When Travelling in Central Queensland Take the Time to Discover the Gorges Way
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FAULTS and FRACTURES in the SURAT BASIN Relationships With
FAULTS AND FRACTURES IN THE SURAT BASIN Relationships with Permeability Final Report Celoxis System ID: 149310 Report release date: 22 September 2017 Short Range Permeability Variations Seismic Analysis and Geological Framework 1 Research Team J. Copley, S. Mukherjee, A. Babaahmadi, F. Zhou, K. Barbosa, S. Hurter, S. Tyson School of Earth and Environmental Sciences Acknowledgements The authors would like to thank the CCSG and member companies (Shell/QGC, Santos, Arrow, Origin) for funding the project. The Queensland Geological Survey and Department of Natural Resources and Mines, Integrated Geoscience as well as the participating companies provided data and discussion about the content of this report. The project was conceived and initiated by J. Esterle and R. Sliwa of Integrated Geoscience. Special thanks to Owen Dixon (GSQ) and Andrew Aouad (Origin) for their contributions. Disclosure This research was undertaken during Term 1 of the UQ Centre for Coal Seam Gas. Term 1 funding was provided by The University of Queensland 22% ($5 million) and the industry members 78% (17.5 million) over 5 years. An additional $3.0 million was provided by industry members for research infrastructure costs. The industry members are Shell (QGC), Santos, Arrow Energy and APLNG. The Centre conducts research across Water, Geoscience, Petroleum Engineering and Social Performance themes. For more information about the Centre’s activities and governance see https://ccsg.centre.uq.edu.au/ Disclaimer The information, opinions and views expressed in this report do not necessarily represent those of The University of Queensland, the Centre for Coal Seam Gas or its constituent members or associated companies. -
Gold in Central Queensland
73 GOLD OCCURRENCES IN CENTRAL QUEENSLAND Extract from the Queensland Mining Guide No attempt is made in this portion of the Mining Guide to deal with the past history of the various mining fields or to describe the many mines being worked in the State. The object rather is to show - both to the individual prospector and to the mining investor - some of the mining possibilities of each of the districts mentioned, passing reference being made to particular mines in certain cases only. Slight reference only has been made to geological features. The relative importance of deposits and districts mentioned cannot be gauged by the lengths of the references in these notes. On many of the old fields the conditions are well known, or can be ascertained at the main centres. Special attention has been drawn to some of the lesser known fields. Any person or company desirous of obtaining further details in relation to any of the nines, deposits, or localities referred to should communicate with the Department of Natural Resources, Mines and Energy Brisbane, or with the nearest Warden, Inspector of Mines, or District Geologist. General area covered by this report The Reworking of Deposits The fact that certain ore-bodies were worked years ago and were abandoned does not necessarily imply that such deposits cannot be worked profitably under different conditions. The metal market is always a primary factor in deciding the success or 1:250 000 scale maps failure of mining ventures. The utilization of First edition 1968/75 modern methods of mining and treatment may bring renewed life to some mines. -
4.0 Overview of the Regional Surface and Subsurface Geology of the Duaringa Basin
Duaringa Basin Report on Hydrological Investigations 4.0 Overview of the Regional Surface and Subsurface Geology of the Duaringa Basin 4.1 Introduction The surface geology of the Duaringa Basin project site and surrounding environment is characterised by the surface exposures of the Tertiary age Duaringa Formation sediments and surrounding exposures of the Permian age sediments (Figure 4.1). The Duaringa Formation is composed of interbedded mudstones, shale, oil shale siltstone and lignite beds and rare sandstone, conglomerate and basalt beds (Day et al., 1983). The Permian age sediments are part of the Bowen Basin stratigraphic sequence. The overlying