Brook Stream
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Brook Stream
Brook Stream (or ''Spiders Castle Dyke'') is a tributary of the Great Stour river in Ashford, Kent, England. The water can be bright orange at times because of iron deposits. The stream runs from its source near Brook A brook is a small river or natural stream of fresh water. It may also refer to: Computing *Brook, a programming language for GPU programming based on C *Brook+, an explicit data-parallel C compiler *BrookGPU, a framework for GPGPU programming ..., 6.1 kilometres, north west to the Great Stour. References Rivers of Kent Borough of Ashford {{England-river-stub ...
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Brook, Kent
Brook is a small village and civil parish in the borough of Ashford in Kent, England, centred east-northeast of the town of Ashford. Geography Brook is in a gently rolling valley top immediately south of the North Downs. The brook referred to rises here and flows east to join the combined East and West Stour, that is, the River Great Stour. The south-east fifth of the parish is woodland. Brook has a small village museum. The human population of this area rose by 3 during the 10 years to the United Kingdom Census 2011. History The 11th century Grade I listed parish church is dedicated to St Mary. There is also a Baptist Baptists form a major branch of Protestantism distinguished by baptizing professing Christian believers only (believer's baptism), and doing so by complete immersion. Baptist churches also generally subscribe to the doctrines of soul compete ... chapel. The church of St. Mary, erected about 1075, is of stone, in the Early Norman style, and has a to ...
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River Stour, Kent
The River Stour is a river in Kent, England that flows into the North Sea at Pegwell Bay. Above Plucks Gutter, where the Little Stour joins it, the river is normally known as the Great Stour. The upper section of the river, above its confluence with the East Stour, Kent, East Stour at Ashford, Kent, Ashford is sometimes known as the Upper Great Stour or West Stour. In the tidal lower reaches, the artificial Stonar Cut short cuts a large loop in the natural river. The Stour has Kent's second largest catchment area (the River Medway having the largest). The lower part of the river is tidal; its original mouth was on the Wantsum Channel, an important sea route in medieval times. The river has three major tributaries, and many minor ones. For much of its length, it flows in a generally south-west to north-east direction. The historic city of Canterbury is situated on the river, as are the former Cinque Ports, Cinque Port of Sandwich, Kent, Sandwich and the railway town of Ashford. ...
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Ashford, Kent
Ashford is a town in the county of Kent, England. It lies on the River Stour, Kent, River Great Stour at the southern or Escarpment, scarp edge of the North Downs, about southeast of central London and northwest of Folkestone by road. In the 2011 census, it had a population of 74,204. The name comes from the Old English ''æscet'', indicating a Ford (crossing), ford near a Clumping (biology), clump of Fraxinus, ash trees. It has been a market town since the Middle Ages, and a regular market continues to be held. St Mary's Parish Church, Ashford, St Mary's Parish Church has been a local landmark since the 13th century, and expanded in the 15th. Today, the church functions in a dual role as a centre for worship and entertainment. The arrival of the railways from the mid 19th century onwards, created a significant source of employment contributing to the town's growth as a rail hub at the centre of five distinct railway lines. The high speed rail line (High Speed 1, HS1 High Sp ...
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Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream."opposite to a tributary"
PhysicalGeography.net, Michael Pidwirny & S ...
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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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Iron
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron A ...
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Deposition (geology)
Deposition is the geological process in which sediments, soil and rocks are added to a landform or landmass. Wind, ice, water, and gravity transport previously weathered surface material, which, at the loss of enough kinetic energy in the fluid, is deposited, building up layers of sediment. Deposition occurs when the forces responsible for sediment transportation are no longer sufficient to overcome the forces of gravity and friction, creating a resistance to motion; this is known as the null-point hypothesis. Deposition can also refer to the buildup of sediment from organically derived matter or chemical processes. For example, chalk is made up partly of the microscopic calcium carbonate skeletons of marine plankton, the deposition of which has induced chemical processes (diagenesis) to deposit further calcium carbonate. Similarly, the formation of coal begins with the deposition of organic material, mainly from plants, in anaerobic conditions. Null-point hypothesis The null ...
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Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ...
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Rivers Of Kent
Four major rivers drain the county of Kent, England. River Medway The catchment area of the Medway covers almost 25% of the county. The detailed map has a diagram of that catchment area, which includes its main tributaries: the rivers Eden, Bourne (or Shode), Teise, Beult, Loose and Len. Tributaries of the River Medway *The River Eden * River Grom *The River Bourne begins its course west of Oldbury Hill on the Greensand Ridge in the parish of Ightham and enters the Medway upstream of East Peckham, near Tonbridge. *The River Teise (pronounced ''tice'' or ''teeze'') begins in Dunorlan Park in Tunbridge Wellshttps://publications.parliament.uk/pa/cm199899/cmselect/cmenvtra/477/477mem24.htm The source of the Teise. ¶13. and flows eastwards through Lamberhurst, passing Bayham Abbey. Here the small River Bewl, on which is the reservoir Bewl Water, joins the Teise. The Teise bifurcates 2 km SW of Marden, the minor stream flows directly to Twyford Bridge, Yalding, while ...
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