These units include a unique landscape feature; the monadnock (residual hill) at Mt. Delegate. This unit is based on sedimentary terrain with some metamorphism. It dominates the landscape and forms a radial drainage pattern. This unit is generally steep, with less steep lower slopes which grade into the surrounding sedimentary/colluvial unit. There is also a river scarp (Queensborough River). Due to the rapid rise in elevation and a range of aspects the soil type varies from shallow stony lithosols to deep red friable gradational profiles in sheltered mid- to lower slopes. This rapid change in elevation also has a marked effect on the vegetation type and its distribution. The main native vegetation type is Montane Sclerophyll Woodland with some Dry Sclerophyll Forest, Montane Forest and Snow Gum Woodland (Mt. Delegate). Geology: Ou;. Ordovician sediments. Black slate, phyllite, shale, sandstone. Siltstone, minor schist, hornfels, contact rock, breccia, scree, quartzite. Rainfall: 700 – 1200 mm per annum, generally 700-1000 mm per annum. Slope: 32-56%. Dominant landform element: Slope. Minor landform element: Drainage depression. |