Online Services | Commonwealth Sites | Help | Governor

Welcome to the Virginia Department Of Forestry

Rosgen Class C4 Forest Reference Stream Monitoring Data

In his book Applied River Morphology, Dave Rosgen describes the C4 Stream Type as "a slightly entrenched, meandering, gravel-dominated, riffle/pool channel with a well developed floodplain."  He goes on to say that:

"The C4 stream type is found in U-shaped glacial valleys; valleys bordered by glacial and Holocene terraces; in mountain meadows and in very broad, course alluvial valleys. Some of the C4 stream types occur in glacial outwash terrain, closer to the lobe where gravel material is present."

"C4 stream channels have gentle gradients of less than 2%, display a high width/depth ratio, are slightly more sinuous and have a higher meander width ratio than the C1, C2 and C3 stream types. The riffle/pool sequence for the C4 stream type averages 5-7 bankfull channel widths in length. The streambanks are generally composed of unconsolidated, heterogeneous, non-cohesive, alluvial materials that are finer than the gravel-dominated bed material. Consequently, the stream is susceptible to accelerated bank erosion. Rates of lateral adjustment are influenced by the presence and condition of riparian vegetation. Sediment supply is moderate to high, unless streambanks are in a very low erodibility condition."

Resources Describing C4 Stream Geomorphology

Resources Describing C4 Stream Hydraulic Geometry

Resources Describing C4 Stream Turbidity

Last modified: Monday, 10-Mar-2008 15:31:55 EDT