Tapawera News Issue 8 11 June 2020
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Abel Tasman.Indd
DAYOUT. IN TASMAN BAY WALKS The relaxed lifestyle, excellent climate, beautiful beaches, picnic Walks in the Motueka - Kaiteriteri - Abel Tasman spots and very popular walks have always attracted New Zealand National Park area: holidaymakers to this area, especially at the end of December and throughout January when the population soars. 1 The Motueka Walkway - 2.5 hours If you want to be sure of your trip, you’ll need to book Pick up a free map at the Motueka Information Centre (well accommodation in advance. Outside those months, there are signposted, just off the High Street). more vacancies There are motels, campsites, backpackers lodges On this track you’ll see some splendid views of Tasman Bay and bed ‘n breakfasts to cater for all budgets in the towns and with glimpses of small-town New Zealand without the tourist surrounding areas. trappings. Interesting features include: Abel Tasman National Park • The Port - the centre of one of Motueka’s main industries If you want to walk the Abel Tasman Track, you’ll need to reserve - fishing. Evidence lies in the rusting hulk of the Janie Seddon, a in advance with the Department of Conservation, as numbers large vessel that lies in the estuary sand near the walkway. of walkers have had to be limited. But using water taxis, it’s • The track leads you beside a tidal estuary that changes possible to do sections of the track on a dayout without worrying from mud flats with wading birds to a beautiful seascape at full about bookings. tide. MOTUEKA • A wide variety of NZ houses from small, older baches Motueka is a small town at the mouth of the Motueka River, (holiday houses) to large, modern homes owned by Motueka’s which flows into Tasman Bay. -
Motupipi-Takaka Terraces and Plains Ecosystem Plant Lists
MOTUPIPI – TAKAKA TERRACES & PLAINS ECOSYSTEM NATIVE PLANT RESTORATION LIST Flats east of the Takaka and Motupipi River floodplains, extending from Pohara inland up the Takaka valley to Uruwhenua and backed in the east by limestone and marble Locality: hill country. Outliers west of Takaka River include terraces of Go-Ahead Creek and those north of One-Spec Creek. Plains and terraces, in the north reaching 40m above sea level and gently dipping to Topography: the north-west, and inland rising up to 80m above sea level. Low-lying towards Motupipi Inlet and coast. Alluvial, sandy and silty loams of moderate fertility derived from a range of sedimentary rocks, marble, granites and schist. Overlying unweathered glacial outwash gravels. Soils and Geology: Mostly well-drained except along low-gradient, meandering water courses and behind strip of sandy coast at Motupipi-Clifton where there are swamp deposits. Not drought- prone. High sunshine hours; frosts mild to moderate; mild annual temperatures. Climate: Rainfall 1600mm on the coast to 2600mm inland. Coastal Influence: Between Motupipi Estuary and Pohara up to ½ km inland. Mixed podocarp-broadleaf forest, especially tōtara, mataī, tītoki and northern rātā on Original Vegetation: the drier sites and kāhikatea and pukatea on the less well-drained sites. Wetlands in low-lying areas. No original vegetation remaining. A few small and isolated secondary forest and Human Modification: treeland remnants persist as well as numerous scattered individual trees, particularly tōtara. [Refer to the Ecosystem Restoration map showing the colour-coded area covered by this list.] KEY TYPE OF FOOD PROVIDED FOR PLANTING RATIO PLANT PREFERENCES BIRDS AND LIZARDS Early Stage plants are able to Wet, Moist, Dry, Sun, Shade, Frost, Saline establish in open sites and can act as F = Fruit/seeds a nursery for later stage plants by 1 = prefers or tolerates providing initial cover. -
