Ōrākei Local Board Open Space Network Plan
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Routes Orakei Mission Bay St Heliers Glendowie Fare Zones & Boundaries
Orakei Routes Fare Zones Tāmaki Glen Innes, St Heliers, Mission Bay, Tamaki Dr, Britomart Mission Bay Link & Boundaries 744 Panmure, Pilkington Rd, Glen Innes, Mt Taylor Dr, St Heliers Glen Innes, West Tamaki Rd, Eastridge, Orakei, Britomart 762 Wellsford St Heliers 774 Mt Taylor Dr, Long Dr, Mission Bay, Tamaki Dr, Britomart Omaha (Monday to Friday peak only) Matakana 775 Glendowie, St Heliers, Mission Bay, Tamaki Dr, Britomart Glendowie (Monday to Friday peak only) Warkworth 781 Mission Bay, Orakei, Victoria Ave, Newmarket, Auckland Museum 782 Sylvia Park, Mt Wellington, Ellerslie, Grand Dr, Meadowbank, Warkworth Southern Bus Timetable Eastridge, Mission Bay 783 Eastern Bays Loop clockwise: St Heliers, Glendowie, Eastridge, Kupe St, Mission Bay, St Heliers Waiwera Helensville Hibiscus Coast Your guide to buses in this area 783 Eastern Bays Loop anticlockwise: St Heliers, Mission Bay, Orewa Wainui Kupe St, Eastridge, Glendowie, St Heliers Kaukapakapa Hibiscus Coast Gulf Harbour Waitoki Upper North Shore Other timetables available in this area that may interest you Albany Waiheke Timetable Routes Constellation Lower North Shore Riverhead Hauraki Gulf Tāmaki Link CityLink, InnerLink, OuterLink, TāmakiLink Takapuna Rangitoto Island Huapai Westgate Link Central Isthmus City Isthmus 66, 68, 650, 670 Waitemata Crosstowns Harbour Britomart Swanson Kingsland Newmarket Beachlands Remuera Rd, Meadowbank, Henderson 75, 650, 747, 751, 755, 781, 782 St Johns, Stonefields Waitakere Panmure New Lynn Waitakere Onehunga 744 762 774 Mt Wellington, 32, -
Letter Template
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). -
TE POU O KĀHU PŌKERE Iwi Management Plan for Ngāti Whātua Ōrākei 2018 Te Pou O Kāhu Pōkere
TE POU O KĀHU PŌKERE Iwi Management Plan for Ngāti Whātua Ōrākei 2018 Te Pou o Kāhu PōKere Ngā Wāhanga o te Mātātaki reflect the stages that Ngāti Whātua Ōrākei go through when laying a challenge. This is commonly referred to as a wero. This document is a wero, a challenge, to work together to better understand the views, perspectives and priorities of Ngāti Whātua Ōrākei in relation to resource management matters. The name of this plan is taken from one of the wāhanga (stages) of the mātātaki (challenge). This is called Te Pou o Kāhu Pōkere. The Kāhu Pōkere is the black hawk and is a central figure on the front of our whare tupuna, Tumutumuwhenua. It is a cultural legacy of the hapū and symbolises kaitiakitanga which is the underlying principle of this work. The purpose of this stage and for Ngāti Whātua Ōrākei is to personify the role of the Kāhu Pōkere. It is elevated and holds dominion to protect those in its care, to look out to the distance, traversing and understanding ones domain and ascertaining the intention of others. Inherent in this stage and in this document is action, movement, focus and to be resolute with clarity and purpose. Te Pou o Kāhu Pōkere is a recognised iwi planning document for the purposes of the Resource Management Act 1991. CoNTeNTs RĀRANGI KŌRERO RĀRANGI KŌRERO (CoNTeNTS) ������������������������������������������������������������������������������������������� 3 KuPu WhAKATAKI (FOREWORD) ����������������������������������������������������������������������������������������� 4 FROM THE MAYOR oF AuCKLAND -
Appendix 4 Mana Whenua
