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’s river : stream character and regional analysis. Volume 2: Appendices.

Kathryn Jerie, Ian Houshold and David Peters Conservation Branch, DPIWE June 2003

Cover Photos: Top: James River on the Central Plateau. Bottom left: Vanishing Falls on the Salisbury River, southern Tasmania (photo by Rolan Eberhard). Bottom right: Sorrel River, south of . Contents

Appendix 1. Conversion from 1:250,000 map codes to lithostructural elements ...... A1-1

Appendix 2. Development of the peat process region from Kirkpatrick and Dickinson (1984) vegetation codes ...... A2-1

Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour...... A3-1

Appendix 4. Regionalisation Results 2. The domains found in the case study area sub-regional domain mosaics...... A4-1

Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area. A5-1

Appendix 6. Regionalisation Results 4. The Upper Macquarie and Aplsey domain mosaics and the system controls on river development and behaviour...... A6-1

Appendix 7. The conservation and management of rivers and streams of King Island...... A7-1

Appendix 8. The rivers of the Region ...... A8-1

Appendix 9. The Upper Macquarie River catchment...... A9-1

Appendix 10. The statewide river characterisation database...... A10-1

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Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

This data is contained in twice, once in alphabetical order of geology code, and again in order of the lithostructural elements.

Table 1: The conversion from 1:250,000 geology map codes to lithostructural elements groups in order of geology codes. Geology Geology description Lithostructural code elements map category Ca Middle Cambrian conglomeratic and arenaceous units. volcano- Cac Dominantly siliceous and . folded & Cal Lithicwacke and conglomerate, with ultramafic detritus in volcano-sediment places. Caq Quartzwacke and conglomerate (Island Road Formation and volcano-sediment correlates). Cas Siliceous sandstone and conglomerate (Trial Ridge volcano-sediment Formation). Cb Undifferentiated low-Ti tholeiitic and boninitic . volcano-sediment Cba Boninitic lavas volcano-sediment Cbt Low-Ti Tholeiitic lavas. volcano-sediment Cbtg Gabbroic rocks associated with low Ti-lavas.. volcano-sediment Cc Feldspathic and -rich lithicwacke, mudstone and volcano-sediment sequences. Ccb . volcano-sediment Ccc Chert. volcano-sediment CD Undifferentiated Wurawina supergroup. Mathinna/Eldon Cd Undifferentiated Wurawina supergroup. volcano-sediment Cda Dominantly andesitic volcanic and intrusive rocks ( includes volcano-sediment Lobster Creek ). Cdb Dominantly shoshonitic, basaltic to andesitic volcanics (Que- volcano-sediment Hellyer and correlates including and Beulah Formation). Cdd Tholeiitic dolerite (Mt Charter area; upper Leven River). volcano-sediment Cdf Quartz- porphyry. volcano-sediment Cdg (includes Dove Granite, Beulah Granite). Cdq Quartz-phyric volcaniclastic, lavas and intrusives volcano-sediment ('Eastern sequence', Fish Creek sequence and possible correlates in Elliot Bay area). Cds Dominantly sedimentary sequences; withj minor volcanic and volcano-sediment volcaniclastic units (includes Farrell ). Cdsp Polymict sedimentary sequences with Middle Cambrian volcano-sediment (Lower Dundas Group, Huskisson Group). Cdsq Dominantly siliciclastic sandstone and conglomerate of partly volcano-sediment Precambrian (Tyennan) provenance (including Beds, Miners Ridge Sandstone and Animal Creek ). Cdsv Dominantly felsic volcanosedimentary sequences of volcano-sediment

A1-1 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

sandstone, siltstone, conglomerate, volcaniclastic and minor (includes Sequence). Cdt Dominantly felsic volcanoclastic sequences (Tyndall Group volcano-sediment and correlates). Cdtl Felsic lavas within Tyndall Group. volcano-sediment Cdv Felsic to intermediate calc-alkaline volcanic rocks (Central volcano-sediment Volcanic Complex and correlates including "Minnnow Keratophyry"). Cg Gabbroic rocks volcano-sediment Cm Polymict conglomerate, lithicwacke, siltstone and mudstone volcano-sediment with rare marine fossils (Scopus Formation). CO Undifferentiated or poorly constrained conglomerate folded quartzite & sequences (includes Roland Conglomerate and Duncan schist Conglomerate). COd Tholeiitic dolerite (Black Bluff Range). volcano-sediment COh Dominantly thick bedded siliceous conglomerate (Huntley folded quartzite & Conglomerate and correlates including Reeds Conglomerate; schist Mt Conglomerate; Misery Conglomerate). COl Thin bedded quartz sandstone, siltstone and minor folded quartzite & conglomerate (Linda Sandstone; Tim Shea Sandstone and schist correlates). COn Dominantly marine sandstone, micaceous siltstone and minor folded quartzite & conglomerate (Newton Creek Sandstone and correlates schist including 'Middle Owen Sandstone'). COs Dominantly siliceous conglomerate and pebbly sandstone folded quartzite & near Queenstown (Sedgwick Conglomerate); correlates of schist dominantly quartzwacke and minor conglomerate near Adamsfield (Singing Creek Formation). COu Undifferentiated or poorly constrained dominantly quartz folded quartzite & sandstone sequences with rare fossils (includes Moina schist Sandstone and correlates with Pioneer Beds at top). COuc Dominantly quartz sandstone and pebble conglomerate folded quartzite & (Cattley Conglomerate and correlates including Florentine schist Valley, Squirrel Creek and Cabbage Tree Formations). COucb Tholeiitic basalt (Mt Tor area; upper Wilmot river). volcano-sediment Cs Layered , and associated rocks. /ultramafic Csd Dominantly serpentinised layered and mafic/ultramafic ("LDH association"). Csp Dominantly layered and dunite ("LDP mafic/ultramafic association"). Csx Undifferentiated serpentised layered pyroxenite, peridotite, mafic/ultramafic and basalt ("LPG association"). Ct and associated rocks. volcano-sediment Cw Turbiditic mafic , red mudstone and chert volcano-sediment (Cleveland-Waratah association and correlates). Cwb Tholeiitic basalt (within Cleveland-Waratah association and volcano-sediment correlates; includes Motton ). Cwc Chert (Cleveland-Waratah association). volcano-sediment Cwmb Tholeiitic basalt and picrite ('Miners Ridge basalt', Birch Inlet volcano-sediment Volcanics, basalts of Mainwaring River area). Dc Terrestrial cavern fillings (Eugenana Beds). Dd Dolerite dykes. dolerite Dg Undifferentiated granitic rocks. granitoids

