Forestry is the dominant land use on teh north-eastern boundary of the catchment. This area is particularly important with respect to water supply catchment. |
0.36% of CMA region | |
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Open forests with deep soils on undulating slopes | |
Cleared pine forestry plantation with new seedlings | |
Component | 1 | 2 | 3 | 4 |
Proportion of soil-landform unit | 20% | 15% | 60% | 5% |
CLIMATE Rainfall (mm) | Annual:1000 | |||
Temperature (oC) | Minimum 6, Maximum 16 | |||
Precipitation less than potential evapotranspiration | October-March | |||
GEOLOGY Age and lithology | Ordovician marine sediments with minor Recent clay, sand and gravel and basalt | |||
Geomorphology | ||||
LANDUSE | Uncleared: Nature conservation; water supply; sport and recreation; residential development; softwood plantations Cleared: Softwood plantations; water supply; residiential development; sheet and beef cattle grazing | |||
TOPOGRAPHY Landscape | Rolling hills | |||
Elevation range (m) | 560-740 | |||
Local relief (m) | 30 | |||
Drainage pattern | Dendritic | |||
Drainage density (km/km2) | 2.2 | |||
Landform | Hills | |||
Landform element | Crest and steep slope | Sloep with deep soil | Slope with shallow soil | Drainage line |
Slope and range (%) | 12 (5-20) | 10 (5-20) | 20 (5-30) | 2 (1-4) |
Slope shape | Convex | Straight | Straight | Concave |
NATIVE VEGETATION Ecological Vegetation Class | Herb-rich Foothll Forest/Shrubby Foothill Forest Complex (49.6%); Shrubby Foothill Forest (4.1%); Sedgy Riparian Woodland (3.4%); Herb-rich Foothill Forest (2.0%) | |||
Dominant species | E. obliqua, E. dives, E. radiata, E. rubida | E. obliqua, E. viminalis, E. radiata, E. rubida, E. cypellocarpa | E. obliqua, E. viminalis, E. radiata, E. rubida, E. dives | E. obliqua, E. viminalis, E. radiata, E. rubida |
SOIL Parent material | In situ weathered sandstone and shale | In situ weathered sandstone and shale | In situ weathered sandstone and shale | Alluvium, colluvium clay, silt, sand and gravel |
Description (Corangamite Soil Group) | Shalow stony brown gradational soils (25) | Red texture contrast and red gradational soils, fine structure (26) | Brown, grey or yellow texture contrast and brown, grey or yellow gradational soils (25) | Brown gradational (earth) soil (34) |
Soil type sites | ||||
Surface texture | Gravelly loam | Fine sandy loam to clay loam | Fine sandy loam to clay loam | Clay loam |
Permeability | High | High | Moderate to high | Moderate |
Depth (m) | 0.5 | 2 | 1 | 2 |
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS | Steep slopes and low permeability leads to overland flow. This flow often creates sheet and rill erosion with major rainfall events. Leaching of salts also occur. | Steep slopes and low permeability leads to overland flow. This flow often creates sheet and rill erosion with major rainfall events. Leaching of salts also occur with nutrient decline. | Steep slopes and low permeability leads to overland flow. This flow often creates sheet and rill erosion with major rainfall events. Leaching of salts also occur with nutrient decline. | Moderate permeability and overland flow are common. Subsurface waterlogging is seasonal.. Gully erosion and leaching of salts also occur. Surface compaction can benefit from controlled traffic. |