The Proposed Auckland Unitary Plan (notified 30 September 2013) Proposed track changes for council’s closing statement 22 July 2015 Sites highlighted green are recommended to be amendend to reflect accurate location on schedule and maps Sites highlighted orange are recommended to be deleted because location is not confirmed Sites highlighted grey are recommended to be deleted because Mana Whenua have not assigned values Sites highlighted red are recommended to be deleted because they are non-Māori or duplicates Sites highlighted blue are recommended to be deleted because unknown whether natural feature or archaeological PART 5 • APPENDICES» Appendix 4 Mana Whenua Appendix 4.2 Schedule of Ssites and places of value to Mana Whenua [all provisions in this appendix are: rcp/dp] NZAA Site Values ID CHI Number Location Te Haruhi Bay | Shakespear Regional Park | abcef ID 1 87 R10_699 Whangaparaoa Peninsula | Hauraki Gulf. Whangaparapara | Aotea Island | Great Barrier ID 2 502 S09_116 Island. | Hauraki Gulf | Auckland City Bluebell Point | Tawharanui Regional Park | bc ID 3 829 R09_235 Hauraki Gulf | Rodney | Auckland ID 4 1066 Q11_412 abcdef Parawai | Te Henga | Bethells Beach Rangiriri Creek | Capes Road | Pollok | Awhitu abcdef ID 5 1752 R12_799 Peninsula | Manukau Harbour ID 6 3832 R11_581 bc Papahinu | Pukaki Creek | Papatoetoe ID 7 3835 R11_591 bc Waokauri Creek | Pukaki Creek | Papatoetoe ID 8 3843 R11_599 abc Waokauri Creek | Papatoetoe ID 9 3845 R11_601 bc Waokauri Creek | Papatoetoe ID 10 3846 R11_603 bc Waokauri Creek | Papatoetoe -
Auckland Transport Glen Innes to Tamaki Drive Cycle Route
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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. -
March 2013 1 Appendix 3.1: Schedule Of
Draft Auckland Unitary Plan – March 2013 Appendix 3.1: Schedule of Outstanding Natural Features Introduction The following criteria are used to determine the contents of this schedule, and will be used to consider any proposed additions to it. a. the extent to which the landform feature or geological site contributes to the understanding of the geology or evolution of the biota in the region, New Zealand or the earth (includes type localities of rock formations, minerals and fossils) b. the rarity or unusual nature of the site or feature; c. the extent to which the feature or site is an outstanding representative example of the diversity of natural landforms and geological features in Auckland; d. the extent to which the landform or geological feature or site is a component of a recognisable group of geologically associated features; e. the extent to which the landform or geological feature or site contributes to the aesthetic value or visual legibility of the wider natural landscape; f. the community association with, or public appreciation of the values of the feature or site g. the potential value of the feature or site for public education; h. the potential value of the feature or site to provide additional understanding of the geological or biotic history of the region; i. the state of preservation of the feature or site; j. the extent to which a feature or site is associated with an historically important natural event, geologically related industry, or individual involved in earth science research k. the importance of the feature or site to Mana Whenua; l. -
History Booklet U3A Meadowbank 2000-2010
U3A MEADOWBANK INC. July 2000 – 2010. The idea of U3A was born in France (1973), adapted and changed in Britain (1981), Spread to Australia (1984) and NZ (1989) and in 2000 we arrived – U3A Meadowbank! TABLE OF CONTENTS Introduction from the President (Sabine Fenton 2010) History of the U3A movement as a whole/ internationally. Developments in New Zealand/ Auckland/ and the U3A Auckland Network. U3A Meadowbank – Beginnings/Getting started. Who were the ‘movers and shakers’- Key people who made it happen. The first ten years Management of U3A Meadowbank Presidents and their role (Plus committee members) Monthly Meetings and speakers Key developments and issues over time U3A Meadowbank groups Stories from a selection of groups Individual stories Plans for the 10 year celebrations The future – where to now? The last word (Lou Holder President elect 2011) References Appendices Appendix one - U3A groups in the Auckland region Appendix two - U3A Meadowbank study/interest groups Appendix three - Peter Laslett’s principles FROM THE PRESIDENT