The Slanter (The Stanter), Gilgunnia, Blaxland Co., New South Wales, Australia
|Latitude & Longitude (WGS84):||32° 24' 36'' South , 146° 2' 23'' East|
|Latitude & Longitude (decimal):||-32.41025,146.03985|
|Köppen climate type:||BSk : Cold semi-arid (steppe) climate|
|Age:||419.2 ± 3.2 to 393.3 ± 1.2 Ma|
|Geologic Time:||Early Devonian|
|Reference for age:||Gilligan, L.B., Suppel, D.W. (1993) Metallogenic Study and Mineral Deposit Data Sheets: Nymagee 1:250 000 Metallogenic Map (SI/55-2). Geological Survey of New South Wales, Sydney, 171 pages.|
A former gold mine operated via shafts and underground workings.
Operated circa 1897.
2 valid minerals.
Rock Types Recorded
Select Rock List TypeAlphabetical List Tree Diagram
Entries shown in red are rocks recorded for this region.
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
|Pragian - Ludlow|
407.6 - 427.4 Ma
Age: Paleozoic (407.6 - 427.4 Ma)
Stratigraphic Name: Amphitheatre Group
Description: Clastic sediments, undivided.
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).