LOCAL GLACIATION IN CATSKILL MOUNTAINS 119 



each of which had its glaciers. The first of these has a morainic loop 

 just as perfect, though not so large, as the one which holds the lake. 

 It shows even better the lateral moraines on each side running diag- 

 onally down the hill and joining in the terminal loop. Within this 

 moraine, and concentric with it is another smaller, though very distinct, 

 loop. Between these moraines and the mountain, the bottom of the 

 basin is moraine-filled like that of the larger valley already described. 



Fig. 4. — A view along the moraine front from the point where the loop joins the 

 hillside. Above this point the lateral moraine continues for nearly half a mile up 

 the hillside. Below, it swings in a beautiful crescent across the valley. 



The second basin is less pronounced than the first, and contains, 

 consequently, a less conspicuous, though perfectly distinct, moraine. 



Between the terminal moraine and the mountain is a hummocky 

 topography resembling that in the other basins. 



The remaining basin, lying west of the lake, I did not examine 

 closely. It is thickly wooded, and may or may not contain local 

 moraines. 



