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Clapham, North Yorkshire
Clapham is a village in the civil parish of Clapham cum Newby in the Craven district of North Yorkshire, England. It was previously in the West Riding of Yorkshire. It lies within the Yorkshire Dales National Park, north-west of Settle, and just off the A65 road. History The church of St James in Clapham was founded in Norman times, and originally dedicated to St Michael. It is mentioned in records dating back to 1160. The village and church were burned during a Scottish raid following the Battle of Bannockburn in the early 14th century. The church tower was probably erected following this incident, but the rest of the church dates from the 19th century. In the 14th century John de Clapham, who took his surname from the village, was a supporter of the Earl of Warwick and lived at Clapdale Castle. His descendants took part in the Wars of the Roses on the side of the House of Lancaster. Since the 18th century Clapham has been home to the Farrer family who established their ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clapham Cum Newby
Clapham cum Newby is a civil parish in the Craven district of North Yorkshire, England. It was formerly in the Settle Rural District. It contains the villages of Clapham and Newby. According to the 2001 UK census, Clapham cum Newby parish had a population of 659, falling to 640 at the 2011 Census. History Listed monuments Clapham cum Newby has 47 listed buildings and monuments. Perhaps the oldest is the base of a standing cross, located outside the Manor House. The base was reportedly constructed during the reign (1199–1216) of King John, who granted Clapham a market charter. At some point over the next seven centuries, the original cross was removed from its base. In 1897, to commemorate the Diamond jubilee of Queen Victoria, a new shaft and cross were installed on top of the original base. The village church was constructed in the 15th century. The church was rebuilt and altered in the 19th century, leaving only the tower from the original building. While the Manor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ingleborough
Ingleborough () is the second-highest mountain in the Yorkshire Dales, England. It is one of the Yorkshire Three Peaks (the other two being Whernside and Pen-y-ghent), and is frequently climbed as part of the Three Peaks walk. A large part of Ingleborough is designated as a Site of Special Scientific Interest and National Nature Reserve and is the home of a new joint project, Wild Ingleborough, with aims to improve the landscape for wildlife and people. Name The first element of the name "Ingleborough" has been variably explained as a Scots term for 'beacon, fire', an Old Danish term meaning 'English' or a derivative of Old English ''ing'', 'peak'. The second element is derived from the Old English word ''burh'', meaning "a fortified place"; in this case, a hill fort. The summit plateau of Ingleborough is encircled by the remains of a massive stone rampart, containing the foundations of Iron Age huts. Geography Ingleborough is in the south-western corner of the Yorkshi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forest Of Bowland
The Forest of Bowland, also known as the Bowland Fells and formerly the Chase of Bowland, is an area of gritstone fells, deep valleys and peat moorland, mostly in north-east Lancashire, England, with a small part in North Yorkshire (however roughly half of the area falls into the area of the historic West Riding of Yorkshire). It is a western outlier of the Pennines. The Forest of Bowland was designated an Area of Outstanding Natural Beauty (AONB) in 1964. The AONB also includes a detached part known as the Forest of Pendle separated from the main part by the Ribble Valley, and anciently a royal forest with its own separate history. One of the best-known features of the area is Pendle Hill, which lies in Pendle Forest. There are more than 500 listed buildings and 18 scheduled monuments within the AONB. The Trough of Bowland is a pass connecting the valley of the Marshaw Wyre with that of Langden Brook, and dividing the upland core of Bowland into two main blocks. The hills ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Fault
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Craven Fault
The Craven Fault System is the name applied by geologists to the group of crustal faults in the Pennines that form the southern edge of the Askrigg Block and which partly bounds the Craven Basin. Sections of the system's component faults which include the North, Middle and South Craven faults and the Feizor FaultBritish Geological Survey 1:50,000 scale geological map (England and Wales) sheet 60 ''Settle'' are evident at the surface in the form of degraded faults scarps where Carboniferous Limestone abuts millstone grit. The fault system is approximately coincident with the southwestern edge of the Yorkshire Dales National Park and the northeastern edge of the Bowland Fells. Location The Craven Faults are major crustal fractures across the Pennines. These faults constitute a zone crossing the backbone of England from west to east commencing near Leck, Lancashire at then branching three ways: * The North Craven Fault extends about to . * The Mid Craven Fault extends abo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artificial Waterfall
