Taieri River Morphology and Riparian Management Strategy (Strath Taieri) May 2016
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Proceedings of the Indiana Academy of Science
Origin of the Mitchell Plain in South-Central Indiana 1 Richard L. Powell, Indiana Geological Survey The pre-karst surface of the southern part of the Mitchell Plain was leveled by surface streams of late Tertiary age that headed on the plain or within the Norman Upland and flowed through re-entrant valleys in the Crawford Upland into the pre-Pleistocene Ohio River. The karst features and subterranean drainage characteristic of the Mitchell Plain developed as a lower base level was established by rejuvenation during the late Tertiary or early Pleistocene. These ancient stream routes were first noticed on the Corydon West, Depauw, Fredericksburg, Hardinsburg, Leavenworth, Mauckport, Milltown, and New Amsterdam topographic quadrangles, which cover part of the Mitchell Plain and the Crawford Upland. The ancient stream courses are represented by three kinds of topographic features which are well shown on these maps : hanging dry valleys, bedrock terraces, and abandoned meander loops. The topographic features were checked on aerial photographs and in the field to determine their geologic characteristics. The fossil drainage system studied occupies part of the present drainage basins of Blue River, Indian Creek, and Buck Creek, which are tributaries of the Ohio River (fig. 1). This combined drainage area Figure 1. Map of south-central Indiana showing- the location of drainage features. includes approximately 900 square miles mostly in Crawford, Harrison, and Washington Counties. This drainage basin includes parts of three physiographic units: the Norman Upland, the Mitchell Plain, and the Crawford Upland (2). The Norman Upland is upheld by resistant shales and siltstones of early Mississippian age, which form an eastward facing cuesta that is called the Knobstone Escarpment. -
Otago Conservancy
A Directory of Wetlands in New Zealand OTAGO CONSERVANCY Sutton Salt Lake (67) Location: 45o34'S, 170o05'E. 2.7 km from Sutton and 8 km from Middlemarch, Straith-Tari area, Otago Region, South Island. Area: 3.7 ha. Altitude: 250 m. Overview: Sutton Salt Lake is a valuable example of an inland or athalassic saline lake, with a considerable variety of saline habitats around its margin and in adjacent slightly saline boggy depressions. The lake is situated in one of the few areas in New Zealand where conditions favour saline lakes (i.e. where precipitation is lower than evaporation). An endemic aquatic animal, Ephydrella novaezealandiae, is present, and there is an interesting pattern of vegetation zonation. Physical features: Sutton Salt Lake is a natural, inland or athalassic saline lake with an average depth of 30 cm and a salinity of 15%. The lake has no known inflow or outflow. The soils are saline and alkaline at the lake margin (sodium-saturated clays), and surrounded by yellow-grey earths and dry subdygrous Matarae. The parent material is loess. Shallow boggy depressions exist near the lake, and there is a narrow fringe of salt tolerant vegetation at the lake margin. Algal communities are present, and often submerged by lake water. The average annual rainfall is about 480 mm, while annual evaporation is about 710 mm. Ecological features: Sutton Salt Lake is one of only five examples of inland saline habitats of botanical value in Central Otago. This is the only area in New Zealand which is suitable for the existence of this habitat, since in general rainfall is high, evaporation is low, and endorheic drainage systems are absent. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Clyde Railway Station, Recreation Reserve, Clyde
Review of existing conservation plans for the Clyde Museums Feasibility Study Project Clyde Railway Station, Recreation Reserve, Clyde. Date Plan Published: December 2011 Commissioned by Central Otago District Council Prepared by Robin Miller MNZIBS MRICS Origin Consultants Ltd August 2018 Architecture Heritage Archaeology Origin Consultants Ltd Rear of 38 Buckingham Street, Arrowtown & Level 4, Security Buildings, 115 Stuart Street, Dunedin Review of existing conservation plans for Clyde Museums Project Building: Clyde Railway Station Date of conservation plan: December 2011 Brief history: • Opened on 2nd April 1907 as a Troup Type B station. • Construction of the railway began on 7th June 1878 with an estimated construction duration of 6 years to reach Wanaka – the line actually reached Cromwell in 1921 where it stopped. • The station serviced the fruit industry and the demand for excursion trains, but suffered from competition from road transport, particularly from 1960 onwards. The 1980 station on the outskirts of the town was built to serve the construction of the Clyde dam; the engineering works to which closed the line to Cromwell and the 1907 station. After that, the line between Middlemarch to Clyde was abandoned completely in 1990. • Apart from the station and a short section of line, a few former railway houses remain nearby, together with the goods shed that was relocated to the adjacent Briar Herb Factory Museum site. • In 1997, the station was registered as a Category II Historic Place (Heritage New Zealand Pouhere Taonga) and it is also a protected building in the CODC District Plan. Summary of findings: • The station building has high heritage significance on both a local & regional basis. -
Waste for Otago (The Omnibus Plan Change)
Key Issues Report Plan Change 8 to the Regional Plan: Water for Otago and Plan Change 1 to the Regional Plan: Waste for Otago (The Omnibus Plan Change) Appendices Appendix A: Minster’s direction matter to be called in to the environment court Appendix B: Letter from EPA commissioning the report Appendix C: Minister’s letter in response to the Skelton report Appendix D: Skelton report Appendix E: ORC’s letter in responding to the Minister with work programme Appendix F: Relevant sections of the Regional Plan: Water for Otago Appendix G: Relevant sections of the Regional Plan: Waste for Otago Appendix H: Relevant provisions of the Resource Management Act 1991 Appendix I: National Policy Statement for Freshwater Management 2020 Appendix J: Relevant provisions of the National Environmental Standards for Freshwater 2020 Appendix K: Relevant provisions of the Resource Management (Stock Exclusion) Regulations 2020 Appendix L: Relevant provisions of Otago Regional Council Plans and Regional Policy Statements Appendix M: Relevant provisions of Iwi management plans APPENDIX A Ministerial direction to refer the Otago Regional Council’s proposed Omnibus Plan Change to its Regional Plans to the Environment Court Having had regard to all the relevant factors, I consider that the matters requested to be called in by Otago Regional Council (ORC), being the proposed Omnibus Plan Change (comprised of Water Plan Change 8 – Discharge Management, and Waste Plan Change 1 – Dust Suppressants and Landfills) to its relevant regional plans are part of a proposal of national significance. Under section 142(2) of the Resource Management Act 1991 (RMA), I direct those matters to be referred to the Environment Court for decision. -
Mountain Biking View Trip Dates North West Passage Book Now
Mountain Biking View Trip Dates North West Passage Book Now Trip Grade: Blue 6 North West Passage All Inclusive We’ve created a wild mountain bike adventure that will take you through some of the wildest and most remote terrain in the UK. Falling between our Hebridean Trail and Coast to Coast trips in terms of its physical and technical challenge, the North West Passage will take you on an intricate route from the Atlantic Ocean to the North Sea and then back to the Atlantic. Starting out in Fort William on the West Coast we ease into our ride following the imposing geological fault line that is the Great Glen. From here the trail becomes more remote as we journey north to the stunning Glen Affric - widely considered as Scotland’s most beautiful glen. We spend a day exploring here before pushing further into the Northern Highlands. Big mountains, wild rivers and lonely glens dominate the landscapes, punctuated by trails which are perfect for mountain biking. Reaching the North Sea coast, our final day offers the unique opportunity to traverse an entire country in one day. Starting from the East Coast our route eventually leads us to the sheltered and dramatic Atlantic shores of Ullapool on Scotland’s mountainous West Coast. Highlights • Journey through some of the wildest and most remote terrain in the UK • Explore Glen Affric - widely considered as Scotland’s most beautiful glen • Traverse an entire country in one day, from the North Sea to the Atlantic Book with confidence • We guarantee this trip will run as soon as 2 people have booked • Maximum of 8 places available per departure PLEASE NOTE – The itinerary may be subject to change at the discretion of the Wilderness Scotland Guide with regard to weather conditions and other factors. -
I-SITE Visitor Information Centres
www.isite.nz FIND YOUR NEW THING AT i-SITE Get help from i-SITE local experts. Live chat, free phone or in-person at over 60 locations. Redwoods Treewalk, Rotorua tairawhitigisborne.co.nz NORTHLAND THE COROMANDEL / LAKE TAUPŌ/ 42 Palmerston North i-SITE WEST COAST CENTRAL OTAGO/ BAY OF PLENTY RUAPEHU The Square, PALMERSTON NORTH SOUTHERN LAKES northlandnz.com (06) 350 1922 For the latest westcoastnz.com Cape Reinga/ information, including lakewanaka.co.nz thecoromandel.com lovetaupo.com Tararua i-SITE Te Rerenga Wairua Far North i-SITE (Kaitaia) 43 live chat visit 56 Westport i-SITE queenstownnz.co.nz 1 bayofplentynz.com visitruapehu.com 45 Vogel Street, WOODVILLE Te Ahu, Cnr Matthews Ave & Coal Town Museum, fiordland.org.nz rotoruanz.com (06) 376 0217 123 Palmerston Street South Street, KAITAIA isite.nz centralotagonz.com 31 Taupō i-SITE WESTPORT | (03) 789 6658 Maungataniwha (09) 408 9450 Whitianga i-SITE Foxton i-SITE Kaitaia Forest Bay of Islands 44 Herekino Omahuta 16 Raetea Forest Kerikeri or free phone 30 Tongariro Street, TAUPŌ Forest Forest Puketi Forest Opua Waikino 66 Albert Street, WHITIANGA Cnr Main & Wharf Streets, Forest Forest Warawara Poor Knights Islands (07) 376 0027 Forest Kaikohe Russell Hokianga i-SITE Forest Marine Reserve 0800 474 830 DOC Paparoa National 2 Kaiikanui Twin Coast FOXTON | (06) 366 0999 Forest (07) 866 5555 Cycle Trail Mataraua 57 Forest Waipoua Park Visitor Centre DOC Tititea/Mt Aspiring 29 State Highway 12, OPONONI, Forest Marlborough WHANGAREI 69 Taumarunui i-SITE Forest Pukenui Forest -
Community Emergency Response Guide Mosgiel-Taieri
Community Emergency Response Guide Mosgiel-Taieri 1 contents... Introduction 3 During a Landslide 20 After a Landslip 21 Mosgiel Map 4 Key Hazards 5 Pandemic 22 Flooding 5 Before a Pandemic 22 Fire / Wildfire 5 During a Pandemic 22 Earthquake 6 After a Pandemic 22 Major Storms / Snowstorms 6 Coping in Emergencies 23 Land Instability 7 What Would You Do? 24 Pandemic 7 Stuck at Home? 24 Can’t Get Home? 24 Floods 8 Before a Flood 8 Have to Evacuate? 25 During a Flood 8 No Power? 25 After a Flood 9 No Water? 26 Flood Maps 10 No Phone or Internet? 26 Caring for Pets and Livestock 27 Fire 12 Before a Fire 12 Emergency Planning 28 During a Fire 12 Step 1: Household Emergency Plan 28 After a Fire 13 Step 2: Emergency Kit 28 Step 3: Stay Connected 28 Earthquake 14 Before an Earthquake 14 Household Emergency Plan 29 During an Earthquake 14 Emergency Kit 32 After an Earthquake 15 Stay Connected 33 Local Dunedin Faults 16 Key Civil Defence Sites 34 Storms / Snowstorms 18 Before a Storm 18 Roles and Responsibilities 36 During a Storm 18 Community Response Group 37 After a Storm 19 Notes 38 Land Instability 20 Contact Information 39 Before a Landslide 20 2 introduction...Intro- Mosgiel and the Taieri Plain The Taieri Plain lies to the west of Dunedin and has a mix of rural and urban environs with Mosgiel being an important service town for the area’s rural community. There are several settlements across the Plain including the following: Henley is at the southern extremity of the City of Dunedin, 35 kilometres from the city centre, close to Lake Waihola, and at the confluence of the Taieri and Waipori Rivers. -
A Geomorphic Classification System
A Geomorphic Classification System U.S.D.A. Forest Service Geomorphology Working Group Haskins, Donald M.1, Correll, Cynthia S.2, Foster, Richard A.3, Chatoian, John M.4, Fincher, James M.5, Strenger, Steven 6, Keys, James E. Jr.7, Maxwell, James R.8 and King, Thomas 9 February 1998 Version 1.4 1 Forest Geologist, Shasta-Trinity National Forests, Pacific Southwest Region, Redding, CA; 2 Soil Scientist, Range Staff, Washington Office, Prineville, OR; 3 Area Soil Scientist, Chatham Area, Tongass National Forest, Alaska Region, Sitka, AK; 4 Regional Geologist, Pacific Southwest Region, San Francisco, CA; 5 Integrated Resource Inventory Program Manager, Alaska Region, Juneau, AK; 6 Supervisory Soil Scientist, Southwest Region, Albuquerque, NM; 7 Interagency Liaison for Washington Office ECOMAP Group, Southern Region, Atlanta, GA; 8 Water Program Leader, Rocky Mountain Region, Golden, CO; and 9 Geology Program Manager, Washington Office, Washington, DC. A Geomorphic Classification System 1 Table of Contents Abstract .......................................................................................................................................... 5 I. INTRODUCTION................................................................................................................. 6 History of Classification Efforts in the Forest Service ............................................................... 6 History of Development .............................................................................................................. 7 Goals -
Geography and Health Research Report Series Report Number: 2
The Taieri Catchment and Community Health Survey Margot Parkes 2003 Geography and Health Research Report Series Report Number: 2 Disclaimer: While every effort has been made to ensure that the information in this publication is accurate, the Department of Geography, University of Otago and Public Health South do not accept any responsibility or liability for error of fact, omission, interpretation or opinion which may be present, nor for the consequences of any decision based on this information. Published by: Department of Geography, University of Otago & Public Health South. Dunedin 2003 Background: This report presents and discusses the findings from the Taieri Catchment & Community Health Survey conducted in June 2000. The catchment survey was part of a larger research project known as ‘The Taieri Catchment and Community Health Project’ (TC&CH Project), a collaborative research project initiated by Dr. Margot Parkes and colleagues at the University of Otago. The survey was developed in consultation with community reference groups who participated in the TC&CH Project. A more detailed account of the design, findings and implications of this survey, and the TC&CH Project are presented in the author’s doctoral thesis: Parkes M. (2003). Linking Ecosystems and Social Systems for Health and Sustainability: Public Health Lessons from the Taieri River Catchment. A thesis submitted for the Degree of Doctor of Philosophy at the University of Otago, Dunedin, New Zealand. For more information regarding the survey or the TC&CH Project, please contact: Dr Margot Parkes Division of Ecology and Health, John A Burns School of Medicine University of Hawaii at Manoa, Honolulu, HI 96822, Hawaii, USA. -
Otago Region Waters of the Maniototo
Waters of the Maniototo Otago Region Waters of the Maniototo ON THE MANIOTOTO there are several irrigation dams that have been built to collect water during the winter period for release over the summer. These dams never run dry and have turned into good fisheries. Most of these waters are on private land but permission has been granted by the landowners to fish. Therefore it is up to us, as anglers, to respect the wishes of the landowners as sometimes they have areas closed for lambing, stock or paddock work. Please take your rubbish away with you and on no account dig for worms on their property. Also leave your dog at home or chain it to your vehicle. WEST EWEBURN DAM: This water is set in the hills behind the Naseby forest and has its own stock of brown trout which don't grow to a very large size. All methods are used and the season runs from 1 October to 30 April, with a bag limit of six fish. Access: Off State Highway 85 on the Wedderburn- Naseby plantation road, then turn left into Reservoir road that takes you to the dam wall. COALPIT DAM: Built during the mining era to store water for gold recovery, it is situated in the Naseby forest and has been consistently stocked by Fish and Game over the years. It often gets an influx of trout from draining the water race in April. It is home to both rainbow and brown trout, and do not be surprised to catch a brook char as they are picked up by the Mt Ida race. -
SFU Library Thesis Template
Bedrock Structural Influences on River Morphology by Michael J. Curran BA, Colorado College, 2013 Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geography Faculty of Environment © Michael Curran 2020 SIMON FRASER UNIVERSITY Spring 2020 Copyright in this work rests with the author. Please ensure that any reproduction or re-use is done in accordance with the relevant national copyright legislation. Approval Name: Michael Curran Degree: Master of Science Title: Bedrock Structural Influences on River Morphology Examining Committee: Chair: Rosemary Collard Assistant Professor Jeremy G. Venditti Senior Supervisor Professor John J. Clague Supervisor Professor Emeritus Doug Stead Supervisor Professor Allison Pfeiffer External Examiner Assistant Professor Department of Geology Western Washington University Date Defended/Approved: April 16, 2020 ii Abstract Bedrock rivers largely set the pace for landscape evolution in unglaciated terrain and yet little is known about what controls their morphologies. I examine the role that geologic structure plays in the alignment and morphology of bedrock canyons at different scales. At the watershed scale, I examine the striking alignment of the Fraser River with the Fraser River Fault zone and its largely unmapped secondary fault structures. I explore how large sediment inputs affect bedrock canyons alignment and their morphological characteristics. At the reach scale, I investigate how geological structure influences bedrock canyon width. I find that width constrictions coincide with dominant sub- horizontal joint sets whereas widenings coincide with dominant sub-vertical joint sets. I consider this in the context of sequential constrictions and widenings and propose a conceptual model where sub-vertical jointing makes canyon walls more susceptible to failure due to river undercutting than horizontal jointing.