Glaciated Confined:
channels above the lower limit of Pleistocene valley glaciation that have small valley-bottom widths as a result of close lateral confinement between valley side slopes (in our definition of this process domain, valley width < 50 m). These channels typically have steeper downstream bed gradients (> 2%) and coarser bed sediment than unconfined channels.
Click a link below to learn about Glaciated 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: