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Secluded Luxury Killcare Beach House
132 Northern Advocate Tuesday, January 30, 2018 Travel JUSTINE TYERMAN finds a jewel on the New South Wales Central Coast. FACTBOX LOVE watching the sunrise at the beach, the ■ Justine Tyerman was a light creeping along the guest of Luxe Houses: Isand transforming it from www.luxehouses.com, at beige to gold. The early NSW Central Coast morning sun has a luminous property Killcare Beach effect on the sea and the surf SECLUDED House: sparkles with www.luxehouses.com.au/ phosphorescence. The holiday-house/killcare- smudged mauve horizon is beach-house/ edged in gilt as the fiery orb ■ Getting there: Air New leaps from night hiding. Sun Luxury Zealand flies direct to beams flood the house with Sydney from Auckland, dazzling light as I sit in the Wellington, Christchurch window seat watching the and Queenstown. early-bird surfers and www.airnewzealand.co.nz swimmers. ■ JUCY Rentals assisted Our family of four drove up with transport: from Sydney for a long www.jucy.co.nz weekend of R&R at Killcare ■ All reservations with Beach after a hectic week in Luxe Houses include the big city. We stayed at access to concierge Killcare Beach House, a services who can arrange beautiful, secluded vacation (at additional cost) private home overlooking the sea, charter jets, helicopter highly recommended by Luxe transfers, yachts, Houses. Much thought has launches, jet-boats, gone into the interior design private chefs, waiter staff and furnishing of this tranquil for guest occasions, retreat. The floor tiles are the butlers, drivers, bespoke colour of sand and the fabrics spa treatments, and textures echo the experienced nannies, landscape. -
Equisetalean Plant Remains from the Early to Middle Triassic of New South Wales, Australia
Records of the Australian Museum (2001) Vol. 53: 9–20. ISSN 0067-1975 Equisetalean Plant Remains from the Early to Middle Triassic of New South Wales, Australia W.B. KEITH HOLMES “Noonee Nyrang”, Gulgong Road, Wellington NSW 2820, Australia Honorary Research Fellow, Geology Department, University of New England, Armidale NSW 2351, Australia [email protected] Present address: National Botanical Institute, Private Bag X101, Pretoria, 0001, South Africa ABSTRACT. Equisetalean fossil plant remains of Early to Middle Triassic age from New South Wales are described. Robust and persistent nodal diaphragms composed of three zones; a broad central pith disc, a vascular cylinder and a cortical region surrounded by a sheath of conjoined leaf bases, are placed in Nododendron benolongensis n.sp. The new genus Townroviamites is erected for stems previously assigned to Phyllotheca brookvalensis which bear whorls of leaves forming a narrow basal sheath and the number of leaves matches the number of vascular bundles. Finely striated stems bearing leaf whorls consisting of several foliar lobes each formed from four to seven linear conjoined leaves are described as Paraschizoneura jonesii n.sp. Doubts are raised about the presence of the common Permian Gondwanan sphenophyte species Phyllotheca australis and the Northern Hemisphere genus Neocalamites in Middle Triassic floras of Gondwana. HOLMES, W.B. KEITH, 2001. Equisetalean plant remains from the Early to Middle Triassic of New South Wales, Australia. Records of the Australian Museum 53(1): 9–20. The plant Phylum Sphenophyta, which includes the Permian Period, the increasing aridity and decline in the equisetaleans, commonly known as “horse-tails” or vegetation of northern Pangaea was in contrast to that in “scouring rushes”, first appeared during the Devonian southern Pangaea—Gondwana—where flourishing swamp Period (Taylor & Taylor, 1993). -
Tasman Peninsula
