Report 96-214 Collision Between the Container Vessel Sydney Express
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TE ARA O NGA TUPUNA HERITAGE TRAIL MAIN FEATURES of the TRAIL: This Trail Will Take About Four Hours to Drive and View at an Easy TE ARA O NGA TUPUNA Pace
WELLINGTON’S TE ARA O NGA TUPUNA HERITAGE TRAIL MAIN FEATURES OF THE TRAIL: This trail will take about four hours to drive and view at an easy TE ARA O NGA TUPUNA pace. Vantage points are mostly accessible by wheelchair but there are steps at some sites such as Rangitatau and Uruhau pa. A Pou (carved post), a rock or an information panel mark various sites on the trail. These sites have been identified with a symbol. While the trail participants will appreciate that many of the traditional sites occupied by Maori in the past have either been built over or destroyed, but they still have a strong spiritual presence. There are several more modern Maori buildings such as Pipitea Marae and Tapu Te Ranga Marae, to give trail participants a selection of Maori sites through different periods of history. ABOUT THE TRAIL: The trail starts at the Pipitea Marae in Thorndon Quay, opposite the Railway Station, and finishes at Owhiro Bay on the often wild, southern coast of Wellington. While not all the old pa, kainga, cultivation and burial sites of Wellington have been included in this trail, those that are have been selected for their accessibility to the public, and their viewing interest. Rock Pou Information panel Alexander Turnbull Library The Wellington City Council is grateful for the significant contribution made by the original heritage Trails comittee to the development of this trail — Oroya Day, Sallie Hill, Ken Scadden and Con Flinkenberg. Historical research: Matene Love, Miria Pomare, Roger Whelan Author: Matene Love This trail was developed as a joint project between Wellingtion City Council, the Wellington Tenths Trust and Ngati Toa. -
Elegant Report
C U L T U R A L IMPACT R E P O R T Wellington Airport Limited – South Runway extension Rongotai – Hue te Taka IN ASSOCIATION WITH PORT NICHOLSON BLOCK SETTLEMENT TRUST, WELLINGTON TENTHS TRUST AND TE ATIAWA KI TE UPOKO O TE IKA A MAUI POTIKI TRUST (MIO) OCTOBER 2015 CULTURAL IMPACT REPORT Wellington Airport – South Runway extension RONGOTAI – HUE TE TAKA TABLE OF CONTENTS EXECUTIVE SUMMARY ...........................................................................................................................3 THE PROJECT .............................................................................................................................................4 KEY MAORI VALUES ASSOCIATED WITH THIS AREA ..................................................................6 FISHING AND FISHERIES IN THE AREA ...........................................................................................................8 MARINE FLORA .......................................................................................................................................... 10 BLACK-BACKED GULLS ............................................................................................................................. 10 WATER QUALITY........................................................................................................................................ 11 Consultation .......................................................................................................................................... 12 RECREATION USE OF THE -
CTENOPHORA Comb Jellies
