Identifying Resource Management Conflicts: Stakeholder Study Regarding Flood Protection in Wairarapa Moana
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Stakeholder Study: Resource Management of Wairarapa Moana
Natalie Diltz Jena Mazzucco Austin Scott Jeffrey Sirocki March 2, 2016 STAKEHOLDER STUDY: RESOURCE MANAGEMENT OF WAIRARAPA MOANA Identification and Analysis of Wairarapa Moana Stakeholder Opinions Regarding the Management of the Blundell Barrage Gates Abstract This project aided the Greater Wellington Regional Council (GWRC) in collecting opinions from five stakeholder groups concerning management of the naturally flooding Lake Wairarapa in New Zealand. Our team conducted a total of twenty-nine interviews with the Rangitāne (Māori), Department of Conservation, South Wairarapa District Council, landowners, and recreational water users regarding the Blundell Barrage Gates which play a vital role in flood management. Interview discussions indicate that water quality, sources of pollution, water levels, flood management, and future operation of the barrage gates are controversial. We identified communication, collaboration, and education as three areas of focus for the GWRC as they continue to improve their management of the region. i Executive Summary This project is concerned with Wairarapa Moana, a water system located in the Wairarapa region, situated on the North Island of New Zealand. Wairarapa Moana consists of the three main water bodies, shown in Figure 1; the coastal lake is Lake Onoke, the inland lake is Lake Wairarapa, and the main river is the Ruamahanga. The system is dynamic, which means water can flow in both directions. Both tidal movements and rainfall affect the direction of flow. The area is low-lying and sits between two mountain ranges exposing much of the land to seasonal flooding. The Greater Wellington Regional Council, the governing body for the Wellington region, developed the Lower Wairarapa Valley Development Scheme (LWVDS), to control flooding in the 1960s. -
Circulation and Mixing in Greater Cook Strait, New Zealand
OCEANOLOGICA ACTA 1983- VOL. 6- N" 4 ~ -----!~- Cook Strait Circulation and mixing Upwelling Tidal mixing Circulation in greater Cook S.trait, Plume Détroit de Cook Upwelling .New Zealand Mélange Circulation Panache Malcolm J. Bowrnan a, Alick C. Kibblewhite b, Richard A. Murtagh a, Stephen M. Chiswell a, Brian G. Sanderson c a Marine Sciences Research Center, State University of New York, Stony Brook, NY 11794, USA. b Physics Department, University of Auckland, Auckland, New Zealand. c Department of Oceanography, University of British Columbia, Vancouver, B.C., Canada. Received 9/8/82, in revised form 2/5/83, accepted 6/5/83. ABSTRACT The shelf seas of Central New Zealand are strongly influenced by both wind and tidally driven circulation and mixing. The region is characterized by sudden and large variations in bathymetry; winds are highly variable and often intense. Cook Strait canyon is a mixing basin for waters of both subtropical and subantarctic origins. During weak winds, patterns of summer stratification and the loci of tidal mixing fronts correlate weil with the h/u3 stratification index. Under increasing wind stress, these prevailing patterns are easily upset, particularly for winds b1owing to the southeasterly quarter. Under such conditions, slope currents develop along the North Island west coast which eject warm, nutrient depleted subtropical water into the surface layers of the Strait. Coastal upwelling occurs on the flanks of Cook Strait canyon in the southeastern approaches. Under storm force winds to the south and southeast, intensifying transport through the Strait leads to increased upwelling of subsurface water occupying Cook Strait canyon at depth. -
Review of Tsunamigenic Sources of the Bay of Plenty Region, GNS Science Consultancy Report 2011/224
