wellington fault line map

Wellington (Māori: Te Whanganui-a-Tara [tɛ ˈfaŋanʉi a taɾa]) is the capital city of New Zealand.It is located at the south-western tip of the North Island, between Cook Strait and the Remutaka Range.Wellington is the major population centre of the southern North Island, and is the administrative centre of the Wellington Region, which also includes the Kapiti Coast and the Wairarapa. I think the Wellington Fault is the thick one in your map Vinnieg. Many of the Wellington Region™s faults can produce large earthquakes. The fault line map looks like part of the human nervous system, as if the islands were made of nerves splitting off into intricate connected branches. According to the GNS, it last ruptured some 300-500 years ago -and has an estimated recurrence interval of 500-1000 years. Select a label to find out more. Horizontal movement is expected to be in the range of 3 to 5.5m. Pressure is building along the Alpine Fault, one of the most active fault lines in the world and New Zealand is in a race to be ready. Most Californians live within 30 miles of an active fault. The South Island's main fault line, the 600km long Alpine Fault, hasn't ruptured since 1717. . [2] The most recent rupture event along this section is constrained to 150–450 yrs BP. What would a major Wellington earthquake be like? Send keyboard focus to media. Go downtown and inspect a main road that sits on a fault line. LAWA Bathing Water Quality Map Viewer. Several earthquake fault lines run through the Wellington region, including the Wellington Fault, which runs west of the city centre along Glenmore Street and Tinakori Road to the Aotea Quay motorway interchange and then up the western Hutt Valley. The annual Esri Map Book showcases the most creative and fascinating maps presented at the annual Esri International User Conference Map Gallery exhibition. Found insideIn Down South, writer Bruce Ansley goes on a journey back to his beloved South Island. This segment is relatively linear with a strike of 033°. The Alpine Fault ruptures—on average—every 330 years with a magnitude 8 earthquake. Nicola Litchfield, GNS Science: The map at the moment is showing where the aftershocks are, and the green circles, or ovals, are showing places where we observed fault rupture, when we flew in a . WRC/RP-T-96/13 Greater Wellington Regional Council, Wellington, New Zealand. Found inside – Page 634Instead there are many faults which are sub - parallel to the fault line , and the characters of these may reasonably be attributed to the Wellington Fault ... An iso-seismal map is used to determine the hazard for a particular location in the seismic design standard that engineers use. The 2016 Kaikōura earthquake which loaded the fault line with pressure has been described as "the most complex earthquake ever . Fault, an active transcurrent fault known to extend from Cook Strait north for 50 km (Kingma 1967). >99%. The devastating earthquake that tore through Christchurch on Tuesday is the product of a new fault line in the Earth's crust that seismologists . Chance of 1 or more M6.7 or greater earthquakes striking CA. The fault, capable of generating a maximum earthquake of between magnitude 6.3 and 7.1, was . There are over 10,000 Vicmap Topographic Maps available at scales of 1:25 000, 1:30 000 (A3 and A4), 1:50 000 . No front page content has been created yet. Information available includes the age of the most recent activity on each fault segment, surface rupture areas, and whether or not the faults are visible at the surface. In the 1970s and 1980five active fault maps s were published as the Late Quaternary Tectonic Map of New Zealand series. Greater Wellington Regional Council (1996). The Ohariu Fault passes through Porirua City, but has a lower return period than the Wellington Fault. If we're unable to resolve a complaint, you can call Utilities Disputes on 0800 22 33 40 or visit utilitiesdisputes.co.nz. more. 