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RB 80/00089 Yunta town water supply. 1979 groundwater investigation.
3 of 6 wells were drilled along a water course 5 km west of Yunta, obtaining supplies of over 30 kl/day from a fractured rock aquifer but salinity ranged from 3 500 mg/l to 4 800 mg/l. Discharge testing of the best well showed a strip-aquifer type...-
Document
Published: 01 Aug 1980
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Hallett (part of the Nackara Gold Project). Annual reports and final report to licence expiry/full surrender, for the period 9/8/2002 to 4/10/2012.
An area of high country in the far northern Mount Lofty Ranges was taken under licence to try to find the primary source(s) of widely dispersed detrital gold known from Recent and Tertiary cover sediments in the region, while focussing mainly on...-
Document
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RB 2012/00004 MARREE, South Australia, [geological map] sheet SH54-5. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The MARREE mapsheet area includes the south-western portion of the Strzelecki Desert plus parts of the Tirari Desert, north-western Flinders Ranges and north-eastern Willouran Ranges, between latitudes 29 to 30 degrees S and longitudes 138 to 139...-
Document
Published: 01 Apr 2012
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ExpNotes MARREE: Explanatory Notes MARREE
A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...-
Document
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Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (3D pdf version 1)
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
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Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (GOCAD version 1).
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
