- Großarl and Hüttschlag represent historic copper mining towns that were primarily active during the 15th and 17th centuries
- 3 main deposit locations: Tofern, Schwarzwand and Karteis
- Historical production figures generally show average Cu contents of > 1.0%
Deposit characteristics (according to Weber, 1997 “Handbuch der Lagerstätten“)
- Deposit type: Vulcanosedimentary-exhalative
- stratiform pyrite mineralisation with high grade Cu (Tennantite-Tetrahedrite series)
- Ore-bearing structures: Elongated, low-thickness lenticular ore bodies and enrichments
- Mineralogy:
- Primary: Pyrite, chalcopyrite, magnetite, chlorite
- Associated: Pyrrhotite, hematite and traces of bornite, galenite, fahlore (i.e., grey copper ore) and arsenopyrite
- Host rock: Metavolcanites (Tuffs and tuffites)
- Copper reserves/resources* (Status of 1975; metal content in t):
- A + B + C Vorräte (Austrian resource standard): (1,0 %) 1,000 t Cu
- Potential resources: (1,0 %) 5,000 t Cu
- Special feature: Quartz veins in the green schists sometimes carry epigenetic bornite mineralisation rich in free gold
Priority exploration targets and historical data*
- Karteis:
- Hosts 3-4 adits, which are still accessible through tunnels
- Presence of abundant and coarse-grained chalcopyrite
- Quartz-pyrite bank with 3-4% Cu and about 35% S
- Average Cu-value of >2 % from pyrite and Cu-enriched samples
- 8 % Cu in chalcopyrite sample
- Length of the deposit is about 2 km and was mined to a depth of 60m
- Presumption of another parallel deposit
- Kreeberg:
- Represents a straight continuation of the Karteis deposit
- Individual samples taken from outcrops in 1918 showed a Cu-content of 2.4% to 7.5% in the chemical analysis.
- Ores were mined continuously from the surface to a depth of 200 m and a thickness of 24 m
- In addition, the Kreeberg deposit should contain coarse nickel ores
- Tofern (Alt- and Astentofern):
- Tofern is separated by the Tofernbach into two deposit parts, namely "Alttofern" and "Astentofern". The latter is said to be particularly rich in copper minerals.
- Soil material from the valley floor yielded 9000 ppm Cu (After a soil survey from the Environmental Protection Department of the Salzburg Provincial Government)
- Total length of mineralised zone is 7 km
- Astentofern contains the longest gallery of the Großarl mining area, which is about 1000-1100 m long
* Data collected from historical reports from 1937/38, as well as from a governmental soil survey from 1998
Current work program
- License area expansion by >100% to cover the entire known copper producing district.
- Systematic field sampling and mapping of all historic targets.
- 3D spatial modeling of all historic data and records.
- Drone aeromagnetic survey to investigate extension zones to known deposits.
- Submission of drill permit applications to test historic deposits for compliant Cu-Au-Ag grades.






