no K I L L A R N E Y. 



rocky declivity ; clofe to the torrent ftream, 

 which breaks impetuoufly from rock to rock, 

 with a roar that kindles expectation. The pic- 

 ture in your fancy will not exceed the reality ; 

 a great ftream burfts from the deep bofom of a 

 wooded glen, hollowed into a retired recefs of 

 rocks and trees, itfelf a moft pleafing and ro- 

 mantic fpot, were there not a drop of water ; 

 the firft fall is many feet perpendicularly over 

 a rock, to the eye it immediately makes another, 

 the bafon into which it pours being concealed j 

 from this bafon it forces itfelf impetuoufly be- 

 tween two rocks; this fecond fall is alfo of a 

 confiderable height, but the lower one, the 

 third, is the, moft confiderable, it iffues in the 

 fame manner from a bafon hid from the point 

 of view. Thefe bafons being large, there ap- 

 pears a fpace of feveral yards between each fall, 

 which adds much to the pifturefque fcenery> 

 the whole is within an arch of wood, that 

 hangs over it ; the quantity of water is fo con- 

 fiderable as to make an almoft deafening noile, 

 and uniting with the torrent below, where the 

 fragments of rock are large and numerous, 

 throw an air of grandeur over the whole. It 

 is about feventy feet high. Coaft from hence 

 the woody ihores of Tomys and Glena, they 

 are upon the whole much the moft beautiful 

 onesl have any where feenj Glena woods hav- 

 ing more oak, and fome arbutus's, are the 

 finer and deeper ihades; Tomys has a great 

 quantity of birch, whole foliage is not fo lux- 

 uriant. The reader may figure to himfeif what 

 thefe woods are, when he is informed that they 



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