| Geology Freshwater sediments, mainly alluvium and fan deposits, deposited during the Pliocene to Early Pleistocene Epochs (5 to 1.8 mya). Landform Rolling low hills. The terrain is weakly to moderately dissected. |
| ![]() |
![]() This photo indicates the position in the landscape of the Coongulla map unit and the density of the vegetation that occurs on it. |
This map unit is included within the Stockdale Land System as described by Aldrick et al. (1992). Soils Most of the soils on this map unit are texture contrast soils, with hard-setting gritty loam to fine sandy clay loam surface soils abruptly overlying yellowish brown and yellow mottled clays from about 25 to 40 cm. Quartz gravel and small stones are a common feature of these soils. Remnants of lateritic material, or strongly cemented conglomerate, often termed ironstone, may occur at the surface or within the soil profile. Small, localised areas of deep sand may occur within this map unit. ![]() Stony soil profile in road cutting near Lake Glenmaggie. |
This map unit is similar to Coongulla, but 30% or less of the area is comprised of the Glenmaggie map unit. | ![]() |