The Tonle Sap Lake is the most prominent feature on the map of Cambodia - a huge dumbbell-shaped body of water stretching across the northwest of the country. In the wet season, the lake is one of the largest freshwater lakes in Asia, swelling to an expansive 12,000 km2. During the dry half of the year it shrinks to as small as 2500 km2, draining into the Tonle Sap River, which meanders southeast, eventually merging with the Mekong River at the 'chaktomuk' confluence at Phnom Penh. During the wet season a unique hydrologic phenomenon causes the Tonle Sap River to reverse direction, filling the lake.
The engine of this phenomenon is the Mekong River, which becomes bloated with snow melt and runoff from the monsoon rains. The swollen Mekong backs up into the Tonle Sap at the point where the rivers meet at Chaktomuk, forcing the waters of the Tonle Sap River back into the lake. The inflow expands the area of lake more than five-fold, inundating the surrounding forested floodplain and supporting an extraordinarily rich and diverse eco-system.
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