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Description
Billabong ( BIL -ə-bong) is an Australian term for an oxbow lake, an isolated crescentic pond left behind after a river loop is cut off when the river channel changes course. Billabongs are usually formed when the path of a creek or river changes due to bank erosion, leaving the former channel deprived of further inflow and becoming a dead-end gully holding only residual water that has not yet drained or evaporated. As a result of the arid climate of many parts of Australia, these "dead rivers" often fill with water seasonally but can be dry for a greater part of the year.
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