wellington fault line lower hutt
Commercial re-use may be allowed on request. Ticket Information: Admission: Free; 10 weekly payments. It is extremely dangerous, as the fault is surrounded big residential areas, infrastructure and at some parts is crossed by roads, pipelines and bridges, this could prove devastating in the event of a large earthquake along the fault. 1 poster (Actual poster measures 420 x 590 mm and has a white border with a DSIR logo) Shipping Cost: Calculated at Checkout Weight: 100.00 Grams. This view shows the Wellington Fault, which forms a sharp edge to the Hutt Valley, with Petone and Lower Hutt at centre left of the photograph. 15 Whites Line West, Woburn, Lower Hutt, Wellington, 5010, New Zealand × 7 Principal Scientist, GNS Science, Lower Hutt, New Zealand INTRODUCTION The Wellington-Hutt Valley segment of the Wellington Fault (Figure 1), extending from offshore Cook Strait to Kaitoke, near Upper Hutt, is widely perceived to pose the greatest risk to life, property and societal infrastructure of any known Check that the broad indication of hazard from the maps is correct for a particular site. / Learning Home The impacts of the ground shaking will vary around the region depending on: There will be other damaging effects of a large Wellington earthquake: Many slips will occur throughout the region, especially if the hill slopes are already saturated by recent rainfall. The Wellington Fault passes under significant infrastructure such as the ferry terminal, motorway, railway, and several bridges along the Hutt Valley, all of which could be put out of action when the fault next ruptures. Map publication … Friends & Family Performance. Quiz Night. Permission of GNS Science must be obtained before any use of this image. To the west (left) the grassed median strip of California Drive was constructed along the line of the fault.' If there’s a safety issue with electricity, you should call Wellington Electricity’s 24 hour emergency line - 0800 248 148. more news . Come join us for a great night! Our mobile coffee trailer is fully equipped and self contained, so we can travel anywhere. The content of this field is kept private and will not be shown publicly. Within Wellington harbour and on rivers and lakes in the region there may also be a ‘seiche’, as was observed in the harbour after the 1855 Wairarapa earthquake. Wellington Electricity is a member of the Utilities Disputes Energy Complaints Scheme. 17 Apr 2021 - 3:30pm to 5:00pm. Lower Hutt. We've got wheels! The Government welcomes the approval for the Ngā Ūranga ki Pito-one section of Te Ara Tupua, the walking and cycling link between Wellington and Lower Hutt.. / Earthquakes DSIR Geology and Geophysics landforms series. / Wellington Fault The Wellington Fault is one of the major active dextral strike-slip faults of southern North Island. So you'll get a big smile as we make you the perfect coffee. Email ... more. Homer, D.L. In flat areas underlain by unconsolidated sediments the ground can liquefy, tilting buildings and causing buried pipelines and other structures to float to the surface. The railway line from central Wellington reached Lower Hutt station (subsequently Western Hutt) in April 1874, with the line running north up the west side of the Hutt River to … (In many case, this could prove cost-effective towards mitigation.) All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. Households Organisations Community Keep up to … This area has been planned with a number of special features to protect residents. No … Through the rest of the suburb, the fault line runs down the centre of California Drive. The location of the faultline between Wellington and the Scarplet in Totara Park was mapped in the 1940s, when the war effort put a new emphasis on … Two million years of movement in the Wellington earthquake fault line underneath the Hutt Valley has helped form one of the region's most powerful rivers. Lower Hutt: DSIR Geology & Geophysics. Obtain professional advice on implications and available countermeasures. Fault-line scarp of Wellington-Hutt Valley segment of the Wellington Fault. Wednesdays 7:30pm - 10:00pm The Salvation Army Crossroads Hall, corner of Cuba and High Streets, Petone, Lower Hutt. 2. This view shows the Wellington Fault, which forms a sharp edge to the Hutt Valley, with Petone and Lower Hutt at centre left of the photograph. Fortunately, New Zealand has a state-of-the-practice and strongly enforced building code that makes our structures well designed to cope with earthquake shaking. While the most affordable suburb is Taita, which has a median house price of $560,600. No front page content has been created yet. Wellington