7 A OJ? TASMAN PENINSULA M.R. Banks, E.A. Calholln, RJ. Ford and E. Williams University of Tasmania (MRB and the laie R.J. Ford). b!ewcastle fo rmerly University of Tasmama (EAC) and (ie,a/Ogle,Cl; Survey of Tasmania (E'W) (wjth two text-figures lUld one plate) On Tasman Peninsula, southeastern Tasmania, almost hOrizontal Permian marine and Triassic non-marine lOcks were inllUded by Jurassic dolerite, faulted and overiain by basalt Marine processes operating on the Jurassic and older rocks have prcl(iU!ced with many erosional features widely noted for their grandeur a self-renewing economic asset. Key Words: Tasman Peninsula, Tasmania, Permian, dolerite, erosional coastline, submarine topography. From SMITH, S.J. (Ed.), 1989: IS lllSTORY ENOUGH ? PA ST, PRESENT AND FUTURE USE OF THE RESOURCES OF TA SMAN PENINSULA Royal Society of Tasmania, Hobart: 7-23. INTRODUCTION Coal was discovered ncar Plunkett Point by surveyors Woodward and Hughes in 1833 (GO 33/ Tasman Peninsula is known for its spectacular coastal 16/264·5; TSA) and the seam visited by Captain scenery - cliffs and the great dolerite columns O'Hara Booth on May 23, 1833 (Heard 1981, p.158). which form cliffs in places, These columns were Dr John Lhotsky reported to Sir John Franklin on the first geological features noted on the peninsula. this coal and the coal mining methods in 1837 (CSO Matthew Flinders, who saw the columns in 1798, 5/72/1584; TSA). His thorough report was supported reported (1801, pp.2--3) that the columns at Cape by a coloured map (CSO 5/11/147; TSA) showing Pillar, Tasman Island and Cape "Basaltcs" (Raoul) some outcrops of different rock This map, were "not strictlybasaltes", that they were although not the Australian not the same in form as those Causeway Dictionary of (Vol. -
Final Research Report for the Australian Flora Foundation Research Grant 1993
FINAL RESEARCH REPORT FOR THE AUSTRALIAN FLORA FOUNDATION RESEARCH GRANT 1993 Development, Germination and Dormancy of Actinotus helianthi (Flannel Flower) Seeds Lynette A Lee, Dr Peter B Goodwin Department of Crop Sciences, University of Sydney NSW 2006 Introduction Actinotus helianthi, the Sydney or Common Flannel Flower, has considerable horticultural potential as a cut flower, and as a rockery or container plant. It belongs to the family Apiaceae (syn. Umbelliferae), which includes many well known culinary herbs and vegetables, such as carrot, celery, parsley and dill. Flannel flowers are one of. the more common and attractive wildflowers found growing naturally in sandstone country along the east coast of NSW and southern Queensland. However, their use in cultivation is presently restricted because of erratic germination from seed. The aim of the current project was to investigate the development, germination and dormancy of flannel flower seeds in order to obtain a greater understanding of their germination requirements, and to thereby find a means of achieving better germination from seed. This will in turn help to reduce pressure, on wild populations, by increasing the production of plants in cultivation. Specifically, the objectives of this project were: i) to investigate whether the poor seed germination is due to low seed viability or seed dormancy; ii) to examine ways of improving germination; iii) and to study the seed anatomy. Materials and Methods: During late 1992 and early 1993, seed was collected from eight locations around NSW, in areas extending from the Royal National Park south of Sydney to South West Rocks on the North Coast (see Appendix 1). -
Background Paper on New South Wales Geology with a Focus on Basins Containing Coal Seam Gas Resources
Background Paper on New South Wales Geology With a Focus on Basins Containing Coal Seam Gas Resources for Office of the NSW Chief Scientist and Engineer by Colin R. Ward and Bryce F.J. Kelly School of Biological, Earth and Environmental Sciences University of New South Wales Date of Issue: 28 August 2013 Our Reference: J083550 CONTENTS Page 1. AIMS OF THE BACKGROUND PAPER .............................................................. 1 1.1. SIGNIFICANCE OF AUSTRALIAN CSG RESOURCES AND PRODUCTION ................... 1 1.2. DISCLOSURE .................................................................................................... 2 2. GEOLOGY AND EVALUATION OF COAL AND COAL SEAM GAS RESOURCES ............................................................................................................. 3 2.1. NATURE AND ORIGIN OF COAL ........................................................................... 3 2.2. CHEMICAL AND PHYSICAL PROPERTIES OF COAL ................................................ 4 2.3. PETROGRAPHIC PROPERTIES OF COAL ............................................................... 4 2.4. GEOLOGICAL FEATURES OF COAL SEAMS .......................................................... 6 2.5. NATURE AND ORIGIN OF GAS IN COAL SEAMS .................................................... 8 2.6. GAS CONTENT DETERMINATION ........................................................................10 2.7. SORPTION ISOTHERMS AND GAS HOLDING CAPACITY .........................................11 2.8. METHANE SATURATION ....................................................................................12 -
03 Agency Responses
03 Agency Responses CONTENTS Submission Summary & Responses Civil Aviation Safety Authority Darkinjung Local Aboriginal Land Council Department of Industry (Crown Lands) Department of Industry (Water) Department of Planning & Environment Department of Primary Industries (Agriculture) Department of Primary Industries (Fisheries) Forestry Corporation of NSW National Parks and Wildlife Services Office of Environment and Heritage Office of Environment and Heritage (Heritage Branch) Resources and Geoscience Roads and Martime Services Rural Fire Service Subsidence Advisory NSW Transport for NSW Agency Consultation Submission Summary & Responses Agency Issue Response Commonwealth No response received N/A Department of Environment Central Coast Councils area of Noted responsibility does not incorporate any Civil Aviation certified or registered aerodromes and Safety Authority therefore CASA has not comment on CCLEP. The CCLEP does not acknowledge the The Draft CCLEP based on the Standard Aboriginal Cultural Landscape & fails to Instrument LEP and as a consolidation of address the requirements of the the current WLEP 2013 and GLEP 2014. proposed future State legislation Any amendments a result of the final (Aboriginal Culture and Heritage Aboriginal Cultural Heritage Bill will be Reforms). made to the Standard Instrument LEP or further considered by the Comprehensive LEP. Culturally sensitive areas are incorrectly The timing and scope of works for the mapped in the Somersby Industrial Consolidated LEP does not allow for an Estate. archaeological study /ground truthing to be undertaken. Until this is resolved, any DA in the locality should be inclusive of a search of OEH is currently undertaking work with the Aboriginal Heritage Investigation Darkinjung to identify culturally Management System (AHIMS). Further significant sites. -
Moullean Conservation Management Strategy 2017-2037
The Moullean Conservation Management Strategy 2017 - 2037 October 2017 WWF-Australia PO Box 4010, Wembley, WA 6913 The project to develop this Conservation Management Strategy is supported by funding from the Western Australian Government’s State NRM Program, supported by Royalties for Regions. Prepared by Nathan McQuoid, Landscape Ecologist Editorial adviser Chris Greenwood, Words in Time. This Conservation Strategy was prepared with the assistance of the planning team: Merril Halley, Southwest Species Conservation Manager, WWF-Australia; Rebecca Boyland, Species Conservation Project Ofcer, WWF-Australia; Natasha Moore, Conservation Ofcer - Central Wheatbelt District, Parks and Wildlife Service, Department of Biodiversity, Conservation and Attractions (DBCA); Brett Beecham, Conservation Ofcer - Wheatbelt Region, Parks and Wildlife Service, DBCA; and David Jollife, District Nature Conservation Ofcer - Central Wheatbelt District, Parks and Wildlife Service, DBCA. The following people were consulted and contributed to the Strategy development process, and their assistance and input is acknowledged, in particular: • Rhonda Murphy, Aboriginal Heritage Unit of the Department of Biodiversity, Conservation and Attractions. • Rowan Hegglun, Wheatbelt NRM. • Reg Hayden, Njakinjaki Elder, Merredin. • Mick Hayden, Njakinjaki traditional owner and tour operator, Merredin. • Robyn McCarthy, Merredin Tourism Centre Manager. • Dr Jack Kinnear, Conservation Biologist, Perth. • Professor Steve Hopper, UWA Albany. • Dr David Pearson, Senior Research Scientist, Parks and Wildlife Service, DBCA. • Vaughan Smith, District Manager - Central Wheatbelt District, Parks and Wildlife Service, DBCA. • Jazmin Lindley, Nature Conservation Ofcer - Central Wheatbelt District, Parks and Wildlife Service, DBCA. • Phil Lewis, Ornithologist, Korrelocking. • David Collins, Greening Australia, Northam. • Landowners: Maxine Kerenyi, Malcolm French, John Hammond, Dr Tracey Moore, Laurie Shaw, Murray McDonald, and Barry and Maxine Cornish. -
The Influence of Natural Geological Formations and Patterns on Contemporary Landscape Design