DISCLAIMER This report has been prepared by the Institute of Geological and Nuclear Sciences Limited (GNS Science) exclusively for and under contract to Bay of Plenty 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 Bay of Plenty regional Council and shall not be liable to any person other than Bay of Plenty regional Council, on any ground, for any loss, damage or expense arising from such use or reliance. The data presented in this Report are available to GNS Science for other use from June 2012. BIBLIOGRAPHIC REFERENCE Prasetya, G. and Wang, X. 2011. Review of tsunamigenic sources of the Bay of Plenty region, GNS Science Consultancy Report 2011/224. 74 p. Project Number: 410W1369 Confidential 2011 CONTENTS EXECUTIVE SUMMARY ....................................................................................................... VII 1.0 INTRODUCTION .......................................................................................................... 1 2.0 OVERVIEW OF PREVIOUS STUDIES ........................................................................ 1 2.1 Joint Tsunami Research Project of EBOP and EW (Bell et al. 2004) ............................ 1 2.2 Tsunami Source Study (Goff et al. 2006) ....................................................................... 4 2.2.1 Mw 8.5 Scenarios.............................................................................................. 5 2.2.1.1 -
A Gravity Survey of the Wharekauhau Thrust, Palliser Bay, New Zealand
New Zealand Journal of Geology and Geophysics ISSN: 0028-8306 (Print) 1175-8791 (Online) Journal homepage: http://www.tandfonline.com/loi/tnzg20 A gravity survey of the Wharekauhau Thrust, Palliser Bay, New Zealand Alastair F. McClymont To cite this article: Alastair F. McClymont (2000) A gravity survey of the Wharekauhau Thrust, Palliser Bay, New Zealand, New Zealand Journal of Geology and Geophysics, 43:2, 303-306, DOI: 10.1080/00288306.2000.9514888 To link to this article: http://dx.doi.org/10.1080/00288306.2000.9514888 Published online: 23 Mar 2010. Submit your article to this journal Article views: 117 View related articles Citing articles: 2 View citing articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tnzg20 Download by: [121.75.88.191] Date: 27 March 2017, At: 18:58 New Zealand Journal of Geology & Geophysics, 2000, Vol. 43: 303-306 303 0028-8306/00/4302-0303 $7.00/0 © The Royal Society of New Zealand 2000 Short communication A gravity survey of the Wharekauhau Thrust, Palliser Bay, New Zealand ALASTAIR F. McCLYMONT TECTONIC SETTING School of Earth Sciences The Wairarapa Fault is one of six major faults of the North Victoria University of Wellington Island Dextral Fault Belt (Beanland 1995), a zone of P.O. Box 600 dominantly dextral strike-slip faults that lie within, and strike Wellington, New Zealand parallel to, the Australia-Pacific plate boundary along the southern North Island of New Zealand (Fig. 1). The M+8 earthquake in 1855 caused surface rupturing along the Abstract A gravity survey undertaken at Wharekauhau, Wairarapa Fault for a distance of at least 148 km (Grapes Palliser Bay, New Zealand, determines the geometry of the 1999). -
Wairarapa Moana Whakaora Te Repo, Ka Ora Te Taonga Wai Restoring Our Wetland Treasure
Wairarapa Moana Whakaora te repo, ka ora te taonga Wai Restoring our wetland treasure Barton’s Lagoon on the north Lake Wairarapa The Wairarapa Moana Wetlands Project began in 2008 to enhance the native ecology, recreation and cultural opportunities on the public land in the area. The project partners are Greater Wellington, Department of Conservation, Rangitane o Wairarapa, Kahungunu ki Wairarapa, local hapu and South Wairarapa District Council. They in turn are working with community groups, farmers and environmental and recreational groups to restore our wetland treasure. Everyone recognises you can’t succeed in a project this size without all interested parties being involved. Restoring the edge wetlands The project got a major shot in the arm with a successful bid for funding from the Government’s Fresh Start for Freshwater Clean Up Fund to improve the water quality of the edge wetlands. The Ministry for the Environment will contribute $1 million over the next three years. This funding will be matched by the following funding partners in cash or in kind – Ducks Unlimited, Dairy NZ, Department of Conservation and Greater Wellington Regional Council. The priority for the fresh start project is to enhance the wetland habitat around the edge of Lake Wairarapa and Lake Onoke by improving water quality through restoring selected wetland areas – Boggy Pond, Matthews Lagoon, Wairio Wetlands, JK Donald Reserve and Barton’s Lagoon stand out as priorities. This booklet is a very simplified look at Wairarapa Moana and what this funding sets out to achieve. 1 2 3 Poor water quality – our inherited problem Lake Wairarapa is among New Zealand’s 10 dirtiest lakes. -
