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RB 46/00057 Buccleuch Beds - Standard subsurface section. Coonalpyn township bore, Hundred of Coneybeer, secn 56.
Published: 01 Jan 1958 Created: 04 Nov 2024 Revised: 04 Nov 2024
Author: Ludbrook, N.H.

Coonalpyn Town Water Suply bore No. 2 is selected as the standard subsurface section for beds of the Buccleuch Formation (formerly Buccleuch Group) of Late Eocene age. The bore penetrated Bridgewater, Coomandook and Buccleuch Formations and was...

Coonalpyn Town Water Suply bore No. 2 is selected as the standard subsurface section for beds of the Buccleuch Formation (formerly Buccleuch Group) of Late Eocene age. The bore penetrated Bridgewater, Coomandook and Buccleuch Formations and was completed in sands of the Renmark Group (formerly Knight Group).

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About this record

Record No rb4600057
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 Buccleuch Formation
Commodity
    Notes 
    Geographic Locality: Coonalpyn;Hd Coneybeer, secn 56
Doc No: RB 46/00057
    Geographic Locality: Coonalpyn;Hd Coneybeer, secn 56
Doc No: RB 46/00057
    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/rb4600057
    Citation Ludbrook, N.H. 1958. RB 46/00057 Buccleuch Beds - Standard subsurface section. Coonalpyn township bore, Hundred of Coneybeer, secn 56. Departmental Publication - Hydrogeological Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/rb4600057

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[139.5,-36],[140,-36],[140,-35.5],[139.5,-35.5],[139.5,-36]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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