Unglaciated Unconfined:
channels below the lower limit of Pleistocene valley glaciation that have large valley-bottom widths (in our definition of this process domain, valley width > 125 m). These channels typically have lesser downstream bed gradients (< 2%) and finer bed sediment than confined channels.
Click a link below to learn about Unglaciated Unconfined 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: