Wolverhampton - Geography

Geography

Wolverhampton lies northwest of its larger near-neighbour Birmingham, and forms the second largest part of the West Midlands conurbation. To the north and west lies the Staffordshire and Shropshire countryside.

Wolverhampton
Climate chart (explanation)
J F M A M J J A S O N D
63 7 1 44 7 1 51 10 3 49 12 4 53 16 6 59 18 9 47 21 11 58 21 11 64 18 9 61 14 6 62 10 3 67 7 2
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: "Averages 1971–2000". Met Office. http://www.metoffice.gov.uk/climate/uk/averages/19712000/sites/penkridge.html.
Imperial conversion
J F M A M J J A S O N D
2.5 44 34 1.7 44 34 2 49 37 1.9 54 38 2.1 60 43 2.3 65 48 1.9 70 52 2.3 69 52 2.5 64 48 2.4 56 44 2.4 49 38 2.6 45 35
Average max. and min. temperatures in °F
Precipitation totals in inches

Wolverhampton city centre falls outside of the area traditionally known as the Black Country, although some districts such as Bilston and Heath Town and the Willenhall side of Wolverhampton fall within the Black Country coalfields, leading to confusion as to whether the entire city falls within the region. Modern usage has tended towards using the term to refer to the western part of the West Midlands county, excluding Birmingham, Solihull and Coventry. Examples would be UK Government regional bodies such as the Black Country Development Corporation, under whose remit the city fell.

The city lies upon the Midlands Plateau at approximately 120 m (394 ft) above sea level. There are no major rivers within the city, although the River Penk and River Tame (tributaries of the River Trent) rise in the city, as does Smestow Brook, a tributary of the River Stour, and thence the River Severn. This means that the city lies astride the main east-west watershed (British usage, meaning drainage divide, of England.

The geology of the city is complex, with a combination of Triassic and Carboniferous geology; specifically Bunter and Keuper sandstone, and Upper and Middle Coal measures. There is also an area of dolerite intrusions.

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