Tertiary age Duaringa Formation does not form part of the formal Bowen Basin stratigraphic sequence. The surface exposures of the Duaringa Formation can be differentiated into recent exposures and older lateritic tablelands. There are also some small outcrops of Tertiary age volcanics exposed through the Tertiary age and Permian age sediments present in and near the Duaringa Basin. The significant rivers, such as the Mackenzie River and Dawson River, which traverse the Duaringa Basin, have deposited large volumes of alluvial sediment in broad braided plains on both the Duaringa Formation and Permian age sediments. The Duaringa Basin along with the Biloela Basin and Hillsborough Basin formed during the opening of the Coral Sea during the Eocene between 52 and 34 million years ago (SRK, 2008). These basins are bounded by NE to SW trending bounding faults along their western margins. Movement along these faults is largely sinistal (left lateral). However, there has been significant downward movement on the eastern side of the fault blocks, which has opened deep asymmetrical grabens (Veevers and Powell, 1994). -
The Modelled Distribution of the Five-Clawed Worm-Skink (Anomalopus Mackayii)
Map 2: The modelled distribution of the five-clawed worm-skink (Anomalopus mackayii) Injune Koko SF Allies Creek SF Kilkivan Wandoan Proston Gympie Jarrah SF Goomeri Barakula SF Wondai SF Gurulmundi SF Mitchell Wallumbilla Roma Diamondy SF Kingaroy Yuleba Nudley SF Miles Chinchilla Conondale FR Yuleba SF Jandowae Blackbutt Bunya Mountains NP Kilcoy Benarkin SF Toogoolawah Surat Braemar SF Dalby Esk Tara Kumbarilla SF Toowoomba Dunmore SF Laidley Western Creek SF Boondandilla SF Millmerran Boonah St George Main Range NP Warwick Whetstone SF State Forest Durikai SF Border Ranges NP Inglewood Goondiwindi Toonumbar NP Boggabilla Yelarbon Stanthorpe Dthinna Dthinnawan CCAZ Texas Girraween NP Sundown NP Wallangarra Mungindi Girard SF Tenterfield Torrington SCA Ashford Lightning Ridge Moree Deepwater Collarenebri Warialda Glen Innes Inverell Bingara Walgett Guy Fawkes River NP Bundarra Wee Waa Mt Kaputar NP Dorrigo Narrabri Barraba Pilliga West CCAZ Pilliga CCAZ Armidale Pilliga East SF Pilliga West SF Euligal SF Pilliga East CCAZ Manilla Timallallie CCAZ Oxley Wild Rivers NP Coonamble Baradine Pilliga NR INDICATIVE MAP ONLY: For the latest departmental information, please refer to the Protected Matters Search Tool at www.environment.gov.au/epbc/index.html km 0 20 40 60 80 100 Legend Species Known/Likely to Occur Species May Occur Brigalow Belt IBRA Region ! Cities & Towns Roads Major Rivers Perennial Lake ! ! ! ! ! ! !! ! ! !! ! ! ! !! ! ! ! ! ! ! !! ! ! !! ! !! ! Non-perennial Lake Produced by: Environmental Resources Information Network (ERIN) Conservation Areas COPYRIGHT Commonwealth of Australia, 2011 Forestry & Indigenous Lands Contextual data sources: DEWHA (2006), Collaborative Australian Protected Areas Database Geoscience Australia (2006), Geodata Topo 250K Topographic Data CAVEAT: The information presented in this map has been provided by a range of groups and agencies. -
RACQ Unroadworthy Roads Technical Appendix
RACQ Unroadworthy Roads Technical Appendix Author Public Policy Date March 2016 Title: RACQ Unroadworthy Roads Technical Appendix Issued Date: March 2016 Page: 1 of 104 List of roads with number of responses to identified problems cont’d IDENTIFIED PROBLEMS Tight Vegetation Poor or Slippery / curves / Narrow Narrow Poor Hazardous Poor or or objects Lack of inadequate Rough Loose blind road / bridge / road Poor Poor roadside no guard block overtaking Flood Poor road Steep Road Name # Responses Surface surface crests lanes culvert markings signing shoulders objects rails visibility opportunities prone drainage lighting grade Bruce Highway 67 38 9 10 27 17 14 8 27 8 11 8 30 22 15 11 1 Pacific Motorway 32 8 1 1 6 1 3 - 4 - - 1 4 - 2 - - Mount Lindesay Highway 21 5 - - 5 - 1 2 4 1 1 - 14 4 2 3 1 Captain Cook Highway 19 5 2 2 2 1 2 - 2 2 1 1 1 4 5 - - Rickertt Road 19 18 3 - 8 3 6 1 13 3 2 - 6 16 9 10 - D'Aguilar Highway 16 12 5 4 6 1 4 1 6 2 1 3 12 2 5 1 1 Kennedy Highway 15 2 5 7 6 1 - - 6 1 5 2 13 1 - 1 1 Warrego Highway 14 11 3 3 5 2 3 2 6 2 - 2 3 3 3 2 - New England Highway 11 9 2 2 4 2 1 1 4 2 2 1 5 2 1 - - Telegraph Road 11 4 - - - - - - 2 - - - - 1 1 - - Kingsford Smith Drive 10 8 2 - 4 - 3 - 2 - - - - - 1 - - Maleny-Kenilworth Road 10 10 2 4 10 4 2 1 8 4 - 1 5 - 2 - - Gore Highway 9 8 1 - 5 - - - 5 1 2 - 2 2 - - - Samford Road 9 7 2 3 6 - 1 1 1 2 - - 2 - 2 - - Tinaburra Drive 9 7 3 5 9 2 4 2 6 2 - 1 3 - - 4 - Burnett Highway 8 8 - 3 4 4 2 2 7 2 1 2 5 3 4 1 - Beachmere Road 7 6 1 2 7 6 1 2 7 - 1 2 2 6 3 3 - Beechmont Road 7 1 2 7 7 -
