The Condition of Twelve Lakes in the Rotorua Lakes Region Using Lakespi
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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. -
Current Measurements in Lakes Rotorua and Rotoehu 2010 and 2011
Current measurements in Lakes Rotorua and Rotoehu 2010 and 2011 NIWA Client Report: HAM2011-015 February 2011 NIWA Project: BOP11203 Current measurements in Lakes Rotorua and Rotoehu 2010 and 2011 Max Gibbs Rod Budd Cliff Hart Scott Stephens Aslan Wright-Stow Scott Edhouse NIWA contact/Corresponding author Max Gibbs Prepared for Bay of Plenty Regional Council NIWA Client Report: HAM2011-015 February 2011 NIWA Project: BOP11203 National Institute of Water & Atmospheric Research Ltd Gate 10, Silverdale Road, Hamilton P O Box 11115, Hamilton, New Zealand Phone +64-7-856 7026, Fax +64-7-856 0151 www.niwa.co.nz All rights reserved. This publication may not be reproduced or copied in any form without the permission of the client. Such permission is to be given only in accordance with the terms of the client's contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Contents Executive Summary iv 1. Introduction 1 2. Methods 2 2.1 Current meters 2 2.2 Lake Rotorua 3 2.3 Lake Rotoehu 4 3. Results and discussion 6 3.1 Lake Rotorua July/August 2010 6 3.1.1 Current velocity 6 3.1.2 Current direction 7 3.1.3 Wind velocity and direction 7 3.1.4 Wind-water coupling 8 3.2 Lake Rotorua November/December 2010 10 3.2.1 Current velocity 12 3.2.2 Current direction 13 3.2.3 Wind velocity and direction 13 3.2.4 Wind-water coupling 15 3.2.5 Water column decoupling 16 3.3 Lake Rotoehu January/February 2011 16 3.3.1 Wind velocity and direction 17 3.3.2 Mid-lake site current velocity and direction 19 3.3.3 Southern lake site current velocity and direction 22 3.3.4 Lake Rotoehu current synthesis 25 4. -
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. -
Proc. 10Th New Zealand Geothermal Workshop 1988 GEOPHYSICAL EXPLORATION for PROSPECTIVE GEOTHERMAL RESOURCES in the TARAWERA
123 Proc. 10th New Zealand Geothermal Workshop 1988 GEOPHYSICAL EXPLORATION FOR PROSPECTIVE GEOTHERMAL RESOURCES IN THE TARAWERA FOREST C. J. BROMLEY2, J. J. BOTTOMLEY1, C.F. PEARSON2 1. FLETCHER CHALLENGE LTD 2. GEOPHYSICAL CONSULTANT (formerly KRTA LTD) ABSTRACT An integrated geophysical survey, involving GEOLOGY resistivity, gravity and magnetic measurements, was conducted early in 1987 over a 300km2 area Geological inferences suggest that the most within and north of the Tarawera Forest, to promising geothermal prospects are located along investigate potential geothermal resources for the north-eastern boundary of Haroharo Caldera, Fletcher Challenge Ltd. Two significant which lies within the Okataina Volcanic Centre. anomalies have been delineated. The first is the The Haroharo and Tarawera complexes have been Tikorangi resistivity and magnetic low, sporadically active for the last 250,000 years, associated with the north-eastern boundary of the most recently in 1886. This suggests that a magma Haroharo Caldera and centered south of the chamber still underlies the caldera (Nairn, 1981). Tikorangi solfataras. The second anomaly, which Important structural features of the caldera in- is situated within the Puhipuhi Basin, east of clude its margin and the Haroharo and Tarawera the caldera, is postulated to represent a vent lineations. As a result of multiple, shallow separate but cooling geothermal system, with dip slumping, associated with the caldera margin, implications of possible epithermal enhanced vertical permeability in the upper mineralisation. kilometre may be distributed over a broad zone. In addition, the underlying ring fault probably Interpretation of the gravity measurements has creates a deep zone of substantial permeability. led to identification of a north-east trending Recent vents form two broad parallel lineations graben passing through Lake Rotoma, and orientated at 50° which are probably associated intersecting the Haroharo Caldera near with deep-seated basement fractures. -
Lake Rotorua Catchment Landscape Assessment
