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Olympic Invasives Working Group 2018 Annual Report
Olympic Invasives Working Group 2018 Annual Report Bohemian knotweed on Fisher Cove Rd, Clallam County, leading to Lake Sutherland, treated for the first time as part of the Clallam County Road Department Integrated Weed Management Plan. Report Prepared by Clallam County Noxious Weed Control Board A patch of knotweed found growing on Ennis Creek in Port Angeles. Report prepared by Jim Knape Cathy Lucero Clallam County Noxious Weed Control Board January 2019 223 East 4th Street Ste 15 Port Angeles WA 98362 360-417-2442 [email protected] http://www.clallam.net/weed/projects.html This report can also be found at http://www.clallam.net/weed/annualreports.html CONTENTS EXECUTIVE SUMMARY................................................................................................. 1 PROJECT DESCRIPTION .............................................................................................. 7 2018 PROJECT ACTIVITIES .......................................................................................... 7 2018 PROJECT PROTOCOLS ..................................................................................... 11 OBSERVATIONS AND CONCLUSIONS ...................................................................... 14 RECOMMENDATIONS ................................................................................................. 15 PROJECT ACTIVITIES BY WATERSHED ................................................................... 18 CLALLAM COUNTY ...........................................................................................................18 -
Coastal Rivers - Special Rules
Puget Sound and Coastal Rivers - Special Rules With various fish populations across the state being listed under the Endangered SpeciesAct, WDFW must provide as much protection as possible for all life stages of these populations, in particular for rearing juveniles. For many years, the standard stream rule opened rivers, streams, and beaver ponds to fishing for Game Fish from the first Saturday in June – October 31, with an 8" minimum size, 2 fish/day limit. Consequently, much of the juvenile rearing habitat for resident trout and Dolly Varden and anadromous salmon, steelhead, cutthroat, and Bull Trout was open for fishing. As a result, these juvenile salmonids were at risk of being incidentally caught and may have not survived being handled and released, especially if bait was used. In 2010 we adopted a new management strategy that offered additional protection to stocks in streams draining into Puget Sound and the Strait of Juan de Fuca. In 2012 this strategy was extended to the Coast. The basic rule in these waters is that all rivers, streams, and beaver ponds are CLOSED to fishing unless they are listed in the following tables within the Puget Sound, Strait, and Coastal River sections of the pamphlet (see pages 23-51). These tables detail ALL of the fishing opportunity in these drainages. Areas open to fisheries are presented by river system unless the waters drain directly to salt water. All other waters in these drainages are closed to fishing. Beaver ponds located within or connected to streams listed as open toTROUT and Other Game Fish follow the same rules as the stream unless otherwise listed. -
Abstracts from the 3Rd Symposium on the Hydrogeology of Washington State
Abstracts from the 3rd Symposium on the Hydrogeology of Washington State October 16 – 18, 2000 Landmark Convention Center Tacoma, Washington Presented By: The Washington State Department of Ecology The Washington Hydrologic Society The United States Geological Survey Table of Contents Acknowledgments ......................................................................... ii Abstracts for Oral Presentations, by Session Gravel Mining ........................................................................1 Contaminant Fate and Transport ..........................................5 Water Availability.................................................................11 Aquifer Test Design.............................................................18 Watershed Management.....................................................22 Contaminated Ground Water and Sediments .....................28 Flooding and Geologic Hazards..........................................33 Databases ...........................................................................40 Aquifer Protection................................................................44 Remediation Technologies..................................................47 Ground Water Contaminant Topics.....................................51 Ground Water-Surface Water Interaction............................55 Riparian Ecology .................................................................62 Geophysical Investigations..................................................69 Abstracts for Poster Presentations, -
Valley Formation by Fluvial and Glacial Erosion
