Quaternary palaeochannel evolution and groundwater movement in the Coleambally Irrigation District of New South Wales

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1 University of Wollongong Research Online University of Wollongong Thesis Collection University of Wollongong Thesis Collections 2 Quaternary palaeochannel evolution and groundwater movement in the Coleambally Irrigation istrict of New South Wales Kevin Pucillo University of Wollongong Recommended Citation Pucillo, Kevin, Quaternary palaeochannel evolution and groundwater movement in the Coleambally Irrigation istrict of New South Wales, Ph thesis, School of arth and nvironmental Sciences, University of Wollongong, 2. Research Online is the open access institutional repository for the University of Wollongong. For further information contact Manager Repository Services: morgan@uow.edu.au.

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6 RIV IRRIT ION RR BINYH ST RIN TON PO INT I MU RRU MB WY Figure 4.6*. Position of CIC and NSW WR boreholes in the Coleambally district. WH IT T ON Murrumbidgee River ST C RR IN TO N ST NRRN Murrumbidgee River URO Y N W ON ROSS R OO STURT ONI R 19 1 COCKYS 9 6 W MIN T ON R 7 19 CH T N CT OU N R 221 RCI C R 4 C N CITRUS R M IN MC Y RTH C M 6 3 W R 2 HRV YS 1 6 N R HWY O R M O RH 66 M OY S SI Y IBRT R OS CR 93 C 9 6 MCRTY 8 BY NN R THURRO W R. POIN T JRI RI C N U R O R MM Y 1 39 R RI R. POIN T S N JRI TH 4 ON RORT S W MBIN 48 7 BO NONS MCN R I BR V FI Y S PU 29 N O MC 17 MM Y WOO. POIN T MR TH RI R TO N C PR S NS 189 BO 7 17 JRI R HUTCHIN S CO MM I 17 H Y US H NN B RI R. POINT JRI FRNB NK T 2 RN C O RR P 21 R 21 1 STON S UC I FIR KRS K R MR ROO OON R P 61 NIN 92 KNT 6 CHN N 17 HU NT 22 M N N IN SOUTH BOUNRY SH P MUNT Z M RC R CUY BU N W HW Y 17 1 PRICK Y OV 7 R OV MY JIM BURK ROSW O OWNS CIFFOR V WIN 4 39 CU PIN R ISHR 78 2 KINF RR 41 O 1 7 Z FR ST KY MRTIN B 21 UO 641 NR S ON R 17 MORUN H KO KR Colombo Creek Yanko Creek egend Topographic Contours NSW_WR Bores CI Properties Peizometers xternal Farms Major rainage CI Boundary Minor rainage CIC Bores Roads Kilometers 1

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8 Coly4 Cross-section H Buried Borehole levation (m H) 1 egend Fluvial roup Figure.1*. Paleaochannel stratigraphy at sections Coly1, Coly2, Coly3, Coly4 and Coly. ll intersected palaeochannel belts and previously mapped palaeochannel positions are indicated. irection of palaeo-flow is out of the page for all cross-sections. 2. Channel Belt Zones Marginal Channel Sediments 1 2 Kilometers Waddi Cararbury Coarse Channel Sediments Palaeochannel Position Tie ine Tubbo Boona Floodplain and Intermediate Sediments Yamma F Bundure I H J 1 Coly3 Cross-section 9 F C Coly Cross-section I levation (m H) 1 Buried J Southern Prior Stream (Schumm, 1968) Coleambally System (Page, 1994; Page et al., 1996) Bundure rm, Coleambally System (Page, 1994; Page et al., 1996) B egend 1 Coly Cross-section Coly_1 1 Coly_2 9 Coly_3 Coly_4 9 Coly_ 2, 1,2 2,, 7, Upper Shepparton Channel Belts C Banandra Boona Bundure Cararbury idgell Tubbo Waddi Yamma 1, Meters Coly1 Cross-section levation (m H) levation (m H) Kerabury System (Page, 1994; Page et al., 1996) levation (m H) Northern Prior Stream (Schumm, 1968) Kerabury System (Page, 1994; Page et al., 1996) Coly2 Cross-section Northern Prior Stream (Schumm, 1968) Kerabury System (Page, 1994; Page et al., 1996) Buried B Central Prior Stream (Schumm, 1968) Yamma rm, Coleambally System (Page, 1994; Page et al., 1996)

