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Schedule 6 Outstanding Natural Features Overlay Schedule
Schedule 6 Outstanding Natural Features Overlay Schedule Schedule 6 Outstanding Natural Features Overlay Schedule [rcp/dp] Introduction The factors in B4.2.2(4) have been used to determine the features included in Schedule 6 Outstanding Natural Features Overlay Schedule, and will be used to assess proposed future additions to the schedule. ID Name Location Site type Description Unitary Plan criteria 2 Algies Beach Algies Bay E This site is one of the a, b, g melange best examples of an exposure of the contact between Northland Allocthon and Miocene Waitemata Group rocks. 3 Ambury Road Mangere F A complex 140m long a, b, c, lava cave Bridge lava cave with two d, g, i branches and many well- preserved flow features. Part of the cave contains unusual lava stalagmites with corresponding stalactites above. 4 Anawhata Waitākere A This locality includes a a, c, e, gorge and combination of g, i, l beach unmodified landforms, produced by the dynamic geomorphic processes of the Waitakere coast. Anawhata Beach is an exposed sandy beach, accumulated between dramatic rocky headlands. Inland from the beach, the Anawhata Stream has incised a deep gorge into the surrounding conglomerate rock. 5 Anawhata Waitākere E A well-exposed, and a, b, g, l intrusion unusual mushroom-shaped andesite intrusion in sea cliffs in a small embayment around rocks at the north side of Anawhata Beach. 6 Arataki Titirangi E The best and most easily a, c, l volcanic accessible exposure in breccia and the eastern Waitākere sandstone Ranges illustrating the interfingering nature of Auckland Unitary Plan Operative in part 1 Schedule 6 Outstanding Natural Features Overlay Schedule the coarse volcanic breccias from the Waitākere Volcano with the volcanic-poor Waitematā Basin sandstone and siltstones. -
Dilemma of Geoconservation of Monogenetic Volcanic Sites Under Fast Urbanization and Infrastructure Developments with Special Re
sustainability Article Dilemma of Geoconservation of Monogenetic Volcanic Sites under Fast Urbanization and Infrastructure Developments with Special Relevance to the Auckland Volcanic Field, New Zealand Károly Németh 1,2,3,* , Ilmars Gravis 3 and Boglárka Németh 1 1 School of Agriculture and Environment, Massey University, Palmerston North 4442, New Zealand; [email protected] 2 Institute of Earth Physics and Space Science, 9400 Sopron, Hungary 3 The Geoconservation Trust Aotearoa, 52 Hukutaia Road, Op¯ otiki¯ 3122, New Zealand; [email protected] * Correspondence: [email protected]; Tel.: +64-27-4791484 Abstract: Geoheritage is an important aspect in developing workable strategies for natural hazard resilience. This is reflected in the UNESCO IGCP Project (# 692. Geoheritage for Geohazard Resilience) that continues to successfully develop global awareness of the multifaced aspects of geoheritage research. Geohazards form a great variety of natural phenomena that should be properly identified, and their importance communicated to all levels of society. This is especially the case in urban areas such as Auckland. The largest socio-economic urban center in New Zealand, Auckland faces potential volcanic hazards as it sits on an active Quaternary monogenetic volcanic field. Individual volcanic geosites of young eruptive products are considered to form the foundation of community Citation: Németh, K.; Gravis, I.; outreach demonstrating causes and consequences of volcanism associated volcanism. However, in Németh, B. Dilemma of recent decades, rapid urban development has increased demand for raw materials and encroached Geoconservation of Monogenetic on natural sites which would be ideal for such outreach. The dramatic loss of volcanic geoheritage Volcanic Sites under Fast of Auckland is alarming. -
Auckland Volcanic Field Magmatism, Volcanism, and Hazard: a Review
