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The University of Sydney
THE UNIVERSITY OF SYDNEY Copyright and use of this thesis This thesis must be used in accordance with the provisions of the Copyright Act 1968. Reproduction of material protected by copyright may be an infringement of copyright and copyright owners may be entitled to take legal action against persons who infringe their copyright. Section 51 (2) of the Copyright Act permits an authorized officer of a university library or archives to provide a copy (by communication or otherwise) of an unpublished thesis kept in the library or archives, to a person who satisfies the authorized officer that he or she requires the reproduction for the purposes of research or study. The Copyright Act grants the creator of a work a number of moral rights, specifically the right of attribution, the right against false attribution and the right of integrity. You may infringe the author’s moral rights if you: - fail to acknowledge the author of this thesis if you quote sections from the work - attribute this thesis to another author -subject this thesis to derogatory treatment which may prejudice the author’s reputation For further information contact the University’s Copyright Service. sydney.edu.au/copyright A STRUCTURAL ANALYSIS OF THE SOUTHERN HORNSBY PLATEAU, SYDNEY BASIN, NEW SOUTH WALES by Anthony Richard Norman, B.Sc. (Hons) A thesis submitted in fulfilment of the requirements for the degree of Master of Science DEPARTMENT OF GEOLOGY AND GEOPHYSICS UNIVERSITY OF SYDNEY September, 1986 ABSTRACT The Hornsby Plateau rises north of Sydney. Aerial photo interpretation of an area north of Hornsby and south of the Hawkesbury River revealed two well defined extensive traces. -
5. Parramatta
5. PARRAMATTA 5.1 Introduction Parramatta Local Government Area occupies an area of 60 square kilometres, straddling the upper reaches of the Parramatta River, in eastern parts of the western Sydney region. There is a marked difference in landscape type between those areas to the north and south of the Parramatta River. To the south and west, undulating Wianamatta shales of the Fairfield Basin are broken by low-lying fingers of Quaternary alluvium along the major creek lines such as Prospect Creek, Duck River, the upper parts of Toongabbie Creek and their tributaries. A small sandstone outcrop along an upper section of Duck River has little impact on topography, but is reflected in the disjunct occurrence of sandstone species. To the north of the river the Hornsby Plateau-Cumberland Plain interface is marked by steep rises. Small remnants of Wianamatta shales occur on ridge-tops and deep valleys are incised into Hawkesbury sandstone along creeks draining from the plateau. Soil landscapes reflect this variation in geology across the LGA. To the south and west the dominant soil landscape on the shales is Blacktown, with Birrong on the alluvium in drainage lines along the creeks. In the north-east beyond the still undulating shale and Blacktown soil landscape close to the river, the edge of the Hornsby Plateau produces a complex mosaic of soil landscapes including the shale-based Glenorie on the ridges, sandstone-based Gymea and Hawkesbury on the slopes and in the valleys, and patches of Lucas Heights associated with outcropping Mittagong Formation lying between Wianamatta shale and Hawkesbury Sandstone. -
Bibliography of Environmental Theses for the Blue Mountains Region, New South Wales, Australia
Selected bibliography of environmental theses for the Blue Mountains region, New South Wales, Australia Prepared by Ian R. C. Baird Version 2, March 2019. With contributions from Margaret Baker, Nakia Belmer, Rosalie Chapple, Ben Croak, Kirstie Fryirs, Alex Gold, Sarsha Gorissen, Julia James, John Low, Brian Marshall, Scott Mooney, Peter Rickwood, Susan Rutherford, Judy Smith and Lyndal Sullivan. Includes some theses that deal with the Blue Mountains region in part only. Most recent Masters and PhD theses will be available online for download from relevant university library websites or the National Library of Australia’s Trove digital