Explanatory Notes for the Mineral-Resources Map of the Circum-Pacific Region Southwest Quadrant 1:10,000,000
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Buller District Council Bylaw Amendment to the Buller District
Buller District Council Bylaw Amendment to the Buller District Council general bylaw NZS 9201 Part 12 Control of Dogs Section 206 Control of dogs 1204.5 Dogs may be exercised free of restraining devices under the owners constant observation and voice control where there is no likelihood to contravene Section 1204.2 of these Bylaws in the following areas: (1) River edges, beach frontage, including dune areas (excluding conservation areas), or (2) The Westport domain, Brougham street domain, the southern end of the Carters beach domain or, (3) In Reefton, the Strand, adjacent the racecourse on the Crampton road reserve, and the old cemetery on Buller Road. 1205.3 Where a dog is not under control in terms of Section 1202 of this bylaw, the dog control officer may, where the owner is known, and has not been convicted of an offence, or been the recipient of an infringement notice and the dog has not been impounded within the preceding 12 month period, return the dog to the owner forthwith, providing, (a) The owner can be readily located, and (b) The owner is able to receive the dog, and (c) The owner is willing to pay a recovery fee, and (d) The dog if over 3 months of age is registered, and Buller District Council, P O Box 21, Westport Ph: (03) 788 9111 Fax (03) 788 8041 www.bullerdc.govt.nz (e) The conditions under which the dog is kept are satisfactory 1205.4 Any dog that has been impounded due to lack of control shall not be released unless the dog control officer is satisfied that the conditions and facilities under which the dog is normally kept are of a standard to prevent the dog from being able to roam at large. -
Natural Values and Resource Use in the Limmen Bight
NATURAL VALUES AND RESOURCE USE IN THE LIMMEN BIGHT REGION © Australian Marine Conservation Society, January 2019 Australian Marine Conservation Society Phone: +61 (07) 3846 6777 Freecall: 1800 066 299 Email: [email protected] PO Box 5815 West End QLD 4101 Keep Top End Coasts Healthy Alliance Keep Top End Coasts Healthy is an alliance of environment groups including the Australian Marine Conservation Society, the Pew Charitable Trusts and the Environment Centre of the Northern Territory. Authors: Chris Smyth and Joel Turner, Centre for Conservation Geography Printing: Printed on 100% recycled paper by IMAGE OFFSET, Darwin. Maps: Centre for Conservation Geography This report is an independent research paper prepared by the Centre for Conservation Geography commissioned by, and for the exclusive use of, the Keep Top End Coasts Healthy (KTECH) alliance. The report must only be used by KTECH, or with the explicit permission of KTECH. The matters covered in the report are those agreed to between KTECH and the authors. The report does not purport to consider exhaustively all values of the Limmen Bight region. The authors do not accept liability for any loss or damage, including without limitation, compensatory, direct, indirect, or consequential damages and claims of third parties that may be caused directly or indirectly through the use of, reliance upon or interpretation of the contents of the report. Cover photos: Main - Limmen River. Photo: David Hancock Inset (L-R): Green Turtle, Recreational fishing is an important leisure activity in -
“The Next Generation in Iron Ore”
“The Next Generation in Iron Ore” Amex Resources Ltd (ASX(ASX::AXZ)AXZ) Amex Resources Ltd (‘Amex’) is an iron ore focused, mineral resources development company listed on the Australian Securities Exchange (ASX). The Company is currently concentrating on Feasibility Studies and Development of its Mba Delta Ironsand Project, in the Fiji Islands. Philosophy The Company’s philosophy is to: “To acquire, explore and develop mineral properties that show real potential for production of economic iron ore mineralisation, in order to increase shareholder wealth” Projects The Company’s focus is the Mba Delta Ironsand Project in Fiji. Amex also maintains an aggressive program of exploration and project generation. The Company’s project portfolio includes: • Mba Delta Ironsand Project, Viti Levu, Fiji – Development, • Mt Maguire Iron Ore Project, Ashburton, WA – Exploration, • Paraburdoo South Iron Ore Project, Pilbara, WA – Exploration, • Channar West Iron Ore Project, Pilbara, WA – Application. The Company continues to evaluate iron ore properties in the Asia-Pacific region for