COOBER PEDY - data.sarig.sa.gov.au
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" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! " " " " " " " " ! ! ! ! ! ! ! ! ! ! ( " " " " " " " " ! ! ! ! ! ! ! ! ! ! ( " " " " " " " " ! ! ! ! ! ! ! ! ! ! ( " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " Ç Ç Ç Ç Ç Ç Ì Ì Ç Ç Ç ALm Qhe 2 _____ Qpe 9 2 _ 8 Qr 1 Qe ALmc Tem sf TQr 1 Qe 8 Qp ca Tem si1 Qpa 7 Qprg 1 Qe ALm Kmb Qe 8 Tp 4 _____ Kmb Tig 1 Qhl 1 Qe ALm Qprg 1 Qe 8 _____ ?Qe 3 Qe Tem si1 Qe Qe Qpa 8 Kmb Qhe 7 Qp ca Qe 3 Qhl 1 _____ Knc Qhe 2 Qpa 8 ALm Qhe 2 Kmb Qe 8 ALmc Qe ____ Qp ca Qp ca Qe Tem si1 Qe 3 Qe 8 Qpa 7 Tem si1 Tp 4 _____ Kmb TQr 1 Qe 8 Qe ALm Qe 3 Qe 8 _____ Tig 2 Qe 8 ALm TQr 1 ALmc Tem si1 Qprb Qpa 9 Qhe 2 _____ Qpe 9 Qe Qe Qpa 7 Tem sf Qprg 1 Kmb Qprg 1 Qpa 3 Qhl 1 Tem sf _____ Knc Kmb Tem si1 _____ Kmb Qhe 7 Tem si1 ALmc ALm Qp ca Qe Qhe 2 _____ Qpe 9 _____ Qe 3 Qe 3 TQr 1 Tig 2 Qhe 2 _____ Qpe 9 ALmc Qp ca Qe 8 Qhe 2 Tem si1 Tem si1 TQr 1 Qp ca Qhe 2 TQr 1 Tem sf Qpa 8 TQr 1 Qprb Tem si1 Qprg Tig 2 Qe Tem si1 ALm Qhl 1 Qprg LM 2 Tem si1 Qhe 2 Qpa 8 Qhe 2 Tem si1 ?ALmg Qe 8 Qpei Qprb Tem si1 _____ Kmb Qhe 2 Qhe 2 Tem si1 Qpa 7 Qe Qhe 2 Qprg 1 Q Qpa 9 Qprg 1 Qprb Kmb Qpa 7 Qe 8 Qe ALm Qe 8 JK-a Qhl 1 Tem si1 Qp ca Qprb Tem si1 _____ Kmb Tem si1 Qe 3 Qe Qha 1 Qprg Tem si1 Qhl 1 Qhl 1 _____ Tem sf _____ Knc P-s JK-a Qpa 8 Qp ca Qe 8 JK-a Qe TQr 1 Qprg Tp 4 _____ Kmb Qe 8 _____ Tig 2 Kmb Qprg Tp 4 _____ Kmb Qpa 8 ALm Qe 8 _____ Tig 2 Qhl 1 ALm Qpa 7 Tem si1 Qe 8 _____ Tig 2 Qhe 7 Qe 8 _____ Tig 2 Qe JK-a Tig 2 Tem sf Qhe 2 Qp ca TQr 1 Kmb Kmb ALm Qp ca Qe Qpa 7 Qe Qhe 2 _____ Qpe 9 Qprg 1 Qp ca _____ Kmb ALm Tig 2 Kmb Qprg TQr 1 Qhe 2 _____ Qpe 9 ALmc Qpa 8 Tem si1 Qe __ Tem si1 _____ Kmb Qhe 2 Qe 3 Qp ca TQr 1 Tem sf ?ALm Tig 2 Qhe 2 Qhe 2 _____ Qpe 1 _____ Qe 3 Tem sf Qpa 8 Qe Kmb ALm Qe 1 Qp ca Qe Qhe 4 Qpr 1 ALmc 2 Tem si1 Lz 4 Qp ca Qe 8 Qpr 1 ALm a Mae Qe 8 Qe 8 Tem si1 Qhl 1 Tem si1 Tem sf ALmg ALm Qp ca Tem si1 Qprb Qe 3 Qe 3 Qhl 1 Qe 8 ALmc 2 Tem si1 Qpa 8 Qe Qprb Qhe 7 Qp ca Qe ALm ALm Qhl 1 Qhl 1 Tem si1 Qhl 1 Qe Qe TQr 1 Qe 8 TQr 1 Qprg 1 Qprb Qhe 2 Qprg 1 Qhl 1 Qhe 2 Qp ca Qe Qhe 2 TQr 1 Qhe 2 _____ Qpe 9 Tem si1 ALmc 2 JK-a Qpa 9 Qhl 1 Qe 3 Qe ____ Qp ca Qha 1 Qe 8 _____ Tig 2 Qhe 2 Qprg Qhe 2 _____ Qpe 1 _____ Qe 3 Qe 3 Tem si1 ALmc Qhl 1 Qhe 7 Qp ca Tig 2 Qhe 2 _____ Qpe 9 Tig 2 Qe 3 Qe 8 TQr 1 Qha 1 Qprg Qhl 1 _____ Tem sf _____ Knc Kmb Qhe 2 _____ Qpe 9 TQr 1 Qhe 2 _____ Qpe 9 Tig 2 Tem si1 JK-a Qhe 7 Kmb Qpa 9 Qe 8 Qprg 1 Qprb ______ Kmb Tem si1 JK-a Qha 1 Qpa 7 Tem si1 ALm Qp ca Kmb Qhl 1 _____ Knc Qe Qhe 2 Qe Qe Qp ca Qp ca Qe ALm Qhe 2 _____ Qpe 9 Kmb Qha 1 Qe 3 Qe ____ Qp ca Tem si1 Qhl 1 _____ Tig 1 Qe 8 Tem si1 Qpa 8 Qprg 1 ALm ALm Qp ca Qp ca Tem si1 Qe 8 _____ Tig 2 Qp ca ALm Qhl 1 Qe Tig 1 Qe Kmb Tp 4 _____ Kmb Qe ____ Qp ca Qp ca ALm Tem si1 TQr 1 Qprb Qprb Qprg 1 Qp ca Kmb Tem si1 _____ Kmb Qe ____ Qp ca Tem si1 Qpa 3 Qhe 2 _____ Qpe 9 Qpr 6 _____ Qprb Qe Tem si1 Qe ____ Qp ca Qpa 7 Kmb ALmc Qp ca Qprg 1 Qpa 8 Kmb Qprg 1 Qprg Kmb Qe 8 ALm Qe 8 Qprg 1 Qe Tem si1 Tem sf Qprb Knc Qhe 2 Qp ca Tem si1 Qe 3 Qhe 2 Qhe 2 _____ Qpe 9 Qe Tem si1 Qhl 1 Qp ca Qpa 8 Qe 8 Tig 2 ALmc ALm Qp ca Qprg 1 Qprg Qe 3 Tem si1 Knc Tem sf _____ Knc Qhe 2 Qe Qha 1 TQr 1 Tem si1 TQr 1 Qhe 2 JK-a Tem si1 ALm Qe Qp ca Qprg Qe 8 _____ ?Qe 3 Qprb Tem sf _____ Knc Qe ____ Qp ca Kmb Kmb Qe 8 Qp gy Tem si1 ALm Qe Qe Qe Qhe 2 _____ Qpe 9 P-s Qprg Qhl 1 _____ Tem sf _____ Knc Qprg Qpa 3 Qhl 1 _____ Knc Qhe 2 _____ Qpe 9 Tem si1 P-s Qe 8 Kmb ALm Qhe 4 Qe Tem sf Knc Kmb Qhl 1 _____ Knc Qp ca Qprg Qhl 1 Tem si1 Kmb Qpa 7 Qprb Qhl 1 Qe Qhl 1 Qp ca Tem sf _____ Knc Kmb Kmb Qprg 1 SEQUOIA, Fe GOLF BORE, Au PENRHYN, COAL GREENEWOOD, Au CHALLENGER, Au, Ag CHALLENGER NO.3, Au LAKE PHILLIPSON, COAL PERFECTION WELL, RHYO COOBER PEDY, OPAL, ALU FITZGERALD DAM, GRNT, FEST Bore 17 Bore 24 Old Well Ian Bore Golf Bore Nins Bore Bore No 4 Bore No 5 Skye Bore Bore No 1 Blue Bore No 8 Bore Willy Bore No 53 Bore Gulda Bore No 44 Bore Bundi Bore Comet Bore No 42 Bore Ibis Bores Ibis Bores Billy Bore Dalray Bore Jacobs Bore Wirrida Bore Boulder Bore Century Bore Sequoia Bore Bedouri Bore Garford Bore Birthday Well Pibroch Bores Old Skye Bore Princess Bore Columba Bores Campfire Bore Ping Pong Bore Bell Bird Bore Satellite Bore Sandstone Bore Four Mile Bore Eaglehawk Bore Nestling Bores Coolingee Bore Coronation Bore Perfection Well Bon Leigh Bores Ants Nest Bores Turkey Flat Bore Burntiltaby Bore Top Of Hill Bore Cross Roads Bore Park Bores & Tank New Surprise Bore Ross Salt Springs Four Corners Bore Nelson Bore & Tank White Elephant Bore Old Homestead Bores Fescuva Bores & Tank Cleanskin Swamp Bore Twenty Mile Waterhole Eight Mile Swamp Bore West Roberts Bore & Tank Top Waterhole Lagoon Waterhole Top Box Waterhole Junction Waterhole Junction Waterhole Eight Mile Watrhole Packsaddle Waterhole Bottom Box Waterhole Horse Camp Waterhole Finger Post Waterhole Twelve Mile Waterhole Twenty Mile Waterhole Sixteen Mile Waterhole Fourteen Mile Waterhole Centipede Creek Waterhole MT BRADY STONY HILL ROBIN RISE ALLAN RISE MORTON RISE LEONARD RISE J K JUNCTION WILDINGI GATE COMMONWEALTH HILL NORTH EAST CORNER GATE Comet Ingomar Jumbuck Garford Mc Douall Peak Gina Outstation Commonwealth Hill Gina Wirrida