The big rivers of Myanmar move enormous amounts of silt. Their water is brown and their banks
muddy. Some of the land around the Gulf
of Motama walks around, with erosion reducing land in some places and
sedimentation creating new lands elsewhere.
Both processes create issues.
Reduction of arable land and increased salinization on the one hand and
conflicts over land rights on the newly established flats on the other.


To unload, you
reverse the process: you pump water into
the hold to recreate a slurry and you pump that into a small dyked area. The sand settles there and the water runs
back in the river. It is high quality
sand, fine and uniform in shape. The
gravel less so: it often needs to be
shifted at the ultimate jobsite.
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