1. Multiple braided streams are usually present and active during water flows. 2. This type of sediment layering may create a " braided stream channel ". 3. In North America an anabranch is called a " braided stream ". 4. Braided streams occur in rivers with high slope and / or large sediment load.5. This bed sequence indicates an alluvial fan, meandering stream or braided stream origin. 6. An outwash plain might contain surficial braided stream complexes that rework the original deposits. 7. Below the reservoir a braided stream alternates with a single, small channel flowing through irrigated land. 8. Gravels exposed at Langport Railway Cutting show scour-and-fill structures consistent with braided stream deposition. 9. When these torrents reach the mouths of the canyons, they widen and slow, branching out into braided streams . 10. Host rocks are typically submature to supermature, polymictic conglomerates and sandstones deposited in alluvial fan and braided stream environments.
