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Wye during the most romantic and meanderin" part of its course, extending fromį'in-Co))t Hill to Miller's Dale. Mnnsal Dale is jjarticularly interesting. Geologist may trace in it the four limestone strata, with three of the intervening beds Bonsai Dale extends two miles west from Cromford. The high and elevated rocks in this grand dale areĬalled Dove Dale Church, Lover's Leap, Pickering's Sugar Loaves, Tissington Spire.s, Nearly north-west of Thorpe, between Derbyshire and Staflbrdshire, about five milesĪlong the course of the Dove. Of the dales or valleys, Dove Dale is undoubtedly the most celebrated. That have obtained the name of Caverns are natural chasms or exhausted and neg. Smaller dimensions in various parts of the Peak : but it is doubtful whether some There are other caves, some of them abounding with crystals and stalactites of The latter is entered by a curious natural arch or portico. Subterranean scenery, liei/nard's Cavern and Hall are situate in Dove Dale, and are wonderfully diversified in positionĪnd extent as well as in the grotesque forms of the concretions and their awful The caverns at Matlock B Uh are numerous : they are called the liatland, the Cum-īerlanJ, the Fluor, the Devonshire, cVc. Generally called the Crystallized Cavern, is situate south-west of Bradwell, andĮxtends through numerous subterranean chambers, above four hundred yards. South of Eyam Church, is small but very rich in beautiful concretions or stalactites.īagsl)aw''s' Cavern, which, on account of the superior elegance of its stalactites, is In the limestone rock, north of a village called Peak-Forest town - jMerliti's Cave, Stream of accumulated waters vents itself through this chasm - Pool's Hole isĪbout half a mile south-west of Buxton - Elden Hole is a very deep o])en hole It"has a wide entrance, with a concreted roof, and in rainy seasoris a
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The most remarkable are Peak Cavern or the DcviVs Cave atĬastleton. The caverns or chasms in the lower limestone rock are among the peculiar fea. Substances immersed for any time in their waters. Which being replete with calcarious particles appear to petrify pieces of wood or other Nated, with salt, sulphur, or witli mineral combinations. Hav and West Hallam are powerful saline and chalybeate springs, which rise in theĬoal shale In all the mountainous ridges, springs are discovered variously impreg. Resembles that at Harrogate, but is much weaker. S])ring At Kedleston park, east of the elegant mansion of Lord Scarsdale, there isĪ medicinal spring, sulphureous and salt. Have termed the great Derbyshire Fault At MatUick town there is a chalybeate. They rise in thatĮxtensive disruption of the chain of limestone rocks, which the geological writers The temperature of the springs is fiti degrees. Matlock is known as well by its bold and beautiful scenery asīy'its h()t baths. In the midst of this dislocation the interesting river Grees and on the opposite sides of the dislocated limestone, west of Buxton, thereĪre cold springs and a bath.
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X)r with an elegant 3Iap of the Counttj, 'i
#Phlo fly rods full
Full text of " The Peak guide, containing the topographical, statistical, and general history of Buxton, Chatsworth, Edensor, Castlteon, Bakewell, Haddon, Matlock, and Cromford with an introduction, giving a succinct account of the trade and manufactures of the county an alphabetical list of noblemen and gentlemen's seats, and several road sketches.