Wirrida Hypo Hill Stuart Range Jewellers Shop Kingsmill Camp Great Victoria Desert Mc Douall Peak Woolshed Coober Pedy Aerodrome Lake Phillipson Lake Wirrida Lake Woorong Wurley Lagoon Burntiltaby Claypan Four Mile Swamp Birthday Swamp Arkeeta Claypans Mickey Swamp Ti-tree Swamps Wildingi Claypan Coolingee Swamp DIGITAL EDITION SUBJECT TO AMENDMENT See published printed map for further information COOBER PEDY SH5306 -3021.358 9965.315 -1480.152 -148.16 1183.832 COOBER PEDY Solid Geology - Linear Structure COMMODITIES MINING Ç Ì Ì Ç GEOLOGICAL BOUNDARY CULTURAL FEATURES ! " ) HYDROGRAPHIC AND GEOMORPHIC FEATURES ! ! " LINEAR STRUCTURES STRUCTURAL FEATURES ! ! ! ! ! ! ! ! ! ! ! ! ! D C ! Solid Geology Í Í Í Í Í Í PLIOCENE HOLOCENE Qha 1 Qhe Qhe 2 Qhe 4 Qhe 7 Qhl 1 TERTIARY-PLEISTOCENE TQr 1 CRETACEOUS-PALEOCENE KTa\dw PLEISTOCENE-HOLOCENE Qe Qe 3 Qe 8 Qr 1 JURASSIC-CRETACEOUS JK-a PERMIAN P-s MESOPROTEROZOIC Mae PALAEO-MESOPROTEROZOIC LM 2 PALAEOPROTEROZOIC L 60 ARCHAEAN-PALAEOPROTEROZOIC ALm ALmc ALmc 2 Í Í Í Í Í Í Í Í Í Í Í ALmg Tp 4 Tp\si 1 OLIGOCENE-PLIOCENE Topm EOCENE-MIOCENE Tem 2 Tem\sf Tem\si 1 CRETACEOUS Kmb 1 Kmb K-c EOCENE-PLEISTOCENE Tig 2 Tbp Tig 1 PLEISTOCENE Qpa 3 Qpa 7 Qpa 8 Qpa 9 Qpe 1 Qpe 8 Qpe 9 Qpei Qp\ca Qp\gy Qprg 1 Qprg Qpr 5 Qpr 6 Qprb
Transcript of COOBER PEDY - data.sarig.sa.gov.au
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Qe
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Qprg1
Qe8_____?Qe3
Qe
Temsi1
Qe
Qe
Qpa8
Kmb
Qhe7
Qpca
Qe3Qhl1_____Knc
Qhe2
Qpa8
ALm
Qhe2
Kmb
Qe8
ALmc
Qe____Qpca
Qpca
Qe
Temsi1
Qe3
Qe8
Qpa7
Temsi1
Tp4_____Kmb
TQr1
Qe8
Qe
ALm
Qe3
Qe8_____Tig2
Qe8
ALm
TQr1
ALmc
Temsi1
Qprb
Qpa9
Qhe2_____Qpe9 Qe
Qe
Qpa7
Temsf
Qprg1
Kmb
Qprg1
Qpa3
Qhl1
Temsf_____Knc
Kmb
Temsi1_____Kmb
Qhe7
Temsi1ALmc
ALm
Qpca
Qe
Qhe2_____Qpe9_____Qe3
Qe3
TQr1
Tig2
Qhe2_____Qpe9
ALmc
Qpca
Qe8
Qhe2
Temsi1
Temsi1
TQr1
Qpca
Qhe2
TQr1
Temsf
Qpa8
TQr1
Qprb
Temsi1
Qprg
Tig2
Qe
Temsi1
ALm
Qhl1
Qprg
LM2
Temsi1
Qhe2
Qpa8
Qhe2
Temsi1?ALmg
Qe8
Qpei
Qprb
Temsi1_____Kmb
Qhe2
Qhe2
Temsi1
Qpa7
Qe
Qhe2
Qprg1
Qhl1
Qpa9
Qprg1
Qprb
Kmb
Qpa7
Qe8
Qe
ALmQe8
JK-a
Qhl1
Temsi1
Qpca
Qprb
Temsi1_____Kmb
Temsi1
Qe3
Qe
Qha1Qprg
Temsi1
Qhl1Qhl1_____Temsf_____Knc
P-sJK-a
Qpa8
Qpca
Qe8
JK-a
Qe
TQr1
Qprg
Tp4_____Kmb
Qe8_____Tig2
Kmb
QprgTp4_____Kmb
Qpa8
ALm
Qe8_____Tig2
Qhl1
ALm
Qpa7
Temsi1
Qe8_____Tig2
Qhe7
Qe8_____Tig2
Qe
JK-a
Tig2 Temsf
Qhe2
Qpca
TQr1
Kmb
Kmb
ALm Qpca
Qe
Qpa7
Qe
Qhe2_____Qpe9
Qprg1
Qpca_____Kmb
ALm
Tig2
Kmb
Qprg
TQr1
Qhe2_____Qpe9
ALmc
Qpa8 Temsi1
Qe
TpQrr_______Kmb
Temsi1_____Kmb
Qhe2
Qe3
Qpca
TQr1
Temsf
?ALm
Tig2
Qhe2
Qhe2_____Qpe1_____Qe3
Temsf
Qpa8
Qe
Kmb
ALm
Qe1
Qpca
Qe
Qhe4
Qpr1_____JK-a
