This dataset consists of a series of approximate WSW to ENE oriented 'geological structures' interpreted from residual gravity bedrock depth in the Goulburn-Murray area of Victoria. These structures segment the Goulburn River Valley into an upper, middle and lower Goulburn bedrock valley system suggesting that it is a broadening out upland groundwater system for most of its length.
The dataset was compiled by GHD to inform the report 'Potential Influences of Geological Structures on Groundwater Flow Systems' for DEPI's Secure Allocation Future Entitlements (SAFE) Project.
Search Words:
Inland waters
,
Geoscientific information
Publication Date:
20 November 2022
Dataset Status:
Victoria
Progress:
Completed
Access Constraint:
Creative Commons Attribution 4.0 (CC-BY)
(
License Text
)
General
Data Existence:
Metadata Name
Descriptions
Resource Name:
GEOL_STRUCT_GOULBURN_MURRAY
Title:
Geological Structures, Goulburn-Murray Area
Anzlic ID:
ANZVI0803005023
Custodian:
Owner:
Jurisdiction:
Victoria
Abstract:
This dataset consists of a series of approximate WSW to ENE oriented 'geological structures' interpreted from residual gravity bedrock depth in the Goulburn-Murray area of Victoria. These structures segment the Goulburn River Valley into an upper, middle and lower Goulburn bedrock valley system suggesting that it is a broadening out upland groundwater system for most of its length.
The dataset was compiled by GHD to inform the report 'Potential Influences of Geological Structures on Groundwater Flow Systems' for DEPI's Secure Allocation Future Entitlements (SAFE) Project.
Search Words:
Inland waters
,
Geoscientific information
Purpose:
Geographic Extent Polygon:
Geographic Bounding Box:
-34
141
150
-39
Beginning to Ending Date:
2011-06-30 - 2012-06-30
Maintainence and Update Frequency:
As needed
Stored Data Format:
Available Format(s) Types:
DIGITAL
Positional Accuracy:
Not known
Attribute Accuracy:
Not known
Logical Consistency:
Not known
Data Source:
Dataset Source: The geological structures have been interpreted predominantly from residual gravity bedrock depth using Surfer10 for the Goulburn-Murray area.
Dataset Originality: Derived
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