Boffa Miskell Report – Wellington City Landscape Evaluation (June 2019)
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Explore Wellington
EXPLORE Old Coach Rd 1 Makara Peak Mountain Bike Park This dual use track runs North SKYLINE and South along the ridge MAORI HISTORY AND KEY Wellington City Council set aside 200 TRACK between Old Coach Road in SIGNIFICANCE OUTER GREEN START/FINISH hectares of retired farmland South- EXPLORE Johnsonville and Makara Saddle BELT Carmichael St West of the city for a mountain bike in Karori. park in 1998. Volunteers immediately While European settlers named parts of the skyline, SKYLINE TRACK most of the central ridge was known to local Maori began development of the Makara Allow up to five hours to traverse 12kms of Wellington’s ridge tops 2 as Te Wharangi (broad open space). This ridge was Peak Mountain Bike Park by planting WELLINGTON following the Outer Green Belt onto Mt Kaukau, the Crow’s Nest, NORTHERN Truscott Ave not inhabited by Maori, but they traversed frequently trees and cutting new tracks. In the Discover Wellington’s Town Belt, reserves and walkways Kilmister Tops and Johnston Hill. Take time to indulge in the stunning WALKWAY Reserve and by foot when moving between Te Whanganui-a- Johnsonville Park first year, six tracks were built and rural, city and coastal views along the way. On a clear day, views of Tara and Owhariu. EXISTING TRACK 14,000 native seedlings planted. the Kaikoura ranges, the Marlborough Sounds, Wellington city and John Sims Dr Nalanda Cres A significant effort was also put into MT KAUKAU 3 dleiferooM dR harbour, and the Tararua and Orongorongo ranges will take your The Old Maori Trail runs from Makara Beach all the 1 9 POINTS OF controlling possums and goats, breath away. -
Modeling Site Effects in the Lower Hutt Valley, New Zealand
2694 MODELING SITE EFFECTS IN THE LOWER HUTT VALLEY, NEW ZEALAND Brian M ADAMS1, John B BERRILL2, Rob O DAVIS3 And John J TABER4 SUMMARY Lower Hutt City lies atop a wedge of Quaternary sediments forming a long alluvial valley. On its western edge the sediments butt up against the near vertical wall of the potentially active Wellington Fault, capable of an earthquake of moment magnitude 7.6. A two-dimensional linear finite-element method has been used to model the propagation of antiplane SH waves within the soft sediments and surrounding bedrock. The technique has proved to be an efficient and accurate means of modeling fine geological detail. Two detailed geological cross-sections through the Lower Hutt were modeled to gain an overall impression of the valley's seismic behaviour. It was found that horizontally propagating surface waves, generated at the valley edges, are the cause of significant amplification. The aptly named basin-edge effect – speculated to be the cause of a belt of severe shaking during the 1995 Kobe earthquake – is observed in the simulation results, occuring some 70-200 metres out from the fault. Fourier spectral ratios across the valley indicate a behaviour dominated by two-dimensional resonance, and compare favourably in magnitude with previously collected weak motion data. Certain resonant frequencies within the range 0.3-2.5 hertz are amplified up to 14 times that for nearby outcropping bedrock. Results are likely to be conservative due to the linear modeling, yet exclude fault-rupture effects due to the teleseismic nature of the input scheme. INTRODUCTION In this paper we describe our use of a two-dimensional finite-element numerical scheme to simulate ground motions from earthquake shaking in the soft sediments in-filling the Lower Hutt Valley. -
Wellington Harbour Sub-Region