This booklet has been produced to document and celebrate the 10th anniversary of U3A Meadowbank. I would like to congratulate that handful of people who established our U3A for people who could not be accommodated in the existing Auckland U3As of Remuera, Howick and St Heliers. With a great vision, with energy and enthusiasm, they created a dedicated community of learners that grew from modest beginnings to become one of the most successful U3As in New Zealand over the past ten years. Reaching the important milestone of the 10th anniversary, gives us an opportunity to look back, take stock and plan for the future. -
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. -
To View an Individual Route Map, Click on the Route Number
Ngataringa Bayswater PROPOSED SERVICES Bay KEY SYMBOLS FREQUENT SERVICES LOCAL SERVICES PEAK PERIOD SERVICES Little Shoal Station or key connection point Birkenhead Bay Northwestern Northwest to Britomart via Crosstown 6a Crosstown 6 extension to 101 Pt Chevalier to Auckland University services Northwestern Motorway and Selwyn Village via Jervois Rd Northcote Cheltenham Rail Line Great North Rd To viewNorthcote an individualPoint route map, click on the route number (Passenger Service) Titirangi to Britomart via 106 Freemans Bay to Britomart Loop 209 Beach North Shore Northern Express routes New North Rd and Blockhouse Bay Stanley Waitemata service Train Station NX1, NX2 and NX3 138 Henderson to New Lynn via Mangere Town Centre to Ferries to Northcote, Point Harbour City LINK - Wynyard Quarter to Avondale Peninsula Wynyard Quarter via Favona, Auckland Harbour Birkenhead, West Harbour, North City Link 309X Bridge Beach Haven and Karangahape Rd via Queen St 187 Lynfield to New Lynn via Mangere Bridge, Queenstown Rd Ferries to West Harbour, Hobsonville Head Ferry Terminal Beach Haven and Stanley Bay (see City Centre map) Blockhouse Bay and Pah Rd (non stop Hobsonville Services in this Inner LINK - Inner loop via Parnell, Greenwoods Corner to Newmarket) Services to 191 New Lynn to Blockhouse Bay via North Shore - direction only Inner Link Newmarket, Karangahape Rd, Avondale Peninsula and Whitney St Panmure to Wynyard Quarter via Ferry to 701 Lunn Ave and Remuera Rd not part of this Ponsonby and Victoria Park 296 Bayswater Devonport Onehunga -
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 ............................................................................................................................ -
List of Office Bearers 2004
Parnell Cricket Club Incorporated - Established 1858 ANNUAL REPORT, ACCOUNTS and BALANCE SHEET End of an Era Farewell to • David Goddard Premier XI from 2008/9, Captain from 2014/15. He scored 2363 runs, took 232 wickets and held 85 catches • Ian Trott Head Coach, including Coach of Mens’ Premier XI, from 2007/8. ACA’s Coach of the Year 2007/8 and 2014/15. • Michael Ravlic Premier player from 2011/12 taking 315 wickets, including 85 in the 2012/13 Season - a Club all time record In this Era – from 2007/8, Parnell CC’s Mens’ Premier Grade XI won the: • 2007/8 and 2010/11 Tom Hellaby Cup, Minor Tier Championship and promotion to Major Tier for 2008/9 and 2011/12 • 2009/10 and 2012/13 Jeff Crowe Cup, Limited Overs Championship – also Finalist 2010/11 and 2013/14 • 2013/14, 2015/16 and 2016/17 Allan Thompson Memorial Trophy – Runner-up in the Major 2 Day Championship • 2014/15 Hedley Howarth Trophy - Two Day Major Championship And, on the recommendation of the Auckland Umpires, was awarded Auckland Cricket’s • 2009/10, 2012/13, 2014/15 and 2017/18 Spirit of Cricket Award – (inaugural winner in 2009/10) • 2015/16 and 2017/18 Grosvenor Cup – the “best all round Premier Grade team”. Thank you David, Ian and Michael for your outstanding contributions to Parnell CC - all at the Club wish you well for the future. 2017 – 2018 : 160th Season 1. 160 Years From 1857/58 to 2017/18 and to ……….. Mid March the Club celebrated it’s 160th Jubilee.