LAKE ROTORUA CATCHMENT LANDSCAPE ASSESSMENT :: JUNE 2010 WEB VERSION Rotorua District Council Contact Details Email: [email protected] Phone: +64 7 348 4199 After hours: +64 7 348 4195 Fax: +64 7 346 3143 Post: Rotorua District Council Private Bag 3029 Rotorua Mail Centre Rotorua 3046 New Zealand Street Address: Rotorua District Council, Civic Centre 1061 Haupapa Street Rotorua New Zealand Prepared for by Rotorua DistrictWEB Council VERSIONBoffa Miskell Limited A07141_RdL_Rotorua_Southern_Lakes_Landscape_Assessment\Graphics\A07141_001_[prev_T05132_050]_Lake_Rotorua_Catchment_Lsc_Assessmt.indd WEB VERSION WEB VERSION Contents Executive Summary Introduction 1 250 EasterN Rural Terrace ������������������������������������������������������������������������������������������������������������������������������63 Uses of Landscape Character Assessment ����������������������������������������������������������������������������������������������������������������2 25.1: Eastern Rural Terrace 63 260 EasterN Rural Hills ������������������������������������������������������������������������������������������������������������������������������������65 What is “Landscape”? �������������������������������������������������������������������������������������������������������������������������������������������������2 26.1: Eastern Rural Hills 65 Landscape Change in the Lake Rotorua Catchment2 270 MOUNT NGONGOtaHA ���������������������������������������������������������������������������������������������������������������������������������67 -
Annual Report 2019
Annual Report 2019 - 2020 I te wā i tuhia ai te pūrongo ā-tau At the time of writing the 2019 | 2020 Annual 2019/2020, e tāmia ana a Aotearoa Report, Aotearoa is still whānui i te mate urutā, arā i te Korona. weathering the storm of the COVID-19 global Nā konā i raru ai ngā huinga raraunga pandemic. While not me ngā kaupapa e whakaaturia ana i relevant to the data sets and kaupapa presented tēnei pūrongo, ka mutu, e mārama ana in this report, we are mātau kua horapa āna kawenga ki tēnā cognisant of the impact this event has had on iwi, ki tēnā hapū huri noa i te ao. our iwi, hapū and every E mihi ana ngā tarahitī o TTA ki te person on our planet. The Tūhourangi Tribal manawaroa o Tūhourangi whānui, te Authority Trustees would āhei ki te papare ā-iwi, te tiaki pai i ō like to acknowledge the resilience of our tātau kōeke, te aha, te aha. Tēnei te mihi Tūhourangi whānau – o te ngākau māhaki ki a koutou katoa. our ability to collectively respond and look after He mea tuku iho ki a Tūhourangi tōna our koeke and most aumangea – ka mutu, ehara tātau i te vulnerable has been humbling. tauhou ki ngā piki me ngā heke o tēnei Tūhourangi has a legacy ao matemate, ko te hū o Tarawera of resilience – our history tērā, ko ngā pakanga o mua tērā. E is steeped in overcoming adversity, from the whakapono ana ka puta te ihu, kia Tarawera eruption in whakahōnoretia ō tātau tūpuna, kia 1886 to times of hardship before. -
Lake Ōkareka 21
Contents Purpose 1 Overview 1 Lake Rotorua 2016-2017 1 Lake Rotoehu 2016-2017 3 Lake Rotoiti 2016-2017 3 Lake Ōkāreka 2016-2017 3 Key achievements 5 Rotorua Te Arawa Lakes Annual Water Quality Results 10 Lake Rotorua 13 Lake Rotoehu 17 Lake Rotoiti 19 Lake Ōkareka 21 Actions and Outcomes for Non Deed Lakes 23 Communications and stakeholder engagement update 26 Science update 27 Land Technical Advisory Group 27 Water Quality Technical Advisory Group 27 Rotorua Te Arawa Lakes Programme – DRAFT Annual Report 2016-2017 i Environmental modelling 28 Action Plans and sewage reticulation 28 Financials 29 Rotorua Te Arawa Lakes Programme – DRAFT Annual Report 2016-2017 ii Purpose The purpose of this document is to report progress against the 2016-2017 Annual Work Programme of the Rotorua Te Arawa Lakes Programme (the Programme), for the year ending 30 June 2017. This report is in accordance with Clause 5.1 and 5.2 of Deed of Funding with the Crown, for the Programme. In this report, progress made on individual interventions is reported against the Annual Work Programme commitments. The overarching goal of the Deed of Funding Agreement is to meet community aspirations for water quality in the four Deed Funded lakes: Rotoiti, Rotorua, Ōkāreka and Rotoehu. Each of these lakes has a target water quality set by the community in the Bay of Plenty Regional Water and Land Plan. This target water quality is set by Trophic Level Index (TLI) and this report provides an update on the status of water quality across the Rotorua Te Arawa Lakes, against the targets set for all lakes, Deed and non-Deed funded. -
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. -
GNS Science Consultancy Report 2013/155