1 This is an Accepted Manuscript of an article published by Taylor & Francis in New Zealand 2 Journal of Geology and Geophysics on 18 March 2020, available online: 3 http://www.tandfonline.com/10.1080/00288306.2020.1736102 4 5 6 Auckland Volcanic Field magmatism, volcanism, and hazard: a review 7 8 9 Jenni L Hopkins*1, Elaine R Smid*2, Jennifer D Eccles2, Josh L Hayes3, Bruce W Hayward4, Lucy E McGee5, 10 Kasper van Wijk2, Thomas M Wilson3, Shane J Cronin2, Graham S Leonard6, Jan M Lindsay2, Karoly 11 Németh7, Ian E M Smith2 12 13 *Corresponding Author(s): [email protected] / [email protected] 14 15 1Victoria University of Wellington, PO Box 600, Wellington, New Zealand 16 2 University of Auckland, Private Bag 92019, Auckland, New Zealand 17 3 University of Canterbury, Private Bag 4800, Christchurch, New Zealand 18 4 Geomarine Research, 19 Debron Ave, Remuera, Auckland, New Zealand 19 5 University of Adelaide, Adelaide, Australia 20 6 GNS Science, PO Box 30-368, Lower Hutt, New Zealand 21 7 Massey University, Private Bag 11 222, Palmerston North, New Zealand 22 23 24 25 26 27 Manuscript prepared for submission to the IAVCEI special issue of New Zealand Journal of Geology and 28 Geophysics 29 30 31 1 32 33 Keywords 34 intraplate, monogenetic volcanism, chronology, tephrochronology, volcanic hazard assessment, faulting, 35 magma ascent rates, geochemistry, eruption scenarios, New Zealand 2 36 Abstract 37 Auckland Volcanic Field (AVF) is a basaltic intraplate volcanic field in North Island, New Zealand, 38 upon which >1.6 million people live. -
Auckland Council District Plan Operative Manukau Section 2002: Plan Amendment 76
I K Maori Values Assessment Maori Values Appendix I Redoubt Road – Mill Road Corridor Project Ngati Te Ata Waiohua Maori Values Assessment for Auckland Transport Dec 2012 1 “Ka Pa Taua Ko nga Kahu Pokere Ko nga Kuri Rangaunu o Tamaki E kore e ngaro i te Hinepouri” “Our chieftainship in Tamaki will never be lost to darkness” Na Te Rangi Hahautu, Te Rangi Kaimata 2 Table of Contents Foreword 4-6 Introduction 7-9 Purpose & Authorship 10 Project Site Location 11 Definition of a Maori Values Assessment (MVA) 12-13 Ngati Te Ata Waiohua and the Treaty 14-17 Ngati Te Ata Waiohua Kaitiakitanga 18-20 Te Kaitiakitanga o Te Taio Environment 21-32 Redoubt Road – Mill Road Cultural Landscape: Traditional Relationship, Use, and Occupation & Historic Heritage Values 33-40 Conclusion & Recommendations 41-43 Sources 44 Appendices: 1. Extract from AE Tonson Old Manukau (Auckland 1966, pp.15-16) 45-46 2. Ngati Te Ata Waiohua Cultural and Archaeological Protocols 47-50 3. Ngati Te Ata Waiohua Artisans 51-52 4. Kaitiaki Native Tree Planting and Weed Clearance Team 53 Fig. 1. Puhinui Stream Forest Trail – Auckland Council ‘Walkway of the Month’ in August 2011. Source: AC web site. 3 Foreword Ngati Te Ata Waiohua’s issues and values originate from our worldview and our tikanga. They are not available to be compromised or interpreted by those without our history, our whakapapa, and our matauranga. Ngati Te Ata descends from Te Waiohua – the enduring spirit of Hua. This is a name signifi- cant to a number of Auckland iwi. -
Age of the Auckland Volcanic Field Jan Lindsay and Graham Leonard
Age of the Auckland Volcanic Field Jan Lindsay and Graham Leonard IESE Report 1-2009.02 | June 2009 ISBN: [print] 978-0-473-15316-8 [PDF] 978-0-473-15416-5 Age of the Auckland Volcanic Field Jan Lindsay1 and Graham Leonard2 1School of Environment & Institute of Earth Science and Engineering, The University of Auckland, Private Bag 92019, Auckland, New Zealand; [email protected] 2GNS Science, PO Box 30368, Lower Hutt 5040 New Zealand; [email protected] IESE Report 1-2009.02 | June 2009 ISBN: [print] 978-0-473-15316-8 [PDF] 978-0-473-15416-5 This report was prepared by IESE as part of the DEVORA Project. Disclaimer: While the information contained in this report is believed to be correct at the time of publication, the Institute of Earth Science and Engineering and its working parties and agents involved in preparation and publication, do not accept any liability for its contents or for any consequences arising from its use. Copyright: This work is copyright of the Institute of Earth Science and Engineering. The content may be used with acknowledgement to the Institute of Earth Science and Engineering and the appropriate citation. TABLE OF CONTENTS INTRODUCTION .......................................................................................................................... 2 Project objectives ..................................................................................................................... 2 Methodology ............................................................................................................................ -