Patterns of Persistence of the Northern Quoll Dasyurus Hallucatus in Queensland
Surviving the toads: patterns of persistence of the northern quoll Dasyurus hallucatus in Queensland. Report to The Australian Government’s Natural Heritage Trust March 2008 Surviving the toads: patterns of persistence of the northern quoll Dasyurus hallucatus in Queensland. Report submitted to the Natural Heritage Trust Strategic Reserve Program, as a component of project 2005/162: Monitoring & Management of Cane Toad Impact in the Northern Territory. J.C.Z. Woinarski1, M. Oakwood2, J. Winter3, S. Burnett4, D. Milne1, P. Foster5, H. Myles3, and B. Holmes6. 1. Department of Natural Resources Environment and The Arts, PO Box 496, Palmerston, NT, 0831. 2. Envirotek, PO Box 180, Coramba NSW 2450 3. PO Box 151, Ravenshoe Qld 4888; and School of Marine and Tropical Biology, James Cook University, Townsville. 4. PO Box 1219, Maleny 4552; [email protected] Box 1219, Maleny, 4552 5. “Bliss" Environment Centre, 1023D Coramba Rd, Karangi NSW 2450 6. 74 Scott Rd, Herston 4006; [email protected] Photos: front cover – Northern quoll at Cape Upstart. Photo: M. Oakwood & P. Foster CONTENTS Summary 2 Introduction 4 relevant ecology 7 Methods 8 northern quoll Queensland distributional database 8 field survey 8 Analysis 10 change in historical distribution 10 field survey 11 Results 12 change in historical distribution 12 field survey 14 Discussion 15 Acknowledgements 19 References 20 List of Tables 1. Locations of study sites sampled in 2006-07. 25 2. Environmental and other attributes recorded at field survey transects. 27 3. Frequency distribution of quoll records across different time periods. 30 4. Comparison of quoll and non-quoll records for environmental variables. -
2011-12-Annual-Report-Inc-Financial-Report.Pdf
2011 - 2012 Contents About Central Highlands Regional Council ................................................................ 2 Our Vision ................................................................................................................. 3 Our Mission ............................................................................................................... 3 Our Values and Commitment .................................................................................... 3 A Message from Our Mayor and CEO ....................................................................... 4 Our Mayor and Councillors April 28 2012 – June 30 2012 ......................................... 5 Our Mayor and Councillors 2011 – April 28 2012 ...................................................... 7 Our Senior Executive Team ...................................................................................... 9 Our Employees ....................................................................................................... 11 Community Financial Report ................................................................................... 13 Assessment of Council Performance in Implementing its Long Term Community Plan ................................................................................................................................ 19 Meeting Our Corporate Plan Objectives .................................................................. 19 Achievements by Department ................................................................................ -
Office of the Inspector-General Emergency Management GPO Box 1425, Mail Cluster 15.7 BRISBANE, QLD 4001 [email protected]
