The Economic Effects of the Eruptions of Mt. St. Helens
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Role of the Estuary in the Recovery of Columbia River Basin Salmon and Steelhead: an Evaluation of the Effects of Selected Factors on Salmonid Population Viability
NOAA Technical Memorandum NMFS-NWFSC-69 Role of the Estuary in the Recovery of Columbia River Basin Salmon and Steelhead: An Evaluation of the Effects of Selected Factors on Salmonid Population Viability September 2005 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Marine Fisheries Service NOAA Technical Memorandum NMFS Series The Northwest Fisheries Science Center of the National Marine Fisheries Service, NOAA, uses the NOAA Technical Memorandum NMFS series to issue infor- mal scientific and technical publications when com- plete formal review and editorial processing are not appropriate or feasible due to time constraints. Docu- ments published in this series may be referenced in the scientific and technical literature. The NMFS-NWFSC Technical Memorandum series of the Northwest Fisheries Science Center continues the NMFS-F/NWC series established in 1970 by the Northwest & Alaska Fisheries Science Center, which has since been split into the Northwest Fisheries Science Center and the Alaska Fisheries Science Center. The NMFS-AFSC Technical Memorandum series is now being used by the Alaska Fisheries Science Center. Reference throughout this document to trade names does not imply endorsement by the National Marine Fisheries Service, NOAA. This document should be cited as follows: Fresh, K.L., E. Casillas, L.L. Johnson, and D.L. Bottom. 2005. Role of the estuary in the recovery of Columbia River basin salmon and steelhead: an evaluation of the effects of selected factors on salmo- nid population viability. U.S. Dept. Commer., NOAA Tech. Memo. NMFS-NWFSC-69, 105 p. NOAA Technical Memorandum NMFS-NWFSC-69 Role of the Estuary in the Recovery of Columbia River Basin Salmon and Steelhead: An Evaluation of the Effects of Selected Factors on Salmonid Population Viability Kurt L. -
Dacite Block and Ash Avalanche Hazards in Mountainous Terrain: 2360 Yr
DACITE BLOCK AND ASH AVALANCHE HAZARDS IN MOUNTAINOUS TERRAIN: 2360 YR. BP ERUPTION OF MOUNT MEAGER, BRITISH COLUMBIA by MARTIN L. STEWART B.Sc, (Honours), Carleton University, 1998 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in THE FACULTY OF GRADUATE STUDIES DEPARTMENT OF EARTH AND OCEAN SCIENCES We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA December 2002 © Martin L. Stewart, 2002 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of LoM^ r QatA^ Sc/t^n? The University of British Columbia Vancouver, Canada Date IB * zooi DE-6 (2/88) Abstract The Mount Meager volcanic complex hosts deposits from the youngest known explosive volcanic eruption in Canada (2360 yr. BP). These deposits reflect the consequences of erupting dacite magmas into a region of extreme topographic relief. Regions of this kind represent one of the most hazardous and, potentially, high risk natural environments on the planet. Mapping of the Pebble Creek Formation deposits has elucidated a unique distribution of hazardous events of varying intensity, timing, and frequency associated with the 2360 yr. -
Garibaldi Provincial Park 2010 Olympic Venue
1 Garibaldi Provincial Park 2010 Olympic Venue Garibaldi Provincial Park, located in the traditional territory of the Squamish people, forms much of the backdrop to Whistler/ Blackcomb, site of the downhill events of the 2010 Winter Games. Sitting in the heart of the Coast Mountains, the park takes its name from the towering 2,678 metre peak, Mount Garibaldi. Garibaldi Park is known for its pristine beauty and spectacular natural features. Just 70 km north of Vancouver, the park offers over 90 km of established hiking trails, and is a favourite year-round destination for outdoor enthusiasts. Interesting Garibaldi Park Facts • The southern portion of Garibaldi Park is home to the Garibaldi Volcano, part of the Garibaldi Volcanic Belt and made up of