theses repository. Theses related to the Jenolan Caves area cited here may be held by the Jenolan Caves Reserve Trust archive. Additional uncited Honours and Grad. Dip. Env. Sc. theses with relevance to the Jenolan Caves area may also be held by the archive. Allan, T. L. (1986) Structure and stratigraphy of Palaeozoic rocks in the Jenolan Caves area NSW. B.Sc. (Honours) thesis, University of Sydney. Avaramides, P. (1997) Marble tombstones as environmental indicators. PhD thesis, University of Sydney. Baird, I. R. C. (2012) The wetland habitats, biogeography and population dynamics of Petalura gigantea (Odonata: Petaluridae) in the Blue Mountains of New South Wales. PhD thesis, Western Sydney University. Available from http://handle.uws.edu.au:8081/1959.7/509925 Baker, A. C. (2009) The dynamics of litterfall in eucalypt woodland surrounding pine plantations. PhD thesis, University of Technology, Sydney. Available from http://trove.nla.gov.au/work/36355084 Bartley, M. J. (1985) The contribution of fire to variation in plant species composition and cover in sclerophyll shrub woodland and low open-forest in the Blue Mountains, New South Wales. -
Australian Atomic Energy Commission Research Establishment Lucas Heights
AAEC/TM317 93 LU AUSTRALIAN ATOMIC ENERGY COMMISSION RESEARCH ESTABLISHMENT LUCAS HEIGHTS PRELIMINARY REGIONAL STUDY OF SURFACE RADIOACTIVITY IN THE BROKEN BAY-ILLAWARRA-KATOOMBA AREA by I.A.MUMME J.C.DUGGLEBY R.J.FINN D.E.PARSONS APRIL 1966 AUSTRALIAN ATOMIC ENERGY COMMISSION RESEARCH ESTABLISHMENT LUCAS HEIGHTS PRELIMINARY REGIONAL STUDY OP SURFACE RADIOACTIVITY IN THE BROKEN BAY-ILLAWARRA-KATOOMBA AREA by 1. A. MUMME J. C. DUGGLEBY R. J. FINN D. E. PARSONS ABSTRACT Natural background radiation has been measured along typical road traverses in the environs of Sydney and Lucas Heights. Soil samples were taken and radioactive elements identified by gamma spectrometry. The gamma—ray dose rates were in the range 20—40 mrad/year though higher and lower values were recorded. The normal gamma—ray intensities at the surface were generally related to the nature of the underlying weathered rock formation?. The characteristic dose rates are listed. CONTENTS Page No, 1. INTRODUCTION . ± 2. THE GEOLOGICAL DISTRIBUTION OF GAMMA-EMITTING NUCLIDES 1 2.1 Naturally Occurring Radioactive Elements 1 2.2 Potassium ]_ 2.3 Thorium and Uranium Series 2 3. GEOLOGY OF THE AREA 3 4. DESCRIPTION OF THE MONITORS 4 4.1 The Car-borne Monitor 4 4.2 The Gamma-spectrometer 5 5. THE SURVEY PROCEDURE 5 6. RESULTS OF THE SURVEY 7 6.1 Treatment of Results 7 6.2 Discussion of the Results 8 6.3 Validity of the Results 8 7. CONCLUSION 9 8. ACKNOWLEDGEMENTS 10 9. REFERENCES 10 Table 1. The abundances of thorium and uranium in igneous rocks. Table 2. -
Guide to Authors
GEOSCIENCE AUSTRALIA Potential geologic sources of seismic hazard in the Sydney Basin Proceedings volume of a one day workshop Edited by Dan Clark Record 2009/11 GeoCat # 65991 APPLYING GEOSCIENCE TO AUSTRALIA’S MOST IMPORTANT CHALLENGES Potential geologic sources of seismic hazard in the Sydney Basin geology geomorphology seismicity hazard studies future directions Proceedings volume of a one day workshop: Wednesday 13th April 2005 GEOSCIENCE AUSTRALIA RECORD 2009/11 1 Workshop coordinator: Dan Clark 1. Natural Hazard Impacts Project, Geospatial and Earth Monitoring Division, Geoscience Australia. Email: [email protected]. Seismic Hazard in Sydney Proceedings of the one day workshop Department of Resources, Energy and Tourism Minister for Resources and Energy: The Hon. Martin Ferguson, AM MP Secretary: Mr John Pierce Geoscience Australia Chief Executive Officer: Dr Neil Williams PSM © Commonwealth of Australia, Geoscience Australia, 2009 This material is copyright Commonwealth of Australia. Other than the Coat of Arms and departmental logo, you may reproduce, distribute, adapt and otherwise freely deal with this material for all purposes without charge on the condition that you include the acknowledgement "© Commonwealth of Australia 2008, Potential geologic sources of seismic hazard in the Sydney Basin" on all uses. You may not sub-licence this material or use it in a misleading context. While every effort has been made to ensure accuracy, the Commonwealth does not accept any responsibility for the accuracy, completeness or currency of this material, and will not be liable for any loss or damage arising from use of, or reliance on, the material. Nothing in this licence affects the operation of any applicable exception or limitation contained in the Copyright Act 1968. -