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. This series included the first, and in fact only, published New Zealand-wide active fault map paper (Officers of the Geological Survey 1983. Be Your Own Mentor gives advice from top women on how to: Devise a short-term and long-term career strategy Gain visibility in the workplace and in your field Create opportunities to gain valuable experience Change your career path ... Principal active faults in black and Wairarapa fault zone in yellow, with splay zones at . Found inside – Page 171... and traced on the palinspastic map as restoration proceeded . This line is offset 40 km on the Wellington Fault , 65 km on the Wairarapa Fault , and a ... The Wellington fault is the closest of many faults that pose major earthquake hazards for New Zealand's capitol city. Found inside – Page 232PERSON D.C. CO BUTLER VEIN 50 LODE Veins , tunnels , and faults at elevation of ... C. CO LINE ORM BUTLER 1 FIRST LEVEL PODLE DRE 14t Veins , stopes , and ... Use this tool to quickly find and download free maps as image files (TIFF and GeoTIFF formats). / Science Topics These plate movements have resulted in three major fault-lines running either through or very close to Wellington City - the Ohariu Fault, the Wairarapa Fault, and the Wellington Fault. Today the Hutt River flows from the southern Tararua Ranges through the Hutt Valley to the Petone foreshore. Wellington Field, Sumner County, KS Amplitude envelope map of the Mississippian reflection Instantaneous frequency map of the Mississippian reflection #1-32 #1-32 #1- 28 #1-Can we relate real data seismic amplitude and frequency to reservoir thickness as it has been suggested by the modeling? In an emergency please contact our 24 hour Electricity Emergency Line 0800 248 148 For all other matters, please view our contact details here or call your electricity retailer.. Check out our Wellington Fault video here. The new website shows information about the region's properties, planning zones and geographic features. Add to new collection. These include: Holocene. [1], Although no historic earthquake has been recorded for this fault, the potential impact of rupture along the Wellington-Hutt Valley section on the Wellington area makes it one of the greatest natural hazards in New Zealand. The 53 km long arcuate Tararua segment starts just north of Kaitoke along the eastern side of the Tararua Range. Found inside – Page 21913.2 Wellington Field Faults and Fractures Based on core observations, ... which is linked to the subsurface stress field, it was possible to map fracture ... Ayrat Sirazhiev, M.S. In the summer season, you can use this map to see the most recent bathing water quality information for popular bathing sites. Found inside – Page 26418) who considered it to extend across Cook Strait to join the Wellington Fault; this correlation has also been made by Lensen (1958a). Found inside – Page 73... capping the Wellington coal seam , form a cuesta ridge with a very steep front slope or fault - line scarp bordering the valley ( see Plate IIIB ) . Found inside – Page 110Map of faults of northern Wairarapa: Active faults are indicated by solid lines; extrapolated and inactive faults are shown by dashed lines; air photograph ... Scientists in New Zealand say the discovery of another major fault line in Wellington, capable of magnitude 7 earthquakes, does not greatly increase the risk to the capital. For instance, in the event of the Wellington Fault rupture, the city could expect several hundred deaths, several thousand injured, and billions of dollars of damage. The arrows show the directions of relative motion along the fault. As with the original edition, about a third of this book is devoted to an account of the life of Charlie Douglas, and about two thirds to his writings, which have been only lightly edited. It appears to be coming out of the harbour, while the Ohariu is closer to the coast. Written to show how one actually describes, measures and records rock structures such as folds and faults with the emphasis on accuracy, detail and on-going interpretation throughout, this handbook gives students and enthusiasts the ... Geologic maps of 7.5-minute topographic quadrangles covering parts of the Seattle fault and southern Whidbey Island fault zone are available on the DNR website as: Many of the larger faults are oblique strike slip faults, having a combination of sideways and vertical movement.To explore in detail a map of New Zealand's known active faults go to our active faults database and click on the link near the bottom of the page.. Known faults in California. This text explores the natural history of Texas and more than 2900 springs in 183 Texas counties. The Wellington Fault is an active seismic fault in the southern part of the North Island of New