Mount Garibaldi, Atwell Peak, and Dalton Dome. This stratavolcano, so named because of its conelike layers of hardened lava, rock and volcanic ash, last erupted 10,000 to 13,000 years ago under glacial ice. It is this event that is responsible for forming some of the fascinating geological features in the park, such as Opal Cone, the Table and Black Tusk. • The “Barrier” is a natural rock formation created by the volcanic explosion of Mount Price thousands of years ago; the lava created a natural dam for the melt streams from nearby glaciers. As a result Garibaldi Lake formed. The lake reaches depths of up to 300 metres in places and is rich in silt (or ‘rock flour’), which gives the lake its characteristic milky blue colour. www.bcparks.ca 2 Garibaldi Provincial Park 2010 Olympic Venue History In 1860, while surveying Howe Sound on board the Royal Navy ship H.M.S. -
Garibaldi Provincial Park M ASTER LAN P
Garibaldi Provincial Park M ASTER LAN P Prepared by South Coast Region North Vancouver, B.C. Canadian Cataloguing in Publication Data Main entry under title: Garibaldi Provincial Park master plan On cover: Master plan for Garibaldi Provincial Park. Includes bibliographical references. ISBN 0-7726-1208-0 1. Garibaldi Provincial Park (B.C.) 2. Parks – British Columbia – Planning. I. British Columbia. Ministry of Parks. South Coast Region. II Title: Master plan for Garibaldi Provincial Park. FC3815.G37G37 1990 33.78”30971131 C90-092256-7 F1089.G3G37 1990 TABLE OF CONTENTS GARIBALDI PROVINCIAL PARK Page 1.0 PLAN HIGHLIGHTS 1 2.0 INTRODUCTION 2 2.1 Plan Purpose 2 2.2 Background Summary 3 3.0 ROLE OF THE PARK 4 3.1 Regional and Provincial Context 4 3.2 Conservation Role 6 3.3 Recreation Role 6 4.0 ZONING 8 5.0 NATURAL AND CULTURAL RESOURCE MANAGEMENT 11 5.1 Introduction 11 5.2 Natural Resources Management: Objectives/Policies/Actions 11 5.2.1 Land Management 11 5.2.2 Vegetation Management 15 5.2.3 Water Management 15 5.2.4 Visual Resource Management 16 5.2.5 Wildlife Management 16 5.2.6 Fish Management 17 5.3 Cultural Resources 17 6.0 VISITOR SERVICES 6.1 Introduction 18 6.2 Visitor Opportunities/Facilities 19 6.2.1 Hiking/Backpacking 19 6.2.2 Angling 20 6.2.3 Mountain Biking 20 6.2.4 Winter Recreation 21 6.2.5 Recreational Services 21 6.2.6 Outdoor Education 22 TABLE OF CONTENTS VISITOR SERVICES (Continued) Page 6.2.7 Other Activities 22 6.3 Management Services 22 6.3.1 Headquarters and Service Yards 22 6.3.2 Site and Facility Design Standards -
Community Risk Assessment
COMMUNITY RISK ASSESSMENT Squamish-Lillooet Regional District Abstract This Community Risk Assessment is a component of the SLRD Comprehensive Emergency Management Plan. A Community Risk Assessment is the foundation for any local authority emergency management program. It informs risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflects their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. SLRD Emergency Program [email protected] Version: 1.0 Published: January, 2021 SLRD Community Risk Assessment SLRD Emergency Management Program Executive Summary This Community Risk Assessment (CRA) is a component of the Squamish-Lillooet Regional District (SLRD) Comprehensive Emergency Management Plan and presents a survey and analysis of known hazards, risks and related community vulnerabilities in the SLRD. The purpose of a CRA is to: • Consider all known hazards that may trigger a risk event and impact communities of the SLRD; • Identify what would trigger a risk event to occur; and • Determine what the potential impact would be if the risk event did occur. The results of the CRA inform risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflect their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. -
U.S. Environmental Protection Agency's National Estuary Program