The Age and Origin of Miocene-Pliocene Fault Reactivations in the Upper Plate of an Incipient Subduction Zone, Puysegur Margin
RESEARCH ARTICLE The Age and Origin of Miocene‐Pliocene Fault 10.1029/2019TC005674 Reactivations in the Upper Plate of an Key Points: • Structural analyses and 40Ar/39Ar Incipient Subduction Zone, Puysegur geochronology reveal multiple fault reactivations accompanying Margin, New Zealand subduction initiation at the K. A. Klepeis1 , L. E. Webb1 , H. J. Blatchford1,2 , R. Jongens3 , R. E. Turnbull4 , and Puysegur Margin 5 • The data show how fault motions J. J. Schwartz are linked to events occurring at the 1 2 Puysegur Trench and deep within Department of Geology, University of Vermont, Burlington, VT, USA, Now at Department of Earth Sciences, University continental lithosphere of Minnesota, Minneapolis, MN, USA, 3Anatoki Geoscience Ltd, Dunedin, New Zealand, 4Dunedin Research Centre, GNS • Two episodes of Late Science, Dunedin, New Zealand, 5Department of Geological Sciences, California State University, Northridge, Northridge, Miocene‐Pliocene reverse faulting CA, USA resulted in short pulses of accelerated rock uplift and topographic growth Abstract Structural observations and 40Ar/39Ar geochronology on pseudotachylyte, mylonite, and other Supporting Information: fault zone materials from Fiordland, New Zealand, reveal a multistage history of fault reactivation and • Supporting information S1 uplift above an incipient ocean‐continent subduction zone. The integrated data allow us to distinguish • Table S1 true fault reactivations from cases where different styles of brittle and ductile deformation happen • Figure S1 • Table S2 together. Five stages of faulting record the initiation and evolution of subduction at the Puysegur Trench. Stage 1 normal faults (40–25 Ma) formed during continental rifting prior to subduction. These faults were reactivated as dextral strike‐slip shear zones when subduction began at ~25 Ma. -
Former Faunal Areas: Some Sub-Fossil Evidence
N.Z. ECOLOGICAL SOCIETY 17 Former Faunal Areas: Some Sub-Fossil Evidence R. J. Scarlett. Any discussion of former faunal areas described small Euryapteryx which I collect- based on the distribution of fossil or sub- ed on Stewart Island in Nov. 1954. Zelornis fossil bones is complicated when those bones haasti is known from Takaka, Canterbury, are of various geological ages. Nevertheless, Otago and Southland. study of the regions in which the genera and In the North Island, four closely related species of moa are found makes possible small species, Zelornis exilis, Euryapteryx some tentative conclusions. curtus (Owen), E. tane, and E. geranoides The evidence is unevenly distributed be- are recognised. The first three range from cause some areas--the best sources are caves, N. Auckland to Wanganui and Napier, and swamps and sandhilIs--are better suited to geranoides from Tom Bowling Bay, N. the preservation of bones, or have been Auckland, to Takaka. better explored. The 'South Island Megalap- Emeus crassus (Owen) and Emeus huttoni teryx didinus (Owen) ranged down the west coast to Inangahua Junction, from Takaka (Owen) are known from Marlborough, and to coastal Marlborough, down the East are common in Canterbury and Otago. Coast to Southland and the Te Anau-Lake Pachyornis elephantopus Owen ranged from Wakatipu area. egegalapteryx benhami Takaka to Marlborough and from Canter- Archey is known only from the Nelson area. bury to Southland. P. murihiku Oliver was found near InvercargilI, and P. australis Anomalopteryx didiformis (Owen) has Oliver in Southland and Nelson. The-North virtually the same South Island distribution Island P. -
Late Holocene Sediment Deposition in Lake Wairarapa
