Ordovician-silurian granodiorite. The map boundary was drawn on the basis of radiometric data as well as the geological map. As a result some highly metamorphosed sediments e.g. mica schists, may be included in this unit. The underlying rocks are similar to those underlying the Dargo map unit but the topography is much steeper. Accordingly, this map unit has remained largely uncleared.
Landform
Rolling to steep hills.
Soils
No soil profiles were examined. Rock outcrops were noted. If a sufficiently deep soil is formed, it is likely to be brown sandy clay loam overlying a brown or red medium clay (sandy).
Land Management
There is insufficient land which is cleared to make comments on land management issues.