Swinsto Cave
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Swinsto Cave
Swinsto Cave is a limestone cave in West Kingsdale, North Yorkshire, England. It leads into Kingsdale Master Cave and it is popular with cavers as it is possible to descend by abseiling down the pitches, retrieving the rope each time, and exiting through ''Valley Entrance'' of Kingsdale Master Cave at the base of the hill. It is part of a long cave system that drains both flanks of Kingsdale. Description The entrance is in a shakehole, and enters a small active stream passage. This soon enlarges to walking size before reaching a pitch with water entering from one side. Below a long passage (''The Long Crawl'') which has some flat-out wet sections, leads to a short second pitch. Below this a succession of three pitches rapidly descends to a spray-lashed chamber. A little beyond here the long ''Turbary Inlet'' enters from the right. At the end of this an excavated rift leads up into ''McShea Chamber'' in Turbary Pot, an alternative entrance. The main passage continues, desce ...
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Kingsdale
Kingsdale is a valley on the western edge of the Yorkshire Dales National Park in northern England. The name Kingsdale derives from a combination of Old Norse and Old English (''Kyen'' and ''Dael'') which means ''The valley where the cows were kept''. Humans were active in Kingsdale from 6,700 BC onwards. Evidence of fire-pits used by hunter-gatherers have been found in the dale. The larger part of the valley lies within the county of North Yorkshire but its highest reaches fall just within Cumbria. It is defined by the hills of Whernside to its east and Gragareth to its west. Kingsdale is drained by the south-westward flowing Kingsdale Beck which assumes the name River Twiss before joining the River Doe at Ingleton to become the River Greta. The single minor public road which serves the valley is followed by the Yorkshire Dales Cycle Way. There are several nationally important caves within the valley (such as Rowten Pot Rowten Pot is one of several entrances into the lo ...
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Karst
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 (perhaps by debris) 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. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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List Of UK Caving Fatalities
This is a list of recreational caving fatalities in the United Kingdom. It includes all verified deaths associated with the exploration of natural caves and disused mines in the modern era (post 1880). Deaths involving members of the general public who may have slipped down a shaft, or wandered into a cave without being aware of the risks, have been excluded. Caving cannot be considered a particularly dangerous pastime. In 2018, there were up to 4,000 regular cavers in the UK, and about 70,000 people who went on instructor-led courses into caves in the Yorkshire Dales, but there were no fatalities. List of fatalities The following is a list of the 137 identified recorded fatalities associated with recreational caving in the UK. The main causes of death have been drowning when cave diving, drowning as the result of flooding or negotiating deep water, injuries incurred from falling from a height, and injuries incurred as the result of rock falls. In ten cases the bodies have not ...
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Vadose
The vadose zone, also termed the unsaturated zone, is the part of Earth between the land surface and the top of the phreatic zone, the position at which the groundwater (the water in the soil's pores) is at atmospheric pressure ("vadose" is from the Latin word for "shallow"). Hence, the vadose zone extends from the top of the ground surface to the water table. Water in the vadose zone has a pressure head less than atmospheric pressure, and is retained by a combination of adhesion (''funiculary groundwater''), and capillary action (''capillary groundwater''). If the vadose zone envelops soil, the water contained therein is termed soil moisture. In fine grained soils, capillary action can cause the pores of the soil to be fully saturated above the water table at a pressure less than atmospheric. The vadose zone does not include the area that is still saturated above the water table, often referred to as the capillary fringe. Freeze, R.A. and Cherry, J.A., 1979. Groundwater. Engl ...
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Yordas Cave
Yordas Cave is a solutional cave in Kingsdale, North Yorkshire, England. It has been renowned since the eighteenth century as a natural curiosity, and was a show cave during the nineteenth century. It is now a popular destination for cavers, walkers, and outdoor activity groups. Description The old show cave entrance is in a plantation of trees from the road, at the base of a small cliff, at the bottom of a small gorge. A flight of three steps descend from the entrance archway into the Main Chamber, long, and wide. A stream flows across the floor, and disappears into some low passages to the left. Also on the left, a low passage can be followed for a few metres to the Back Door entrance in a shakehole. At the upstream end of the chamber two passages soon unite in the spray-lashed Chapter House chamber, where a waterfall enters and the showcave ended. Above the waterfall, a passage leads to a junction, with the water flowing from a low long passage which leads to the base o ...
