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RB 47/00028 Probable stratigraphy of water bores at Murrayville, Victoria.
Published: 01 Jan 1958 Created: 04 Nov 2024 Revised: 04 Nov 2024
Author: Ludbrook, N.H.

Water Bores in the Murrayville area mostly intersect only the late Tertiary sequence of the Loxton Sands and Bookpurnong beds. Mid Tertiary limestones are encountered only below depths of about 300 feet. A similar sequence, reported to carry large...

Water Bores in the Murrayville area mostly intersect only the late Tertiary sequence of the Loxton Sands and Bookpurnong beds. Mid Tertiary limestones are encountered only below depths of about 300 feet. A similar sequence, reported to carry large supplies of underground water, occurs in the Hundred of Peebinga.

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About this record

Record No rb4700028
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Departmental Publication - Hydrogeological Publication
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province Murray Basin
Mine Name
Stratigraphy
Commodity
    Notes 
    Geographic Locality: Victoria;Pinnaroo;Hd Peebinga, secn 27
Doc No: RB 47/00028
    Geographic Locality: Victoria;Pinnaroo;Hd Peebinga, secn 27
Doc No: RB 47/00028
    Language English
    Metadata Standard ISO 19115-3

    Citations

    Use constraints License
    License Creative Commons Attribution 4.0
    Persistent identifier https://pid.sarig.sa.gov.au/document/rb4700028
    Citation Ludbrook, N.H. 1958. RB 47/00028 Probable stratigraphy of water bores at Murrayville, Victoria. Departmental Publication - Hydrogeological Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/rb4700028

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[140.5,-35.5],[141,-35.5],[141,-35],[140.5,-35],[140.5,-35.5]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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