The Sydney Basin Bioregion
185 CHAPTER 15 The Sydney Basin Bioregion 1. Location 2. Climate The Sydney Basin Bioregion lies on the central east coast of NSW and covers The Sydney Basin Bioregion is dominated by a temperate climate an area of approximately 3,624,008 ha (IBRA 5.1). It occupies about 4.53% of characterised by warm summers with no dry season. A sub-humid climate NSW and is one of two bioregions contained wholly within the state. The occurs across significant areas in the northeast of the bioregion. A small area bioregion extends from just north of Batemans Bay to Nelson Bay on the in the west of the bioregion around the Blue Mountains falls in a montane central coast, and almost as far west as Mudgee.The bioregion is bordered to climate zone. Snow can occasionally occur in this area of higher elevation. the north by the North Coast and Brigalow Belt South bioregions, to the Rainfall can occur throughout the year, but varies across the bioregion in south by the South East Corner Bioregion and to the west by the South relation to altitude and distance from the coast, with wetter areas being Eastern Highlands and South Western Slopes bioregions. closer to the coast or in higher altitudes. As well as Sydney itself, the Sydney Basin Bioregion encompasses the towns Temperature varies across the bioregion, with areas of higher temperature of Wollongong, Nowra, Newcastle, Cessnock, Muswellbrook and Blue occurring along the coast and in the Hunter valley and areas of lower Mountains towns such as Katoomba and Mt Victoria. -
Biodiversity Investment Opportunities Map Mapping Priority Investment Areas for the Cumberland Subregion
Biodiversity Investment Opportunities Map Mapping Priority Investment Areas for the Cumberland Subregion © Copyright State of NSW and Office of Environment and Heritage Cover photo: BIO Map Priority Investment Areas comprising Nurragingy Reserve (Core Area) and associated Regional Biodiversity Corridor in the Blacktown LGA. Photo credit: Western Sydney Parklands Trust. With the exception of photographs, the State of NSW and Office of Environment and Heritage are pleased to allow this material to be reproduced in whole or in part for educational and non-commercial use, provided the meaning is unchanged and its source, publisher and authorship are acknowledged. Specific permission is required for the reproduction of photographs. The Office of Environment and Heritage (OEH) has compiled this document in good faith, exercising all due care and attention. No representation is made about the accuracy, completeness or suitability of the information in this publication for any particular purpose. OEH shall not be liable for any damage which may occur to any person or organisation taking action or not on the basis of this publication. Readers should seek appropriate advice when applying the information to their specific needs. Published by: Office of Environment and Heritage NSW 59 Goulburn Street, Sydney NSW 2000 PO Box A290, Sydney South NSW 1232 Phone: (02) 9995 5000 (switchboard) Phone: 131 555 (environment information and publications requests) Phone: 1300 361 967 (national parks, climate change and energy efficiency information, and publications requests) Fax: (02) 9995 5999 TTY: (02) 9211 4723 Email: [email protected] Website: www.environment.nsw.gov.au Report pollution and environmental incidents Environment Line: 131 555 (NSW only) or [email protected] See also www.environment.nsw.gov.au ISBN 978-1-74359-952-5 OEH 2015/0198 May 2015 Contents Summary v 1. -
Australian Museum Magazine