Moutere Gravels
LAND USE ON THE MOUTERE GRAVELS, I\TELSON, AND THE DilPORTANOE OF PHYSIC.AL AND EOONMIC FACTORS IN DEVJt~LOPHTG THE F'T:?ESE:NT PATTERN. THESIS FOR THE DEGREE OF MASTER OF ARTS ( Honours ) GEOGRAPHY UNIVERSITY OF NEW ZEALAND 1953 H. B. BOURNE-WEBB.- - TABLE OF CONTENTS. CRAFTER 1. INTRODUCTION. Page i. Terminology. Location. Maps. General Description. CH.AFTER 11. HISTORY OF LAND USE. Page 1. Natural Vegetation 1840. Land use in 1860. Land use in 1905. Land use in 1915. Land use in 1930. CHA.PrER 111. PRESENT DAY LAND USE. Page 17. Intensively farmed areas. Forestry in the region. Reversion in the region. CHA.PrER l V. A NOTE ON TEE GEOLOGY OF THE REGION Page 48. Geological History. Composition of the gravels. Structure and surface forms. Slope. Effect on land use. CHA.mm v. CLIMATE OF THE REGION. Page 55. Effect on land use. CRAFTER Vl. SOILS ON Tlffi: MGm'ERE GRAVELS. Page 59. Soil.tYJDes. Effect on land use. CHAPrER Vll. ECONOMIC FACTORS WrIICH HAVE INFLUENCED TEE LAND USE PATTERN. Page 66. ILLUSTRATIONS AND MAPS. ~- After page. l. Location. ii. 2. Natu.ral Vegetation. i2. 3. Land use in 1905. 6. Land use regions and generalized land use. 5. Terraces and sub-regions at Motupiko. 27a. 6. Slope Map. Folder at back. 7. Rainfall Distribution. 55. 8. Soils. 59. PLATES. Page. 1. Lower Moutere 20. 2. Tapawera. 29. 3. View of Orcharding Arf;;a. 34a. 4. Contoured Orchard. 37. 5. Reversion and Orchards. 38a. 6. Golden Downs State Forest. 39a. 7. Japanese Larch. 40a. B. -
MUSIC MAN Community 3-7
October 2017 Inside this issue: MUSIC MAN Community 3-7 Recreation 9-11 Arts and Crafts 13 Moutere Youth 15 Food 17 Animals 19-21 Gardening 22 Health & Wellbeing 23 Trade & Services 26 directory Recycled materials are a perfect basis for Lawrie Feely’s stringed instruments Special points of interest: and stored for 30 years, and I’ve used it in a lot of my L O C A L L I V E S instruments. Each wood has a different sound.” His favourite is the strum stick—a portable version of Every Friday Sharing table the dulcimer that can be played like a guitar instead of MHCC Eight-string island ukuleles, strum sticks and mountain on a table. “Backpackers love them,” he says. Also dulcimers are everywhere to be seen in Lawrie Feely’s popular is a stringed instrument that can be played by workshop. Created from recycled venetian blinds, fruit anyone who’s capable of a single finger tune on the 14 October: The Andrew bowls, tabletops and bedheads, each one looks and piano. “You can make music out of anything,” says London Trio—page 11 sounds unique. Lawrie, pulling out a ‘tin-canjo’ with a decorative biscuit- Lawrie has been making instruments since going to a tin body to prove his point. 70th birthday party down South and playing along with a 20 October: Musical When he’s not making instruments, Lawrie can be found group of ladies from the marae on the ukulele. “Next repairing horse gear, such as covers, bridles and saddle bingo—page 10 day, I took some photos and measurements and made strapping. -
A Directory of Wetlands in New Zealand: Nelson/Marlborough