Scientific Journal of Latvia University of Life Sciences and Technologies Landscape Architecture and Art, Volume 17, Number 17 DOI: 10.22616/j.landarchart.2020.17.05 Inspirative Geology - the Influence of Natural Geological Formations and Patterns on Contemporary Landscape Design Nawarah Al Basha, Anna Eplényi PhD, Gábor Sándor Szent István University, Faculty of Landscape Architecture and Urban Design, Hungary Abstract. Throughout the history of landscape design, we have witnessed many examples where natural features were used as symbolic elements of manmade landscapes and gardens. This influence of landscape geology had its impact on contemporary landscape architecture, resulting in diverse and innovative applications, which are the main topic of our discussion. The article is intended to demonstrate the trend of drawing inspiration from natural landscape features in contemporary landscape architecture in a new and complex way, focusing particularly on the influence of geology, geomorphology and tectonics. A study was conducted on twelve available, published contemporary landscape projects from the last two decades analysing the imitation of nature in the designs, with photo documentation and description. The aim is to identify how ‘native geology’ can influence today’s landscape architecture, which formations are inspirative, where and how they are integrated to the contemporary artistic design. Furthermore, in order to develop a complex understanding on how these references applied to the sites enhance the experience of the space. The selected projects are compared according to pairs of contrasting qualities that are related to measurable characteristics of a space. This will finally lead to identifying some common trends of today’s landscape architecture in applying this geology-inspired design approach. -
Body Fossils and Root-Penetration Structures
CHAPTER 16 BODY FOSSILS AND ROOT-PENETRATION STRUCTURES 482 BODY FOSSILS AND ROOT-PENETRATION STRUCTURES RECORDED FROM THE STUDY AREA 16.1. INTRODUCTION There are three major groups of body fossils that occur in the Triassic rocks of the study area, including the Hawkesbury Sandstone. The first group comprises fossil plant remains, which are abundant and previously well studied (e.g. Helby, 1969a,b & 1973; Retallack, 1976, 1977a, b, c, & 1980), and root-penetration structures. The second group comprises fossil animal remains which are extremely rare and, except for locally abundant fossil freshwater fish in shale lenses in the Hawkesbury Sandstone and the Gosford (=Terrigal) Formation (see Reggatt, in Packham 1969, P.407; and Branagan, in Packham 1969, p.415-416), include the bones of amphibians (e.g. Warren, 1972 & 1983; and Beale, 1985) and bivalve mollusc shells of mytilid affinity (Grant-Mackie et al., 1985). Additionally, the freshwater fossil pelecypod, Unio, the branchiopod Estheria, and a variety of insects have been recorded from the Hawkesbury Sandstone (cf. Branagan, in Packham 1969, p.417). The third group comprises microfossils (microfauna and microflora) (e.g. Helby, in Packham, 1969 p.404-405 and 417; Retallack, 1980; Grant-Mackie et al., 1985). The abundance of spores, megaspores, intact spore tetrads, and abundant quantities of other microscopic organic materials including acritarchs (possibility having been reworked) have been suggested as evi dence that the palaeoenvironment of the Newport Formation was as marginal marine, possibly of lagoonal or estuarine character (Grant-Mackie et al., 1985). 483 16.2. TAXONOMY OF THE PLANT REMAINS AND ROOT-PENETRATION STRUCTURES 16.2.1. -
The Vertebrate Fauna of Werakata National Park and Werakata State Conservation Area
The Vertebrate fauna of Werakata National Park and Werakata State Conservation Area THE VERTEBRATE FAUNA OF WERAKATA NATIONAL PARK AND WERAKATA STATE CONSERVATION AREA Information and Assessment Section Metropolitan Branch Environment Protection and Regulation Group Department of Environment and Climate Change (NSW) November 2008 For enquiries regarding this report please Published by: contact Martin Schulz or Daniel Connolly of the Department of Environment and Climate Information and Assessment Section, Change Metropolitan Branch, Climate Change and 43 Bridge St, Hurstville NSW 2220 Environment Protection Group, Department of PO Box 1967, Hurstville NSW 1482 Environment and Climate