19 January 2021 Phone (07) 866 2090 Circulation 8,000 New Te Korowai Doctor Welcomed with Pōwhiri

Total Page:16

File Type:pdf, Size:1020Kb

19 January 2021 Phone (07) 866 2090 Circulation 8,000 New Te Korowai Doctor Welcomed with Pōwhiri Issue 933 - 19 January 2021 Phone (07) 866 2090 Circulation 8,000 New Te Korowai doctor welcomed with pōwhiri Dr Ned Azar, the new GP at Te Korowai Hauora o Hauraki in Whitianga, and his family were welcomed to Mercury Bay with a small pōwhiri at the Wharekaho marae on Saturday last week. Pictured are some of those who attended the pōwhiri. From the left - Dr David Wilson (a senior GP in Mercury Bay for many years), Joe Davis (rangatira of Ngāti Hei), Michelle Azar, Aiden Azar, Dr Ned Azar and Ashleigh Battaerd (nurse practitioner at Te Korowai in Whitianga) with her son, Lex. Read the story on page 3. Distributed throughout the Coromandel Peninsula, coast to coast from Thames to north of Colville - www.theinformer.co.nz Several Mercury Bay Golf Club buildings destroyed in fire Only a week after putting out a blaze that destroyed a house in Whitianga, the Whitianga Hahei) as well as the Cooks Beach Brigade’s water tanker were on the scene. Volunteer Fire Brigade were on Saturday last week again called to a building on fire, this time Fire and Emergency New Zealand investigated the scene last Sunday morning. at the Mercury Bay Golf Club. The Mercury Bay Golf Course was closed on Sunday, but reopened for play on Monday this week. With the help of the Cooks Beach and Hahei Volunteer Fire Brigades the fire was successfully In an email sent to Mercury Bay Golf Club members on Sunday, Graham Eccles, club president extinguished, but unfortunately the greenkeeper’s shed, members’ trundler shed and main golf asked all members to give the club greenkeeper “…space as things will not be operating for cart shed have been destroyed. The equipment, golf clubs and golf carts inside the sheds have him as normal.” also been destroyed. Pictured in the photo on the left is former Whitianga fire chief, Merv George, on the scene on Putting the fire out hasn’t been without challenges as several fuel tanks were close to the flames. Saturday. In the photo on the right is Whitianga Station Officer Julian Lee (left) and Hahei Chief At one time four fire appliances (two from Whitianga and one each from Cooks Beach and Fire Office Ian Carter keeping an eye on things. What’s happening in the night sky? Night sky information provided and sponsored by Week of Wednesday, 20 January to Wednesday, 27 January - Summer is the time of the wonderful constellation Orion, the hunter, in the evening sky. It is a huge constellation with the distinctly pinkish star Betelgeuse at its lower right, just below the part of it we call “The Pot.” This star is actually an enormous red giant and if placed where the Sun is would extend out to Jupiter with the planets Mercury, Venus, Earth and Mars all inside it. However, the most pinkish object in the sky now is actually Mars, the “red planet,” which is getting rapidly further from us in its two year orbit around the Sun and can be seen low in the northern sky. The International Space Station (ISS) makes some early morning passes this week. Wednesday, 20 January - A first quarter Moon lies directly to the left of reddish Mars in the evening. Thursday, 21 January - The Moon is now directly above reddish Mars all evening. Friday, 22 January - The Moon can be found about halfway between Mars on the left and the Pleiades or Mataraki on Astronomy Tours and B&B the right in the evening. Saturday, 23 January - Early risers can see the ISS from 5:51am in the NW eventually passing right beside Venus. In the evening Phone (07) 866 5343 Matariki lies just below an increasingly bright Moon. Sunday, 24 January - Faint Mercury is at its furthest from the Sun tonight and might be visible very low in the west just after sunset. Tuesday, 26 January - The ISS makes a bright pass from 5:05am in the NW, passing high overhead. www.stargazersbb.com Whitianga and Hot Water Beach tides Tides data sponsored by nzwindows.co.nz 4 Dakota Drive Whitianga Wednesday Thursday Friday Saturday Sunday Monday Tuesday Wednesday Tel 07 869 5990 Page 2 The Mercury Bay Informer - www.theinformer.co.nz Issue 933 - 19 January 2021 New Te Korowai doctor welcomed with pōwhiri By Stephan Bosman Dr Ned Azar and his family were welcomed doing their own thing and the kids are mostly to Mercury Bay with a small pōwhiri at theon their phones or in front of their computers. Wharekaho marae on Saturday last week. We knew from first-hand experience that life on Ned will be working as a GP alongside nurse the Coromandel has so much more to offer.” practitioner, Ashleigh Battaerd, at Te Korowai Once the decision was made to move back to Hauora o Hauraki in Whitianga. New Zealand, Ned started looking at available Te Korowai was