DOCSLIB.ORG

Copyrighted Material

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Copyrighted Material Index Note: Page numbers in italic refer to fi gures; those in bold to tables. abandonment, 111, 142, 158, 159, 161, average recurrence interval (ARI), 60 point, 133, 143, 148, 151, 152, 165 162, 210, 218 Avon River, NSW, 64 scroll, 143, 165 of channels, 76, 161, 163, 172, 189, 220 avulsion, 74, 161, 163, 186–187, 208 transverse, 141 abrasion, 33, 95, 115 unit, 151 abstraction, water, 272, 275 b-axis, 81 basefl ow, 48, 56 accommodation space, 34 backswamps, 14, 105, 112, 155, 170, 171, analysis, 58–59 accretion 188, 200, 221 basins abandoned channel, 158 formation of, 111, 170, 218 endorheic, 31, 255 counterpoint, 159, 159 backwater pool, 136 exorheic, 31 lateral, 156–157, 157, 258 badlands, 36, 38 zero-order, 51 oblique, 157 Bagnold criterion, 88 bedform, 115 vertical, 157–158, 158, 258 Bagnold equation, 91 confi gurations, 97, 100 accumulation zones, 108 banks deposition, 104 adjustment erosion of, 117–124 generation, 95–98 lateral, 186 processes, 117–124, 118 and bedload movement, 98–101 natural capacity for, 21, 223–224, 288 exposures, 112 bedload, 81–84 and river evolution, 255–261 forming, and bed degradation, 121 deposits, 156 pathways of, 225–227, 228 height of, factor of safety (FSh), 120 movement, 95–98 components, 226 mass failure of, 118 and bedform generation, 98–101 afforestation, 270, 273–274, 291, 296 morphology of, 120–123, 122 sheets, 98 Africa, rift valley, 240 processes, 117–124 transport, 29, 97 aggradation, 31, 38, 53, 117, 117, 208, protection of, 279 bedrock, 179 210 retreat cycle, 119 erodibility, 38 alluvium, 33, 33, 54 shear, factor of safety (FSτ), 120 steps, 31, 38, 136 removal of, 161 stability of, 120 beds see also ridges, alluvial strength of, 74, 197 degradation of, and bank forming Amazon Basin, 310, 313 Barnard River, NSW, 64 processes, 121 analogy, reasoning by, 265 barriers, 299, 303, 304, 307–308, 308 material, 33 analysis, basin-wide, 112 bars, 98, 133, 141, 149 downstream gradation in, 96 Andes, 240 bank-attached, 153 properties of, 202 annual exceedence probability, 60 COPYRIGHTEDbedrock core, 142, 143 MATERIALsize of, 201 antidunes, 97–98, 115 channel junction, 148 processes, 117–124 aquifers, 49 compound, 151, 152 and channel shape, 117 areas, variable source, 50–51 diagonal, 141 Bega catchment, NSW, 41, 42, 292, 300, armouring, 86, 92–93, 94, 103, 278, 287, expansion of, 141 312–315 305 forced, 143, 149, 152 Bega River, NSW, 99 associations, process–form, 231, 257, 265, lateral, 142, 148 behaviour, and change, 21–22, 21 293, 305 linguoid, 141 Bellinger catchment, NSW, 41–42, 42 auger holes, 112–113 longitudinal, 141, 151 benches, 123, 126, 143, 148 Australia, 314 mid-channel, 151–152 concave bank, 143, 148, 165 Geomorphic Analysis of River Systems: An Approach to Reading the Landscape, First Edition. Kirstie A. Fryirs and Gary J. Brierley. © 2013 Kirstie A. Fryirs and Gary J. Brierley. Published 2013 by Blackwell Publishing Ltd. 336 Index bend rotation, 184 relief of (H), 36 initiation of, 51–52 berms, 149 response gradients of, 26 irregular, 127, 127 boulder, 148, 187 runoff from, 50–51 laterally stable, 184 bifurcation ratio (Rb), 40 shape of, 34–35, 34, 43, 56 migration billabongs, 14, 158, 161, 188, 200–201 synthesising controls in, 305–309 lateral, 159, 161, 160, 208 biophysical processes, linkages of, 320 topography of, 57 rates of, 123 biostabilisation, 87 cavitation, 85, 136 zones, 321 bioturbation, 105, 170 celerity, 23, 72 morphology of, and hydraulic blankets, 303, 304, 307–308, 308 chain-of-ponds see ponds, chain of geometry, 127–131 blockages, 17, 39, 95, 303, 305, 307–308, change number of, 183–184, 184 318–319 and behaviour, 21–23, 21 planform, 179, 184–186, 201–202, boosters, 307 irreversible, 292 204 boundary conditions levels of, 237 measurement, 183, 196–197, 198 altered, 246–255, 266 reversible, 292 relationships, 111 fl ux, 7, 12–14, 13, 27, 223–224, 257 Channel Country, Australia, 192, 242, resistance, 67 predicting river responses to, 245 resisting forces in, 70–72 229–230, 238 Channel Scablands, Washington State, roughness of, 70, 70, 294 imposed, 7, 12–14, 13, 27, 37, 43, 206, 251 sand-bed, 97 222, 238, 302 channelisation, 277, 279 sediment entrainment in, 86–87 boundary resistance, 67 geomorphic effects of, 279, 280, 289 sediment transport in, 87–94 Brahmaputra, India, 310 channels, 248 shape of, 117–127, 125, 127 braided channels see channels, braided abandoned, 74, 158, 161, 162, 173, and bank processes in, 126 braided index (Bi), 184 189, 221 and bed processes, 117, 126 braiding, 184, 185, 196–197, 229 adjustment of infl uences on, 117–124 braidplains, 163, 210, 235, 251 lateral, 208 sinuosity, 183 bridge crossings, 279 vertical, 208 slope of, 31, 54 Bridge River, British Columbia, 245 wholesale, 208 stabilisation of, 279 British Columbia, 219 asymmetrical, 126, 127 supply-limited, 101 Bu Boys equation, 91 avulsion, 74, 161, 163, 208 symmetrical, 126, 127 Budderoo National Park, NSW, 175 base level cut of, 31 transport-limited, 101 buffering capacity, 25 boundary condition classifi cation, vertical adjustment in, 117 buffers, 303, 304, 307–308, 308 124 width of, 54 braided, 158, 159 Chezy coeffi cient, 75 Canadian Shield, 245 capacity-limited, 101 Chezy equation, 71 canals, 128, 197, 233, 271, 289 chute, 151 Chironomidae, 87 Cann River, Victoria, 281, 288 competence-limited, 101 chronology, 111 canopy drip, 46 compound, 126, 127 chutes, 98 capacity, 90 contraction of, 187, 208 channels, 151 cascades, 137, 180 coupled, 303 cut-offs, 151, 170 catastrophism, 24, 212 crevasse, 170 and pool trains, 98 catchments, 10, 12, 28, 42, 264 cross-sections of, 54 circularity ratio (Rc), 34 accumulation zone of, 79 decoupled, 303 Clarence River, NSW, 175, 216 area of (A), 34 deposition in, 65–67 clay, 84–85, 108 effective, 308 depth of, 54 climate, 236, 241–244, 266 area–discharge relationships, 59 discontinuous, 189–190, 221–222, change, 244, 275 confi guration infl uence, 41–42 221 river responses to, 250–255 defi nition of, 29 entrenchment of, 274 contemporary, 246 elements of, 30 erosion in, 65–67 imprint of past conditions, 244–246 human impacts on, 293–295 expansion of, 187, 208 regions, 311 hydrology of, 44–64 formation of, 52, 55 variability, 267 knowledge of, 322–323 geometry of, 74, 110, 116–131, 197, coeffi cient of variation (Cv), 62, 64, linkages in, 14–17 198, 201–202, 294 312 morphometrics of, 34–37 grain interactions in, 93–95 colluvium, 52, 300 as nested hierarchies, 9–12 gravel-bed, 130 colonisation, vegetative, 74, 123 position in, 124 impelling forces in, 68–70 Colorado River, USA, 278, 313 process zones in, 29–31, 30, 33, 306 incised, 117 Columbia River, USA, 251 relationships, 202–203 development of, 54 complex response, 24, 26, 28, 206 Index 337 component technique, 75 cut-offs, 161, 162, 170 and river fl ow, 54–56 condensation nuclei, 45 chute, 161, 162 sediment (Qs), 92–93 confi guration, 2–3, 7, 21, 25, 26–27, 79, neck, 161, 162 disconnectivity, 14–17 206, 233 cyclones, 250, 266 discontinuities, 264 bed, 71, 97, 137, 177 discriminant analysis, 195 of catchment, 31, 38–39, 41–42 dams, 249, 250, 271, 277–278, 304 disequilibrium, 20 channel, 71, 76, 210, 220, 259 as barriers, 303 distal fi ning, 157 plan view, 174, 183 geomorphic impacts of, 278, 287 disturbance events, 22–23 spatial, 9–12 ice, 251 press, 22 valley, 179 landslide, 305, 307 pulsed, 22 confi ned rivers, 34, 174, 175, 179–181, transverse clast, 99 ramp, 23 181, 195, 316 Darcy–Weisbach coeffi cient (ff), 75, responses to, 237 bedrock, 32, 77, 215 95 system responses to, 23 geomorphic adjustment in, 257 Darcy–Weisbach equation, 71 diversity, respect for, 321 and sediment transfer, 305 Darcy’s law, 48 drag, 87 sinuosity in, 183 Dart Brook, NSW, 182 fl uid, 85 width/depth ratio in, 125 dating tools, 264 drainage confi ned valleys, 29, 