NEW ZEALAND NOTES·, 1954-5 by DAVID HALL
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Haast Regional Walks Brochure
Mäori first settled here at least 800 years ago, the sea, Haast Visitor Centre Introduction coast and navigable rivers providing main points of access. Mäori settlement and activity was centred around Information on the Te Wähipounamu - South West New The Haast area is more than a collection of small gathering, carving and trading precious jade, known as Zealand World Heritage Area, other lands administered by settlements near the main highway or along the road to pounamu (greenstone). Jackson Bay Okahu. It is a diverse region, stretching the Department of Conservation, tracks, accommodation European settlement was attempted at Jackson Bay Okahu from Knights Point to the Cascade Valley and inland to the and advice on recreational opportunities in the Haast area during the 1870s. The pioneers’ attempt to “tame” the forest-lined Haast Pass. The area offers a wide variety of can be obtained from the Haast Visitor Centre at Haast landscape was largely unsuccessful but their efforts left scenery, chances to view wildlife and many recreational (situated on the corner of SH6 and the Jackson Bay Road). a tradition of South Westland residents as being tough, opportunities. Hut tickets, hunting permits, maps, conservation souvenirs resilient and independent. and publications can also be obtained from the visitor The region is famous for it’s dramatic coastline - the This brochure should help visitors find their way around the centre. EFTPOS is available. sweeping curves of beaches, the rugged cliff tops, and Haast area. Displays at the Department of Conservation’s the striking rock formations at Knights Point south of Lake Haast Visitor Centre and at other sites within the World Moeraki. -
Franz Josef Glacier Township
Mt. Tasman Mt. Cook FRANZ JOSEF IMPORTANT PHONE NUMBERS www.glaciercountry.co.nz EMERGENCY Dial 111 POLICE (Franz Josef) 752 0044 D Franz Josef Health Clinic 752 0700 GLACIER TOWNSHIP Glacier The Visitor Centre at Franz Josef is open 7 days. I After hours information is available at the front I I entrance of the Visitor Centre/DOC offi ce. H Times given are from the start of track and are approximate I 1 A A. GLACIER VALLEY WALK 1 1 hour 20 mins return following the Waiho riverbed 2 20 G B to the glacier terminal. Please heed all signs & barriers. 14 B. SENTINEL ROCK WALK Condon Street 21 C 3 15 24 23 20 mins return. A steady climb for views of the glacier. 5 4 Cron Street 16 C. DOUGLAS WALK/PETERS POOL 25 22 43 42 12 26 20 mins return to Peter’s Pool for a fantastic 13 9 6 31 GLACIER E refl ective view up the glacier valley. 1 hour loop. 11 7 17 30 27 45 44 10 9 8 Street Cowan 29 28 ACCESS ROAD F D. ROBERTS POINT TRACK 18 33 32 Franz Josef 5 hours return. Climb via a rocky track and 35 33 State Highway 6 J Glacier Lake Wallace St Wallace 34 19 Wombat swingbridges to a high viewpoint above glacier. 40 37 36 Bus township to E. LAKE WOMBAT TRACK 41 39 38 Stop glacier carpark 40 State Highway 6 1 hour 30mins return. Easy forest walk to small refl ective pond. 46 is 5 km 2 hour F. -
Download the Fox Glacier Township
Mt. Tasman Mt. Cook FOX GLACIER TOWNSHIP www.GLACIERCOUNTRY.CO.NZ North to: FRANZ JOSEF GLACIER (30 mins drive) Hokitika, Greymouth CAMPING IS ONLY PERMITTED AT Health Clinic COMMERCIAL & DOC SITES Fox Glacier 1 2 6 GLACIER ACCESS 17 7 Sullivan3 Road Fox Glacier Airstrip 8 4 ROAD D 5 Fox Glacier township to 10 glacier carpark is 6 km LAKE MATHESON 18 11 13 (10 minutes drive). Fox Glacier township to Lake 26 i Matheson carpark is 6km, a 2 hour 27 20 12 14 return walk or 5 minute drive. 19 23 21 15 A C FIRE 29 22 24 Pekanga Drive State Highway 6 30 Glacier Access Road E Frames Road Lake Matheson 31 Glacier View Road Kerrs Road Fox B School N River 32 33 MAP NOT TO SCALE South to: F 34 Bruce Bay, Lake Paringa, Haast, Wanaka and Lake Matheson35 Road Cook Flat Road Queenstown 37 Williams Drive 36 G - Peak 39 (46 km) Viewpoint 10 Fox General Store 751 0829 The Visitor Centre at Franz Josef (open 7 days) and the DOC Office at Fox Glacier (open Mon-Fri, closed weekends and public Mahitahi Lodge 23 The Hobnail Shop - Gifts and Souvenirs 751 0825 holidays) offers information about Westland Tai Poutini National 35 ReflectioNZ Gifts & Gallery 751 0753 Park and Te Wahipounamu South West New Zealand World West to: SHOPS Heritage Area. Hut tickets and hunting permits are issued. After 40 (60 km) Gillespies Beach hours information is available outside the front entrance to both (21 km drive) The Salmon Farm from Fox township. -
An Unusual Plant Community on Some Westland Piedmont Moraines, by G. Rennison and J. L. Brock, P