U.S. Environmental Protection Agency’s National Estuary Program Story Map Text-only File 1) Introduction Welcome to the National Estuary Program story map. Since 1987, the EPA National Estuary Program (NEP) has made a unique and lasting contribution to protecting and restoring our nation's estuaries, delivering environmental and public health benefits to the American people. This story map describes the 28 National Estuary Programs, the issues they face, and how place-based partnerships coordinate local actions. To use this tool, click through the four tabs at the top and scroll around to learn about our National Estuary Programs. Want to learn more about a specific NEP? 1. Click on the "Get to Know the NEPs" tab. 2. Click on the map or scroll through the list to find the NEP you are interested in. 3. Click the link in the NEP description to explore a story map created just for that NEP. Program Overview Our 28 NEPs are located along the Atlantic, Gulf, and Pacific coasts and in Puerto Rico. The NEPs employ a watershed approach, extensive public participation, and collaborative science-based problem- solving to address watershed challenges. To address these challenges, the NEPs develop and implement long-term plans (called Comprehensive Conservation and Management Plans (link opens in new tab)) to coordinate local actions. The NEPs and their partners have protected and restored approximately 2 million acres of habitat. On average, NEPs leverage $19 for every $1 provided by the EPA, demonstrating the value of federal government support for locally-driven efforts. View the NEPmap. What is an estuary? An estuary is a partially-enclosed, coastal water body where freshwater from rivers and streams mixes with salt water from the ocean. -
Do Sturgeon Limit Burrowing Shrimp Populations in Pacific Northwest Estuaries?
Environ Biol Fish (2008) 83:283–296 DOI 10.1007/s10641-008-9333-y Do sturgeon limit burrowing shrimp populations in Pacific Northwest Estuaries? Brett R. Dumbauld & David L. Holden & Olaf P. Langness Received: 22 January 2007 /Accepted: 28 January 2008 /Published online: 4 March 2008 # Springer Science + Business Media B.V. 2008 Abstract Green sturgeon, Acipenser medirostris, and we present evidence from exclusion studies and field white sturgeon, Acipenser transmontanus, are fre- observation that the predator making the pits can have quent inhabitants of coastal estuaries from northern a significant cumulative negative effect on burrowing California, USA to British Columbia, Canada. An shrimp density. These burrowing shrimp present a analysis of stomach contents from 95 green stur- threat to the aquaculture industry in Washington State geon and six white sturgeon commercially landed in due to their ability to de-stabilize the substrate on Willapa Bay, Grays Harbor, and the Columbia River which shellfish are grown. Despite an active burrowing estuary during 2000–2005 revealed that 17–97% had shrimp control program in these estuaries, it seems empty stomachs, but those fish with items in their unlikely that current burrowing shrimp abundance and guts fed predominantly on benthic prey items and availability as food is a limiting factor for threatened fish. Burrowing thalassinid shrimp (mostly Neo- green sturgeon stocks. However, these large predators trypaea californiensis) were important food items for may have performed an important top down control both white and especially for green sturgeon taken in function on shrimp populations in the past when they Willapa Bay, Washington during summer 2003, where were more abundant. -
Implications for Hazard Assessment at Mount Meager, BC
Discrimination of hot versus cold avalanche deposits: Implications for hazard assessment at Mount Meager, B.C. M. L. Stewart, J. K. Russell, C. J. Hickson To cite this version: M. L. Stewart, J. K. Russell, C. J. Hickson. Discrimination of hot versus cold avalanche deposits: Implications for hazard assessment at Mount Meager, B.C.. Natural Hazards and Earth System Sciences, Copernicus Publ. / European Geosciences Union, 2003, 3 (6), pp.713-724. hal-00299093 HAL Id: hal-00299093 https://hal.archives-ouvertes.fr/hal-00299093 Submitted on 1 Jan 2003 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Natural Hazards and Earth System Sciences (2003) 3: 713–724 © European