Environmental Geochemistry of Rotorua Lakes

Total Page:16

File Type:pdf, Size:1020Kb

Environmental Geochemistry of Rotorua Lakes Environmental Geochemistry of Rotorua lakes LEADER: Chris Hendy, Associate Professor, University of Waikato, Hamilton, New Zealand START: Leaves from Rotorua on Friday 22 November, 2013 END: Finishes in Rotorua on Saturday 23 November, 2013 DURATION: Two days SCOPE: This field trip will explore the unique aspects of lakes set in two modern rhyolitic volcanic centres. The environmental problems of eutrophication and sediment diagenesis, and the remediation strategies undertaken, will be demonstrated. Highlights of the trip, other than the spectacular scenery, will be examining the vast volumes of methane accumulated in the sediments of Lake Rotorua and the huge pock marks created by its ebullition; and cruising over the recently rediscovered Pink Terraces in Lake Rotomahana. DESCRIPTION: There are 14 lakes of volcanic origin in the Rotorua District. Some are craters, some calderas and the remainder dammed by pyroclastic flows. All are set in a landscape dominated by rhyolitic material ranging from rhyolite flows through ignimbrite to pumiceous sands, gravels and tephras. Several of the lakes have significant geothermal activity within them and many have geothermal springs within their catchments. Land use changes within the last century has greatly accelerated eutrophication in nearly all of the lakes to the point that large scale intervention is underway to attempt to halt the declining water quality. The field trip will encompass cruises on three lakes: 1. Lake Rotorua: This is the oldest lake in New Zealand, probably in excess of 100 m of sediment (very low density diatomaceous ooze), supersaturated in methane and peppered with pockmarks 50 m in diameter and 5 m deep. We will fit a sub bottom sounder on the Lakeland Queen to display these as we cruise over them and Chris Hendy will take a core of the sediments. 2. Lake Tarawera 3. Lake Rotomahana: Geothermally active with silica precipitating onto the sediments, and the site of the Pink and White Terraces destroyed in the Tarawera Eruption of 1886. We will also visit several other lakes: 4. Lakes Rotoiti, where a diversion wall has recently been installed to reduce the flow of nutrient rich waters from Rotorua eutrophying Rotoiti. 5. Lake Rotoehu, where draft tubes are being installed in 2012 to prevent anoxia in the bottom waters and limit the recycling of nutrients from the sediments 6. Lake Rotoma, the cleanest lake in the Rotorua District 7. Lake Okaro, formerly the most eutrophic lake in the Rotorua District, but where an extensive artificial wetland and reorganization of the dairy farm occupying the catchment (which we will visit) plus in-lake water treatment have dramatically improved the trophic status of the lake 8. Lake Rotowhero: a 19m deep hydrothermal explosion crater with boiling water entering from the bottom maintaining a constant temperature of 34°C and a pH of 3.4. This is an extremely productive lake with a single species of green algae supporting a vast population of insects and insect eating bird life. Visits will also be made to: 9. Haumarana Springs: the largest springs in the North Island resulting from solution cavernous weathering of the underlying ignimbrite and the single biggest source of phosphorus to Lake Rotorua 10. Okere Falls: another example of cavernous weathering in ignimbrite where a cave can be walked through that has clearly developed along intersecting joints 11. Tarawera Falls: spectacular cavernous weathering in rhyolite 12. Exiting from Lake Rotomahana will take us through the Waimungu Geothermal Park. PROVISIONAL ITINERARY: To be notified SPECIAL REQUIREMENTS: A moderate level of fitness is required. Sturdy footwear is essential and wet weather gear, sun hat and sunscreen are advised. MAXIMUM NUMBER OF PARTICIPANTS: 20 MINIMUM NUMBER OF PARTICIPANTS: 8 COST: $370. Cost will include transport (by minivan, bus or coach), lake cruise fees, lunches, dinner and accommodation on Friday night and breakfast Saturday morning in Kawerau. FURTHER INFORMATION: Email Chris Hendy at [email protected] GALLERY Lake Rotorua, with Rotorua city in the left foreground. Photo Lloyd Homer. Lake Rotomahana (centre), with Waimangu thermal area in the foreground, MtTarawera in the distance and Mt Edgecumbe in the far distance. Photo Lloyd Homer. Tarawera Falls .
