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  • 1
    Publication Date: 2014-11-15
    Description: In the summer of 1794 William George Maton, together with his friends Charles Hatchett and Thomas Rackett, embarked on a tour into Cornwall visiting the more southerly parts of Dorset and Devon en route . Rackett and Maton completed a second tour two years later, covering the rest of Dorset and Devon together with Somerset. An account of the tours was subsequently published by Maton, providing a contemporary description of SW England during the latter part of the eighteenth century. This was perhaps the first description of the region by scientifically aware travellers. They explored valleys, descended mines, visited smelters and collected minerals and must be regarded as among the earliest geotourists. Many sites which they visited, such as Roche Rock in Cornwall, Kent's Cavern in Devon and Wookey Hole in Somerset, became major attractions for geoscientists in the following centuries. Discussions in the text suggest that the travellers looked at the rocks with neptunist eyes. Maton summarized the geological and mineralogical references on a map which used shading with lines rather than colour to differentiate individual strata. Although rudimentary and inaccurate, the map is of considerable historic importance.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 2
    Publication Date: 2016-12-21
    Description: In around 1670 purging mineral waters were discovered on the western slopes of Shooter's Hill near Woolwich, to the east of London. They were promoted through an anonymous broadsheet, a single copy of which is held by the British Library. The probable author of this has been identified as Nathaniel Hodges, a physician who remained in London treating the sick during the plague year of 1665. Epsom Salts were produced at Shooter's Hill around 1700 and undercut in price those from Epsom and Acton to the west of London. The waters continued to be used by local people for the following 200 years but never achieved national fame, and the source had disappeared by the 1920s. The waters were derived from thin sandy horizons within the London Clay Formation and were characterized by high concentrations of Mg and SO 4 . The mineralogy of the clays suggests that pyrite oxidation in the weathered zone forms acid solutions leading to the dissolution of carbonates, particularly dolomite. Varying concentrations of dolomite account for variations in the Mg content of London Clay groundwaters and for the distribution of a number of historic purging waters around London.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 3
    Publication Date: 2018-03-07
    Description: The viability of any fort or garrison depends on the availability of a reliable water supply. The source of choice is an underlying aquifer, reached by a secure on-site well or borehole. Unfortunately, at coastal and maritime sites, seawater intrusion can cause problems. In the late eighteenth century a deep well was sunk to supply the garrison at Sheerness, Kent, which successfully exploited sands beneath the London Clay. At Landguard Fort in Suffolk, a shallow gallery was designed to skim freshwater overlying saline water within loose sand and shingle. In the mid-nineteenth century, a network of forts was built to defend the Royal Dockyard at Portsmouth, which included some offshore forts on the Spithead shoals. Boreholes were drilled beneath these forts to abstract water from the Chalk thought to lie beneath. The Chalk proved to be at too great a depth, but the Bracklesham Group yielded a sustainable supply from 〈200 m. In carrying out these projects, military engineers sank wells and drilled speculative boreholes, taking financial risks, unacceptable in other parts of the public sector. They developed new technologies and their innovative ideas and discoveries led to an increased understanding of the distribution and use of groundwater.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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