A1-2 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

Dga Undifferentiated alkali-feldspar granite/granite/adamellite (I- granitoids type). Dgaa Dominantly adamellite/granite and associated dykes. granitoids Dgaas Dominantly adamellite/ granite (S-type). granitoids Dgaf Alkali-feldspar granite (I-type). granitoids Dgafs Dominantly alkali-feldspar-granite (S-type). granitoids Dgas Undifferentiated alkali-feldspar-granite/ granite/ adamellite granitoids (S-type). Dgd Dominantly . granitoids Dgn Dominantly / adamellite. granitoids Dgr Dominantly granodiorite. granitoids Dl dykes and intrusive bodies. dolerite Dp Felsic pyroclastic rocks (St. Marys Porphyrite, volcanic granitoids equivalent of I-type granodiorite). Jb Basalt (tholeiitic), comagmatic with Jurassic dolerite (Lune basalt River area). Jd Dolerite (tholeiitic) with locally developed . dolerite Ka Appinitic lava and intrusives, associated with lamprophyre dolerite dykes (Cape Portland area). Ks and related alkaline rocks (Cygnet and Kettering dolerite area). Laa (Tyennan Region and Arthur Metamorphic volcano-sediment Complex). Lac Chloritic schist with minor , and folded quartzite & (Arthur Metamorphic Complex). schist Lap Phyllite with minor schist, foliated quartzite and folded quartzite & dolomite, and rare conglomerate. schist Lat Quartz--schist, quartzite, phyllite and rare dolomite folded quartzite & (Keith Schist and correlates). schist Lc Undifferentiated Clark Group rocks and correlates. folded quartzite & schist Lcd Dominantly carbonate. carbonate Lcm Dominantly mudstone and siltstone. folded lutite Lcq Dominantly orthoquartzite. folded quartzite & schist Ldb Tholeiitic basalt. volcano-sediment Lds Shallow water quartz sandstone and siltstone with carbonate volcano-sediment and chert beds (Success Creek Group and correlates). Ldv Turbiditic volcaniclastic - mafic volcanic rocks (Crimson volcano-sediment Creek Formation and correlates). Lg Granitic rocks. granitoids Lh Quartz-rich lithicwacke, conglomerate and black . folded lutite Lm Tholeiitic dolerite dykes (Rocky Cape Dyke swarm). dolerite Lo Unmetamorphosed quartzwacke turbidite sequences ( Burnie volcano-sediment and Oonah Formation and correlates). Lob Alkali basalt and dolerite (within Burnie and Oonah volcano-sediment Formations; includes Cooee Dolerite). Lod Dolomitic mudstone, siltstone and sandstone. volcano-sediment Loq Quartzwacke of high-grade metamorphic provenance (Burnie volcano-sediment and Oonah Formations and correlates). Lr Undifferentiated the Rocky Cape Group rocks. folded lutite Lrc Dominantly dark, laminated, commonly pyritic siltstone and folded lutite

A1-3 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

mudstone (Cowrie Siltstone and similar sequences). Lrd Well-bedded, cross-bedded, orthoquartzite and subordinate folded quartzite & siltstone (Detention Subgroup). schist Lri Laminated grey siltstone, mudstone and dolomite (Irby folded lutite Siltstone). Lrj Well-bedded, cross-bedded, orthoquartzite, platy quartzite folded quartzite & and siltstone (Jacobs Quartzite). schist Lrs Unassigned quartzite sequences. folded quartzite & schist Ls Undifferentiated sequences including carbonate, clastic and volcano-sediment volcaniclastic turbiditic rocks and tholeiitic basalt (Togari and Ahrberg groups). Lsb Tholeiitic basalt (Spinks Creek Volcanics, Bernafai Volcanics volcano-sediment and correlates). Lsc Basal siliceous conglomerate and sandstone (Forest folded quartzite & Conglomerate and Quartzite, Donaldson Formation and schist correlates). Lsd Shallow marine dolomite and minor (Smithton carbonate Dolomite and correlates). Lsr Pale-, thin bedded, laminated quartz siltstone with folded lutite subordinate interbedded fissile . Commonly silicified. Lss Shallow marine dolomite, chert, shale and (Black carbonate River Dolomite, Savage Dolomite and correlates). Lsv Turbiditic mudstone, siltsone, lithicwacke and diamictite with volcano-sediment dominantly mafic detritus Lt Undifferentiated pelitic rocks and quartzite sequences, with folded quartzite & . schist Ltb Dominantly schistose conglomerate (Goat Island folded quartzite & Conglomerate and correlates). schist Ltd Dolomite. carbonate Ltp Dominantly pelitic sequences, mainly phyllite, with folded quartzite & greenschist facies metamorphism. schist Ltpc Pelitic schist. folded quartzite & schist Ltpg Garnetiferous pelitic schist. folded quartzite & schist Lts Dominantly quartzite. folded quartzite & schist Ltsg Garnetiferous quartzite. folded quartzite & schist Ltsl Platy or schistose micaceous quartzite. folded quartzite & schist Luf Schistose conglomerate, quartzite, slate. phyllite and silicified folded quartzite & conglomerate (sequences of uncertain assignment including schist Wedge River Beds) Lw Undifferentiated Weld River Group rocks and correlates. carbonate Lwa Basal conglomerate and sandstone. folded quartzite & schist Lwc Dolomite, diamictite and mudstone. carbonate Lwt Shallow-marine dolomite. carbonate OD Turbidite sequences, undifferentiated (Mathinna Group). Mathinna/Eldon ODp Dominantly pelitic turbidite sequences (Mathinna Group). Mathinna/Eldon ODq Micaceous quartzwacke turbidite sequences (Mathinna Mathinna/Eldon