Recommended publications
  • Water Resource Use a Matter of Perspective: a Case Study of The
    WATER RESOURCE USE A MATTER OF PERSPECTIVE: A CASE STUDY OF THE KAITUNA RIVER CLAIM, WAITANGI TRIBUNAL a thesis submitted in partial fulfilment of the requirements for the degree of MASTER OF ARTS IN GEOGRAPHY in the university of canterbury . by. TIMOTHY W fRASER 1988 contents ACKNOWLEDGEMENTS iii LIST OF FIGURES, PLATES AND TABLES v LIST OF MAPS vi ABS1RACT vii CHAPTER PAGE one INTRODUCTION 1.1 Introduction .............................................. 1 1.2 A Case Study for Bicultural Research ............... .. 6 1.3 Thesis Structure ................................. .. 10 two THE SEWAGE DISPOSAL PROBLEM OF ROTORUA CITY: THE KAITUNA RIVER CLAIM 2.1 Introduction ........................................................ 14 2.2 The Problem ........................................................ 15 2.3 A General Response ........._...................................... 24 2.4. The Kaituna River Claim Waitangi Tribunal.................... 32 2.5 Options Pursued After the Waitangi Tribunal Hearing........ 38 2.6 Concluding Remarks .. .. .. .. ... .. .. .. .. .. ... ... 40 three A DOMINANT CULTURAL PERSPECTIVE: THE ENGINEERING SOLUTION 3.1 Introduction ........................................................ 42 3.2 Roots of a Technological Perspective .......................... 43 3.3 Rise of the Engineer .............................................. 47 3.4 Developing a Water Resource Use Strategy ................... 52 ii 3.5 Water and Soil Legislation: 1941 and 1967 ................... 55 3.6 The Dominant Perspective Challenged ........................
    [Show full text]
  • 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.
    [Show full text]
  • THE NEW ZEALAND GAZETTE No
    1384' THE NEW ZEALAND GAZETTE No. 39 In Bankruptcy-Supreme Court Rogers, Hugh Arthur, 87 Clinkard Avenue, Rotorua, NOTICE is hereby given that dividends are payable at my workman. B. 64/74. office on all proved claims in the under-mentioned estate: Rowley, Henry Byers, 7 Pukeko Street, Rotorua, con­ crete worker. B. 62/76. Paaka Joe Teoti, formerly of 30 Chesney Court, Inver­ Sale, Graham John, 18 Brents Road, Rotorua, builder. cargill, labourer, now of 254 Crinan Street, Invercargill, B. 12/75. first and final dividend of I 00 cents in the dollar. Sale, William Hall, 18 Brents Road, Rotorua, builder. W. E. OSMAND, Official Assignee. B. 29/74. Saunders, Barry Francis, 753 Main Road, Mount Maun­ Supreme Court, Invercargill. ganui, dredgehand. B. 37 /75. Snowden, William, 61 Bellingham Crescent, Rotorua, millhand. B. 4/75. IN BANKRUPTCY-IN THE SUPREME COURT AT Tapu, Kenneth Daniel, 18 Seymour Place, Tauranga, ROTORUA driver. B. 25 /74. Te Torno, Leonard Robert Puhanga, 61 Wallace Crescent, NOTICE is hereby given that statements of accounts in respect Rotorua, unemployed commercial cleaner. B. 60/75. of the under-mentioned estates together with the report of the Thomas, William Halsey, 121 Oregon Drive, Murupara, Audit Office thereon, have been duly filed in the above bush supervisor. B. 19/74. Court; and I hereby further give notice that at the sitting of the Court, to be held on Friday, the 19th day of May 1978, Dated at Hamilton, this 3rd day of May 1978. I intend to apply for an order releasing me from the admin­ A.
