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Pocklington is a spring line settlement at the foot of the Yorkshire Wolds. The rocks underlying this area were deposited on the bed of a tropical ocean. When the land rose, the chalk wolds were formed from the exoskeletons of micro-organisms covering the sea floor.
This is a route-map template for the Pocklington Beck, a UK waterway.. For a key to symbols, see {{waterways legend}}.; For information on using this template, see Template:Routemap.
Water from the beck was diverted south of Pocklington in 1818 to feed the Pocklington Canal. [17] When this canal fell into disuse, neither waterway was maintained which led to flooding on both waterways. [18] Flooding remains an issue on the beck, and in the 21st century the beck has flooded the town of Pocklington in 2007, 2012 and in 2015.
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Note: Per consensus and convention, most route-map templates are used in a single article in order to separate their complex and fragile syntax from normal article wikitext. See these discussions , for more information. Suitable instructions belong here – please add to {{UK-waterway-routemap}}.
The Pocklington Canal is a broad canal which runs for 9.5 miles (15.3 km) through nine locks from the Canal Head near Pocklington in the East Riding of Yorkshire, England, to the River Derwent which it joins near East Cottingwith. Most of it lies within a designated Site of Special Scientific Interest.
Millington is a small village and civil parish in the East Riding of Yorkshire, England.It is situated approximately 2 miles (3.2 km) north-east of Pocklington.. Looking down on Millington from the Yorkshire Wolds Way
Boundaries of Goole and Pocklington — constituency of UK Parliament — since 2024: Source No source specified. Please edit this file description and provide a source. Date 5 April 2024 Author Rcsprinter123. Permission (Reusing this file) See below.