A1-4 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

Group). Ol Shallow marine limestone sequence with minor siltstone and carbonate sandstone (Gordon Group). Ola Mainly siltstone and fine-grained sandstone (Arndell Mathinna/Eldon Sandstone, "Rinadeena Shale" and correlates). P Undifferentiated Late Carboniferous-Permian glacial, Parmeener glaciomarine and non-marine sedimentary rocks. Pc Freshwater sandstone with measures. Parmeener Pf Freshwater and paralic sandstone and mudstone with some Parmeener coal measures. Pl Lower glaciomarine sequences of mudstone, pebbly Parmeener mudstone, pebbly sandstone, minor limestone and Tasmanite oil shale. PR Undifferentiated Parmeener Supergroup rocks. Parmeener Pt Basal tillite. Parmeener Pu Upper glaciomarine sequences of pebbly mudstone, pebbly Parmeener sandstone and limestone. Q Undifferentiated Quaternary . undifferentiated Q Qh and of alluvial, lacustrine and littoral origin. undifferentiated Q Qp Glacial, periglacial and fluvioglacial sediments including glacial and interglacial deposits. Qpg Pleistocene glacial and glacigene deposits. glacial Qpl Limestone. carbonate Qps Coastal sand and gravel. coastal Q Qpt Talus, vegetated and active. talus & R Undifferentiated Triassic fluviolacustrine sequences of Parmeener sandstone, siltstone and mudstone. Rb Alkali basalt/hawaiite (St Marys area). basalt Rq Dominantly quartz sandstone. Parmeener Rv Dominantly lithic sandstone with felsic volcaniclastics. Parmeener Rvc Lithic sandstone, siltstone and mudstone with some coal and Parmeener basal quartz sandstone. Rvv Dominantly siltstone, lithic sandstone and mudstone. Parmeener SD Shallow marine quartz sandstone, siltstone and shale (Eldon Mathinna/Eldon and Tiger Range Groups and correlates). SDa Siltstone, shale and minor quartz sandstone (Austral Creek Mathinna/Eldon Siltstone, Amber Slate and Keel Quartzite). SDb Siltstone, shale and fine-grained sandstone (Bell Shale, Mathinna/Eldon McLeod Formation and correlates). SDc Shallow marine quartz sandstone and pebble conglomerate Mathinna/Eldon (Crotty Quartzite and correlates). SDf Shallow marine quartz sandstone (Florence Quartzite, Richen Mathinna/Eldon Siltstone and correlates). SDl Limestone. carbonate Tb Basalt (tholeiitic to alkalic) and related pyroclastic rocks. basalt Tc Conglomerate, gravel and grit. Tertiary Tf Ferricrete, and derived lag deposits. Tertiary Tm Marine limestone. carbonate TQ Undifferentiated Cainozoic sediments. undifferentiated Q Ts Dominantly non-marine sequences of gravel, sand, silt, Tertiary and . water water water

A1-5 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

Table 2: The conversion from 1:250,000 geology map codes to lithostructural elements groups in order of lithostructure Geology Geology description Lithostructural code elements map category Jb Basalt (tholeiitic), comagmatic with Jurassic dolerite (Lune basalt River area). Rb Alkali olivine basalt/hawaiite (St Marys area). basalt Tb Basalt (tholeiitic to alkalic) and related pyroclastic rocks. basalt Dc Terrestrial cavern fillings (Eugenana Beds). carbonate Lcd Dominantly carbonate. carbonate Lsd Shallow marine dolomite and minor limestone (Smithton carbonate Dolomite and correlates). Lss Shallow marine dolomite, chert, shale and diamictite (Black carbonate River Dolomite, Savage Dolomite and correlates). Ltd Dolomite. carbonate Lw Undifferentiated Weld River Group rocks and correlates. carbonate Lwc Dolomite, diamictite and mudstone. carbonate Lwt Shallow-marine dolomite. carbonate Ol Shallow marine limestone sequence with minor siltstone and carbonate sandstone (Gordon Group). Qpl Limestone. carbonate SDl Limestone. carbonate Tm Marine limestone. carbonate Qpt Talus, vegetated and active. coarse slope deposits Qps Coastal sand and gravel. coastal Q Dd Dolerite dykes. dolerite Dl Lamprophyre dykes and intrusive bodies. dolerite Jd Dolerite (tholeiitic) with locally developed granophyre. dolerite Ka Appinitic lava and intrusives, associated with lamprophyre dolerite dykes (Cape Portland area). Ks Syenite and related alkaline rocks (Cygnet and Kettering dolerite area). Lm Tholeiitic dolerite dykes (Rocky Cape Dyke swarm). dolerite Lcm Dominantly mudstone and siltstone. folded lutite Lh Quartz-rich lithicwacke, conglomerate and black slate. folded lutite Lr Undifferentiated the Rocky Cape Group rocks. folded lutite Lrc Dominantly dark, laminated, commonly pyritic siltstone and folded lutite mudstone (Cowrie Siltstone and similar sequences). Lri Laminated grey siltstone, mudstone and dolomite (Irby folded lutite Siltstone). Lsr Pale-weathering, thin bedded, laminated quartz siltstone with folded lutite subordinate interbedded fissile shale. Commonly silicified. Cac Dominantly siliceous conglomerate and sandstone. folded quartzite & schist CO Undifferentiated or poorly constrained conglomerate folded quartzite & sequences (includes Roland Conglomerate and Duncan schist Conglomerate). COh Dominantly thick bedded siliceous conglomerate (Huntley folded quartzite & Conglomerate and correlates including Reeds Conglomerate; schist Mt Zeehan Conglomerate; Misery Conglomerate).