ALmc2Temsi1
Lz4
Qpca
Qe8
Qpr1_____ALm
ALmQpca
Mae
Qe8
Qe8
Temsi1
Qhl1
Temsi1
Temsf
ALmg
ALm
Qpca
Temsi1
Qprb
Qe3
Qe3
Qhl1
Qe8
ALmc2
Temsi1
Qpa8
Qe
Qprb
Qhe7
Qpca
Qe
ALm
ALm
Qhl1
Qhl1
Temsi1
Qhl1
Qe
Qe
TQr1
Qe8
TQr1
Qprg1 Qprb
Qhe2
Qprg1
Qhl1
Qhe2
Qpca
Qe
Qhe2
TQr1
Qhe2_____Qpe9
Temsi1
ALmc2
JK-a
Qpa9
Qhl1 Qe3
Qe____Qpca
Qha1
Qe8_____Tig2
Qhe2
Qprg
Qhe2_____Qpe1_____Qe3Qe3
Temsi1ALmc
Qhl1Qhe7
Qpca
Tig2
Qhe2_____Qpe9
Tig2
Qe3
Qe8
TQr1
Qha1
Qprg
Qhl1_____Temsf_____Knc
Kmb
Qhe2_____Qpe9
TQr1
Qhe2_____Qpe9
Tig2
Temsi1
JK-a
Qhe7
KmbQpa9
Qe8
Qprg1
Qprb______Kmb
Temsi1
JK-a
Qha1
Qpa7
Temsi1
ALmQpca
Kmb
Qhl1_____Knc
Qe
Qhe2
Qe
Qe
Qpca
Qpca
Qe
ALm
Qhe2_____Qpe9
Kmb
Qha1
Qe3
Qe____Qpca
Temsi1
Qhl1_____Tig1
Qe8
Temsi1
Qpa8
Qprg1
ALm
ALm
Qpca
Qpca
Temsi1
Qe8_____Tig2
Qpca
ALm
Qhl1
Qe
Tig1
Qe
Kmb
Tp4_____Kmb
Qe____QpcaQpca
ALmTemsi1
TQr1
Qprb
Qprb
Qprg1
Qpca
Kmb
Temsi1_____Kmb
Qe____Qpca
Temsi1
Qpa3
Qhe2_____Qpe9Qpr6_____Qprb
Qe
Temsi1
Qe____Qpca
Qpa7
Kmb
ALmc
Qpca
Qprg1
Qpa8
KmbQprg1
Qprg
Kmb
Qe8
ALmQe8
Qprg1
Qe
Temsi1
Temsf
Qprb
Knc
Qhe2
Qpca
Temsi1
Qe3
Qhe2
Qhe2_____Qpe9
Qe
Temsi1
Qhl1
Qpca
Qpa8
Qe8
Tig2
ALmc
ALm
Qpca
Qprg1
Qprg
Qe3
Temsi1
KncTemsf_____Knc
Qhe2
Qe
Qha1
TQr1
Temsi1
TQr1
Qhe2
JK-a
Temsi1
ALmQe
Qpca
Qprg
Qe8_____?Qe3
Qprb
Temsf_____Knc
Qe____Qpca
Kmb
Kmb
Qe8
Qpgy
Temsi1
ALm
Qe
Qe
Qe
Qhe2_____Qpe9
P-s
Qprg
Qhl1_____Temsf_____Knc
Qprg
Qpa3
Qhl1_____Knc
Qhe2_____Qpe9
Temsi1
P-s
Qe8
Kmb
ALm
Qhe4
Qe
Temsf
Knc
Kmb
Qhl1_____Knc
Qpca
Qprg
Qhl1
Temsi1
Kmb
Qpa7
Qprb
Qhl1
Qe
Qhl1
Qpca
Temsf_____Knc
Kmb
KmbQprg1
SEQUOIA, Fe
GOLF BORE, Au
PENRHYN, COAL
GREENEWOOD, Au
CHALLENGER, Au, Ag
CHALLENGER NO.3, Au
LAKE PHILLIPSON, COAL
PERFECTION WELL, RHYO
COOBER PEDY, OPAL, ALU
FITZGERALD DAM, GRNT, FEST
Bore 17
Bore 24
Old Well
Ian Bore
Golf Bore
Nins Bore
Bore No 4
Bore No 5
Skye Bore
Bore No 1
Blue Bore
No 8 Bore
Willy Bore
No 53 Bore
Gulda Bore
No 44 Bore
Bundi Bore
Comet Bore
No 42 Bore
Ibis BoresIbis Bores
Billy Bore
Dalray Bore
Jacobs Bore
Wirrida Bore
Boulder Bore
Century BoreSequoia Bore
Bedouri Bore
Garford Bore
Birthday Well
Pibroch Bores
Old Skye Bore
Princess Bore
Columba BoresCampfire Bore
Ping Pong BoreBell Bird Bore
Satellite Bore
Sandstone Bore
Four Mile Bore
Eaglehawk Bore
Nestling Bores
Coolingee Bore
Coronation Bore
Perfection WellBon Leigh Bores
Ants Nest Bores
Turkey Flat Bore
Burntiltaby Bore
Top Of Hill Bore
Cross Roads Bore
Park Bores & Tank
New Surprise Bore
Ross Salt SpringsFour Corners Bore
Nelson Bore & Tank
White Elephant Bore
Old Homestead Bores
Fescuva Bores & Tank
Cleanskin Swamp Bore
Twenty Mile Waterhole
Eight Mile Swamp Bore
West Roberts Bore & Tank
Top Waterhole
Lagoon Waterhole