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 January 2015. BIBLIOGRAPHIC REFERENCE Tschritter, C.; White, P. 2014. Three-dimensional geological model of the greater Lake Tarawera catchment. GNS Science Consultancy Report 2013/155. 42 p. Project number 631W1026 Confidential 2013 CONTENTS EXECUTIVE SUMMARY ....................................................................................................... III 1.0 INTRODUCTION ........................................................................................................ 1 2.0 REVIEW OF GEOLOGY AND HHYDROGEOLOGY IN THE GREATER LAKE TARAWERA CATCHMENT ............................................................................. 2 2.1 History and Structure ..................................................................................................... 2 2.2 Major Geological Units in the Study Area ..................................................................... 2 2.2.1 Okataina Rhyolites .......................................................................................... -
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THERE’S A LOT MORE TO FISH&GAMENZ MAGAZINE AND ONLINE THAN JUST THE SPECIAL ISSUES issueninetyfive FISH & GAME NEW ZEALAND New Zealand $9.90 incl GST issueninetysix FISH & GAME NEW ZEALAND THE AUTHORITY ON FRESHWATER FISHING AND GAME BIRD HUNTING IN NEW ZEALAND New Zealand $9.90 incl GST issue ninetyseven New Zealand $9.90 incl GST BROADEN YOUR ANGLING HORIZONS The Best Month For Fishing ISSUE NINETY FIVE As Good As It Gets Capturing Aerial Antics Moods Of The Tutaekuri JANUARY 2017 22/12/16 2:57 pm ISSUE NINETY SIX So You ThinkYou Can Cast F&G cover Iss95.indd 1 The Fortuity Of Fly Fishing APRIL 2017 Moods Of Bridges I SSUE N 4/04/17 12:34 pm We’re Fishing I Where NETY Red Rock Trout SEVEN F&G cover Iss96.indd 1 Post-Season Shakedown JULY Cracking The Canal Code 2017 Brothers In Arms CATCH THE OTHER FOUR & DON’T MISS OUT! Check out the latest subscription deal online at www.fishandgamenz.co.nz - today! BDMAREVOLUTION_ J000140 J000140_advert.indd 1 17/07/17 3:05 pm Fish & Game 1 2 3 5 4 6 Check www.fishandgame.org.nz for details of regional boundaries Code of Conduct ....................................................................... 4 National Sports Fishing Regulations ..................................... 5 First Schedule ............................................................................ 7 1. Northland ............................................................................ 11 2. Auckland/Waikato ............................................................ 14 3. Eastern ................................................................................. -
Proposals Considered by the NZGB on 18 October 2019 For: Ngāmotu [Assign a New Name]
Proposals considered by the NZGB on 18 October 2019 for: Ngāmotu [assign a new name] Otangiwao [altered from Otangiwai Point] NZTopo50-BE38 Crown copyright reserved Inset map LINZ ‘Topo’ basemap Summary The proposals are to restore two original Māori names by: - assigning Ngāmotu to an unnamed peninsula on the west shores of Lake Rotomā, approximately 30km east-northeast of Rotorua, and - altering Otangiwai Point (unofficial recorded) to Otangiwao, for the small point on the southwest shore of Lake Rotomā, correcting the spelling and dropping the English generic term, Point. The proposers, Ngāti Tamateatūtahi/Ngāti Kawiti, advise they are mana whenua, and their preference is no English generic term be included with either name. A local marae, Tapuaeharuru, Te Tatau o Te Arawa (a governance body), and the Bay of Plenty Regional Council support the proposals. Ngāti Pikiao, Rotorua Lakes District Council, and other iwi and post Settlement entities with interests in the area have not provided their views. Ngāmotu names are duplicated many times in the North Island, including a hill ~30km southeast of the proposal. The NZGB may consider adding a generic term to Ngāmotu, for example, Ngāmotu Peninsula, to make the name unique and the feature easily identifiable in an emergency. A local use name Doctors Point may apply to the entire feature or only the eastern end. Otangiwai Point is a popular site for diving, including commercial operations, so to identify the feature in an emergency the NZGB may consider retaining the ‘Point’ generic term, which is in long term use. Otangiwai Point is also known as Ngātangiwao, and Letterbox Island (or Letterbox Point) is a local use name.