32, 108, 179–181, Davis, William Morris, 17 area, 34 181, 203–204, 233, 264, 315–316 defl ation, 273 basins, 7, 29 bankfull stage in, 55 degradation, 117, 208 see also catchments boulder mounds in, 142 pathway, 290 density (Dd), 36, 57 channel shape in, 127 dells, 190 network evolutionary pathways in, 237 deposition, 7, 84, 113 composition, 29 fl oodplains in, 156, 193, 201, 203 history of, 264 evolution, 36 forced features in, 137 in river systems, 103–104, 108–109 extension, 36, 36 river behaviour in, 214, 216 deposits pattern, 36–37 confi nement see valley confi nement bedload, 165 annular, 37 confl uence density, 38 bottom stratum, 165 contorted, 37 connectivity, 14–17, 319 overbank, 165 dendritic, 36–38 channel–fl oodplain, 170 supraplatform, 151 geologic controls on, 37–41, 37 and dams, 277 suspended-load, 156, 164 multi-basinal, 37 landscape, 7, 27, 302–304 tephra, 249 parallel, 37 spatial and temporal, 17 top stratum, 165 radial, 37 variability in, 16 valley fi ll, 171 rectangular, 37–38 conservation of energy principle, 65 wake, 99 trellis, 37–38 context within-channel, 165 dredging, 279 geologic/tectonic and climatic, 266 depth, 54, 116, 128 drill holes, 112–113 spatial and temporal, 3, 17, 26 description, 7 dunes, 97 continuity equation, 54, 128 desertifi cation, 273 fl attened, 98 controls desiccation, 117 point, 143, 149 antecedent, 24 desnagging, 271, 279 sand, 252 catchment-scale, 29–43 detachment, 85 dynamics, non-linear, 27 Coon Creek, USA, 300 digital elevation models (DEMs), 34 Cooper Creek, Australia, 149, 175, discharge (Q), 33, 33, 54, 64, 116, 197 earthquakes, 250, 306 220 bankfull, 55 ecological resilience, 320 corrasion, 85, 136 conditions, 123 ecosystem engineers, 243 corrosion, 136 dominant formative, 211 eddying, 85 cosmogenic dating, 264 effective,
Load more

Recommended publications
  • Orocline-Driven Transtensional Basins: Insights from the Lower Permian Manning Basin
    PUBLICATIONS Tectonics RESEARCH ARTICLE Orocline-driven transtensional basins: Insights 10.1002/2015TC004021 from the Lower Permian Manning Key Points: Basin (eastern Australia) • Structures in the Manning Basin confirm the existence of the Llyam White1, Gideon Rosenbaum1, Charlotte M. Allen2, and Uri Shaanan1 Manning Orocline • The Manning Basin is an Early 1School of Earth Sciences, University of Queensland, Brisbane, Queensland, Australia, 2Institute for Future Environments, Permian sinistral transtensional pull-apart basin Queensland University of Technology, Brisbane, Queensland, Australia • Spatiotemporal relationships link basin formation to oroclinal bending Abstract The New England Orogen in eastern Australia exhibits an oroclinal structure, but its geometry and geodynamic evolution are controversial. Here we present new data from the southernmost part of the Supporting Information: • Supporting Information S1 oroclinal structure, the Manning Orocline, which supposedly developed in the Early Permian, contemporaneously and/or shortly after the deposition of the Lower Permian Manning Basin. New U-Pb detrital zircon data provide Correspondence to: a maximum depositional age of ~288 Ma. Structural evidence from rocks of the Manning Basin indicates that L. White, both bedding and preoroclinal fold axial planes are approximately oriented parallel to the trace of the Manning [email protected] Orocline. Brittle deformation was dominated by sinistral strike-slip faulting, particularly along a major fault zone (Peel-Manning Fault System), which is marked by the occurrence of a serpentinitic mélange, and separates Citation: tectonostratigraphic units of the New England Orogen. Our revised geological map shows that the Manning White, L., G. Rosenbaum, C. M. Allen, and U. Shaanan (2016), Orocline-driven Basin is bounded by faults and serpentinites, thus indicating that basin formation was intimately linked to transtensional basins: Insights from the deformation along the Peel-Manning Fault System.