Late Holocene Sediment Deposition in Lake Wairarapa Martha Ingrid Trodahl A thesis submitted to Victoria University of Wellington in partial fulfilment of the requirements for the degree of Master of Science in Physical Geography December 2010 -1- Abstract Lake Wairarapa is a highly modified lacustrine system at the southern end of the North Island, New Zealand. Not only is it situated in a region that is affected by catchment altering natural phenomena such as earthquakes, storms and fire, but both the catchment and hydrology of the lake have also been significantly altered by humans. Polynesian settlers arrived in the area approximately 700BP and proceeded to deforest the lowlands. European settlers began arriving from 1844AD onwards, completing deforestation of the lowlands and Eastern Uplands. In 1964 the Lower Wairarapa Valley Development Scheme was commissioned in an effort to alleviate flooding. This scheme significantly altered the hydrological regime of the lake. Interest in the condition of the lake and associated wetlands, and the realization that it has important recreational, cultural and ecological value, began to develop in the 1990‟s. This has led to a desire to see the lake restored to a more natural condition while still maintaining its flood protection capabilities. However, the lake has only been monitored over the last several decades. Any evidence of the lakes condition prior to this time is anecdotal and little is known of its natural tendencies and functions. This research has investigated and quantified morphological changes to Lake Wairarapa at the decadal and millenial scale using a combination of aerial photograph analysis, bathymetric survey comparison and lakebed core analysis. -
CYCLE TRAIL PETONE ORONGORONGO RIMUTAKA 2-3 DAYS 115Km Cycle Trail
RIMUTAKA CYCLE TRAIL RIMUTAKA PETONE ORONGORONGO RIMUTAKA 2-3 DAYS 115km Cycle Trail Trail Info Summit Tunnel © Caleb Smith BELOW LEFT: Caspian terns © Rod Morris, Department of Conservation BELOW RIGHT: Seal Colony at Cape Palliser © Destination Wairarapa 2-3 Days Starting on Wellington’s doorstep, this trail winds the Rimutaka Rail Trail, one of the most 115km through the Rimutaka Ranges to the Wairarapa popular and historic trails in the region. Valley and the mouth of the Orongorongo River. After emerging in the Wairarapa, famous for vineyards and sheep farming, TRAIL GRADES: the trail follows a country road past rom the head of Wellington large river and great swimming spots to PETONE FORESHORE TO Lake Wairarapa to Ocean Beach. The Harbour, the Rimutaka Cycle cool off on a hot summer’s day as the MAYMORN - GRADE 2 (EASY). fi nal section is the shortest, but also 35km trail with an easy grade. Trail cuts through the trail gradually climbs to the head of the F the most adventurous. Aptly named The MAYMORN TO CROSS CREEK bush- clad Rimutaka Mountain Range, Hutt Valley. Wild Coast, it skirts around Turakirae - GRADE 2-3 (EASY TO passing through tunnels on an old INTERMEDIATE) 25km into New Beyond the valley the trail enters the Head, where the Rimutaka Range rail trail, and skirting around the wild Zealand’s bush-clad past. Tunnel Gully area in the Pakuratahi dives into the pounding Pacifi c Ocean. southern coast. CROSS CREEK TO OCEAN BEACH - Forest on what was once the main The trail then runs west to the mouth GRADE 3 (INTERMEDIATE) The fi rst stage is an easy riverside cycle railway line between Wellington and the of the Orongorongo River where the 36km on-road ride alongside Lake path called the Hutt River Trail. -
Palliser Bay & Cape Palliser
Executive Summary The Heritage Technical Report is one of eight reports written to feed into the preparation of the Wairarapa Coastal Strategy. The process, which includes the development of a Discussion Document, the technical reports, an Issues and Options Paper and extensive public consultation, is being undertaken by the Wairarapa Coastal Strategy Group. This group consists of representatives from Masterton, Carterton and South Wairarapa District Councils, the Wellington Regional Council and local Iwi, and was formed after concerns that development was proceeding along the Wairarapa coast in an ad hoc and fragmented way. The Heritage Technical Report provides an overview of the statutory framework of heritage provisions. It includes a timeline of occupation over the past 1000 years as well as an inventory of sites along the Wairarapa coast. It provides an analysis of what heritage is important, and what pressures currently threaten heritage. It also comments on what methods are used to protect heritage in the Wairarapa and recommends improvements to existing responses, and new