A1-6 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

COl Thin bedded quartz sandstone, siltstone and minor folded quartzite & conglomerate (Linda Sandstone; Tim Shea Sandstone and schist correlates). COn Dominantly marine sandstone, micaceous siltstone and minor folded quartzite & conglomerate (Newton Creek Sandstone and correlates schist including 'Middle Owen Sandstone'). COs Dominantly siliceous conglomerate and pebbly sandstone folded quartzite & near Queenstown (Sedgwick Conglomerate); correlates of schist dominantly quartzwacke turbidite and minor conglomerate near Adamsfield (Singing Creek Formation). COu Undifferentiated or poorly constrained dominantly quartz folded quartzite & sandstone sequences with rare fossils (includes Moina schist Sandstone and correlates with Pioneer Beds at top). COuc Dominantly quartz sandstone and pebble conglomerate folded quartzite & (Cattley Conglomerate and correlates including Florentine schist Valley, Squirrel Creek and Cabbage Tree Formations). Lac Chloritic schist with minor phyllite, dolomite and magnesite folded quartzite & (Arthur Metamorphic Complex). schist Lap Phyllite with minor pelite schist, foliated quartzite and folded quartzite & dolomite, and rare conglomerate. schist Lat Quartz-mica-schist, quartzite, phyllite and rare dolomite folded quartzite & (Keith Schist and correlates). schist Lc Undifferentiated Clark Group rocks and correlates. folded quartzite & schist Lcq Dominantly orthoquartzite. folded quartzite & schist Lrd Well-bedded, cross-bedded, orthoquartzite and subordinate folded quartzite & siltstone (Detention Subgroup). schist Lrj Well-bedded, cross-bedded, orthoquartzite, platy quartzite folded quartzite & and siltstone (Jacobs Quartzite). schist Lrs Unassigned quartzite sequences. folded quartzite & schist Lsc Basal siliceous conglomerate and sandstone (Forest folded quartzite & Conglomerate and Quartzite, Donaldson Formation and schist correlates). Lt Undifferentiated pelitic rocks and quartzite sequences, with folded quartzite & greenschist facies metamorphism. schist Ltb Dominantly schistose conglomerate (Goat Island folded quartzite & Conglomerate and correlates). schist Ltp Dominantly pelitic sequences, mainly phyllite, with folded quartzite & greenschist facies metamorphism. schist Ltpc Pelitic schist. folded quartzite & schist Ltpg Garnetiferous pelitic schist. folded quartzite & schist Lts Dominantly quartzite. folded quartzite & schist Ltsg Garnetiferous quartzite. folded quartzite & schist Ltsl Platy or schistose micaceous quartzite. folded quartzite & schist Luf Schistose conglomerate, quartzite, slate. phyllite and silicified folded quartzite & conglomerate (sequences of uncertain assignment including schist

A1-7 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

Wedge River Beds) Lwa Basal conglomerate and sandstone. folded quartzite & schist Qp Glacial, periglacial and fluvioglacial sediments including till glacial and interglacial deposits. Qpg Pleistocene glacial and glacigene deposits. glacial Cdg Granite (includes Dove Granite, Beulah Granite). granitoids Dg Undifferentiated granitic rocks. granitoids Dga Undifferentiated alkali-feldspar granite/granite/adamellite (I- granitoids type). Dgaa Dominantly adamellite/granite and associated dykes. granitoids Dgaas Dominantly adamellite/ granite (S-type). granitoids

Dgaf Alkali-feldspar granite (I-type). granitoids Dgafs Dominantly alkali-feldspar-granite (S-type). granitoids Dgas Undifferentiated alkali-feldspar-granite/ granite/ adamellite granitoids (S-type). Dgd Dominantly diorite. granitoids Dgn Dominantly granodiorite / adamellite. granitoids Dgr Dominantly granodiorite. granitoids Dp Felsic pyroclastic rocks (St. Marys Porphyrite, volcanic granitoids equivalent of I-type granodiorite). Lg Granitic rocks. granitoids Cs Layered peridotite, serpentinite and associated rocks. mafic/ultramafic Csd Dominantly serpentinised layered dunite and harzburgite mafic/ultramafic ("LDH association"). Csp Dominantly layered pyroxenite and dunite ("LDP mafic/ultramafic association"). Csx Undifferentiated serpentised layered pyroxenite, peridotite, mafic/ultramafic gabbro and basalt ("LPG association"). CD Undifferentiated Wurawina supergroup. Mathinna/Eldon OD Turbidite sequences, undifferentiated (Mathinna Group). Mathinna/Eldon ODp Dominantly pelitic turbidite sequences (Mathinna Group). Mathinna/Eldon ODq Micaceous quartzwacke turbidite sequences (Mathinna Mathinna/Eldon Group). Ola Mainly siltstone and fine-grained sandstone (Arndell Mathinna/Eldon Sandstone, "Rinadeena Shale" and correlates). SD Shallow marine quartz sandstone, siltstone and shale (Eldon Mathinna/Eldon and Tiger Range Groups and correlates). SDa Siltstone, shale and minor quartz sandstone (Austral Creek Mathinna/Eldon Siltstone, Amber Slate and Keel Quartzite). SDb Siltstone, shale and fine-grained sandstone (Bell Shale, Mathinna/Eldon McLeod Formation and correlates). SDc Shallow marine quartz sandstone and pebble conglomerate Mathinna/Eldon (Crotty Quartzite and correlates). SDf Shallow marine quartz sandstone (Florence Quartzite, Richen Mathinna/Eldon Siltstone and correlates). P Undifferentiated Late Carboniferous-Permian glacial, Parmeener glaciomarine and non-marine sedimentary rocks. Pc Freshwater sandstone with coal measures. Parmeener Pf Freshwater and paralic sandstone and mudstone with some Parmeener coal measures.

