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Regional Plan for the Tarawera River Catchment
Environment Bay of Plenty P O Box 364 Whakatane NEW ZEALAND Environmental Publication 2003/24 ISSN: 1175-9372 REGIONAL PLAN FOR THE TARAWERA RIVER CATCHMENT 1 February 2004 Environment Bay of Plenty Bay of Plenty Regional Council 1 February 2004 Tarawera River Catchment Plan Reader’s Guide READER’S GUIDE There may be some parts of this regional plan that you are interested in reading. To find these parts quickly, the following guide gives a brief summary of what each chapter is about. Chapter 1 - Introduction: Names the regional plan, outlines its purpose and aims, discusses topics and issues to be managed, the geographical area of the plan, and sets its duration. Chapter 2 - Preparation of the Regional Plan for the Tarawera River Catchment: Provides a summary of how the regional plan was prepared, research undertaken and the people and organisations consulted. Chapter 3 - Statutory Framework: Outlines the primary parts or sections of the Resource Management Act 1991 relevant to the preparation of the regional plan. It also includes definitions of “Issues”, “Objectives”, “Policies”, and “Methods”. Chapter 4 - Policy Framework: Establishes how this regional plan relates to other planning documents at the national, regional and district level. Chapter 5 - Responsibilities: Identifies the principle local body and governmental organisations with resource management responsibilities, and gives a brief resume of their primary functions and duties. Chapter 6 - Physical Description of the Tarawera Catchment: Provides background information on the area covered by the regional plan. Discusses the Tarawera River catchment in four sub-areas, namely the Tarawera Lakes and their catchments, the catchment of the Upper Reach of the Tarawera River, the catchment of the Lower Reach of the Tarawera River, and the Tarawera River mouth. -
Anglers' Notice for Fish and Game Region Conservation
ANGLERS’ NOTICE FOR FISH AND GAME REGION CONSERVATION ACT 1987 FRESHWATER FISHERIES REGULATIONS 1983 Pursuant to section 26R(3) of the Conservation Act 1987, the Minister of Conservation approves the following Anglers’ Notice, subject to the First and Second Schedules of this Notice, for the following Fish and Game Region: Eastern NOTICE This Notice shall come into force on the 1st day of October 2017. 1. APPLICATION OF THIS NOTICE 1.1 This Anglers’ Notice sets out the conditions under which a current licence holder may fish for sports fish in the area to which the notice relates, being conditions relating to— a.) the size and limit bag for any species of sports fish: b.) any open or closed season in any specified waters in the area, and the sports fish in respect of which they are open or closed: c.) any requirements, restrictions, or prohibitions on fishing tackle, methods, or the use of any gear, equipment, or device: d.) the hours of fishing: e.) the handling, treatment, or disposal of any sports fish. 1.2 This Anglers’ Notice applies to sports fish which include species of trout, salmon and also perch and tench (and rudd in Auckland /Waikato Region only). 1.3 Perch and tench (and rudd in Auckland /Waikato Region only) are also classed as coarse fish in this Notice. 1.4 Within coarse fishing waters (as defined in this Notice) special provisions enable the use of coarse fishing methods that would otherwise be prohibited. 1.5 Outside of coarse fishing waters a current licence holder may fish for coarse fish wherever sports fishing is permitted, subject to the general provisions in this Notice that apply for that region. -
Heading/Title Aquatic Pest Report 2019