established by the Hauraki opportunities on the Peninsula. Te Korowai was Māori Trust Board in the mid-1990s. One of the one of his first ports of call. “I loved being part of organisation’s general goals is to “…enhance Te Korowai before,” he said. “The organisation the quality of life of all whānau, hapu, iwi,has a genuine desire to see everyone in the their friends and other persons living within Hauraki area, including the Coromandel, the traditional tribal boundaries of Hauraki.” healthy and happy. Staff and patients are all In addition to Whitianga, the organisation has treated like family. It was fortunate that the offices and clinics in Thames, Paeroa, Te Aroha expected growth in patient numbers stimulated and Coromandel Town. discussions about a GP joining the team at Te In explaining the pōwhiri to everyone present Korowai in Whitianga and I was delighted when on Saturday, Ngāti Hei rangatira, Joe Davis, I was offered a position.” said Ned is the first doctor to join Te Korowai With the coronavirus pandemic still raging in Whitianga and his arrival in Mercury Bay around the world, the family are relieved to be signals a special moment for tangata whenua. in New Zealand. “COVID-19 didn’t influence Following the pōwhiri, everyone enjoyed our decision to come to New Zealand, but now lunch and The Informer have had an opportunity being able to see for ourselves how normal to talk to Ned, his wife, Michelle, and their life is here compared to the UK is even more 11-year-old son, Aiden. The family arrived inconfirmation that we’ve done the right thing,” managed isolation in Auckland from the United said Michelle. Kingdom, their home country, just before Ned agreed. “I’m not much into politics, Christmas last year. It’s not their first time in but the current government in the UK has a lot New Zealand. “I worked for Te Korowai in to answer for,” he said. “They could have done Thames from November 2015 to February much better in the management of the pandemic. 2017,” said Ned. “We’ve moved from ThamesThe New Zealand government has done an to Havelock North for another eight months outstanding job and, as a result, Kiwis are able before returning to the UK late in 2017.” to enjoy summer with almost no restrictions to Michelle first raised the idea of returningspeak of.” to New Zealand with Ned early last year. Not even two weeks out of managed isolation “The Coromandel made a huge impression on and Aiden is already making the most of the us,” said Michelle. “It’s in a roundabout way Coromandel summer. He has completed a surf good that we spent some time in Hawkes Bay lifesaving summer programme in Tairua and is during our first time in New Zealand as it made talking about his ideal surfboard. “Aiden is keen us realise just how special the Peninsula is.” to get into diving too,” said Ned. “I guess it’s Ned said Aiden is an outdoors child who time to become a real Kiwi dad and get a ute. loves the water. “In the UK, families are That will make transporting all the gear around disconnected,” he said. “Everyone is justso much easier.” Issue 699933 - 2719 JulyJanuary 2016 2021 The Mercury Bay Informer - www.theinformer.co.nz Page 3 Whiti Fest summer busking festival to liven up the streets of Whitianga A contribution by Creative Mercury Bay In just over two weeks a new performing Other locations will feature a range of acts, Bay, says the team is excited to share Whiti Fest “Whiti Fest wouldn’t be possible without arts event will hit the streets of Whitianga - some from Mercury Bay’s talented youth with the Mercury Bay community. “We have funding from the Creative Communities Whiti Fest, Mercury Bay’s first busking festival. performers, including 10-year-old violinistbeen absolutely blown away by the number Scheme and Pub Charity,” says Anusha. Whiti Fest will take place on Sunday, Dashiell Wallace, 17-year-old ukulele playerof registrations from performers,” she says. “We are very appreciative to both funding 7 February (Waitangi Day long weekend) from Charli MacDougall and pianist Sarah Morcom. “As a team we have selected a variety of local bodies for their support. The hope is that we 10:30am to 3:30pm across five locations in Some favourites from Creative Mercury performing artists to make Whiti Fest a true can make Whiti Fest an annual tradition in the Whitianga Town Centre. Proudly brought Bay’s successful Bubble Bites series are celebration of the performing arts.” Mercury Bay.” to you by Creative Mercury Bay, the event also performing - poet and artist Pete Delete,Each performer will be paid a modest fee for Creative Mercury Bay’s main purpose will showcase a wide range of performing soul/blues duo Soul Sax and freestyle rock ‘n their performance and like a traditional busking is to facilitate performing arts events that artists from the Mercury Bay area, including roll blues guitarist Scott Burst.