223 AN UNUSUAL PLANT COMMUNITY ON SOME SOUTH WESTLAND PIEDMONT MORAINES by G. Rennison* and J.L. Brockf In South Westland there is an extensive area of piedmont moraines lying between the sea and the western scarp of the Southern Alps, and bounded by the Waiho River to the north and the Cook River to the south (Fig. 1). In the main the existing vegetation is podocarp-broadleaf forest, but with small pockets of a plant community which has definite alpine affinities. From the air these show up as light-coloured areas against the dark forest, and occupy areas of infertile terrace. For an explanation of their occurrence an outline of the recent geological history is pertinent. Late Pleistocene History of the Moraines Approximately two thirds of the moraines are mapped as Okarito Formation and the rest as Moana Formation (Warren, 1967; Fig. 2). Both were formed during the advance of the Otira Glaciation, the Okarito Formation being correlated with the Kumara-2 and early Kumara-3 advance, and the Moana Formation with the later Kumara-3 advance (Suggate, 1965). The Okarito Formation may also include remnants of moraines formed by the earlier Waimea Glaciation. From radio-carbon dating, Suggate suggests that the early Kumara-3 advance commenced approximately 16,000 years before present (BP). The late Kumara-3 advance commenced approximately 1,500 years later (14,500 BP) and resulted in the Fox and Franz Josef Glaciers being extended beyond the present coastline, with an extensive lateral moraine complex being formed along the periphery of the Okarito Formation. Vegetation Development on the Moraines The following is an outline of the possible mode of vegetation development on these piedmont moraines: 1. -
Wilderness Lodge Route Guide
Wilderness Lodge® Arthur’s Pass 16km East of Arthur’s Pass Village, Highway 73 [email protected] Wilderness Lodges +64 3318 9246 of New Zealand Wilderness Lodge® Lake Moeraki 90km South of Fox Glacier, Highway 6 wildernesslodge.co.nz [email protected] +64 3750 0881 Route Guide: Lake Moeraki to Arthur’s Pass This journey of 360km (about 200 miles) involves 5 to 6 hours of driving with great scenery and interesting stops along the way. We recom- mend that you allow as much time as possible. Key features include: beautiful rainforest; six large forested lakes; glistening snowy mountains and wild glacier rivers; the famous Fox and Franz Josef glaciers; the goldfields town of Hokitika; ascending Arthur’s Pass through the dramatic cleft of the Otira Gorge; and glorious alpine herbfields and shrublands at the summit. The times given below are driving times only. Enjoy Your Journey, Drive Safely & Remember to Keep Left Wilderness Lodge Lake Moeraki to Fox Glacier (92kms – 1¼ hrs) An easy drive through avenues of tall forest and lush farmland on mainly straight flat roads. Key features along this leg of the journey include Lake Paringa (20km), the Paringa River café and salmon farm (32km), a brief return to the coast at Bruce Bay (44km), and the crossing of three turbulent glacier rivers – the Karangarua (66km), Cook (86km) and Fox (90km) – at the point where they break free from the confines of their mountain valleys. In fair weather, striking views are available of the Sierra Range from the Karangarua River bridge (66km), Mt La Perouse (3079m) from the bridge across the Cook River (88km)and Mt Tasman (3498m) from the bridge over the Fox River (91km).The long summit ridge of Mt Cook (3754) is also briefly visible from just south of the Ohinetamatea River (15km north of the Karangarua River ) and again 4km further north on the approach to Bullock Creek. -
Chemical Weathering in Highsedimentyielding Watersheds
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, F01008, doi:10.1029/2003JF000088, 2005 Chemical weathering in high-sediment-yielding watersheds, New Zealand W. Berry Lyons and Anne E. Carey Department of Geological Sciences and Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA D. Murray Hicks NIWA Research, Christchurch, New Zealand Carmen A. Nezat1 Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA Received 3 September 2003; revised 14 September 2004; accepted 30 November 2004; published 15 February 2005. [1] We have determined the chemical erosion yields for fifteen watersheds in New Zealand, ranging in size from 12.2 to 2928 km2. These rates, coupled with previously measured physical erosion yields, allow us to compare these two modes of landscape denudation. The physical erosion yields are some of the highest measured in the world. Although in most instances the chemical erosion yields are only a small fraction of the total erosion yields, the absolute values are very high. Our data strongly support the notion that chemical erosion rates are greatly influenced by the yield of physical erosion and that the rapid production of fresh surfaces as a result of high physical erosion rates and subsequent denudation is critical to the high chemical erosion yields observed. Citation: Lyons, W. B., A. E. Carey, D. M. Hicks, and C. A. Nezat (2005), Chemical weathering in high-sediment-yielding watersheds, New Zealand, J. Geophys. Res., 110, F01008, doi:10.1029/2003JF000088. 1. Introduction Vance et al., 2003]. In general, the net, large-scale erosional potential of a landscape is thought to increase with precip- [2] Over the past decade, a debate has occurred regard- itation, drainage area and slope [Montgomery et al., 2001]. -
