|Latitude & Longitude (WGS84):||23° 25' 21'' South , 116° 58' 9'' East|
|Latitude & Longitude (decimal):||-23.42255,116.96920|
|Köppen climate type:||BWh : Hot deserts climate|
Approximately 4 kilometres south-east of Bali Lo, and 11 kilometres south-south-west of the Ashburton Downs homestead.
The secondary mineral assemblage at Bali South is distinguished from the Anticline and Bali Lo prospects mainly by the absence of beudantite, and other members of the alunite-beudantite-crandallite group, and by the presence of antimony rich minerals. The deposit appears to not be on the same anticlinal structure as Bali Lo and the Anticline prospect but its own fault zone.
16 valid minerals.
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
1600 - 2500 Ma
|Paleoproterozoic sedimentary rocks|
Age: Proterozoic (1600 - 2500 Ma)
Stratigraphic Name: Wyloo Group
Comments: Ashburton Basin
Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. 
1800 - 2050 Ma
Age: Orosirian (1800 - 2050 Ma)
Stratigraphic Name: Ashburton Formation
Reference: Raymond, O.L., Liu, S., Gallagher, R., Zhang, W., Highet, L.M. Surface Geology of Australia 1:1 million scale dataset 2012 edition. Commonwealth of Australia (Geoscience Australia).