Mahere-Ā-Tau 2020/21 Annual Plan 2020/21

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Mahere-Ā-Tau 2020/21 Annual Plan 2020/21 Mahere-ā-Tau 2020/21 Annual Plan 2020/21 WHAT GREATER WELLINGTON DOES IN OUR REGION Greater Wellington has a role as an environmental protection organisation for our region. Greater Wellington has another role as the owner of Metlink, the organisation that delivers public transport across the region. Now, these might seem like incompatible roles but that’s not necessarily the case. More people using public transport, means fewer cars on the road, means less pollution and a cleaner environment. Further down, you’ll find more information about what Greater Wellington does across the region. WHAT GREATER WELLINGTON IS DOING IN THE HUTT VALLEY We’re continuing to work on We’re upgrading the Hutt Restoring the lower the RiverLink project Valley Line through the Future Kilmister block in Rail project Belmont Regional Park RiverLink is one of Greater Wellington’s major projects. It’s being delivered in We know how frustrating it can be when Located in the hills between Porirua collaboration by Greater Wellington, there are delays on the Hutt Valley and Hutt Valley, Belmont Regional Park Hutt City Council and the New Zealand railway line during peak times. contains much of the headwaters of the Transport Agency to achieve some big western side of the valley. improvements for Lower Hutt. To reduce these delays and allow more people to travel on the trains in the The Kilmister block within Belmont RiverLink will make Hutt City safer from future, KiwiRail and Greater Wellington Regional Park has been grazed under severe floods, help the city develop are working together to upgrade the licence for many years. Council has and improve transport connections Hutt Valley Line through the Future Rail signalled its intention to phase out between the city centre and the project. Work includes double tracking grazing activities and as part of this Wellington region. the railway line between Trentham and work is underway to revegetate the Upper Hutt stations, station upgrade lower Kilmister block with native plants. In 2020/21 Greater Wellington will work at Trentham and Wallaceville and continue its work on Hutt river flood a new overhead power system. Over time this work will see ecosystem protection. We’ll focus on progressing health restored in this area of Belmont development of the design and Park. lodgement of resource consents for the RiverLink project. How did we calculate your 2020/21 rates? After reviewing our work programme and Your individual rate demand may differ from budgets for 2020/21 in light of the current the figures above as they are an average across COVID-19 pandemic, Council adopted an the whole region. Each area within the region average rates increase of three percent, has a different set of inputs on which your rates across the region. are calculated. What this means is that your rates bill is likely to differ from that of your This equates to approximately an average of neighbour’s and your neighbouring areas. $0.21 (incl. GST) and $1.18 (excl. GST) increase per For a more personalised estimate of your week for the residential and business ratepayer 2020/21 rates please check out our rates respectively and an average decrease of $0.18 calculator at rates.gw.govt.nz (excl. GST) for the rural ratepayer region-wide. What do your rates pay for? 10% 52% 21% 13% 4% Regional Leadership Public Transport Environment Flood Protection and Regional Parks Control Works and Forests How do rates contribute to Greater Wellington’s overall income? General Rates 11% Other operating revenue 25% Targeted rates 19% Interest and dividends 1% 2% Transport improvement grants 7% Water supply levy 35% Government subsidies Rates Change in Change in Hutt Valley 2020/21 amount per annum amount per week Residential Hutt City $670.15 $14.04 higher $0.27 higher (incl. GST) Upper Hutt City $584.51 $27.84 higher $0.54 higher Business Hutt City $2,167.61 $45.96 higher $0.88 higher (excl. GST) Upper Hutt City $1,877.35 $140.38 lower $2.70 lower Rural Hutt City $529.60 $3.57 higher $0.07 higher (excl. GST) Upper Hutt City $455.35 $14.57 lower $0.28 lower Here are some of the activities that Greater Wellington will be doing across the region. Finalising and Implementing year two Finalising and implementing the of the Greater Wellington implementing the Parks proposed Natural Regional Pest Management Network Plan. Resources Plan (pNRP). Plan 2019-2039. This plan is designed to provide The pNRP sets out guidelines The plan establishes a framework a coherent, consolidated for people that use the region’s for managing or eradicating management regime for the resources. specified plants or animals within network as a whole as well as the Wellington region. specific management provisions for each park. Delivering the second year Consultation and adoption Delivering programmes, of the Wellington Regional of the Regional Land such as Movin’March, Erosion Control Initiative Transport Plan. to encourage active programme. This plan is a blueprint for a travel and use of public Erosion is an issue across New transport network that will keep transport. Zealand; this programme targets the Wellington region on the the Wairarapa region. move. Continuing to work with Working with our bus Implementing a number of KiwiRail and Transdev to operators to continually improvements to our water improve the rail network. improve bus service supply infrastructure. performance. To read the full 2020/21 Annual Plan see gw.govt.nz/annual-plan.