Zealand. [2] While a major rupture on the Wellington Fault can be expected anytime in the next 500 years, a significant earthquake on other faults in the Wellington area have a shorter 150 year return time. 721 earthquakes in the past 365 days. Map via Wikicommon Found inside – Page 62Locate these positions on the lines of section and as far as possible identify on the map the extent of the outcrop of these two major unconformities . Subdivision of the land in the 1960s took account of the fault, and no houses were built directly across it. The Wellington Fault consists of three main sections. It terminates near Putara. This interactive map shows where the major volcanoes are, the types of volcanoes and various facts such as when they last erupted. Latest results show that a great earthquake, one of the biggest in New Zealand's modern history, is due. Found inside – Page 634Instead there are many faults which are sub - parallel to the fault line , and the characters of these may reasonably be attributed to the Wellington Fault ... 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. CANCEL. New Zealand Earthquake Faults. At 3 AM on May 29, 2013, the South Island's technological uncon­scious roars […] Tha Alpine Fault is due for a powerful earthquake in New Zealand. When you have eliminated the JavaScript , whatever remains must be an empty page. Home Wellington is located on six active faults. The California Geological Survey's interactive map allows users to identify the location and classification of faults throughout California. The Ohariu Fault passes through Porirua City, but has a lower return period than the Wellington Fault. Much of the area is . Found inside – Page 58Cotton, C. A. 1951: Fault Valleys and Shutter Ridges at Wellington. ... EHARA, S. 1960: Median Line of Southwestern Japan, the Boundary between both the ... This segment has had a lateral slip-rate of 6.0–7.6 mm per year for at least the last 140,000 years, from the progressive offset of dated river terraces. The Topo50 map series provides topographic mapping for the New Zealand mainland and Chatham Islands at 1:50,000 scale. [3], "Paleoseismicity of the Wellington – Hutt Valley Segment of the Wellington Fault, North Island, New Zealand", "How often do earthquakes occur along the fault? Region - the Wellington fault system. Title: District Plan Volume 3: Map 52 - Hazard (Fault Line) Area: Wellington Fault - Map 3 Author: Wellington City Council Further north, events with similar slip have occured every 500-1000 year. Fault rupture of the ground surface, strong ground shaking, liquefaction, and landsliding will be the principle earthquake hazards associated with a large (≥Mw 7.2) surface-rupture earthqauake on the Northern Ohariu fault. That map shows 31 name) d active faults and 15 Found inside – Page 195Though not strictly in line with any particular theory , such a ... Practically all the forms of relief associated with the Wellington Fault in the vicinity ... / Wellington Fault / Major Faults in New Zealand / Earthquakes / Science Topics / Learning / Home - GNS Science", https://en.wikipedia.org/w/index.php?title=Wellington_Fault&oldid=951024617, Creative Commons Attribution-ShareAlike License, This page was last edited on 15 April 2020, at 02:46. Found inside – Page 361The fault lines marked on the geological map were similarly plotted. Because the individual faults tend to be continuous over long distances, ... Found inside – Page 179and extended the Wellington Fault southwards to Cook Strait. ... western side of the Hutt Valley as a fault-line feature and showed on his map ( 1956, fig. There are major fault lines running the length of New Zealand. Wairarapa Maps are Online. The Aotea Fault and the Wellington Fault. 30. © GNS Science 2017, version PROJECT_VERSION created BUILD_DATE, The Wellington Fault runs along the centre of California Drive. [1], This 75 km long curved fault segment is mapped on the floor of the Cook Strait before crossing the Wellington peninsula through Long Gully and along the northwestern edge of Wellington Harbour, past Lower Hutt terminating near Kaitoke. Many of the larger faults are oblique-slip faults, which can cause a combination of horizontal and vertical movement. Totara Park - suburb on a fault line. (BRANZ) Despite the large number of active faults in New Zealand, some regions are more prone to earthquakes than others. New Zealand Earthquake fault zones including Kaikoura Area, Livingstone, Porters Pass-Amberly, Medbury, Cant Range Front, Spey-Mica Burn and Porters Pass-Amberly Fault Zone. Sheet 1 Wellington (1st ed.) How do we know which fault is most likely to rupture next in Wellington. The strike of this section changes from 041° in the south to 020° in the north. 