<i>Dilophosaurus</i> Genus of theropod dinosaur from Early Jurassic

Dilophosaurus is a genus of theropod dinosaurs that lived in what is now North America during the Early Jurassic, about 186 million years ago. Three skeletons were discovered in northern Arizona in 1940, and the two best preserved were collected in 1942. The most complete specimen became the holotype of a new species in the genus Megalosaurus, named M. wetherilli by Samuel P. Welles in 1954. Welles found a larger skeleton belonging to the same species in 1964. Realizing it bore crests on its skull, he assigned the species to the new genus Dilophosaurus in 1970, as Dilophosaurus wetherilli. The genus name means "two-crested lizard", and the species name honors John Wetherill, a Navajo councilor. Further specimens have since been found, including an infant. Fossil footprints have also been attributed to the animal, including resting traces. Another species, Dilophosaurus sinensis from China, was named in 1993, but was later found to belong to the genus Sinosaurus.

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<span class="mw-page-title-main">Cuyahoga Valley National Park</span> National park in Ohio, United States

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<span class="mw-page-title-main">Tuscarora Sandstone</span> Bedrock unit in Pennsylvania, Maryland, West Virginia, and Virginia, US

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<span class="mw-page-title-main">Dakota Formation</span> Rock units in midwestern North America

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<span class="mw-page-title-main">Hamilton Group</span> Geological Group in North America

The Hamilton Group is a Devonian-age geological group which is located in the Appalachian region of the United States. It is present in New York, Pennsylvania, Maryland, Ohio, West Virginia, northwestern Virginia and Ontario, Canada, and is mainly composed of marine shale with some sandstone.

<span class="mw-page-title-main">Marcellus Formation</span> Middle Devonian age unit of sedimentary rock

The Marcellus Formation or the Marcellus Shale is a Middle Devonian age unit of sedimentary rock found in eastern North America. Named for a distinctive outcrop near the village of Marcellus, New York, in the United States, it extends throughout much of the Appalachian Basin.

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<span class="mw-page-title-main">Saguaro National Park</span> National park in Arizona, United States

Saguaro National Park is a national park of the United States in southeastern Arizona. The 92,000-acre (37,000 ha) park consists of two separate areas—the Tucson Mountain District (TMD), about 10 miles (16 km) west of Tucson, and the Rincon Mountain District (RMD), about 10 miles (16 km) east of the city. Both districts preserve Sonoran Desert landscapes, fauna, and flora, including the giant saguaro cactus.

<span class="mw-page-title-main">20th century in ichnology</span>

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<span class="mw-page-title-main">St. Clara Female Academy</span> Wisconsin womens school

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<span class="mw-page-title-main">Euclid Creek</span> River in Ohio, United States

Euclid Creek is a 43-mile (69 km) long stream located in Cuyahoga and Lake counties in the state of Ohio in the United States. The 11.5-mile (18.5 km) long main branch runs from the Euclid Creek Reservation of the Cleveland Metroparks to Lake Erie. The west branch is usually considered part of the main branch, and extends another 16 miles (26 km) to the creek's headwaters in Beachwood, Ohio. The east branch runs for 19 miles (31 km) and has headwaters in Willoughby Hills, Ohio.

<span class="mw-page-title-main">Stadium Square Historic District</span> United States historic place

The Stadium Square Historic District is a historic district located in Cleveland Heights, Ohio, in the United States. The district contains properties along the north and south sides of Superior Park Drive between S. Taylor and S. Compton Roads, as well as Taylor Tudor properties on S. Taylor Road at Superior Park Drive. The 6.92-acre (0.0280 km2) site contains residential homes and mixed-use structures, all built beginning in 1926. Cleveland Heights proposed constructing a football stadium on the site in 1927. The stadium was never built, and the historic district takes its name from the original name given the commercial complex. The Stadium Square Historic District is a largely undisturbed example of early 20th century Tudor Revival architecture.

References

  1. Gábor, Mezősi (2016). The Physical Geography of Hungary. Springer. p. 21. ISBN   9783319451831.
  2. "This Rajasthan school in Thar desert stays cool without air conditioning". Hindustan Times. 2023-08-09. Retrieved 2023-10-19.
  3. Bulletin, Issue 25. Wisconsin Geological and Natural History Survey. 1912. p. 25.
  4. "Jacobsville sandstone". Ohio State University. Archived from the original on 23 August 2011. Retrieved 19 June 2011.
  5. Smock, John (1888). "Building Stone in the State of New York" (PDF). Bulletin of the New York State Museum. 3: 16.
  6. Sego, Mickey. "Berea Grit Sandstone". Berea Historical Society. Archived from the original on November 8, 2014. Retrieved April 1, 2015.
  7. "Ohio Sandstone". Brooklyn.CUNY.edu. Retrieved 21 November 2012.
  8. "Bluestone Rock/Village". Bluestone Heights. Retrieved April 1, 2015.
  9. Rosy, Liza. "Sandstone Paving" . Retrieved March 22, 2022.