Air, land and water in the Wellington region – state and trends Wellington Harbour sub-region This is a summary of the key findings from State of the Environment Key points monitoring we carry out in the Wellington Harbour and south coast • Air quality is very good overall, except catchments. It is one of five sub-region summaries of eight technical during winter in some residential areas reports which give the full picture of the health of the Wellington on cold and calm evenings – when fine region’s air, land and water resources. These reports are produced particles produced by woodburners don’t every five years. disperse The findings are being fed into the current review of Greater • The quality of the groundwater is very Wellington’s regional plans – the ‘rule books’ for ensuring our high region’s natural resources are sustainably managed. • Most of the freshwater used in the sub- region goes to public water supply – You can find out how to have a say in our regional plan review on there’s very little water left to allocate from the back page. the major rivers or groundwater aquifers Key features • River and stream health is excellent at sites This sub-region is home to most of the people living in the Wellington near the ranges but is degraded further region – although it only makes up 14% of the region’s land area downstream, especially in urban areas (1,183km2). It covers Wellington, Upper Hutt and Hutt cities, and also • Most beach and river recreation sites we the Wainuiomata Valley and Wellington’s south coast. -
Wellington Regional TRAILS for the FUTURE a Strategic Framework for Trails in the Wellington Region
Wellington Regional TRAILS FOR THE FUTURE A strategic framework for trails in the Wellington Region September 2017 Acknowledgements The Wellington Regional Trails Framework has been prepared by TRC Tourism Ltd (www.trctourism.com) for the government authorities and trails partners of the Wellington Region. The assistance of the working group and all stakeholders who contributed is greatly appreciated. Authors: Janet Mackay, Chris Rose. Cover photo credit: Erica Herron ISBN: 978-0-947521-06-6 Disclaimer Any representation, statement, opinion or advice expressed or implied in this document is made in good faith, but on the basis that TRC Tourism is not liable to any person for any damage or loss whatsoever that has occurred or may occur in relation to that person taking or not taking action in respect of any representation, statement or advice referred to in this document. Wellington Regional TRAILS FOR THE FUTURE A strategic framework for trails in the Wellington Region ii Wellington Regional Trails for the Future Executive Summary Introduction The Wellington region sits on the southern end of New Zealand’s North Island and contains some outstanding trail-based experiences and the potential to significantly grow the use of outdoor trails. Many other destinations internationally are growing their trail-based tourism infrastructure, marketing, and cooperative efforts to capitalise on their region’s strengths in order to offer world class experiences. The Wellington region has the potential to be such a destination, adding to its already very successful positioning as a capital city with a great cultural scene based on Te Papa and other assets and events, and a thriving food, wine and craft beer scene. -
Wellington Walks – Ara Rēhia O Pōneke Is Your Guide to Some of the Short Walks, Loop Walks and Walkways in Our City
Detail map: Te Ahumairangi (Tinakori Hill) Detail map: Mount Victoria (Matairangi) Tracks are good quality but can be steep in places. Tracks are good quality but can be steep in places. ade North North Wellington Otari-Wilton’ss BushBush OrientalOriental ParadePar W ADESTOWN WeldWeld Street Street Wade Street Oriental Bay Walks Grass St. WILTON Oriental Parade O RIEN T A L B A Y Ara Rēhia o Pōneke Northern Walkway PalliserPalliser Rd.Rd. Skyline Walkway To City ROSENEATH Majoribanks Street City to Sea Walkway LookoutLookout Rd.Rd. Te Ara o Ngā Tūpuna Mount Victoria Lookout MOUNT (Tangi(Tangi TeTe Keo)Keo) Te Ahumairangi Hill GrantGrant RoadRoad VICT ORIA Lookout PoplarPoplar GGroroveve PiriePirie St.St. THORNDON AlexandraAlexandra RoadRoad Hobbit Hideaway The Beehive Film Location TinakoriTinakori RoadRoad & ParliameParliamentnt rangi Kaupapa RoadStSt Mary’sMary’s StreetStreet OOrangi Kaupapa Road buildingsbuildings WaitoaWaitoa Rd.Rd. HataitaiHataitai RoadHRoadATAITAI Welellingtonlington BotanicBotanic GardenGarden A B Southern Walkway Loop walks City to Sea Walkway Matairangi Nature Trail Lookout Walkway Northern Walkway Other tracks Southern Walkway Hataitai to City Walkway 00 130130 260260 520520 Te Ahumairangi metresmetres Be prepared For more information Your safety is your responsibility. Before you go, Find our handy webmap to navigate on your mobile at remember these five simple rules: wcc.govt.nz/trailmaps. This map is available in English and Te Reo Māori. 1. Plan your trip. Our tracks are clearly marked but it’s a good idea to check our website for maps and track details. Find detailed track descriptions, maps and the Welly Walks app at wcc.govt.nz/walks 2. Tell someone where you’re going. -