A1-8 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

Pl Lower glaciomarine sequences of mudstone, pebbly Parmeener mudstone, pebbly sandstone, minor limestone and Tasmanite oil shale. PR Undifferentiated Parmeener Supergroup rocks. Parmeener Pt Basal tillite. Parmeener Pu Upper glaciomarine sequences of pebbly mudstone, pebbly Parmeener sandstone and limestone. R Undifferentiated Triassic fluviolacustrine sequences of Parmeener sandstone, siltstone and mudstone. Rq Dominantly quartz sandstone. Parmeener Rv Dominantly lithic sandstone with felsic volcaniclastics. Parmeener Rvc Lithic sandstone, siltstone and mudstone with some coal and Parmeener basal quartz sandstone. Rvv Dominantly siltstone, lithic sandstone and mudstone. Parmeener Tc Conglomerate, gravel and grit. Tertiary Tf Ferricrete, laterite and derived lag deposits. Tertiary Ts Dominantly non-marine sequences of gravel, sand, silt, clay Tertiary and regolith. Q Undifferentiated Quaternary sediments. undifferentiated Q Qh Sand gravel and mud of alluvial, lacustrine and littoral origin. undifferentiated Q TQ Undifferentiated Cainozoic sediments. undifferentiated Q Ca Middle Cambrian conglomeratic and arenaceous units. volcano-sediment Cal Lithicwacke and conglomerate, with ultramafic detritus in volcano-sediment places. Caq Quartzwacke and conglomerate (Island Road Formation and volcano-sediment correlates). Cas Siliceous sandstone and conglomerate (Trial Ridge volcano-sediment Formation). Cb Undifferentiated low-Ti tholeiitic and boninitic lavas. volcano-sediment Cba Boninitic lavas volcano-sediment Cbt Low-Ti Tholeiitic lavas. volcano-sediment Cbtg Gabbroic rocks associated with low Ti-lavas.. volcano-sediment Cc Feldspathic and quartz-rich lithicwacke, mudstone and chert volcano-sediment sequences. Ccb Basalt. volcano-sediment Ccc Chert. volcano-sediment Cd Undifferentiated Wurawina supergroup. volcano-sediment Cda Dominantly andesitic volcanic and intrusive rocks ( includes volcano-sediment Lobster Creek Porphyry). Cdb Dominantly shoshonitic, basaltic to andesitic volcanics (Que- volcano-sediment Hellyer basalts and correlates including and Beulah Formation). Cdd Tholeiitic dolerite (Mt Charter area; upper Leven River). volcano-sediment Cdf Quartz-feldspar porphyry. volcano-sediment Cdq Quartz-phyric felsic volcaniclastic, lavas and intrusives volcano-sediment ('Eastern sequence', Fish Creek sequence and possible correlates in Elliot Bay area). Cds Dominantly sedimentary sequences; withj minor volcanic and volcano-sediment volcaniclastic units (includes Farrell Slates). Cdsp Polymict sedimentary sequences with Middle Cambrian volcano-sediment fossils (Lower Dundas Group, Huskisson Group). Cdsq Dominantly siliciclastic sandstone and conglomerate of partly volcano-sediment

A1-9 Appendix 1. Conversion from 1:250,000 geology map codes to lithostructural elements

Precambrian (Tyennan) provenance (including Sticht Range Beds, Miners Ridge Sandstone and Animal Creek Greywacke). Cdsv Dominantly felsic volcanosedimentary sequences of volcano-sediment sandstone, siltstone, conglomerate, volcaniclastic breccia and minor lava (includes Yolande River Sequence). Cdt Dominantly felsic volcanoclastic sequences (Tyndall Group volcano-sediment and correlates). Cdtl Felsic lavas within Tyndall Group. volcano-sediment Cdv Felsic to intermediate calc-alkaline volcanic rocks (Central volcano-sediment Volcanic Complex and correlates including "Minnnow Keratophyry"). Cg Gabbroic rocks volcano-sediment Cm Polymict conglomerate, lithicwacke, siltstone and mudstone volcano-sediment with rare marine fossils (Scopus Formation). COd Tholeiitic dolerite (Black Bluff Range). volcano-sediment COucb Tholeiitic basalt (Mt Tor area; upper Wilmot river). volcano-sediment

Ct Tonalite and associated rocks. volcano-sediment Cw Turbiditic mafic volcaniclastics, red mudstone and chert volcano-sediment (Cleveland-Waratah association and correlates). Cwb Tholeiitic basalt (within Cleveland-Waratah association and volcano-sediment correlates; includes Motton Spilite). Cwc Chert (Cleveland-Waratah association). volcano-sediment Cwmb Tholeiitic basalt and picrite ('Miners Ridge basalt', Birch Inlet volcano-sediment Volcanics, basalts of Mainwaring River area). Laa Amphibolite (Tyennan Region and Arthur Metamorphic volcano-sediment Complex). Ldb Tholeiitic basalt. volcano-sediment Lds Shallow water quartz sandstone and siltstone with carbonate volcano-sediment and chert beds (Success Creek Group and correlates). Ldv Turbiditic volcaniclastic - mafic volcanic rocks (Crimson volcano-sediment Creek Formation and correlates). Lo Unmetamorphosed quartzwacke turbidite sequences ( Burnie volcano-sediment and Oonah Formation and correlates). Lob Alkali basalt and dolerite (within Burnie and Oonah volcano-sediment Formations; includes Cooee Dolerite). Lod Dolomitic mudstone, siltstone and sandstone. volcano-sediment Loq Quartzwacke of high-grade metamorphic provenance (Burnie volcano-sediment and Oonah Formations and correlates). Ls Undifferentiated sequences including carbonate, clastic and volcano-sediment volcaniclastic turbiditic rocks and tholeiitic basalt (Togari and Ahrberg groups). Lsb Tholeiitic basalt (Spinks Creek Volcanics, Bernafai Volcanics volcano-sediment and correlates). Lsv Turbiditic mudstone, siltsone, lithicwacke and diamictite with volcano-sediment dominantly mafic detritus water water water

A1-10 Appendix 2. Development of the peat process region from vegetation codes

Appendix 2. Development of the peat process region from Kirkpatrick and Dickinson (1984) vegetation codes

The table below lists the vegetation types from Kirkpatrick and Dickinson (1984) that were used to define the peat process region. The second column lists any conditions. Table 1: Vegetation types contributing to the peat process region. Vegetation type from Kirkpatrick and Circumstances where it is considered Dickinson (1984) part of the peat process region. Buttongrass moorland All Buttongrass moorland wet scrub mosaic All Rainforest wet scrub mosaic All Eucalyptus simmondsii [E. nitida] All Lake Wills complex All Western Central Plateau subalpine complex Only near February Plains Eastern alpine complex Only near Cloister Lagoon Wet scrub Only polygons on Collingwood River and west of E. coccifera Only on Permian slopes of Mount Picton and Hartz Mountains Western alpine Only on Dennison Range Heath Only on South Bruny – Cape Bruny and Tasman Head Rainforest Only on siliceous geology Recently burned rainforest Only on siliceous geology

References Kirkpatrick, J. B. and K. J. M. Dickinson (1984). Tasmania : vegetation map. Hobart, Forestry Commission.

