Annexure a to Procedural Minute 6
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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). -
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 -
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. -
Minutes of Howick Local Board
Howick Local Board OPEN MINUTES Minutes of a meeting of the Howick Local Board held in the Howick Local Board Meeting Room, Pakuranga Library Complex, 7 Aylesbury Street, Pakuranga on Monday, 16 August 2021 at 6.00pm. PRESENT Chairperson Adele White Deputy Chairperson John Spiller Members Katrina Bungard David Collings Bruce Kendall Mike Turinsky Bob Wichman Peter Young, JP ABSENT Member Bo Burns With apology Howick Local Board 16 August 2021 1 Welcome The Chair opened the meeting and welcomed those present. 2 Apologies Resolution number HW/2021/119 MOVED by Member B Wichman, seconded by Deputy Chairperson J Spiller: That the Howick Local Board: a) accept the apology from Member B Burns for absence. CARRIED 3 Declaration of Interest There were no declarations of interest. 4 Confirmation of Minutes Resolution number HW/2021/120 MOVED by Chairperson A White, seconded by Member B Wichman: That the Howick Local Board: a) confirm the ordinary minutes of its meeting, held on Monday, 19 July 2021, as a true and correct record. CARRIED 5 Leave of Absence There were no leaves of absence. 6 Acknowledgements The Chair acknowledged the Howick Youth Council and read the following acknowledgement: I wish to acknowledge the ongoing success of the Howick Youth Council as they celebrate their ten year anniversary. These multi-talented young people work on a voluntary basis, to bring together, mentor, inform and support the youth of the Howick ward whilst growing themselves to be confident and capable leaders. I congratulate Howick Youth Council – past and present. We know our community will be in great hands in the years to come. -
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. -
Hidden Eruptions
HIDDEN ERUPTIONS The Search for AUCKLAND’S VOLCANIC PAST FACT SHEET 02 Fun volcanic facts from the DEtermining VOlcanic Risk in Auckland (DEVORA) Project The Auckland region has a long history of being affected by volcanic eruptions. The region has experienced at least 53 eruptions from the Auckland Volcanic Field (AVF) in the past 200,000 years, and it has been covered by ash from central North Island volcanoes at least 300 times during that period. To determine exactly how often the Auckland region has been affected by eruptions, scientists study ash layers that have been preserved in lake beds. They now think that ash has How can we tell where fallen on Auckland at least once every 600 years! ash layers come from? Scientists have drilled 7 lakes and dried-up lakes looking for ash: Colour /Te Kopua Kai a Hiku, Panmure Basin A white layer = Ash from a larger, more , Pukaki Lagoon, What is volcanic ash? Lake Pupuke /Whakamuhu, distant volcano (e.g. Taupo). Ōrākei Basin, Glover Park When volcanoes erupt, they eject small fragments /Te Hopua a Rangi, and Gloucester Park A black layer = Ash from a smaller, local of broken rock and lava into the air. This material /Te Kopua o Matakerepō. Auckland volcano (e.g. Mt. Wellington). is called tephra. Tephra less than 2mm in size is Onepoto Basin called ash. Ash is so small and light that it is easily picked up and carried by the wind. Ash can travel Location in the core hundreds of kilometres before settling out of the Some large-scale volcanic eruptions are ash cloud and falling to the ground. -
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. -
Auckland Progress Results
Progress Result Issue: Mayor (1) Date: 09/10/2010 Auckland Council Time: 12:23:00 Candidate Affiliation Candidate No Votes Received Rank AUSTIN, Aileen Independent 101 1552 BANKS, John Independent 102 161167 BARR, Marlene Independent 103 692 BRIGHT, Penny 104 2529 BROWN, Len Independent 105 2213651 CHAPMAN, Hugh Independent 106 1878 CRAIG, Colin Independent 107 40483 DAVE, Nga Independent 108 840 FONG, Harry Independent 109 1434 GILLIES, Shannon 110 467 KAHUI, Vinnie 111 1120 MCCULLOCH, Alan Independent 112 1520 MCDONALD, Steve Independent 113 643 NEESON, Vanessa Independent 115 2885 O'CONNOR, Phil Christians Against Abortion 116 1209 PRAST, Simon Independent 117 3578 PRESLAND, Raymond 118 278 ROSS, Mark Independent 119 3076 VERMUNT, Annalucia Communist League 120 427 WILLIAMS, Andrew Independent Progressive Leadership 121 3813 WILLMOTT, David Roads First 122 519 YOUNG, Wayne 123 553 INFORMAL 124 1261 BLANK 125 3752 Progress Result Issue: Rodney Ward (1) Date: 09/10/2010 Auckland Council Time: 12:23:00 Candidate Affiliation Candidate No Votes Received Rank ASHTON, Tom Independent 201 3941 PEREIRA, Vincent Independent 202 444 ROSE, Christine 203 5553 WEBSTER, Penny Independent 204 8063 1 INFORMAL 205 21 BLANK 206 701 Progress Result Issue: Albany Ward (2) Date: 09/10/2010 Auckland Council Time: 12:23:00 Candidate Affiliation Candidate No Votes Received Rank BALOUCH, Uzra Independent 221 736 BELL, Rodney Independent 222 3151 BRADLEY, Ian Independent 223 5273 CONDER, Laurie Independent 224 1419 COOPER, David Independent 225 2821 COOPER, -
Towards Characterising Rhyolitic Tephra Layers from New
Aberystwyth University Towards characterising rhyolitic tephra layers from New Zealand with rapid, non-destructive -XRF core scanning Peti, Leonie; Augustinus, Paul C.; Gadd, Patricia S.; Davies, Sarah Published in: Quaternary International DOI: 10.1016/j.quaint.2018.06.039 Publication date: 2019 Citation for published version (APA): Peti, L., Augustinus, P. C., Gadd, P. S., & Davies, S. (2019). Towards characterising rhyolitic tephra layers from New Zealand with rapid, non-destructive -XRF core scanning. Quaternary International, 514, 161-172. https://doi.org/10.1016/j.quaint.2018.06.039 General rights Copyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the Aberystwyth Research Portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. tel: +44 1970 62 2400 email: [email protected] Download date: 11. Oct. 2021 Accepted Manuscript Towards characterising rhyolitic tephra layers from New Zealand with rapid, non- destructive μ-XRF core scanning Leonie Peti, Paul C. Augustinus, Patricia S. -
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.