A Repeat Bird Survey of the Upper Waimakariri River
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The Wrybill <I>Anarhynchus Frontalis</I>: a Brief Review of Status, Threats and Work in Progress
The Wrybill Anarhynchus frontalis: a brief review of status, threats and work in progress ADRIAN C. RIEGEN '1 & JOHN E. DOWDING 2 •231 ForestHill Road, Waiatarua, Auckland 8, NewZealand, e-maih riegen @xtra.co. nz; 2p.o. BOX36-274, Merivale, Christchurch 8030, New Zealand, e-maih [email protected]. nz Riegen,A.C. & Dowding, J.E. 2003. The Wrybill Anarhynchusfrontalis:a brief review of status,threats and work in progress.Wader Study Group Bull. 100: 20-24. The Wrybill is a threatenedplover endemic to New Zealandand unique in havinga bill curvedto the right.It is specializedfor breedingon bareshingle in thebraided riverbeds of Canterburyand Otago in the SouthIsland. After breeding,almost the entirepopulation migrates north and wintersin the harboursaround Auckland. The speciesis classifiedas Vulnerable. Based on countsof winteringflocks, the population currently appears to number4,500-5,000 individuals.However, countingproblems mean that trendsare difficult to determine. The mainthreats to theWrybill arebelieved to be predationon thebreeding grounds, degradation of breeding habitat,and floodingof nests.In a recentstudy in the MackenzieBasin, predation by introducedmammals (mainly stoats,cats and possibly ferrets) had a substantialimpact on Wrybill survivaland productivity. Prey- switchingby predatorsfollowing the introductionof rabbithaemorrhagic disease in 1997 probablyincreased predationrates on breedingwaders. A recentstudy of stoatsin the TasmanRiver showedthat 11% of stoat densexamined contained Wrybill remains.Breeding habitat is beinglost in somerivers and degraded in oth- ers,mainly by waterabstraction and flow manipulation,invasion of weeds,and human recreational use. Flood- ing causessome loss of nestsbut is alsobeneficial, keeping nesting areas weed-free. The breedingrange of the speciesappears to be contractingand fragmenting, with the bulk of the popula- tion now breedingin three large catchments. -
New Zealand Comprehensive II Trip Report 31St October to 16Th November 2016 (17 Days)
New Zealand Comprehensive II Trip Report 31st October to 16th November 2016 (17 days) The Critically Endangered South Island Takahe by Erik Forsyth Trip report compiled by Tour Leader: Erik Forsyth RBL New Zealand – Comprehensive II Trip Report 2016 2 Tour Summary New Zealand is a must for the serious seabird enthusiast. Not only will you see a variety of albatross, petrels and shearwaters, there are multiple- chances of getting out on the high seas and finding something unusual. Seabirds dominate this tour and views of most birds are alongside the boat. There are also several land birds which are unique to these islands: kiwis - terrestrial nocturnal inhabitants, the huge swamp hen-like Takahe - prehistoric in its looks and movements, and wattlebirds, the saddlebacks and Kokako - poor flyers with short wings Salvin’s Albatross by Erik Forsyth which bound along the branches and on the ground. On this tour we had so many highlights, including close encounters with North Island, South Island and Little Spotted Kiwi, Wandering, Northern and Southern Royal, Black-browed, Shy, Salvin’s and Chatham Albatrosses, Mottled and Black Petrels, Buller’s and Hutton’s Shearwater and South Island Takahe, North Island Kokako, the tiny Rifleman and the very cute New Zealand (South Island wren) Rockwren. With a few members of the group already at the hotel (the afternoon before the tour started), we jumped into our van and drove to the nearby Puketutu Island. Here we had a good introduction to New Zealand birding. Arriving at a bay, the canals were teeming with Black Swans, Australasian Shovelers, Mallard and several White-faced Herons. -
New Zealand Great Spotted Kiwi Quest 5Th January to 9Th January 2022 (5 Days)
