History of the Fylde of LancashirePorter, John (Writer on the Fylde of Lancashire)
History
History of the Fylde of Lancashire
Porter, John (Writer on the Fylde of Lancashire)
Lancashire (England) -- History
No. of grains.
Water 964.74
Chloride of Sodium (Table salt) 27.06
Chloride of Magnesium 3.67
Sulphate of Magnesia (Epsom Salts) 2.30
Sulphate of Lime 1.40
Carbonate of Lime 0.03
Carbonate of Magnesia ⎫
Carbonic Acid ⎪
Potash ⎬ Traces
Iodine ⎪
Extractive matter ⎪
Bromide of Magnesium ⎭
----------
1,000
There are few, we imagine, who have not at one time or another admired
the luminous appearance of the sea on certain evenings. This astonishing
and beautiful phenomenon is brought about by the presence in the water
of myriads of tiny beings, called Noctilucæ, which possess the power of
emitting a phosphorescent light, and seemingly convert the bursting waves
into masses of liquid fire. The immense expanse of sea spreading out from
the westerly border of the Fylde has, independently of its association
with the Gulph Stream, a marked influence in equalising the climate and
averting those sudden and extreme degrees of heat and cold commonly
experienced inland. The atmosphere over water does not undergo such rapid
alterations in its temperature as that over land, and hence it happens
that localities situated near the coast are cooler in summer and warmer
in winter than others far removed from its vicinity. Most people will
have observed that after a calm sunny day at the seaside, a breeze from
the land invariably arises after sunset, due to the fact that the air
over the earth being cooled and condensed much sooner than that over the
sea, the heavier body of atmosphere endeavours to displace the warmer and
lighter one. A gentle evaporation is daily taking place from the surface
of the sea, by which the air becomes loaded with moisture, remaining
suspended until the coolness of evening sets in, when it is deposited
on the ground as dew. The water thus obtained from the deep is not pure
brine, as might at first sight appear, but is freed from its salts by
the process of natural distillation which has been undergone. Similar
evaporation also goes on from the surfaces of the Ribble and Wyre, and it
is doubtless chiefly owing to the Fylde being almost environed by water,
constantly disseminating dew, that its fecundity is not only so great,
but also so constant. The following is a list of the seaweeds to be found
on the coast:—
MELANOSPERMEÆ OR OLIVE GREEN SEAWEEDS.
TRIBE—FUCACEÆ.
Fucus nodosus Knobbed Wrack
” serratus Serrated ”
” canaliculatus Channelled ”
” vesiculosus Bladder ”
TRIBE—SPOROCHNACEÆ.
Desmarestia aculeata Spring Desmarestia
” viridis Green ”
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