addition to its project portfolio. Recent Highlights Amex is currently completing Feasibility Studies over its Mba Delta Ironsand Project. Highlights from the Company’s exploration and development program include: • Increased JORC Resource and status upgraded to ‘Indicated’: 220 Million Tonnes @ 10.9% Fe (Iron) • Pilot plant commissioned and producing samples of concentrate for export from Fiji for evaluation by potential end users and strategic partners in China. • Concentrates high quality, grading >58% Fe through simple magnetic separation, with low impurities: 58.5% Fe & 0.65% V2O5 with 5.2% Al 2O3 0.37% CaO 0.05% K 20 3.4% MgO 0.04% Na 2O 0.03% P <0.01% S, 1.5% SiO 2 & 6.5% TiO 2. -
Springs of the Mataranka Area 4
THE BIG PICTURE SPRINGS OF THE MATARANKA AREA 4. THE SWAMP Timor Sea A cavernous limestone aquifer extends The large swampy area located on the south side of across a large part of the Northern Territory the Roper River also owes it’s existence to a and into Queensland. The springs at The Mataranka area is notable for its many springs. geological structure that has caused the aquifer to DARWIN Mataranka are one of several outlet points for become shallower and to thin out towards the Roper the aquifer. Other big springs are found on 295000mE This map shows the location of the main springs and other groundwater discharge features. River (see the cross-section). This has resulted in a the Flora, Katherine and Daly Rivers and in broad area underlain by a shallow watertable and Queensland on the Lawn Hill Creek and It explains why the springs are there and describes some of their characteristics. zones of seepage. Extensive tufa deposits formed there because a ridge of bedrock located downstream Daly River Springs KATHERINE Gulf Gregory River. At Mataranka the water of originates from areas to the southeast as far of the seepage zone, ponded the water in a similar Flora River Springs MATARANKA Carpentaria away as the Barkly Tablelands and from the manner to the rock bars in streams as described in 300000mE northwest as far as the King River. Qa1 the note on tufa formation. The ridge formed a base for tufa to accumulate. Tufa dams merged and grew - Waterhouse Cmt over older ones, eventually forming a continuous sheet of limestone. -
Trans-Lithospheric Diapirism Explains the Presence of Ultra-High Pressure
ARTICLE https://doi.org/10.1038/s43247-021-00122-w OPEN Trans-lithospheric diapirism explains the presence of ultra-high pressure rocks in the European Variscides ✉ Petra Maierová1 , Karel Schulmann1,2, Pavla Štípská1,2, Taras Gerya 3 & Ondrej Lexa 4 The classical concept of collisional orogens suggests that mountain belts form as a crustal wedge between the downgoing and overriding plates. However, this orogenic style is not compatible with the presence of (ultra-)high pressure crustal and mantle rocks far from the plate interface in the Bohemian Massif of Central Europe. Here we use a comparison between geological observations and thermo-mechanical numerical models to explain their formation. 1234567890():,; We suggest that continental crust was first deeply subducted, then flowed laterally under- neath the lithosphere and eventually rose in the form of large partially molten trans- lithospheric diapirs. We further show that trans-lithospheric diapirism produces a specific rock association of (ultra-)high pressure crustal and mantle rocks and ultra-potassic magmas that alternates with the less metamorphosed rocks of the upper plate. Similar rock asso- ciations have been described in other convergent zones, both modern and ancient. We speculate that trans-lithospheric diapirism could be a common process. 1 Center for Lithospheric Research, Czech Geological Survey, Prague 1, Czech Republic. 2 EOST, Institute de Physique de Globe, Université de Strasbourg, Strasbourg, France. 3 Institute of Geophysics, Department of Earth Science, ETH-Zurich, -
Review West Coast Regional Coastal
