Gillingwater's History of Lowestoft: a reprint: with a chapter of more recent eventsGillingwater, Edmund
History
Gillingwater's History of Lowestoft: a reprint: with a chapter of more recent events
Gillingwater, Edmund
Lothingland (England); Lowestoft (England)
vicars to build or purchase parsonage-houses in those parishes where
there are none. It was also thought desirable, that a garden, the
property of the late Mr. Arrow, and not far distant from the house,
should be purchased; the purchase-money for which was £120, but included
in the £550 given. The deeds of conveyance executed on this occasion are
in the possession of the vicar.”
In 1831, the Rev. F. Cunningham purchased part of a garden and right of
way, which cost £77 7s. 3d., which he presented to the vicarage, and
likewise put the vicarage-house into a thorough state of repair.
The river Waveney in ancient days sought its junction with the Ocean
through Lake Lothing, between Lowestoft and Kirkley. Its channel, which
is proved to have been shallow, by the discovery of fossil elephants’
teeth, as already related, was open in Camden’s time, who calls Kirkley a
haven town. Reyce, who wrote his account of Suffolk a few years after,
describes it as still navigable, for he says, “and then Leystoffe, until
you come to that part of Yarmouth which is on the south side of the river
Hiere, do finish the number of our havens.” The sea, however, aided by
the fury of the eastern gales, gradually raised a barrier of sand and
shingle about a quarter-of-a-mile wide, by which all navigation was
finally interrupted. Still, whenever a violent storm arose from the
north-west in conjunction with a spring tide, the sea would flow into
Lake Lothing with great rapidity, and threaten the adjacent low grounds
with inundation. To guard against these irruptions, and prevent the
consequent damages, a break-water was formed on the sandy isthmus,
between Lowestoft and Kirkley, as a security for the marshes which lay
contiguous to the river. It is not, however, apparent when this
embankment was first complete; for, in a Commission of Sewers, held in
February, 1652, a levy was made to repair the breaches effected by the
ocean in this bank or walls. These operations must have been imperfectly
conducted, for even so late as 1712, a shallow channel was still
maintained between the sea and Lake Lothing; for it was then customary
for a man to stand there with boots on, to carry children through the
water, who went from Lowestoft to Pakefield fair. Subsequently, the
barrier was so greatly strengthened, that all apprehension of damage from
the ocean had vanished, when, on the 14th of December, 1717; the sea
forced its way over the beach with such irresistible violence, as to
carry away Mutford Bridge at the distance of two miles from the shore.
The writer has been led to assert, in his introduction to the Hundred of
Lothingland, from false information, that this was the last attempt of
the ocean to regain its ancient passage to the lake. Such, however, is
not the fact, for on the 2nd of February, 1791, a remarkable high tide
once more burst over the isthmus of sand, and again carried away the
bridge at Mutford, built in 1760. On this occasion the salt water flowed
Public-domain text, read in full here on John Shaqi.
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