Office of the Inspector-General Emergency Management GPO Box 1425, Mail Cluster 15.7 BRISBANE, QLD 4001 [email protected] I agree to my submission being treated as outlined in the “Guide to providing submissions” on the IGEM website. Dear Office of the Inspector-General Emergency Management Review Team, Thank you for the opportunity to comment on the 2018 Queensland Bushfires Review. This submission is made on behalf of the Queensland Conservation Council Inc. (QCC). QCC was established in 1969 and is the peak environment conservation organisation in Queensland, with some 50-member groups including ten regional councils, as well as thousands of supporters. We note that the review is focused on key preparedness and response elements for both bushfires and hot weather events, with scope to reflect on the heatwaves in Far North Queensland in November 2018. QCC recognises the tragedy of recent extreme weather events, with loss of life, extensive property damage and the loss of areas of the state’s natural heritage that will take hundreds of years to recover. The cumulative impacts of climate change, including unprecedented extreme temperatures and increased variability in rainfall that have led to the warming and drying of previously humid, subtropical areas1. Further information on this issue can be found in the Climate Council’s recent report Escalating Queensland Bushfire Threat: Interim conclusions and Be prepared: Climate Change and the Queensland Bushfire threat. The impacts of climate change have destabilised Queensland’s historically fire resilient rainforests such as those in the Eungella National Park and Deepwater National Park and led to the catastrophic fire conditions experienced. -
Father Hayes and the Carnarvons
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Queensland eSpace Father Hayes and the Carnarvons FATHER HAYES WAS A MEMBER OF THREE EXPEDITIONS ORGANISED BY THE QUEENSLAND BRANCH OF THE ROYAL GEOGRAPHICAL SOCIETY OF AUSTRALASIA TO THE CARNARVON RANGE IN 1937, 1938 AND 1940. ROSLYN FOLLETT RECOUNTS FATHER HAYES’ CONTRIBUTION TO THESE TRIPS. Following his ordination in 1918, Father British Museum scientific excursion Hayes’ first appointment was as Assistant- to the area, was appointed botanist. Priest at Ipswich. His interest in geology Theodore Culman and Al Burne were the originated there. photographers. “I was always going home with stones “When the party was chosen they were in my pocket. I told the priest in charge short of an ethnologist. Mr Culman that I was going to become a geologist asked Archbishop Duhig, whom he knew and he asked what the deuce that would through their association on various be”, Father Hayes recalled.1 charitable organisations, if he knew of anyone willing to join the expedition and Father Hayes’ chance to work as a Above: share the hardships of an arduous journey. Main: The Royal geologist began when he was invited to Archbishop Duhig at once suggested and Geographical Society of participate in a number of scientific trips released Father Leo Hayes”2 Australasia Expedition to the to the Carnarvons. In 1932, a section of Carnarvon Ranges in 1937. the Carnarvon Gorge had been declared a Father Hayes joined the party as geologist Father Hayes is fourth from national park, following lobbying from the and ethnologist. -
Boost Our Beef Roads East-West Link Bedourie - Rockhampton
boost our beef roads East-west link Bedourie - Rockhampton This is the state of 148 km of the Springsure-Tambo section of the east-west link that carries 225,500 head of cattle each year. Between Bedourie/Birdsville and Springsure is 431 kilomtres of unsealed road owned by both the Queensland Government and councils requiring an investment of $225 million. the funding promise $100 million Northern The road substandard infrastructure and major Australia Beef Roads disruptions during weather events. The East-West link is council and state Program. Since 2010, the road has been closed government roads traversing the Diamantina, $600 million Northern 21 times for a period of up to 35 days. Barcoo, Blackall-Tambo, Central Highlands Australia Roads Program and Rockhampton local government areas The cost of transporting in these with the potential for greater use from conditions increases as a result of $5 billion Northern Australia channel country producers who access longer travel times causing driver Infrastructure Facility southern markets due to road conditions. fatigue and safety issues, along with $3.5 billion over 10 years Users include some of Australia’s increased maintenance, such as tyre Roads of Strategic largest pastoral companies: AA Co, wear and fuel, the cost of which is borne Importance initiative. Napco, Hewitt Australia and Enniskillen by the transport company and passed Pastoral Co. based in the Upper Nogoa onto the grazier. Region. The condition of the road exposes the bid stock to greater than average dust The road is used primarily by southern The Central Highlands Regional smothering, which is an animal welfare producers moving European Union Council and the Blackall-Tambo concern. -