Electricity may notify complainants in writing that it could take up to 40 working days to resolve a complaint, where a good reason exists. The Hutt Valley follows an active earthquake fault (the Wellington Fault) and in 1855 movement of an adjacent fault line (the Wairarapa Fault) lifted parts of the Valley by over 1.5m and drained the estuarine swamps of Petone and Waiwhetu. / Science Topics Notes on earthquake hazard mitigation measures 1. Rupture of the Wellington Fault, (as well as the many other active faults in the Wellington region, including the Wairarapa Fault, the Ohariu Fault and the subduction interface) would cause a variety of major earthquake hazards. Cotton (1914) also noted that the Hutt Valley continues the line of the Wellington Fault north-eastwards, and in 1921 presented his “downwarping” theory to account for the formation of the Port Nicholson—Lower Hutt Basin. The net subsidence of the Lower Hutt Valley recorded over the last c.300,000 years is the cumulative result of Wellington Fault generated subsidence and Wairarapa Fault generated uplift. Search 242 New Line jobs now available in Lower Hutt, Wellington on Indeed.com, the world's largest job site. the bedrock geology – for example, the soft and less consolidated sand and gravel sediments underlying much of the lower Hutt Valley will behave differently to the hard greywacke hills surrounding Wellington City. The Wellington Fault runs through the Upper Hutt suburb of Totara Park. When: Wed 28 Oct 2020, 7:30pm–10:00pm : Where: Salvation Army Hall, 72 Cuba St, Lower Hutt, Wellington Region . Sing Your Heart Out - Faultline Chorus Open Night. The eastern (nearer) side of the Wellington Fault has subsided, and has been filled with gravel from the Hutt River. Home | Community | Community Emergency Hubs | Lower Hutt ... Wainuiomata (Wellington Road) Arakura Primary School: 209 Wellington Road: Wainuiomata (Wellington Road) Hub Guide, August 2017 (pdf 2.1 MB) Waterloo: Waterloo School : 26 Hardy Street: Waterloo Hub Guide, May 2017 (pdf 2.4 MB) See a map of the region's hubs. The line of the fault extends southwestwards (left) along the median strip of California Drive - an excellent example of urban planning designed to take into account the presence of an active fault line.' © Crown Copyright. This photograph was transferred from the Lower Hutt Public Library. You have not rated this page yet. How helpful was this page? The Wellington Fault is a major active fault that runs from Cook Strait, through Wellington City, the harbour, the Hutt Valley and beyond into the Tararua Range. Thanks, your feedback has been successfully submitted . Description This photograph was transferred from the Lower Hutt Public Library. This Combined Earthquake hazard shapefile is a compilation of all "combined earthquake hazard" ArcInfo coverages in major urban areas of the Wellington Region. Wellington Region; Lower Hutt; 1,277,951 members 456,522 events published You missed this – Subscribe & Avoid FOMO! My List Share Tweet. How much do the Wellington fault lines move? the type of building you are in. i.e. We'll bring the coffee to you in Lower Hutt, Kapiti, Wellington or Porirua! All non-text content is subject to specific conditions. the size and depth of the earthquake - this determines the frequency and amplitude (strength) of the seismic waves as they travel through the earths crust. Wellington Fault New Zealand's capital city lies within the earthquake-generating collision zone between two of the Earth's great tectonic plates, and sits on top of one of the zone's most active geological faults - the Wellington Fault. The coverages represent overlays of all previous earthquake hazard data. What would a major Wellington earthquake be like? Lower Hutt is made up of 28 suburbs. The most severe and damaging effect will be the strong ground shaking. Eileen McSaveney, 'Active faults - New Zealand’s longest active faults', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/en/photograph/4364/wellington-fault-in-the-hutt-valley (accessed 6 March 2021), Story by Eileen McSaveney, published 12 Jun 2006, reviewed & revised 1 Aug 2017. Note: for a close up view of photo click on 'Zoom to 100%' icon to left of photo. There are currently no known outages Are you without power? The most expensive suburb is Days Bay, which has a median house price of $1,099,600. If your power is out and there are no safety issues, contact your individual electricity retailer. In recent times, Dr Ismail has focused on commercial and industrial buildings in Lower Hutt, specifically those around the Wellington Fault line, to identify which buildings may be at risk in an earthquake, and how that risk can