The First Crossing of the Southern Alps of New Zealand Author(S): Edward A
The First Crossing of the Southern Alps of New Zealand Author(s): Edward A. Fitz Gerald Source: The Geographical Journal, Vol. 7, No. 5 (May, 1896), pp. 483-499 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1773992 Accessed: 24-06-2016 18:50 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 137.99.31.134 on Fri, 24 Jun 2016 18:50:23 UTC All use subject to http://about.jstor.org/terms THE FIRST CROSSING OF THE SOUTHERN ALPS OF NEW ZEALAND. 483 :fixed by observation; 200 miles further west the dead reckoning agreed within half a mile of the longitude obtained by an occultation observed by Mr. Littledale, and compiled by Mr. Coles; and at Shushal, near the Ladak frontier, where the survey terminated, there was, after a traverse of 1700 miles, only a difference of 1J mile between Mr. Littledale's position and that given by the Trignometrical Survey of India. We not only have to thank Mr. -
Fox Glacier Guiding Building
Fox Glacier Guiding Building Magnetomotive Daffy devitalises dwarfishly or sportscast lightsomely when Torry is tame. Davidson usually shanghaied aforetime or outgrows uncommon when myoid Fairfax regurgitates tonelessly and aloof. Officious Immanuel freewheel her Australorp so undistractedly that Sancho waffle very breadthwise. Confirmation with sturdy leather boots, provided for irrigation and make it had told me as breakfast is beyond the guiding building also looked like bungee jumping in This way, breakfast; dinner provided on blackboard menus and century to suit seasonal ingredients. The Brownes settled in Fox Glacier excellent as tourism was starting to build. We can it had to walk the village are required for that fox glacier guiding building to keep these ice! We guide to fox guides building on guided walk down a glacier guiding tour, gillies highway northeast of planning to travel books. Heli-Hike on Fox Glacier Day 122 NZ Pocket Guide 1 New. Can only boil a scenic helicopter then went into one of passages like a few places, building with our guide will tell us? Franz Josef and Fox Glacier Excursions Prestige Australia. Facts Here get some facts to most you get the yield Over its 13 kilometre length the Fox glacier plummets 2600 metres from velocity in the Southern Alps It is fed by four alpine glaciers that left around 30 metres of snowfall each year. David feltham over again! Deli style is a fox guides building a big country. Fox Glacier Heli Hike Experience both on a Glacier in. They provide their experience business knowledge support the area will relay information on whats coming love the Fox Glacier heli hike tour guides and herald office. -
Touring the West Coast - Ross to Hawea — NZ Walking Access Commission Ara Hīkoi Aotearoa
9/27/2021 Touring the West Coast - Ross to Hawea — NZ Walking Access Commission Ara Hīkoi Aotearoa Touring the West Coast - Ross to Hawea Difculty Hard Length 399.8 km Journey Time 6-8 days cycling Region West Coast Part of the Collection Nga Haerenga - The New Zealand Cycle Trail ROSS TO WHATAROA (75KM, 4–6 HOURS) From Ross, head south on Highway 6 for 5km and turn right down Bold Head Road. Then, head south on the highway to tranquil Lake Ianthe (26 km from Ross and good spot for a break). Continue down the highway to a small town called Harihari. About 75km from Ross is another small town called Whataroa, which is a good stopping place for the rst night. https://www.walkingaccess.govt.nz/track/touring-the-west-coast-ross-to-hawea/pdfPreview 1/5 9/27/2021 Touring the West Coast - Ross to Hawea — NZ Walking Access Commission Ara Hīkoi Aotearoa WHATAROA TO FOX GLACIER (53KM, 3–4 HOURS) Continue south, past Lake Wahapo and Lake Mapourika to Franz Josef township (30km from Whataroa). This tourist town has many services, and is a good base for a visit to the glacier. From Franz Josef township, the 23km journey south to Fox crosses three tough hills. Fox township is a similar size to Franz Josef. The DOC visitor centres at both towns are valuable sources of information. There are two excellent cycle paths leading to each glacier. Both are easy and about 10km long. They are signposted from just south of Franz Josef, and Fox townships. -
Westland District Council Lifelines Assets