A2-1

Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

This appendix consists of graphs that show the average and range of values of each system control on river development and behaviour, in each of the river domains. For the categorical system controls, graphs show the percentage of the total area of the domain that consists of that system control. For the continuous system controls, the graphs show the average value and the range from the 5th to the 95th percentile. Also included is a graph that shows the area covered by each domain.

To keep the data consistent with its presentation in other places in this report, the scale of some system controls has been altered. These units are described in Table 1, and it is important that you read these and remember them when interpreting the graphs.

A3-1 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Table 1. The units used to describe the system controls. System control Units Possible Notes range Geomorphic process Percent of 0 – 100 history domain covered by each process region Lithostructural elements Percent of 0 – 100 domain covered by each element Effective precipitation Centimetres -6.9 – Conversion from the commonly 256 used mm to cm was required in order to present all controls on one graph. Note that effective precipitation can be negative because it is rainfall minus evaporation. Coefficient of variation Dimensionless, 0 – 199 Multiplied by 100 in order to of effective precipitation multiplied by present all controls on one graph. 100 When the coefficient of variation is equal to 100, then the standard deviation in the data is equal to the mean. Average annual Millimetres 0 – 108 maximum daily rainfall Coefficient of variation Dimensionless, 0 – 52 Multiplied by 100 in order to of average annual multiplied by present all controls on one graph. maximum daily rainfall 100 When the coefficient of variation is equal to 100, then the standard deviation in the data is equal to the mean. Cross sectional curvature Standardised -32 – 41 Negative values denote valleys, (3x3 cell window) scale positive denote ridges. Cross sectional curvature Standardised -70 – 75 Negative values denote valleys, (15x15 cell window) scale positive denote ridges. Profile curvature Standardised -47 –43 Negative values denote an upward scale break of slope (eg of valley floor and valley wall), positive denotes downward breaks of slope (eg edge of western tiers). Relief Standardised 0 – 200 scale Slope Degrees 0 – 62

A3-2 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour. Geomorphic process history

120 aeolian 100 80 60 40

% of domain of % 20 0 0 100 200domain 300 400 500

120 100 glacmax 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 last glac 100 80 60 40

% of domain of % 20 0 0 100 200domain 300 400 500

120 peat 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 100 periglac 80 60 40

% of domain of % 20 0 0 100 200domain 300 400 500

A3-3 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour. Lithostructural elements

120 100 basalt 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 carbonate 100 80 60 40

% of domain of % 20 0 0 100 200domain 300 400 500

120 Cainozoic undifferentiated 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 coastal and 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 dolerite 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 folded lutite 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

A3-4 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

120 100 folded quartzite 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 glacial 100 80 60 40

% of domain of % 20 0 0 100 200domain 300 400 500

120 Granitoids 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 mafic and ultramafics 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 Mathinna/Eldon groups 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 100 Parmeener Supergroup 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

A3-5 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

120 coa rse slope de posits 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

120 Tertiary sediments 100 80 60 40

% of domain % of 20 0 0 100 200domain 300 400 500

120 Volcano-sedimentary sequences 100 80 60 40

% of domain 20 0 0 100 200domain 300 400 500

A3-6 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Coefficient of variation of effective precipitation (x100) 200 150 100 50 0 0 102030405060708090100dom ain

200 150 100 50 0 100 110 120 130 140domain 150 160 170 180 190 200

200 150 100 50 0 200 210 220 230 240domain 250 260 270 280 290 300

200 150 100 50 0 300 310 320 330 340domain 350 360 370 380 390 400

200 150 100 50 0 400 410 420 430 440domain 450 460 470 480 490 500

A3-7 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Effective precipitation (mm) 2500 2000 1500 1000 500 0 -500 0 102030405060708090100domain

2500 2000 1500 1000 500 0 -500 100 110 120 130 140domain 150 160 170 180 190 200

2500 2000 1500 1000 500 0 -500 200 210 220 230 240domain 250 260 270 280 290 300

2500 2000 1500 1000 500 0 -500 300 310 320 330 340domain 350 360 370 380 390 400

2500 2000 1500 1000 500 0 -500400 410 420 430 440domain 450 460 470 480 490 500

A3-8 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Coefficient of variation of average annual maximum daily rainfall (x100) 60 40 20 0 0 102030405060708090100domain

60 40 20 0 100 110 120 130 140domain 150 160 170 180 190 200

60 40 20 0 200 210 220 230 240domain 250 260 270 280 290 300

60 40 20 0 300 310 320 330 340domain 350 360 370 380 390 400

60 40

20 0 400 410 420 430 440domain 450 460 470 480 490 500

A3-9 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Average annual maximum daily rainfall (mm)

100

50

0 0 102030405060708090100domain

100

50

0 100 110 120 130 140domain 150 160 170 180 190 200

100

50

0 200 210 220 230 240domain 250 260 270 280 290 300

100

50

0 300 310 320 330 340domain 350 360 370 380 390 400

100

50

0 400 410 420 430 440domain 450 460 470 480 490 500

A3-10 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Cross sectional curvature, 3x3 pixel window (600x600 m) 30 15 0 -15 -30 0 102030405060708090100domain

30 15 0 -15 -30 100 110 120 130 140domain 150 160 170 180 190 200

30 15 0 -15 -30 200 210 220 230 240domain 250 260 270 280 290 300

30 15 0 -15 -30 300 310 320 330 340domain 350 360 370 380 390 400

30 15 0 -15 -30 400 410 420 430 440domain 450 460 470 480 490 500

A3-11 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Cross sectional curvature, 15x15 pixel window (3x3km) 80 40 0 -40 -80 0 102030405060708090100domain

80 40 0 -40 100 110 120 130 140domain 150 160 170 180 190 200

80 40 0 -40 -80 200 210 220 230 240domain 250 260 270 280 290 300

80 40 0 -40 -80 300 310 320 330 340domain 350 360 370 380 390 400

80 40 0 -40 -80 400 410 420 430 440domain 450 460 470 480 490 500

A3-12 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Relief (arbitrary scale) 200 160 120 80 40 0 0 102030405060708090100domain