Top Box Waterhole
Junction Waterhole
Junction Waterhole
Eight Mile Watrhole
Packsaddle Waterhole
Bottom Box Waterhole
Horse Camp Waterhole
Finger Post Waterhole
Twelve Mile Waterhole
Twenty Mile Waterhole
Sixteen Mile Waterhole
Fourteen Mile Waterhole
Centipede Creek Waterhole
MT BRADY
STONY HILL
ROBIN RISE
ALLAN RISE
MORTON RISE
LEONARD RISE
J K JUNCTION
WILDINGI GATE
COMMONWEALTH HILL
NORTH EAST CORNER GATE
Comet
Ingomar
Jumbuck
Garford
Mc Douall Peak
Gina Outstation
Commonwealth Hill
Gina
Wirrida
Wirrida
Hypo Hill
Stuart Range
Jewellers Shop
Kingsmill Camp
Great Victoria Desert
Mc Douall Peak Woolshed
Coober Pedy Aerodrome
Lake Phillipson
Lake Wirrida
Lake WoorongWurley Lagoon
Burntiltaby Claypan
Four Mile Swamp
Birthday Swamp
Arkeeta Claypans
Mickey Swamp
Ti-tree Swamps
Wildingi Claypan
Coolingee Swamp
360000
360000
370000
370000
380000
380000
390000
390000
400000
400000
410000
410000
420000
420000
430000
430000
440000
440000
450000
450000
460000
460000
470000
470000
480000
480000
490000
490000
500000
5000006680000
6680000
6690000
6690000
6700000
6700000
6710000
6710000
6720000
6720000
6730000
6730000
6740000
6740000
6750000
6750000
6760000
6760000
6770000
6770000
6780000
6780000
6790000
6790000
The Total Magnetic Intensity Image has been compiled usingaeromagnetic data from the
Department for Energy and Mining, S outh Australia.Aeromagnetic data have been merged, gridded and imageprocessed by the Geological S urvey of S outh Australia.
S CALE 1:1000000 S CALE 1:1000000 Modified from Interpreted Crystalline Basement Geology Of The Gawler Craton (Fairclough et al. 2003)Interpreted S olid Geology Of The Curnamona Province (Burtt and Betts, 2003),Musgrave Block, Central Australia: regional geology from interpretation of
aeromagnetic data (R ankin and Newton, 2002), S olid Geology S outh Australia (Cowley, 2006).
5 0 5 10 15 20 25KILOMETR ES KILOMETR ES
S A GEOLOGICAL ATLAS S ER IES S HEET
GEOLOGICAL S U R V EY OF S OUTH AUS TR ALIADEPAR TMENT FOR ENER GY AND MINING
S OLID GEOLOGY INTER PR ETATIONTOTAL MAGNETIC INTENS ITY IMAGE
AUS TR ALIA 1:250 000
+6.25°E
+6.00°E
+5.75°E
+5.50°E
+5.25°E
+6.50°E
GILES
BAR TON
W AR R INA
TAR COOLA KINGOONY A
TAL LAR INGA BIL LA KALINACOOBER PEDY
MUR LOOCOPPIE
Y erada5639
Ingomar5838
J umbuck5638
W oorong5738
Phillipson5739
Coober Pedy5839
W A
NTQ LD
S ANS W
V IC
TAS
INDEX TO 1:100 000 S HEETS
INDEX TO ADJOINING 1: 250 000 S HEETSMagnetic Declination 2000
(Annual variation +1.4 minutes)
S CALE 1:250,000
DIGITAL EDITIONSUBJECT TO AMENDMENT
See published printed map for further information
A two standard deviation contrast stretch has been applied to the raster image above.
