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Caves Of Ryd
The Caves of Ryd is a number of diabase pillars on the east side of the mountain of Billingen Billingen is the largest of the thirteen mesas in the Swedish county of Västra Götaland, with a maximum altitude of . The mesa extends in a north-southerly direct with a length of and a width of . Billingen is divided into two parts by an eas ... in Sweden. It is a popular lookout point over the city of Skövde, and is easily accessible on foot. The road is steep and difficult to travel by car. Underneath the pillars, there is difficult terrain occupied by big boulders. Many species of moss grows here. The Caves of Ryd were likely created from a landslide many years ago, during which the diabase pillars broke loose and slipped over the shale underneath creating a ravine-like shape rather than a cave-like one. A short way north of the Caves of Ryd lies the remains of the castle Ymsingsborg, which is also a popular lookout point. References

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Diabase
Diabase (), also called dolerite () or microgabbro, is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. Diabase dikes and sills are typically shallow intrusive bodies and often exhibit fine-grained to aphanitic chilled margins which may contain tachylite (dark mafic glass). ''Diabase'' is the preferred name in North America, while ''dolerite'' is the preferred name in the rest of the English-speaking world, where sometimes the name ''diabase'' refers to altered dolerites and basalts. Some geologists prefer to avoid confusion by using the name ''microgabbro''. The name ''diabase'' comes from the French ', and ultimately from the Greek - meaning "act of crossing over, transition". Petrography Diabase normally has a fine but visible texture of euhedral lath-shaped plagioclase crystals (62%) set in a finer matrix of clinopyroxene, typically augite (20–29%), with minor olivine (3% up to 12% in olivine diabase), magnetite (2%), an ...
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Billingen
Billingen is the largest of the thirteen mesas in the Swedish county of Västra Götaland, with a maximum altitude of . The mesa extends in a north-southerly direct with a length of and a width of . Billingen is divided into two parts by an east-west valley between Skövde and Varnhem. The mesa plateau is covered with vast forests and moorlands, including the nature reserve Blängsmossen with its unique flora. The limestone at Billingen has been quarried for a long time for concrete manufacturing; diabase is also still quarried there; The mesa, located between the two great lakes Vänern and Vättern, is also a popular nature resort with several nearby hotels, and an annual orienteering tournament is held here.Billingens fritidsområde - Skövde Kommun - www.skovde.se [Baidu]  


Sweden
Sweden, formally the Kingdom of Sweden,The United Nations Group of Experts on Geographical Names states that the country's formal name is the Kingdom of SwedenUNGEGN World Geographical Names, Sweden./ref> is a Nordic country located on the Scandinavian Peninsula in Northern Europe. It borders Norway to the west and north, Finland to the east, and is connected to Denmark in the southwest by a bridgetunnel across the Öresund. At , Sweden is the largest Nordic country, the third-largest country in the European Union, and the fifth-largest country in Europe. The capital and largest city is Stockholm. Sweden has a total population of 10.5 million, and a low population density of , with around 87% of Swedes residing in urban areas in the central and southern half of the country. Sweden has a nature dominated by forests and a large amount of lakes, including some of the largest in Europe. Many long rivers run from the Scandes range through the landscape, primarily ...
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Skövde
Skövde () is a locality and urban centre in Skövde Municipality and Västra Götaland County, in the Västergötland (Western Gothland region) in central Southern Sweden. Skövde is situated some 150 km northeast of Gothenburg, between Sweden's two largest lakes, Vänern and Vättern. It lies on the eastern slope of a low mountain ridge, Billingen (304 m), which cuts through the plain between the lakes. The Western Main Railway ( Västra Stambanan) was built through Skövde in the 1850s, which gave the town a dramatic industrial and population boost. Today, Skövde is home to the headquarters for Skaraborg's District Court and is the Västra Götaland's fourth-largest urban area as well as Sweden's 32nd biggest locality (by population) with 39,580 inhabitants in 2020. History Skövde traces its history back to the Medieval Age. In Skövde's city coat of arms is the image of Saint Elin (also known as Saint Helena), who was considered a pious woman from Skövde. She ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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Landforms Of Västra Götaland County
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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