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10 WI 1 WI Floodplain rainage Channels 187 entle Rise in Floodplain Surface (1) T: 19.2 ± 1.1 ka (3) T: 37.1 ± 1.7 ka Channel Fill (epth 4.2 m) KPH_ (2) (epth 2. m) Page and Nanson (1996) une-floodplain Interface (epth 4.1 m) (1) (.7 m H) KPH_4 T: 23.2 ± 1.2 ka 33 (2.8 m H) KPH_3 KPH_2 Position of Kerarbury System (Waddi Reach) (8.6 m H) KPH_1 (. m H) WI 3 Hyperbolic Reflectors Overhead Power ines une-floodplain Interface (.2 m H) Parallel Reflectors T: 38.6 ± 1.7 ka une-floodplain Interface T: 37. ± 2. ka (epth 6.6 m) T: 36.2 ± 1.8 ka (epth 4.1 m) (epth 4.1 m) KPH_6 WI 4 (4.8 m H) une-floodplain Interface (1) une-floodplain Interface Figure 7.6*. round penetrating radar imaging and thermoluminescence dating results from source-bordering dunes along the Waddi channel belt at Uri Park. For site details refer to Figure 7.2 Waddi 4 une ooking Northwest From Waddi 3 T: 47. ± 2.1 ka (epth 3.9 m) une-floodplain Interface

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12 Figure 7.7*. round penetrating radar imaging and thermoluminescence dating results from source-bordering dunes along the Boona channel belt at Property 1/7. For site details refer to figure 7.3 Boona 1 32 KPH_8 (1.9 m H) 3 KPH_9 (.2 m H) T: 26.8 ± 1.3 ka (epth 3.4 m) KPH_7 (7.4 m H) (1) (2) T: 76.2 ± 4. ka T: 32.2 ± 2.3 ka (epth 3.1 m) (epth 7. m) une-floodplain Interface une-floodplain Interface On-lapping Reflectors ipping Reflectors une-floodplain Interface Wire Fence Wire Fence

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14 Coly4 Cross-section Figure 8.3*. istribution of permeable sediments and their relationship to palaeochannel units at sections Coly1, Coly2, Coly3, Coly4 and Coly. Trends in piezometric level at each section for the period from are also shown. H Kilometers levation (m H) egend Waddi Borehole Fluvial roup Permeability roup Marginal Channel Sediments Piezometer ata ( - 3 meters) 1 Transitional Zone Max September evel (199-24) Coarse Channel Sediments oamy Sand Boona Minimum September evel (199-24) Yamma Standard eviation of September ata (199-24) Floodplain and Intermediate Sediments Sandy oam Bundure 2,6 1,3 2,6,2 7,8 1,4 Meters H J 1 - H levation (m H) Palaeochannel Position Tie ine I Mean September Piezometric (-3m) evel m (H) 9 Cararbury Tubbo F Coly South Mean September evel (199-24) Sand and ravel Coly North Standard eviation (m) Channel Belt Zones B - 1 egend Coly Cross-section Coly_1 Hydrogeological Zone Boundary Coly_2 Transitional Zone Coly_4 Coly_ Coly_ Upper Shepparton Channel Belts C Banandra Boona Bundure Cararbury idgell Tubbo Waddi Yamma Coly3 Cross-section Coly2 Cross-section Coly Cross-section F I 1 Coly North Zone F Coly South Zone Transitional Zone I C J levation (m H) 4. Standard eviation (m) Standard eviation (m) 9 Transitional Zone levation (m H) levation (m H) levation (m H) levation (m H) levation (m H) C J Standard eviation (m) Coly1 Cross-section B levation (m H) levation (m H) Transitional Zone Coly South Zone B Standard eviation (m) Coly North Zone

Quaternary palaeochannel evolution and groundwater movement in the Coleambally Irrigation District of New South Wales

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