Plant Life on Banks Peninsula
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A Tour of Christchurch New Zealand Aotearoa & Some of the Sights We
Welcome to a Tour of Christchurch New Zealand Aotearoa & some of the sights we would have liked to have shown you • A bit of history about the Chch FF Club and a welcome from President Jan Harrison New Zealand is a long flight from most large countries New Zealand is made up of two main islands and several very small islands How do we as a country work? • NZ is very multi cultural and has a population of just over 5 million • About 1.6 M in our largest city Auckland • Christchurch has just on 400,000 • Nationally we have a single tier Government with 120 members who are elected from areas as well as separate Maori representation. • Parliamentary system is based on a unitary state with a constitutional monarchy. How has Covid 19 affected us? • Because of being small islands and having a single tier Govt who acted very early and with strong measures Covid 19, whilst having had an impact on the economy, has been well contained • We are currently at level 1 where the disease is contained but we remain in a state of being prepared to put measurers in place quickly should there be any new community transmission. • There are no restrictions on gathering size and our sports events can have large crowds. • Our borders are closed to general visitor entry. • We are very blessed South Island Clubs Christchurch Christchurch Places we like to share with our visiting ambassadors First a little about Christchurch • Located on the east coast of the South Island, Christchurch, whose Maori name is Otautahi (the place of tautahi), is a city of contrasts. -
Bays Area Community Directory 2020
BAYS AREA COMMUNITY DIRECTORY 2020 1 | P a g e Proudly supported by Contents Welcome to the 2020 edition of the Bays Area Community Directory ............... 3 Emergency Information .............................................................................................. 4 Local Emergency Services ...................................................................................... 4 Community Response Teams.................................................................................. 5 Christchurch Hospital ............................................................................................... 5 After Hours Medical Care ........................................................................................ 5 Natural disasters ........................................................................................................ 5 Defibrillator Locations............................................................................................... 9 How to Stay Informed - Radio ............................................................................... 10 Notes about this directory ........................................................................................ 11 Key local organisations .......................................................................................... 11 Charitable Status .................................................................................................... 11 Public interest/good .............................................................................................. -
Urban Greening Manual. How to Put Nature Into Our Neighbourhoods
Urban Greening Manual How to Put Nature into Our Neighbourhoods Application of Low Impact Urban Design and Development (LIUDD) Principles, with a Biodiversity Focus, for New Zealand Developers and Homeowners Maria Ignatieva, Colin Meurk, Marjorie van Roon, Robyn Simcock and Glenn Stewart Landcare Research Science Series No. 35 Coastal plant signature featuring sand coprosma, sea spurge, sedges, ngaio and cabbage trees, New Brighton, Christchurch. Photo: Colin Meurk Scree garden plant signatures on the Wellington Governors Bay native bush and rock gardens, the Waterfront – featuring sedges, knobby clubrush, silver and latter employing korokio, pohuehue, mikimiki, NZ fl ax, other tussock grasses, rengarenga, pohuehue, NZ iris, NZ lancewood, and cotulas in the lawn. Photo: Colin Meurk linen fl ax and reeds in swales beyond. Photo: Colin Meurk Large scale formal native (and adjacent conventional English) garden with totara, matai and miro hedges, kahikatea avenue, copses of different tree types and a diverse New Zealand border