Volcanoes of Auckland
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ATTACHMENT 5 Geological Assessment (Tonkin & Taylor) Job No: 1007709 10 January 2019 McConnell Property PO Box 614 Auckland 1140 Attention: Matt Anderson Dear Matt Orakei ONF Assessment 1- 3 Purewa Rd, Meadowbank Introduction McConnell Property is proposing to undertake the development of a multi-story apartment building at 1 - 3 Purewa Road, Meadowbank. The property is located within an area covered by the Outstanding Natural Feature (ONF) overlay of the Auckland Unitary Plan. The overlay relates to the Orakei Basin volcano located to the west of the property. The ONF overlay requires consent for the earthworks and the proposed built form associated with the development of the site. McConnell Property has commissioned Tonkin & Taylor Ltd (T+T) to provide a geological assessment of the property with respect to both the ONF overlay and the geological characteristics of the property. The purpose of the assessment is to place the property in context of the significant geological features identified by the ONF overlay, and to assess the geological effects of the proposed development. Proposed Development The proposal (as shown in the architectural drawings appended to the application) is to remove the existing houses and much of the vegetation from the site, and to develop the site with a new four- storey residential apartment building with a single-level basement for parking. The development will involve excavation of the site, which will require cuts of up to approximately 6m below existing ground level (bgl). The cut depths vary across the site, resulting in the average cut depth being less than 6m bgl. Site Description The site is located at the end of the eastern arm of the ridgeline that encloses the Orakei Basin (Figure 1). -
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. -
Age of the Auckland Volcanic Field: a Review of Existing Data
New Zealand Journal of Geology and Geophysics ISSN: 0028-8306 (Print) 1175-8791 (Online) Journal homepage: http://www.tandfonline.com/loi/tnzg20 Age of the Auckland Volcanic Field: a review of existing data JM Lindsay , GS Leonard , ER Smid & BW Hayward To cite this article: JM Lindsay , GS Leonard , ER Smid & BW Hayward (2011) Age of the Auckland Volcanic Field: a review of existing data, New Zealand Journal of Geology and Geophysics, 54:4, 379-401, DOI: 10.1080/00288306.2011.595805 To link to this article: http://dx.doi.org/10.1080/00288306.2011.595805 Published online: 07 Nov 2011. Submit your article to this journal Article views: 1375 View related articles Citing articles: 25 View citing articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tnzg20 Download by: [109.56.190.155] Date: 28 February 2017, At: 14:34 New Zealand Journal of Geology and Geophysics Vol. 54, No. 4, December 2011, 379Á401 Age of the Auckland Volcanic Field: a review of existing data JM Lindsaya,c*, GS Leonardb, ER Smidc and BW Haywardd aSchool of Environment, The University of Auckland, Auckland, New Zealand; bGNS Science, Lower Hutt, New Zealand; cInstitute of Earth Science and Engineering, The University of Auckland, Auckland, New Zealand; dGeomarine Research, St Johns, Auckland, New Zealand (Received 10 March 2011; final version received 1 June 2011) Determining magnitudeÁfrequency relationships, a critical first step in assessing volcanic hazard, has been hampered in the Auckland Volcanic Field (AVF) by the difficulty in dating past eruptions from the field’s c. -
Pukekawa — the Domain Volcano
Pukekawa — the Domain Volcano New Zealand is a land of volcanoes The springs provided Auckland’s first leading the Ngapuhi from the North and earthquakes. Volcanic activity has piped water supply in 1866. The and Potatau Te Wherowhero leading played a major role in shaping New Domain Wintergarden’s fernery occu- the local Ngati Whatua. A sacred Zealand since its earliest origins, pies a disused scoria quarry on the Totara tree planted by Princess Te around 500 million years ago. north side of the small central scoria Puea Herangi to commemorate the Auckland City is built on an active field cone. battles and the eventual settlement of of small basalt volcanoes. Forty-eight the dispute stands on Pukekaroa sur- have erupted within 29km of the city Maori Use of Pukekawa rounded by a