of the summer months decreased by 6%. The James Bay area's water flow is most affected by the hydroelectric project from January to April because rivers have their lowest runoff rates in the winter months when freezing occurs. Additionally, runoff rates in the damming system can be altered to meet power needs, which are highest in the winter and lowest in the summer, thereby more completely reversing the natural water flow cycle. As evidenced by the 500% increase in its winter runoff, the La Grande River is the pillar of the James Bay project's hydroelectric capacity, with the runoff increasing from an average yearly amount of 1,700 m3/s to 3,400 m3/s, and from 500 m3/s to 5,000 m3/s in the winter. This immense harnessing of the area's energy at La Grande was made possible by reducing the Eastmain River's water flow at its mouth by 90% and by reducing that of the Caniaspiscau River's by 45%, and then by diverting these rivers into La Grande. Not only does this alter the runoff amount of the Eastmain and the Caniaspiscau Rivers, but also their drainage location, since prior to having been directly merged with La Grande, these rivers’ drainage locations were separate from the La Grande River. The summer runoff rate of La Grande increased by 40%, making the average annual runoff rate 91% greater than its natural rate. Because of the change in the runoff rates of James Bay, massively increasing in the winter months, and increasing considerably in the summer as well, there has been more extreme fluctuation in the water levels. This has killed many trees along the shoreline, which are not equipped with deep enough root systems and tolerance of prolonged exposure to seawater to withstand these fluctuations. As well, the increased riverbank erosion downstream of the dams has washed the flora’s habitat down the river. The result has been considerable decay (decomposition) of dead trees along the shoreline, consequently releasing stored mercury into the area's terrestrial ecosystem through bioaccumulation in decomposers and detritovores and eventual biomagnification up the food web. This has left the area's Cree susceptible to mercury poisoning from both land and sea. Any shoreline plants that could potentially provide vegetation growth to replace any of the lost wetland habitats in these zones of periodic fluctuations are destroyed. Changes in migration routes Other changes in the delicate balance of the James Bay ecosystem can