Recommended publications
  • Geology of Fanal Island (Motukino), Outer Hauraki Gulf, North Auckland
    TANE 26,1980 GEOLOGY OF FANAL ISLAND (MOTUKINO), OUTER HAURAKI GULF, NORTH AUCKLAND by G.H. Browne and DA. Greig Department of Geology, University of Auckland, Private Bag, Auckland SUMMARY Fanal Island (Motukino) consists of thin flow banded rhyolite of presumed Pliocene age. The island represents the southern and western remnant of a cumulo-dome, whose northern portion has been eroded by the sea. The rocks of the island (Fanal Formation) are subdivided into a basal Flow Banded Member (new) and an upper Agglomerate Member (new). The distinction between the rhyolitic lithologies of Burgess and Fanal Islands is not considered as significant as previous authors. Two phases of concentric folding are recognised and their relationships described. Joint orientations are probably of igneous origin. INTRODUCTION AND GEOLOGICAL SETTING Fanal Island is the eastern-most and largest island of the Mokohinau group of islands, lying northwest of Great Barrier Island in the Hauraki Gulf, some 105 kilometres from Auckland City. The May 1979 A.U.F.C. scientific camp provided an opportunity to examine the geology of the island. The Mokohinaus form part of a long discontinuous chain of rhyolitic volcanics that outcrop within the Coromandel Volcanic Zone (Fig. 1). This northerly trending belt, extends from the Poor Knights Group in the north to the Aldermen Islands in the south, a distance of some 210 kilometres, and is equivalent to the Whitianga Arc of Ballance (1976) which was active some 6 to 3 m.y. ago. Kear (1964) had previously included Mayor Island within this rhyolitic chain, but Cole (1978) has argued that Mayor Island was part of a separate north-east trending tensional graben structure known as the Ngatoro Basin.
    [Show full text]
  • Of New Zealand Volume 31 Part 3 September 1984
    NOTORNIS Journal of the Ornithological Society of New Zealand Volume 31 Part 3 September 1984 OFFICERS 1984 - 85 President - B. BROWN, 20 Redmount Place, Red Hill, Papakura Vice-president - R. B. SIBSON, 580 Remuera Road, Auckland 5 Editor - B. D. HEATHER, 10 Jocelyn Crescent, Silverstream Treasurer - D. F. BOOTH, P.O. Box 35337, Browns Bay, Auckland 10 Secretary - R. S. SLACK, c/o P.O., Pauatahanui, Wellington Council Members: SEN D. BELL, Zoology Dept, Victoria University, Private Bag, Wellington BRIAN D. BELL, 9 Ferry Road, Seatoun, Wellington P. C. BULL, 131A Waterloo Road, Lower Hutt D. E. CROCKETT, 21 McMilIan Avenue, Kamo, Whangarei P. D. GAZE, Ecology Division, DSIR, Private Bag, Nelson J. HAWKINS, 772 Atawhai Drive, Nelson P. M. SAGAR, 38A Yardley Street, Christchurch 4 Conveners and Organisers: Rare Birds Committee: Secretary, J. F. M. FENNELL, 224 Horndon Street, DarfieId, Canterbury Beach Patrol: R. G. POWLESLAND, Wildlife Service, Dept. of Internal Affairs, Private Bag, Wellington Librarian: A. 3. GOODWIN, R.D. 1, Clevedon Nest Records: D. E. CROCKETT Classified Summarised Notes - North Island: L. HOWELL, P.O. Box 57, Kaitaia South Island: P. D. GAZE, Ecology Division, DSIR, Private Bag, Nelson S.W. Pacific Islands Records: J. L. MOORE, 32 Brook St, Lower Hutt Assistant Editor: A. BLACKBURN, 10 Score Road, Gisborne Reviews Editor: D. H. BRATHWAITE, P.O. Box 31022 Ilam, Christchurch 4 Editor of OSNZ news: P. SAGAR, 38A Yardley St, Christchurch 4 SUBSCRIPTIONS AND MEMBERSHIP Annual Subscription: Ordinary member $20; Husband & wife mem- bers $30; Junior member (under 20) $15; Life Member $400; Family member (one Notornis per household) being other family of a member in the same household as a member $10; Institution $40; Overseas member and overseas institution $5.00 extra (postage).