Recommended publications
  • Level 3 Chamber of Commerce House 15 Daly Street Lower Hutt Wellington 5010 New Zealand 30 April 2021 Hon Michael Wood Minister
    Level 3 Chamber of Commerce House 15 Daly Street Lower Hutt Wellington 5010 New Zealand 30 April 2021 Hon Michael Wood Minister of Transport By email; [email protected] Dear Minister, NZ Upgrade Programme – Melling Interchange The Board and membership of the Hutt Valley Chamber of Commerce and Industry is alarmed and deeply disappointed to read recent media articles regarding the inclusion of Melling Interchange in the Government’s reassessment of infrastructure development projects. As you may be aware the Hutt Valley Chamber has been calling for the re-development of the Melling Interchange with SH2 for many years. As a national roading project the current Melling/SH2 intersection is completely inadequate, causing traffic bottlenecks daily and regular accidents. It is a crucial piece of local infrastructure that is a constant chokepoint for all our businesses trying to move people, materials and products around the valley, the region, and nationally. It is an economic drain on our local Hutt Valley economy as well as the wider Wellington region and continues to get worse every year. However, it is not a stand alone transport project. The redevelopment of the SH2/Melling interchange underpins the greater RiverLink project which completely transforms the Lower Hutt city centre. RiverLink is regarded as a shining example of how Waka Kotahi, the Greater Wellington Regional Council and the Hutt City Council can work collaboratively, leveraging combined budgets to deliver a single project in a cohesive manner. It includes improving public transport to the city centre with upgraded railway infrastructure, new active transport modes with cycling and walking, as well as enabling new housing options for city centre residents.
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  • 2. Hutt Valley Line
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  • 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.
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  • 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.
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  • Te Whanganui a Tara Customary Tenure, 1750–1850
    Te Whanganui-a-Tara Customary Tenure 1750-1850 Penny Ehrhardt ( Te Whanganui-a-Tara Customary Tenure 1750-1850 Penny Ehrhardt A Report Commissioned by the Waitangi Tribunal December 1992 Waitangi Tribunal Division Department of Justice Wellington Contents Introduction .................................................. 3 1: Literature Survey 1.1 Primary Sources ............................................ 4 1.2 Secoundary Sources ......................................... 5 2: Historical Narrative 2.1 Te Whanganui-a-Tara (Wellington) before 1820 .................. 11 2.1.1 Te Whanganui-a-Tara before Ngati Ira move into the district 11 2.1.2 Ngati Ira ........................................... 10 2.1.3 Two Northern Taua .................................. 12 2.2 Migration of Kawhia and Taranaki tribes to Kapiti ............... 14 2.2.1 Te Rauparaha's decision to migrate south ................ 14 2.2.2 Te Ati Awa join the heke .............................. 15 2.2.3 Response of the Southern Tribes ........................ 16 2.2.4 Waiorua ........................................... 17 2.2.5 Further Heke to the Kapiti Coast ....................... 19 2.3 The Changing Occupation of Te Whanganui-a-Tara .............. 19 2.3.1 Ngati Tama and Ngati Mutunga move to the region ........ 19 2.3.2 Origins of Ngamotu's claims in Te Whanganui-a-Tara ...... 22 2.3.3 Haowhenua ......................................... 23 2.3.4 Ngati Mutunga leave Te Whanganui-a-Tara .............. 24 2.3.5 Ngati Mutunga's gift ................................. 25 2.3.6 Interests in Te Whanganui-a-Tara between Ngati Mutunga's departure and the arrival of the Tory ........................ 26 2.4 Pakeha involvement in Te Whanganui-Tara ..................... 28 2.4.1 Land made tapu for the Wesleyan Mission ................ 28 2.4.2 New Zealand Company "purchase" ..................... 29 2.4.3 Maori Perceptions of the "sale" ........................