    [Show full text]
  • Water Flow Between Ohau Channel and Lake Rotoiti Following Implementation of the Diversion Wall Part B
    Water flow between Ohau Channel and Lake Rotoiti following implementation of the diversion wall Part B CBER Contract Report 116 Prepared for Bay of Plenty Regional Council By David P. Hamilton, Wendy Paul, Chris McBride and Dirk Immenga Centre for Biodiversity and Ecology Research The University of Waikato Private Bag 3105 Hamilton, 3240 New Zealand 2010 1 Table of contents Figures ................................................................................................................................. 3 Tables .................................................................................................................................. 5 Executive Summary ............................................................................................................ 6 Background ..................................................................................................................... 9 Water temperature ........................................................................................................ 13 Discussion ......................................................................................................................... 27 Acknowledgments ............................................................................................................. 29 References ......................................................................................................................... 30 Front cover – Photo of diversion wall taken by Wendy Paul 2 Figures Figure 1. ...........................................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • Okere Adventures
    Okere Adventures Okere Falls Reserve, 761 SH33, Rotorua Application for Concession and Resource Consent for Commercial Recreation 18728AP2 15 May 2019 Okere Adventures Okere Falls Scenic Reserve, 761 SH33, Rotorua Application for Concession and Resource Consent for Commercial Recreation Prepared by: Ella Tennent Senior Planner MNZPI Reviewed and Approved for Release by: Sarah Hunt Senior Planner MNZPI Date: 15 May 2019 Reference: 18728AP2 Status: Final This document supersedes all previous issues and is the property of Cheal Consultants Limited. Any unauthorised employment or reproduction, in full or part is forbidden. This document has been prepared for a specific purpose for the above client and shall not be used for any other unauthorised purpose. Cheal Consultants Limited does not acknowledge any duty of care or responsibility to any other party. © Cheal Consultants Limited TABLE OF CONTENTS 1. INTRODUCTION .................................................................................................................................. 6 2. SITE DESCRIPTION ............................................................................................................................... 6 2.1 Activity Site ................................................................................................................................................... 6 2.2 Parking and Check-in Sites ...................................................................................................................... 11 2.3 Surrounding Environment ........................................................................................................................
    [Show full text]
  • Rotorua Wastewater Treatment Plant Applications for Resource Consents and Assessment of Environmental Effects
    ROTORUA WASTEWATER TREATMENT PLANT APPLICATIONS FOR RESOURCE CONSENTS AND ASSESSMENT OF ENVIRONMENTAL EFFECTS APPLICATION EDITION Prepared for the Rotorua Lakes Council 20 August 2018 Rotorua Wastewater Treatment Plant Application for Resource Consents and Assessment of Environmental Effects Rotorua Wastewater Treatment Plant Discharges Application for Resource Consents and Assessment Environmental Effects Authors Overall Approach, Technical, Alternatives, Consultation, Jim Bradley Stantec New Zealand Project Background Dr Rob Lieffering Stantec New Zealand Structure, Conditions, Statutory Assessment Adam Jellie Stantec New Zealand Planning, Consultation Sections Dr Doug Boddy Stantec New Zealand Air Discharges Kirsten Norquay Stantec New Zealand Public Health Risk Assessment Graham McBride NIWA Quantitative Microbial Risk Assessment Existing Scheme Wastewater Treatment Plant, Alison Lowe Rotorua Lakes Council Monitoring and Water Environment Effects Assessment Johnathon Bannatyne APR Consultants Project Context, Growth, Economics, Tourism Dr David Hamilton University of Waikato Water Environment Effects Assessment Dr Jonathan Abell Ecofish Research Water Environment Effects Assessment Dr Christopher Dada University of Waikato Water Environment Effects Assessment Chris McBride University of Waikato Water Environment Effects Assessment Antoine Coffin Te Onewa Consultants Tangata Whenua Consultation Willie Shaw Wildlands Consultants Ecological Assessment Richard Hart Wildlands Consultants Natural Character, Landscape and Amenity Richard
    [Show full text]