    [Show full text]
  • “Revitalising the Gulf” Plan by Stephan Bosman and Lachie Harvey
    Issue 956 - 29 June 2021 Phone (07) 866 2090 Circulation 8,000 Not everyone happy with government’s “Revitalising the Gulf” plan By Stephan Bosman and Lachie Harvey This aerial photo was taken overhead Te Whanganui-A-Hei Marine Reserve on Saturday last week. Under the “Revitalising the Gulf - Government Action on the Sea Change Plan” document that was released early last week, the marine reserve will be extended by an additional 14km². A plan to better protect the Hauraki Gulf Whitianga over Queen’s Birthday Weekend seaboard of the Peninsula. Two large areas to to marine reserves, but will allow for (an area covering 1.2 million hectares from addressing the state of the ocean surrounding the north and south of the Alderman Islands customary take. In addition to trawl fishing, north of Auckland to Waihi Beach, including the Coromandel. and the waters surrounding Slipper Island sand extraction and mining will be prohibited the Waitemata Harbour, the Firth of Thames, According to the document, the will be classified as “High protection Areas”, in Seafloor Protection Areas. Great Barrier Island and the east coast of the government’s plan has two primary and Te Whanganui-A-Hei Marine Reserve According to the government, the most Coromandel Peninsula) may finally be on the goals - to provide effective kaitiakitanga at Cathedral Cove will be extended by an notable benefits of the document will be horizon. Central government released early (guardianship) of the Hauraki Gulf, along additional 14km². an increase in the shellfish population, last week a document setting out their goals with healthy functioning ecosystems.
    [Show full text]
  • Archaeological Site Survey of Shoe Island and the Slipper Island Group
    TANE 21, 1975 ARCHAEOLOGICAL SITE SURVEY OF SHOE ISLAND AND THE SLIPPER ISLAND GROUP by E. Gael Atwell*, J.R.H. Spencer f, Gillian F. Puch** and P.R. Moore ft SUMMARY Twenty archaeological sites were recorded on Shoe Island and the Slipper Island Group. Of these, sixteen are new records. Evidence of former Maori occupation is found in the form of pa, pits, terracing, midden, obsidian and other artifacts. With its ready access to fresh water, suitable agricultural areas, coastal resources, and excellent defensive positions, Slipper Island appears to have been permanently occupied by the Maoris. INTRODUCTION Descriptions of archaeological sites on the Slipper and Shoe Island Group were compiled during the A.U.F.C. Scientific Camp in August 1973. Records for Slipper Island, where the main camp was set up, are the most detailed. However, a two day trip to Shoe Island by P.R. Moore and one day trips to Rabbit and Penguin Islands by B.W. Hawyard and others provided observations testifying to their occupation by the Maori. Although some detailed survey work was carried out, the main aim was to provide a more complete coverage of sites than was previously on file in the records of the New Zealand Archaeological Association (N.Z.A.A.). They would not only fill in a small gap in the growing record of sites on islands along, the East Coast but would also provide a basis for any further work in this group. PREVIOUS WORK. Of the four islands mentioned above, only on Slipper Island has evidence been recorded of a resident Maori population prior to European contact.
