Geography
Husky Lakes are tidal lakes, with tide heights averaging 2 m, and occupy a fault zone separating geological blocks. The lakes are almost partitioned into several separate water bodies by bow-shaped, nearly parallel, ridge-like peninsulas that project across them from north and south shores. These relic ice-pushed ridges narrow the lakes to less than 50 m in places and are highest at the inland end of the lakes, reaching heights of 30 m. Inland the lakes are shallow (10 m) and flat-bottomed, deepening towards the outlet to 66 m with uneven lake beds.