Constructing a Temporal Eruption Record for the Auckland Volcanic Field Via Bayesian Age Reconciliation
Constructing a temporal eruption record for the Auckland Volcanic Field via Bayesian age reconciliation Emily Kawabata, Mark Bebbington, Shane Cronin, Ting Wang Massey University, University of Auckland, University of Otago The Auckland Volcanic Field High population density, lifelines narrowly constrained - WHERE is the next eruption likely to be? 2 Spatio-temporal hazard estimates Monogenetic volcanic fields have multiple volcanoes; a new eruption is expected to create a new volcano. Events are infrequent. For land-use and emergency planning purposes: where is the next eruption likely to be? In short time frame, answered(?) by monitoring data (seismicity, gas, ...) What about in a period of repose? Probability forecast: estimate the hazard λ(x) such that the probability of an event in the neighbourhood of x , (i.e., y:||y-x|| < ∆x) ~ λ(x) π (∆x)2 We know the spatial locations of Look for spatial patterns (events are more (most) vents likely to occur `near’ previous events?) BUT! Want PRESENT DAY hazard Does the pattern change over time? 3 The Auckland Volcanic Field 51(?) small basaltic volcanoes young (~250,000 years) Most recent eruption ~600 years ago Data: • Stratigraphy, ~33 vents constrained in at least one direction • Age determinations • Paleomagnetism ~5+ vents • C14, ~13 vents • Tephrostratigraphy, 22+ tephra in 5 locations • Ar-Ar, ~4 vents • Thermoluminesence, 2 vents • K-Ar, unreliable due to excess Ar reliability Decreasing • Relative geomorphology or weathering Also: known vent locations, reasonable volume data (Allen and Smith 1994; Kereszturi et al. 2013) 4 A Monte Carlo sample of age-orderings Name Mean Age (ka) Age Error (ka) Min Order Max Order By reverse engineering the tephra Onepoto Basin 248.4 27.8 1 7 Albert Park 229.8 39.5 1 7 dispersal, Bebbington and Cronin ..... -
Maori Gardening: an Archaeological Perspective
Maori gardening An archaeological perspective Louise Furey Published by Science & Technical Publishing Department of Conservation PO Box 10–420 Wellington, New Zealand Cover: Pa, stone row enclosures and puke (garden mounds) at Waikekeno, Wairarapa. Photo: Kevin L. Jones, DOC. © Copyright October 2006, New Zealand Department of Conservation ISBN 0–478–14122–X This report was prepared for publication by Science & Technical Publishing; editing by Lynette Clelland and Amanda Todd, and layout by Amanda Todd. Publication was approved by the Chief Scientist (Research, Development & Improvement Division), Department of Conservation, Wellington, New Zealand. In the interest of forest conservation, we support paperless electronic publishing. When printing, recycled paper is used wherever possible. CONTENTS Abstract 5 1. Introduction 6 2. Maori cultigens 10 2.1 Kumara 10 2.2 Taro 13 2.3 Yam 14 2.4 Gourd 14 2.5 Ti pore 15 2.6 Aute 16 3. Gardening techniques 17 3.1 Garden location 17 3.2 Garden size 17 3.3 Fallowing 18 3.4 Garden preparation 18 3.5 Soil additives 19 4. Limitations to growth of Maori cultigens 20 5. Archaeological evidence of Maori gardening 23 5.1 Stone structures 24 5.1.1 Stone walls and rows 24 5.1.2 Stone alignments 31 5.1.3 Stone heaps 31 5.1.4 Stone mounds 31 5.1.5 Stone facing 34 5.2 Ditches and trenches 34 5.2.1 Steep-slope trenches 36 5.2.2 Trenches on gentle slopes 38 5.2.3 Trench boundary divisions 39 5.2.4 Wetland ditches 40 5.3 Borrow pits 44 5.4 Garden soils 46 5.5 Garden terraces 52 6. -
Annexure a to Procedural Minute 6