200 160 120 80 40 0 100 110 120 130 140domain 150 160 170 180 190 200

200 160 120 80 40 0 200 210 220 230 240domain 250 260 270 280 290 300

200 160 120 80 40 0 300 310 320 330 340domain 350 360 370 380 390 400

200 160 120 80 40 0 400 410 420 430 440domain 450 460 470 480 490 500

A3-13 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Profile curvature 3x3 pixel window (600x600 m) 30 15 0 -15 -30 -45 0 102030405060708090100domain

15 0 -15 -30 -45 100 110 120 130 140domain 150 160 170 180 190 200

30 15 0 -15 -30 200 210 220 230 240domain 250 260 270 280 290 300

30 15 0 -15 -30 300 310 320 330 340domain 350 360 370 380 390 400

30 15 0 -15 -30 400 410 420 430 440domain 450 460 470 480 490 500

A3-14 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

Slope (degrees) 75 60 45 30 15 0 0 102030405060708090100domain

75 60 45 30 15 0 100 110 120 130 140domain 150 160 170 180 190 200

75 60 45 30 15 0 200 210 220 230 240domain 250 260 270 280 290 300

75 60 45 30 15 0 300 310 320 330 340domain 350 360 370 380 390 400

75 60 45 30 15 0 400 410 420 430 440domain 450 460 470 480 490 500

A3-15 Appendix 3. Regionalisation Results 1. The relationship between the stream domains and the system controls on river development and behaviour.

2 Area of each domain (km ). Note the logarithmic scale.

1000000 10000 100 1 0 102030405060708090100domain

1000000 10000 100 1 100 110 120 130 140domain 150 160 170 180 190 200

1000000 10000 100 1 200 210 220 230 240domain 250 260 270 280 290 300

1000000 10000 100 1 300 310 320 330 340domain 350 360 370 380 390 400

1000000 10000 100 1 400 410 420 430 440domain 450 460 470 480 490 500

A3-16 Appendix 4. Regionalisation Results 2. The domains found in the case study area sub- regional domain mosaics.

Appendix 4. Regionalisation Results 2. The domains found in the case study area sub-regional domain mosaics.

This appendix refers to the domain mosaics identified in the case study area of the upper Macquarie and Apsley catchments. It shows graphically the domain components of each mosaic.

Midlands boundary 100

80

60

40

20

Percent of Area 0 206 88 326 223 155 310 342 142 292 247 133 346 363

Domain

Macquarie Tier 100

80 60

40 20

Percent of Area 0 206 88 342 223 133 275 140 310 363 63 142 132 155 292

Domain

Midlands 100

80 60

40 20

Percent of Area 0 206 342 275 88

Domain

A4-1 Appendix 4. Regionalisation Results 2. The domains found in the case study area sub- regional domain mosaics.

Apsley uplands 100 80 60 40 20 Percent ofarea 0 93 181 87 145 244 338 170 248 487 171 233 341 446 349 184 438

Domain

Apsley lowlands 100 80

60 40

20 Percent of area 0 384 349 93 216 171 377 244 114 181

Domain

Crest of the Eastern Tiers 100

80 60

40 20

Percent of Area 0 93 244 233 438 171 145 441 184 384

Domain

100 Eastern draining uplands

80

60

40 20

Percent of Area 0 93 244 170 145 248 233 184 438 283 349 171 441

Domain

100 Eastern draining foothills 80 60 40 20 0 Percent of Area of Percent 93 244 170 438 145 171 349 441 343

Domain

A4-2 Appendix 4. Regionalisation Results 2. The domains found in the case study area sub- regional domain mosaics.

100 Eastern Draining lowlands

Pe 80 rce nt 60 of 40 Ar ea 20

0 41 93 28 34 17 39 38 7 1 9 1 9 4 Domain

100 West draining uplands

80 Pe rce60 nt of 40 Ar 20 ea 0 93 18 23 14 24 26 44 30 34 36 4 3 5 8 4 1 5 9 8 Domain

100 West draining basalt basin

80 Pe rce60 nt of 40 Ar 20 ea 0 93 38 34 17 21 36 4 9 1 6 8 Domain

100 The Pink subregion mosaics

80 Pe rce60 nt of 40 Ar 20 ea 0 97 41 32 28 18 40 26 24 43 93 30 14 20 28 30 14 31 8 2 0 4 7 4 8 9 8 0 8 3 5 5 6 Domain

100 Eastern Tiers western foothills Pe 80 rce60 nt 40 of Ar 20 ea 0 13 88 14 20 93 23 31 20 22 24 21 17 36 15 32 14 32 24 18 2 0 6 5 0 8 3 7 3 0 6 5 6 5 4 4 4 Domain

A4-3

Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

These graphs show the relationship between the domains found in each subregion in the upper Macquarie and Apsley case study area, and the system controls on river development and behaviour. The system controls and their effect on the landscape are described in chapter 4.

For each subregion, the graphs are arranged in order of spatial dominance, with the domain covering the largest area of the subregion presented first. The top 4 domains by area are graphed for each mosaic, and where there are domains that were diagnostic of the mosaic that cover a smaller area, these are also graphed.

For ease of comparison between domains, all the system controls for each domain are presented on one graph. Strictly speaking, each control should be graphed separately, because the scale is different for each. To present all the data on one graph has required the use of some unusual units, such as expressing precipitation in centimetres. These units are described in Table 1, and it is important that you read these and remember them when interpreting the graphs. For the climate and topography variables, the columns represent the average value for the domain, and the error bars represent the 5th and 95th percentiles of the range of data.