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. (b) Geological map of the Wellington region [Begg and Johnston, 2000]. Found inside – Page 191A dominant feature of the area is the Wellington Fault. ... METHODS Topographic maps, even on a scale of 1: 15 840, are not sufficiently detailed for ... Found inside – Page 1This is an ideal field guide to geological mapping for2nd/3rd year undergraduates and postgraduatesof Geology, Hydrogeology and Geological Engineering. Geologyteachers and amateur geologists may find it a handy guide. Dr Ristau says: "The most noteworthy fault for Wellington is the Wellington fault line which runs . Found inside – Page 91VI SUPPLEMENTARY NOTES ON WELLINGTON PHYSIOGRAPHY1 O FAULT - LINE VALLEYS N the map accompanying my former ' Notes on Wellington Physiography ' the ... This map shows the active fault lines that lay beneath the Greater Wellington Region and the areas that are prone to ground shaking. A fault line or a fault is a fracture in the crust which had the crust moved. texts accompanying these published maps. The Wellington Fault runs under California Drive in Totara Park, Upper Hutt. Pākihi Supergoup: 5 million years ago – present, Where to explore the Wellington Fault (YouTube Video, 9m 43s). 500+. The Wellington Fault is also capable of producing earthquakes of up to magnitude-8. Found inside – Page 37It was all that cat's fault. How could he think with it ... Keeper had used temporal technology to defeat Midas prematurely and upset the time line. Horizontal movement is expected to be in the range of 3 to 5.5m. However, in a way, Wellington is considered New Zealand's riskiest city. However at this locality, it can be seen as an obvious straight scarp (slope) uplifted on its western side. Students discuss major causes of earthquakes and identify famous fault lines, access and map information about ten largest earthquakes in world from 1989 to 1998, and theorize about location of these earthquakes as they relate to Earth's. That's according to a new study that's . Park at Harcourt Park off Akatarawa Rd, or on California Drive. Today the Hutt River flows from the southern Tararua Ranges through the Hutt Valley to the Petone foreshore. The Kaitoke basin is a small pull-apart basin formed at the 2 km lateral offset between this segment and the Tararua segment, near Kaitoke.[2]. Notes on earthquake hazard mitigation measures 1. The last big earthquake to hit Wellington was in 1855, almost twenty years after the beginning of European colonisation. New Zealand is part of the so-called Pacific "Ring of Fire" that has regular . The Ruahine Fault (which is a branch of the Wellington Fault) between the Ohara Depression and the Napier-Taupo Highway is estimated to produce a 7.5 to 8 magnitude earthquake every 400 to 500 years. The fault crosses the Hutt River and some adjacent river terraces at a right angle in this location, and it is possible to see how the terraces have been offset by earthquakes along the fault. 2020 Christmas Cracker Concert - Faultline Chorus & Friends. The Topo250 map series provides topographic mapping for the New Zealand mainland and Chatham Islands at 1:250,000 scale. No. San Andreas Map: The red line on this map follows the surface trace of the San Andreas Fault across California. These features have been formed by several earthquakes over the last few thousand years. / Learning CANCEL. This report provides information for use in both short- and long term land-planning decisions, particularly at the county level, and an indication of the present and future economic impact of mineral and energy development. Kilometres beneath Wellington the light, thick Australian plate rides over the heavier, but thinner Pacific plate. Found inside – Page 311Other fault - line features ( e.g. , stream lineations ) are nevertheless evident . for locality map . Vote : ( i ) Gradual lengthening of the distance ... New Zealand earthquake caused by new fault line. This site uses cookies to improve your experience and to help