New Zealand Great Spotted Kiwi Quest 5th January to 9th January 2022 (5 days) Pipipi by Adam Riley Our Great Spotted Kiwi tour is designed to seek out one of New Zealand’s most sought-after endemics. By no means guaranteed, we have two nights each at prime localities where we will maximise searching for this species. RBL New Zealand – Great Spotted Kiwi Quest Itinerary 2 Other attractions are hiking through pristine Red Beech forest surrounded by breath-taking glacier-lined mountains, where Pipipi (Brown Creeper) Blue Duck, the cute New Zealand Rockwren, New Zealand Falcon, Malherb’s (Orange-fronted) Parakeet, Fernbird, Rifleman and the friendly Kea can be found. THE TOUR AT A GLANCE… THE ITINERARY Day 1 Christchurch to Arthurs Pass Day 2 Arthurs Pass area Day 3 Arthurs Pass to Punikaiki Day 4 Punikaiki area Day 5 Punikaiki to Christchurch and depart TOUR ROUTE MAP… RBL New Zealand – Great Spotted Kiwi Quest Itinerary 3 THE TOUR IN DETAIL… Day 1: Christchurch to Arthur’s Pass. After departing Christchurch, our first stop will be the Ashley River Mouth where we will scan the mudflats for Variable and South Island Pied Oystercatchers, Bar-tailed Godwit, Pied Stilt, Wrybill and Royal Spoonbill. Less frequently recorded species may include Far Eastern Curlew, Whimbrel, the rare Black Stilt and in the surrounding trees Little Owl. Later in the morning we will drive towards Arthur’s Pass keeping a careful watch for New Zealand Falcon. A small lake at the side of the road often has New Zealand Falcon by Erik Forsyth a breeding pair of Great Crested Grebe as well as Masked Lapwing and occasionally Double-banded Plover. -
Waipara River Management Strategy
Waipara River Management Strategy Prepared by the Waipara River Working Party Contents Introduction . 3 What is the Waipara River Management Strategy?.. .. .. .. .. .. .. .. .. .4 Strategy background .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .5 Physical description of the Waipara River . 6 Ecology . 8 Geology . 10 Māori cultural values.. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 14 Geological, Ecological & Māori Cultural Values - Action Plan.. .. .. .. .. .. 16 Quality of the river environment .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 18 Access Rights And Privileges. 23 Recreational activities. 26 Karetu Bridge To White Gorge - Management Area.. .. .. .. .. .. .. .. .. 32 White Gorge To Stringers Bridge - Management Area . .35 Stringers Bridge To Barnetts Road - Management Area . 38 State Highway 1 Bridge - Management Area . 41 Wash Creek To Webbs Road - Management Area. 44 Waipara River Mouth - Management Area . 47 Acknowledgements . .51 References . .52 White Gorge Upstream To ensure that the Waipara River is managed in a way that is environmentally MISSION STATEMENT: sustainable while ensuring public access is maintained to areas of public interest. 2 Introduction The Waipara River is a small sized, hill-fed river located on the northern fringe of the The management areas of the river are as follows: Canterbury plains within the Hurunui District. The river flows from the eastern foot- • Karetu Bridge to White Gorge hills of the Southern Alps to Pegasus Bay in the west. The Waipara River is strongly influenced by the geology and structure of the area that it flows through and con- • White Gorge to Stringers Bridge tains a number of historically, scientifically and naturally important sites. The river • Stringers Bridge to Barnetts Road is highly valued by the community for its natural, physical, spiritual and recreational • State Highway 1 Bridge (Barnetts Road to Wash Creek) qualities. -
SHOREBIRDS of the HAURAKI GULF Around the Shores of the Hauraki Gulf Marine Park
This poster celebrates the species of birds commonly encountered SHOREBIRDS OF THE HAURAKI GULF around the shores of the Hauraki Gulf Marine Park. Red knot Calidris canutus Huahou Eastern curlew Numenius madagascariensis 24cm, 120g | Arctic migrant 63cm, 900g | Arctic migrant South Island pied oystercatcher Haematopus finschi Torea Black stilt 46cm, 550g | Endemic Himantopus novaezelandiae Kaki 40cm, 220g | Endemic Pied stilt Himantopus himantopus leucocephalus Poaka 35cm, 190g | Native (breeding) (non-breeding) Variable oystercatcher Haematopus unicolor Toreapango 48cm, 725g | Endemic Bar-tailed godwit Limosa lapponica baueri Kuaka male: 39cm, 300g | female: 41cm, 350g | Arctic migrant Spur-winged plover Vanellus miles novaehollandiae 38cm, 360g | Native Whimbrel Numenius phaeopus variegatus Wrybill Anarhynchus frontalis 43cm, 450g | Arctic migrant Ngutu pare Ruddy turnstone 20cm, 60g | Endemic Arenaria interpres Northern New Zealand dotterel Charadrius obscurus aquilonius Tuturiwhatu 23cm, 120g | Arctic migrant Shore plover 25cm, 160g | Endemic Thinornis novaeseelandiae Tuturuatu Banded dotterel Charadrius bicinctus bicinctus Pohowera 20cm, 60g | Endemic 20cm, 60g | Endemic (male breeding) Pacific golden plover Pluvialis fulva (juvenile) 25cm, 130g | Arctic migrant (female non-breeding) (breeding) Black-fronted dotterel Curlew sandpiper Calidris ferruginea Elseyornis melanops 19cm, 60g | Arctic migrant 17cm, 33g | Native (male-breeding) (non-breeding) (breeding) (non-breeding) Terek sandpiper Tringa cinerea 23cm, 70g | Arctic migrant -
Which Subspecies of Mongolian Dotterel Visit New Zealand?