THREE Phylum CTENOPHORA comb jellies HERMES MIANZAN, ELLIOT W. Dawson, CLAUDIA E. MILLS tenophores have been described as the most beautiful, delicate, seem- ingly innocent yet most voracious, sinister and destructive of plankton Corganisms. They are exclusively marine, are found in all oceans at all depths, have many different shapes, and range in size from a few millimetres diameter to two metres long. They are mostly planktonic, but one order is bottom- dwelling with a creeping mode of existence. The planktonic forms are stunningly beautiful, diaphanous creatures, flashing iridescence as their comb-like cilia plates catch the light. Their bodies are soft, fragile, gelatinous. The phylum is small and well defined, with about 150 species worldwide (Mills 2008). Like the Cnidaria, they are radiate animals and at one time the two phyla were linked together as the Coelenterata. Ctenophoran symmetry is biradial and the general body plan somewhat more complicated than that of Cnidaria (Harbison & Madin 1982; Mills & Miller 1984; Harbison 1985). The two phyla are now thought to be only very distantly related. Recent evidence from ribosomal RNA sequencing shows that the Ctenophora lie close to the Porifera as the second-most-basic group of the Metazoa (Bridge et al. 1995; Collins 1998; Podar et al. 2001). Similarity in body form between pelagic ctenophores and medusae is a phenomenon of convergence. Ctenophores (literally, comb bearers) are named for their eight symmetrical tracks (comb rows) of fused ciliary plates (ctenes) on the body surface (Hernán- dez-Nicaise & Franc 1993). These constitute the locomotory apparatus that Leucothea sp. characterises the group. -
AN ACT of GOD Gusting to 60 Knots at Pipitea Wharf
time it was not normal to maintain a 24 hour ripping out the starboard propeller and shaft radio watch while the ferries were at sea, and and punching a hole into the engineroom. With THE WAHINE DISASTER – weather updates were often missed. no power, Captain Robertson ordered both On approaching the entrance to Wellington anchors to be dropped manually. This took Harbour, Captain Robertson contacted the some 45 minutes as the ship ground against pilot station on Beacon Hill via VHF, and the reef as she drifted further into the harbour, MORE heard there was a southerly of 50 knots, making more holes and taking on water. AN ACT OF GOD gusting to 60 knots at Pipitea Wharf. A tug Unfortunately, tragedy and sadness followed, POWER had been called out for another ship to be and there were heroic actions by many, as the BY KEITH INGRAM moved in the harbour and would be available story of the Wahine disaster is well documented. if the Wahine required her for berthing. This But what have we learnt from this disaster? MORE was not unusual for Wellington, which has Fifty-one lives lost is an expensive lesson. a reputation of presenting ferry masters with Clearly the country, and Wellington in FREEDOM some challenging times as they try to maintain particular, was not geared up to respond to this From the most the timetable and navigate their ships in and type of shipping disaster. Yes, a brave fleet of out of Wellington’s harbour. small, recreational craft did set sail to assist powerful inverter As the captain committed the ship to enter once it was realised that the survivors were charger available! the harbour, the weather quickly closed in, the being dragged across the harbour to the rugged wind intensity built and all visibility was lost shores of the Pencarrow coast. -
MARICO Marine NZ Limited WELLINGTON HARBOUR PORT
WELLINGTON HARBOUR PORT AND HARBOUR MARINE SAFETY CODE NAVIGATIONAL RISK ASSESSMENT Prepared For : Greater Wellington Regional Council and CentrePort Ltd Report Number : 05NZ104 Issue : 1.1 : February 2006 MARICO Marine NZ Limited Report No: 05NZ104 WELLINGTON HARBOUR Issue: Issue 1.1 Operational Risk Assessment WELLINGTON HARBOUR PORT AND HARBOUR MARINE SAFETY CODE NAVIGATIONAL RISK ASSESSMENT Prepared for: Greater Wellington Regional Council PO Box 11646 142 Wakefield Street Wellington CentrePort Ltd CentrePort House Hinemoa Street Wellington Authors: Will Lins and John Riding Checked By: Gordon Wood/Antony Dingle MARICO Marine NZ Limited 56 Kents Road Reikorangi Waikane February 2006 05NZ104_Issue1-1 Page: i Report No: 05NZ104 WELLINGTON HARBOUR Issue: Issue 1.1 Operational Risk Assessment CONTENTS EXECUTIVE SUMMARY 1 INTRODUCTION 1 1.1 PURPOSE AND SCOPE 1 1.2 PREVIOUS RISK ASSESSMENTS OF RELEVANCE 2 2 METHODOLOGY 3 2.1 INTERVIEWS AND FAMILIARISATION TRIPS 3 2.2 INCIDENT DATA AND DOCUMENT REVIEW 4 2.3 HAZID MEETINGS AND WORKSHOPS 5 2.4 RISK ASSESSMENT SCORING 5 2.5 IDENTIFICATION OF RISK CONTROL MEASURES 6 2.6 RISK MANAGEMENT SOFTWARE UTILISED 6 3 CRITERIA FOR DEVELOPMENT OF RISK MANAGEMENT 7 3.1 RISK MANAGEMENT DEFINITIONS 7 3.2 RISK MITIGATION ACTION CRITERIA 9 4 WELLINGTON HARBOUR - OVERVIEW AND TRAFFIC PROFILE 12 4.1 HARBOUR LIMITS AND PILOTAGE DISTRICT 14 4.2 WELLINGTON HARBOUR – CLIMATOLOGY 16 4.3 SEISMIC AND WAVE CONSIDERATIONS – TSUNAMI, SEICHES AND LONG WAVES 17 4.4 WELLINGTON TRAFFIC PROFILE 17 4.5 OTHER VESSEL TRENDS OF -
