Cit Holdings Limited in Relation to Topic 019 Outstanding Natural Feature Overlay
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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. -
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. -
Newsletterauckland Manukau Eastern Transport Initiative
Capturing Panmure’s past About the AMETI transport projects As AMETI progresses and the Panmure area is transformed, we take a look back at the history The Auckland Manukau Eastern Transport Initiative (AMETI) is a group of transport projects of one of Auckland’s first settlements….. for the south east (Panmure, Mt Wellington, Pakuranga, Howick and Botany). Key North south road NewsletterAuckland Manukau Eastern Transport Initiative. AMETI October 2013 Phase 1 Panmure Merton Rd extension l North/South Rd l New Panmure Station A p i The University of r Auckland a n Phase 2 Panmure to Pakuranga a Makeover for historic lagoon A l New Panmure Intersection Quarry v e l Busway Lagoon Dr & Pakuranga Rd Stonefields Link Rd l New Panmure Bridge Work gets underway on a major makeover for a forgotten corner of Panmure. M l New Reeves Rd Flyover orr i n R d A forgotten and neglected historic corner of Panmure Watercare is also carrying out a stormwater Future developments is getting a major makeover as part of one of Auckland’s pipe upgrade. South Eastern Connections biggest transport projects. Study Just off Mt Wellington Highway, Van Damme’s Lagoon New north-south road Pillkington Rd H obson Work is underway on upgrading and has been through a number of changes in its history. Panmure Station St s new bus/rail D re unn C revitalising Van Damme’s Lagoon and reserve Rd es interchange Mo Coat un (story continues on page three) ta in Gre as part of AMETI. E R en Rd llersl d ie Pan mu re Jellicoe Rd Hwy Pleas New Panmure ant V Mt Wellington iew Mt Wellington intersection Shopping Centre Panmure to Pakuranga y Ellerslie-Panmure Highway Bridge opens w d Major milestone – R north side busway H and Panmure n el L o r a t I g o o lling e n W D In 1841, the government purchased what was then known More than 2500 men, women and children arrived in t r M as the Kohimarama block from Ngati Paoa. -
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. -
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. -
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. -
Otahuhu Historic Heritage Survey
OTAHUHU HISTORIC HERITAGE SURVEY Overview Report PREPARED FOR AUCKLAND COUNCIL BY MATTHEWS & MATTHEWS ARCHITECTS LTD IN ASSOCIATION WITH LYN WILLIAMS LISA TRUTTMAN BRUCE W HAYWARD CLOUGH & ASSOCIATES LTD JP ADAM RA SKIDMORE URBAN DESIGN LTD FINAL August 2014 OTAHUHU HISTORIC HERITAGE SURVEY 2013 Contents 1.0 INTRODUCTION .................................................................................................. 4 1.1 Brief .................................................................................................................. 4 1.2 The Study area ................................................................................................. 5 1.3 Methodology and Approach .............................................................................. 5 1.4 Acknowledgements ........................................................................................... 5 1.5 Overview of report structure and component parts ........................................... 7 2.0 ŌTĀHUHU STUDY AREA-SUMMARY OF HISTORIC HERITAGE ISSUES ....... 9 2.1 Built Heritage Overview and recommendations ................................................ 9 2.2 Overview and recommendations in relation to geology .................................. 12 2.3 Overview and recommendations in relation to archaeology ........................... 13 2.4 Overview and recommendations Landscape History ...................................... 13 2.5 Overview and recommendations related to Maori Ancestral Relationships and issues identified. .................................................................................................. -
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 ............................................................................................................................ -
Ōrākei Local Board Open Space Network Plan
Ōrākei Local Board Open Space Network Plan September 2019 1 Cover image – view over a section of the Pourewa Creek (source, Flickr). 2 Table of Contents EXECUTIVE SUMMARY SECTION 1 - THE ŌRĀKEI OPEN SPACE NETWORK ................................................................................... Section 1 introduces the Ōrākei local board area and investigates the current state of the open space network plan. 1.1 Purpose of the network plan ............................................................................................. 5 1.2 Ōrākei Local Board area ................................................................................................... 5 1.3 Strategic context ............................................................................................................... 7 1.4 Current state ..................................................................................................................... 8 Treasure .................................................................................................................. 8 Enjoy ..................................................................................................................... 16 Connect ................................................................................................................. 22 Utilise ..................................................................................................................... 23 SECTION 2 – KEY MOVES ............................................................................................................................... -
Part 2 Present and Future Trends
PART 2 - CONTENTS PART 2 PRESENT AND FUTURE TRENDS 2.1 THE FORM OF HOWICK 2.2 GROWTH OF HOWICK 2.3 ETHNIC ORIGIN OF POPULATION 2.4 EMPLOYMENT 2.5 DWELLINGS AND RESIDENTIAL BUILDING 2.6 CONTEXT OF THE PLANNING SCHEME HOWICK THIRD REVIEW PART 2 - PRESENT AND FUTURE TRENDS 2.1 THE FORM OF HOWICK 111 Howick settlement has existed since 1847 and is today a well established residential suburb. It is located on the shores of the Hauraki Gulf, approximately eleven kilometres north of Manukau City Centre, at the perimeter of the urban area. The Hutchinson Road and Bradbury Road ridges define the western boundary of the district. Continuing from the latter ridge is the topographical backbone of Howick, the ridge which the main road follows, with its high points at Stockade Hill and Minerva Terrace. On the seaward side, a series of ridges and valleys slope toward the cost. A number of these are marked by streams with considerable tree cover. On the landward side, the main ridge forms a basin with a southward orientation which drains to the Tamaki River. The hilly topography has had a strong effect on the roading network with many roads following the ridges. It also means that most parts of the District can enjoy views either of the sea, the countryside or of a suburban landscape. Three major factors have made Howick an attractive residential location. First, the considerable length of north-east facing coastline and beaches backed by sloping land with extensive views to the islands of the gulf.