Notornis, 2000, Vol. 47: 125-126 0029-4470 O The Ornithological Society of New Zealand, Inc. 2000 SHORT NOTE Which subspecies of Mongolian dotterel visit New Zealand? G.R. PARRISH 145 Church Street, Whangarei The Mongolian dotterel (Lesser sand plover, Charadrius no white patches in its black mask. The crown was very mongolus) breeds across eastern Asia from the Himalayas pale chestnut with a pale whitish supercilium stripe. The to northeast Siberia. The five subspecies form two groups: nape, hindneck, side of neck, foreneck and breast were a the C. m. atifvons group includes C. m. atifrons, C. m. deep brick red colour. The band at the upper and lower pamirensis, and C. m. schaeferi, and breeds in central breast was sharply demarcated from the white of the throat Russia, the Himalayas, and southern and eastern Tibet; and belly. This band appeared to extend to the upper flanks the C. m. mongolus group comprises C. rn. mongolus, but my vision was obscured by glasswort. There was no and C. m. stegmanni which breed in eastern inland Russia, black line dividing the white of the throat and the red of Kamchatka, the Commander Islands, and the Chukotsk the breast. The back and wings were greyish brown with Peninsula. Members of the C. m. atifrons group winter some white around the edge of the wing feathers. I from Africa to India and the Greater Sunda Islands, concluded it was a Mongolian dotterel of the C. m. whereas those of the C. m. mongolus group winter "atrifrons group" (Hayman et al. 1986). It closely between Taiwan and Australia (Hayman et al. -
The Kaiapoi River Has Historically Been Valued As a Freshwater Tidal Waterway and Port That Provided for Many Unique Values and Activities
Assessment of the state of a tidal waterway - the Lower Kaiapoi River Report No. R18/7 ISBN 978-1-98-852079-7 (print) 978-1-98-852080-3 (web) Assessment of the state of a tidal waterway - the Lower Kaiapoi River Report No. R18/7 ISBN 978-1-98-852079-7 (print) 978-1-98-852080-3 (web) Adrian Meredith March 2018 Name Date Prepared by: Adrian Meredith March 2018 Principal Scientist Reviewed by: Helen Shaw, Surface Water June 2018 Science Manager Suzanne Gabites, Team Leader June 2018 Hydrological Science Approved by: Tim Davie July 2018 Chief Scientist Report No. R18/7 ISBN 978-1-98-852079-7 (print) 978-1-98-852080-3 (web) 200 Tuam Street PO Box 345 Christchurch 8140 Phone (03) 365 3828 Fax (03) 365 3194 75 Church Street PO Box 550 Timaru 7940 Phone (03) 687 7800 Fax (03) 687 7808 Website: www.ecan.govt.nz Customer Services Phone 0800 324 636 Assessment of the state of a tidal waterway - the Lower Kaiapoi River Executive summary The lower Kaiapoi River is a large river channel that traverses Kaiapoi township and drains to the large alpine fed braided Waimakariri River less than two kilometres from the sea. It is unique in being a previous channel of the Waimakariri River (the North Branch), receiving drainage from several major plains tributaries, and being strongly tidal over several kilometres of its length. It is a highly valued river, a culturally important waterway, a designated port and navigational waterway, and an important recreational and fishery resource. However, in recent years there have been complaints of degradation of its water quality and ecology. -
Pegasus, Woodend & Waikuku
Pegasus, Woodend & Waikuku COMMUNITY DIRECTORY 2019/20 Local services, businesses, retail & community groups Compiled and produced by the Pegasus Residents’ Group Inc. Available online at www.pegasusresidentsgroup.com Middle two photos courtesy of Allan McGregor Photography A-Z INDEX SEE PAGE 64 A familiar face to CATEGORY INDEX North Canterbury motorists ESSENTIAL SERVICES ............................. 4 Lions ............................................................. 13 Member of Parliament ................................. 14 COMMUNITY SUPPORT ........................ 5 Pet Home Care & Boarding ........................... 14 for over 40 years! Preschooler Activities/Playgroups ................ 14 LOCAL SERVICES, BUSINESS, RETAIL Photography/Video ...................................... 14 Accommodation ............................................. 6 Professional Services .................................... 14 Accounting/Bookwork .................................... 6 Promotional Services .................................... 15 Animal Care and Supplies ............................... 6 Real Estate .................................................... 15 Automotive Services ....................................... 6 Retail - Alcohol.............................................. 15 Car Sales ......................................................... 7 Retail - Antiques ........................................... 15 Celebrant ........................................................ 7 Retail - Arts & Crafts .................................... -
“Glacial Lake Speight”, New Zealand? an Example for the Validity of Detailed Geomorphological Assessment with the Study of Mountain Glaciations
Express report E&G Quaternary Sci. J., 67, 25–31, 2018 https://doi.org/10.5194/egqsj-67-25-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Disestablishing “Glacial Lake Speight”, New Zealand? An example for the validity of detailed geomorphological assessment with the study of mountain glaciations Stefan Winkler1, David Bell2, Maree Hemmingsen3, Kate Pedley2, and Anna Schoch4 1Department of Geography and Geology, University of Würzburg, Am Hubland, 97074 Würzburg, Germany 2Department of Geological Sciences, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand 3Primary Science Solutions Ltd., Woodbury Street 75, Russley, Christchurch 8042, New Zealand 4Department of Geography, University of Bonn, Meckenheimer Allee 166, 53115 Bonn, Germany Correspondence: Stefan Winkler ([email protected]) Relevant dates: Received: 30 May 2018 – Revised: 10 August 2018 – Accepted: 21 August 2018 – Published: 28 August 2018 How to cite: Winkler, S., Bell, D., Hemmingsen, M., Pedley, K., and Schoch, A.: Disestablishing “Glacial Lake Speight”, New Zealand? An example for the validity of detailed geomorphological assessment with the study of mountain glaciations, E&G Quaternary Sci. J., 67, 25–31, https://doi.org/10.5194/egqsj- 67-25-2018, 2018. 1 Introduction implications beyond these fluvial aspects. Palaeoseismolog- ical studies claim to have detected signals of major Alpine The middle Waimakariri River catchment in the Southern Fault earthquakes in coastal environments along the eastern Alps of New Zealand, informally defined here as its reach up- seaboard of the South Island (McFadgen and Goff, 2005). stream of Waimakariri Gorge to the junction of Bealey River This requires high connectivity between the lower reaches of (Fig. -
Draft Canterbury CMS 2013 Vol II: Maps
BU18 BV17 BV18 BV16 Donoghues BV17 BV18 BV16 BV17 M ik onu Fergusons i R iv Kakapotahi er Pukekura W a i ta h Waitaha a a R iv e r Lake Ianthe/Matahi W an g anui Rive r BV16 BV17 BV18 BW15 BW16 BW17 BW18 Saltwater Lagoon Herepo W ha ta ro a Ri aitangi ver W taon a R ive r Lake Rotokino Rotokino Ōkārito Lagoon Te Taho Ōkārito The Forks Lake Wahapo BW15 BW16 BW16 BW17 BW17 BW18 r e v i R to ri kā Ō Lake Mapourika Perth River Tatare HAKATERE W ai CONSERVATION h o R PARK i v e r C a l le r y BW15 R BW16 AORAKI TE KAHUI BW17 BW18 iv BX15 e BX16 MOUNT COOK KAUPEKA BX17 BX18 r NATIONAL PARK CONSERVATION PARK Map 6.6 Public conservation land inventory Conservation Management Strategy Canterbury 01 2 4 6 8 Map 6 of 24 Km Conservation unit data is current as of 21/12/2012 51 Public conservation land inventory Canterbury Map table 6.7 Conservation Conservation Unit Name Legal Status Conservation Legal Description Description Unit number Unit Area I35028 Adams Wilderness Area CAWL 7143.0 Wilderness Area - s.20 Conservation Act 1987 - J35001 Rangitata/Rakaia Head Waters Conservation Area CAST 53959.6 Stewardship Area - s.25 Conservation Act 1987 Priority ecosystem J35002 Rakaia Forest Conservation Area CAST 4891.6 Stewardship Area - s.25 Conservation Act 1987 Priority ecosystem J35007 Marginal Strip - Double Hill CAMSM 19.8 Moveable Marginal Strip - s.24(1) & (2) Conservation Act 1987 - J35009 Local Purpose Reserve Public Utility Lake Stream RALP 0.5 Local Purpose Reserve - s.23 Reserves Act 1977 - K34001 Central Southern Alps Wilberforce Conservation -