A Directory of Wetlands in New Zealand NELSON/MARLBOROUGH CONSERVANCY Farewell Spit (39) Location: 40o32'S, 172o50'E. At the northern extremity of Golden Bay and the northwestern extremity of South Island, 38 km from the town of Takaka, Tasman District. Area: 11,388 ha (land area c.1,961 ha; inter-tidal zone c.9,427 ha). Altitude: Sea level to 3 m. - 155 - A Directory of Wetlands in New Zealand Overview: Farewell Spit is a classic recurved spit, approximately 30 km long, composed predominantly of uniform quartz sand derived from rivers draining westwards and transported northward by the westland current. The north is exposed to the Tasman Sea, but the south has extensive tidal mudflats. These provide feeding areas for large numbers of waterfowl. Some 95 species were recorded on the spit in March 1974, and more than 83 species of wetland birds are regularly recorded at the spit. The sand dunes provide habitat for a diverse and unusual plant community. Farewell Spit was listed as a wetland of international importance under the Ramsar Convention on 13 August 1976. Physical features: Farewell Spit is a classic recurved spit. The material forming the spit is derived from erosion of the Southern Alps and West Coast sea cliffs, transported northwards by a long-shore current. Since the estimated origin of the spit 6,500 years ago, an estimated 2.2 million cubic metres of sand have been deposited per annum. Wind transports more surface sand towards Golden Bay, although the majority of sand lies below the mean low water mark. -
Newsletter 26Th October 2018.Pub
Murchison Area School 61 Waller Street P O Box 73 Murchison 7049 Phone 03 5239 072 [email protected] 26th October 2018 Term 4 School Wide Value — Consideration Kia ora, Moghrey Mie, I have spoken in recent weeks about our ERO (Education Review Office) report that we had last term. The final report has now been published and is an official document for all to see. I have placed this on our school website (www.murchison.school.nz ). It can also be found on the ERO website at www.ero.govt.nz . The following are some extracts from the report: 1) “Respectful and caring relationships contribute to equitable and successful outcomes for students. Students learn in a settled and supportive learning environment. Teachers know students very well as individuals and as learners and focus on their holistic wellbeing and academic success. Individual students’ learning is well tracked and monitored by classroom teachers. The school and wider community work closely to support and enrich students’ learning.” 2) “Students who need extra assistance to succeed are very well supported. There are improved systems to effectively identify, monitor and support these students. The school works constructively with parents and experts beyond the school to find solutions to improve student outcomes at home and at school. Students with additional learning needs benefit from well -considered individual learning plans and are supported towards full inclusion.” 3) “The vision, values and priorities that underpin the school’s culture and curriculum are well known and evident in practice. This includes restorative practices and growth mindset approaches.The school’s valued outcomes for students are regularly shared to build and embed understanding. -
Car Company Nelson U7 2018