Valley formation by ¯uvial and glacial erosion David R. Montgomery Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195, USA ABSTRACT Cross-valley pro®les from the west slope of the Olympic Peninsula, Washington, are used to investigate the relative effects of ¯uvial and glacial erosion on valley formation. Unlike most ranges where glaciers and rivers sequentially occupied the same valleys, neighboring valleys in the Olympic Mountains developed in similar lithologies but were subject to different degrees of glaciation, allowing comparison of the net effect of glacial and ¯uvial processes integrated over many glacial cycles. Upslope drainage area was used to normalize comparisons of valley width, ridge-crest-to-valley-bottom relief, and valley cross-sectional area as measures of net differences in the mass of rock excavated from below ridgelines for 131 valley-spanning transects. Valley width, relief, and cross-sectional areas are similar for glaciated, partly glaciated, and unglaciated (¯uvial) valleys with drainage areas of ,10 km2, but diverge downslope. Glaciated valleys draining .50 km2 reach two to four times the cross-sectional area and have to 500 m greater relief than comparable ¯uvial valleys; partly glaciated valleys have intermediate dimensions. At dis- tances of .5 km from valley heads, the cumulative upstream volume of rock removed to form valleys is two to four times greater in glacially incised valleys than in ¯uvial valleys. The ®nding of strong differences in the net result of valley excavation by ¯uvial and glacial erosion supports the interpretation that alpine glaciers are more effective erosional agents than are rivers and implies that large alpine valleys deepened and enlarged in response to Pleistocene glaciation. -
Appendix B.Pdf
Draft Environmental Impact Statement Thorndyke Resource | June 25, 2014 Jefferson County Department of Community Development Appendix B Official Letters and Applicable Regulations T-ROC Substantially Complete Letter B-1 T-ROC 408 Scoping Letter B-2 Jefferson County Ordinance 08-0706-04 B-3 Jefferson County 1989 Shoreline Master Program B-4 Jefferson County Comprehensive Plan and Unified Development Code Explanations B-5 B-1 T-ROC Substantially Complete Letter B-2 T-ROC 408 Scoping Letter B-3 Jefferson County Ordinance 08-0706-04 CC'. D~ S '1-04Q- STATE OF WASHINGTON County of Jefferson AN ORDINANCE AMENDING } 08-040706- THE COUNTY'S COMPREHENSIVE } PLAN TO ACHIEVE COMPLIANCE } WITH THE FINAL DECISION AND } ORDER OF THE WESTERN } WASHINGTON GROWTH } MANAGEMENT HEARINGS BOARD } REGARDING MLA 02-# 235,THE FHM } APPLICATION FOR A MINERAL } RESOURCES LAND OVERLAY } WHEREAS, the Board of Jefferson CommissionersOrdinance #(" as County the Board")has, required by the Growth Management Act,as codified at RCW 36.OI070A.et seq., annually creates and implements a process by which citizens and entities can propose amendments to the County's Comprehensive Plan (or CP")," the CP having been originally adopted via Resolution No. 72-98 on August 28, 1998 and as subsequently amended and; WHEREAS, a modified version of the proposed amendment known as MLA 02-# 235 [Fred Hill Materials-Mineral Resource Overlay Designation or "MRLO"]was approved to the extent of 690 acres (the "Approved Alternative")by the Board during December 2002; and WHEREAS, the Board's approval of the CP amendment known as MLA 02-# 235 through Ordinance #14-021213- also(known as "Ordinance 14")was timely appealed to the Western Washington Growth Management Hearings Board (or WWGMHB"),said WWGMHB remanding the MLA back to the County for further environmental review. -
Tectonic Geomorphology and the Record of Quaternary Plate Boundary Deformation in the Olympic Mountains
Geological Society of America Field Guide 4 2003 Tectonic geomorphology and the record of Quaternary plate boundary deformation in the Olympic Mountains Frank J. Pazzaglia Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015, USA Glenn D. Thackray Department of Geosciences, Idaho State University, Pocatello, Idaho 83209, USA Mark T. Brandon Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520-8109, USA Karl W. Wegmann Washington Department of Natural Resources, Division of Geology & Earth Resources, Olympia, Washington 98504-7007, USA John Gosse Department of Earth Sciences, Room 3006, Life Sciences Centre, Dalhousie University, Halifax, Nova Scotia B3H 4J1, Canada Eric McDonald Desert Research Institute, Division of Earth and Ecosystem Sciences, 2215 Raggio Parkway, Reno, Nevada 89512, USA Antonio F. Garcia Department of Physics, California Polytechnic State University, San Luis Obispo, California 93407, USA Don Prothero Department of Geology, Occidental College, 1600 Campus Road, Los Angeles, California 90041-3314, USA ABSTRACT We use Quaternary stratigraphy to reconstruct landscape evolution and measure tectonic deformation of the Olympic Mountains section of the Pacifi c Northwest Coast Range. An important motivation for understanding orogenesis here, and throughout the Coast Range, is the concern about the relationship of active deformation to seismic hazards associated with the Cascadia subduction zone. There is also much interest in apportioning the nature of the deformation, whether cyclic or permanent, whether it involves mainly shortening parallel or normal to the margin, and how the deformation on the pro- versus retrowedge sides of the orogen compare. Pre-Holocene stratigraphy and structure provide the only records of suffi cient duration to separate long-term permanent deformation from earthquake-cycle elastic deformation. -
