Rainton Waggonway, branch to Penshaw (Wharton Main)

Rainton Waggonway, branch to Penshaw (Wharton Main)

HER Number
17102
District
Sunderland
Site Name
Rainton Waggonway, branch to Penshaw (Wharton Main)
Place
Penshaw
Map Sheet
NZ35SW
Class
Transport
Site Type: Broad
Tramway Transport Site
Site Type: Specific
Wagonway
General Period
POST MEDIEVAL
Specific Period
Hanoverian 1714 to 1837
Form of Evidence
Documentary Evidence
Description
By 1697, the Wharton family’s Rainton Waggonway carried coal from their Rainton Ducks Colliery across Dubmire and Hall Moors and over Sedgeletch from where the line took up an old waggonway route used by Sir John Duck through Newbottle, Penshaw and down Waggon Hill to the south bank of the River Wear. Branches were added to the waggonway from Newbottle Colliery for the Earl of Scarborough’s coal in 1723 and another from Smith’s Colliery in Morton but the route that these branch lines took has not been established. In 1730, the colliery passed by marriage to the Tempest family. Over the middle years of the 18th century, the course of the main way around Dubmires was altered because of wayleave problems and for a time the line became circuitous. By the late 1760s, the line had reverted to its former course. Branch lines were added to deep collieries. Wharton Main or Penshaw Colliery lay close to the River Wear and was sunk to the Hutton Seam at 84 fathoms. It is shown on Casson’s map of the Coalfield of 1801.
Easting
431970
Northing
553550
Grid Reference
NZ431970553550
Sources
Alan Williams Archaeology, 2013, Waggonways to the South Bank of the River Tyne and to the River Wear; Turnbull, L, 2012, Railways Before George Stephenson (entry 86G) p163 & 172; Casson, 1801, Map of the Coalfield