2003•Unpublished venueRequires access

DETAILED REGOLITH-LANDFORM MAPPING FOR MINERAL EXPLORATION: THE WAHRATTA 1:25,000 REGOLITH-LANDFORM MAP

Andrea L. Foster, Crc Leme

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Abstract

INTRODUCTION The Wahratta 1:25,000 scale regolith-landform map sheet area, 25 km to the east of Broken Hill, in western New South Wales, contains some of the eastern-most exposures of Broken Hill-type rocks and is dominated by regolith cover. Less than 5% of the area has exposed bedrock. The Wahratta 1:25,000 regolith-landform map characterises the distribution of regolith materials and their associated landforms, previously mapped as uniform “Cainozoic cover” in an area where prospective rocks are likely to exist at depth.

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INTRODUCTION The Wahratta 1:25,000 scale regolith-landform map sheet area, 25 km to the east of Broken Hill, in western New South Wales, contains some of the eastern-most exposures of Broken Hill-type rocks and is dominated by regolith cover. Less than 5% of the area has exposed bedrock. The Wahratta 1:25,000 regolith-landform map characterises the distribution of regolith materials and their associated landforms, previously mapped as uniform “Cainozoic cover” in an area where prospective rocks are likely to exist at depth.

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Available abstract

INTRODUCTION The Wahratta 1:25,000 scale regolith-landform map sheet area, 25 km to the east of Broken Hill, in western New South Wales, contains some of the eastern-most exposures of Broken Hill-type rocks and is dominated by regolith cover. Less than 5% of the area has exposed bedrock. The Wahratta 1:25,000 regolith-landform map characterises the distribution of regolith materials and their associated landforms, previously mapped as uniform “Cainozoic cover” in an area where prospective rocks are likely to exist at depth.

Key concepts: Regolith, Landform, Geology, Bedrock, Geomorphology, Mineral exploration, Earth science, Geochemistry

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