It is foreign to my plan to enumerate, and it might be difficult to discover, all the changes and revolutions which have taken place here; and I shall merely mention, that this district formerly constituted a regal forest, and we find Robert Fitzharding holding it by grant in the time of King John. We have a “lodge farm,” it is true, and the adjoining grange, the “conygar,” _i. e._ coneygard, the rabbit-keeper’s dwelling, may, perhaps, have been the situation of the sylvan warren; but there are no remains, or any other indications, of a forest ever having been in existence. Names and traditional tales are all that remain in most places now to remind us of the ancient state of England, or to make credible the narratives of our old historians, who lived when Britain was a forest. Where shall we look for the remnants of that mighty wood, filled with boars, bulls, and savage beasts, that surrounded London? Even in our own days, heaths, moors, and wilds, have disappeared, so as to leave no indications of their former state but the name. Woods and forests seem to be the original productions of most soils and countries favorable for the abode of mankind, as if inviting a settlement, and offering materials for its use. As colonies increase, wants are augmented; the woods are consumed; the plow is introduced, division of property follows; a total change and obliteration ensues, though the ancient appellation by which the district was known yet continues. The parish consists in parts of a poor, shattery gray clay, beneath which we find, in some places, a coarse lias; in others a spongy, rough, impure limestone; in other parts a thin stratum of soil is spread over an immense and irregular rock of carbonate of lime, running to an unknown depth: this in many cases protrudes in great blocks through the thin skin of earth. The rock, though usually stratified, has no uniform dip, but trends to different directions; in some places it appears as if immense sheets of semifluid matter had been pushed out of the station it had settled in, by some other or later-formed heavy-moving mass, or met with an impediment, and so rolled up: that these sheets had not fully hardened at the time of being moved is yet made probable by the whole crystallization of the mass being interrupted; so that no part adheres firmly, but separates into small shattery fragments when struck. This substance we burn in very large quantities for building purposes, and for manure, which, by the facility which we have of obtaining small coal, is rendered at the low rate of three-pence a bushel at the kiln. Our farmers, availing themselves of this cheap article, use considerable quantities, composted with earth, for their different crops, at the rate of not less than a hundred bushels to the acre. This is a favorite substance for their potato land. The return in general is not so large as when grown in manure from the yard; but the root is said to be more mealy, and better flavored.