Geosciences Union 2003 Natural Hazards and Earth System Sciences Discrimination of hot versus cold avalanche deposits: Implications for hazard assessment at Mount Meager, B.C. M. L. Stewart1, J. K. Russell1, and C. J. Hickson2 1Igneous Petrology Laboratory, Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, British Columbia, Canada 2Pacific Division, Geological Survey of Canada, Vancouver B.C., Canada Received: 5 February 2003 – Revised: 26 May 2003 – Accepted: 29 May 2003 Abstract. The surficial deposits surrounding the Mount represent an obvious hazard and, in many instances, the na- Meager volcanic complex include numerous avalanche de- ture or magnitude of these volcanic hazards can be substan- posits. -
Canadian Volcanoes, Based on Recent Seismic Activity; There Are Over 200 Geological Young Volcanic Centres
Volcanoes of Canada 1 V4 C.J. Hickson and M. Ulmi, Jan. 3, 2006 • Global Volcanism and Plate tectonics Where do volcanoes occur? Driving forces • Volcano chemistry and eruption types • Volcanic Hazards Pyroclastic flows and surges Lava flows Ash fall (tephra) Lahars/Debris Flows Debris Avalanches Volcanic Gases • Anatomy of an Eruption – Mt. St. Helens • Volcanoes of Canada Stikine volcanic belt Presentation Outline Anahim volcanic belt Wells Gray – Clearwater volcanic field 2 Garibaldi volcanic belt • USA volcanoes – Cascade Magmatic Arc V4 Volcanoes in Our Backyard Global Volcanism and Plate tectonics In Canada, British Columbia and Yukon are the host to a vast wealth of volcanic 3 landforms. V4 How many active volcanoes are there on Earth? • Erupting now about 20 • Each year 50-70 • Each decade about 160 • Historical eruptions about 550 Global Volcanism and Plate tectonics • Holocene eruptions (last 10,000 years) about 1500 Although none of Canada’s volcanoes are erupting now, they have been active as recently as a couple of 4 hundred years ago. V4 The Earth’s Beginning Global Volcanism and Plate tectonics 5 V4 The Earth’s Beginning These global forces have created, mountain Global Volcanism and Plate tectonics ranges, continents and oceans. 6 V4 continental crust ic ocean crust mantle Where do volcanoes occur? Global Volcanism and Plate tectonics 7 V4 Driving Forces: Moving Plates Global Volcanism and Plate tectonics 8 V4 Driving Forces: Subduction Global Volcanism and Plate tectonics 9 V4 Driving Forces: Hot Spots Global Volcanism and Plate tectonics 10 V4 Driving Forces: Rifting Global Volcanism and Plate tectonics Ocean plates moving apart create new crust. -
Volume II, Chapter 2 Columbia River Estuary and Lower Mainstem Subbasins
Volume II, Chapter 2 Columbia River Estuary and Lower Mainstem Subbasins TABLE OF CONTENTS 2.0 COLUMBIA RIVER ESTUARY AND LOWER MAINSTEM ................................ 2-1 2.1 Subbasin Description.................................................................................................. 2-5 2.1.1 Purpose................................................................................................................. 2-5 2.1.2 History ................................................................................................................. 2-5 2.1.3 Physical Setting.................................................................................................... 2-7 2.1.4 Fish and Wildlife Resources ................................................................................ 2-8 2.1.5 Habitat Classification......................................................................................... 2-20 2.1.6 Estuary and Lower Mainstem Zones ................................................................. 2-27 2.1.7 Major Land Uses................................................................................................ 2-29 2.1.8 Areas of Biological Significance ....................................................................... 2-29 2.2 Focal Species............................................................................................................. 2-31 2.2.1 Selection Process............................................................................................... 2-31 2.2.2 Ocean-type Salmonids -