    [Show full text]
  • Coromandel Town Whitianga Hahei/Hotwater Tairua Pauanui Whangamata Waihi Paeroa
    Discover that HOMEGROWN in ~ THE COROMANDEL good for your soul Produce, Restaurants, Cafes & Arts moment OFFICIAL VISITOR GUIDE REFER TO CENTRE FOLDOUT www.thecoromandel.com Hauraki Rail Trail, Karangahake Gorge KEY Marine Reserve Walks Golf Course Gold Heritage Fishing Information Centres Surfing Cycleway Airports Kauri Heritage Camping CAPE COLVILLE Fletcher Bay PORT JACKSON COASTAL WALKWAY Stony Bay MOEHAU RANGE Sandy Bay Fantail Bay PORT CHARLES HAURAKI GULF Waikawau Bay Otautu Bay COLVILLE Amodeo Bay Kennedy Bay Papa Aroha NEW CHUM BEACH KUAOTUNU Otama Shelly Beach MATARANGI BAY Beach WHANGAPOUA BEACH Long Bay Opito Bay COROMANDEL Coromandel Harbour To Auckland TOWN Waitaia Bay PASSENGER FERRY Te Kouma Te Kouma Harbour WHITIANGA Mercury Bay Manaia Harbour Manaia 309 Cooks Marine Reserve Kauris Beach Ferry CATHEDRAL COVE Landing HAHEI COROMANDEL RANGE Waikawau HOT WATER COROGLEN BEACH 25 WHENUAKITE Orere 25 Point TAPU Sailors Grave Rangihau Square Valley Te Karo Bay WAIOMU Kauri TE PURU TAIRUA To Auckland Pinnacles Broken PAUANUI 70km KAIAUA Hut Hills Hikuai DOC PINNACLES Puketui Tararu Info WALK Shorebird Coast Centre Slipper Island 1 FIRTH (Whakahau) OF THAMES THAMES Kauaeranga Valley OPOUTERE Pukorokoro/Miranda 25a Kopu ONEMANA MARAMARUA 25 Pipiroa To Auckland Kopuarahi Waitakaruru 2 WHANGAMATA Hauraki Plains Maratoto Valley Wentworth 2 NGATEA Mangatarata Valley Whenuakura Island 25 27 Kerepehi Hikutaia Kopuatai HAURAKI 26 Waimama Bay Wet Lands RAIL TRAIL Whiritoa To Rotorua/ Netherton Taupo PAEROA Waikino Mackaytown WAIHI 2 OROKAWA
    [Show full text]
  • Coromandel Harbour the COROMANDEL There Are Many Beautiful Places in the World, Only a Few Can Be Described As Truly Special
    FREE OFFICIAL VISITOR GUIDE www.thecoromandel.com Coromandel Harbour THE COROMANDEL There are many beautiful places in the world, only a few can be described as truly special. With a thousand natural hideaways to enjoy, gorgeous beaches, dramatic rainforests, friendly people and fantastic fresh food The Coromandel experience is truly unique and not to be missed. The Coromandel, New Zealanders’ favourite destination, is within an hour and a half drive of the major centres of Auckland and Hamilton and their International Airports, and yet the region is a world away from the hustle and bustle of city life. Drive, sail or fly to The Coromandel and bunk down on nature’s doorstep while catching up with locals who love to show you why The Coromandel is good for your soul. CONTENTS Regional Map 4 - 5 Our Towns 6 - 15 Our Region 16 - 26 Walks 27 - 32 3 On & Around the Water 33 - 40 Other Activities 41 - 48 Homegrown Cuisine 49 - 54 Tours & Transport 55 - 57 Accommodation 59 - 70 Events 71 - 73 Local Radio Stations 74 DISCLAIMER: While all care has been taken in preparing this publication, Destination Coromandel accepts no responsibility for any errors, omissions or the offers or details of operator listings. Prices, timetables and other details or terms of business may change without notice. Published Oct 2015. Destination Coromandel PO Box 592, Thames, New Zealand P 07 868 0017 F 07 868 5986 E [email protected] W www.thecoromandel.com Cover Photo: Northern Coromandel CAPE COLVILLE Fletcher Bay PORT JACKSON Stony Bay The Coromandel ‘Must Do’s’ MOEHAU RANG Sandy Bay Fantail Bay Cathedral Cove PORT CHARLES Hot Water Beach E The Pinnacles Karangahake Gorge Waik New Chum Beach Otautu Bay Hauraki Rail Trail Gold Discovery COLVILLE plus so much more..
