The memorials of the hamlet of Knightsbridge : $b With notices of its immediate neighbourhood — John Shaqi
The memorials of the hamlet of Knightsbridge : $b With notices of its immediate neighbourhoodDavis, Henry George
History
The memorials of the hamlet of Knightsbridge : $b With notices of its immediate neighbourhood
Davis, Henry George
Knightsbridge (London, England)
In 1578, Mr. Walcot states only six persons were rated by the St.
Margaret’s overseers in Knightsbridge and Kensington; and in 1687 only
five people are rated in St. Martin’s books for the whole of Pimlico.
The progress of building appears to have taken place not so much
progressively as in two distinct movements. The first was from 1770 to
1780, and the other from 1825 to our own time; on examination, it will be
found that few of our streets were built at other periods. A letter
before me of a skilled carpenter, written in 1783, tells his friends in
the country he gets 2s. 8d. per day for his labour, and that he is
allowed to make seven days per week, “and if the peace continueth” he
shall be able to realise 20s. or a guinea per week; for his lodging he
paid 2s. per week. If this was a fair sample of the rate of wages then,
the mechanic’s financial condition must have improved to an extent little
credited perhaps by themselves.
The air of Knightsbridge has always been considered pure and salubrious.
Swift brought Harrison to the place for the benefit of pure air; and
fifty years since it still maintained the character, for Lady Hester
Stanhope sent a faithful footman here for the same relief. Constitution
Hill and Montpelier Square derived their names from this fact. The main
street of Knightsbridge, from Hyde Park Corner to Kensington, stands on a
peculiar but well-defined terrace of the London clay, which separates the
gravels of Hyde Park from those more southward, {269} and is rather more
than thirty feet deep. The yellow gravel of Hyde Park, says Sir Charles
Lyell, is, comparatively speaking, of modern date, consisting of slightly
rolled angular fragments, in which portions of the white opaque coating
of the original chalk-flint remain uncovered. Southward of the clayey
line just mentioned the surface soil is a “made” one. Underneath the
native earth are thick layers of sand, beneath which is a blue clayey
earth, and then a sediment, consisting chiefly of cockle and oyster
shells, which beautifully retain their appearance. Thus the soil of our
locality is a porous one, and rapidly absorbs the surface water; an
advantage greatly tending to the health of the inhabitants, for parts of
Pimlico are but slightly above high-water mark, and the air would
consequently be very moist and relaxing.
In a sanitary point of view all is not fair, even in Belgravia; behind
its imposing mansions many a foul spot is hypocritically hidden; and
although much has been done by the medical officer, there yet remains
plenty of work on hand for him: too many spots yet requiring thorough
transformation, and a vigilant watch to be kept, that selfishness be not
permitted to triumph over public good. {270}
Public-domain text, read in full here on John Shaqi.
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