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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 ...
London stock bricks, rather dimly lit. 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.
The Thames Valley is an area in South East England that extends along the River Thames west of London towards Oxford. The area is a major tourist destination and economic hub on the M4 corridor, with a high concentration of technology companies. The area east of Reading is defined by Natural England as the Thames Valley National Character Area ...
The Thames Archway Company was a company formed in 1805 to build the first tunnel under the Thames river in London . The development of docks on both sides of the river around the Isle of Dogs indicated that a river crossing of some kind was needed. A tunnel from Rotherhithe to Limehouse was suggested in about 1803 in which the Nothumbrian [1 ...
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 ...
After the river took its present-day course, many of the banks of the Thames Estuary and the Thames Valley in London were partly covered in marshland, as was the adjoining Lower Lea Valley. Streams and rivers like the River Lea , Tyburn Brook and Bollo Brook drained into the river, while some islands, e.g. Thorney Island , formed over the ages.
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