    [Show full text]
  • 69 G E O L O G Y of T H E a L D E R M E N ISLANDS By
    69 GEOLOGY OF THE ALDERMEN ISLANDS by B.W. Hayward* and P.R. Moore* SUMMARY The Aldermen Islands are the much eroded remnants of a once far larger complex of rhyolite domes, associated ignimbrites and pyroclastic sediments. The majority of rocks present are rhyolitic lavas and pyroclastic sediments of the Whitianga Group (Pliocene in age) which unconformably overlie (Miocene - lower Pliocene) andesitic Beesons Island Volcanics. Whitianga rocks comprise five intrusive and extrusive domes of the Minden Rhyolite Subgroup, intruded along an east-west trending line from Ruamahua-nui to Hongiora. Remains of coulees that are inferred to have been derived from these domes are exposed on islands to the north and south of this line. Pyroclastic flows, tephra showers and breccia flows of this rhyolitic eruptive period have formed the widely varied deposits of the Coroglen Subgroup exposed on most islands. INTRODUCTION This island group, situated 18 km east of Tairua, off the east coast of the Coromandel Peninsula consists of four main islands and six smaller ones, and scores of rocky islets (Hayward, 1973). A geological survey of the Aldermen Islands was carried out by the authors during the seven day Auckland University Field Club Scientific Camp in May 1972. Rock specimen numbers referred to are those of the petrology collections of the Geology Department, University of Auckland, and fossil record numbers are those allotted in the archival N.Z. Fossil Record File. PREVIOUS WORK Prior to this study, very little was known of the geology of these islands. Sladden and Falla (1927) presented a short report by J.A.
    [Show full text]
  • Ecological Restoration of New Zealand Islands
    CONTENTS Introduction D.R. Towns, I.A.E. Atkinson, and C.H. Daugherty .... ... .. .... .. .... ... .... ... .... .... iii SECTION I: RESOURCES AND MANAGEMENT New Zealand as an archipelago: An international perspective Jared M. Diamond . 3 The significance of the biological resources of New Zealand islands for ecological restoration C.H. Daugherty, D.R. Towns, I.A.E. Atkinson, G.W. Gibbs . 9 The significance of island reserves for ecological restoration of marine communities W.J.Ballantine. 22 Reconstructing the ambiguous: Can island ecosystems be restored? Daniel Simberloff. 37 How representative can restored islands really be? An analysis of climo-edaphic environments in New Zealand Colin D. Meurk and Paul M. Blaschke . 52 Ecological restoration on islands: Prerequisites for success I.A.E Atkinson . 73 The potential for ecological restoration in the Mercury Islands D.R. Towns, I.A.E. Atkinson, C.H. Daugherty . 91 Motuhora: A whale of an island S. Smale and K. Owen . ... ... .. ... .... .. ... .. ... ... ... ... ... .... ... .... ..... 109 Mana Island revegetation: Data from late Holocene pollen analysis P.I. Chester and J.I. Raine ... ... ... .... .... ... .. ... .. .... ... .... .. .... ..... 113 The silent majority: A plea for the consideration of invertebrates in New Zealand island management - George W. Gibbs .. ... .. ... .. .... ... .. .... ... .. ... ... ... ... .... ... ..... ..... 123 Community effects of biological introductions and their implications for restoration Daniel Simberloff . 128 Eradication of introduced animals from the islands of New Zealand C.R. Veitch and Brian D. Bell . 137 Mapara: Island management "mainland" style Alan Saunders . 147 Key archaeological features of the offshore islands of New Zealand Janet Davidson . .. ... ... ... .. ... ... .. .... ... .. ... .. .... .. ..... .. .... ...... 150 Potential for ecological restoration of islands for indigenous fauna and flora John L. Craig .. .. ... .. ... ... ... .... .. ... ... .. ... .. .... ... ... .... .... ..... .. 156 Public involvement in island restoration Mark Bellingham .