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Rowten Cave
Rowten Pot is one of several entrances into the long cave system that drains Kingsdale in North Yorkshire, England. Its entrance is a shaft some long, wide, and at the southern end deep. Description A stream enters from just below the surface at the northern end. The cave is largely vertical, but at the bottom the stream flows through a short section of passage into the underground West Kingsdale river. This connects downstream with the ''Kingsdale Master Cave'' through three short sumps. Upstream, longer sumps may be followed up the valley for over , passing below the final pitch of Aquamole Pot. The cave is usually descended using single rope techniques, and is popular with cavers, being spacious and offering a variety of aerial routes. The three short sumps which connect to the Kingsdale Master Cave can be free-dived. The water which descends Rowten Pot sinks to the west of the pot on the other side of Turbary Road, into a shallow horizontal cave system, known as '' ...
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Carboniferous Period
The Carboniferous ( ) is a Period (geology), geologic period and System (stratigraphy), system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago (Myr, Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin ''wikt:carbo#Latin, carbō'' ("coal") and ''wikt:fero#Latin, ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare (geologist), William Conybeare and William Phillips (geologist), William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian (geology), Mississippian and the later Pennsylvanian (geology), Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Stegocephalia, Tetrapods ( ...
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Turbary Pot
Turbary is the ancient right to cut turf, or peat, for fuel on a particular area of bog. The word may also be used to describe the associated piece of bog or peatland and, by extension, the material extracted from the turbary. Turbary rights, which are more fully expressed legally as ''common of turbary'', are often associated with commonage, or, in some cases, rights over another person's land. Turbary was not always an unpaid right (easement), but, at least in Ireland, regulations governed the price that could be charged. Turf was widely used as fuel for cooking and domestic heating but also for commercial purposes such as evaporating brine to produce salt. The right to take peat was particularly important in areas where firewood was scarce. The right to collect firewood was protected by estovers. In the New Forest of southern England, a particular right of turbary belongs not to an individual person, dwelling or plot of land, but to a particular hearth and chimney. Ecology ...
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North Yorkshire
North Yorkshire is the largest ceremonial counties of England, ceremonial county (lieutenancy area) in England, covering an area of . Around 40% of the county is covered by National parks of the United Kingdom, national parks, including most of the Yorkshire Dales and the North York Moors. It is one of four counties in England to hold the name Yorkshire; the three other counties are the East Riding of Yorkshire, South Yorkshire and West Yorkshire. North Yorkshire may also refer to a non-metropolitan county, which covers most of the ceremonial county's area () and population (a mid-2016 estimate by the Office for National Statistics, ONS of 602,300), and is administered by North Yorkshire County Council. The non-metropolitan county does not include four areas of the ceremonial county: the City of York, Middlesbrough, Redcar and Cleveland and the southern part of the Borough of Stockton-on-Tees, which are all administered by Unitary authorities of England, unitary authorities. ...
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Shakehole
A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are locally also known as ''vrtače'' and shakeholes, and to openings where surface water enters into underground passages known as ''ponor'', swallow hole or swallet. A ''cenote'' is a type of sinkhole that exposes groundwater underneath. A ''sink'' or ''stream sink'' are more general terms for sites that drain surface water, possibly by infiltration into sediment or crumbled rock. Most sinkholes are caused by karst processes – the chemical dissolution of carbonate rocks, collapse or suffosion processes. Sinkholes are usually circular and vary in size from tens to hundreds of meters both in diameter and depth, and vary in form from soil-lined bowls to bedrock-edged chasms. Sinkholes may form gradually or suddenly, and are found worldwide. Formation Natural processes Sinkholes may capture surf ...
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England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ...
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