responses. The principal legislation for heritage resources in New Zealand is the Historic Places Act 1993 (HPA). The purpose of the Act is to “promote the identification, protection, preservation, and conservation of the historical and cultural heritage of New Zealand.” The Resource Management Act 1991 (RMA) also recognises and provides for the protection of heritage. It sets out the principles of Matters of National Importance (Section 6), Other Matters (Section 7), and Treaty of Waitangi (Section 8). All three sections have implications for heritage on the coast. In particular, “the relationship of Maori and their…ancestral lands, waahi tapu and other taonga ” is identified as a matter of national importance. -
Lake Wairarapa Water Balance Investigation Stage 1 Report – Interim Findings and Recommendations
Lake Wairarapa water balance investigation Stage 1 report – interim findings and recommendations M Thompson D Mzila Environmental Science Department For more information, contact the Greater Wellington Regional Council: Wellington Masterton GW/ESCI-T-15/47 PO Box PO Box 41 ISBN: 978-1-927217-76-4 (online) T 04 384 5708 T 06 378 2484 June 2015 F 04 385 6960 F 06 378 2146 www.gw.govt.nz www.gw.govt.nz www.gw.govt.nz [email protected] Report prepared by: M Thompson Senior Environmental Scientist - Hydrology D Mzila Senior Environmental Scientist - Groundwater Report reviewed by: N Boyens Team Leader, Hydrology Report approved for release by: G Sevicke-Jones Manager, Environmental Science Date: June 2015 DISCLAIMER This report has been prepared by Environmental Science staff of Greater Wellington Regional Council (GWRC) and as such does not constitute Council policy. In preparing this report, the authors have used the best currently available data and have exercised all reasonable skill and care in presenting and interpreting these data. Nevertheless, GWRC does not accept any liability, whether direct, indirect, or consequential, arising out of the provision of the data and associated information within this report. Furthermore, as GWRC endeavours to continuously improve data quality, amendments to data included in, or used in the preparation of, this report may occur without notice at any time. GWRC requests that if excerpts or inferences are drawn from this report for further use, due care should be taken to ensure the appropriate context is preserved and is accurately reflected and referenced in subsequent written or verbal communications. -
The Tectonic Evolution of Pegasus Basin and the Hikurangi Trench, Offshore New Zealand
THE TECTONIC EVOLUTION OF PEGASUS BASIN AND THE HIKURANGI TRENCH, OFFSHORE NEW ZEALAND by Sarah E. King A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date:_________________ Signed:_________________________ Sarah E. King Signed:_________________________ Dr. Bruce Trudgill Thesis Advisor Golden, Colorado Date _________________ Signed:_________________________ Dr. M. Stephen Enders Professor and Interim Department Head Department of Geology and Geological Engineering ii ABSTRACT The Pegasus Basin overlies part of the tectonic transition between oblique southwest subduction of the Paciic Plate below the East Coast of the North Island of New Zealand, and the strike-slip faulting that dominates the majority of the South Island of New Zealand. The transition from this strike-slip zone into the actively subducting Hikurangi Trench requires a signiicant translation of plate motion from margin parallel to margin normal within the Pegasus Basin. The purpose of this research was to understand the distribution of strain along this complex transition, and to identify how shortening is manifested on structures through time. The diferent stress regimes along the coast may correspond to diferent shortening amounts absorbed on a variety of structures that translate strain accommodation through the major tectonic transition from compressional subduction to strike-slip displacement. Interpretations of 2D seismic proiles guided by models of margins with comparable tectonic settings ensure geologically restorable interpretations and reasonable shortening values within this transition zone. Restorations of depth converted seismic cross sections constrain ages of the faults and establish controls on their timing and activation.