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Gentleman's Magazine 1747 p.523
No such disagreeable objects interrupt the traveller here;
if he guards against the precipices, he has no other danger
to encounter.
The most common plants which I observed are,
Adianthum nigrum officinarum (of Ray) black
maiden hair.
Lujula, acetosa sylvestris, wood or mountain sorrel.
Muscus squammosus montanus repens, sabinae folio.
Muscus clavatus juniperinis foliis reflexis, clavis
singularibus sine pediculis. Several mosses of the
capsulated kind.
Brush moss.
Rorella longifolia perennis, and other sun-dews.
The shrubs rising from the latices of the rocks, are dwarf
birch, dwarf mountain oak, of so untractable a genius that
no soil will meliorate it.
Fraxinus sylvestris, ornus montana, wild mountain
ash, with red fruit. I do not remember to have seen this
tree in the South, nearer than Derbyshire; it differs
both in size and leaf from the service tree, of which
species it is, according to the botanists, and is a very
beautiful one when the fruit is ripe; the superstitious use
it against witchcraft.
The only bird peculiar to these rocks is the raven.
It is a received Cumberland proverb, that the
mountains of Caudebeck are worth all England
besides, but it has not yet been verify'd by experience; and
if we may be allow'd to conjecture from the nature of their
stones, found in the rivulets and quarries, it may be
difficult to say when they will. Most of their lapilli are a
fluor of the stalactite kind, or a sparry talc resembling
white flint, variegated with hexagonal crystalline spars,
whose points will cut glass like the adamant, but
immediately lose that property from their fragil quality.
Others are impregnated with the marcasite of lead, but so
blended with an arsenical sulphur that they evaporate in the
process of separation, and others are of the copperas kind;
all of them containing such heterogeneal qualities in their
composition, as never to yield a proper gratification for
the tryal. Their quarries, also, only abound with a fissile
blue-ish slate, useful for the covering of their houses, but
very remote from the metalline nature: Indeed in
Brandlegill-beck, and the Northern descents, copper
has been formerly dug, but the mines are long since worn
out; hereabouts the lapis calaminaris is also found.
Under mount Skiddow is the head of the river
Cauda; it issues thro' a narrow trough, and takes its
winding course with great rapidity to Mosedale, where
it turns northward for Carlisle. Near two miles above
that village (Mosedale) it receives a small rivulet
from Bouscale-tarn, a lake near a mile in
circumference, on the side of a high mountain, so strangely
surrounded with a more eminent amphitheatrical ridge of
quarry rocks, that it is excluded the benefit of the sun for
at least four months, in the middle of winter; but this is
not its only singularity. Several of the most credible
inhabitants thereabouts, affirming that they frequently see
the stars in it at mid-day; but in order to discover that
phaenomenon, the firmament must be perfectly clear, the air
stable, and the water unagitated. These circumstances not
concurring at the time I was there, depriv'd me of the
pleasure of that sight, and of recommending it to the
naturalists upon my own ocular evidence, which I regret the
want of, as I question if the like has been any where else
observed. The spectator must be situated at least 200 yards
above the lake, and as much below the summit of the
semi-ambient ridge; and as there are other high mountains,
which in that position may break and deaden the solar rays,
I can only give an implicit credit to the power of their
agency, 'till I am convinc'd of their effects, and am
qualified to send it better recommended to the publick.
At Grisedale the water turns bothways, so that in a
sudden shower you may with your foot only, send the
rain-water, either to Carlisle or Cockermouth,
by the channels of Cauda or Lender-maken. This
last springs under Saddle back, a Parnassian
eminence, with two prominent peaks; the most northerly is
called Blencarter, a suprizingly high precipice of
the quarry kind.
Souter-fell is a distinguish'd mountain of itself,
encompass'd quite round with a turbinated trough,
thro' which the Lender-maken is convey'd. The West
and North sides are barricadoed with rocks, the East is more
plain but withal steep, and seemingly 900 yards in height,
but every where of difficult access. It was on this
Fell that the astonishing phaenomenon appear'd to
exhibit itself, which in 1735, 1737 and 1745 made so much
noise in the North, that I went on purpose to examine the
spectators, who asserted the fact, and continue in their
assertion very positively to this day.
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