    [Show full text]
  • Government Gazette of the STATE of NEW SOUTH WALES Number 112 Monday, 3 September 2007 Published Under Authority by Government Advertising
    6835 Government Gazette OF THE STATE OF NEW SOUTH WALES Number 112 Monday, 3 September 2007 Published under authority by Government Advertising SPECIAL SUPPLEMENT EXOTIC DISEASES OF ANIMALS ACT 1991 ORDER - Section 15 Declaration of Restricted Areas – Hunter Valley and Tamworth I, IAN JAMES ROTH, Deputy Chief Veterinary Offi cer, with the powers the Minister has delegated to me under section 67 of the Exotic Diseases of Animals Act 1991 (“the Act”) and pursuant to section 15 of the Act: 1. revoke each of the orders declared under section 15 of the Act that are listed in Schedule 1 below (“the Orders”); 2. declare the area specifi ed in Schedule 2 to be a restricted area; and 3. declare that the classes of animals, animal products, fodder, fi ttings or vehicles to which this order applies are those described in Schedule 3. SCHEDULE 1 Title of Order Date of Order Declaration of Restricted Area – Moonbi 27 August 2007 Declaration of Restricted Area – Woonooka Road Moonbi 29 August 2007 Declaration of Restricted Area – Anambah 29 August 2007 Declaration of Restricted Area – Muswellbrook 29 August 2007 Declaration of Restricted Area – Aberdeen 29 August 2007 Declaration of Restricted Area – East Maitland 29 August 2007 Declaration of Restricted Area – Timbumburi 29 August 2007 Declaration of Restricted Area – McCullys Gap 30 August 2007 Declaration of Restricted Area – Bunnan 31 August 2007 Declaration of Restricted Area - Gloucester 31 August 2007 Declaration of Restricted Area – Eagleton 29 August 2007 SCHEDULE 2 The area shown in the map below and within the local government areas administered by the following councils: Cessnock City Council Dungog Shire Council Gloucester Shire Council Great Lakes Council Liverpool Plains Shire Council 6836 SPECIAL SUPPLEMENT 3 September 2007 Maitland City Council Muswellbrook Shire Council Newcastle City Council Port Stephens Council Singleton Shire Council Tamworth City Council Upper Hunter Shire Council NEW SOUTH WALES GOVERNMENT GAZETTE No.
    [Show full text]
  • HERITAGE STOCK HORSE ASSESSMENTS (A-C) Updated: 1St November 2019 Approved Modern Breeds Unknown Thoroughbred Breeds After 1945 After 1960
    HERITAGE STOCK HORSE ASSESSMENTS (A-C) Updated: 1st November 2019 Approved Modern Breeds Unknown Thoroughbred Breeds after 1945 after 1960 Name of Horse RegNo TB AB MB UB HSH Status Maximum Max 6.25% Max. 12.5% 100% Not Eligible 25% Combined Max 12.5% A BIT RASH 77780 Y 0 0 0 TB A COOL ACRE 234949 N 0 73.44 0 MB A GENTLE NUDGE BP-78750 Y 0 0 0 TB A LITTLE GOLD 77748 Y 0 0 0 TB A REWARD 74617 N 0 0 0 HSH A RIOT IN PARIS 74193 Y 0 0 0 TB A TOUCH OF CLASS 135153 Y 0 0 0 TB A TOUCH OF MAGIC 73306 N 0 0 0 HSH AACC CLEOPATRA 186032 N 0 43.75 0 LH AACC ELWOOD C2-188289 N 0 46.88 0 LH AACC EXPRESS C2-187868 N 0 46.88 0 LH AACC EXPRESSION 188286 N 0 12.5 0 LH AACC FEDERER 236049 N 0 25 12.5 LH AACC FORECAST C2-191980 N 0 53.13 0 MB AACC JEMIMA 197137 N 0 0 12.5 HSH AACC JODIE C2-178715 N 0 0 25 LH AACC RIPCURL C2-187870 N 0 59.38 0 MB AACC SPRITE 197922 N 0 50 0 MB AACC TRAVESTY 198605 N 0 40.63 6.25 LH AACC VALOAK 198022 N 0 34.38 12.5 LH AB RAY 35943 N 0 0 0 HSH ABA RAY 47264 N 0 0 0 HSH ABACIOMI 77441 Y 0 0 0 TB ABALMORES EXCEPTIONAL BELLA C1-199588 N 0 23.44 0 LH ABBA DABBA 30090 N 0 0 0 HSH ABBAGAIL 117120 N 0 0 0 HSH ABBALEE 33598 N 0 0 0 HSH ABBAMANDA 70990 N 0 0 0 HSH ABBCARS LITTLE WILDY 161304 N 4.69 0 0 HSH ABBELENA C1-237821 N 0 48.44 0 LH ABBELYSTIC 135950 N 0 0 0 HSH ABBER RAY DEE 103846 N 0 0 0 HSH ABBESS 130020 N 0 0 0 HSH ABBEY 448 N 0 0 0 HSH ABBEY BOY 56588 N 0 0 0 HSH ABBEY DOLL 106005 N 0 0 0 HSH ABBEY OKER 441 N 0 0 0 HSH ABBEY RUSH 152445 N 0 0 0 HSH ABBEY SKYE SM-161379 N 0 0 0 HSH ABBEY STAR 20213 N 0 0 0 HSH ABBEY SUE 63232 N 0 0 0 HSH ABBEY TANGO 20928 N 0 0 0 HSH Modern Breed - MBP 100%, MB 50-100% Heritage Stock Horse - HSH Approved Breed - ABP 100%, AB 50-100% Limited Heritage - LH (not eligible under other categories) Thoroughbred - TB Unknown Breed - UBP 100%, UB 50-100% Page 1 of 170 HERITAGE STOCK HORSE ASSESSMENTS (A-C) Updated: 1st November 2019 Approved Modern Breeds Unknown Thoroughbred Breeds after 1945 after 1960 Name of Horse RegNo TB AB MB UB HSH Status Maximum Max 6.25% Max.
    [Show full text]
  • December 2017
    DECEMBER 2017 Newsletter of the Australian National Placenames Survey an initiative of the Australian Academy of Humanities, supported by the Geographical Names Board of NSW In search of the Basaltic Rock In August 1840 the Police District of Macquarie was Of the placenames listed in the original description all formally gazetted. It was described as: but one have endured. The exception is the Basaltic Rock, first described in an article on the opening of the Embracing the whole of the county of Macquarie, above north-eastern districts published in 1842: Crescent Head; bounded on the north by a line bearing west to a range heading Maria’s and Wilson’s Rivers, and before we quit New England, we must notice the by this range and a line from thence bearing south-westerly remarkable object described on the maps as the Basaltic to Werrekembe, at the source of the Hasting’s River, and by Rock. This is an insulated, and perpendicular column of the range heading the Apsley River to the Basaltic Rock, basalt, composed of hexagonal prisms closely cemented, and thence by a range to the range heading the River Peel; it forms an interesting feature of research to the geologist, on the south by the range heading Hunter’s River to the and a picturesque and singular object of contemplation to source of the Barnard, and by this river and the Manning the amateur tourist.5 to Farquhar’s Inlet on the sea shore, which forms the eastern boundary of the district to the point northward of Crescent Head aforesaid.1 Despite the reference to the ‘county of Macquarie’ no such county had yet been proclaimed so the creation of the police district was, in fact, the first time that the boundaries of the Macquarie district had been officially published.
    [Show full text]
  • Gazetteer of Streams of Texas
    DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 448 GAZETTEER OF STREAMS OF TEXAS PREPARED UNDER THE DIRECTION OF GLENN A. GRAY WASHINGTON GOVERNMENT FEINTING OFFICE 1919 GAZETTEER OF STREAMS OF TEXAS. Prepared under the direction of GLENN A. GRAY. INTRODUCTION. The following pages contain a gazetteer of streams, lakes, and ponds as shown by the topographic maps of Texas which were pre­ pared by the United States Geological Survey and, in areas not covered by the topographic maps, by State of Texas county maps and the post-route map of Texas. For many streams a contour map of Texas, prepared in 1899 by Robert T. Hill, was consulted, as well as maps compiled by private surveys, engineering corporations, the State Board of Water Engineers, and the International Boundary Commission. An effort has been made to eliminate errors where practicable by personal reconnaissance. All the descriptions are based on the best available maps, and their accuracy therefore depends on that of the maps. Descriptions of streams in the central part of the State, adjacent to the Bio Grande above Brewster County, and in parts of Brewster, Terrell, Bowie, Casg, Btirleson, Brazos, Grimes, Washington, Harris, Bexar, Wichita, Wilbarger, Montague, Coke, and Graysoh counties were compiled by means of topographic maps and are of a good degree of accuracy. It should be understood, however, that all statements of elevation, length, and fall are roughly approximate. The Geological Survey topographic maps used are cited in the de­ scriptions of the streams and are listed below.
    [Show full text]
  • The Riverfront Plan Asheville, North Carolina
    The Riverfront Plan Asheville, North Carolina ^ ’■■i ^ S r " ^ ^W7st»-v5t : j r v : . roAjvncNu-J.'’ ®® Cover illustrations complivnents of Sandra Smathers-Jarman. Below, a view of Riverside Park and the French Broad River, ca. 1912.; photo courtesy of North Carolina Collection, Pack Memorial Public Library. Opposite, the same view in 1989; photo: J. Weiland. The Riverfront Plan Asheville, North Carolina April 26 - 29, 1989 A joint venture of: Urban Design Assistance Team, N.C. Chapter, The American Institute of Architects Community Assistance Team, N.C. Chapter, The American Society of Landscape Architects Sponsor: French Broad Riverfront Planning Cor Editor/Book Desigrt r.f * PREFACE For the greater part of the history of this Earth, atmospheric and AshevUle has reached a point In its history where the function and tectonic forces have forged the Blue Ridge Mountains and the character of the French Broad River must begin to respond to the Great Smokies. Over a much shorter period of time, plant and needs of its residents in a cultural and recreational way as well as animal ecosystems have flourished, creating the natural environ­ an economic way. It is a resource of such spectacular grandeur ment that surrounds Asheville today. Finally, at the end of a that the city can only benefit from its careful redevelopment. sequence of evolutionary events, man occupied the valleys and floodplains, seeking sustenance and shelter. The Riverfront Plan is a creation of many mmds, of citizens and professionals from the fields of architecture, landscape architec­ The French Broad River emerged from its source a long time ago in ture, and city and regional planning.
    [Show full text]
  • Shrimp Geochronology of the Southern New England Orogen
    University of Wollongong Research Online Faculty of Science, Medicine & Health - Honours Theses University of Wollongong Thesis Collections 2011 Shrimp Geochronology of the southern New England Orogen Thomas W. Line University of Wollongong Follow this and additional works at: https://ro.uow.edu.au/thsci University of Wollongong Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorise you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: This work is copyright. Apart from any use permitted under the Copyright Act 1968, no part of this work may be reproduced by any process, nor may any other exclusive right be exercised, without the permission of the author. Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. A court may impose penalties and award damages in relation to offences and infringements relating to copyright material. Higher penalties may apply, and higher damages may be awarded, for offences and infringements involving the conversion of material into digital or electronic form. Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong. Recommended Citation Line, Thomas W., Shrimp Geochronology of the southern New England Orogen, Bachelor of Science (Honours), School of Earth & Environmental Sciences, University of Wollongong, 2011.
    [Show full text]
  • Insights Into Platypus Population Structure and History from Whole-Genome Sequencing
    bioRxiv preprint doi: https://doi.org/10.1101/221481; this version posted December 18, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. Insights into platypus population structure and history from whole-genome sequencing 1,2 1 1 3 4 Hilary C. Martin †, Elizabeth M. Batty †, Julie Hussin †, Portia Westall , Tasman Daish ,Stephen Kolomyjec5, Paolo Piazza1,6, Rory Bowden1, Margaret Hawkins7, Tom Grant8, Craig Moritz9, Frank 4 3, 1,10, Grutzner , Jaime Gongora ⇤, Peter Donnelly ⇤. 1. Wellcome Centre for Human Genetics, University of Oxford, Oxford, OX1 7BN, UK. 2. Wellcome Trust Sanger Institute, Wellcome Genome Campus, Hinxton, UK 3. The University of Sydney, Sydney School of Veterinary Science, New South Wales 2006, Australia. 4. University of Adelaide, Adelaide, Australia. 5. School of Biological Sciences, Lake Superior State University, Sault Sainte Marie, MI 49783. 6. Faculty of Medicine, Department of Medicine, Imperial College, London, UK. 7. Taronga Zoo, Mosman, NSW 2088, Australia. 8. University of New South Wales, Sydney, NSW 2052, Australia. 9. Research School of Biology and Centre for Biodiversity Analysis, The Australian National University, Acton, Australian Capital Territory 2601, Australia. 10. Department of Statistics, University of Oxford, Oxford, OX1 3TG, UK. Contributed equally. To whom correspondence should be addressed: [email protected], [email protected] † ⇤ Abstract The platypus is an egg-laying mammal which, alongside the echidna, occupies a unique place in the mammalian phylogenetic tree.
    [Show full text]
  • Water Sharing Plan for the Lower North Coast Unregulated and Alluvial Water Sources
    Water Sharing Plan for the Lower North Coast Unregulated and Alluvial Water Sources Background document for amended plan 2016 Published by the NSW Department of Primary Industries, Water Water Sharing Plan for the Lower North Coast Unregulated and Alluvial Water Sources - Background document for amended plan 2016 First published in November 2016 Incorporates amendments to the plan following inclusion of the Karuah River Water Source More information This report may be cited as: Betterridge L., Rabbidge T., (2016) Water Sharing Plan for the Lower North Coast Unregulated and Alluvial Water Sources: Background document for amended plan 2016, NSW Department of Primary Industries, Sydney www.dpi.nsw.gov.au Acknowledgments Cover image: Little Manning River in Woko National Park, John Spencer/ OEH © State of New South Wales through the Department of Trade and Investment, Regional Infrastructure and Services, 2016. You may copy, distribute and otherwise freely deal with this publication for any purpose, provided that you attribute the NSW Department of Primary Industries as the owner. Disclaimer: The information contained in this publication is based on knowledge and understanding at the time of writing (November 2016). However, because of advances in knowledge, users are reminded of the need to ensure that information upon which they rely is up to date and to check currency of the information with the appropriate officer of the Department of Primary Industries or the user’s independent adviser. WSP for Lower North Coast unregulated and alluvial water sources: Background document 2016 Contents Introduction .......................................................................................................................... 1 An amended plan for the unregulated Lower North Coast catchments .......................... 2 Purpose of the Plan .............................................................................................................
    [Show full text]
  • NSW Freshwater Fishing Guide 2008
    XXXXXXXXX D DPI6646_NOV07 Contents D Ccontents About this guide 4 hand-hauled yabby net 20 Message from the minister 6 dams and weirs 22 NSW recreational fishing fee 8 Useful knots, rigs and bait 24 interstate and overseas visitors 8 How to weigh your fish with a ruler 27 how much is the fee? 8 Freshwater fishing enclosures 28 where do I pay the fee? 8 Why do we close areas to fishing? 32 Where do my fishing fees go? 9 Lake Hume and Lake Mulwala 32 recereational fishing trusts 9 Catch and release fishing 33 expenditure committee 10 Major native freshwater fishing species 34 fish stocking 12 Crayfish 37 more fisheries officers on patrol 12 Trout and salmon fishing 38 essential recreational research fishing rules for trout and salmon 38 and monitoring 12 notified trout waters 40 watch out for fishcare volunteers 12 classifications 46 more facilities for fishers 12 closed waters 46 fishing workshops 14 illegal fishing methods 47 tell us where you would like fees spent 14 trout and salmon fishing species 48 Freshwater legal lengths 15 Fish hatcheries and fish stocking 50 Bag and possession limits 15 native fish stocking programs 50 explanation of terms 15 trout and salmon 53 measuring a fish 15 fish stocking policy 54 measuring a Murray cray 15 hatchery tours 54 why have bag and size limits? 15 Threatened and protected species 55 bag and size limits for native species 16 Conserving aquatic habitat 58 General fishing 17 department initiatives 58 fishing access 17 what can fishers do? 59 recereational fishing guides 17 report illegal activities 61 traps and nets 17 Pest species 61 Murray river 17 Fishcare volunteer program 63 fishing lines 17 Take a kid fishing! 63 illegal fishing methods 17 Fisheries officers 64 yabby traps 18 Consuming your catch 65 shrimp traps 20 Inland offices and contact details 67 hoop net or lift net 20 2008 NSW Recreational Freshwater Fishing Guide 3 E About this guide This freshwater recreational fishing guide is produced by NSW Department Copyright of Primary Industries, PO Box 21 Cronulla NSW 2230.
