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RB 83/00019 1:250 000 Geological Series - Explanatory Notes. DALHOUSIE, South Australia.
The geomorphology of DALHOUSIE broadly consists of stony uplands which include mound springs in the west, and dunefield lowlands in the east on the edge of the Simpson Desert. Strongly folded ?Adelaidean sediments are overlain by a more gently folded...-
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Published: 01 Nov 1984
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RB 86/00058 (Revised edition, 2016) Excursion guide. Silcrete field workshop, South Australia, August 19-30, 1985.
Guide covers an area extending from the western margin of Lake Torrens to Coober Pedy, and down to Ceduna. Characteristics of the silcretes in the Tertiary sequences, field relationships, and other criteria which might be used to interpret processes...-
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Published: 01 Jun 1916
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RB 76/00119 Silcrete sediments and stratigraphy.
There is no abstract created for this record-
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Published: 01 Jan 1976
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RB 79/00104 Regressive Tertiary Miocene lake system and silicified strandlines, Billa Kalina area, South Australia.
A system of parallel arcuate ridges dominates the topography of the Billa Kalina area; facies relationships indicate that they are silicified strandlines of a Miocene lake which have been etched out by later erosion. Clays and dolomites of the Miocene...-
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Published: 05 Sep 1979
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RB 2014/00005 WINTINNA, South Australia, [geological map] sheet SG53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The WINTINNA 1:250 000 mapsheet area lies between latitudes 27° to 28° South and longitudes 133°30’ to 135°00’ East. This ~16 400 square km area includes the Marla and Cadney Park settlements, and is crossed by the Stuart Highway and Adelaide to...-
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Published: 01 Mar 2015
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ExpNotes WINTINNA: Explanatory Notes WINTINNA, SG 53-14.
A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...-
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