Washington Division of Geology and Earth Resources Open File Report
FOREST SLOPE STABILITY PILOT PROJECT UPPER DESCHUTES RIVER, WASHINGTON for Department of Ecology ' by Gerald W. Thorsen Kurt L. Othberg Open File Report 79-16 Department of Natural Resources Division of Geology and Earth Resources Olympia, WA 98504 1978 SLOPE STABILITY PILOT PROJECT for Department of Ecology by Gerald W. Thorsen Kurt L. Othberg Department of Natural Resources Division of Geology and Earth Resources Olympia, WA 98504 1978 CONTENTS Introduction l Upper Deschutes Basin Study 1 Physical setting l Geologic setting 2 Geomorphic terrains 4 Deschutes headwaters terrain 4 Weathered bedrock terrain 5 Glaciated terrain 7 Landforms 8 Moraines - Terraces 8 Landslides 9 Selected References 11-12 Proposed methodology for Forest Slope Stability Studies 12 Advisory group 12 Field teams 13 Representative basins 13 Background studies 13 Co mp i 1at i on · 13 Reconnaissance 14 Field studies 14 Report - maps 14 Educational phase 14 Appendix Brief analyses of three other basins in Western Washington Sul tan Bas in, ilorth Cascades Grays River Basin, Southwest Washington Upper Clearwater River Basin, Southwest Olympics Applicability of the DNR-SCS soil surveys to slope stability mapping, with specific reference to. the upper Deschutes Introduction Background on DNR-SCS soils mapping Extractable data Summary and conclusions An.notated bibliography on forest slope stability I LL UST RA TIO NS Upper Deschutes River Basin maps in pocket Road system in pocket Bedrock outcrop in pocket Geomorphic terrain map in pocket Landform map in pocket ! I ntroduc ti on One of the areas of interest to the Washington State Department of Ecology in regard to its water quality responsibilities is "non-point pollution" in the form of stream turbidity. -
Pazzaglia2002 a Fluvial Record of Plate-Boundary
Pazzaglia, F. J., Brandon, M. T., and Wegmann, K., 2002, A fluvial record of plate-boundary deformation in the Olympics Mountains, in Moore, G., ed., Field Guide to Geologic Processes in Cascadia: Oregon Department of Geology and Mineral Industries, Special Paper 36, p. 223-256 A fluvial record of plate-boundary deformation in the Olympics Mountains Frank J. Pazzaglia Department of Earth and Environmental Sciences Lehigh University Bethlehem, PA 18015 Mark T. Brandon Department of Geology and Geophysics Yale University New Haven, CT 06520-8109 Karl W. Wegmann Washington Dept. of Natural Resource Division of Geology & Earth Resources Olympia, WA 98504-7007 Trip Overview We have constructed a 2-day field trip designed to exhibit the geology, geomorphology, and active tectonics of the Pacific coast of the Olympic Peninsula. The trip is organized around the following three major topics that should generate lively discourse on how to use and interpret basic field relationships in tectonic geomorphology research: (1) What is a river terrace, how is it made, and what do river terraces tell us about active tectonics? (2) What is driving orogenesis for the Olympic Mountain segment of the Cascadia Subduction Zone? Is it shortening parallel to the direction of plate convergence, shortening normal to the direction of plate convergence, or some combination of both? Are there any geomorphic or stratigraphic field relationships that can actually be used to track the horizontal movement of rocks and thus interpret the shortening history over geologic time scales? (3) We know that uplift along Cascadia includes the effects of cyclic earthquake-related deformation, and long-term steady deformation. -
Clearwater River Wild Steelhead Spawning Timing
CL EARWATER R IVER WILD STE ELHEAD SPAWNING TIMING C. J . Cederholm Washington State Department of Natural Res our ces Rural Route 1, Box 1375 Fo rks, Washington 98331 ABSTRACT: Steelhead spawning timing in the mainstem and tributar ies of the Clearwater River was monitored from 1973 t o 1980. Gen erally, spawning begins in Janua ry and lasts until late June with mos t tributaries peaking i n Mar ch and April, and the main river peaking in e arly Ma y . Th e spawning timing in the t r ibutaries is more protracte d whe n compared to the main rive r which is sharply peaking . Spawning genera lly occurs in the spring, well after the ma jor annual freshets of No vember through February . It is sug gested that this spring spawning timing is an adaptation to avoid egg l oss caused by streamb ed scour, and to e l i minate competition with salmon spawners. Commencement of spawning co inc ides with springtime dec lining streamflows and increasing water tempe ratures . Spawning escapements in the Clearwater Ri ver have increased stead ily over the study peri od, due mainly to r educ tions in the Quinault Tribal commercial gil l ne t fi shery catch at Quee ts , and possibly due to an ove rall improvement in l ogg ing road construc tion and maintenance pract i ces in the watershed . Th e l argely ind i genous na tive steelhead spawning populations of the Clearwater Ri ver ma y also be influenced by straying adults r e t urning from extens i ve hatchery smol t plants in the Qu eets and c losely adjoining rivers. -
Jefferson County Shoreline Master Program Update Project Ecology Grant # G0600343
