Unglaciated Partially Confined
channels below the lower limit of Pleistocene valley glaciation that have moderate valley-bottom widths, typically as a result of close lateral confinement by the valley side slope on one side and greater width on the other side of the channel (in our definition of this process domain, valley width of 50-125 m).
Click a link below to learn about Unglaciated Partially Confined Channels:
| Channel Morphology | Disturbance Regime | Riparian Vegetation |
| In-Channel Wood and Beavers | Hillslope Influences | Aquatic Organisms |
To learn more about each process domain click a link below: