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ICM Technical Report
The Motueka and Riwaka catchments : a technical report summarising the present state of knowledge of the catchments, management issues and research needs for integrated catchment management / compiled by L.R. Basher. -- Lincoln, Canterbury, N.Z. : Landcare Research New Zealand, 2003. ISBN 0-478-09351-9 1. Water resources development New Zealand Motueka River Watershed. 2. Water resources development New Zealand Riwaka River Watershed. 3. Motueka River Watershed (N.Z.) 4. Riwaka River Watershed (N.Z.) I. Basher, L. R. UDC 556.51(931.312.3):556.18 The Motueka and Riwaka catchments A technical report summarising the present state of knowledge of the catchments, management issues and research needs for integrated catchment management Compiled by L.R. Basher1 Contributors J.R.F. Barringer1, W.B. Bowden2, T. Davie1, N.A. Deans3, M. Doyle4, A.D. Fenemor5, P. Gaze6, M. Gibbs7, P. Gillespie7, G. Harmsworth8, L. Mackenzie7, S. Markham4, S. Moore6, C. J. Phillips1, M. Rutledge6, R. Smith4, J.T. Thomas4, E. Verstappen4, S. Wynne-Jones6, R. Young7 1 Landcare Research, Lincoln 2 Formerly Landcare Research, Lincoln; now University of Vermont, Burlington, Vermont, USA 3 Nelson Marlborough Region, Fish & Game New Zealand, Richmond 4 Tasman District Council, Richmond 5 Landcare Research, Nelson 6 Department of Conservation, Nelson 7 Cawthron Institute, Nelson 8 Landcare Research, Palmerston North May 2003 Preface When beginning any new research to managing our land, rivers and coast in an programme, a key first step is to understand interconnected holistic fashion. ICM encompasses existing knowledge about the topic. This report the principles of integration among science is the synthesis of existing knowledge about the disciplines, integration between communities, environment of the Motueka River catchment. -
Tasman District LANDSCAPE STUDY 2021
Tasman District LANDSCAPE STUDY 2021 OUTSTANDING NATURAL FEATURES AND LANDSCAPES DRAFT for Landowner Consultation Prepared for: Tasman District Council bridgetgilbert March 2021 | Status: DRAFT landscapearchitecture [INSERT PROJECT TEAM LOGOS HERE] 2 3 Y Y D D U U ST ST E E E CAP CAP S S D D N N A A L Contents L CT CT I I TR Front material to be inserted TR Section A: Executive Summary ���������������������������������������������������������5 N DIS N Copyright information DIS N A Acknowledgements A SM SM A Short description of document for referencing purposes Section B: Introduction to the Tasman District Landscape Study �������9 A T T Background 10 Project Team: Tasman District Council Landscape Assessment ‘Principles’ 13 Bridget Gilbert Landscape Characterisation 14 Dr Bruce Hayward Landscape Evaluation 17 Davidson Environmental Limited Mike Harding Is it a ‘Landscape’ or ‘Feature’? 18 Boffa Miskell Limited Threshold For ‘Natural’ 20 Threshold For ‘Outstanding’ 21 Expert Geoscience Input 22 Expert Ecology Input 23 Cultural Values and Iwi Consultation 23 Shared and Recognised Values 24 GIS Data Sources and Mapping 26 ONFs 26 ONL and ONF Mapping 28 DRAFT FOR LANDOWNER CONSULTATION LANDOWNER FOR DRAFT CONSULTATION LANDOWNER FOR DRAFT ONL and ONF Schedules 30 Section C: Tasman District Landscape Study Methodology �������������33 Assumptions 36 Section D: Outstanding Natural Landscapes ����������������������������������39 Contents: Outstanding Natural Landscapes 40 Section E: Outstanding Natural Features ����������������������������������������89 -
150Th Celebrations 1868- 2018
th 150 Celebrations 1868- 2018 1 This burgeoning document includes the 1968 centennial booklet and the 1993 jubilee publication. A chapter to commemorate the 2018 sesquicentennial adds to the accounts of life at Ngatimoti School. Many thanks to Kirsten Braniff for organising, digitising and overseeing this work, and to Jennifer Beatson, Fiona Nelson and Edward Stevens for helping with interviewing and transcribing. 2018 Introduction Ngatimoti School is a welcoming, vibrant place with a very rich past and an exciting present and future. There are three values I’d like to highlight as we celebrate the sesquicentennial of Ngatimoti School. The first is connections and community. It is this sense of connection and community that is vital to the success of Ngatimoti School. The foundations of our school were developed on these values and they continue to be at its core. This is reflected in the number of former staff, students and families attending our 150th celebrations. These connections and sense of community are also evident in the successful festivals we hold each year and in the support we have from our school families and wider that contribute to our sense of whanau at Ngatimoti School. The second value is achievement. It is not only academic achievement which we celebrate at Ngatimoti School, but achievements in a broader sense. Our broad R.I.V.E.R. values flow through our school and are a part of the expected culture. The third refers to history, of which we are celebrating. The proud history of Ngatimoti School is marked by the strong commitment by the Board of Trustees and staff to continue to provide stellar educational and experiential opportunities for our tamariki. -
Geology of the Kaikoura Area
13 Geology of the Kaikoura Area 1 : 2 5 0 0 0 0 G e o l o g i c a l M a p M. S. Rattenbury D. B. Townsend M. R. Johnston (Compilers) Age Oxygen New (ka) isotopeZealand International New Zealand Age International New Zealand events stages 251.0 (Ma) 0 Changhsingian ‘Makarewan’ YDm Haweran Wq 1 2 ‘Waiitian’ YDw 3 Castlecliffian Wc 4 Late ocene Wuchiapingian Pleist- ‘Puruhauan’ YDp Quat 100 5 d'Urville 1.8 260.4 (Lopingian) Gelasian Nukumaruan Wn 6 Capitanian Flettian YAf Late Piacenzian Mangapanian Wm Wanganui 200 Waipipian Wp 7 3.6 Haweran Middle Wordian 8 Pliocene Zanclean Opoitian Wo (Guadalupian) Roadian 270.6 Barrettian YAr Early 300 5.3 9 Kungurian Kapitean Tk 10 Aparima Messinian Mangapirian YAm 400 11 Permian Artinskian 12 Telfordian YAt 500 13 Early Tortonian Tongaporutuan Tt Taranaki Sakmarian Late 14 (Cisuralian) (unassigned) Ypt 600 15 Asselian 16 299.0 11.2 17 Gzhelian 700 18 Waiauan Sw 19 Serravallian 20 Castlecliffian Kasimovian 21 800 Moscovian Southland Middle Lillburnian Sl Miocene 900 Pennsylvanian Bashkirian Langhian Clifdenian Sc 16.4 1000 318.1 Serpukhovian Altonian Pl Tertiary Burdigalian Pareora (unassigned) F CENOZOIC Early Otaian Po Aquitanian Waitakian Lw 23.8 Carboniferous Visean Chattian Duntroonian Ld 28.5 Late Landon Mississippian Rupelian Whaingaroan Lwh Oligocene Early 33.7 Runangan Ar Late Priabonian Bartonian Kaiatan Ak 41.3 Arnold Bortonian Ab Tournasian Lutetian Porangan Dp Middle Eocene Heretaungan Dh 49.0 359.2 Mangaorapan Dm Famennian Ypresian Early Waipawan Dw JU 55.5 Late Frasnian Thanetian 385.3 -
ICM Report FINAL.Pmd
114 Appendix 1 Key characteristics of the soils of the Motueka Catchment (from Chittenden et al. 1966; New Zealand Soil Bureau 1968) SOILAppendix MAP 1 Key characteristics SOIL of the soils of the MotuekaAREA Catchment PARENT (from Chittenden et al. 1966; New Zealand Soil Bureau ANNUAL 1968) FERTILITY DRAINAGE UNIT NAME# CLASS* (km2) MATERIAL RAINFALL (mm) CLASS SOILS OF THE FLOODPLAINS AND LOW TERRACES Riwaka zl and sl (98a) RFW (Recent) 40 Alluvium (from greywacke, granite, limestone, 1000–1300 Moderate to high Well drained quartzite, and basic igneous rocks) Riwaka zl (wet phase) (98a) GOO (Gley Recent) 2 Alluvium (from greywacke, granite, limestone, 1000–1300 Moderate to high Poor quartzite, and basic igneous rocks) Sherry s&sl (98c) RST (Recent) 31 Alluvium (from granite) 1000–2500 Low Well drained Wangapeka st sl (99c) RFW (Recent) 11 Alluvium (from greywacke, argillite, quartzite, 1500–2000 Low to moderate Well drained limestone, granite) Tapawera sl (33g) RFW (Recent) 13 Alluvium (from greywacke, argillite, sandstone, 890–1150 Low to moderate Well drained ultrabasic rocks, Moutere gravels) Motupiko l (33g) RFAW(Recent-YBE) 64 Alluvium (from Moutere gravels, greywacke, 890–1150 Low Well drained argillite, sandstone) Braeburn sl (89d) RFMA (Gley) 2 Alluvium (from Moutere gravels) 890–1150 Very low Imperfect Braeburn cyl (89d) GRA (Gley) 1 Alluvium (from Moutere gravels) 890–1150 Very low Poor Dovedale grl (33g) RFAW (Recent-YBE) 30 Alluvium (from Moutere gravels) 890–1150 Low Well drained Motukarara zl (92) GRQ (Saline Gley Recent) -
Uj-Zéland Barlangjai
