River Pinn

In today's world, River Pinn has become a topic of increasing interest to a wide spectrum of people. Its relevance ranges from the personal to the professional sphere, and impacts various areas of daily life. With the advancement of technology and globalization, River Pinn has gained even greater importance, generating debates, research and developments that have transformed the way we perceive and approach this topic. In this article, we will explore different perspectives and approaches related to River Pinn, in order to delve into its relevance and implications in today's world.

River Pinn
View of bend in river
River Pinn at Ickenham
River Pinn is located in London Borough of Hillingdon
Source of the Pinn
Source of the Pinn
Mid-course
Mid-course
River Pinn (London Borough of Hillingdon)
River Pinn is located in England
Source of the Pinn
Source of the Pinn
Mid-course
Mid-course
River Pinn (England)
Location
CountryEngland
RegionGreater London
Physical characteristics
Source 
 • location51°37′12.5″N 0°20′54.1″W / 51.620139°N 0.348361°W / 51.620139; -0.348361
 • elevationRoughly 120 m (390 ft)
Mouth 
 • location
51°30′52″N 0°28′48″W / 51.51444°N 0.48000°W / 51.51444; -0.48000
 • elevation
31 m (102 ft)
Basin features
ProgressionPinnColneThames

The Pinn is a suburban, outer west London river. It has dendritic headwaters, the furthest is considered its source – in Harrow Weald. Its confluence with Frays River makes it a tributary of the Colne. It is one of three principal rivers wholly in the historic county of Middlesex.

Route

The river runs through Pinner, the northern halves of Eastcote and Ruislip: the latter may be a notable rise-lip of land as 17th century maps often have the place name but likely derives from "rush leap" from the local width of the river. It then runs through Ickenham and on to Uxbridge, where it passes through the former grounds of RAF Uxbridge and Brunel University. The Pinn continues on to Pield Heath and Cowley, passing under the Grand Union canal before joining the Frays River, an anabranch of the Colne, at Yiewsley.

During the Second World War only, the Pinn was dammed near Pinner High Street for water for putting out fires from air raids.

The middle and lower thirds of the course are between the Colne and Crane, all flowing south, thus making up parallel drainage.

Celandine Route

This is a 12-mile (19 km) walk through woodland, meadows and parks. It finishes at the Grand Union Canal towpath parallel to the Fray's River anabranch of the Colne.

Connections

A short walk east along the Slough Arm of the Grand Union Canal connects.

The Grand Union Canal towpath connects, linking in Brentford (east south-east), Watford and the Midlands (north), and the Paddington Arm (central London, east).

Water quality

All local sewerage runs to the distant Mogden Sewage Treatment Works discharging its treated waters to the Tideway. This spares the Pinn from the incident nitrogen, bleach (ammonia) and other chemical biohazards which many of its catchment homes and business use and/or discharge.

The Pinn's flow is weak save for after moderate or heavy rain. Worn tyre and motor oil run-off is from some roadside drains at biohazardous levels, particularly below the A40 road which is a trunk route of six lanes at this point (this becomes the M40 motorway to the west) – about 0.62 miles (1 km) of this slopes down to the river.

See also

Citations and footnotes

  1. ^ a b "River Pinn". London Borough of Hillingdon. 26 June 2007. Retrieved 14 March 2011.
  2. ^ "Cowley: Introduction", A History of the County of Middlesex: Volume 3: Shepperton, Staines, Stanwell, Sunbury, Teddington, Heston and Isleworth, Twickenham, Cowley, Cranford, West Drayton, Greenford, Hanwell, Harefield and Harlington (1962), pp. 170-172. Institute of Historical Research, University of London. Retrieved 27 October 2008.
  1. ^ The others are the Brent and Crane

External links

51°30′51″N 0°28′47″W / 51.5142°N 0.4797°W / 51.5142; -0.4797