    [Show full text]
  • Gondwana Rainforests of Australia
    151°E 152°E 153°E 154°E W eirR i r v e r e v i R r e m e r r e C B Ri v Mi ond ne ra llmerran a mi Ri ver r e m e o vi o Clifton R C Kalbar t r e S S bl ° ° A 8 Boonah 8 2 Allora r 2 e v Wond i ul er v Gold Coast R i Range n R a g g NP o n Main ra Lamington e L Range NP N Springbrook Warwick NP NP Tweed Heads Mount Barney NP Mount Bendidee Chinghee NP NP o R us er Riv Mooball Bogangar Mount r Killarney Wollumbin e vi Inglewood Clunie R NP Koreelah NP ic R Pottsville Beach NP NP hm eed ondR w i ve T Mount r Border Ranges Mebbin JerusalemB Tooloom NP NP r Brunswick Heads Maryland Toonumbar NP un Q U E E N S L A N D NP s wick River NP Captains NP Creek NR r Byron Bay uma e Nightcap D resq iv Kyogle R R Yabbra NP ive o r o n NP Stanthorpe oo Richmond B o Range o Cataract n o NP o NP e B Riv r ns o Boonoo ls Lismore Sundown i Texas NP Girraween Bald Boonoo W Casino NP Rock NP Ballina NP Basket Swamp Mallanganee NP NP S S ° ° 9 Mount 9 2 Timbarra Pikapene 2 Mole R Broadwater ive NP NP r NP Tenterfield Bungawalbin Kwiambal Evans Head NP NP Bundjalung Beard NP y Ashford River Capoompeta Washp r ool e Iluka NR NP v Fortis i NP R Deepwater ) Creek a Yamba r r NP r Maclean a e N E W S O U T H W A L E S v N E W S O U T H W A L E S b i R Se ern m v er i e Warialda R iv Butterleaf t ( G c y ibraltar n NP ck re R o Ra la nge C Kings NP Plains Barool Yuraygir NP NP Nymboida NP NP Ramornie Ma nn River NP Grafton Inverell Glen In nes O ra ra R i Bingara ver Hen r r B y R ive o R yd iver M ac North Solitary Islands G in v er w t yre Ri y Warra S di S °
    [Show full text]
  • Vegetation Formations, Classes and Communities
    Appendix 11: Vegetatiion formatiions, cllasses and communiities Vegetation Vegetation class Vegetation community PVP developer equivalent vegetation Landscape and diagnostic features formation* type Dry sclerophyll Clarence Dry Sclerophyll Forests Baryulgil Serpentinite Complex Eucalyptus ophitica - White Mahogany open forest on Low open or open forest. On serpentinite geology near serpentinite near Baryulgil of the North Coast Baryulgil. Dry sclerophyll Clarence Dry Sclerophyll Forests Coast Range Spotted Gum- Spotted Gum - Blackbutt open forest of the lower Tall to very tall dry open forest. Restricted and patchy Blackbutt Clarence Valley of the North Coast distribution along the Coast Range in the lower Clarence Valley, with a disjunct western occurrence in Grange State Forest. Dry sclerophyll Clarence Dry Sclerophyll Forests Dry Foothills Spotted Gum Spotted Gum dry grassy open forest of the foothills of Tall to very tall open forest. On slopes and ridges of dry the northern North Coast foothills areas of the coastal hinterland and gorges of the northern parts of the North Coast. Dry sclerophyll Clarence Dry Sclerophyll Forests Foothill Grey Gum-Ironbark- Grey Gum - Grey Ironbark open forest of the Clarence Tall to very tall dry forest with a mixed canopy. On Spotted Gum lowlands of the North Coast sandstone and siliceous soils in the Clarence lowlands with a western extension through the southern Richmond Range inland to Ewingar State Forest and the Mann River. Dry sclerophyll Clarence Dry Sclerophyll Forests Foothills Grey Gum-Spotted Gum Grey Gum - Spotted Gum open forest of the southern Tall to very tall open forest. On high and low quartz Clarence lowlands of the North Coast sediments in the southern portion of the Clarence- Moreton Basin mainly south of the Clarence River.
    [Show full text]