Aquatic Pest Report 2019 Bay of Plenty Regional Council Environmental Publication 2019/03 FebruaryHeading/title 2019 PreparedSubheading by Freya Ewing and Thomas Bailey (Summer Students) 5Month Quay YearStreet P O Box 364 WhakatānePrepared by NEW ZEALAND ISSN: 1175-9372 (Print) ISSN: 1179-9471 (Online) Cover photo: Rowan Wells (NIWA) Acknowledgements We would like to thank Hamish Lass, Biosecurity Officer for his support and guidance, and Lucas MacDonald, Biosecurity Officer for his assistance and advice across all advocacy work. Our acknowledgements also go to Greg Corbett and the remainder of the Biosecurity Team at the Bay of Plenty Regional Council, we are grateful for the encouragement and support we received from all of you. We would also like to show our gratitude to Geoff Ewert for his continued commitment to the Rotorua Lakes, in particular with fixing weed cordons and the running of the boat wash station. We are also immensely grateful to Sarah Van Der Boom from Freshwater Biosecurity Partnership Program for her help with data collection. Lastly, we would like to thank Sam Beaumont and the remainder of the team at Ministry for Primary Industries, for the supplying of merchandise and collateral, signage and guidance. BAY OF PLENTY REGIONAL COUNCIL TOI MOANA 1 Executive summary Many of New Zealand’s most well-known lakes and rivers can be found in the Bay of Plenty region and are therefore known to attract significant visitor numbers annually. The preservation and protection of these waterways are what attracts so many international and domestic tourists to them. Due to the close proximity of the Bay of Plenty lakes and rivers, and their popularity, they are extremely susceptible to invasive pest species. -
Works Produced from the Just Another Masterpiece Education Programme We Hope You Are All Keeping Warm and Dry During the Cold Winter Season
Works produced from the Just Another Masterpiece education programme We hope you are all keeping warm and dry during the cold winter season. Our Digital Technology Educator Jessica Wilkes has settled well in to her position after starting in term one. Jessica is originally from Auckland but has been teaching for the last few years in Westport. She will be leading the teaching and learning programmes that are technology based in the Makerspace on the 2nd floor of Te Aka Mauri (The Library and Children’s Health Hub). Alongside the technology programmes from Year 1 - 10, we are also pleased to offer support for NCEA Digital Technology internal and external assessments. Please see more details further on in this booklet. In terms 3 and 4 we are offering a range of new programmes in visual art and social science, some for a limited period so get in quick. Land of the Taniwha has curriculum links to both visual arts and social science. Students will learn more about Te Arawa and significant places through links to well known taniwha such as Pekehaua from Te Awahou, Kataore from Tikitapu and the infamous monster that dwelt at Kuirau. Just Another Masterpiece is a programme developed for students to teach a deeper understanding of abstract art while examining design elements. Students will be able to create their own abstract mono print to take back to school. Balancing Power - The Function of Local Government delves into the working of local government and is relevant and topical due to the local body elections this year. Making a return year is our Tarawera Te Maunga Tapu programme. -
1. Kerosene Creek 2. Wairua Stream
1. Kerosene Creek First on our list of hot pools in Rotorua is the world-famous Kerosene Creek. 35 minutes from Rotorua and down a gravel road will take you to the thermal pool and waterfall at Kerosene Creek. The creek is popular not just for its geothermal activity but its beautiful surroundings. Location: 28km south of Rotorua. Take State Highway 5, then travel about 2km down Old Waiotapu Road. 2. Wairua Stream Wairua Stream is a bit harder to get to as you have to get a boat across Lake Tarawera, making it a local’s paradise. It is near Te Rata Bay and is one of the most picturesque hot pools near Rotorua. Location: About 25 minutes out of Rotorua down Spencer Road, Lake Tarawera. By boat, launch at Stoney Point and head straight across Lake Tarawera to the headlands on the right of Mt Tarawera. Go straight through these headlands to where the lake opens. Steer gently to starboard and make for the only beach in this area. 3. Wai-o-Tapu / The Bridge / The Secret Spot When it comes to Rotorua hot pools, it does not get more popular thank this one. Funnily enough, it is supposed to be a secret. Get the remnants from the Wai-O-Tapu geothermal attraction by bathing in the hot pool formed by the hot Wai-O-Tapu stream meeting the cool river. It’s a thermal pool, completely natural and completely free! Location: Just outside the Wai-O-Tapu geothermal park (under the bridge). 30km south of Rotorua just off State Highway 5. -