JEFFERSON COUNTY SHORELINE MASTER PROGRAM UPDATE PROJECT ECOLOGY GRANT # G0600343 Final Shoreline Inventory and Characterization Report – Revised November 2008 Prepared for: Jefferson County Department of Community Development Prepared by: ESA Adolfson in association with Coastal Geologic Services, Inc. Shannon & Wilson, Inc Jefferson County Final Shoreline Inventory and Characterization Report – Revised November 2008 1 ACKNOWLEDGEMENTS 2 This document was prepared with guidance from a Shoreline Technical Advisory Committee 3 (STAC) and Shoreline Policy Advisory Committee (SPAC). The County gratefully 4 acknowledges the committee members for contributing to this effort. STAC Members: SPAC Members: Hans Daubenberger Al Bergstein (alt. Cyrilla Cook) Hugh Shipman, Al Latham Jeffree Stewart Aleta Erickson (alt. Randy Johnson) Jill Silver Bill Mahler (alt. Bill Brock) Jim Brennan Bill Miller John Cambalik Connie Muggli Marty Ereth David Roberts (alt. Hugo Flores) Michael Adams (alt. Anne Murphy) Dick Broders Peter Bahls (Jude Rubin) Eveleen Muehlethaler (alt. Frank Espy/Alice Peter Best McConaughy) Randi Thurston (alt. Jeff Davis) Hans Daubenberger (alt. Steve Todd) Richard Brocksmith (alt. Scott Brewer) Jeffree Stewart Stephen Stanley (alt. Susan Grigsby) Jerry Gorsline Steve Allison John Cambalik Steve Todd Johnathon Ciesla Yvonne Dettlaff Judy Surber Karen Best (alt. Kevin Tuuri) Keith Dublanica Larry Crockett (alt Eric Toewes) Margie Shirato (alt. Randi Thurston/Jeff Davis) Marty Ereth Mike McHenry Peter Downey Ross Goodwin Sarah Krueger (alt. Reed Waite) Scott Brewer (alt Richard Brocksmith) Steve Allison (alt. Bob Howell/Tim Snowden) 5 The County also gratefully acknowledges the following for their contributions to this effort: 6 • Battelle’s Marine Sciences Laboratory - Heida Diefenderfer and her colleagues for 7 providing detailed information on the ecology of the nearshore environment as part of 8 their effort to rank and prioritize nearshore restoration opportunities. -
Olympic Invasives Working Group 2019 Annual Report
Olympic Invasives Working Group 2019 Annual Report Bohemian knotweed on the sand spit at the mouth of the Hoko River. Report Prepared by Clallam County Noxious Weed Control Board A patch of knotweed contiguous to a previous treatment site (dead stalks visible in the foreground) that CCNWCB staff was finally able to treat in 2019 with new permission. Report prepared by Shea McDonald Cathy Lucero Clallam County Noxious Weed Control Board January 2020 223 East 4th Street Ste 15 Port Angeles WA 98362 360-417-2442 [email protected] http://www.clallam.net/weed/projects.html This report can also be found at http://www.clallam.net/weed/annualreports.html CONTENTS EXECUTIVE SUMMARY ............................................................................................................ 1 PROJECT DESCRIPTION .......................................................................................................... 7 2019 PROJECT ACTIVITIES ...................................................................................................... 7 2019 PROJECT PROTOCOLS ................................................................................................. 11 OBSERVATIONS AND CONCLUSIONS .................................................................................. 14 2020 PROJECT PRIORITIES INCLUDE ................................................................................... 15 RECOMENDATIONS ................................................................................................................ 16 PROJECT ACTIVITIES -
2001 Queets Coho Stock Review
Exhibit D.6.b STT Report November 2001 QUEETS COHO Stock Assessment Salmon Technical Team Pacific Fishery Management Council 7700 NE Ambassador Place, Suite 200 Portland, OR 97220-1384 (503) 326-6352 F:\!master\cm\stt\rpt\D6d_STTrpt_Queets.doc STK.SAL.A14.QTSCO TABLE OF CONTENTS TABLE OF CONTENTS................................................................................................................. i EXECUTIVE SUMMARY ............................................................................................................ ii INTRODUCTION .......................................................................................................................... 1 STOCK DESCRIPTION ................................................................................................................ 1 Location & Geography ............................................................................................................... 1 Coho Production Components ................................................................................................ 3 Natural Coho Production ........................................................................................................ 3 Supplemental Production........................................................................................................ 3 Hatchery Production ............................................................................................................... 4 Management Objectives.............................................................................................................