Car Company Nelson U7 2018 Draw dated 3/5/18 Game times are posted on the Monday prior on our website http://www.tasmanrugby.co.nz/draws-results/juniorage-grade Date Home Away Venue Week 1 5/5/2018 Tapawera: U7 V Murchison: U7 Tapawera 5/5/2018 Rangers: U7 V Riwaka: Aqua Taxi U7 Black Upper Moutere 5/5/2018 Wanderers: U7 Gold V Waimea Old Boys: U7 Griffins Lord Rutherford Park 5/5/2018 Wanderers: U7 Stripes V Riwaka: Aqua Taxi U7 White Lord Rutherford Park 5/5/2018 Wanderers: U7 Blue V Waimea Old Boys: U7 Mako Lord Rutherford Park 5/5/2018 Nelson: U7 Blue V Nelson: U7 White Neale Park 5/5/2018 Waimea Old Boys: U7 Red V Huia: U7 Jubilee Park 5/5/2018 Waimea Old Boys: U7 White V Stoke: U7 White Jubilee Park 5/5/2018 Marist: U7 V Stoke: U7 Red Tahunanui Week 2 12/5/2018 Wanderers: U7 Stripes V Murchison: U7 Lord Rutherford Park 12/5/2018 Wanderers: U7 Gold V Riwaka: Aqua Taxi U7 Black Lord Rutherford Park 12/5/2018 Wanderers: U7 Blue V Riwaka: Aqua Taxi U7 White Lord Rutherford Park 12/5/2018 Stoke: U7 Red V Waimea Old Boys: U7 Red Greenmeadows 12/5/2018 Rangers: U7 V Tapawera: U7 Upper Moutere 12/5/2018 Huia: U7 V Waimea Old Boys: U7 Griffins Sports Park Motueka 12/5/2018 Nelson: U7 White V Waimea Old Boys: U7 White Neale Park 12/5/2018 Nelson: U7 Blue V Marist: U7 Neale Park 12/5/2018 Stoke: U7 White V Waimea Old Boys: U7 Mako Greenmeadows Week 3 19/5/2018 Tapawera: U7 V Wanderers: U7 Stripes Tapawera 19/5/2018 Murchison: U7 V Wanderers: U7 Blue Murchison 19/5/2018 Waimea Old Boys: U7 Griffins V Stoke: U7 Red Jubilee Park 19/5/2018 Waimea -
New Zealand 16 Marlborough Nelson Chapter
©Lonely Planet Publications Pty Ltd Marlborough & Nelson Why Go? Marlborough Region ....400 For many travellers, Marlborough and Nelson will be their Picton ........................... 400 introduction to what South Islanders refer to as the ‘Main- Marlborough Sounds ...404 land’. Having left windy Wellington, and made a white- Queen Charlotte Track ...407 knuckled crossing of Cook Strait, folk are often surprised to fi nd the sun shining and the temperature up to 10 degrees Kenepuru & Pelorus Sounds.............409 warmer. Good pals, these two neighbouring regions have much Blenheim ........................411 in common beyond an amenable climate: both boast re- Kaikoura ........................ 416 nowned coastal holiday spots, particularly the Marlborough Nelson ...........................423 Sounds and Abel Tasman National Park. There are two other Nelson Lakes national parks (Kahurangi and Nelson Lakes) and more National Park ................430 mountain ranges than you can poke a stick at. Motueka ........................432 And so it follows that these two regions have an abun- Motueka to Abel dance of luscious produce: summer cherries for a starter, Tasman ..........................435 but most famously the grapes that work their way into the Golden Bay ....................440 wineglasses of the world’s fi nest restaurants. Keep your pen- Kahurangi National knife and picnic set at the ready. Park ...............................444 When to Go? Best Places to Eat The forecast is good: Marlborough and Nelson soak up some » Green Dolphin (p 422 ) of New Zealand’s sunniest weather. January and February are the warmest months, with daytime temperatures aver- » Wither Hills (p 414 ) aging 22°C; July is the coldest, averaging 12°C. It’s wetter » Hopgood’s (p 428 ) and more windswept the closer you get to Farewell Spit and » Sans Souci Inn (p 442 ) the West Coast. -
Conservation Campsites South Island 2019-20 Nelson