Eastern Walkway
EXPLORE Wahine Disaster, 1968 BROADWAY Though there have been worse shipping The Eastern Walkway extends GORE disasters in New Zealand with greater along the southern end of B EASTERN STEWART E loss, the sinking of the Wahine on STRATHMORE AVE A Miramar Peninsula from the MONORGAN RD WALKWAY C April 10 is by far the most well known. O Pass of Branda to Tarakena Bay. Scots N The tragedy can be attributed to one INGLIS ST Fort Dorset EXPLORE H College STRATHMORE major cause – the weather. The storm I The track is 2.5 km long and L LYONS L Walk overleaf HECTOR ST which exploded upon Wellington was takes about one and a half hours to complete. The track surface is BEACON Miramar PARK HILL RES one of the worst ever recorded in New mainly gravel and much of the track is exposed. Golf Zealand. Its ferocity was due to a A WELLINGTON D SIGNALLERS START combination of two storms which Discover Wellington’s Town Belt, reserves and walkways The route is described here from the Pass of Branda to Tarakena Bay, Course N P A A happened to merge directly over R R A but marker posts mean it can be walked in either direction or in the T B U F Wellington. DUFF DRIVE DUFF O recommended circular route back along Breaker Bay Road (see map). W Wellington SS A T PA At 6.41am the Wahine struck on the L S There is also an extra walk which can be done out to Point Dorset, D E LEVESON C 2 southernmost rocks of Barrett Reef where International E T DY allow one hour to discover World War II gun batteries and observation N ANNA the vessel grounded and suffered severe Airport AVE damage to her hull whereby seawater posts. -
Heritage Trail PDWCC49264
heritage trail PDWCC49264 Wellington City Council “The winds and the woodenness … are only incidental to the grand fact of Wellington’s harbour… It is more tremendous by far than Sydney’s overvaunted harbour, if only because it is uncluttered by islets and fjords, but stands there like a noble bowl among its surrounding mountains. It looks symmetrical, purposeful, altogether functional… It might have been scooped out by a million bull-dozers.” — James Morris, Cities (1963) Introduction Wellington Harbour is a large expanse of water, more like a lake than a harbour, up to 28 metres deep and occupying nearly 50 square kilometres. These natural attributes have helped Wellington become one of this country’s most important ports. The harbour is also a wonderful recreational facility, with yachts fi lling the water on weekends, fi shermen lining its shores and hundreds walking its margins. Though it is no longer so central to Wellington’s life, the harbour has a unique location and appearance. It is ever changeable, like the city’s weather – calm one moment and then rough and agitated the next. The trail you are about to walk is almost exclusively on reclaimed land. Wellington’s waterfront changed dramatically as the demands for more land and wharfage grew. Wellington’s original shoreline, today some distance inland, is the subject of its own walk. Just how the present shoreline was formed, and the uses the land created behind it has been put to, are the main subjects of this trail. 1 wellington’s maritime heritage trail Lambton Harbour – the beginnings When the fi rst New Zealand Company settlers arrived in Wellington in early 1840 they settled on the fl at land at Petone, at the north end of Wellington Harbour. -
Required Knowledge for Cook Strait Endorsement[PDF