  • And H.M. I. Map Island Of
    Whiteford and Bibby THE DISCHARGE INTO LAKE ROTOMAHANA, NORTH ISLAND, NEW ZEALAND P.C. and H.M. Institute of Geological and Nuclear Sciences, Wellington, New Zealand Key words: Heat flow, lake Rotomahana, New Zealand ABSTRACT White Modern Lake Rotomahana was formed during the 1886 eruption island of Mt Tarawera. Heat flow measurements made in the bottom sediments using a marine temperature probe indicate a thcrmal area in the half of lake which has a total condrictivc heat flow of MW. The convective heat Lake discharged into the lake, calculated from tlie rate of incrcase in of the lake, is estimated to bc 145 MW. The ratio of conductive to convective heat flow is similar to that measured in thermal areas beneath Lake Rotorua, North Lake Rolomahana Island, New Zealand. INTRODUCTION The Taupo Volcanic Zone in North Island, New Zealand (Fig. 1) is a volcanic belt extending from the volcanoes, Mt Ruapehu and Mt Ngauruhoe, in the southwest to Whale Island and White Island offshore to the northeast. Lake Rotomahana is one of the southernmost of the Rotorua lakes, lying within the Taupo Volcanic Zone 2 km south of Lake Tarawera and 5 km southwest of Tarawera volcano. To the southwest is the Waimangu thcrmal area (Fig. 2), which contains active thermal features such as or boiling pools, silica deposits, steaming cliffs, and hot ground, and is a well known tourist spot for viewing thermal activity. It is thought that a substantial portion I. Map of Lake in of tlie total heat output of the Waimangu thermal system occurs Island of through the floor of Lake Rotomahana.
    [Show full text]
  • Part 2 Geological History.Indd
    2. Geological History Activities Curriculum Curriculum Environmental Page Activity title level link education aspect 2a Formation of the L 3–5 Science 37 Rotorua lakes 2b Silent Card Shuffl e L 3–5 Science 39 2c Mt Ngongotaha L 3–5 Science About, In 42 2d Looking at Sediment Any level Science About, In 53 2e How Wet is your Any level Science 55 Sediment? 2f What is in your L 5 Science 58 Sediment? Relevant resources: • Rotorua’s Volcanic Past – video – hire from Rotorua Public Library • Rotorua Museum Education Resources » Te Arawa – Mai Maketu ki Tongariro » Legends, Landforms and Learning » Tarawera photo kit » Tarawera Resource kit • Pollution Busters newsletter # 5 Volcanoes • Learning Media - Building Science Concepts • Book 12 – Volcanoes: Hot Rock in a Cool World Levels: 3–4 • Book 52 – The Land Changes: Keeping Earth’s Systems in Balance: Levels: 3–4 • Learning Media – Readers » The Changing Land, Jane Buxton, ISBN 0478214162, explores how the elements can affect Earth and change its shape The Rotorua Lakes Education Resource 35 Activity 2a Formation of the Rotorua Lakes Curriculum links Science Any level 2 Resources required Science • PowerPoint presentation by Will Esler, University of Waikato (on CD) • The Life and Times of Lake Rotorua and Lake Rotoiti (see background notes) • Graphic of Rotorua lake edge 9000 years ago Method 1 View the PowerPoint (ppt) before using it with the class, or set a small group this responsibility. Identify good stopping places for discussion or questions. Have some questions already identifi ed e.g. What was the signifi cant event during this time? Why was it signifi cant? Who/what was responsible for this event occurring? If a small group has previewed the ppt then they can act as a lead questioner/facilitator for one of the groups below.
    [Show full text]
  • Lost Glories, Found
    he dazzling Pink and White Terraces Researchers from Woods Hole Oceano- air. The same geothermal process creates on the shores of Lake Rotomahana graphic Institution (WHOI) who joined the geysers and mineral formations at atT one time were the greatest national trea- the expedition —Dan Fornari, Amy Kuku- Yellowstone National Park. sure of New Zealand. They were cherished lya, and Robin Littlefield—said they had At the White Terraces, scalding, silica- by the Maori and known far and wide as never worked on a project with such deep laden water burbled from a crater about the eighth natural wonder of the world. cultural meaning. “This was actually a 100 feet above the lake and cascaded down Then, during an immense volcanic erup- burial ground,” said Kukulya. “Some of the about 50 wide, scalloped steps. As the water tion in 1886, they disappeared. people we met lost their ancestors there.” cooled, silica precipitated out of solution, “It was such an iconic feature to the dribbling over the steps and creating for- country,” said Cornel de Ronde, the New Not just another hot springs mations that looked like candle wax. The Zealand geologist who led a team that The terraces formed when a magma White Terraces covered an area equivalent rediscovered the Pinks in 2011. “In terms chamber heated groundwater and sent it to seven football fields. The Pink Terraces, of the people’s psyche and what it means spurting out of the ground, carrying dis- about half a mile across the lake from the to them, the equivalent for Americans solved minerals that rapidly crystallized Whites, were smaller but still impressive.