NELSON/TASMAN Note: Campsites 1–8 and 11 are pack in, pack out (no rubbish or recycling facilities). See page 3. Westhaven (Te Tai Tapu) Marine Reserve North-west Nelson Forest Park 1 Kahurangi Marine Takaka Tonga Island Reserve 2 Marine Reserve ABEL TASMAN NATIONAL PARK 60 3 Horoirangi Motueka Marine KAHURANGI Reserve NATIONAL 60 6 Karamea PARK NELSON Picton Nelson Visitor Centre 4 6 Wakefield 1 Mount 5 6 Richmond Forest Park BLENHEIM 67 6 63 6 Westport 7 9 10 Murchison 6 8 Rotoiti/Nelson Lakes 1 Visitor Centre 69 65 11 Punakaiki NELSON Marine ReservePunakaiki Reefton LAKES NATIONAL PARK 7 6 7 Kaikōura Greymouth 70 Hanmer Springs 7 Kumara Nelson Visitor Centre P Millers Acre/Taha o te Awa Hokitika 73 79 Trafalgar St, Nelson 1 P (03) 546 9339 7 6 P [email protected] Rotoiti / Nelson Lakes Visitor Centre Waiau Glacier Coast P View Road, St Arnaud Marine Reserve P (03) 521 1806 Oxford 72 Rangiora 73 0 25 50 km P [email protected] Kaiapoi Franz Josef/Waiau 77 73 CHRISTCHURCH Methven 5 6 1 72 77 Lake 75 Tauparikākā Ellesmere Marine Reserve Akaroa Haast 80 ASHBURTON Lake 1 6 Pukaki 8 Fairlie Geraldine 79 Hautai Marine Temuka Reserve Twizel 8 Makaroa 8 TIMARU Lake Hāwea 8 1 6 Lake 83 Wanaka Waimate Wanaka Kurow Milford Sound 82 94 6 83 Arrowtown 85 6 Cromwell OAMARU QUEENSTOWN 8 Ranfurly Lake Clyde Wakatipu Alexandra 85 Lake Te Anau 94 6 Palmerston Te Anau 87 8 Lake Waikouaiti Manapouri 94 1 Mossburn Lumsden DUNEDIN 94 90 Fairfield Dipton 8 1 96 6 GORE Milton Winton 1 96 Mataura Balclutha 1 Kaka Point 99 Riverton/ INVERCARGILL Aparima Legend 1 Visitor centre " Campsite Oban Stewart Island/ National park Rakiura Conservation park Other public conservation land Marine reserve Marine mammal sanctuary 0 25 50 100 km NELSON/TASMAN Photo: DOC 1 Tōtaranui 269 This large and very popular campsite is a great base for activities; it’s a good entrance point to the Abel Tasman Coast Track. -
Abel Tasman Coast Track Brochure
Plan and prepare ABEL TASMAN ABEL TASMAN COAST TRACK Takaka COAST TRACK HEAPHY TRACK Duration: 3–5 days Great Walks season: Distance: 60 km (one way) All year Motueka Karamea NELSON Nelson Picton Visitor Centre Wakefield BLENHEIM Westport Murchison St Arnaud Rotoiti/Nelson Lakes Visitor Centre Punakaiki Reefton Paparoa National Park Visitor Centre Kaikoura Greymouth Hanmer Springs Kumara Hokitika Arthur’s Pass National Park Visitor Centre Oxford Rangiora Kaiapoi Franz Josef/Waiau Westland Tai Poutini National Park Visitor Centre CHRISTCHURCH Ōtautahi/Christchurch Visitor Centre Methven Aoraki/Mount Cook Aoraki/Mt Cook National Park Akaroa Visitor Centre Haast ASHBURTON Awarua/Haast Visitor Centre Geraldine Fairlie Temuka Twizel Makaroa TIMARU ROUTEBURN TRACK Wanaka Kurow Waimate Milford Sound Tititea/Mount Aspiring National Park Visitor Centre Arrowtown MILFORD TRACK Cromwell QUEENSTOWN OAMARU Whakatipu-wai-Māori/ Ranfurly Queenstown Visitor Centre Clyde Alexandra KEPLER TRACK Palmerston Te Anau Te Rua-o-te-moko/Fiordland National Park Visitor Centre Waikouaiti Mossburn Lumsden DUNEDIN Fairfield Ōtepoti/Dunedin Visitor Centre Dipton GORE Milton Winton Mataura Balclutha Kaka Point Riverton/ Aparima INVERCARGILL RAKIURA TRACK Oban Stewart Island/ Rakiura National Park Rakiura Visitor Centre Elevation profile & track guide Tinline Akersten Bay ABEL Campsite Te Pukatea Bay Bark Bay Hut 30 campers Campsite and Campsite 6 campers Campsite 14 campers 34 bunks Coquille Bay Observation Beach Anchorage Hut 80 campers Campsite Campsite and Campsite TASMAN 12 campers 12 campers 34 bunks Apple Tree Bay 100 campers Mārahau Shelter Campsite Watering Cove Torrent and car park 30 campers Campsite Bay Village COAST 160 m 10 campers Campsite 20 campers 80 m TRACK 0 m 4 hr / 12.4 km 4 hr / 11.5 km With a mild climate, golden beaches and lush, coastal native bush, the Abel Tasman Coast Track has it all. -
P a C I F I C O C E a N S O U
