Page:The parochial history of Cornwall.djvu/145

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All the cultivated parts of this parish, north and north-west of the town, rest on this rock: and the barren parts on a schistose rock, which is very siliceous, affording by its partial disintegration no more than a shallow, meagre soil; silica predominating in the one, and argillaceous earth, or alumine, in the other. The characteristic rocks of these genera occur next to the granite in the parishes of Blisland and St. Breward, and they will be noticed in the description of the latter parish.


The editor is aware that the article Bodmin has extended to a very great length. It might easily have been extended much further from interesting materials collected by Mr. Wallis relative to the past and present state of this chief seat of our ecclesiastical establishments. On their abolition the town unquestionably fell into great decay, till about the middle of the last century, when roads were made in all directions, and Bodmin, from being almost inaccessible by the modern system of travelling, became an extensive thoroughfare; the market has grown into one of the first in Cornwall, and the whole town is renovated by trade and industry.

If any further apology is required, the editor hopes that he may be excused for some partiality towards a place which he has represented in eight successive Parliaments, after as many unanimous elections.




Is situate in the hundred of East, and hath upon the north, Pillaton; south, Salt-Ash, and part of St. Stephen's; east, Landulph; west, Landrake. For the first name, it signifies "Flemings' Parish;" for bio, bleau, pleu, in Cornish, is of that signification (viz. a parish);