Proposed Auckland Unitary Plan Appendix 3.1 Schedule for the Outstanding Natural Features Overlay Owner/ Approral/ Sub#/ Point Name Theme Topic Subtopic Summary Submission Type Support Evidence Comentary Investigate 81 Mt Royal Rd, Mt Albert, and all other lava cave Appendix 3.1 - Schedule for the entrances, for inclusion in the SEA schedule [Note - relates to Outstanding Natural Outstanding Natural Features ONFs. Refer to Albert-Eden Local Board Views, Volume 26, page 5716-3481 Auckland Council Features (ONF) Rules Overlay Add 30/103]. Local Government no iv Investigate the 'Spring', located under Crystal Motors at 11 Ruru Appendix 3.1 - Schedule for the St, Eden Terrace, for inclusion in the SEA schedule [Note - Outstanding Natural Outstanding Natural Features relates to ONFs. Refer to Albert-Eden Local Board Views, Volume 5716-3482 Auckland Council Features (ONF) Rules Overlay Add 26, page 30/103]. Local Government no iv Auckland Volcanic Appendix 3.1 - Schedule for the Include volcanic features in former outlying district such as Cones Society Outstanding Natural Outstanding Natural Features Franklin within the PAUP including Pukekohe Hill, Puni Mountain, 4485-11 Incorporated Features (ONF) Rules Overlay Add Pukekohe East crater. Key Stakeholder no iv Auckland Volcanic Appendix 3.1 - Schedule for the Cones Society Outstanding Natural Outstanding Natural Features Include Pukekohe Hill and Puni Mountain as outstanding natural 4485-13 Incorporated Features (ONF) Rules Overlay Add features. Key Stakeholder no iv Auckland Volcanic Appendix 3.1 - Schedule for the Cones Society Outstanding Natural Outstanding Natural Features Apply V1 and V2 overlays to volcanic reserves and surrounding 4485-21 Incorporated Features (ONF) Rules Overlay Add Includeareas. -
Local Board Information and Agreements Draft Long-Term Plan 2012-2022
DRAFT LONG-TERM PLAN 2012-2022_ VOLUME FOUR LOCAL BOARD INFORMATION AND AGREEMENTS DRAFT LONG-TERM PLAN 2012-2022_ VOLUME FOUR LOCAL BOARD INFORMATION AND AGREEMENTS About this volume About this volume This is Volume Four of the four volumes that make up the draft LTP. It is set out in two parts, one which provides background on the role of local boards, their decision-making responsibilities and some general information about local board plans and physical boundaries. The second part contains the individual local board agreements for all 21 local boards, which contain detailed information about local activities, services, projects and programmes and the corresponding budgets for the period 1 July 2012 to 30 June 2013. Here we have also included additional information like ten-year budgets for each board and a capital projects list. What this volume covers: the status of draft local board agreements how to have your say during the public consultation period an overview of the local boards local board activities information on the development of local board plans and agreements local board financial information including a consolidated statement of expenditure on local activities about each local board, with an overview of the local board including their strategic priorities and a message from the chairperson draft local board agreements for each local board covering scope of activities levels of service and performance measures local activities including key initiatives and projects expenditure and funding notes to the local board agreements contact details, how to contact your local board, including individual contact details for each local board member an appendix to each Local Board information section which includes their expenditure statements and capital projects for the ten-year period 2012 to 2022. -
Modern Analogues for Miocene to Pleistocene Alkali
Cent. Eur. J. Geosci. • 2(3) • 2010 • 339-361 DOI: 10.2478/v10085-010-0013-8 Central European Journal of Geosciences Modern analogues for Miocene to Pleistocene alkali basaltic phreatomagmatic fields in the Pannonian Basin: “soft-substrate” to “combined” aquifer controlled phreatomagmatism in intraplate volcanic fields Research Article Károly Németh1∗, Shane J. Cronin1, Miguel J. Haller2, Marco Brenna1, Gábor Csillag3 1 Volcanic Risk Solutions CS-INR, Massey University, PO Box 11 222, Palmerston North, New Zealand, 2 Universidad Nacional de la Patagonia San Juan Bosco – Sede Puerto Madryn, Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina, 3 Geological Institute of Hungary, Department of Geological Research, Stefánia út 14, Budapest H-1143, Hungary, Received 29 April 2010; accepted 4 June 2010 Abstract: The Pannonian Basin (Central Europe) hosts numerous alkali basaltic volcanic fields in an area similar to 200 000 km2. These volcanic fields were formed in an approximate time span of 8 million years producing small- volume volcanoes