The Sedimentation and Drainage History of Haroharo Caldera and the Tarawera River System, Taupo Volcanic Zone, New Zealand
The Sedimentation and Drainage History of Haroharo Caldera and The Tarawera River System, Taupo Volcanic Zone, New Zealand Prepared by K A Hodgson and I A Nairn Environment Bay of Plenty Operations Publication 2004/03 August 2004 5 Quay Street P O Box 364 Whakatane NEW ZEALAND ISSN 1176 - 5550 Working with our communities for a better environment Environment Bay of Plenty i Acknowledgements The Department of Conservation (Rotorua Lakes Office) permitted our studies in lake and river reserves. Fletcher Challenge Forests (and its successors) provided detailed contour maps and aerial photographs. Bryan Davy and Hugh Bibby (GNS) provided a pre- publication copy of their paper on seismic imaging in Lake Tarawera. PGSF Contract IANX0201 funded this study. Sedimentation and Drainage History, Tarawera River System Operations Publication 2004/03 Environment Bay of Plenty iii Executive Summary Haroharo caldera has been formed by the coalescence of multiple collapse structures over the last 350 kyr, the latest major collapse accompanying voluminous rhyolite pyroclastic eruptions at ~50 ka. The caldera has formed a sink for precipitation on surrounding catchments, with overflow via the Tarawera River through the Whakatane graben to the sea at ~30 km to NE. Lakes have probably always occupied at least part of the caldera floor, but the early lacustrine history is largely obscured by younger eruptives. Since 26 ka, the Haroharo, Okareka, Rotoma and Tarawera volcanic complexes have grown within the caldera during eleven eruption episodes, confining ten lakes on the caldera margins. Growth of the volcanic complexes has greatly altered drainage paths and ponding areas within and marginal to the caldera, so that the present ~700 km2 caldera catchment area is about half the ~1400 km2 area that drained into the caldera between 26 ka and 9.5 ka. -
Tarawera Eruption and After Author(S): James Park Source: the Geographical Journal, Vol
Tarawera Eruption and after Author(s): James Park Source: The Geographical Journal, Vol. 37, No. 1 (Jan., 1911), pp. 42-49 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1777578 Accessed: 21-05-2016 04:05 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 129.180.1.217 on Sat, 21 May 2016 04:05:18 UTC All use subject to http://about.jstor.org/terms 42 TARAWERA ERUPTION AND AFTER. This upheaval was described, in a report, by Mr. Allard, who was in charge of some drilling operations for petroleum in the neighbourhood at the time, as follows:- " Halfway between Mempakal and Lambedan, on the 21st of September, inl the afternoon, a small island was formed. Some natives were out gathering oysters, and noticed a good many bubbles rising, after which a gradual upheaval took place, and went on all night, forming a hill of about 200 yards by 150 yards, and 50 to 60 feet high. It seems to consist of nothing but slatey-looking clay, with a few sandstones in it, exactly similar to what we have been boring through. -
WHAT S on Artist Talks to Activity Trails
