THE SEAWALL OF GEORGETOWN Construction of the Sea Wall began in 1855 after a flood in February of that year inundated the Kingston ward of Georgetown and washed away Camp House (the former residence for governors of the colony). The first section, which ran from Fort Groyne to Round House was completed by 1860. In 1874, the Public Works department of British Guiana committed to the construction of a continuous wall from Camp Street to Kitty. By 1882, the Sea Wall had been extended to reach as far as Unity Village. Seawalls were found necessary because of constant erosion of land by the sea. Historians note that two estates, Kierfield and Sandy Point, Guyana, known to be existing in 1792 north of the present Georgetown Seawall, were completely washed away by 1804. Earth walls are called sea-dams. The foreshore is subject to cycles of erosion and accretion. (Tables of erosion and accretion, started by G.O. Case have been maintained by the government). It appears that accretion in the early 1840s was followed by erosion in the late 1840s. By 1855, the great Kingston Flood took place when the sea-dam was breached. It was after this catastrophe that the sea wall between Fort William Frederick and the Round House was started in 1858. Built principally by convict labor with granite from the Penal Settlement at Mazaruni (now Mazaruni Prison), it was completed in 1892. In 1903 the Georgetown Seawall Bandstand was built with funds subscribed by the public as a memorial to Queen Victoria. The shelter north of the bandstand, called the Koh-i-noor Shelter, was erected in 1903. Serious flooding resulting from breaches in the sea wall took place at Enmore in 1955, at Buxton in 1959, and at Bladen Hall in 1961.
Posted on: Tue, 02 Sep 2014 11:18:13 +0000
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