typically considered to be monogenetic. Polycyclic monogenetic volcanic complexes are also common in each field however. The original morphology of volcanic landforms, especially phreatomagmatic volcanoes, is commonly modified. by erosion, commonly aided by tectonic uplift. The phreatomagmatic volcanoes eroded to the level of their sub-surface architecture expose crater to conduit filling as well as diatreme facies of pyroclastic rock assemblages. Uncertainties due to the strong erosion influenced by tectonic uplifts, fast and broad climatic changes, vegetation cover variations, and rapidly changing fluvio-lacustrine events in the past 8 million years in the Pannonian Basin have created a need to reconstruct and visualise the paleoenvironment into which the monogenetic volcanoes erupted. -
Landscape Environmental Baseline Report Final
AUCKLAND INTERNATIONAL AIRPORT PROPOSED SECOND RUNWAY LANDSCAPE BASELINE REPORT Client: Auckland International Airport Limited Project: Proposed Second Runway Report: Landscape Baseline Report Status: Final Date: 23 October 2015 Author: Gavin Lister and Matthew Jones Isthmus PO Box 90 366 Auckland 1142 +64 9 309 7281 [email protected] 151023_3346_GL_AIAL Second Runway_Landscape and Urban Design Baseline Report_p.2 CONTENTS EXECUTIVE SUMMARY ........................................................................................................ 5 INTRODUCTION .................................................................................................................. 7 ANALYSIS OF EXISTING LANDSCAPE .................................................................................... 8 ‘Northern Area of Influence’ ............................................................................................... 8 Northern Landscape ........................................................................................................... 8 Natural features ............................................................................................................................ 8 Activities and aesthetics ............................................................................................................... 8 History ........................................................................................................................................... 9 Future airport urban centre ......................................................................................................... -
Submission of Civic Trust Auckland
Submission of Civic Trust Auckland to Heritage New Zealand Pouhere Taonga - Upgrading List No. 6055 Ōtuataua Stonefields, Auckland to Category 1 Full Name: Mrs Audrey van Ryn (Secretary) Organisation: Civic Trust Auckland Phone (daytime): 379 4008 Phone (evening): 368 1516 Mobile: 021 035 4431 Email: [email protected] Postal address: PO Box 74 049 Greenlane Civic Trust Auckland (CTA) is a non-profit public interest group, incorporated in 1968, with activities and interests throughout the greater Auckland region. Our objects include the following: To promote the recognition and protection of the heritage value of sites, buildings, places or areas. To acknowledge the relationship of Maori and their culture and traditions with their ancestral lands, water, sites, waahi tapu and other taonga. CTA supports upgrading List No. 6055 Ōtuataua Stonefields, Auckland from Category 2 to Category 1. 1. We support the recognition of Ihumātao / Te Ihu o Mataoho as places of special or outstanding historical and cultural significance, under s 65(4)(a)(i), and having manifest significance and value under s 66(3)(a)-(k). The areas also qualify as wahi tupuna under s 66(5). 2. We note that upgrading the Ōtuataua Stonefields to Category 1 may also provide additional evidence for gaining world heritage status for the important Auckland volcanic field. 3. We support the inclusion of Lots 1-2 DP 481169 (RT 674557), also known as the Puketaapapa Block or Wallace Block. 4. We support the full increased extent with the addition of Te Motu a Hiara, Waitomokia, Maungataketake, Ooruarangi and Puketaapapa papakaainga. 5. There is an interesting photo not included in the listing review report that Heritage NZ may wish to consider for inclusion in the final listing.