Plate 7. Vine Thicket (Type 3),Goodedulla National Park, West of Rockhampton (Site 73)
Plate 7. Vine thicket (type 3),Goodedulla National Park, west of Rockhampton (site 73). Note browning and loss of foliage due to extreme drought conditions (August 1994). Species include Backhousia kingii, Crown insularis, Owenia venosa, Geijera paniculata and Acalypha eretnorum (foreground). - - Plate 8. Interior of (type 3) vine thicket, "Cerberus", west of Marlborough (site 67). Species include Backhousia kingii, E.vcoecaria dallackyana, Guettardella putaininosa and Planclunzella cotinifolia var. pubescens. 142 CHAPTER FOUR A REGIONAL CONTEXT FOR VINE THICKET COMMUNITIES - FLORISTIC PATTERNS IN THE BRIGALOW BELT BIOGEOGRAPHIC REGION AND RELATIONSHIPS WITH ENVIRONMENTAL ATTRIBUTES, PARTICULARLY CLIMATE. Although the core area of distribution and major remnants of semi-evergreen vine thicket are located in central and southern Queensland, outliers of these communities occur extensively in the northern and southern Brigalow Belt Biogeographic Region. Time and other constraints resulted in the southern (i.e. north-western New South Wales) vine thickets being excluded from the detailed field survey (Chapter 3) and in the northern vine thickets being relatively under-sampled. The latter areas have since been included in a comprehensive floristic survey of northern inland vine thickets by Fensham (1995). Floristic data are available for several southern vine thicket locations (Floyd 1991, J.B.Williams, unpubl. lists), three of which were included in Webb, Tracey and Williams (1984) floristic analysis of Australian rainforests. It was considered desirable to test the robustness of the vine thicket classification/typology derived above (Chapter 3) using an enlarged floristic data set compiled across the entire Brigalow Belt Biogeographic Region. Inclusion of site data from Fenshams (1995) survey has two purposes; (i) to improve the intensity of sampling from the northern Brigalow Belt Biogeographic Region (see above) and (ii) to provide an opportunity to compare the vine thicket classifications from this study and that of Fensham, using a common data set. -
Matters of National Environmental Significance Report
Gold Coast Quarry EIS ATTACHMENT D SITE ACCESS PLANS September 2013 Cardno Chenoweth 99 Gold Coast Quarry EIS ATTACHMENT E SITE TOPOGRAPHY September 2013 Cardno Chenoweth 99 Pacific Motorway 176 176 RP899491 RP899491 N 6889750 m E 539000 m E 539250 m E 539500 m E 539750 m E 540000 m E 540250 m E 540500 m E 540750 m E 541000 m E 541250 m E 541500 m N 6889750 m 903 905 SP210678 SP245339 144 905 WD4736 SP245339 N 6889500 m N 6889500 m Old Coach Road 22 SP238363 N 6889250 m N 6889250 m N 6889000 m N 6889000 m 103 105 5 SP127528 SP144215 RP162129 Barden Ridge Road 103 SP127528 Chesterfield Drive N 6888750 m N 6888750 m 1 RP106195 4 RP162129 RP853810 RP162129 927 6 4 5 SP220598 RP853810 3 RP854351 RP162129 2 N 6888500 m 5 N 6888500 m RP803474 SP105668 12 WD6568 SP105668 7 11 1 SP187063 105 2 3 F:\Jobs\1400\1454 Cardno Boral_Tallebudgera GCQ\000 Generic\Drawings\1454_017 Topography_aerial.dwg 15 SP144215 RP812114 RP803474 RP903701 1 Tallebudgera Creek Road 3 RP148506 FILE NAME: 13 RP803474 SP105668 901 RP907357 2 3 RP803474 SP187063 RP164840 6 N 6888250 m N 6888250 m 14 SP105668 600 SP251058 3 JOB SUB #: 901 1 SP145343 RP205290 RP148504 2 27 Samuel Drive 104 RP811199 RP190638 RP180320 2 8 October 2012 30 2 RP180320 SP150481 N 6888000 m RP838498 31 N 6888000 m RP180321 E 539000 m E 539250 m E 539500 m E 539750 m E 540000 m E 540250 m E 540500 m E 540750 m E 541000 m E 541250 m E 541500 m CREATED: REV DESCRIPTION DATE BY Legend: PROJECT: TITLE: Site Boundary Tallebudgera Figure 13 - Aerial Photo and Topography Photography: Nearmap.