palisade. centre over the last 150 000 years. The The Domain has been altered signifi- Later Use of Auckland’s most recent eruption, 600 years ago, cantly by contact with humans. When Volcanoes formed Rangitoto Island at the en- Maori people arrived in Auckland they trance to Auckland Harbour. Because cleared the land for gardens, particu- Pukekawa was part of the land which of the intensity of past volcanic and larly choosing the fertile north-facing Ngati Whatua sold to the Europeans geologic activity within the Auckland who by 1860 had drained and filled region another eruption possible. slopes of the volcanic cones. Later their descendants looked to more per- the swamp and turned it into cricket Auckland Domain Volcano manent settlements, so that parts of fields. -
Auckland Trail Notes Contents
22 October 2020 Auckland trail notes Contents • Mangawhai to Pakiri • Mt Tamahunga (Te Hikoi O Te Kiri) Track • Govan Wilson to Puhoi Valley • Puhoi Track • Puhoi to Wenderholm by kayak • Puhoi to Wenderholm by walk • Wenderholm to Stillwater • Okura to Long Bay • North Shore Coastal Walk • Coast to Coast Walkway • Onehunga to Puhinui • Puhinui Stream Track • Totara Park to Mangatawhiri River • Hunua Ranges • Mangatawhiri to Mercer Mangawhai to Pakiri Route From Mangawhai Heads carpark, follow the road to the walkway by 44 Wintle Street which leads down to the estuary. Follow the estuary past a camping ground, a boat ramp & holiday baches until wooden steps lead up to the Findlay Street walkway. From Findlay Street, head left into Molesworth Drive until reaching Mangawhai Village. Then a right into Moir Street, left into Insley Street and across the estuary then left into Black Swamp Road. Follow this road until reaching Pacific Road which leads you through a forestry block to the beach and the next stage of Te Araroa. Bypass Note: You could obtain a boat ride across the estuary to the Mangawhai Spit to avoid the road walking section. Care of sand-nesting birds is required on this Scientific Wildlife Reserve - please stick to the shoreline. Just 1km south, a stream cuts across the beach and it can go over thigh height, as can other water crossings on this track. Follow the coast southwards for another 2km, then take the 1 track over Te Ārai Point. Once back on the beach, continue south for 12km (fording Poutawa Stream on the way) until you cross the Pākiri River then head inland to reach the end of Pākiri River Road. -
Auckland Plan Targets: Monitoring Report 2015 with DATA for the SOUTHERN INITIATIVE AREA
Auckland plan targets: monitoring report 2015 WITH DATA FOR THE SOUTHERN INITIATIVE AREA Auckland Plan Targets: Monitoring Report 2015 With Data for the Southern Initiative Area March 2016 Technical Report 2016/007 Auckland Council Technical Report 2016/007 ISSN 2230-4525 (Print) ISSN 2230-4533 (Online) ISBN 978-0-9941350-0-1 (Print) ISBN 978-0-9941350-1-8 (PDF) This report has been peer reviewed by the Peer Review Panel. Submitted for review on 26 February 2016 Review completed on 18 March 2016 Reviewed by one reviewer. Approved for Auckland Council publication by: Name: Dr Lucy Baragwanath Position: Manager, Research and Evaluation Unit Date: 18 March 2016 Recommended citation Wilson, R., Reid, A and Bishop, C (2016). Auckland Plan targets: monitoring report 2015 with data for the Southern Initiative area. Auckland Council technical report, TR2016/007 Note This technical report updates and replaces Auckland Council technical report TR2015/030 Auckland Plan Targets: monitoring report 2015 which does not contain data for the Southern Initiative area. © 2016 Auckland Council This publication is provided strictly subject to Auckland Council's copyright and other intellectual property rights (if any) in the publication. Users of the publication may only access, reproduce and use the publication, in a secure digital medium or hard copy, for responsible genuine non-commercial purposes relating to personal, public service or educational purposes, provided that the publication is only ever accurately reproduced and proper attribution of its source, publication date and authorship is attached to any use or reproduction. This publication must not be used in any way for any commercial purpose without the prior written consent of Auckland Council. -
A U C K L a N D C O U N C