SPRING Kia ora, SEASON This spring Rotorua Museum Memorial Dr brings you an exciting mix of Whakaue St exhibitions. View local art, vintage New Zealand tourism Pukaki St Fenton St Fenton posters and explore unique Hinemaru St heritage collections. Arawa St Princes Gate Queens Dr Rotorua Our events offer something Government Rotorua Gardens Museum Oruawhata Dr for all ages from music Haupapa St Queens Dr Tutanekai St Tutanekai performances to family days, Pukuatua St WHAT S ON artist talks to activity trails. Hinemoa St Fenton St Fenton Eruera St Eruera St Queens Dr Museum Café Enjoy delicious coffee and a tasty all-day menu with lovely views overlooking Government Gardens. (detail), date unknown. Rotorua Trust Heritage Collection (detail), date unknown. Rotorua Trust Museum Gift Shop Browse a great range of quality New Zealand crafts, Whakarewarewa (detail), 2015. Finalist 2015 Rotorua Museum Art Awards. souvenirs and books. Pı¯ngao Kete Pı¯ngao Friends of Rotorua Museum Peter MoriartyPeter (1918-1985), Jill Fleming, Become a member of Friends of Rotorua Museum. Enjoy openings, talks and more. Email: rotoruamuseumfriends @gmail.com 9am – 5pm (MAR – NOV) Contact Details OPEN DAILY Rotorua Museum Phone: 07 350 1814 9am – 6pm Oruawhata Drive (DEC – FEB) Government Gardens Rotorua rotoruamuseum.co.nz 2015 Rotorua Museum AEIOU Art Awards Exhibition Explore the Until 11 October 2015 Ma¯ori Alphabet EVENTS Highlighting the exceptional talent of artists 21 November 2015 – MORE FM People’s Under the Wing – Family Day from the Bay of Plenty, this exhibition 1 May 2016 Choice Award Join bugman Ruud Kleinpaste showcases winners and selected entries Vote for your favourite work in for fun talks, trails & activities. -
Controls on Rhyolite Lava Dome Eruptions in the Taupo Volcanic Zone
Controls on rhyolite lava dome eruptions in the Taupo Volcanic Zone Paul Allan Ashwell A thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Geological Sciences at the University of Canterbury October 2013 P a g e | II Dedicated to Eva Ashwell P a g e | III View from Ruawahia, across the 1886AD fissure and Wahanga dome towards the Bay of Plenty and White Island (extreme distance, centre left) P a g e | IV Abstract he evolution of rhyolitic lava from effusion to cessation of activity is poorly understood. T Recent lava dome eruptions at Unzen, Colima, Chaiten and Soufrière Hills have vastly increased our knowledge on the changes in behaviour of active domes. However, in ancient domes, little knowledge of the evolution of individual extrusion events exists. Instead, internal structures and facies variations can be used to assess the mechanisms of eruption. Rhyolitic magma rising in a conduit vesiculates and undergoes shear, such that lava erupting at the surface will be a mix of glass and sheared vesicles that form a permeable network, and with or without phenocryst or microlites. This foam will undergo compression from overburden in the shallow conduit and lava dome, forcing the vesicles to close and affecting the permeable network. High temperature, uniaxial compression experiments on crystal-rich and crystal-poor lavas have quantified the evolution of porosity and permeability in such environments. The deformation mechanisms involved in uniaxial deformation are viscous deformation and cracking. Crack production is controlled by strain rate and crystallinity, as strain is localised in crystals in crystal rich lavas. -
Wood Calderas and Geothermal Systems in The
WOOD CALDERAS AND GEOTHERMAL SYSTEMS IN THE TAUPO VOLCANIC ZONE, NEW ZEALAND C Peter Wood Institute of Geological Nuclear Sciences Ltd, Wairakei Research Centre Taupo, New Zealand Key Words: Calderas, Geothermal Systems, Taupo Volcanic Zone. New Zcaland 2. TAUPO VOLCANIC ZONE The Taupo Volcanic Zone Fig. 1) is the consequence of plate subduction beneath the North Island of New Zcaland. ABSTRACT The thin continental crust (-15 km, Stem and Davey, 1987) spreads at rates up to 18 (Darby and Williams, 1991) Silicic calderas and geothermal systems in Taupo Volcanic in active rifting and subsidence. Since c. 1.6 Ma, the Zone (TVZ) of New Zealand are spatially related. Eight calderas, central TVZ has been the most frequently active and productive active since 1.6 Ma, occupy 45% of the Boundaries of region of rhyolitic volcanism on earth (Houghton et al., 1994). calderas arc often speculative, but of 20 geothermal systems producing an estimated 10 - 15 of rhyolite, and considercd, 15 occur on or next to a caldera margin where there is subordinate dacite, andesite and basalt. Debate continues whether enhanced deep permeability: the best examples are at Haroharo TVZ is a migrating andesitic arc and zone of asymmetric crustal where systems occur at the intersection of volcanic lineations and spreading (eg. Stem, or an andesite-dacite arc with bimodal caldera embayments, and at Rotorua. Drillhole evidence supports rhyolite-basalt back arc (eg. Cole, 1990). Whichever is the case, a realignment of caldera margin through the Wairakei- it is a matter of observation that most geothermal fields are geothermal field. Four geothermal systems have no known contained within the area of rhyolite volcanism. -