30° 00'
29° 30'
29° 00'
133° 30' 134° 00' 134° 30' 135° 00'
29° 00'
133° 30' 134° 00' 134° 30' 135° 00'
30° 00'
29° 30'
29° 00'
133° 30' 134° 00' 134° 30' 135° 00'
30° 00'29° 30'
29° 00'
133° 30' 134° 00' 134° 30' 135° 00'
30° 00'
29° 30'
29° 00'
133° 30' 134° 00' 134° 30' 135° 00'
30° 00'29° 30'
29° 00'
133° 30' 134° 00' 134° 30' 135° 00'
COOBER PEDYSH5306
nTesla
-3021.358 9965.315
-1480.152 -148.16 1183.832
S H5306
COOBER PEDY
Solid Geology - Linear Structure
....................................................................Fault position accurate............................................................Fault position approx imate
.....................................................................................Mylonite zone
30° 00'29° 30'
COMMODITIESAg S ilverAL U AluniteAu GoldCOAL CoalFe IronFES T Ironstone -
constructionmaterials
GR NT GraniteOPAL OpalR HY O R hyoliteMINING
...................................................... ÇDEPOS IT - NO MINING........ ÌMINE - METAL S AND INDUS TR IAL MINER AL S
........................................................................................ ÌQ UAR R Y - CONS TR UCTION MATER IAL S (HAR DR OCK)
..........................
ÇDIGGINGS - AL L U V IAL GOLD/GEMS
GEOLOGICAL BOUNDARY
........................................................................FLOOD PLAIN......................GEOLOGICAL BOUNDAR Y INFER R ED
...GEOLOGICAL BOUNDAR Y POS ITION ACCUR ATE
......................................................................GEOLOGICAL BOUNDAR Y POS ITIONAPPR OX IMATE
CULTURAL FEATURES
................................................................PR INCIPAL R OAD...........................................................S ECONDAR Y R OAD
......................................................................MINOR R OADS.........................................................V EHICULAR TR ACKS
..................................................OPER ATIONAL R AILW AY.......................................................................................FENCE
.............................................................. !IDENTIFIED POINT................................................................................. "BUILDING
...................................................................................... )Y AR DS.............................................................LANDING GR OUND
HYDROGRAPHIC AND GEOMORPHIC FEATURES
........................................................INTER MITTENT LAKE..................................................MAJOR W ATER COUR S E...................................................MINOR W ATER COUR S E
.........................................................................FLOODPLAIN....................................................................................S W AMP
.......................................................................... !W ATER HOLE......................................................................................... !BOR E
......................................................................... "W ATER TANK..........................................................................S AND R IDGE
LINEAR STRUCTURES
.......................................................................AL L U V IAL FAN
.......................................................................ES CAR PMENT........................................FAULT POS ITION ACCUR ATE
................................FAULT POS ITION APPR OX IMATE....................................................................................... ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !
GILGAI
STRUCTURAL FEATURES
............................TECTONIC FOLIATION - V ER TICAL!
!
!
!
!
!
!
!
!
!
!
!
!
!
D
C
S CALE 1:2000000
A: Detailed ground traversesB: Image interpretation with limited ground traversesC: Image interpretation with potentially some minor ground traversesD: Image interpretation only
GEOLOGICAL R ELIABILITY DIAGR AM
Coober Pedy sheet published 1981!Geological Field Observations
Solid Geology
Mount W oods ComplexL s
Mulgathing ComplexALm
Peake MetamorphicsL eGairdner DoleriteN-g
Ma8 Gawler R ange V olcanicsUnit 8
L36 Palaeoproterozoicunit 36
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
LM14 Palaeoproterozoic-Mesoproterozoic unit 14
Mh6 Hiltaba S uite Unit 6 L37 Palaeoproterozoicunit 37
L38 Palaeoproterozoicunit 38
L39 Palaeoproterozoicunit 39
R E F E R E N C E
PLIOCENE
HOLOCENE
HOLOCENE AL L U V IAL/FL U V IAL UNIT 1: Present day Holocene alluvium;current bedload.Qha1HOLOCENE AEOLIAN S EDIMENTS : Undifferentiated Holocene aeoliansediments.QheHOLOCENE AEOLIAN UNIT 2: Holocene sand capping dunes indunefields.Qhe2
HOLOCENE AEOLIAN UNIT 4: Holocene gypsiferous dunes/lunettes.Qhe4HOLOCENE AEOLIAN UNIT 7: Holocene variably oriented sand dunes,with appreciable drainage influence. Based on Q hs1, COOBER PEDY .Qhe7
HOLOCENE LACU S TR INE/PLAY A UNIT 1: Holocene playa sediments.Qhl1
TERTIARY-PLEISTOCENE
TER TIAR Y -PLEIS TOCENE R EGOLITH/COL L U V IAL UNIT 1: Ferricrete,massive, nodular, pisolitic, cellular or vermiform, variably dissected andreworked, often with ferruginous lag; ferruginous gravel, sand, silt andclay. Alluvial, colluvial to regolith origin. Early Tertiary to Pleistocene.