Hydrodynamic Inundation Modelling for Wellington Harbour, 2015
DISCLAIMER This report has been prepared by the Institute of Geological and Nuclear Sciences Limited (GNS Science) exclusively for and under contract to the Wellington Region Emergency Management Office and the Greater Wellington Regional Council. Unless otherwise agreed in writing by GNS Science, GNS Science accepts no responsibility for any use of, or reliance on any contents of this Report by any person other than the Wellington Region Emergency Management Office and the Greater Wellington Regional Council and shall not be liable to any person other than the Wellington Region Emergency Management Office and the Greater Wellington Regional Council, on any ground, for any loss, damage or expense arising from such use or reliance. Use of Data: Date that GNS Science can use associated data: October 2015 Wellington Harbour Bathymetry disclaimer: This report publishes results that are reliant on the 1m grid Wellington Harbour Bathymetric data set (‘the Data’) provided by the National Institute for Water and Atmospheric Research (NIWA). GNS Science and NIWA make no representations or warranties regarding the accuracy or completeness of ‘the Data’ the use to which ‘the Data’ has been put in this report, or the results in this report which have been obtained from using the Data. GNS Science and NIWA accept no liability for any loss or damage (whether direct or indirect) incurred by any person through the use of or reliance on ‘the Data’ or use or reliance on the results in this report which have been obtained from using the Data. BIBLIOGRAPHIC REFERENCE Mueller, C.; Power, W.L.; Wang, X. 2015. -
NZL FM List in Regional Order Oct19.Xlsx
NEW ZEALAND FM LISTING IN REGION ORDER to 1 October 2019 Copyright NZRDXL 2017-2019 Full-time broadcasters plus their LPFM relays (other LPFM operators excluded) Changes after 2020 WRTH Deadline are in RED WRTH MHz City Station kW Region Owner/Group Notes Address 88.6 Auckland Mai FM 10 Auckland MediaWorks 89.4 Auckland Newstalk ZB Auckland NZME 90.2 Auckland The Rock Auckland MediaWorks 90.6 Waiheke Island Chinese R 90.6FM 1.6 Auckland Independent 18 91.0 Auckland ZM 50 Auckland NZME 91.8 Auckland More FM Auckland MediaWorks 92.6 Auckland RNZ Concert 50 Auckland RNZ Skytower 92.9 Orewa The Sound Auckland MediaWorks Moirs Hill. Ex Radio Live 93.4 Auckland The Breeze Auckland MediaWorks 5 93.8 Auckland The Sound Auckland MediaWorks 94.2 Auckland The Edge Auckland MediaWorks 95.0 Auckland 95bFM 12.6 Auckland Student 6 95.8 Auckland Flava Auckland NZME 34 96.6 Auckland George Auckland MediaWorks 97.4 Auckland The Hits Auckland NZME 10 98.2 Auckland Mix 50 Auckland NZME 5 99.0 Auckland Radio Hauraki Auckland NZME 99.4 Auckland Chinese R. FM99.4 1.6 Auckland Independent 21 99.8 Auckland Life FM Auckland Rhema 100.6 Auckland Magic Music Auckland MediaWorks ex Radio Live 101.4 Auckland RNZ National 10 Auckland RNZ Skytower 102.2 Auckland OnRoute FM Auckland Independent Low power NZTA Trial till September 2017 103.8 Auckland Niu FM 15.8 Auckland Pacific Media 104.2 Auckland Chinese Radio FM104.2 3 Auckland Independent 104.6 Auckland Planet FM 15.8 Auckland Access 105.4 Auckland Coast 50 Auckland NZME 29 106.2 Auckland Humm FM 10 Auckland Independent -
Mana Island Ecological Restoration Plan
