Delivering Water to the Region's Cities
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Greater Wellington Regional Council Collects Water from Rivers and An
Greater Wellington Regional Council collects water from rivers and an aquifer, treats it to meet New Zealand’s drinking water standards and distributes this high-quality water to four city councils – Hutt, Porirua, Upper Hutt and Wellington – for their supply to consumers. Where does your water come from? How does the water get to your place? Our Te Marua Water Treatment Plant treats water from the The Regional Council operates 183km of pipes, which Hutt River, either directly or via two storage lakes near the connect its water sources and treatment plants to 43 city plant. The lakes hold 3,400 million litres, and are used to reservoirs. These pipes are up to 1,100mm in diameter. make up for any shortage of water from rivers, or after heavy Two main pipelines link the Te Marua and Wainuiomata rain when river water is too dirty to treat effectively. treatment plants to Wellington (see overleaf), with a connecting pipeline and pumping station at Ngauranga Gorge that allows the transfer of water from either pipeline to the other. This cross-connection gives security from disruption, by allowing water supply to all parts of the network from more than one source. Normally, water from each of our treatment plants is supplied to specific areas: Bulk water from: Is sent to: Te Marua Upper Hutt, Stokes Valley, Porirua and Wellington’s northern and western suburbs The Te Marua Water Treatment Plant Wainuiomata Wainuiomata and Wellington and storage lakes Waterloo Lower Hutt, Eastbourne and Wellington Our Wainuiomata Water Treatment Plant treats water from Gear Island Wellington (if required) the Wainuiomata and Orongorongo rivers and several smaller streams. -
Newsletter January 2015
Friends of Baring Head Newsletter Visit us on line at http://www.baringhead.org.nz/ or follow us on Facebook January 2015 Number 9 Message from the Chair The regional park at Baring Head provides visitors with all sorts of recreation activities as well as opportunities for volunteer workers to protect and enhance the environment. For some time now the Friends have been thinking how to allow visitors and volunteers to combine their involvement in both of these interests and the first trip we’ve arranged for summer 2014/15 showed us this approach has real possibilities. The Friends arranged with a four-wheel drive group, the Cross Country Group, to transport people over to the Fitzroy Bay beach from the bridge car-park for a small charge. Available seats were in great demand, with some people having to be asked to wait for trips later in the summer. Many of those lucky enough to claim a seat hadn’t previously been to Baring Head and some weren’t even sure where it was! The first part of the trip was to the coast where, after an introductory talk and a chance to look at a new beachcombing booklet (see below in Finding out about what your beachcombing turns up) visitors were able to walk along the beach, finding treasures, removing horned poppy and picking up rubbish. The much- reduced horned poppy density is obvious along the sections of the beach that have been tackled – good work previous visitors and volunteers! On this occasion, more of the weed was cleared, particularly further south and near the climbing rocks. -
2015 Sunday Festival Report and Survey Results
2015 Sunday Festival Report and Survey Results CONTENTS 1.0 INTRODUCTION ..................................................................................................................... 3 2.0 BACKGROUND ....................................................................................................................... 3 3.0 PURPOSE ................................................................................................................................ 3 4.0 FESTIVAL PROFILE .................................................................................................................. 4 5.0 SURVEY METHODOLOGY ..................................................................................................... 11 6.0 FINDINGS ............................................................................................................................. 12 Who came to Te Rā? ...................................................................................................... 12 Where did people at Te Rā festival come from? ............................................................ 13 How did people hear about Te Rā? ................................................................................ 14 What the Te Rā festival means for those who came...................................................... 14 What did people think of Te Rā 2015? ........................................................................... 16 Entertainment, hauora and mātauranga tents and the youth zone .............................. 17 Stalls food -
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. -
Background and Issues Paper 2010
