The History of Lynn, Vol. 1 [of 2]Richards, William
History
The History of Lynn, Vol. 1 [of 2]
Richards, William
Fens, The (England); King's Lynn (England)
“The soil to which the trees are fixed, and in which they grew, is a
soft greasy clay; but for many inches above the surface, the soil is
composed of rotten leaves, scarcely distinguishable to the eye, many
of which may be separated by putting the soil in water and
dexterously and patiently using the Spatula, or blunt knife. By this
method I obtained some imperfect leaves of the _Ilexaquifolium_,
which are now in the Herbarium of the right honourable Sir Joseph
Banks; and some other leaves, though less perfect, seem to belong to
some species of willow. In this stratum of rotten leaves we could
also distinguish some roots of _Arundo Phragmites_.
“These islets, according to the most accurate information, extend at
least twelve miles in length, and about a mile in breadth, opposite
to Sutton shore. The water without them toward the sea, generally
deepens suddenly, so as to form a steep bank. The channels between
the several islets, when the islets are dry, in the lowest ebbs of
the year, are from four to twelve feet deep: their bottoms are clay
or sand, and their direction is generally from east to west.
“A well, dug at Sutton by Joshua Searby, shews that a moor of the
same nature is found under ground in that part of the country, at the
depth of sixteen feet, consequently very nearly on the same level
with that which constitutes the islets. The disposition of the
strata was found to be nearly as follows: clay sixteen feet; moor,
similar to that of the islets, three or four ditto; soft moor, like
the scourings of a ditch bottom, mixed with shells and silt, twenty
feet; marly clay, one foot; chalky rock, from one to two feet; clay,
thirty-one yards; gravel and water; the water has a chalybeate taste.
In order to ascertain the course of this subterraneous stratum of
decayed vegetables, Sir Joseph Banks directed a boring to be made in
the fields belonging to the royal Society in the parish of
Mablethorpe. Moor of a similar nature to that of Searby’s well, and
the islets, was found very nearly on the same level, about four feet
thick, and under a soft clay.
Public-domain text, read in full here on John Shaqi.
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