Castlt Caq. by the KEV. PREBENDARY MEADE. the Soil
Castlt Caq. BY THE KEV. PREBENDARY MEADE. his town was anciently called Carith, and Kari. It T is situate on the brow of an elevated tract of land, which shelters it from the East, and which is part of that oolite chain which passes through England from the North East to the South West. The soil is a sandy loam, associated with the lower oolite, and was famous for the growth of potatoes before the occurrence of the fatal disease. On the hill above the town the quarries are worked, which supply the building-stone to this neigh- bourhood—a stone possessing that peculiar orange tint, which, in some localities, has given it the name of the “gingerbread rock.” Westward the descent leads im- mediately upon the extended level of the lias ; and, as is usual, the junction of the upper with the lower strata is marked by a great fertility of soil. The traveller who merely passes through the streets of Cary, or looks out of a carriage window at the station, can scarcely imagine how extensive and beautiful is the view from the eminence overhanging the town. Here the inhabitants have, of ancient usage, a pleasant and healthful resort ; where, emerging from the streets below, they may CASTLE CARY. 83 imbibe the purer breeze coming directly from the channel, and watch “ The golden sun Gallop the zodiac in his glistering car.” The objects presenting themselves to view from this point deserve, perhaps, more particular enumeration. The eminence itself is called Lodgehill, probably from its having been formerly the site of some ranger’s dwelling, or hunting box belonging to the lords of Castle Cary.
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