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The London Brick Company owes its origins to John Cathles Hill, a developer-architect who built houses in London and Peterborough. In 1889, Hill bought the small T.W. Hardy & Sons brickyard at Fletton in Peterborough, and the business was incorporated as the London Brick Company in 1900. [1] ". Fletton" is the generic name given to bricks made ...
The barge is named after the Sittingbourne entrepreneur, George Smeed (1812–1881) who began business in 1846 in Murston. The building of Victorian London created a vast demand for bricks. The yellow Kent Stock Brick which was cheaper to make than the more traditional red brick; Sittingbourne had the brickearth needed to make them, and easy ...
London Clay is an ideal medium for boring tunnels, which is one reason why the London Underground railway network expanded very quickly north of the River Thames. However, south of the Thames, the stratum at tube level is composed of water-bearing sand and gravel (not good for tunnelling) with London Clay below, which partly explains why there ...
Ancestral Thames. The Ancestral Thames is the geologically ancient precursor to the present day River Thames. The river has its origins in the emergence of Britain from a Cretaceous sea over 60 million years ago. Parts of the river's course were profoundly modified by the Anglian (or Elsterian) glaciation some 450,000 years ago.
London stock brick is the type of handmade brick which was used for the majority of building work in London and South East England until the increase in the use of Flettons and other machine-made bricks in the early 20th century. Its distinctive yellow colour is due to the addition of chalk. Another important admixture is 'spanish', which is ...
Slough (/ s l aʊ /) is a town in Berkshire, England, in the Thames Valley 20 miles (32 km) west of central London and 19 miles (31 km) north-east of Reading, at the intersection of the M4, M40 and M25 motorways. It is part of the historic county of Buckinghamshire. [1] In 2021 Census, the population of the town was 143,184. [2]
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