1 Interpretation of Gravity and Magnetic Anomalies at Lake
Interpretation of gravity and magnetic anomalies at Lake Rotomahana: geological and hydrothermal implications F. Caratori Tontini a*, C.E.J. de Ronde a, B.J. Scott b, S. Soengkono b, V. Stagpoole a, C. Timm a, M. Tivey c a GNS Science, 1 Fairway Dr, Lower Hutt 5010, New Zealand b GNS Science, 114 Karetoto Road, RD4, Taupo 3384, New Zealand c Woods Hole Oceanographic Institution, 266 Woods Hole Rd., Woods Hole, MA 02543, USA Keywords: Lake Rotomahana; hydrothermal systems; magnetic anomalies; gravity anomalies; phreatomagmatic eruptions; basaltic dikes. * Corresponding author: Fabio Caratori Tontini GNS Science 1 Fairway dr Lower Hutt 5010 New Zealand Tel: +64 4 5704760 Email: [email protected] 1 ABSTRACT We investigate the geological and hydrothermal setting at Lake Rotomahana, using recently collected potential-field data, integrated with pre-existing regional gravity and aeromagnetic compilations. The lake is located on the southwest margin of the Okataina Volcanic Center (Haroharo caldera) and had well-known, pre-1886 Tarawera eruption hydrothermal manifestations (the famous Pink and White Terraces). Its present physiography was set by the caldera collapse during the 1886 eruption, together with the appearance of surface activities at the Waimangu Valley. Gravity models suggest subsidence associated with the Haroharo caldera is wider than the previously mapped extent of the caldera margins. Magnetic anomalies closely correlate with heat-flux data and surface hydrothermal manifestations and indicate that the west and northwestern shore of Lake Rotomahana are characterized by a large, well-developed hydrothermal field. The field extends beyond the lake area with deep connections to the Waimangu area to the south. -
Rotorua 1 Princes Arch Gateway Architecture Seems to Be a Big City Activity
ITINERARY n.33 NOT ON MAP 9 10 11 13 15 2 4 1 5 6 7 8 3 14 12 The Blue Baths, 1933 1901 City Guide: Rotorua 1 Princes Arch Gateway Architecture seems to be a big city activity. It is, of course, possible to think of exceptions - Mario Arawa Street Botta in the mountain resort town of Lugano, Peter Zumthor beavering away in the tiny Swiss village of Haldenstein, or more close at hand, John Scott seeming to pluck inspired designs from the coastal air of Haumoana – but almost every significant architect is associated with a particular metropolis, and much of what we assume is important about architectural culture seems to rely on metropolitan densities of wealth and sophistication. Even here in decidedly un-metropolitan New Zealand, the big cities seem to predominate. A scan of the list of NZIA National Awards reveals the dominance of Christchurch, Wellington, and (particularly) Auckland; places like Gisborne, Russell, or Levin rarely make the list. It is hard to know whether this is because of a lack of architectural ambition among small town architects, or because their important opportunities are usually snaffled by big city design firms; Aucklanders often complain about Aussies jetting in to snatch plum commissions, but seem not to hesitate at getting on a plane to Queenstown or Paraparaumu to pick up projects. Rotorua is one of the many provincial cities in New Zealand where civic architecture has largely been created by those that don’t live there. In Rotorua, this was exaggerated by the peculiar role outside authorities, particularly the central government, have played in its development – it was unique in the Commonwealth in being a government-controlled town.