A5-1 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Table 1. The units used to describe the system controls. System control Units Possible Notes range Geomorphic process Percent of 0 – 100 history domain covered by each process region Lithostructural Percent of 0 – 100 elements domain covered by each element Effective Centimetres -6.9 – 256 Conversion from the commonly precipitation used mm to cm was required in order to present all controls on one graph. Note that effective precipitation can be negative because it is rainfall minus evaporation. Coefficient of Dimensionless, 0 – 199 Multiplied by 100 in order to variation of effective multiplied by 100 present all controls on one graph. precipitation When the coefficient of variation is equal to 100, then the standard deviation in the data is equal to the mean. Average annual Millimetres 0 – 108 maximum daily rainfall Coefficient of Dimensionless, 0 – 52 Multiplied by 100 in order to variation of average multiplied by 100 present all controls on one graph. annual maximum When the coefficient of variation daily rainfall is equal to 100, then the standard deviation in the data is equal to the mean. Cross sectional Standardised -32 – 41 Negative values denote valleys, curvature (3x3 cell scale positive denote ridges. window) Cross sectional Standardised -70 – 75 Negative values denote valleys, curvature (15x15 cell scale positive denote ridges. window) Profile curvature Standardised -47 –43 Negative values denote an upward scale break of slope (eg contact of valley floor and valley wall), positive denotes downward breaks of slope (eg edge of western tiers). Relief Standardised 0 – 200 scale Slope Degrees 0 – 62

A5-2 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Apsley uplands 93 (37 % of mosaic) 250

200

150

100

50

0

-50

181 (20 % of mosaic) 250

200

150

100

50

0

-50

87 (6 % of mosaic) 250

200

150

100

50

0

-50

145 (6 % of mosaic) 250

200

150

100

50

0

-50

A5-3 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

338 (5 % of mosaic) 250

200

150

100

50

0

-50

487 (2.5 % of mosaic) 250

200

150

100

50

0

-50

341 (1.5 % of mosaic) 250

200

150

100

50

0

-50

446 (1.2 % of mosaic) 250

200

150

100

50

0

-50

A5-4 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Apsley lowlands 384 (58 % of mosaic) 250

200

150

100

50

0

-50

349 (13 % of mosaic) 250

200

150

100

50

0

-50

93 (10 % of mosaic) 250

200

150

100

50

0

-50

216 (8.4 % of mosaic) 250

200

150

100

50

0

-50

A5-5 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

171 (4.3 % of mosaic) 250

200

150

100

50

0

-50

A5-6 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Crest of the Eastern Tiers 93 (81% of mosaic) 200

150

100

50

0

-50

244 (7.6% of mosaic) 200

150

100

50

0

-50

233 (4.7% of mosaic) 200

150

100

50

0

-50

438 (2.0% of mosaic) 200

150

100

50

0

-50

A5-7 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Eastern Uplands 93 (55% of mosaic) 200

150

100

50

0

-50

244 (11% of mosaic) 200

150

100

50

0

-50

170 (7.5% of mosaic) 200

150

100

50

0

-50

145 (6.6% of mosaic) 200

150

100

50

0

-50

A5-8 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

248 (5.2% of mosaic) 200

150

100

50

0

-50

233 (4.9% of mosaic) 200

150

100

50

0

-50

184 (2.7% of mosaic) 200

150

100

50

0

-50

438 (2.6% of mosaic) 200

150

100

50

0

-50

A5-9 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

283 (1.6% of mosaic) 200

150

100

50

0

-50

A5-10 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Eastern Foothiills 93 (71 % of mosaic) 200

150

100

50

0

-50

244 (13 % of mosaic) 200

150

100

50

0

-50

170 (4% of mosaic) 200

150

100

50

0

-50

438 (2% of mosaic) 200

150

100

50

0

-50

A5-11 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Eastern lowlands 417 (61% of mosaic) 200

150

100

50

0

-50

93 (16% of mosaic) 200

150

100

50

0

-50

281 (14% of mosaic) 200

150

100

50

0

-50

349 (5% of mosaic) 200

150

100

50

0

-50

A5-12 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

West draining uplands 93 (68% of mosaic) 200

150

100

50

0

-50

184 (6.3% of mosaic) 200

150

100

50

0

-50

233 (5.0% of mosaic) 200

150

100

50

0

-50

145 (4.4% of mosaic) 200

150

100

50

0

-50

A5-13 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

West draining basalt basin 93 (66% of mosaic) 200

150

100

50

0

-50

384 (20% of mosaic) 200

150

100

50

0

-50

349 (9.3% of mosaic) 200

150

100

50

0

-50

171 (3.8% of mosaic) 200

150

100

50

0

-50

A5-14 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Eastern Tiers Western Foothills 132 (38% of mosaic) 200

150

100

50

0

-50

88 (16% of mosaic) 200

150

100

50

0

-50

140 (9.6% of mosaic) 200

150

100

50

0

-50

206 (7.5% of mosaic) 200

150

100

50

0

-50

A5-15 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

93 (5.5% of mosaic) 200

150

100

50

0

-50

235 (3.9% of mosaic) 200

150

100

50

0

-50

247 (1.8% of mosaic) 200

150

100

50

0

-50

213 (1.7% of mosaic) 200

150

100

50

0

-50

A5-16 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Midlands Boundary 206 (56% of mosaic) 200

150

100

50

0

-50

88 (21% of mosaic) 200

150

100

50

0

-50

326 (3.7% of mosaic) 200

150

100

50

0

-50

223 (3% of mosaic) 200

150

100

50

0

-50

A5-17 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

310 ( % of mosaic) 200

150

100

50

0

-50

292 (1.6% of mosaic) 200

150

100

50

0

-50

133 (1.1% of mosaic) 200

150

100

50

0

-50

363 (0.7% of mosaic) 200

150

100

50

0

-50

A5-18 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Macquarie Tier 206 (55% of mosaic) 200

150

100

50

0

-50

88 (20% of mosaic) 200

150

100

50

0

-50

342 (5.0% of mosaic) 200

150

100

50

0

-50

223 (2.4% of mosaic) 200

150

100

50

0

-50

A5-19 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

133 (1.9% of mosaic) 200

150

100

50

0

-50

310 (1.7% of mosaic) 200

150

100

50

0

-50

363 (1.7% of mosaic) 200

150

100

50

0

-50

63 (1.6% of mosaic) 200

150

100

50

0

-50

A5-20 Appendix 5. Regionalisation Results 3. The domain based variability in system controls in the domain mosaics of the upper Macquarie and Apsley case study area.

Midlands 206 (52% of mosaic) 200

150

100

50

0

-50

342 (44% of mosaic) 200

150

100

50

0

-50

275 (2.3% of mosaic) 200

150

100

50

0

-50

A5-21