TQr1
CRETACEOUS-PALEOCENE
CR ETACEOUS -PALEOCENE DEEP W EATHER ING: Undifferentiateddeep weathering.KTa\dw
PLEISTOCENE-HOLOCENE
Q UATER NAR Y AEOLIAN S EDIMENTS : Undifferentiated Q uaternaryaeolian sediments.QeQ UATER NAR Y AEOLIAN UNIT 3: Q uaternary gypsiferous dunes/lunettes.Qe3Q UATER NAR Y AEOLIAN UNIT 8: Q uaternary sand, orange-brown tored-brown, calcareous and rarely gypseous in part. Based on Q s1,COOBER PEDY .
Qe8Q UATER NAR Y R EGOLITH/COL L U V IAL UNIT 1: Q uaternarygibber-mantled colluvium. Based on Q on MUR L OOCOPPIE.Qr1 JURASSIC-CRETACEOUS
ALGEBUCKINA S ANDS TONE: S andstone, fine to coarse-grained, withgranule and pebble layers, and shale intraclasts. Cross-bedded.JK-a
PERMIAN
S TUAR T R ANGE FOR MATION: S hale, homogenous marine, with minorsiltstone and sandstone. Deposited in a quiet water restricted marineenvironment.
P-sMESOPROTEROZOIC
EALBAR A R HY OLITE: R hyolite, flow banded; rhyodacite. ignimbritic; tuff.MaePALAEO-MESOPROTEROZOIC
PALAEOPR OTER OZOIC-MES OPR OTER OZOIC UNIT 2: UndifferentiatedEngenina Adamellite and Balta Granite. Based on Prot-gamma onCOOBER PEDY .
LM2PALAEOPROTEROZOIC
PALAEOPR OTER OZOIC UNIT 60: Diorite; amphibolite dykes,comagmatic with L58, L59. BAR TON sheet.L60
ARCHAEAN-PALAEOPROTEROZOIC
MULGATHING COMPLEX : Paragneiss, arenaceous and aluminous; ironformation; granitic gneiss; felsic and mafic-ultramafic volcanic and intrusiverocks. Granulite to amphibolite facies. Protoliths ~2560–2460 Ma.
ALmCHR IS TIE GNEIS S : Gneiss with migmatitic layers, paragneiss, carbonate,calcsilicate, quartzite. Age (U-Pb)2437+/-11Ma. W ith banded ironformation.
ALmcCHR IS TIE GNEIS S UNIT 2: Banded iron formation:qtz-mgt-diop-hyp-amph gneiss; qtz- microcline-plag gneiss.Age(U-Pb)2437+/-11Ma. BAR TON sheet.
ALmc2
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
Í Í Í Í Í Í Í
GLENLOTH GR ANITE: Granite, granodiorite, pink-brown to grey, quartz,microcline and plagioclase. W ith remnants of gneiss and biotite andhornblende schlieren. ~2509-2436 Ma.
ALmg
PLIOCENE UNIT 4: Pliocene Colluvial breccia, gravel, jasper breccia,burrows. Based on Czn on COOBER PEDY .Tp4PLIOCENE S ILCR ETE UNIT 1: Pliocene pedogenic and groundwatersilcrete, TAL L AR INGA sheet.Tp\si1
OLIGOCENE-PLIOCENE
MUNJ ENA FOR MATION: Conglomeratic sand, clayey sand and breccia.Poorly sorted.Topm
EOCENE-MIOCENE
EOCENE-MIOCENE UNIT 2: Eocene to Miocene poorly sorted sand,conglomeratic sand; colluvial silt, clay, breccia. S ilicified. Based on Ts,COOBER PEDY .
Tem2EOCENE-MIOCENE S ILCR ETE/FER R ICR ETE: Undifferentiated Eoceneto Miocene silcrete/ferricrete.Tem\sfEOCENE-MIOCENE S ILCR ETE UNIT 1: R egionally older silcrete; approxL ate Eocene-Mid Miocene.Tem\si1
CRETACEOUS
BUL L DOG S HALE UNIT 1: Dark brown claystone, "cone-in-cone"limestone, thin conglomeratic sandstone, characterised by lag boulderfields. Basal unit, based on Klt, MUR L OOCOPPIE.
Kmb1
BUL L DOG S HALE: Mudstone, grey, bioturbated, fossiliferous and shaly;minor silt to very fine-grained sandstone intervals.Kmb
CADNA-OW IE FOR MATION: S andstone, fine-grained, withcoarse-grained sandstone beds, and pale grey siltstone, minorconglomerate.
