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Leck, Lancashire
Leck is a civil parish in the English county of Lancashire. The parish of Leck had a population of 189 recorded in the 2001 census. In the 2011 census Leck was grouped with Ireby (2001 pop. 78) to give a total of 260. It is located next to the Leck Beck close to the main A65, south east of the Cumbrian town of Kirkby Lonsdale. Administratively it forms part of the City of Lancaster, Lancaster itself being away. The Church of St Peter was built in 1878-79 and burnt down in 1913, but was accurately re-built in 1915. Geology Leck is located on two ancient geological fault lines: the Dent Fault and the Craven Fault. These meet at around . In the Carboniferous to Jurassic periods these major earth movements formed the dramatic landscape of Lonsdale and the Aire Gap in Craven District Craven is a local government district of North Yorkshire, England centred on the market town of Skipton. In 1974, Craven District was formed as the merger of Skipton urban district, Settle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carnforth
Carnforth is a market town and civil parish in the City of Lancaster in Lancashire, England, situated at the north-east end of Morecambe Bay. The parish of Carnforth had a population of 5,560 in the 2011 census, an increase from the 5,350 recorded in the 2001 census. The town is situated around 7 miles north of Lancaster, 17 miles south of Kendal, 40 miles east (bisected by Morecambe Bay) of Barrow-in-Furness and 28 miles northwest of Settle. The town is also close to the Cumbria/Lancashire border. Carnforth grew in the 19th century through the presence of the railway and ironworks. Due to the closeness of the coast and the hills, Carnforth is a popular base for walkers and cyclists exploring the area. The River Keer, the West Coast Main Line (WCML), the A6 and the Lancaster Canal pass through the town. The M6 motorway passes just to the east, linked to Carnforth by the A601(M). History The name "Carnforth" is thought to derive from its old function as a ford of the Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lancaster, Lancashire
Lancaster (, ) is a city and the county town of Lancashire, England, standing on the River Lune. Its population of 52,234 compares with one of 138,375 in the wider City of Lancaster local government district. The House of Lancaster was a branch of the English royal family. The Duchy of Lancaster still holds large estates on behalf of Charles III, who is also Duke of Lancaster. Its long history is marked by Lancaster Castle, Lancaster Priory Church, Lancaster Cathedral and the Ashton Memorial. It is the seat of Lancaster University and has a campus of the University of Cumbria. The Port of Lancaster played a big role in the city's growth, but for many years the outport of Glasson Dock has become the main shipping facility. History The name of the city first appeared in the Domesday Book of 1086, as ''Loncastre'', where "Lon" refers to the River Lune and "castre" (from the Old English ''cæster'' and Latin ''castrum'' for "fort") to the Roman fort that stood on the site. Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Listed Buildings In Leck, Lancashire
Leck, Lancashire, Leck is a Civil parishes in England, civil parish in City of Lancaster, Lancaster, Lancashire, England. It contains 21 Listed building#England and Wales, listed buildings that are recorded in the National Heritage List for England. All of the listed buildings are designated at Grade II, the lowest of the three grades, which is applied to "buildings of national importance and special interest". Other than the small settlement of Leck, the parish is rural. The most substantial building in the parish is Leck Hall; this and associated buildings are listed. Most of the other listed buildings are houses, farmhouses and associated structures. Also listed are a church and stones of various types. Buildings References Citations Sources * * * * * * * * * * * * * * * * * * * * * * * {{DEFAULTSORT:Leck, Lancashire Lists of listed buildings in Lancashire Buildings and structures in the City of Lancaster ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Craven District
Craven is a local government district of North Yorkshire, England centred on the market town of Skipton. In 1974, Craven District was formed as the merger of Skipton urban district, Settle Rural District and most of Skipton Rural District, all in the West Riding of Yorkshire. The population of the Local Authority area at the 2011 Census was 55,409. It comprises the upper reaches of Airedale, Wharfedale, Ribblesdale, and includes most of the Aire Gap and Craven Basin. The name Craven is much older than the modern district, and encompassed a larger area. This history is also reflected in the way the term is still commonly used, for example by the Church of England. History ''Craven'' has been the name of this district throughout recorded history. Note: Select the Thorton in Craven entry. Its extent in the 11th century can be deduced from The Domesday Book but its boundaries now differ according to whether considering administration, taxation or religion. Toponymy The deri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aire Gap
Aire Gap is a pass through the Pennines in England formed by geologic faults and carved out by glaciers. The term is used to describe a geological division, a travel route, or a location that is an entry into the Aire river valley. Geology Geologically the Aire Gap lies between the Craven Fault and the limestone uplands of the Yorkshire Dales to the north and the Forest of Bowland and the millstone grit moors of the South Pennines. The South Pennines is the system between the Aire Gap and the Peak District.Encyclopædia Britannica The gap was formed by the dropping of the Craven Faults in the Carboniferous through Jurassic periods combined with glacial scouring by ice sheets in the Pleistocene Ice Age. The Aire Gap splits the Pennines into north and south by allying with the River Ribble. The Pennine chain is divided into two sections by the Aire Gap formed by the River Aire flowing south, a member of the Humber basin, and the Ribble flowing west and entering the Irish sea. G ... [...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] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' 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 and 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 and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...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] |
Dent Fault
The Dent Fault is a major fault zone on the boundary between the counties of Cumbria and North Yorkshire in northern England. It is named after the village of Dent in Dentdale, on the western margin of the Yorkshire Dales. The fault, or rather the 'Dent Fault System' – a collection of closely associated faults and folds, defines the western edge of the Askrigg Block, a geological structure that underlies the Yorkshire Dales. The fault is associated with the Taythes Anticline to its west and the Fell End Syncline to its east. Other than vertical movement on the fault, there has also been an element of strike-slip movement. To the north, the fault links with the Pennine Fault System in the vicinity of Brough and with the Craven Fault System near Kirkby Lonsdale to the south.Stone et al. 2010 ''British Regional Geology: Northern England'' (5th edition) Keyworth, Notts, British Geological Survey Regional setting The Carboniferous geology of northern England consists of a series ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
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] |
St Peter's Church, Leck
St Peter's Church is in the village of Leck, Lancashire, England. It is an active Anglican parish church in the deanery of Tunstall, the archdeaconry of Lancaster and the diocese of Blackburn. Its benefice is united with those of St Wilfrid, Melling, St John the Baptist, Tunstall, St James the Less, Tatham, the Good Shepherd, Lowgill, and Holy Trinity, Wray, to form the benefice of East Lonsdale. The church is recorded in the National Heritage List for England as a designated Grade II listed building. History The first church on the site was built in 1610; it was a small single-storeyed building. In 1825 it was extended and a small tower was added. The present church was built in 1878–79, and was designed by the Lancaster architects Paley and Austin. It cost £3,000 (), and provided seating for 224 people. The church was damaged by fire in October 1913 and rebuilt by 1915 at a cost of about £5,000, it is said accurately to the original design, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
