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Vol. 11 No. 1 2004<br />

The dirtiest river of England<br />

By P.M. Maurenbrecher<br />

It was a case of taming the River Tame. Yes,”Tame” and<br />

not “Thames”. The River Tame is one of the few rivers<br />

that become contaminated at its source. Birmingham<br />

lies at the heart of England on the watershed between<br />

the west and east. The name Birmingham is synonymous<br />

with industry, heavy industry and lots of pollution. The<br />

Tame is an upper and main tributary of the River Trent<br />

whose estuary is the Humber.<br />

My colleagues in the London office of Binnie and<br />

Partners commiserated with me when they heard I was<br />

the unfortunate to act as “resident engineer” on a site<br />

investigation for a project to clean up the river. This<br />

was in the days when the word “<strong>environment</strong>” or in the<br />

Netherlands “milieu” was just starting to make a<br />

tentative impact. Possibly it was because it was the<br />

winter of 1973/74 when I was to go up north. Going<br />

north of London was like being banished to Siberia, as<br />

the north was ugly and was ravaged by industry<br />

meaning mining, steel works, heavy machinery and lots<br />

of chemical installations.<br />

I was not disappointed when I settled into “The Swan”<br />

at Coleshill Warwickshire. Coleshill was a typically rural<br />

Midlands English town which could support the cast<br />

of a Englands most favourite English serial/soap “The<br />

Archers”. Coleshill had seen better days and could<br />

emulate towns to the south if its buildings were<br />

renovated and restored. Two pictures show “The Swan”<br />

as an inn one would expect from the English tourist<br />

brochures as well as Colehill’s parish church. But that<br />

was all that Coleshill had to show off: it had views of<br />

Figure 1a Proposed dried/caked sludge disposal<br />

location in disused clay pit. Now filled with water and<br />

used as diving recreational facility.<br />

Figure 1b Cross-sections on westside of pit showing<br />

mono-cline type structure consisting of<br />

Carboniderous shales and coal seams. These overlie<br />

Cambrian Merevale shales. Interpretation of geology<br />

based on borehole and publications.<br />

43

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