A U C K L A N D C O U N C I L Decision following the hearing of an application for resource consent SUBJECT: Application for resource consent under section 88 of the Resource Management Act 1991 by Peers Brown Miller Ltd to remove two notable pohutukawa trees from within a grove at 8 Minnehaha Avenue, Takapuna held on Monday, 17 November 2014 commencing at 9.31am CONSENT, PURSUANT TO SECTIONS 104 AND 104B OF THE RESOURCE MANAGEMENT ACT, IS REFUSED. THE FULL DECISION IS SET OUT BELOW Hearing Panel: The Application was heard by Hearings Commissioners consisting of: Ms Kathleen Ryan (Chairperson) Mr Hugh Leersnyder Council Officers: Ms Sally Robins Senior Planner Mr Steven Krebs Arborist Ms Rebecca Fogel Built Heritage Specialist Ms Melissa Democracy Advisor - Hearings Warmenhoven APPEARANCES: For the applicant: Peers Brown Miller Ltd on behalf of N M Growth Limited, represented by: Andrew Braggins (legal counsel) calling the following as witnesses: Sarah Aynsley - Applicant Roger Twiname – Structural Engineer Ross Thurlow – Structural Engineer Rob Pryor – Landscape Architect Gerard Mostert - Arborist Submitters: Maurice Norton for Environment Takapuna Inc Mike Smith Peter Cunningham Hueline Massey for the Tree Council: and Chris Boucher, Arborist, as witness 1 APPLICATION DESCRIPTION Application and Property Details Application Number (s): LX2138339 Site Address: 8 Minnehaha Avenue, Takapuna Applicant's Name: Peers Brown Miller Ltd on behalf of N M Growth Ltd Lodgement Date: 0 August 2013 Notification date: 24 June 2014 Submissions closed -
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. -
Cultural Value Assessment
CULTURAL VALUES ASSESSMENT BY TE ĀKITAI WAIOHUA for DRURY PLAN CHANGES Copyright © 2019 Te Ākitai Waiohua - The information contained in this document is to remain confidential and is supplied only for the purposes of the specified project. It is not to be disclosed to any third party for purposes outside of the specified project without the express permission of Te Ākitai Waiohua. Table of Contents TE ĀKITAI WAIOHUA STRUCTURE ..................................................................................... 3 PRINCIPLES OF THE ENVIRONMENT ................................................................................. 4 KAITIAKITANGA .................................................................................................................... 4 RESOURCE MANAGEMENT ACT ........................................................................................ 6 PRINCIPLES OF THE TREATY OF WAITANGI .................................................................... 7 CULTURAL VALUES ASSESSMENT ................................................................................... 8 PRINCIPLES OF CONSULTATION ....................................................................................... 8 TE ĀKITAI WAIOHUA GENEALOGY .................................................................................... 9 TE ĀKITAI WAIOHUA TIMELINE SUMMARY ..................................................................... 10 TE ĀKITAI WAIOHUA HISTORICAL SUMMARY ................................................................ 13 DRURY PLAN CHANGES................................................................................................... -
Changes to the Marine Biota of the Auckland Harbour, by F. I
TANE 29, 1983 CHANGES TO THE MARINE BIOTA OF THE AUCKLAND HARBOUR by F. I. Dromgoole* and B. A. Fostert * Department of Botany, University of Auckland, Private Bag, Auckland t Department of Zoology, University of Auckland, Private Bag, Auckland SUMMARY The history of study of the marine biota of Auckland Harbour is briefly reviewed, and it is concluded that there is insufficient documented information to make quantitative assessment of changes that have resulted from reclamation, sedimentation and pollution that have occurred with the development of the Port of Auckland. Losses of mangrove and saltmarsh communities are indisputable, but causes of declines in populations of Zostera, Pomatoceros and Perna are not so clear. On the other hand, a number of species have been introduced, and circumstantial evidence suggests these adventives have arrived as ship- fouling. Cases discussed are Codium fragile tomentosoides, Colpomenia bullosa, Limaria orientalis and Sagartia