Waimakariri District Flood Hazard Management Strategy
Waimakariri District Flood Hazard Management Strategy Ashley River Floodplain Investigation Report No. R08/23 ISBN 978-1-86937-804-2 Tony Oliver June 2008 Report R08/23 ISBN 978-1-86937-804-2 58 Kilmore Street PO Box 345 Christchurch Phone (03) 365 3828 Fax (03) 365 3194 75 Church Street PO Box 550 Timaru Phone (03) 688 9069 Fax (03) 688 9067 Website: www.ecan.govt.nz Customer Services Phone 0800 324 636 Environment Canterbury Technical Report EXECUTIVE SUMMARY This study of the Ashley River floodplain uses a combined one and two dimensional hydraulic computer model to estimate flood extent and depths on the Ashley River floodplain. Modelling has indicated the current capacity of the Ashley River stopbanked system is approximately equivalent to the 2% AEP (50 year return period) flood event. Breakouts however, could occur in more frequent events. Stopbank breaches and outflows onto the floodplain could potentially occur anywhere along the stopbanks. Breakout scenarios onto the floodplain have been modelled for the 1%, 0.5% and 0.2% AEP (i.e. 100, 200 and 500 year return period) events at the most likely breakout locations. The modelling indicates significant flooding to large areas of land between the Ashley and Waimakariri Rivers. Kaiapoi and adjacent areas are predicted to be flooded to depths over 1 metres in the 0.2% AEP (500 year return period) event. The impact of future urbanisation in Kaiapoi has also been modelled. It is hoped the floodplain maps and associated depths will assist land use planning within the area and provide information on minimum floor levels for new dwellings located on the floodplain, where appropriate. -
Regions of Liquefaction Damage in Kaiapoi Following the Canterbury Earthquakes and Their Correlation with Former River Channels
Regions Of Liquefaction Damage In Kaiapoi Following The Canterbury Earthquakes And Their Correlation With Former River Channels L.M. Wotherspoon, M.J. Pender & R.P. Orense The University of Auckland, Auckland, New Zealand SUMMARY: The town of Kaiapoi, 17 km north of the city of Christchurch in the Canterbury region of New Zealand, suffered significant damage as a result of liquefaction and lateral spreading during the 2010-2011 Canterbury earthquake sequence. Severe lateral spreading and large volumes of ejecta were present throughout the town and surrounding region. Shifts in the path of the rivers in the region have been extensive since the beginnings of European settlement in the 1850s, and as a result there are multiple areas within the town and surrounding area that were, until recently, channels of the river. Using historical data, areas that had been reclaimed were identified, and when compared with the areas of severe liquefaction damage following these earthquakes, the strong correlation between the two was revealed. The significant damage to buildings, infrastructure and services in these regions highlights the importance of having a clear understanding of historical river modifications in seismically active regions. Keywords: Liquefaction, lateral spreading, Canterbury earthquakes, river modification 1. INTRODUCTION Kaiapoi is a small town approximately 17 km north of the city of Christchurch in the Canterbury region of New Zealand (See Figure 1 and 3a). On 4 September 2010, the Mw7.1 Darfield earthquake occurred 42 km to the south west of Kaiapoi. This earthquake resulted in severe liquefaction-induced damage in both Christchurch and Kaiapoi, with Kaiapoi experiencing some of the most severe damage from the resulting lateral spreading, settlement and ejected material.