Inverted channels formed from accumulated sediments that were cemented by minerals.

A new channel formed 3 miles from the old town, leaving an evil-smelling swamp around the ancient wharves.

Aggradational channels commonly form where the slope is "below grade".

The channel forms the primary navigational conduit for Portland's harbor and riverside industrial areas.

At around 36 N, the channels form an anastomosing (braided) pattern.

The eastern channel formed the boundary between Yorkshire and Lincolnshire.

It is thought that these channels may form heterodimers where their expressions co-localise.

Next a stream channel formed over the land, dumping coarse sand with feldspar.

Sand bars, tow-head islands and new, multiple channels form often and constantly change.

A new channel formed within the old lake bed.