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Philpstoun

Philpstoun

FieldValue
countryScotland
official_namePhilpstoun
gaelic_nameBaile Philip
label_positionbottom
static_image_nameThe Union Canal at Philpstoun (geograph 2417871).jpg
static_image_captionThe Union Canal at Philpstoun
os_grid_referenceNT047770
population_refUnknown (2017)
map_typeScotland
coordinates
unitary_scotlandWest Lothian
lieutenancy_scotlandWest Lothian
constituency_westminsterLinlithgow and East Falkirk
constituency_scottish_parliamentLinlithgow
Lothian
post_townLINLITHGOW
postcode_districtEH49
postcode_areaEH
dial_code01506

Lothian

Philpstoun is a small village in West Lothian, Scotland, situated roughly 2 mi east of the historic county town of Linlithgow. The village originated in the oil shale mining boom of the 19th century. Surrounded by rich arable farm land, the village has a Community Education Centre and a Category B listed church. Philpstoun railway station closed in 1951 and Philpstoun and District Bowling Club closed in February 2012.

The bulk of the village lies between the Union Canal and the Glasgow–Edinburgh railway line, although the easternmost part, Old Philpstoun, lies north of the railway and closer to the M9 motorway.

bing]] near Philpstoun, the result of intensive mining from the middle of the 19th century to the middle of the 20th

Community centre

Philpstoun Community Education Centre is owned and maintained by West Lothian Council. The building was constructed around 1910, originally being referred to as "The Institute at Philpstoun." The building was commissioned by James Ross and Co., Philpstoun Oil Works Ltd, and was constructed along with the three rows of terraced houses to the north of the centre in a development referred to as the "Philpstoun Garden City."

References

References

  1. {{Historic Environment Scotland
  2. Theodore K. Irvine (1914) ''Report on the Housing Conditions in the Scottish Shale Field''
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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