Review of West Coast Region Coastal Hazard Areas Prepared for West Coast Regional Council June 2012 Authors/Contributors: Richard Measures Helen Rouse For any information regarding this report please contact: Helen Rouse Resource Management Consultant +64-3-343 8037 [email protected] National Institute of Water & Atmospheric Research Ltd 10 Kyle Street Riccarton Christchurch 8011 PO Box 8602, Riccarton Christchurch 8440 New Zealand Phone +64-3-348 8987 Fax +64-3-348 5548 NIWA Client Report No: CHC2012-081 Report date: June 2012 NIWA Project: ELF12226 © All rights reserved. This publication may not be reproduced or copied in any form without the permission of the copyright owner(s). Such permission is only to be given in accordance with the terms of the client’s contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Whilst NIWA has used all reasonable endeavours to ensure that the information contained in this document is accurate, NIWA does not give any express or implied warranty as to the completeness of the information contained herein, or that it will be suitable for any purpose(s) other than those specifically contemplated during the Project or agreed by NIWA and the Client. Contents Executive summary .............................................................................................................. 5 1 Introduction ................................................................................................................. 6 -
Come Join Us in “New Zealand's Happiest Place”*
THE BULLER GUIDE TO LIVING WELL Come join us in “New Zealand’s Happiest Place”* * The Happiness of New Zealand Report – UMR Research 2012 Top 10 reasons why people move here • Easy lifestyle and quality of life • We’re kid-safe and family focused • A strong sense of community and caring • So much to see and do right on your doorstep • World-renowned scenery • Get a great house on an average wage • Getting to work, school or play takes just minutes • An unbeatable range of sport and recreation • Great retail, support services and cafes • Great transport links to main centres Click on our interactive menu and links throughout to go directly to the section you would like to see. 0 1 2 3 4 5 6 7 10 great Housing, Perfect Place Education & Sports, Health and Culture, Relocation reasons Living for the Active Community Recreation, Wellbeing The Arts, Support Intro Essentials Retiree Learning Entertainment Heritage & Useful & Climate contacts SPACE & freedom The Buller district covers Reefton just less than 8600 square – gateway to the Buller from the Lewis Pass route from kilometers with 84% in Christchurch - born from gold in the 1860’s and now a conservation land and National modern goldmining town with a wonderfully preserved Park. All of this wonderful play heritage main street. Entry way to the magnificent Victoria Conservation Park. area for a population of around 10,000 people! Westport Choose your town – – our biggest little town of around 5,500 with all mod cons. The service centre for the Buller sited at the mouth or go country of the Buller River. -
Handbook of Western Australian Aboriginal Languages South of the Kimberley Region
PACIFIC LINGUISTICS Series C - 124 HANDBOOK OF WESTERN AUSTRALIAN ABORIGINAL LANGUAGES SOUTH OF THE KIMBERLEY REGION Nicholas Thieberger Department of Linguistics Research School of Pacific Studies THE AUSTRALIAN NATIONAL UNIVERSITY Thieberger, N. Handbook of Western Australian Aboriginal languages south of the Kimberley Region. C-124, viii + 416 pages. Pacific Linguistics, The Australian National University, 1993. DOI:10.15144/PL-C124.cover ©1993 Pacific Linguistics and/or the author(s). Online edition licensed 2015 CC BY-SA 4.0, with permission of PL. A sealang.net/CRCL initiative. Pacific Linguistics is issued through the Linguistic Circle of Canberra and consists of four series: SERIES A: Occasional Papers SERIES c: Books SERIES B: Monographs SERIES D: Special Publications FOUNDING EDITOR: S.A. Wurm EDITORIAL BOARD: T.E. Dutton, A.K. Pawley, M.D. Ross, D.T. Tryon EDITORIAL ADVISERS: B.W.Bender KA. McElhanon University of Hawaii Summer Institute of Linguistics DavidBradley H.P. McKaughan La Trobe University University of Hawaii Michael G. Clyne P. Miihlhausler Monash University University of Adelaide S.H. Elbert G.N. O'Grady University of Hawaii University of Victoria, B.C. KJ. Franklin KL. Pike Summer Institute of Linguistics Summer Institute of Linguistics W.W.Glover E.C. Polome Summer Institute of Linguistics University of Texas G.W.Grace Gillian Sankoff University of Hawaii University of Pennsylvania M.A.K Halliday W.A.L. Stokhof University of Sydney University of Leiden E. Haugen B.K T' sou Harvard University City Polytechnic of Hong Kong A. Healey E.M. Uhlenbeck Summer Institute of Linguistics University of Leiden L.A. -
Submission of Form BA20 Notice of Consent to the Department of Housing