    [Show full text]
  • Tane 22, 1976 Geology of the Whitianga Group, Great Mercury Island
    TANE 22, 1976 GEOLOGY OF THE WHITIANGA GROUP, GREAT MERCURY ISLAND - PART I. COROGLEN SUBGROUP STRATIGRAPHY by B.W. Hayward Department of Geology, University of Auckland, Private Bag, Auckland (Present address: Paleobiology Dept., Smithsonian Institute, Washington D.C. 20560, U.S.A.) SUMMARY A 250m thick, lensing sequence of rhyolitic pyroclastites, epiclastites and pyroclastic flow deposits (Coroglen Subgroup) overlies an irregular surface of older andesites on Great Mercury Island. Deposition was mostly subaerial, but occasionally fluviatile or lacustrine; the source being volcanic vents at the southern end of the island. Rhyolite domes intruded the Coroglen rocks and extruded flows both during and after their deposition. Minor basalt was also erupted contemporaneously with the rhyolite. INTRODUCTION Great Mercury Island lies off the east coast of Coromandel Peninsula (Fig. 1), 20km east of Kennedys Bay. The geology was first studied by Professor R.N. Brothers in the early 1950's but his results have never been published, although they formed the basis of Schofield's (1967) 1:250,000 map. Recently, Skinner (in press) has compiled a 1:63,360 map "from aerial photos using unpublished field data and samples collected by Professor R.N. Brothers." Field work for the present paper was carried out during the A.U.F.C. scientific trip in May 1975. Using the earlier maps of Brothers and Skinner as a base, the study was directed towards resolving some of the discrepancies between the two and towards accurately mapping the outcrop and studying the stratigraphy of the Whitianga Group pyroclastics (Coroglen Subgroup). Needless to say this study has shown that photogeology is no match for actual field observations.
    [Show full text]
  • HOMEGROWN in the COROMANDEL
    HOMEGROWN in THE COROMANDEL OFFICIAL VISITOR GUIDE REFER TO CENTRE FOLDOUT www.thecoromandel.com Hauraki Rail Trail, Karangahake Gorge CAPE COLVILLE Fletcher Bay PORT JACKSON COASTAL WALKWAY Stony Bay MOEHAU RANGE Sandy Bay Fantail Bay PORT CHARLES HAURAKI GULF Waikawau Bay Otautu Bay COLVILLE Amodeo Bay Kennedy Bay Papa Aroha NEW CHUM BEACH KUAOTUNU Otama Shelly Beach MATARANGI BAY Beach WHANGAPOUA BEACH Long Bay Opito Bay COROMANDEL Coromandel Harbour To Auckland TOWN Waitaia Bay PASSENGER FERRY Te Kouma Te Kouma Harbour WHITIANGA Mercury Bay Manaia Harbour Manaia 309 Cooks Marine Reserve Kauris Beach Ferry CATHEDRAL COVE Landing HAHEI C OROMANDEL RANGE Waikawau HOT WATER COROGLEN BEACH 25 WHENUAKITE Orere 25 Point TAPU Sailors Grave Rangihau Square Valley Te Karo Bay WAIOMU Kauri TE PURU TAIRUA To Auckland Pinnacles Broken PAUANUI 70km KAIAUA Hut Hills Hikuai DOC PINNACLES Puketui Tararu Info WALK Shorebird Coast Centre Slipper Island 1 FIRTH (Whakahau) OF THAMES THAMES Kauaeranga Valley OPOUTERE Pukorokoro/Miranda 25a Kopu ONEMANA MARAMARUA Pipiroa 25 To Auckland Waitakaruru Kopuarahi 2 WHANGAMATA Hauraki Plains Maratoto Valley Wentworth 2 NGATEA Mangatarata Valley Whenuakura Island 25 27 Kerepehi Hikutaia Kopuatai HAURAKI 26 Waimama Bay Wet Lands RAIL TRAIL Whiritoa To Rotorua/ Netherton Taupo PAEROA Waikino Mackaytown WAIHI 2 OROKAWA BAY Tirohia KARANGAHAKE GORGE Waitawheta WAIHI BEACH Athenree KEY Kaimai Marine Reserve Walks Golf Course Forest Park Bowentown Gold Heritage Fishing Information Centres Surfing Cycleway Airports TE AROHA To Tauranga 70km Kauri Heritage Camping life asitshouldbe. slow downandreconnectwith abreak, it’s time to relax.Take selling homegrown foodandart, and meetingcreativelocals you. Aftersomeretailtherapy perfect, becauseit’s allabout The Coromandel is a prescription for your own own your is aprescriptionfor wellbeing.
