• 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.