A Landscape in Motion
The meeting point of the Ayeyarwady and Chindwin rivers is a changing environment, constantly reshaped by water and sediment. The Chindwin River, the Ayeyarwady's largest tributary, contributes more than half of the total sediment load below the confluence. This massive influx of sand and silt, originating from the Indo-Myanmar Ranges, is the primary reason for the dramatic changes seen here. The river system forms a braided channel, a network of shifting, interleaving waterways separated by temporary islands and sandbars. This geomorphology is a direct result of a high sediment load combined with dramatic seasonal fluctuations in water discharge.
During the dry season, which peaks in February, the rivers are at their lowest. The confluence narrows, and vast sandbanks emerge, creating obstacles for navigation. The monsoon season, from May to October, completely transforms the landscape. The average monthly water discharge in August can be ten times higher than in February. At its peak, the combined flow of the Ayeyarwady can reach over 32,600 cubic meters per second. This tremendous volume of water submerges the sandbars, erodes the banks, and carves new channels, completely altering the river's path from one year to the next. The water level at Mandalay, upstream of the confluence, can vary by nearly 10 meters between the low and high seasons.