An artificial waterfall is a water feature or fountain which imitates a natural waterfall. Artificial waterfalls have long been featured in traditional Japanese gardens, where they can serve to highlight a scene or to provide focus. The classic gardening manual ''Sakuteiki'', written in the mid-to-late 11th century, lists nine different types. Cascata delle Marmore, The Cascata delle Marmore is an example of a man-made waterfall created by the ancient Ancient Rome, Romans. Artificial waterfalls were popular in Europe in the late 19th and early 20th centuries, including the famous waterfall in Viktoriapark in Berlin.Susan C. Anderson (Editor), Bruce Tabb (Editor), ''Water, Leisure and Culture: European Historical Perspectives'', Berg Publishers, 2002, , page 122 An early American example is Huntington Waterfalls in Golden Gate Park, San Francisco, California. In 1896, ''Gardening Magazine'' reported that it was the only artificial waterfall in a public park in North America. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Wenning
The River Wenning is a tributary of the River Lune, flowing through North Yorkshire and Lancashire. The Wenning is formed from the confluence of Clapham Beck, which rises above Clapham, and Austwick Beck, which rises in Crummackdale above Austwick. It then flows westwards through High Bentham, Low Bentham and Wennington. It joins the River Lune approximately west of Hornby. This river's valley, together with Airedale, Wharfedale and upper Ribblesdale, make up the district of Craven. Wenning, River Wenning River Wenning The River Wenning is a tributary of the River Lune, flowing through North Yorkshire and Lancashire. The Wenning is formed from the confluence of Clapham Beck, which rises above Clapham, and Austwick Beck, which rises in Crummackdale above Aus ... Wenning 1Wenning {{England-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Lune
The River Lune (archaically sometimes Loyne) is a river in length in Cumbria and Lancashire, England. Etymology Several elucidations for the origin of the name ''Lune'' exist. Firstly, it may be that the name is Brittonic in genesis and derived from ''*lǭn'' meaning "full, abundant", or "healthy, pure" (c.f. Old Irish ''slán'', Welsh ''llawn''). Secondly, ''Lune'' may represent Old English ''Ēa Lōn'' (''ēa'' = "river") as a phonetic adaptation of a Romano-British name referring to a Romano-British god Ialonus who was worshipped in the area. Springs The river begins as a stream at Newbiggin, in the parish of Ravenstonedale, Cumbria, at St. Helen's Well (elevation of above sea level) and some neighbouring springs. On the first two miles of its course, it is joined by four streams, two of them as short as itself, but two much longer. These are the Bessy Beck (short), the Dry Beck of 4.9 kilometres' (three miles) length at from St. Helen's Well, the Sandwath Beck (s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ingleborough Cave
Ingleborough Cave (formerly known as Clapham Caves) is a show cave close to the village of Clapham in North Yorkshire, England adjacent to where the water from Gaping Gill resurges. That part of the cave which is open to the public follows a fossil gallery for some . The passage is spacious, and well decorated with stalagmitic formations. Beyond the show cave, the fossil gallery continues until it meets the main stream. The water can be followed upstream through passages under Trow Gill A trow was a type of cargo boat found in the past on the rivers Severn and Wye in Great Britain and used to transport goods. Features The mast could be taken down so that the trow could go under bridges, such as the bridge at Worcester and ..., to where it emerges from a sump at Terminal Lake which has been connected by divers to Gaping Gill, and followed downstream into Lake Pluto which has been connected by divers to Beck Head Stream Cave. A connection has also been made with Fox Hol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gaping Gill
Gaping Gill (also known as Gaping Ghyll) is a natural cave in North Yorkshire, England. It is one of the unmistakable landmarks on the southern slopes of Ingleborough – a deep pothole with the stream Fell Beck flowing into it. After falling through one of the largest known underground chambers in Britain, the water disappears into the bouldery floor and eventually resurges adjacent to Ingleborough Cave. The shaft was the deepest known in Britain, until Titan in Derbyshire was discovered in 1999. Gaping Gill still retains the records for the highest unbroken waterfall in England and the largest underground chamber naturally open to the surface. Features Due to the number of entrances which connect into the cave, many different routes through and around the system are possible. Other entrances include Jib Tunnel, Disappointment Pot, Stream Passage Pot, Bar Pot, Hensler's Pot, Corky's Pot, Rat Hole, and Flood Entrance Pot. The Bradford Pothole Club around Whitsun May ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fell Beck
Fell Beck is a stream located near the foot of Ingleborough, in the Yorkshire Dales National Park. It is notable for the fact that it runs into Gaping Gill, the second-largest natural cave shaft in the UK (after Titan). As it falls down the shaft for 110 metres it is the tallest unbroken waterfall in the UK. It later emerges as Clapham Beck in Beck Head Cave, adjacent to Ingleborough Cave. This was confirmed by cave divers in 1983, and by fluorescent dye tests many years before. At times it is blocked off by a temporary dam to allow members of the public to descend the shaft on a winch. Beyond the village of Clapham, Clapham Beck flows into the River Wenning, which in turn flows into the River Lune and thence to the Irish Sea The Irish Sea or , gv, Y Keayn Yernagh, sco, Erse Sie, gd, Muir Èireann , Ulster-Scots: ''Airish Sea'', cy, Môr Iwerddon . is an extensive body of water that separates the islands of Ireland and Great Britain. It is linked to the Ce .... ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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