luciae. The most conspicuous newcomer, the oyster Crassostrea gigas, may have been deliberately introduced. INTRODUCTION Regular use of the Auckland Harbour by European ships stems from the early 1800s, so there has been ample opportunity for the introduction of adventive fouling species. Maritime reclamation in Auckland Harbour dates back to about 1860 when shores near the commercial centre were filled and extended as wharves and breakwaters. Modification of habitats and inhabitants of the harbour has now been going on for more than 120 years, but scientific study of them has been of much shorter duration. In this paper we wish to document some additions and alterations to the marine biology. Auckland Harbour has three parts (see Fig. -
Sylvia Park and the Mt Wellington Area Sunee Yoo
Give Us Space Improving community well-being by enhancing performance and communication of semi-public space in the evolving public realm Analytical Tools Semi-Public Space Conflicts and Alliances in Primary Metropolitan Centres: Sylvia Park, Mt Wellington, Auckland Background to Case Study: Sylvia Park and the Mt Wellington Area Sunee Yoo [ WORKING DOCUMENT GUS/SP2.2] The Auckland Isthmus Historically, the lands and waters of Tāmaki Makaurau (Auckland) have always been highly contested. The isthmus not only offered rich volcanic soils, many waterways and inlets, but also a strategic location for trade. Auckland was centered on interconnecting trade routes between the Bay of Plenty, Coromandel, Waikato and Northland.*https://teara.govt.nz/en/tamaki-tribes/page-1 Around 1250 A.D., voyagers on canoes from East Polynesia became the earliest settlers of New Zealand. Among the many canoes, the Tainui canoe pulled ashore at Waitematā Harbour (Auckland Harbour) and its descendants put down roots in the Auckland Isthmus.*https://teara.govt.nz/en/tamaki-tribes/page-1 And by the 19th century, much of the Hauraki Gulf, including the eastern coast of Auckland, was inhabited by the descendant tribes of Marutūahu of the Taninui canoe. Fig. 1. Map of the Auckland Metropolitan area illustration the distribution of rich volcanic soils developed on Auckland basalt. Case Study site highlighted. http://www.thebookshelf.auckland.ac.nz/docs/Tane/Tane- 29/2%20Prehistoric%20pa%20sites%20of%20metropolitan%20Auckland.pdf (4) Ngāti Pāoa: Iwi of the Mokoia Pā, Maungarei and Mauinaina (Mt Wellington, Panmure area) For many years prior to European contact, Ngāti Pāoa, a descendant tribe of Marutūahu, occupied the stretch of land from the Thames estuary, the Hūnua Ranges, east Tāmaki, Waiheke Island and the coast northward to Whangaparāoa. -
Appendix 3A Schedule of Archaeological Features
APPENDIX 3A SCHEDULE OF ARCHAEOLOGICAL FEATURES . CITY OF AUCKLAND - DISTRICT PLAN ISTHMUS SECTION - OPERATIVE 1999 Page 1 reprinted 04/07/03 APPENDIX 3A CITY OF AUCKLAND - DISTRICT PLAN Page 2 ISTHMUS SECTION - OPERATIVE 1999 reprinted 04/07/03 APPENDIX 3A SCHEDULE OF ARCHAEOLOGICAL FEATURES Note: A = Archaeological Feature H = Historic/Cultural Value A/G = Archaeological and Geological Feature S = Scientific/Educational Value V = Visual Amenity Value For an explanation of the criteria for scheduling and the rules refer Part 5C.7.4 ARCHAEOLOGICAL FEATURES NOTE: This schedule is not the same as the New Zealand Historic Places Trust Register for Auckland. It is a separate but parallel protection process. Since an archaeological feature may appear in either or both lists care should be taken to ascertain and fulfil any obligations deriving from the feature being included in either or both lists. THIS SCHEDULE DOES NOT INCLUDE PROTECTED ITEMS IN THE CENTRAL AREA OR HAURAKI GULF ISLANDS ADDRESS FEATURE PRINCIPAL FEATURE MAP CRITERIA FOR TYPE REFERENCE SCHEDULING Achilles Point to Karaka Bay cliffline Pa and associated Maori H, S, V A/G B15-06 Cliff Road, Waitara Road, Riddell Road habitation sites. Waitemata vicinity. series sandstone cliffs showing folded strata and Parnell Grit at Karaka Point. Also fallen blocks from the tuff ring of Glover Park. Crater containing pieces of greywacke, sandstone and schist brought up from depth Auckland Domain Pa and associated Maori H, S, V A/G C09-23 Stanley Street, Titoki Street, Carlton Gore habitation sites, early European Road, Park Road, Auckland Hospital, sites, explosion crater, scoria Grafton Road.