050 km 0 30 miles Wharariki Beach Puponga Farewell Spit Pakawau T A S M A N Golden Bay Cook Strait S E A Collingwood 60 Onekaka Bainham D'Urville Pupu Pohara Totaranui Island Marlborough y Trac Springs Sounds h k Takaka ap Abel Tasman e Kahurangi H Canaan National Park National Park Downs Marahau Tasman Bay Mt Domett Upper Takaka Kaiteriteri (1646m) Cobb Riwaka Queen y Ferry to Kohaihai River Motueka w Rai Charlotte Wellington H Moutere Oparara Ruby Bay Valley Track Mt Arthur Valley Mapua 6 Karamea Havelock (1795m) Rabbit Nelson ueka Hwy Is Pelorus Waikawa 6 Karamea Bight Tasman Mountains Stoke Bridge 1 Picton Mot Little Wanganui Tapawera Richmond Marlborough Whites Wangape Bay Mt Richmond Wine Region ka ck Cloudy Bay 67 Tra Forest Park Onamalutu er Blenheim Seddonville ge iv Wairau an u R Renwick Mt Owen d R ira 65 Lagoons (1875m) on Wa Granity Hector ichm r R ive Marfells Kawatiri Kowhai Point R Beach Denniston Gowanbridge Tophouse Seddon 6 Lake Westport Grassmere Cape Rotoroa St Arnaud Awatere Campbell Buller Gorge Murchison Lake Ward Inangahua Rotoroa Lake Rotoiti Tapuae-o-Uenuru (2885m) Coastal 69 Mt Travers Nelson Lakes Pacific (2338m) National Park Cob Victoria Cottage ras Kekerengu Forest Park ou Mt Una Rd aik (2300m) eron d K Reefton ch River 65 Inlan 7 -A Clarence rth l) 1 o Clarence Spencer Mountains na Mt Fyffe Mangamaunu; lesw aso (1402m) Ikamatua o e Meatworks (S Lewis M Springs Acheron Kaikoura Peninsula Junction Pass KaikourasKaikoura Hanmer Forest ardConway Riv Kaikoura Peninsula Conservation Park Seaw70 Lake Sumner Forest Park 7 Hanmer iver Springs R er Waiau Waiau Parnassus S O U T H Culverden P A C I F I C 7 O C E A N Huru Cheviot nui r Arthur's Pass Rive Gore Bay National Park 1 Hurunui. -
The Signature of an Extreme Erosion Event on Suspended Sediment Loads: Motueka River Catchment, South Island, New Zealand
184 Sediment Dynamics in Changing Environments (Proceedings of a symposium held in Christchurch, New Zealand, December 2008). IAHS Publ. 325, 2008. The signature of an extreme erosion event on suspended sediment loads: Motueka River catchment, South Island, New Zealand D. M. HICKS1 & L. R. BASHER2 1 National Institute of Water and Atmospheric Research, PO Box 8602, Christchurch, New Zealand [email protected] 2 Landcare Research, Private Bag 6, Nelson Mail Centre, Nelson 7042, New Zealand Abstract Five years of continuously monitoring turbidity and suspended sediment (SS) at four sites in the Motueka River catchment, northern South Island, New Zealand, has characterised the downstream and temporal dispersion of high SS inputs from an extreme rainfall event. The rainstorm, of >50 year recurrence interval, was concentrated in the upper Motueka and Motupiko tributaries and delivered high sediment outputs from re-activated gully complexes and landslides. These only appear to activate when a rainfall threshold is exceeded. Monitoring stations in these tributaries captured a ~20- to 30-fold increase in SS concentrations and event sediment yields, whereas the monitoring station at the coast recorded only a 2- to 5-fold increase. The high concentrations and event yields decayed exponentially back towards normal levels over ~2–3 years at both upstream and downstream sites. Field observations suggest that this erosion recovery trend relates more to the exhaustion/stabilisation of transient riparian sediment storage than to “healing” of the primary erosion sites by surface-armouring and/or re-vegetation. The downstream decay relates both to dilution (from other tributaries carrying lower SS concentrations) and dispersion processes.