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Skirden Beck
Skirden Beck is a minor river in Lancashire, England (historically in the West Riding of Yorkshire). It is approximately long and has a catchment area of . The Beck is formed at the confluence of New Gill Beck and Grunsagill Beck and flows southward, being joined by Grainings Clough and then Monubent Beck (at ''Forest Becks'' near ''Skirden''). After passing through Bolton-by-Bowland village it collects Bier Beck and Kirk Beck, before passing Bolton Mill. The confluence with Holden Beck occurs just before Skirden Beck falls into the River Ribble near ''Briery Bank Wood''. Tributaries Holden Beck Holden Beck rises at ''Dugdales'' where Threap Green Brook (falling south from ''Ling Hill'' picks up another stream near ''Greenwoods'') and flows southwards to its confluence with Skirden Beck. Through ''Alder House Wood'' and ''Clough Wood'', between ''Mear Gill Top'' and ''Holden'', this stream takes the name Mear Gill. *Fell Brook rises on '' Grindleton Fell'' and drains into Me ...
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Confluence Of Skirden Beck With The Ribble - Geograph
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing ...
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Grindleton
Grindleton is a village and civil parish in the Ribble Valley district of the English county of Lancashire, formerly in the West Riding of Yorkshire. Its 3,700 acres sit within the Forest of Bowland. The population of the civil ward taken at the 2011 census was 772. History Craven in the Domesday Book shows that up till 1066 Earl Tostig was lord of Grindleton and the surrounding areas of West Bradford, Waddington, Bashall Eaves, Great Mitton, Hammerton, Slaidburn, Dunnow, Newton, Bogeuurde, Easington, Radholme Laund and Lees. This amounted to 36 carucates (ca5580 acres/1800ha) of ploughland. The Norman conquest of England added it to the extensive lands of Roger de Poitou. A caput manor in Domesday, Grindleton was subsumed into the Liberty of Slaidburn in the second half of the fourteenth century. Bowland underwent wholesale manorial reorganisation at that time, perhaps in response to the fall in population caused by the Black Death (1348–50) and the absorption of Bowl ...
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Rivers Of Lancashire
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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Bashall Brook
Bashall Brook is a minor river in Lancashire, England. It is long and has a catchment area of . The stream rises at Browsholme Tarn on Browsholme Moor descending through Braddup Clough where it collects Elm Clough and flows south and east past Bashall Eaves, meeting Cow Hey Brook before turning northeast to collect Hollins Clough near Back Ridge Farm. It again turns south, passing the Shireburn Caravan Park at Waddington before joining the River Ribble at the Low Moor area of Clitheroe Clitheroe () is a town and civil parish in the Borough of Ribble Valley, Lancashire, England; it is located north-west of Manchester. It is near the Forest of Bowland and is often used as a base for tourists visiting the area. In 2018, the Cl .... References Rivers of Lancashire Rivers of Ribble Valley {{England-river-stub ...
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Stock Beck
Stock Beck is a minor river in the West Craven area of Pendle, Lancashire (formerly in Yorkshire). It is long and has a catchment area of . Course Rising as Calf Hall Beck near Higher Laithe Farm on Weets Hill it flows north east into Barnoldswick, where it meets Gillians Beck and turns north becoming known as Butts Beck. Stock Beck leaves the town before heading northwest to meet Fools Syke and then Hell Forest Dike near Gilbeber Hill. After passing under the Monks Bridge on the A59 road at Horton it collects Horton Beck and heads west. It meets Flush Beck and then Bottom Beck near the hamlet of Bracewell. After the confluence with Spittle Syke, it passes under the Stock Beck viaduct on the Ribble Valley line and the A682 Long Preston road, north of the village Gisburn and joins the River Ribble The River Ribble runs through North Yorkshire and Lancashire in Northern England. It starts close to the Ribblehead Viaduct in North Yorkshire, and is one of the few that start ...
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Gisburn Forest
Gisburn Forest is a civil parish in the Ribble Valley, in Lancashire, England. Mainly lying within the Forest of Bowland Area of Outstanding Natural Beauty, the parish includes the larger part of the village of Tosside and the hamlet of Grunsagill to the south. Historically, the parish lay within the West Riding of Yorkshire. It had a population of 151 at the 2011 Census. The parish adjoins the Ribble Valley parishes of Easington, Bolton-by-Bowland and Paythorne along with Lawkland, Giggleswick, Rathmell, Wigglesworth and Halton West in the Craven district of North Yorkshire. History Near Brown Hills Beck on the western border of the parish is a bowl barrow thought to date from the late Neolithic or Bronze Age periods. It is an oval mound of earth, and up to high. There is another similar mound on the opposite side of the stream in Easington. The manor of Gisburn Forest was part of the Percy Fee which was listed in the Domesday Book. Matilda de Percy, the widow of Will ...
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Village
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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Middle Ages
In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the post-classical period of global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern period. The medieval period is itself subdivided into the Early, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralized authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the 7th century, North Africa and the Middle East—most recently part of the Eastern Ro ...
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River Ribble
The River Ribble runs through North Yorkshire and Lancashire in Northern England. It starts close to the Ribblehead Viaduct in North Yorkshire, and is one of the few that start in the Yorkshire Dales and flow westwards towards the Irish Sea (the Dee in Dentdale and the Twiss in Kingsdale being notable others). Etymology The name ''Ribble'' may be a Brittonic compound-formation. The second element is the noun ''*pol'', with connotations including "puddle, pond, upland-stream" (Welsh ''pwll''). The first is ''rö-'', an intensive prefix, with nouns meaning "great" (Welsh ''rhy-'', Cornish re-). Ribble may once have been known as ''*Bremetonā-'', underlying the name ''Bremetenacum'', the Roman fort at Ribchester. Involved here is the Brittonic root ''*breμ–'', meaning "roaring" (c.f. Welsh ''brefu''), as observed at the river-names Breamish in Northumberland, Braan in Scotland and Brefi in Wales. History Neolithic to Saxon finds from along the River Ribble during the ...
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River
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as Stream#Creek, creek, Stream#Brook, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to Geographical feature, geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "Burn (landform), burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from Precipitation (meteorology), precipitation through a ...
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Bolton-by-Bowland
Bolton-by-Bowland is a village and civil parish in the Ribble Valley district of Lancashire, England. Before 1974, the village was part of Bowland Rural District in the West Riding of Yorkshire. According to the census of 2001, the parish had a population of just 498, rising marginally to 499 at the census of 2011. History In medieval times, it was known as Bolton-''in''-Bowland, reflecting the shifting boundaries of the ancient Forest of Bowland on whose south east flank the village sits. The manor of Bolton-by-Bowland, however, was not included within the Lordship of Bowland, being a part of the Percy family fee from earliest times. It is thought that there has been a church on the site of St Peter and St Paul's Church since around 1190. The village is on Skirden Beck, near its confluence with the River Ribble. The village has a car park, toilet facilities and a tourist information centre, is the starting point for many of the area's walks. Governance Bolton-by-Bow ...
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Catchment
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the ''drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar but no ...
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