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RB 61/00113 Kingston-on-Murray bridge site bore no. 5, stratigraphy and micropalaeontology - Department of Highways and Local Government.
Published: 01 Jan 1965 Created: 05 Nov 2024 Revised: 05 Nov 2024
Author: Lindsay, J.M.

A foundation test bore in the River Murray near Kingston-on-Murray penetrated river sands underlain by silts, rubbly limestones and sandy intercalations equivalent to the Pata Limestone, and bottomed in silts equivalent to upper Morgan Limestone.

A foundation test bore in the River Murray near Kingston-on-Murray penetrated river sands underlain by silts, rubbly limestones and sandy intercalations equivalent to the Pata Limestone, and bottomed in silts equivalent to upper Morgan Limestone.

About this record

Record No rb6100113
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Departmental Publication - Engineering Geology Publication
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province Murray Basin
Mine Name
Stratigraphy Mannum Formation
Commodity
    Notes 
    Notes: 65/00949
Geographic Locality: Kingston-on-Murray;Murray River
Doc No: RB 61/00113
    Notes: 65/00949
Geographic Locality: Kingston-on-Murray;Murray River
Doc No: RB 61/00113
    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/rb6100113
    Citation Lindsay, J.M. 1965. RB 61/00113 Kingston-on-Murray bridge site bore no. 5, stratigraphy and micropalaeontology - Department of Highways and Local Government. Departmental Publication - Engineering Geology Publication. Government of South Australia.
    https://pid.sarig.sa.gov.au/document/rb6100113

    Technical information

    Status
    Maintenance and Update Frequency
    Geographic Reference GDA2020 (EPSG:7844)
    Geo bounding box {"type":"Polygon","coordinates":[[[140,-34.5],[140.5,-34.5],[140.5,-34],[140,-34],[140,-34.5]]]}
    Purpose 
    
                    
                    
    
                    
                      		
                
    
              
                
                
    
                  
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