404 M.S: UA PEELE: ON 
The rocks about the pool are waterworn in precisely the same 
way as the similar sandstones beneath the present falls at the 
village. The edges of the shaly lamine are frayed and rounded 
as appears in Fig. 4, which is a view of P looking from O in 
Fig. 2. Similar effects are observed on all the rocks about. 
Besides this fraying of: edges, a clear indication of water 
action, is the complete absence of glaciation about the pool, 
though elsewhere these sandstones and shales show unmistaka- 
ble smoothing and grooving on every ledge. Here, despite the 
rounding in detail, the mass contours of the rocks are sharp and 
jagged. They have been deglaciated in the rush of waters. 