K-c
EOCENE-PLEISTOCENE
GAR FOR D FOR MATION UNIT 2: W hite, fossiliferous dolomitic limestone,dolomite and calcareous claystone. Based on Tg2 on COOBER PEDY ,TAL L AR INGA.
Tig2PIDINGA FOR MATION: S iltstone, carbonaceous; lignite; sand,carbonaceous. Palaeochannel fill.Tbp
GAR FOR D FOR MATION UNIT 1: W hite, green, dolomitic, palygorskitic orsepiolitic clay. Based on Tg1 on COOBER PEDY , TAL L AR INGA.Tig1
PLEISTOCENE
PLEIS TOCENE AL L U V IAL/FL U V IAL UNIT 3: Pleistocene high-levelalluvial fan gravel. Based on Q pa1 on preliminary W AR R INA.Qpa3PLEIS TOCENE AL L U V IAL/FL U V IAL UNIT 7: Pleistocene floodplaindeposits: clay, sand, silt, gravel. Based on Q pf, ABMINGA, COOBERPEDY .
Qpa7PLEIS TOCENE AL L U V IAL/FL U V IAL UNIT 8: Pleistocene alluvial/aeolianclayey-silty sand and gravel with some gilgai. Based on Q ps2, COOBERPEDY , TAL L AR INGA.
Qpa8PLEIS TOCENE AL L U V IAL/FL U V IAL UNIT 9: Pleistocene red-brown sand,clayey in part, with buckshot gravel spreads and widely-spaced gilgai.S ome aeolian influence. Based on Q ps3, COOBER PEDY .
Qpa9
PLEIS TOCENE AEOLIAN UNIT 1: Pleistocene dune core sand.Qpe1PLEIS TOCENE AEOLIAN UNIT 8: Pleistocene pale sand, calcareous inpart. Based on Q ps0, TAL L AR INGA.Qpe8PLEIS TOCENE AEOLIAN UNIT 9: Pleistocene red-brown sand associatedwith ferruginous and siliceous duricrusts; buckshot ironstone gravel.Alluvial influence. Based on Q ps1, COOBER PEDY , TAL L AR INGA.
Qpe9
W INTR ENA FOR MATION: S and, brown and orange-brown sand, Dunes,aeolian.Qpei
PLEIS TOCENE CALCR ETE: Undifferentiated Pleistocene calcrete.Qp\caPLEIS TOCENE GY PCR ETE: Undifferentiated Pleistocene gypcrete.Qp\gy
GIDDINNA FOR MATION UNIT 1: S andy facies associated with Mesozoicsandstone. Based on Q pgi on COOBER PEDY .Qprg1
GIDDINNA FOR MATION: Clay and silt, red, gravelly and sandy in part,moderately indurated.Qprg
PLEIS TOCENE R EGOLITH/COL L U V IAL UNIT 5: Pleistocene red sandwith maghemite gravel veneer, typically mulga-covered.Qpr5PLEIS TOCENE R EGOLITH/COL L U V IAL UNIT 6: Pleistocene ironstonegravel spreads on alluvium and colluvium. Based on blue dot overprintwithin Q a on CU R DIMU R KA, Q 2 on KINGOONY A.
Qpr6
BENITOS CLAY : Clay, red-brown to brown, silty.Qprb
Any person purchasing this map may reproduce it for their own useor that of their staff, but not for any other purpose ex cept with the written
permission of the Chief Ex ecutive, Department for Energy and Mining S A, GPO Box 320,Adelaide, S outh Australia, 5001.CR OW N COPY R IGHT R ES ER V EDDepartment for Energy and Mining S A.
Topographic detail based on TOPO-250K GEODATA (source scale 1:250 000)supplied by Geoscience Australia - National Mapping Division, ACT.The relationship between this data and DEM data is not guaranteed.
Computer generated from S A_GEOLOGY database(Digital data available upon request)Current version 2018.Digital
Product of S patial Information S ervices.Published by, and with the authority of, theDepartment for Energy and Mining S A.
Grey numbered lines indicate the 10000 metre Map Grid
The lake boundaries displayed on this map may have been derived from geological interpretationand may not match lakes interpreted by topographic mapping authorities.
Not all structures are represented on this particular map.Mapping and Compilation by M.C. Benbow, B.S c. with contributions by V . V itols, B.S c., L.C.Barnes, B.S c.(Hons), G.W . Krieg, B.S c.(Hons), P.A. R ogers, B.S c.(Hons), G.M. Pitt, B.S c., and
A.F. Crooks, B.S c.
Geological boundaries displayed on this map have beenDerived from geological interpretation and are notintended to be used for navigational purposes.Copies of this map can be obtained from theDepartment for Energy and Mining S A, Adelaide.
2020
Transverse Mercator Projection, Geocentric Datum Australia, 2020.
2020
R .C. Cobcroft, Director, Geological S urvey of S outh Australia.