Change, Hurstville. Phone (02) 995 5000 (switchboard) www.environment.nsw.gov.au This report should be referenced as follows: The Department of Environment and Climate DECC (2008) The Vertebrate Fauna of Change is pleased to allow this material to be Werakata National Park and State Conservation reproduced in whole or in part, provided the Area. Department of Environment and Climate Change NSW, Hurstville. meaning is unchanged and its source, publisher and authorship are acknowledged. Map data is supplied by the Department of ISBN 978 1 74122 880 9 Environment and Climate Change. Maps are copyright Department of Environment and DECC 2008/350 Climate Change NSW. They are not guaranteed November 2008 to be free from error or omission. The Department of Environment and Climate Change and its employees disclaim liability for any act done on the information in -
Formation of Tasmania Times & Processes Parks and Wildlife Service Tasmania
GEODIVERSITY Formation of Tasmania times & processes Parks and Wildlife Service Tasmania Produced in consultation with Nature Conservation Branch, DPIWE DEPARTMENT of TOURISM, PARKS HERITAGE and the ARTS Tasmania’s geodiverstiy has contributed directly to the The Precambrian is a mysterious part of the Earth’s islands biodiversity, that is the numerous and varied geological history as far as animal life was concerned. plant and animal species. The States geodiversity is a Very few fossils have been found, due to the lack of result of continental drift, ice ages, humid hot animals with hard body parts which had not evolved conditions and earthquakes occurring over many yet. The softer organisms were less able to be millions of years. preserved as fossils because the softer parts decomposed. A very brief and summarised account of Tasmania’s geological history is outlined below. Keep in mind that although Tasmania is referred to frequently throughout Cambrian these notes, it was not until about 70 million years ago 600 - 500 million years ago that Tasmania began to look like it does today, an island to the south of the Australian mainland. Volcanoes and the explosion of life on earth The Cambrian period is renowned around the world for Precambrian the explosion of life in the seas. It has been argued that at this time there was greater diversity of life in the seas 1,000 to around 600 million years ago. than currently exists on earth. However this (life) Life was restricted to the oceans & land was an explosion was followed by major extinctions. extensive desert. -
Terra Australis 27 © 2008 ANU E Press
terra australis 27 © 2008 ANU E Press Published by ANU E Press The Australian National University Canberra ACT 0200 Australia Email: [email protected] Web: http://epress.anu.edu.au National Library of Australia Cataloguing-in-Publication entry Author: McDonald, Josephine. Title: Dreamtime superhighway : an analysis of Sydney Basin rock art and prehistoric information exchange / Jo McDonald. ISBN: 9781921536168 (pbk.) 9781921536175 (pdf) Series: Terra Australis ; 27 Notes: Bibliography. Subjects: Rock paintings--New South Wales--Sydney Basin. Petroglyphs--New South Wales--Sydney Basin. Visual communication in art--New South Wales--Sydney Basin. Art, Aboriginal Australian--New South Wales--Sydney Basin. Aboriginal Australians--New South Wales--Sydney Basin--Antiquities. Dewey Number: 709.011309944 Copyright of the text remains with the contributors/authors, 2006. This book is copyright in all countries subscribing to the Berne convention. Apart from any fair dealing for the purpose of private study, research, criticism or review, as permitted under the Copyright Act, no part may be reproduced by any process without written permission. Inquiries should be made to the publisher. Series Editor: Sue O’Connor Typesetting and design: Silvano Jung Cover photograph by Jo McDonalnd Back cover map: Hollandia Nova. Thevenot 1663 by courtesy of the National Library of Australia. Reprinted with permission of the National Library of Australia. Terra Australis Editorial Board: Sue O’Connor, Jack Golson, Simon Haberle, Sally Brockwell, Geoffrey Clark Terra Australis reports the results of archaeological and related research within the south and east of Asia, though mainly Australia, New Guinea and island Melanesia — lands that remained terra australis incognita to generations of prehistorians.