Gents Mag 1761 p.127

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	Gentleman's Magazine 1761 p.127 at length so steep that it cannot be ascended without great difficulty, and in some places not at all. In many parts there are fine quarries of slate, which the neighbouring inhabitants use to cover their houses, but no lime-stones; yet, near the base, no stones but lime-stones are to be found. The loose stones near the summit the people call greet stone. The foot of the mountain abounds with fine springs on every side, and on the west side there is a very remarkable spring near the summit. The top is very level, but so dry and barren that it affords little grass, the rock being but barely covered with earth. It is said to be about a mile in circumference, and several persons now living say, that they have seen races upon it. Upon that part of the top, facing Lancaster and the Irish Sea, there are still to be seen the dimensions of an house, and the remains of what the country people call a beacon, viz. a place erected with stones, three or four yards high, ascended with stone stairs; which served in old time, as old people tell us, to alarm the country, upon the approach of an enemy, a person always being kept there upon watch, in the time of war, who was to give notice in the night, by fire, to other watchmen placed upon other mountains within view, of which there are many, particularly Whernside, Woefall, Camfell, Pennygent, and Pennlehill. There are likewise discoverable a great many other mountains in Westmoreland and Cumberland, besides the town of Lancaster, from which it is distant about 20 miles. The west and north sides are most steep and rocky; there is, one part to the south, where you may ascend on horseback; but whether the work of nature, or of art, I cannot say. A part of the said mountain jutts out to the north east near a mile, but somewhat below the summit; this part is called Park-fell; another part jutts out in the same manner, near a mile, towards the east,and is called Simon-fell; there is likewise another part towards the south, called Little Ingleborough; the summits of all which are much lower than the top of the mountain itself. Near the base, there are holes or chasms called swallows, supposed to be the remains of Noah's deluge; they are among the lime-stone rocks, and are open to an incredible depth. The springs towards the east all come together, and fall into one of these swallows, or holes, called Allan Pott; and after passing under the earth about a mile, thay burst out again, and flow into the river Ribble, whose head, or spring, is but a little further up the valley. The depth of this swallow, or hole, could never be ascertained; it is about 20 poles in circumference, not perfectly circular, but rather oval. In wet foggy weather, it sends out a smoak, or mist, which may be seen a considerable distance. Not far from this hole, nearly north, is another hole, which may be easily descended. In some places the roof is 4 or 5 yards high, and its width is the same; in other places not above a yard; and was it not for the run of water, it is not to be known how far you might walk, by the help of a candle, or other light. There is likewise another hole, or chasm, a little west from the other two, which cannot be descended without difficulty: You are no sooner entered than you have a subterraneous passage, sometimes wide and spacious, sometimes so narrow you are obliged to make use of both hands, as well as feet, to crawl a considerable way; and as I was informed, some persons have gone several hundred yards, and might have gone much further, durst they have ventured. There are a great many more holes, or caverns, well worth the notice of a traveller: some dry, some having a continual run of water; such as Blackside Cove, Sir William's Cove, Atkinson's Chamber, &c. all whose curiosities are more than I can describe. There is likewise, partly south-east, a small rivulet, which falls into a place considerably deep, called Long-Kin; there is likewise another swallow, or hole, called Johnson's Jacket-hole,a place resembling a funnel in shape, but vastly deep; a stone being thrown into it, makes a rumbling noise, and may be heard a considerable time; there is also another, called Gaper-Gill, into which a good many springs fall in one stream, and after a subterraneous passage of upwards of a mile, break out again, and wind thro' Clapham; then afterwards a winding course of several miles, this stream joins the river Lon, or Lune; and, passing by the town of Lancaster, it falls into the Irish Sea: There likewise, both on the west and north sides, a great many springs, which all fall into such cavities, and bursting out again, towards the base of the said mountain, fall likewise into the Irish Sea, by the town of Lancaster; and what seemed very remarkable to me, there was not one rivulet running from
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