best be mitigated. Serving coffee makes us happy! present valley floor. The early valley was heavily forested and early Maori inhabitants had little impact on How often do earthquakes occur along the fault? Top of page. From Melling southwards, the water becomes naturally pressurised beneath a layer of hard clay. Water supplies, electricity and phone lines may also be disrupted so it is a very good idea to have an emergency action plan. View looking NE, with Thorndon in foreground, Wellington Harbour (Port Nicholson) in middle distance, and Hutt Valley in background. The fear is that a rupture of magnitude 7.5 or greater along the Wellington Fault will damage road and water links in the capital so badly that its … How do we know which fault is most likely to rupture next in Wellington? Saturday 5 December 2pm & 5pm St Andrew’s On the Terrace, 30 The Terrace, Wellington, 6011 Faultline... more. The 4.5-kilometre long, five-metre wide shared path will run along Wellington Harbour’s coastal edge, away from State Highway 2 traffic, making it safer and easier for people to walk or cycle between Wellington and Lower Hutt. Within Wellington harbour and on rivers and lakes in the region there may also be a ‘seiche’, as was observed in … Restrictions: R16. GNS Science Reference:
Electricity outages or issues. A seiche occurs when seismic waves passing through the water body set up standing waves that can then inundate the surrounding shorelines. Search 171 Staff Line jobs now available in Lower Hutt, Wellington on Indeed.com, the world's largest job site. Transport routes throughout the region may also be affected by landslides and liquefaction, so that people could be stuck at work or at school or somewhere in between. This pressurised zone, the Waiwhetu artesian aquifer, stretches as far south as the harbour. Today the Hutt River flows from the southern Tararua Ranges through the Hutt Valley to the Petone foreshore. Quaternary stratigraphic studies and fault mapping along the southern part of the fault in Upper Hutt have provided some data on slip rates and recurrence intervals. It is part of a sedimentary basin that includes geologically young, relatively soft sediment fill, deposited at the mouth of the valley; the active Wellington Fault borders the basin to the northwest. Abstract: This report is focused on the lower Hutt Valley, situated on the coastal fringe at the northern edge of Wellington Harbour. View a map of your local council streetlight outages: Lower Hutt or Wellington. CN20124/27 Photograph by Lloyd Homer. One section that the fault traverses, California Park, has been set aside as a recreation reserve. The eastern (nearer) side of the Wellington Fault has subsided, and has been filled with gravel from the Hutt River. / What would a major Wellington earthquake be like? Once we receive your complaint, we have 20 working days to find out what went wrong and resolve the issue. Photo: Annie Douglas. Many of the coastal areas of the lower North Island will be at risk of a tsunami, caused by the Wellington fault displacing the seafloor or triggering a submarine slump. 1: Area of tsunami inundation 2: 20m buffer along major fault traces 3: Ground shaking 4: Liquefaction potential 5: Slope failure. Featured Events. Along most of its length in the Hutt Valley, the Wellington Fault follows close to the line of the Hutt River, and the surface trace has been mostly eroded away. 'Fig. Wellington Regional Council, Wellington, New Zealand. We're friendly! Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence. 11.17, Aerial view showing the scarplet of the Wellington fault crossing California Park. Date Taken 1980s Geotag not … 1990 Earthquake fault line, Wellington Fault, Hutt Valley/Port Nicholson. No thanks, I'll skip. / Major Faults in New Zealand We'll give you a laugh and there is always a bit of friendly banter which will brighten up your day. Wellington Electricity network fault; damaged equipment. 3. The fault line dominates the greater Wellington region’s landscape and is the most predominant geological feature in the area. Water from the Hutt River starts to flow underground around Taita Gorge. The Wellington Fault forms distinctive … 0 Quick view. Many of the coastal areas of the lower North Island will be at risk of a tsunami, caused by the Wellington fault displacing the seafloor or triggering a submarine slump. Wellington Fault subsidence can be calculated by subtracting the Wairarapa Fault uplift from the net subsidence recorded by the buried paleoshorelines beneath the Lower Hutt Valley. 7 Mar 2021 - 6:30pm to 10:00pm. Report an outage. To help improve our service, what feedback can you give us about this page?