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  • Black Shag (Phalacrocorax Carbo): Roost Counts at Melling, Hutt Valley, and Breeding in the Wellington Region, New Zealand
    Notornis, 2007, Vol. 54: 93-98 93 0029-4470 © The Ornithological Society of New Zealand, Inc. Black shag (Phalacrocorax carbo): roost counts at Melling, Hutt Valley, and breeding in the Wellington region, New Zealand R.G. POWLESLAND 64 Roseneath Terrace, Wellington 6011, New Zealand A.R. MUNRO 14 Onehuka Road, Melling, Hutt Valley, New Zealand I.M. WESTBROOKE Research, Development & Improvement Division, Department of Conservation, P.O. Box 13029, Christchurch, New Zealand Abstract We counted the black shags (Phalacrocorax carbo) frequenting a night roost at Melling, 4.5 km up-river from the Hutt River mouth, Wellington, New Zealand, and studied the timing of breeding at various colonies in the Wellington region. Numbers at the roost were counted from Oct 1993 to Sep 1998: maximum and minimum mean monthly counts were in Feb and Aug, respectively. The main egg-laying period of 3 coastal colonies (0-2 km from the coast) (Mar-May) was c.3 months earlier than at 2 inland (5-33 km) colonies (Jun-Aug). We discuss the possibility that the difference in timing of breeding by shags in colonies at different distances from the coast is related to the different timing of peak prey availability in the 2 habitats (coastal marine, and inland riverine). Powlesland, R.G.; Munro, A.R.; Westbrooke, I.M. 2006. Black shag (Phalacrocorax carbo): roost counts at Melling, Hutt Valley, and breeding in the Wellington region, New Zealand. Notornis 54(2): 93-98. Keywords Phalacrocorax carbo; night roosts; breeding phenology; inland; coastal; diet INTRODUCTION the same colony, Lalas (1983) noted that 5 clutches Breeding colonies of the black shag (Phalacrocorax were laid during Sep-Jan; perhaps egg-laying carbo) occur from Northland to Southland (Bull was protracted because “nesting was drastically et al.
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  • Flooding Hazard – Hutt Valley • Learn About River fl Ows at the Taita Gorge Via the fl Ow Phone (This May Be Very Busy If There Is a fl Ood Alert)
    Living with the fl ood hazard The Hutt River Floodplain Management Plan provides a high level of protection but remember fl oods can happen at any time of the year, night or day. The general Flooding Hazard fact sheet provides a lot of useful information on how to be prepared for fl ooding, but here are some further guidelines: • Find out about the fl ood hazard at your home and other places your family use such as work and school • In the Hutt Valley, the Upper Hutt and Hutt City Councils have the primary responsibility for passing fl ood warnings to the community and you should contact them if you are concerned about fl ood risk Flooding Hazard – Hutt Valley • Learn about river fl ows at the Taita Gorge via the fl ow phone (this may be very busy if there is a fl ood alert). Want to know more? Flooding from streams This fact sheet The Hutt River is about the Try checking the rainfall fi gures and water level Never under-estimate the little guys! Events in 1976 and 2004 showed fl ooding hazard catchment and fl ow at Taita Gorge by: that small streams in the Hutt Valley can cause major fl ooding to areas in the Hutt Valley. nearby: There’s more to the Hutt River than Paraparaumu • checking out www.gw.govt.nz, go to It gives some you may think. The river is part of a • December 1976, the Korokoro Stream fl ooded during a storm Environmental Monitoring, then fi nd Rainfall advice on how much bigger system – its catchment.
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  • Hutt Valley DHB
    A deprivation and demographic profile of the Hutt Valley DHB Hutt Valley DHB, showing overall IMD deprivation with the most deprived areas shaded darkest Rachael Yong, Michael Browne, Dr Jinfeng Zhao, Dr Arier Chi Lun Lee, Dr Nichola Shackleton, Dr Sue Crengle, Dr Daniel Exeter 17/10/2017 Statistics New Zealand Disclaimer The results in this report are not official statistics, they have been created for research purposes from the Integrated Data Infrastructure (IDI), managed by Statistics New Zealand. The opinions, findings, recommendations, and conclusions expressed in this paper are those of the author(s) not Statistics NZ or the University of Auckland. Access to the anonymised data used in this study was provided by Statistics NZ in accordance with security and confidentiality provisions of the Statistics Act 1975. Only people authorised by the Statistics Act 1975 are allowed to see data about a particular person, household, business, or organisation and the results in this paper have been confidentialised to protect these groups from identification. Careful consideration has been given to the privacy, security, and confidentiality issues associated with using administrative and survey data in the IDI. Further detail can be found in the Privacy impact assessment for the Integrated Data Infrastructure available from www.stats.govt.nz. The results are based in part on tax data supplied by Inland Revenue to Statistics NZ under the Tax Administration Act 1994. This tax data must be used only for statistical purposes, and no individual information may be published or disclosed in any other form, or provided to Inland Revenue for administrative or regulatory purposes.
