External links
- Cuevas de Sorbas - Visitas Guiadas
- Karst en Yesos de Sorbas
Coordinates: 37°05′32″N2°06′27″W / 37.0921°N 2.1074°W
 | This article about a location in Andalusia, Spain, is a stub. You can help Wikipedia by expanding it. |
Cuevas de Sorbas are the tourist gypsum caves in Sorbas in Almeria, Spain. The formations are 6 million years old and consist of karst in gypsum rock.
Coordinates: 37°05′32″N2°06′27″W / 37.0921°N 2.1074°W
| | This article about a location in Andalusia, Spain, is a stub. You can help Wikipedia by expanding it. |
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground.
USG Corporation, also known as United States Gypsum Corporation, is an American company which manufactures construction materials, most notably drywall and joint compound. The company is the largest distributor of wallboard in the United States and the largest manufacturer of gypsum products in North America. It is also a major consumer of synthetic gypsum, a byproduct of flue-gas desulfurization. Its corporate offices are located at 550 West Adams Street in Chicago, Illinois.
The Delaware Basin is a geologic depositional and structural basin in West Texas and southern New Mexico, famous for holding large oil fields and for a fossilized reef exposed at the surface. Guadalupe Mountains National Park and Carlsbad Caverns National Park protect part of the basin. It is part of the larger Permian Basin, itself contained within the Mid-Continent oil province.
Sorbas is a municipality of Almería province, in the autonomous community of Andalusia, Spain.
Cuevas or Cueva may refer to:
Cueva de Villa Luz, also known as Cueva del Azufre and Cueva de las Sardinas, is a cave near Tapijulapa in the southern Mexican state of Tabasco. The springs within the cave are rich in hydrogen sulfide, a gas that is a potent respiratory toxicant and smells like rotten eggs. Within the water sulfide is oxidized to colloidal sulfur which gives the water a milky appearance, and creates sulfuric acid. The cave is essentially a maze about two kilometers in length and primarily etched out of limestone by the sulfuric acid in the water. Hydrogen sulfide is also used by chemoautotrophic bacteria, which form the base of the food web.
Cuevas Bajas is a town and municipality in the province of Málaga, part of the autonomous community of Andalusia in southern Spain. It belongs to the comarca of Nororma. It is part of the judicial district of Archidona. The municipality is situated 75 kilometers from Málaga and 495 km from Madrid In 2011 it had a population of 1,482 inhabitants. Its surface area is 16.53 km2. Cuevas Bajas has a density of 89.66 inhabitants/km2. The natives are called Cueveños.
Cuevas de San Marcos is a town and municipality in the province of Málaga, part of the autonomous community of Andalusia in southern Spain. The municipality is situated in the northern part of the Antequera region, on the border of the province of Córdoba from the river valley of Genil to the Sierra Malnombre and Camorro de Cuevas Altas. It is also located within the comarca of Nororma. It borders the provinces of Granada and Cordoba to the north, the comarcs of La Axarquía to the south and Antequera to the west. The town is situated at an altitude of 420 meters above sea level.
Benamaurel is a village located in the province of Granada, Spain. According to the 2006 census (INE), the city has a population of 2328 inhabitants. The municipality includes the following localities: Puente Arriba, San Marcos, Cuevas de la Blanca, Huerta Real, Cuevas del Negro y Cuevas de Luna. There is a market held every Sunday morning and a 3-day Moors and Christians festival held in April.
Canalobre Cave is a karst cave located in the small municipality of Busot, Alicante Province, in the Valencian Community of Spain. It has an estimated area of at least 18,950 m2 (204,000 sq ft). It is one of the largest and one of the most popular caves in Valenciana.
The San Andres Formation is a geologic formation found in New Mexico and Texas. It contains fossils characteristic of the late Leonardian (Kungurian) Age) of the Permian Period.
The Yeso Group is a group of geologic formations in New Mexico. It contains fossils characteristic of the Kungurian Age of the early Permian Period.
Diego López de Haro y Sotomayor (1515-1578) was a Spanish noble holding the titles of Señor Lubrín y Sorbas, Almería and 10th Señor del Carpio, a title which was elevated to 1st Marques del Carpio in 1559 by Philip II of Spain.
Yeso Creek is a stream in De Baca County, New Mexico, in the United States.
Erythraeus (Zaracarus) passidonicus is a species of mite belonging to the family Erythraeidae, first described from Greece.
Erythraeus kastaniensis is a species of mite belonging to the family Erythraeidae, first described from Greece.
The Cave of the Angel refers to several cave-related structures located in the Aras mountain range near the town of Lucena, Córdoba province in Spain. The site contains lithic material of an Acheulean typology and dates to that from the Middle Pleistocene to the Upper Pleistocene. There is geological, paleontological, and archaeological evidence indicating an intense and long-term occupation of this site. The numerous bone and lithic remains found in this site, as well as the matrix surrounding them, reveal exposure to fire. This, along with the finding of a wide and deep combustion structure in the stratigraphic profile, support the hypothesis that at the time of the occupation of the site by humans there was processing and consumption of big mammals.
A gypsum cave is a natural karstic formation in gypsum. Gypsum karst is very rare. It depends on deposits of gypsum or anhydrite, often also called alabaster. Chemically it is calcium sulfate, CaSO4.
The Cave of Maltravieso in Cáceres, Extremadura, Spain, was discovered in 1951. It shows traces of human occupation from the Middle Paleolithic. It contains cave art, most notably a total of 71 hand stencils, enumerated in the 1990s using ultraviolet photography, but also linear designs and some animal paintings. In a 2018 study based on uranium-thorium dating, a hand stencil from the Cave of Maltravieso was dated to 64,000 years ago. This would make it Middle Paleolithic art, predating the presence of European early modern humans, with important implications for Neanderthal behavior.