Located in northeast Oregon is the Wallowa Mountains, which contain a rich and understudied glacial history. In order to quantify the number of glaciation stages that have occurred in this locality I will examine twelve lateral moraines that border Wallowa Lake. This beautiful lake stretches 3 and a half miles north to south with a large, bordering moraine on each side and a terminal moraine at the north end. On the west side of the lake there are four moraines and on the east there are eight. As you move from the closest moraine to the farthest from the lake the respective ages of each moraine get older. There has been some age correlation between the west and some of the east moraines as illustrated in Crandell’s “Glaciation at Wallowa Lake,