Karszt és Barlang 2012-14. pp. 57-69. Budapest 2016. Dr. Szentes György UJ-ZELAND BARLANGJAI ÖSSZEFOGLALÁS E tanulmányban a szerző közreadja személyes tapasztlatait és az összegyűjtött információit Új-Zéland különböző típusú barlangjairól. A sok száz barlang és több tucatnyi karsztvidékről e cikk keretei között lehetetlen részletes leírást adni, de igyekszik a legfontosabb barlangokat kiemelni, és keletkezésük sze- r rint bemutatni. Uj-Zéland egészen rövid bemutatása után a szerző a karsztbarlangok mellett leírást ad a lávabarlangokról és a tengerpart látványos abráziós barlangjairól is. BEVEZETÉS Új-Zéland Magyarországtól legtávolabb fekvő ország, a Föld legdélebbi állama. A 270 000 km2 te rületű ország két nagyobb és számos kisebb szigetből áll, melyet a Csendes-óceán vesz körül. A két f nagyobb sziget, a 120 000 km2 nagyságú Északi-sziget és a 150 000 km2 méretű Déli-sziget 1600 km r hosszban húzódik EK-DNy-i irányban mintegy 200-400 km szélességgel. A szigetek földtani felépítése és felszínformája a viszonylag kicsiny területhez képest igen váltotatos. Földtani értelemben a szigetek az Ausztrál-Indiai és a Pacifikus-lemezek összeütközésének következ tében emelkedtek ki az óceánból. A 85 millió éve a Gondwana ősmasszívumból leszakadt földdarab fokozatosan lesüllyedt a Csendes-óceánba, majd a kéregmozgások következtében ismét kiemelkedett. A ll és 2 millió évvel ezelőtti kéregmozgások emelték ki a szigetek hegyvonulatait. A terület ma is a mozgó kőzetlemezek között helyezkedik el, ennek köszönhetően szeizmikusán és vulkanológiailag igen aktív. A változatos kőzetformációk, üledéksorok tükrözik a szigetek létrejöttének és fejlődésének történetét a prekambriumtól a jelenkorig. A Déli-szigeten gyakoriak a prekambriumi és paleozós képződmények, és jellegzetesek a nagy törne- r gü metamorf kőzetformációk. -
Water Resources of the Takaka Water Management Area
Water Resources of the Takaka Water Management Area J T Thomas M M Harvey July 2013 Table of Contents 1. Introduction .............................................................................................................................. 1 2. Geography ................................................................................................................................ 1 2.1 Topography ........................................................................................................................ 1 2.2 Land Cover ......................................................................................................................... 1 2.3 Geology .............................................................................................................................. 4 2.4 Climate/Rainfall .................................................................................................................. 5 3. Water Resources ...................................................................................................................... 7 3.1 Physical Water Resources Monitoring - Flow/Levels/Rainfall/Quality ................................ 7 3.2 Surface Water Resources .................................................................................................. 8 3.2.1 Takaka River ............................................................................................................... 8 3.2.2 Waingaro River ......................................................................................................... -
Salisbury EMU Ecological Values
Biodiversity treasures of the Flora A stocktake of the ecological values of the Salisbury Ecological Management Unit and the threats they face Photo: Ruedi Mossiman A report for Friends of Flora and the Department of Conservation, August 2016 Sandy Toy Summary The Salisbury Ecological Management EMU (EMU) covers 14,520 ha centred on Mt Arthur (Wharepapa) and the Tableland, in the north east corner of Kahurangi National Park. The community group, Friends of Flora (FOF) has been working in partnership with the Department of Conservation (DOC) since 2001 to restore the biodiversity values of this area. The area has a wealth of ecological treasures: 24 different ecosystems at least 88 species categorised as threatened or at risk at least 4 plant and 3 invertebrate species that occur only in the EMU – nowhere else in the world some of the best examples of marble ecosystems in the country the two deepest caves in New Zealand, both of international significance and is one of the best places to experience beech forest birdlife Despite these riches, the sub-fossil remains preserved in the caves are testament to the amount of wildlife lost from the EMU. Many of the remaining specialities persist in precariously small populations. The main threats are non-native predators particularly rodents and mustelids; introduced herbivores particularly hares and deer and other non-native species that disrupt ecosystem functioning such as weeds, pigs and wasps. The subterranean systems are particularly vulnerable to human activities. Management of all these threats is critical to restoring the biodiversity of the Salisbury EMU. In particular, without management, the critically endangered plants in the EMU will become extinct.