6. Restoration of non-forest communities While restoring forest cover to Mana Island is one of the key steps in the restoration programme, restoring forest to most or all of the island would jeopardise the survival of several resident threatened animal and plant species, and reduce the habitat available for some of the threatened animal and plant species proposed for translocation. Cook Strait giant weta are widely regarded as preferring low-growing shrubs and forest margins to the forest interior (Meads 1990), and since removal of stock and mice from Mana Island, giant weta have become abundant throughout the rank pasture. Giant weta are not found in the interior of the forest remnant on Mana Island, and it is likely that their numbers will decline on the island as the forest cover returns. Both of the threatened lizard species resident on Mana Island (McGregor's skink and goldstripe gecko) occur in non-forest habitats on the island. It is expected that both will spread into forest habitats, but possibly at lower densities to where they currently occur in coastal shrublands and flax respectively. Many animal species proposed in this Restoration Plan for translocation to Mana Island prefer or require non-forest habitats: grassland (takahe, snipe, spotted skink), wetlands (brown teal, banded rail, fernbird), flax (flax weevil), shrublands (rock wren) or herbfields (speargrass weevil). Four of the five threatened plant species that survived on Mana Island occur in non- forest communities (Cook's scurvy grass, Melicytus obovatus, rengarenga, Jersey fern), and most of the threatened plants identified as suitable for planting on the island occur in coastal shrublands and herbfields rather than forest. -
Wellington Harbour Ferry
Effective from 15 July 2018 Wellington Harbour Ferry Queens Wharf Matiu / Somes Island Wharf Seatoun Wharf Thanks for travelling with Metlink. Days Bay Wharf Connect with Metlink for timetables and information about bus, train and ferry services in the Wellington region. metlink.org.nz 0800 801 700 [email protected] Printed with mineral-oil-free, soy-based vegetable inks on paper produced using Forestry Stewardship Council® (FSC®) certified mixed-source pulp that complies with environmentally responsible practices and principles. Please recycle and reuse if possible. Before taking a printed timetable, check our timetables online or use the Metlink commuter app. GW/PT-G-18/92 July 2018 July GW/PT-G-18/92 TO DAYS BAY WHARF MONDAY TO FRIDAY FARES FARE INFORMATION Stops AM PM 9997 Queens Wharf 6:20 6:45 7:15 7:40 8:20 8:55 10:00 12:00 2:05 3:30 4:30 5:00 5:30 5:55 6:30 7:05 Child fares: 9995 Seatoun Wharf 4:00 6:15 ONE WAY TICKET Adult Child – are half the adult fares for the equivalent journeys Matiu / Somes Island 10:25 12:25 2:30 9998 Queens Wharf - Days Bay $12.00 $6.00 on ferry sailings 9999 Days Bay Wharf 6:45 7:10 7:40 8:05 8:45 9:20 10:40 12:40 2:45 4:25 4:55 5:25 5:55 6:40 6:55 7:30 Days Bay - Seatoun $12.00 $6.00 – apply to all school children SI SI SI Queens Wharf - Seatoun $12.00 $6.00 – secondary school students must be in school uniform or present valid school photo ID, RETURN TICKET Adult Child if requested TO QUEENS WHARF – passengers entitled to the Accessible Concession MONDAY TO FRIDAY Queens Wharf - Days Bay $24.00 $12.00 -
Wellington City Council Quarterly Report
Wellington City Council Quarterly Report January – March 2008 9835 PDWCC6 A message from the Chief Executive Wellington City Council Quarterly Report – January to March 2008 In March Wellington City Councillors approved the 2008/09 Draft Annual Plan – the first since the Council signed up to its vision of a carbon-neutral Wellington. Carbon neutrality is an ambitious vision that will require significant effort by the Council, central government, businesses and residents. This year's draft plan includes initiatives that if approved, will be small but potentially significant steps towards achieving our goal. One proposal is to generate electricity or LPG from sewage sludge at the Southern Landfill using a bioreactor. In this quarter we established a Climate Change Office to provide a focus for the Council's work on reducing corporate and community greenhouse gas emissions and working toward the goal of carbon neutrality. Early projects for the team include developing a robust methodology for measuring corporate emissions, establishing carbon sinks on Council reserve land using the Government’s Permanent Forest Sink Initiative (PFSI) mechanism, developing sustainable vehicle and green building standards, and supporting the World Environment Day. Other key highlights for the third quarter included: Supporting two major bike events: the Go By Bike Day which saw almost 900 cyclists gathered in Civic Square to enjoy a free breakfast and entertainment; and Bike the Bays which was supported by 1525 cyclists. Supporting successful Waitangi Day celebrations at Waitangi Park and the inaugural Absolutely Pasifika Festival at Frank Kitts Park. Opening the new water play and hydrotherapy services facilities at the Wellington Regional Aquatic Centre. -