Required knowledge for Cook Strait endorsement Last updated: March 2018 This document is uncontrolled if printed, please refer to the Maritime New Zealand website for the latest version. Cook Strait is known locally and internationally as one of the most rugged stretches of water in the world, with strong winds and strong tidal effects that can create, at times, treacherous conditions. Prudent planning must always be completed when thinking about transiting Cook Strait and caution should always be at the foremost of any mariner. The following information has been obtained from the Admiralty Sailing Directions New Zealand Pilot NP51; Charts: NZ 463 – Approaches to Wellington, NZ 6153 – Queen Charlotte Sound, NZ 6154 – Tory Channel Entrance and Picton Harbour; the Royal Port Nicholson Yacht Club Handbook, Central Cruising guide. Currents The current in Cook Strait is strongly influenced by the prevailing winds. The rate may vary from a northerly- going current of 0.5 knots in moderate southerly winds, to an east–northeasterly-going current at 0.4 knots with fresh northerly winds. In light variable winds the current sets east at 0.4 knots. Tidal streams The tidal streams in and around Cook Strait are unreliable and mariners are warned to exercise every precaution when navigating the vicinity. The streams often run in one direction for eight to 10 hours, but cases have been reported of them going 18 hours or more (rare event). When the streams have been running in one direction for an extended period, it has been found that the opposite stream is much weaker, and on some occasions, hardly noticeable. -
Rongotai – Hue Te Taka
C U L T U R A L VALUES R E P O R T Wellington Airport Limited – South Runway extension Rongotai – Hue te Taka IN ASSOCIATION WITH PORT NICHOLSON BLOCK SETTLEMENT TRUST & WELLINGTON TENTHS TRUST NOVEMBER 2014 CULTURAL VALUES REPORT Wellington Airport – South Runway extension RONGOTAI – HUE TE TAKA TABLE OF CONTENTS EXECUTIVE SUMMARY ...........................................................................................................................3 THE PROJECT .............................................................................................................................................4 KEY MAORI VALUES ASSOCIATED WITH THIS AREA ..................................................................6 FISHING AND FISHERIES IN THE AREA ...........................................................................................................7 MARINE FLORA ............................................................................................................................................8 WATER QUALITY..........................................................................................................................................8 MAORI SITES OF SIGNIFICANCE IN THE AREA ...............................................................................8 EARLY MĀORI HISTORY ....................................................................................................................... 15 MOTU KAIRANGI – THE ISLAND ....................................................................................................... -
Wahine in Wellington Harbour, New Zealand on April the 10Th 1968
http://researchcommons.waikato.ac.nz/ Research Commons at the University of Waikato Copyright Statement: The digital copy of this thesis is protected by the Copyright Act 1994 (New Zealand). The thesis may be consulted by you, provided you comply with the provisions of the Act and the following conditions of use: Any use you make of these documents or images must be for research or private study purposes only, and you may not make them available to any other person. Authors control the copyright of their thesis. You will recognise the author’s right to be identified as the author of the thesis, and due acknowledgement will be made to the author where appropriate. You will obtain the author’s permission before publishing any material from the thesis. Positioned as Expert Scientists: Learning science through Mantle-of-the-Expert at years 7/8 A thesis submitted in fulfilment of the requirements for the degree