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fractures and subsequent denudations.* Some of them rise to a considerable 

 height, commanding on all sides grand and extensive views over the adjacent 

 counties and the more distant mountains of "Wales. The intervening vallies are 

 also very picturesque and well wooded. The Railway Stations of Stoke Edith 

 »nd Holm Lacey now render it comparatively easy of access, and it only wants 

 to be better know to be more frequently visited. 



* It is an important question to decide what has become of the drifted matter, 

 the quantity of which must have been enormous ; and, as my friend Mr. Symonds 

 observes, the only drift in the neighbourhood, full of remnants of Silurian rocks, is to be 

 seen at Mordiford, and nowhere elie. 



t S 