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  • Hutt Valley & Melling Train Lines
    To Wellington Monday to Friday AM HVL HVL HVL HVL MEL HVL HVL HVL HVL MEL HVL HVL MEL HVL HVL HVL MEL HVL HVL MEL HVL HVL MEL HVL MEL HVL MEL Upper Hutt 4.30 5.30 6.00 – – 6.20 – 6.40 – – 7.00 – – 7.04 7.18 – – 7.40 – – 8.00 – – 8.30 – 9.00 – At all stations passengers Wallaceville 4.32 5.32 6.02 – – 6.22 – 6.42 – – 7.02 – – 7.07 7.20 – – 7.42 – – 8.02 – – 8.32 – 9.02 – should make themselves Trentham 4.35 5.35 6.05 – – 6.25 – 6.45 – – 7.05 – – 7.10 7.23 – – 7.45 – – 8.05 – – 8.35 – 9.05 – visible to the driver. Heretaunga 4.37 5.37 6.07 – – 6.27 – 6.47 – – 7.07 – – 7.13 7.25 – – 7.47 – – 8.07 – – 8.37 – 9.07 – Silverstream 4.40 5.40 6.10 – – 6.30 – 6.50 – – 7.10 – – 7.16 7.28 – – 7.50 – – 8.10 – – 8.40 – 9.10 – X Express service. Manor Park 4.42 5.42 6.12 – – 6.32 – 6.52 – – 7.12 – – 7.21 7.30 – – 7.52 – – 8.12 – – 8.42 – 9.12 – Pomare 4.45 5.45 6.15 – – 6.35 – 6.55 – – 7.15 – – 7.25 7.33 – – 7.55 – – 8.15 – – 8.45 – 9.15 – Taita 4.47 5.47 6.17 6.20 – 6.37 6.40 6.57 7.00 – 7.17 7.20 – 7.29 7.35 7.40 – 7.57 8.00 – 8.17 8.20 – 8.47 – 9.17 – OP Off peak fares apply.
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  • Buses Replace Trains Temporary Hutt Valley Line Closure Monday 11 - Friday 15 January 2021
    Buses replace trains Temporary Hutt Valley Line Closure Monday 11 - Friday 15 January 2021 Manor Park Shuttle service Wellington Ngauranga Petone Ava Woburn Waterloo Epuni Naenae Wingate Taita Pomare Silverstream Heretaunga Trentham Wallaceville Upper Hutt Buses replace trains Normal train service Bus Replacement Timetable MONDAY 11 - FRIDAY 15 JANUARY 2021 TO WELLINGTON TO UPPER HUTT At these minutes At these minutes past past the hour 10am until 2:30pm the hour 9am until AM PM AM 2pm PM Upper Hutt Station 9:00 9:07 9:20 9:27 9:40 9:47 00 07 20 27 40 47 2:40 Wellington Station 8:30 8:50 10 30 50 2:10 EXPRESS TO TAITA EXPRESS TO TAITA EXPRESS TO TAITA EXPRESS TO TAITA EXPRESS TO TAITA Wallaceville Station 9:02 EXPRESS TO TAITA 9:23 9:43 03 23 43 2:42 Ngauranga Station 8:36 8:56 16 36 56 2:16 Trentham Station 9:26 9:46 06 26 46 Petone Station 8:42 9:02 22 42 02 2:22 Heretaunga Station 9:07 9:28 9:48 08 28 48 2:47 Ava Station 8:44 9:04 24 44 04 2:24 Silverstream Station 9:09 9:32 9:52 12 32 52 2:49 Woburn Station 8:47 9:07 27 47 07 2:27 Manor Park Station Waterloo Station 8:50 9:10 30 50 10 2:30 shuttle to 9:12 9:30 9:30 05 30 30 2:52 Silverstream Station Epuni Station 8:52 9:12 32 52 12 2:32 Pomare Station 9:14 9:39 9:59 19 39 59 2:54 Naenae Station 8:54 9:14 34 54 14 2:34 Taita Station 9:16 9:36 9:41 9:56 10:01 10:16 21 36 41 56 01 16 2:56 Wingate Station 8:56 9:16 36 56 16 2:36 Wingate Station 9:19 9:39 9:59 10:19 39 59 19 2:59 Taita Station 8:59 9:25 45 05 25 2:39 Naenae Station 9:21 9:41 10:01 10:21 41 01 21 3:01 Pomare Station 9:01
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  • 1920S-1940S First Cooperation
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