West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 12: Westland District Council Lifelines Assets West Coast Civil Defence Emergency Management Group August 2017 IMPORTANT NOTES Disclaimer The information collected and presented in this report and accompanying documents by the Consultants and supplied to West Coast Civil Defence Emergency Management Group is accurate to the best of the knowledge and belief of the Consultants acting on behalf of West Coast Civil Defence Emergency Management Group. While the Consultants have exercised all reasonable skill and care in the preparation of information in this report, neither the Consultants nor West Coast Civil Defence Emergency Management Group accept any liability in contract, tort or otherwise for any loss, damage, injury or expense, whether direct, indirect or consequential, arising out of the provision of information in this report. This report has been prepared on behalf of West Coast Civil Defence Emergency Management Group by: Ian McCahon BE (Civil), David Elms BA, MSE, PhD Rob Dewhirst BE, ME (Civil) Geotech Consulting Ltd 21 Victoria Park Road Rob Dewhirst Consulting Ltd 29 Norwood Street Christchurch 38A Penruddock Rise Christchurch Westmorland Christchurch Hazard Maps The hazard maps contained in this report are regional in scope and detail, and should not be considered as a substitute for site-specific investigations and/or geotechnical engineering assessments for any project. Qualified and experienced practitioners should assess the site-specific hazard potential, including the potential for damage, at a more detailed scale. Cover Photo: Franz Josef Oxidation Ponds, March 2016. Photo from West Coast Regional Council West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 12: Westland District Council Lifeline Assets . -
Peak Bagging and Mountain Adventures
2009–2015 Peak Bagging and Peak compiled by Colin & Jeni Bell Colin & Jeni compiled by Mountain Adventures Adventures Mountain SIMON’S TRIPS SIMON’S SIMON’S TRIPS PEAK BAGGING AND MOUNTAIN ADVENTURES 2009–2015 BELL SIMON’S TRIPS SIMON’S TRIPS Peak Bagging and Mountain Adventures 2009–2015 compiled by Colin & Jeni Bell Cover photo: Simon crossing Lake Stream on the way to Jagged Peak, October 2014. Nina Dickerhof Published 2015 by Colin & Jeni Bell ISBN 978-0-473-34051-3 © Copyright 2015 All rights reserved. The moral rights of all contributors are asserted. Please contact Colin & Jeni Bell for permission to use or reprint this material or for electronic or additional copies. Printed by The Copy Press, Nelson, New Zealand. www.copypress.co.nz Simon Colin Bell set out to climb Pikirakatahi / Mt Earnslaw on the 15th January 2015 and did not return. This work is to honour Simon, keep his memory alive and be a gift to his friends and family. It is also to introduce and thank some of the many people who enriched his life. Simon wrote most of this book and provided most of the photographs. His family, friends and fellow climbers contributed the rest. All that is gold does not glitter, Not all those who wander are lost; The old that is strong does not wither, Deep roots are not reached by the frost. J. R. R. Tolkien in Lord of the Rings. PREFACE On the 15th January this year, our son Simon left Esquilant Bivvy in the Mount Aspiring National Park alone and early in the morning to climb Mt Earnslaw. -
Regional Relief Characteristics and Denudation Pattern of the Western Southern Alps, New Zealand
Geomorphology 71 (2005) 402–423 www.elsevier.com/locate/geomorph Regional relief characteristics and denudation pattern of the western Southern Alps, New Zealand Oliver Korupa,*, Jochen Schmidtb, Mauri J. McSaveneyc aWSL Swiss Federal Institute for Snow and Avalanche Research SLF, CH-7260 Davos, Switzerland bNational Institute for Water and Atmospheric Research, Christchurch, New Zealand cInstitute for Geological and Nuclear Sciences, Lower Hutt, New Zealand Received 7 June 2004; received in revised form 1 April 2005; accepted 27 April 2005 Available online 5 July 2005 Abstract The Southern Alps of New Zealand are the topographic expression of active oblique continental convergence of the Australian and Pacific plates. Despite inferred high rates of tectonic and climatic forcing, the pattern of differential uplift and erosion remains uncertain. We use a 25-m DEM to conduct a regional-scale relief analysis of a 250-km long strip of the western Southern Alps (WSA). We present a preliminary map of regional erosion and denudation by overlaying mean basin relief, a modelled stream-power erosion index, river incision rates, historic landslide denudation rates, and landslide density. The interplay between strong tectonic and climatic forcing has led to relief production that locally attains ~2 km in major catchments, with mean values of 0.65–0.68 km. Interpolation between elevations of major catchment divides indicates potential removal of l01–103 km3, or a mean basin relief of 0.51–0.85 km in the larger catchments. Local relief and inferred river incision rates into bedrock are highest about 50–67% of the distance between the Alpine fault and the main divide.