    [Show full text]
  • Kaupapa Māori Community Based Providers in the Health Rotorua Area
    KAUPAPA MĀORI COMMUNITY BASED PROVIDERS IN THE HEALTH ROTORUA AREA An Information Resource for the Health Rotorua Community 2012-2013 KAUPAPA MĀORI COMMUNITY BASED PROVIDERS IN THE HEALTH ROTORUA AREA ORGANISATION SECTOR SERVICE DESCRIPTION OF SERVICE WHO THE SERVICE COST CONTACT PERSON IS FOR Health Cancer Support Service Voluntary support to people with cancer People with cancer and No Cost Bubsie MacFarlane and their family/whānau, including: their family/whānau. [email protected] Guidance and Support Transport support Advocacy in the health system Massage/Mirimiri 1238 Haupapa Street, Rotorua Ph: 07 349 3118 http://www.arohamai.maori.nz/ Social Women’s Support Crisis and post crisis support for women Women who are or No Cost Sylvia Waihi Services ‘Crisis and post crisis support’ and children who are victims of family have experienced family [email protected] violence. Includes one-on-one support, violence assistance with domestic protection orders and advocacy. 1231 Haupapa Street, Rotorua Women’s Support Bi-culturally focused facilitated education Women who are or No Cost Sylvia Waihi Ph: 07 346 2096 ‘Empowering Voices’ programme. Comprises ten sessions. have experienced family [email protected] [email protected] Family violence prevention Topics include recognising and violence education programme understanding the dynamics of family General Manager: Stacey Ford violence, understanding anger and [email protected] aggression and personal power. Monday 6-8pm & Wednesday 12.30pm – 2.30pm Men’s Support Bi-culturally focused facilitated education Men 17+ years old No Cost John Wharepapa ‘Te Pikinga o Te Tangata’ Family programme for men who wish to live [email protected] violence prevention education violence free.
    [Show full text]
  • Kaituna River and Ōngātoro/ Maketu Estuary Strategy
    Kaituna River and Ōngātoro/ Maketu Estuary Strategy From Okere Falls to Ōngātoro/Maketu Estuary Acknowledgements This document has been put together by Environment Bay of Plenty, Western Bay of Plenty District Council, Tauranga City Council and Rotorua District Council – working with representatives from the Kaituna/Maketu community – including iwi, hapū, individuals, community groups and organisations. Special thanks go to: Members of the Working Party, Focus Groups, and tangata whenua for their enthusiasm, commitment and hard work, including: – Maketu Estuary Focus Group – Wetlands and Aquatic Habitat Focus Group – Urban and Industry Development Focus Group – Recreation Focus Group. The wide range of people who put time and energy into participating in public meetings and discussions, providing written feedback and attending the hearings – all of which improved the content of the Strategy. Thanks also to the current and past members of the Kaituna Maketu Joint Council Committee for their guidance and debate. Particular thanks go to Hearings Panel whose recommendations have been incorporated into the Kaituna Maketu Joint Council Committee Public Feedback Report and this Strategy. A summary of the responses to public feedback follows: ▪ Kaituna River to Ōngātoro/Maketu Estuary re-diversion – The Hearing Panel made recommendations based on public feedback and its site visit. The Hearing Panel recommended: – Environment Bay of Plenty commit to progressing the re-diversion of the Kaituna River to the Ōngātoro/Maketu Estuary. – That the preferred option is the full re-diversion of the river back to the estuary with the capability of flood relief through Te Tumu Cut. – In accordance with strong community support, that re-diversion should be advanced as soon as possible by working with mana whenua and landowners on a range of complex issues.
    [Show full text]