John Fardy Lode, Cordillera Mine, Tuena, Georgiana Co., New South Wales, Australia
|Latitude & Longitude (WGS84):||34° 5' 1'' South , 149° 24' 15'' East|
|Latitude & Longitude (decimal):||-34.08376,149.40435|
|Köppen climate type:||Cfb : Temperate oceanic climate|
Part of the Cordillera Mine - operated around 1888-89.
10 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
|Lochkovian - Ludlow|
410.8 - 427.4 Ma
|Campbells Group undifferentiated sediments|
Age: Paleozoic (410.8 - 427.4 Ma)
Stratigraphic Name: Campbells Group undifferentiated sediments
Comments: sedimentary siliciclastic; synthesis of multiple published descriptions
Lithology: Sedimentary siliciclastic
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).