Kara Mine, Hampshire, Tasmania

Introduction
A number of skarn type assemblages exist at the Kara Mine, near Hampshire, Northwest Tasmania. The skarns occupy a trough-like pendant within late Devonian red granite known as the Housetop Granite. At the Kara No.1, ore-grade scheelite mineralisation forms an irregularly-shaped blanket draped 15-25m above the granite. Between the skarn and the granite is a tungsten-poor, quartz-epidote reaction zone (Whitehead, 1990).

Open pit mining of scheelite has been in progress since 1977. Magnetite is also of economic importance.

Minerals

Actinolite Felted green mats
Allanite Minor amounts recorded in the associated granite (Whitehead, 1990)
Andradite Colours from very pale yellow, green, red, brown and black. Forms include pentagonal dodecahedron and combination of dodecahedron and trapezohedron
Anthoinite As a white powdery mixture with mpororoite pseudomorphing scheelite (Matsubara & Kato)
Bavenite Sprays of transparent colourless crystals with a thomsonite-like habit is a rare calcium beryllium silicate. These are associated with fluorite, pyrite and epidote.
Biotite Recorded in the associated granite (Whitehead, 1990)
Calcite As crystals in a variety of habits including: short hexagonal prisms; long hexagonal prisms with flat terminations; long hexagonal prisms with pyramidal terminations. Also as vein infillings in magnetite: white to clear, some with bright pink long-wave fluorescence; golden opening to mamillary surfaces in cavities.
Chalcopyrite
Danalite As red poorly crystalline masses. Possibly the source for the beryllium in bavenite.
Diopside Recorded by C. Whitehead
Epidote Transparent lustrous green crystals
Feldspar K-feldspar recorded in the associated granite (Whitehead, 1990)
Fluorapatite Minor amounts recorded in the associated granite (Whitehead, 1990)
Fluorapophyllite Clear very lustrous crystals may be fluorapophyllite
Fluorite Clear to deep purpleoctahedrons to 5mm in cavities with epidote, pyrite, ?actinolite, and bavenite. Also as druzy secondary colourless octahedral microcrystals in the same cavities. As pink to purple octahedrons enclosed in calcite. Also recorded as minor amounts in the associated granite (Whitehead, 1990).
Halloysite Light brown and earthy (Matsubara & Kato)
Hedenbergite
Horneblende Black fibrous crystals, species not yet determined.
Magnetite Black massive, bright crystals including octahedral, dull crystals to 20mm. Also recorded as minor amounts in the associated granite (Whitehead, 1990).
Malachite As blue-green to bright green rosettes
Molybdenite Small rosettes
Montmorillonite Yellowish green and earthy in "the old trench" (Matsubara & Kato)
Mpororoite As a white powdery mixture with Anthoinite pseudomorphing scheelite (Matsubara & Kato)
Plagioclase An30 recorded in the associated granite (Whitehead, 1990)
Prehnite As pale green botryoidal coatings - to be confirmed
Pyrite As cubes, cube-octahedra
Quartz Recorded in the associated granite (Whitehead, 1990). Found as crystals in cavities in magnetite.
Scheelite Mainly as blebs in magnetite to a few cm across, occasionally as white crystals
Stolzite Orange crystals with epidote
Titanite (Sphene) Crystals not dissolved when calcite etched suspected to be titanite (F. Doedens, pers. comm.). Also recorded as minor amounts in the associated granite (Whitehead, 1990).
Tremolite Fibrous brownish crystals with actinolite and a dark olive green radiating silicate thought to be tremolite
Vesuvianite Recorded by C. Whitehead and confirmed by XRD
Wollastonite
Zircon Minor amounts recorded in the associated granite (Whitehead, 1990)

References
Matsubara, S. & Kato, A., 1984, Mpororoite & Anthoinite from the Kara Mine, Tasmania, Mineralogical Magazine, 48, 397-400
Whitehead, C.H., 1990, Kara Scheelite-Magnetite Deposit, 10th Australian Geological Convention, Hobart 1990, Excursion Guide E2, "Tin & Tungsten Deposits & Related Devonian Granitoids", Geological Survey of Australia