DF.CEM BER 15. 1960 C@B AUSTRALIAN MUSEUM MAGAZINE ' VoL. XllL No. 8 Price- TWO SH ILLlNGS . I A Wandering A lba tross off T hirro ul, New South W~• l e s . Wandering Albatrosses banded near Thirroul have been recaptured as far a ~va y ~.~ . t h e ~o ut h ern ~ Indi a~. Ocean a nd the southern tip of South A m erica. (Sec a rtaclc. I he Utrds of Sydney , on pa~e 24 t.) * THE AUSTRALIAN MUSEUM HYD E PARK, SYDNEY BOARD OF TR USTE E S t> IU~ SID ENT: F. B. SP E CER GROWN TRUSTEE: F . B. SP c CER OFFJGIA L Tt~ USTEES: TH E HO ·. T H E C HIEF JUSTICE. THE HO . THE PRESIDEN r O F T H E LEGISLATI VE CO U C IL. 'I H E HO . T H E CH IEF SECR ETA RY . TH E HON. THE ATf O R EY-GEt--E RAL. T H E H ON. TH E TR EASUR ER. T HE J-101\:. T H E M l IS f E R FOR PUBLIC WORKS. TH I::. HO N. T H E M INIST ER FOR EDUCATION. TH E AUDITOR-GE ERA L. TH E PRESIDE T OF T H E NEW SOUTH WALES ME DICAL BOA RD. THE SURVEYOR-G EI':ERA L A N D C H IE F S U RV EYO R. T H E CROWN SOLIC ITO R . ELECTIVE TRUSTEES: 0 . G. VtCKERY. B.E., M.I. E. (Aust.). F I ~ A K W . -
The Native Vegetation of the Cumberland Plain, Western Sydney: Systematic Classification and Field Identification of Communities
Tozer, Native vegetation of the Cumberland Plain 1 The native vegetation of the Cumberland Plain, western Sydney: systematic classification and field identification of communities Mark Tozer NSW National Parks and Wildlife Service, PO Box 1967 Hurstville 2220, AUSTRALIA phone: (02) 9585 6496, fax.: (02) 9585 6606, e-mail: [email protected] Abstract: Twenty-two vascular plant communities occurring on, and adjacent to the Cumberland Plain and Hornsby Plateau, are defined using a multi-variate analysis of quantitative field survey data. Communities are described using structural features, habitat characteristics and diagnostic species. Diagnostic species are identified using a statistical fidelity measure. The pre–European spatial distribution of communities is estimated using a decision tree approach to derive relationships between community distribution and geological, climatic and topographical variables. Contemporary vegetation cover is estimated from 1:16 000 scale aerial photography (1997/98) and sorted into six categories based on cover of Eucalyptus species. These categories are only approximately related to vegetation condition: high Eucalyptus cover classes are most likely to contain high levels of floristic diversity, but areas with scattered cover or no cover at all may have either high or low diversity. Map accuracy is assessed using independent field samples and is primarily limited by the accuracy of 1:100 000 geological maps. Patterns in overstorey composition were mapped at 1:16 000 scale but were less useful in delineating community boundaries than was hoped because few species are confined to a single community. The extent to which observer bias may influence estimates of the present extent of remnant vegetation is investigated by comparing the interpretations of two observers for a subset of the study area. -
The Native Vegetation of the Cumberland Plain, Western Sydney: Systematic Classification and Field Identification of Communities
Tozer, Native vegetation of the Cumberland Plain 1 The native vegetation of the Cumberland Plain, western Sydney: systematic classification and field identification of communities Mark Tozer NSW National Parks and Wildlife Service, PO Box 1967 Hurstville 2220, AUSTRALIA phone: (02) 9585 6496, fax.: (02) 9585 6606, e-mail: [email protected] Abstract: Twenty-two vascular plant communities occurring on, and adjacent to the Cumberland Plain and Hornsby Plateau, are defined using a multi-variate analysis of quantitative field survey data. Communities are described using structural features, habitat characteristics and diagnostic species. Diagnostic species are identified using a statistical fidelity measure. The pre–European spatial distribution of communities is estimated using a decision tree approach to derive relationships between community distribution and geological, climatic and topographical variables. Contemporary vegetation cover is estimated from 1:16 000 scale aerial photography (1997/98) and sorted into six categories based on cover of Eucalyptus species. These categories are