of trees and shrubs, Broadfi elds, near Prebbleton, Canterbury. Photo: Colin Meurk Urban Greening Manual How to Put Nature into Our Neighbourhoods Application of Low Impact Urban Design and Development (LIUDD) Principles, with a Biodiversity Focus, for New Zealand Developers and Homeowners Maria Ignatieva, Colin Meurk, Marjorie van Roon, Robyn Simcock and Glenn Stewart © Landcare Research New Zealand Ltd 2008 This information may be copied or reproduced electronically and distributed to others without restriction, provided Landcare Research New Zealand Ltd is acknowledged as the source of information. Under no circumstances may a charge be made for this information without the express permission of Landcare Research New Zealand Ltd. -
Section 72 Analysis for 5-Year Review Results Canterbury Regional Pest Management Strategy 2005- 2015
Section 72 Analysis for 5-year Review Results Canterbury Regional Pest Management Strategy 2005- 2015 Report No. U10/3 ISBN 978-1-877574-29-0 (hard copy) ISBN 978-1-877574-30-6 (electronic) R Maw June 2010 Section 72 Analysis for 5-year Review Results Canterbury Regional Pest Management Strategy 2005-2015 ii Section 72 Analysis for 5-year Review Results Canterbury Regional Pest Management Strategy 2005-2015 Table of Contents PART 1: INTRODUCTION ................................................................................................. 1 PART 2: CHILEAN NEEDLE GRASS ............................................................................... 3 2.1 BACKGROUND ........................................................................................................... 3 2.2 DISTRIBUTION ........................................................................................................... 3 2.3 IMPACTS ................................................................................................................... 3 2.4 EFFECTS SUMMARY ................................................................................................... 4 2.5 ANALYSIS ................................................................................................................. 4 2.6 SECTION 72 CONCLUSIONS ....................................................................................... 8 2.7 FUNDING RATIONALE ................................................................................................. 8 2.8 ANNEX 1: MAIN ASSUMPTIONS -
Significance of Substrate Soil Moisture Content for Rockfall Hazard
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2019-11 Manuscript under review for journal Nat. Hazards Earth Syst. Sci. Discussion started: 14 February 2019 c Author(s) 2019. CC BY 4.0 License. Significance of substrate soil moisture content for rockfall hazard assessment Louise Mary Vick1, Valerie Zimmer2, Christopher White3, Chris Massey4, Tim Davies5 1Institute of Geosciences, UiT The Arctic University of Norway, Dramsveien 201, Tromsø 9009, Norway 5 2State Water Resources Control Board, 1001 I Street, Sacramento, California 95814, USA 3Resource Development Consultants Limited, 8/308 Queen Street East, Hastings, Hawkes Bay, New Zealand 4GNS Science, 1 Fairway Drive, Avalon 5010, New Zealand 5Department of Geological Sciences, University of Canterbury, Christchurch 8041, New Zealand 10 Correspondence to: Louise M. Vick ([email protected]) ORCHID: https://orcid.org/0000-0001-9159-071X Abstract. Rockfall modelling is an essential tool for hazard analysis in steep terrain. Calibrating terrain parameters ensures that the model results accurately represent the site-specific hazard. Parameterizing rockfall models is challenging because rockfall runout is highly sensitive to initial conditions, rock shape, size and material properties, terrain morphology, and 15 terrain material properties. This contribution examines the mechanics of terrain scarring due to rockfall on the Port Hills of Christchurch, New Zealand. We use field-scale testing and laboratory direct-shear testing to quantify how the changing moisture content of the loessial soils can influence its strength from soft to hard, and vice versa. We calibrate the three-dimensional rockfall model RAMMS by back analysing several well-documented rockfall events, adopting dry loessial soil conditions. -
Leaf Trait–Palatability Relationships Differ Between Ungulate Species: Evidence from Cafeteria Experiments Using Naïve Tussock Grasses
AvailableLloyd et al.: on-line Leaf at: traits http://www.newzealandecology.org/nzje/ and ungulate palatability 219 Leaf trait–palatability relationships differ between ungulate species: evidence from cafeteria experiments using naïve tussock grasses Kelvin M. Lloyd1*, Meg L. Pollock2, Norman W.H. Mason3 and William G. Lee1 1Landcare Research, Private Bag 1930, Dunedin 9054, New Zealand 2SAC, Hill and Mountain Research Centre, Sustainable Livestock Systems, Kirkton, Crianlarich, FK20 8RU, Scotland, UK 3Landcare Research, Private Bag 3127, Hamilton 3240, New Zealand *Author for correspondence: (Email: [email protected]) Published on-line: 28 January 2010 Abstract: Leaf functional traits have been proposed as general indicators of plant palatability to ungulate herbivores, identifying which species are likely to be most at risk from ungulates, and how ungulate grazing may change ecosystem processes. However, few studies have tested whether leaf trait–palatability relationships are consistent across different ungulate species. The palatability of 44 native New Zealand grass taxa (from the genera Festuca and Chionochloa) to two ungulate herbivores (sheep Ovis aries and red deer Cervus elaphus scoticus) was assessed in cafeteria experiments. There were significant differences between sheep and deer in the selection or avoidance of grass taxa, in part related to differences in response to variation in leaf functional traits. Deer had a greater tendency than sheep to select grasses with a higher specific leaf area (SLA) and to avoid taxa with a low SLA, suggesting that it is not possible to generalise leaf trait–palatability relationships across different ungulate species. Results suggest different ungulate species are likely to have additive effects on the biodiversity and ecosystem functioning of New Zealand’s native grasslands. -
FT2 Earthquake Engineering Geology: Port Hills and Christchurch City
Geosciences 2013 Annual Conference of the Geoscience Society of New Zealand. Christchurch. Field Trip 2 Sunday 24th November 2013 Earthquake Engineering Geology: Port Hills and Christchurch City. Guide authors: David Bell, Janet Brehaut and Maree Hemmingsen Trip Leaders: David Bell and Valerie Zimmer Department of Geological Sciences, University of Canterbury Cover photo: Shag Rock at the entrance to the Avon‐Heathcote Estuary, modified in the Canterbury Earthquake Sequence, and now locally referred to as Shag Pile. Bibliographic reference: Bell, D.H., Brehaut, J., Hemmingsen, M. and Zimmer, V. (2013). Earthquake Engineering Geology: Port Hills and Christchurch City. In: Reid, C.M. & Hampton, S.J. (compilers). Field Trip Guides, Geosciences 2013 Conference, Christchurch, New Zealand. Geoscience Society of New Zealand Miscellaneous Publication 136B. 23 p. ISBN 978‐1‐877480‐34‐8, ISSN 2230‐4487 (print) ISSN 2230‐4495 (online) Earthquake Engineering Geology: Port Hills and Christchurch City Geosciences Health and Safety: Most of the field trip stops will be off‐street in local parks, however please take care if crossing roads. All roads are public, with some being busy and congested due to remediation work in the area. High visibility vests will be provided, so please wear these whenever not on the bus. Sturdy footwear is recommended, however we will not venture far from the coach at most locations. Route: Leave 11.00 am and travel from University of Canterbury to Sumner (Wakefield Avenue). Sumner to Redcliffs, Huntsbury Hill (Vernon Terrace), via Opawa to Porritt Park, and Dallington. Return to University of Canterbury by 5.30 pm. 2 Earthquake Engineering Geology: Port Hills and Christchurch City Geosciences Background New Zealand is located at a plate boundary between the Pacific and Australian plates (Figure 1). -
JB Et Al. 2019 Revised Manuscript
1 Geologic and geomorphic controls on rockfall hazard: how well do past rockfalls predict 2 future distributions? 3 4 Josh Borella 1,2, Mark Quigley 3,2, Zoe Krauss 4,1, Krystina Lincoln 5,1, Januka Attanayake 3, 5 Laura Stamp 5,1, Henry Lanman 6,1, Stephanie Levine 7,1, Sam Hampton 1,2, Darren Gravley 1,2 6 7 1 Frontiers Abroad, 3 Harbour View Terrace, Christchurch, 8082, New Zealand 8 2 Department of Geological Sciences, University of Canterbury, Christchurch, 8041, New Zealand 9 3 School of Earth Sciences, The University of Melbourne, Victoria, 3010, Australia 10 4 Department of Geology, Colorado College, Colorado Springs, CO, 80903, USA 11 5 Department of Geosciences, Williams College, Williamstown, MA, 01267, USA 12 6 Department of Geology, Whitman College, Walla Walla, WA, 99362, USA 13 7 Department of Geology, Carleton College, Northfield, MN, 55057, USA 14 15 Correspondence: Josh Borella ([email protected]) 16 17 KEYWORDS: Rockfall hazard, boulder spatial distributions, frequency-volume distributions, 18 Canterbury Earthquake Sequence, prehistoric rockfall boulders, deforestation, rockfall 19 source characteristics, rockfall physical properties, rockfall numerical modelling, 20 Christchurch 21 22 Abstract 23 24 To evaluate the geospatial hazard relationships between recent (contemporary) rockfalls and 25 their prehistoric predecessors, we compare the locations, physical characteristics, and 26 lithologies of rockfall boulders deposited during the 2010-2011 Canterbury earthquake 27 sequence (CES) (n=185) with those deposited prior to the CES (n=1093). Population ratios of 28 pre-CES to CES boulders at two study sites vary spatially from ~5:1 to 8.5:1. This is interpreted 29 to reflect (i) variations in CES rockfall flux due to intra- and inter-event spatial differences in 30 ground motions (e.g. -
NEW ZEALAND BOTANICAL SOCIETY NEWSLETTER NUMBER 94 December 2008 New Zealand Botanical Society
NEW ZEALAND BOTANICAL SOCIETY NEWSLETTER NUMBER 94 December 2008 New Zealand Botanical Society President: Anthony Wright Secretary/Treasurer: Ewen Cameron Committee: Bruce Clarkson, Colin Webb, Carol West Address: c/- Canterbury Museum Rolleston Avenue CHRISTCHURCH 8013 Subscriptions The 2009 ordinary and institutional subscriptions are $25 (reduced to $18 if paid by the due date on the subscription invoice). The 2009 student subscription, available to full-time students, is $12 (reduced to $9 if paid by the due date on the subscription invoice). Back issues of the Newsletter are available at $7.00 each. Since 1986 the Newsletter has appeared quarterly in March, June, September and December. New subscriptions are always welcome and these, together with back issue orders, should be sent to the Secretary/Treasurer (address above). Subscriptions are due by 28 February each year for that calendar year. Existing subscribers are sent an invoice with the December Newsletter for the next years subscription which offers a reduction if this is paid by the due date. If you are in arrears with your subscription a reminder notice comes attached to each issue of the Newsletter. Deadline for next issue The deadline for the March 2009 issue is 25 February 2008. Please post contributions to: Melanie Newfield 17 Homebush Rd Khandallah Wellington Send email contributions to [email protected]. Files are preferably in MS Word (with the suffix “.doc” but not “.docx”), as an open text document (Open Office document with suffix “.odt”) or saved as RTF or ASCII. Graphics can be sent as TIF JPG, or BMP files. Alternatively photos or line drawings can be posted and will be returned if required. -
Festuca Actae
Festuca actae COMMON NAME Banks Peninsula Fescue SYNONYMS Festuca ovina subsp. matthewsii var. grandiflora Howarth; Festuca novae-zelandicae var. grandiflora (Howarth) St.-Yves; Festuca ovina subsp. novae-zelandiae var grandiflora Howarth; Festuca ovina subsp. matthewsii var. eu-matthewsii Howarth; Festuca petriei forma tenuifolia Howarth FAMILY Poaceae AUTHORITY Festuca actae Connor FLORA CATEGORY Vascular – Native ENDEMIC TAXON Yes Festuca actae. Photographer: Alan Stewart ENDEMIC GENUS No ENDEMIC FAMILY No STRUCTURAL CLASS Grasses NVS CODE FESACT In cultivation. Photographer: John Smith- CHROMOSOME NUMBER Dodsworth 2n = 42 CURRENT CONSERVATION STATUS 2012 | At Risk – Naturally Uncommon | Qualifiers: OL PREVIOUS CONSERVATION STATUSES 2009 | At Risk – Naturally Uncommon 2004 | Range Restricted DISTRIBUTION Endemic. New Zealand: South Island (Banks Peninsula). HABITAT Coastal to montane. On rocks, rock outcrops, bluffs, talus and stabilised, sparsely vegetated slopes FEATURES Slender tussock with intravaginal branches, with fine and long glaucous leaf-blades. Leaf-sheath 50-100 mm, stramineous occasionally reddened, glabrous, striate, margins becoming membranous; apical auricles 0.4-0.7 mm, truncate or rounded, ciliate. Ligule as for auricles. Collar 0.6-1.7 mm, manifestly thickened, usually becoming brown coloured, adaxially with many small white hairs. Leaf-blade 200.0-600.0 × 0.4-0.7 mm, terete or hexagonal and ribbed, glaucous, glabrous except for prickle-teeth at pointed apex, disarticulating at collar, adaxially and on margin a multitude of small (0.10-0.15 mm) white hairs. Culm 250-600 mm, erect or geniculate at base, nodes 2-3 evident, internodes glabrous. Panicle 50-250, with 7-9 nodes of 10-30 spikelets; basal branches 40-50 mm, binate, lax, of 2-6 spikelets and naked below, soon becoming single ascending branches, uppermost 3-5 spikelets solitary on pedicels; rachis glabrous or sparsely prickle-toothed below becoming more so, branches and pedicels prickle- toothed. -
Christchurch Place Names: N - Z
Christchurch Place Names: N - Z Current name Former Origin of name Where Additional information See Source Related sources name Naughty Boys’ In 1961 two boys, In the Avon Created in the 1950s Our Environment “Two boys die after Island Frank Raymond River between when a new river Issue 14 Autumn 1998 cave in soft soil Murray, 12 and Evans Avenue channel was dredged in collapses”, The Peter Edward and Kibblewhite the Avon River near Press, 28 April Leary, 13, Street, New Tovey Street at South 1961, p 12 suffocated after a Brighton. New Brighton to ease tunnel they were flooding problems. It is a digging caved in 400m long island, on them. Local accessible only through residents say the ankle deep mud and has name of the island always been a magnet appears to be for adventurous boys. linked to that Boarded up tunnels can tragedy. still be seen on the island. New Brighton The often-quoted story Rainestown "New Brighton", "Brighton's pioneers of the naming of New Lyttelton Times, 13 are recalled", Brighton has five men April 1868, p 2 Christchurch Star- bringing their bullock “O-rua-paeroa”, Star, Sun, 3 October through modern day 8 May 1896, p 2 1949, p 2 Wainoni in 1860, "Imagine... buying crossing the Avon, “New Brighton New Brighton for settling and buying land memories”, Star, 12 February 1895, p 2 ₤300", Pegasus in the area of the park Post, 20 April 1977, adjacent to the Bower “Early New p 12 Hotel site. A plaque in Brighton”, Star, 20 the park commemorates The Borough of © Christchurch City Libraries February 2016 Page 1 of 156 Christchurch Place Names: N - Z Current name Former Origin of name Where Additional information See Source Related sources name their arrival. -
Dated Historical Biogeography of the Temperate Lohinae (Poaceae, Pooideae) Grasses in the Northern and Southern Hemispheres
-<'!'%, -^,â Availableonlineatwww.sciencedirect.com --~Î:Ùt>~h\ -'-'^ MOLECULAR s^"!! ••;' ScienceDirect PHJLOGENETICS .. ¿•_-;M^ EVOLUTION ELSEVIER Molecular Phylogenetics and Evolution 46 (2008) 932-957 ^^^^^^^ www.elsevier.com/locate/ympev Dated historical biogeography of the temperate LoHinae (Poaceae, Pooideae) grasses in the northern and southern hemispheres Luis A. Inda^, José Gabriel Segarra-Moragues^, Jochen Müller*^, Paul M. Peterson'^, Pilar Catalán^'* ^ High Polytechnic School of Huesca, University of Zaragoza, Ctra. Cuarte km 1, E-22071 Huesca, Spain Institute of Desertification Research, CSIC, Valencia, Spain '^ Friedrich-Schiller University, Jena, Germany Smithsonian Institution, Washington, DC, USA Received 25 May 2007; revised 4 October 2007; accepted 26 November 2007 Available online 5 December 2007 Abstract Divergence times and biogeographical analyses liave been conducted within the Loliinae, one of the largest subtribes of temperate grasses. New sequence data from representatives of the almost unexplored New World, New Zealand, and Eastern Asian centres were added to those of the panMediterranean region and used to reconstruct the phylogeny of the group and to calculate the times of lineage- splitting using Bayesian approaches. The traditional separation between broad-leaved and fine-leaved Festuca species was still main- tained, though several new broad-leaved lineages fell within the fine-leaved clade or were placed in an unsupported intermediate position. A strong biogeographical signal was detected for several Asian-American, American, Neozeylandic, and Macaronesian clades with dif- ferent aifinities to both the broad and the fine-leaved Festuca. Bayesian estimates of divergence and dispersal-vicariance analyses indicate that the broad-leaved and fine-leaved Loliinae likely originated in the Miocene (13 My) in the panMediterranean-SW Asian region and then expanded towards C and E Asia from where they colonized the New World.