of Doctor of Philosophy in Education at The University of Waikato by CAROLYN JULIE SWANSON 2016 i Abstract This study emerged from concern that students disengage from science at an early age. It investigated whether using the drama-based teaching approach Mantle-of- the-Expert would support students’ interest in and learning of science. To do this a mixed method action research study was conducted. A science-based unit was co-taught with the classroom teacher over nine-weeks with a class of year 7/8 students in a semi-rural school. A Mantle-of-the-Expert unit was devised to support learning about buoyancy and stability with the students positioned as expert scientists re-investigating the sinking of the Wahine in Wellington Harbour, New Zealand on April the 10th 1968. -
Offshore Sailing at RPNYC (Extracts from the RPNYC 2015-16 Almanac)
Offshore Sailing at RPNYC (extracts from the RPNYC 2015-16 Almanac) Offshore Notice of Race page 1 Coastal Notice of Race page 5 Offshore Sailing Instructions page 9 Radio information page 14 Cook Strait information page 17 Summary of races and events page 19 Harbour mark locations and descriptions page 21 Race signals page 23 Royal Port Nicholson Yacht Club 2015 – 2016 Season 30 October 2015 – 14 May 2016 Offshore Notice of Race The organising authority is the Royal Port Nicholson Yacht Club (Inc.), (RPNYC) 103 Oriental Parade Wellington | PO Box 9674, Wellington | Tel (04) 939 7069 | Fax (04) 939 7031 1 Rules General and Safety Rules 1.1 All racing will be governed by the rules as defined in The Racing Rules of Sailing along with the Wellington Regional Navigation and Safety Bylaws, the Marlborough District Council Navigation Bylaw 2009, and the Nelson City Council Navigation Safety Bylaw 2012. 1.2 All yachts shall comply with Part II of the Yachting New Zealand (YNZ) Safety Regulations, Category 3 modified as follows: (a) Yachts must start the race with at least 2.5 litres of fresh water per person for each 100 nautical miles (or part thereof) of the course to be sailed. (b) Yachts must carry a liferaft in accordance with safety regulation 17.11. (c) Yachts must carry an additional lifebuoy and equipment in accordance with safety regulation 17.13(b). (d) Yachts must carry a storm jib in accordance with safety regulation 15.15(b). (e) Yachts must carry at least LWL(m) / 0.2 litres of engine fuel. -
Coastal & Underwater Archaeological Sites
COASTAL & UNDERWATER ARCHAEOLOGICAL SITES OF THE WELLINGTON REGION For Greater Wellington Regional Council COASTAL & UNDERWATER ARCHAEOLOGICAL SITES OF THE WELLINGTON REGION Survey for the Coastal Plan Review Report prepared by A N D Y D O D D SUBSURFACE LTD PO Box 31, Paekakariki 5258 Tel 04 902 3290 Email [email protected] for GREATER WELLINGTON REGIONAL COUNCIL 142 – 146 Wakefield Street P O Box 11 646 Wellington 30 June 2013 CONTENTS 1.0 INTRODUCTION 5 1.1 Commission 5 1.2 Process 5 1.3 Sources of Information 6 1.4 Acknowledgements 6 1.5 References 6 INVENTORY OF ARCHAEOLOGICAL SITES Shipwrecks Tyne 7 Subraon 18 St Vincent 29 Wellington, Cyrus, Progress, Yung Pen 40 Hannah Broomfield, Magic 58 Tui 71 Waitaki 85 Willie McLaren 96 Grassmere 109 Halcione 118 Delmira 130 Zuleika 141 Ben Avon 150 Nambucca 162 Woollahra 173 Devon 186 Defender 200 Opua 212 HMNZS South Sea 223 Phyllis 235 Scuttling ground 244 Anchorages Entry Anchorage 256 Kau Bay 266 Shore whaling stations Te Kahuoterangi 276 3 Korohiwa 288 Tohoramaurea 299 Tokomapuna 310 Waiorua 321 Mana 334 Coastal Defence Makara Home Guard defences 345 Point Gordon submarine cables 353 Wharves and landings Mahanga Bay wharf 364 Matiu-Somes lighthouse landing 376 Castlepoint lighthouse landing 387 Shipbuilding Balaena Bay shipbuilding 398 Front cover photo: Diver on the wreck of the Ben Avon, Cape Palliser 4 1.0 INTRODUCTION 1.1 Commission This survey of archaeological and historic sites in the Wellington region coastal marine area has been prepared to compliment a study of historic built heritage commissioned by the Greater Wellington Regional Council in 2010 (Cochran, Murray and Kelly 2012).