Class
|
Rating
|
Example criteria
|
Management implications
|
VL
|
Very low
|
- Blocky colluvial deposits
- Terrain dominated by competent bedrock
|
No or only very minor surface erosion.
|
L
|
Low
|
- Morainal veneers; most rubbly colluvial deposits with high coarse fragment content
|
Expect minor erosion of fines in ditch lines and disturbed soils.
|
M
|
Moderate
|
- Morainal blankets (depends on texture and coarse fragment content; varies across the province)
- Glaciofluvial gravels
- Soft, friable bedrock
|
Expect moderate erosion when water is channeled down road surfaces or ditches.
|
H
|
High
|
- Some morainal blankets steeper than 60%, or steeper than 30% if gullied or poorly drained (depends on texture and coarse fragment content; varies across the province)
- Fine textured lacustrine (silts & clays), glaciolacustrine, glaciomarine, glaciofluvial or aeolian silts, slopes less than 15%
- Glaciofluvial or fluvial sands with low bulk density, slopes less than 30%
- Colluvial deposits derived from the above materials with the same slope or moisture criteria
- Colluvium derived from soft, friable rock (e.g., soft phyllites, some pyroclastics), steeper than 60% or steeper than 30% if gullied
|
Significant erosion problems can be created when water is channeled onto or over exposed soil on these sites.
|
VH
|
Very high
|
- Fine textured lacustrine (silts & clays), glaciolacustrine, glaciomarine, glaciofluvial or aeolian silts, slopes steeper than 15%, or gullied or poorly drained.
- Glaciofluvial or fluvial sands with low bulk density, steeper than 30% or gullied or poorly drained
- Peat, organic soils or tufa on sloping ground
- Colluvial deposits derived from the above materials with the same slope or moisture criteria
|
Severe surface and gully erosion problems can be created when water is channeled onto or over these sites.
|