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RB 00677 Grange 1 well. Subsurface stratigraphy.
Grange No. 1 Well was drilled to a depth of 1983 feet, and penetrated a sedimentary sequence of Quaternary and Tertiary rocks to 1872 feet before bottoming in red shale and grey slates of Proterozoic Age. Pleistocene to Recent sandy clays with some...-
Document
Published: 01 Jan 1962
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RB 62/00004 Adelaide Plains Sub-basin stratigraphy: summary report no. 2, Hd Yatala.
Six water bores from the Hundred of Yatala have been examined to outline their stratigraphic sequences. The average depth of the bores is 450 feet (TDs range from 270 feet to 605 feet). One bottomed in Pleistocene beds, two in Pliocene Dry Creek...-
Document
Published: 06 Jan 1966
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RB 73/00246 Proposed Little Para Dam. Effect on intake to aquifers of Northern Adelaide Plains.
Hydrographs of bores adjacent to the Little Para River show that it is an important source of recharge to aquifers of the Salisbury area. Recharge takes place via shallow aquifers and then to deeper aquifers through semi-confining beds and possibly...-
Document
Published: 01 Jan 1975