Hutt Corridor Plan Review Background and Issues Paper 2010 Important Note: This is a working paper, the purpose of which was to pull together a range of relevant information and statistics, and to identify relevant studies and policies, to assist the technical group in understanding the current context for the Hutt Corridor Plan review. The information and numbers generally reflect what was available during the earlier stages of the plan’s development during 2010. Significant recent updates on project status are noted throughout the paper. Where newer stats or data have become available since this paper was prepared, it has been used directly in the Draft Plan itself. PAGE 1 OF 105 PAGE 2 OF 105 Contents INTRODUCTION..................................................................................................................6 POLICY CONTEXT FOR THE CORRIDOR PLAN REVIEW ...............................................9 1. National context ........................................................................................................................................................9 1.1 New Zealand Transport Strategy 2008..............................................................................................................9 1.2 Government Policy Statement (GPS) on Land Transport Funding...................................................................9 1.3 Safer Journeys 2020 ........................................................................................................................................10 1.4 NZ -
Belmont Walkways — NZ Walking Access Commission Ara Hīkoi Aotearoa
9/28/2021 Belmont walkways — NZ Walking Access Commission Ara Hīkoi Aotearoa Belmont walkways Walking Mountain Biking Dog Friendly Circular Track (Loop) Difculties Easy , Medium , Hard Length 20 km Journey Time Between 1 hour and 8 hours, depending on track Region Wellington https://www.walkingaccess.govt.nz/track/belmont-walkways/pdfPreview 1/7 9/28/2021 Belmont walkways — NZ Walking Access Commission Ara Hīkoi Aotearoa Sub-Regions Porirua , Wellington City Part of Collections Walking Access Commission Walkways , Belmont Regional Park Track maintained by Greater Wellington Regional Council Belmont Walkway is the name for a collection of interconnected walking tracks in the Belmont Regional Park, north of Wellington. The walkway takes in a variety of terrain, including rolling hills, native forest and gentle streams. Below are some of the most popular options. All walking times are for the return trip. Dogs are permitted in the Korokoro, Stratton Street and Dry Creek valleys. Keep them under control and remove droppings. Waterfall Track Moderate grade 1 hour A pleasant scramble for all ages which follows Dry Creek from the park entrance through native bush up towards a small waterfall and back again. Expect wet feet as you cross the stream several times. Flat grassy areas near the start are ideal for picnics. Great for young family groups, especially in summer. Not suitable for buggies. Dogs OK - keep them under control and remove droppings. You can download a map of this walk from the right of this screen. Korokoro Dam Loop Moderate grade 1 hour A walk that takes in the historic Korokoro Dam, regenerating and mature native bush. -
Spaces for Hire
SPACES FOR HIRE A LIST OF SPACES FOR HIRE IN LOWER HUTT SPACES FOR HIRE CONTENTS ALICETOWN ........................................................................................................................................... 5 Transition Towns Community Centre ........................................................................................................... 5 AVALON.................................................................................................................................................. 5 Avalon Pavilion ............................................................................................................................................. 5 Avalon Public Hall ........................................................................................................................................ 6 Hutt Bridge Club ........................................................................................................................................... 6 St. John’s Avalon Uniting Church ................................................................................................................. 7 Ricoh Sports Centre ..................................................................................................................................... 7 BELMONT ............................................................................................................................................... 8 Belmont Memorial Hall (Belmont Domain) .................................................................................................. -
Focus Groups Urban Growth Strategy Hutt City Council
Focus Groups Urban Growth Strategy Hutt City Council March 2013 Prepared for: Wendy Moore & Dwayne Fletcher, Hutt City Council Prepared by: Theo Muller, Sarah Major & Steve Blank, MMResearch™ This study was designed and conducted in accordance with the Code of Practice established by the Market Research Society of New Zealand. TABLE OF CONTENTS 1. Executive Summary ........................................................................1 2. Background ...................................................................................4 2.1 Context ..........................................................................................4 2.2 Key Areas of Exploration ...............................................................4 2.3 Focus Groups ................................................................................5 3. Key Findings ..................................................................................7 3.1 Key Reasons for Living in Hutt City ...............................................7 3.2 Is Hutt City Falling Behind? ...........................................................8 3.3 Is Council active enough in stimulating growth? ..........................8 4. Urban Growth Strategy ....................................................................14 4.1 Greenfield and Infrastructure .......................................................14 4.2 Residential Development: (Wainuiomata / Kelson) .....................14 4.3 Second Wainuiomata Access Road ..............................................17 4.4 Targeted -