show content that is more relevant to your interests. If we're unable to resolve a complaint, you can call Utilities Disputes on 0800 22 33 40 or visit utilitiesdisputes.co.nz. The yellow star is the epicenter of the 1855 M 8.2 Wairarapa earthquake. Phone: 0800 496 734. Find out how flood maps are made. A large, shallow quake along the Wellington Fault, say magnitude 7.4, could cause about 30 deaths and 130 injuries in Porirua if it hit during daytime. Saturday 5 December 2pm & 5pm St Andrew's On the Terrace, 30 The Terrace, Wellington, 6011 Faultline. Found inside – Page 5423—Wairarapa region three-dimensional regional gravity anomaly map. ... Significant fault-lines (from Kingma 1967) are shown as dotted lines in Fig. The Ruahine Fault (which is a branch of the Wellington Fault) between the Ohara Depression and the Napier-Taupo Highway is estimated to produce a 7.5 to 8 magnitude earthquake every 400 to 500 years. 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. En route Wellington to Auckland. Find local businesses, view maps and get driving directions in Google Maps. It forms part of the North Island Fault System, which accommodates the transfer of displacement along the oblique convergent boundary between the Indo-Australian Plate and Pacific Plate. As a result, three major fault-lines run through or very close to Wellington city: the Ōhariu Fault, the Wairarapa Fault and the Wellington Fault. Shaded-relief map of the Wellington region in New Zealand showing the locations of the Wellington Fault, the greater Wellington City area (hatched region), and the 3-D georadar survey sites at Totara Park (TP) and Te Marua (TM). Found inside – Page 78The Wellington Fault passes through the notch in the centre ( note the crushed rock along the fault line ) and the spur end on the right has been moved ... The North Island Fault System runs in a line from the Bay of Plenty to the Wellington coast and is responsible for creating the Kaweka, Ruahine . Found inside – Page 207Geological map of New Zeastudy would not have been possible . This study was funded by the land 1 : 250 000. Wellington , Department of Scientific and New ... HAZARD (FAULT LINE) AREA: WELLINGTON FAULT - MAP 3 1:3,000 Legend Fault Rupture Hazard Area Buffer Area 52 52 0 75 150 225 30037.5 1:3,000 Meters Operative27July2004. Additional fault studies by state and federal geologists in the next few years will help determine the frequency and severity of earthquakes along these fault zones. Geology, 2012 2 High risk faults in New Zealand include the Alpine Fault, Wairararapa Fault, Wellington Fault, and Napier Fault. The Wellington region has been subject to a number of large earthquakes in the past 175 years. Earthquake risk zones. Found inside – Page 138Map showing the level of the top of the greywacke relative to sea level in ... The Wellington Fault Zone lies between the two dashed lines of which line A ... Found inside – Page 280WAIRARAPAF SGF WELLINGTON HARIU F DRY RIVER F WAIRAU R. WARAU BASIN WAIRAU F ... Map showing major active faults in the Cook Strait area for Earthquake ... Many of the Wellington Region™s faults can produce large earthquakes. This shows the fault that runs through the centre of Wellington Harbour and the Hutt Valley. Inset shows the approximate position of the Pacific-Australian plate boundary. Wellington Fault near Totara Park, Upper Hutt (1st of 2) The most recent rupture on the Wellington Fault has formed a low, straight scarp across California Park, Upper Hutt. Houses, transmission lines, pipe lines, and roads cross the fault, and 3-4 m of the net surface-rupture displacement will . ADD TO COLLECTION. The annotated circles and red line indicate shot point and survey line, respectively. J.Thomson / GNS Science, Hutt River at Harcourt Park, Photo J.Thomson / GNS Science, Wellington Fault Scarp at California Park, Photo J.Thomson / GNS Science, Wellington Fault Scarp at Harcourt Park, Photo J.Thomson / GNS Science, Offset Terraces at Harcourt Park, J.Thomson / GNS Science, Fault Trace and River Terraces in Harcourt and California Parks. Found inside – Page 141THE KAIWHARAWHARA CAPTURE W. R. LAUDER Victoria University of Wellington ... belt of shattered and thus weakened rock {shatter belt) on the line of a fault, ... more news. 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.
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