Distribution of Geological Materials in Lower Hutt and Porirua, New Zealand a Component of a Ground Shaking Hazard Assessment
332 DISTRIBUTION OF GEOLOGICAL MATERIALS IN LOWER HUTT AND PORIRUA, NEW ZEALAND A COMPONENT OF A GROUND SHAKING HAZARD ASSESSMENT G. D. Dellow1 , S. A. L. Read 1 , J. G. Begg1 , R. J. Van Dissen1 , N. D. Perrin1 ABSTRACT Geological materials in the Lower Hutt, Eastbourne, Wainuiomata, and Porirua urban areas are mapped and described as part of a multi-disciplinary assessment of seismic ground shaking hazards. Emphasis is mainly on the flat-lying parts of these areas which are underlain by variable Quaternary-age sediments that overlie Permian-Mesowic age 'greywacke' bedrock. Within the Quaternary-age sediments, the two material types recognised on strength characteristics are: 1) Soft sediments, typically composed of normally consolidated, fine-grained materials (sand, silt and clay), with typical standard penetration values (SPT) of <20 blows/300 mm; and 2) Loose to compact coarser-grained materials (sand, gravel), with SPT values of > 20 blows/ 300 mm. The total thickness and nature of Quaternary-age sediments in the study areas is described, with particular emphasis on the thickness and geotechnical properties of near-surface sediments. Such sediments are considered likely to have a significant influence on the an1plification and attenuation of ground shaking intensity during earthquakes. In the Lower Hutt valley, near-surface soft sediments greater than 10 m thick have an areal extent of -16 kni. Such soft sediments underlie much of Petone and the Lower Hutt urban and city centres, and have a maximum known thickness of 27 m near the western end of the Petone foreshore. In the Wainuiomata area, near-surface soft sediments greater than 10 m thick have an areal extent of - 3 krn2, and attain a maximum thickness of 32 m. -
Wellington City Council Quarterly Report
Wellington City Council Quarterly Report October – December 2007 PDWCC67154 A message from the Chief Executive Wellington City Council Quarterly Report – October to December 2007 The lead up to Christmas was a busy time for Wellington City. This quarter included the Local Body Elections, the inauguration of the new Council, high-profile events, and the Council achieving a number of significant milestones. With regard to the environment and sustainability, the Council: • furthered its commitment to making Wellington a carbon-neutral city by presenting a draft Climate Change Action Plan • became one of the first councils in the country to take part in the Government’s public place recycling initiative. Recycling bins are being placed in locations around central Wellington. The Convention Centre also became the first venue of its kind to achieve the ISO 14001 environmental standard. Projects and programmes progressed this quarter included the completion of Cog Park and the opening of the Mount Victoria lookout by the Mayor. Consultation was undertaken on key projects, including the design of the Indoor Community Sports Centre and the upgrade plans for Central Park. The summer calendar of events kicked off in style with the arrival of the LA Galaxy football team and its star player David Beckham. Around 15,000 people, including school children, attended the training session and a crowd of 35,000 watched the match against the Wellington Phoenix. The Pelorus Trust Sky show also attracted a large crowd for the annual fireworks display and families celebrated the start of the festive season with the annual Farmers Santa Parade. This Quarterly Report provides an update on the Council’s consolidated financial performance for the year to date and sets out operational and financial progress towards delivering the outcomes and activities approved in the Council’s Annual Plan.