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. -
Western Ward – What It Is and What We’Re Doing
WESTERN WARD – WHAT IT IS AND WHAT WE’RE DOING FIND OUT MORE ABOUT: • the new approach to planning • who represents you and how you are represented HAVE YOUR SAY Panel members • Tracy Coleman - Chair of the Panel and President of the How do I engage? Maungaraki Community Association • By sharing your input you can contribute to our city’s future. • Paul Caygill - President of the Normandale Residents You can participate in our online Have Your Say forum, Association consultations, surveys, workshops, open days, or talk directly with our Council officers or elected members, as well as • Greg Besa - Alicetown attend Council committee meetings. • Pam Hindmarsh - Kelson • Talking to your local Community Panel is a great way to help • Ellen Jackman - Youth our Council make the right decisions for your community. • Councillor Margaret Cousins What if I have a project I would like Council to consider funding? • Councillor Chris Milne • You can contact all your elected members by phone or email. Panel members endeavour to keep in touch with the other Or talk to your Community Panel any time during the year Western Ward communities not directly represented through to talk about outcomes you want for your community and panel membership. These include the communities of Tirohanga, projects that might help to achieve this. Harbourview, Belmont, Belmont Flats, Manor Park, and Haywards. • You can also contact the Mayor to suggest a project you Councillors focus on achieving the best outcome for the whole would like Council to consider funding, or to raise any issues city, while paying attention to local ward issues. -
Wainuiomata Central Place Name Origins
WainuiomataCentralPlaceNames.docx WAINUIOMATA CENTRAL PLACE NAME ORIGINS This document is about the origin of the names of various features of Central Wainuiomata on the flat area such as houses, parks and suburb names. It excludes road and street names. Wainuiomata is named after the big water or stream of Mata. Wai means water. Nui means big. O means of. Mata refers to a woman's name Roimata. This is an official version. The origins of the word are disputed and other commonly accepted translations are: - Refers to the women living in the now Hutt Valley who came over the Wainuiomata Hill to evade marauding tribes. These tribes in about 1819 were carrying muskets that came north from the Paremata area. In the battle the local tribes were said to have been destroyed. The Paremata Maoris came across the remaining women who were sitting wailing by the stream after the slaughter of their menfolk. From this we have “faces streaming with water”, “tears” or “weeping water”. - Refers to the large pools of water which lay over the swampy surface of the northern end of the Valley, or the river itself which is known to flood the Coast Road / Wainuiomata Valley. From this it can also mean large river from the swamp. - Refers to the whitebait that are present at the mouth of the river. Mata means whitebait. From this we have big river of whitebait. - Refers to flint or obsidian which is hard rock found in the headwaters of the river. - Refers to the origin and personification of water. The area for the purposes of this document covers is from the head of the Wainuiomata River to the mouth where it enters the sea at the Wainuiomata Coast and its tributaries. -
Hutt Corridor Study Stage 1 ! Report Hutt Corridor Study Stage 1
! report Hutt Corridor Study Stage 1 ! report Hutt Corridor Study Stage 1 Prepared for Wellington Regional Council By Beca Carter Hollings & Ferner Ltd March 2002 8110573/041 Rev A ■ L1:69344 Hutt Corridor Study - Stage 1 Table of Contents 1 Introduction..................................................................................................................1 1.1 Purpose and Objectives ............................................................................1 1.2 Scope............................................................................................................1 1.3 Current Needs and Issues ........................................................................2 1.4 Background and Previous Studies..........................................................3 1.5 Report Structure ........................................................................................3 2 Study Approach...........................................................................................................4 2.1 Transportation Model...............................................................................4 2.2 Technical Group ........................................................................................4 2.3 Performance Indicators ............................................................................4 3 Transport Scenarios....................................................................................................6 3.1 Base..............................................................................................................6