Submission of Form BA20 Notice of Consent to the Department of Housing The following contact details should be used in relation to obtaining written consent from the Department of Housing as the adjoining property owner along a shared property boundary. 1. Where the Department of Housing property is occupied or construction has been completed the attached list of suburbs should be used to identify the Regional Office responsible for that suburb. The Notice of Consent Form BA20 and relevant documentation should be submitted to the Regional Manager using the details provided for that particular office. 2. Where construction has not yet commenced on the Department of Housing property or where construction is still in progress then the Notice of Consent Form BA20 and relevant documentation should be submitted to the Manager Professional Services using the details provided. NOTE – Approval will be delayed if the Notice of Consent Form BA20 and relevant documentation is not submitted to the correct processing area. -
Structures in Shallow Marine Sediments Associated with Gas and Fluid Migration
Journal of Marine Science and Engineering Review Structures in Shallow Marine Sediments Associated with Gas and Fluid Migration Gongzheng Ma 1,2, Linsen Zhan 2,3, Hailong Lu 1,2,* and Guiting Hou 1,* 1 School of Earth and Space Sciences, Peking University, Beijing 100871, China; [email protected] 2 Beijing International Center for Gas Hydrate, Peking University, Beijing 100871, China; [email protected] 3 College of Engineering, Peking University, Beijing 100871, China * Correspondence: [email protected] (H.L.); [email protected] (G.H.) Abstract: Geological structure changes, including deformations and ruptures, developed in shallow marine sediments are well recognized but were not systematically reviewed in previous studies. These structures, generally developed at a depth less than 1000 m below seafloor, are considered to play a significant role in the migration, accumulation, and emission of hydrocarbon gases and fluids, and the formation of gas hydrates, and they are also taken as critical factors affecting carbon balance in the marine environment. In this review, these structures in shallow marine sediments are classified into overpressure-associated structures, diapir structures and sediment ruptures based on their geometric characteristics and formation mechanisms. Seepages, pockmarks and gas pipes are the structures associated with overpressure, which are generally induced by gas/fluid pressure changes related to gas and/or fluid accumulation, migration and emission. The mud diapir and salt diapir are diapir structures driven by gravity slides, gravity spread and differential compaction. Landslides, polygonal faults and tectonic faults are sediment ruptures, which are developed by gravity, compaction forces and tectonic forces, respectively. Their formation mechanisms can be attributed to sediment diagenesis, compaction and tectonic activities. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Prospect Magazine 2018 Page2
Major Resource Projects Reindeer Gnu Caribou March 2018 Corvus Port Hedland Salt Wandoo Ridley Tusk Port Hedland Oryx Stag Chamois Yara Pilbara Fertilisers NWSV LNG Mineral symbols Commodities Yara Pilbara Nitrates Pluto LNG Cape Lambert Anketell Balla Balla Precious metal Ag........... Silver Dampier Salt Creek Zn Cu Pb Cape Lambert Au (or as shown) Dampier Salt Balla Balla Fe V Ti Au........... Gold Cape Preston Sherlock Bay Steel alloy metal Cu........... Copper Cape Preston East Whim Creek Cu Spinifex Ridge Mo Cu Ni (or as shown) Devil Creek Gas Fe........... Iron Maitland River Pilgango ora Li Ta Miralga Creek Radio Hill Speciality metal K............. Potassium Li Ta Sulphur Springs Zn Cu Pb Ti–Zr (or as shown) Whundo Zn Cu Kln.......... Kaolin Sino Iron ! MARBLE BAR Base metal Balmoral South Wodgina Li Li2CO3 Li............. Lithium Iron Bridge Mag Iron Mardie Salt Li2CO3..... Lithium carbonate Alumina All sites are bauxite LNG........ Liquefied natural gas Corunna Downs LPG........ Liquefied petroleum gas Mt Webber Coal and lignite McPhee Creek Industrial mineral Mag........ Magnetite PANNAWONICA Big Hill W ! Processing plant Mn.......... Manganese Middle Robe Mesas Mo.......... Molybdenum Mesa J Mesa A – Warramboo Ni............ Nickel Nullagine/Millennium Petroleum symbols Pb........... Lead Caliwingina Bungaroo Creek Nullagine CID Gas field Phos....... Phosphate Weelumurra Firetail Bungaroo South Investigator Oil field REE........ Rare earth elements PIOP/Flinders Mulga Downs Mesa – Ant Hill Mn Serenity Kings Oil and gas field Sisd....... Silica sand Homestead Significant oil discovery Ta............ Tantalum Silvergrass Cloud Break West Pilbara Christmas Creek Processing plant Ti............ Titanium Nammuldi Roy Hill Oil / gas pipeline, operating Tlc........... Talc Eliwana Western Turner Koodaideri Oil / gas pipeline, proposed V............