only approximately related to vegetation condition: high Eucalyptus cover classes are most likely to contain high levels of floristic diversity, but areas with scattered cover or no cover at all may have either high or low diversity. Map accuracy is assessed using independent field samples and is primarily limited by the accuracy of 1:100 000 geological maps. Patterns in overstorey composition were mapped at 1:16 000 scale but were less useful in delineating community boundaries than was hoped because few species are confined to a single community. The extent to which observer bias may influence estimates of the present extent of remnant vegetation is investigated by comparing the interpretations of two observers for a subset of the study area. -
Ecology of Sydney Plant Species the Sydney Region Is Defined As the Central Coast and Central Tablelands Botanical Subdivisions
1016 Cunninghamia Vol. 6(4): 2000 M a c q u Rylstone a r i e Coricudgy R i v e r e g n CC a Orange R Wyong g n i Gosford Bathurst d i Lithgow v Mt Tomah i Blayney D R. y r Windsor C t u a o b Oberon s e x r e s G k Penrith w a R Parramatta CT H i ve – Sydney r n a Abe e Liverpool rcro p m e b Botany Bay ie N R Camden iv Picton er er iv R y l l i Wollongong d n o l l o W N Berry NSW Nowra 050 Sydney kilometres Map of the Sydney region For the Ecology of Sydney Plant Species the Sydney region is defined as the Central Coast and Central Tablelands botanical subdivisions. Benson & McDougall, Ecology of Sydney plant species 7b 1017 Ecology of Sydney plant species Part 7b Dicotyledon families Proteaceae to Rubiaceae Doug Benson and Lyn McDougall Abstract Benson, Doug and McDougall, Lyn (National Herbarium of New South Wales, Royal Botanic Gardens, Sydney, Australia 2000. Email: [email protected]) 2000 Ecology of Sydney plant species: Part 7b Dicotyledon families Proteaceae to Rubiaceae. Cunninghamia 6(4) 1016–1202. Ecological data in tabular form are provided on 246 plant species of the families Proteaceae to Rubiaceae, 216 native and 30 exotics, occurring in the Sydney region, defined by the Central Coast and Central Tablelands botanical subdivisions of New South Wales (approximately bounded by Lake Macquarie, Orange, Crookwell and Nowra). -
Prehistoric Settlement in the Western Cumberland Plain
PREHISTORIC SETTLEMENT IN THE WESTERN CUMBERLAND PLAIN: RESOURCES. ENVIRONMENT AND TECHNOLOGY. by James Leslie Kohen Dip Tech (Sc), B App Sc (NSWIT), A.A.I.S.T. Submitted for the degree of Doctor of Philosophy Macquarie University Sydney 1986 FRONTPIECE. The western Cumberland Plain, viewed across the Nepean River fro* the Lapstone Monocline. ABSTRACT The study of prehistory is subject to the same bias and prejudice as any other scientific discipline. When the rewards are likely to be few and the effort required great, researchers will avoid problem areas in favour of more lucrative fields. One such neglected area of research has been the archaeology of the coastal plains and forests of southeastern Australia, where poor visibility and the diffuse nature of the archaeological record militate against the investment of valuable research time. In the Sydney region, the archaeological data accumulated relate almost exclusively to rock shelter deposits. While such sites do have the potential to provide a great deal of valuable information, they reflect only a fraction of the activities carried out by the prehistoric population. In order to counteract the bias evident in the archaeological investigations, I undertook a systematic archaeological survey of the western Cumberland Plain. In the early chapters of this thesis, I examine the^ environmental setting and the resources which were available to Aboriginal people at the time of European settlement in 1788. After evaluating the ethnographic accounts, a clear picture emerges of two major economic systems operating; one based on coastal resources and one reliant on a wider range of locally abundant foods. Associated with this dichotomy were linguistic, technological and social differences suggestive of dense Aboriginal populations exploiting relatively narrow territories.