Cover at Havieron22 Dec 2020 06:08
The Box cut geology Part1
Quaternary Superficial
Undifferentiated COVER (aeolian sand, alluvium, and evaporates)
5-15m thick.
QUATERNARY/PERMIAN UNCONFORMITY Permian Paterson
Upper Mudstone (UMW) 95-105m thick
Upper Tillite (UMT) 60m thick
Upper Siltstone (LCS) 85m thick
Middle Sandstone (LST) 25m thick
Lower Siltstone (LSL) 35 m thick
Lower Tillite (LFT) 95m thick
Deep Sands are wind-blown aeolian sands associated with sand dunes present throughout the landscape. These soils are dominated by fine sands with no appreciable silt or clay and no pedological development.
• Gradational Loams are characterised by a thin layer of wind-blown aeolian sands that grade rapidly to sandy loam, with a gradual increase in clay content from clay loam to light clay at depth. The influence of wind-blown aeolian sands are less apparent in these soils.
• Gradational Sands are similar to the Deep Sands, except for a change in texture from sand to loam in the deeper B horizon. These soils are characterised by a buried horizon at depth that represents the original soil profile that was covered in wind-blown aeolian sands.
During mining, extraction of resources is proposed to first be undertaken from within the boxcut area and then later, from the decline, with approximately 260,000 m3 of waste proposed to be extracted during this process.
The boxcut area consists of surface layers that have undergone soil forming processes (tertiary cover), and the saprolith positioned below the pedolith that has properties similar to those of the underlying parent material (fresh rock). There are two major horizons in the saprolith, Saprolite and Saprock (Completely Weathered/Oxidised). The base of complete oxidation (BOCO) tends to be approximately 10-50 m below the surface, and the top of the fresh rock (TOFR) approximately 25-100 m below the surface.
• All materials except for the Tertiary Cover, Upper Tillite and Lower Tillite, have clay contents >10% in addition to a considerable proportion of silt and fine sand content. This indicates that these materials have the greatest risk of structural decline, given these materials are also prone to particle breakdown.
• Lower Tillite recorded the highest rock densities and lowest water absorption values. Rock strength was observed to vary based on depth, with Lower Tillite extracted from depths of ~330- 470 m exhibiting highest average rock density and lowest average water absorption, therefore this material is highly suitable for use as a rock armour on outer landform faces.