    [Show full text]
  • Protecting the Hauraki Gulf Islands
    PROTECTING THE HAURAKI GULF ISLANDS Raewyn Peart and Cordelia Woodhouse PROTECTING THE HAURAKI GULF ISLANDS Raewyn Peart and Cordelia Woodhouse First published November 2020 Published by: Environmental Defence Society Incorporated P O Box 91736 Victoria St West Auckland 1142 Phone (09) 302 2972 [email protected] www.eds.org.nz www.environmentguide.org.nz © Environmental Defence Society Incorporated 2020 Design: Neale Wills, Wilsy Design & Production Ltd Photographic images: Raewyn Peart unless otherwise indicated Cover image: Palmers Beach, Aotea/Great Barrier Island Copies can be downloaded from www.eds.org.nz ACKNOWLEDGEMENTS We would like to acknowledge the support of Auckland Council in funding this case study. We would also like to thank all those who generously agreed to be interviewed for this study and the peer reviewers for their invaluable contributions. This case study will form part of a report being supported by the Department of Conservation and Land Information New Zealand. ii PROTECTING THE WAITĀKERE RANGES TABLE OF CONTENTS 1 Introduction 1 PART ONE: OVERALL CONTEXT 3 2 The Hauraki Gulf 3 2.1 Geological formation of islands 3 2.2 Early Māori settlement 4 2.3 Early European settlement 4 3 Statutory management framework 5 3.1 Resource Management Act 5 3.2 National instruments 9 3.3 Hauraki Gulf Marine Park Act 10 3.4 Regional instruments 15 3.5 District instruments 17 3.6 Incorporation of the Hauraki Gulf islands into the Auckland Unitary Plan framework 19 PART TWO: ISLAND CASE STUDIES 21 4 Aotea/Great Barrier Island 21
    [Show full text]
  • Generalised Geology of Shoe Island, the Slipper Island Group and Part of the Mainland
    Fig. 1: Generalised geology of Shoe Island, the Slipper Island Group and part of the mainland. Bathymetric contours are shown together with inferred stream courses during lower sea-levels of the Last Glaciation. The inferred position of the Paku, Shoe and Watchman Rock rhyolite domes and North Trig andesite cone are shown. 42 TANE 20 1974 GEOLOGY OF SHOE ISLAND AND THE SLIPPER ISLAND GROUP by B.W. Hayward*, P.R. Moore*t, D.A.B. MacFarlan* SUMMARY Shoe Island and Watchman Rock are the eroded remnants of hypersthene rhyolite domes (Minden Rhyolite Subgroup; Pliocene-Pleistocene age). Slipper Formation is proposed for the two-pyroxene andesites of Slipper, Penguin and Rabbit Islands. This Formation (Pliocene-Pleistocene age) consists of three members: (a) a shallow intrusion having a minimum outcrop area of 7km2 ;(b) interbedded flows and scoriaceous breccia conformably overlain by (c) sub- aerially bedded pyroclastics. These last two members are the western remnants of a former andesite cone. INTRODUCTION Shoe Island and the Slipper Island Group lie off the east coast of the Coromandel Peninsula, 3-8km from Tairua (Fig. 1). The Slipper Island Group has previously been mapped as Minden Rhyolite5, possible Beesons Island Volcanics3 and Miocene andesite2. Shoe Island is recorded as rhyolite on all these maps. The islands were mapped by the authors during the A.U.F.C. scientific camp in August 1973 — Slipper Island by D.A.B.M. and P.R.M., Penguin and Rabbit Islands by B.W.H., and Shoe Island by P.R.M. Rock specimen numbers refer to the petrology collection of the University of Auckland Geology Department and the fossil record number is that of the N.Z.
    [Show full text]