Garibaldi Park Alpine Jewel of Howe Sound
Garibaldi Park Alpine jewel of Howe Sound Bob Turner Bowen Island Conservancy [email protected] Retired, Geological Survey of Canada “We can create beauty through the dailyness of our lives, standing our ground in the places we love” Terry Tempest Williams Mt Garibaldi from Pam Rocks Bowen Island Trail just below Black Tusk Bioregionalism: Taking root in my home watershed Garibaldi Bowen Island Nch’kay - Sacred Mountain to the Squamish People Sacred Mountain Royal Navy survey ship H.M.S. Plumper, surveying the BCCaptain coast Vancouver’sin 1860 men, 1792 Giuseppe Garibaldi First ascent of Mt Garibaldi, 1907 First ascent of Mt Garibaldi, 1907 Early Mountaineering Garibaldi Lake area was a popular hiking area by 1910 Black Tusk Meadows PGE in Cheakamus Canyon … and BC’s 2nd Provincial Park by 1920 2006 Diamond Head2006 Chalet, 1945 Elfin Lakes, 1950s Ottar Brandvold Garibaldi today The famous western edge of Park Cheakamus Lake Access Rubble Creek Access Garibaldi Lake Mt Garibaldi Elfin Lakes Diamond Head Access Black Tusk, May 1986 A geologist’s view: Garibaldi’s FIRE and ICE story Deception Peak from Polemonium Ridge “FIRE”: We live in volcano country! Volcanoes Garibaldi the inevitable consequence of collision (subduction) zones The volcano factory Figure credit: Geological Survey of Canada Mount Garibaldi Garibaldi – just the top end of a 60-100 km deep plumbing system Figure credit: “Black Tusk” Black Tusk Helm Cr lava flow Cinder Cone Garibaldi Lake Mt Price volcano Mt Price, The Table Barrier lava flow Mt Garibaldi Opal Cone Elfin Lakes Opal Cone volcano Black Tusk volcano Diamond Head parking lot Ring Creek lava flow Not just 1 volcano, but 13! … and 4 lava flows Could Garibaldi erupt? Vital signs Last eruption 9000 years ago No hot springsGaribaldi’s or fumeroles vital signs Some seismicity; unclear significance …. -
Demographics of Piscivorous Colonial Waterbirds and Management Implications for ESA-Listed Salmonids on the Columbia Plateau
Jessica Y. Adkins, Donald E. Lyons, Peter J. Loschl, Department of Fisheries and Wildlife, 104 Nash Hall, Oregon State University, Corvallis, Oregon 97331 Daniel D. Roby, U.S. Geological Survey-Oregon Cooperative Fish and Wildlife Research Unit1, Department of Fisheries and Wildlife, 104 Nash Hall, Oregon State University, Corvallis, Oregon 97331 Ken Collis2, Allen F. Evans, Nathan J. Hostetter, Real Time Research, Inc., 52 S.W. Roosevelt Avenue, Bend, Oregon 97702 Demographics of Piscivorous Colonial Waterbirds and Management Implications for ESA-listed Salmonids on the Columbia Plateau Abstract We investigated colony size, productivity, and limiting factors for five piscivorous waterbird species nesting at 18 loca- tions on the Columbia Plateau (Washington) during 2004–2010 with emphasis on species with a history of salmonid (Oncorhynchus spp.) depredation. Numbers of nesting Caspian terns (Hydroprogne caspia) and double-crested cormorants (Phalacrocorax auritus) were stable at about 700–1,000 breeding pairs at five colonies and about 1,200–1,500 breed- ing pairs at four colonies, respectively. Numbers of American white pelicans (Pelecanus erythrorhynchos) increased at Badger Island, the sole breeding colony for the species on the Columbia Plateau, from about 900 individuals in 2007 to over 2,000 individuals in 2010. Overall numbers of breeding California gulls (Larus californicus) and ring-billed gulls (L. delawarensis) declined during the study, mostly because of the abandonment of a large colony in the mid-Columbia River. Three gull colonies below the confluence of the Snake and Columbia rivers increased substantially, however. Factors that may limit colony size and productivity for piscivorous waterbirds nesting on the Columbia Plateau included availability of suitable nesting habitat, interspecific competition for nest sites, predation, gull kleptoparasitism, food availability, and human disturbance.