City of Forks 2018-2038 Comprehensive Plan
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Gold and Fish Pamphlet: Rules for Mineral Prospecting and Placer Mining
WASHINGTON DEPARTMENT OF FISH AND WILDLIFE Gold and Fish Rules for Mineral Prospecting and Placer Mining May 2021 WDFW | 2020 GOLD and FISH - 2nd Edition Table of Contents Mineral Prospecting and Placer Mining Rules 1 Agencies with an Interest in Mineral Prospecting 1 Definitions of Terms 8 Mineral Prospecting in Freshwater Without Timing Restrictions 12 Mineral Prospecting in Freshwaters With Timing Restrictions 14 Mineral Prospecting on Ocean Beaches 16 Authorized Work Times 17 Penalties 42 List of Figures Figure 1. High-banker 9 Figure 2. Mini high-banker 9 Figure 3. Mini rocker box (top view and bottom view) 9 Figure 4. Pan 10 Figure 5. Power sluice/suction dredge combination 10 Figure 6. Cross section of a typical redd 10 Fig u re 7. Rocker box (top view and bottom view) 10 Figure 8. Sluice 11 Figure 9. Spiral wheel 11 Figure 10. Suction dredge . 11 Figure 11. Cross section of a typical body of water, showing areas where excavation is not permitted under rules for mineral prospecting without timing restrictions Dashed lines indicate areas where excavation is not permitted 12 Figure 12. Permitted and prohibited excavation sites in a typical body of water under rules for mineral prospecting without timing restrictions Dashed lines indicate areas where excavation is not permitted 12 Figure 13. Limits on excavating, collecting, and removing aggregate on stream banks 14 Figure 14. Excavating, collecting, and removing aggregate within the wetted perimeter is not permitted 1 4 Figure 15. Cross section of a typical body of water showing unstable slopes, stable areas, and permissible or prohibited excavation sites under rules for mineral prospecting with timing restrictions Dashed lines indicates areas where excavation is not permitted 15 Figure 16. -
Case Studies of Three Salmon and Steelhead Stocks in Oregon and Washington, Including Population Status, Threats, and Monitoring Recommendations
HOW HEALTHY ARE HEALTHY STOCKS? Case Studies of Three Salmon and Steelhead Stocks in Oregon and Washington, including Population Status, Threats, and Monitoring Recommendations Prepared for the Native Fish Society April 2001 How Healthy Are Healthy Stocks? Case Studies of Three Salmon and Steelhead Stocks in Oregon and Washington, including Population Status, Threats, and Monitoring Recommendations Prepared for: Bill Bakke, Director Native Fish Society P.O. Box 19570 Portland, Oregon 97280 Prepared by: Peter Bahls, Senior Fish Biologist David Evans and Associates, Inc. 2828 S.W. Corbett Avenue Portland, Oregon 97201 Sponsored by the Native Fish Society and the U.S. Environmental Protection Agency. April 2001 Please cite this document as follows: Bahls, P. 2001. How healthy are healthy stocks? Case studies of three salmon and steelhead stocks in Oregon and Washington, including population status, threats, and monitoring recommendations. David Evans and Associates, Inc. Report. Portland, Oregon, USA. EXECUTIVE SUMMARY Three salmon stocks were chosen for case studies in Oregon and Washington that were previously identified as “healthy” in a coast-wide assessment of stock status (Huntington et al. 1996): fall chinook salmon (Oncorhynchus tshawytscha) of the Wilson River, summer steelhead (O. mykiss) of the Middle Fork John Day (MFJD) River, and winter steelhead (O. mykiss) of the Sol Duc River. The purpose of the study was to examine with a finer focus the status of these three stocks and the array of human influences that affect them. The best available information was used, some of which has become available since the 1996 assessment of healthy stocks was conducted. Recommendations for monitoring were developed to address priority data gaps and most pressing threats to the species. -
The Bogachiel River System
The Bogachiel River System Within the Bogachiel River system, a number of stream reaches qualify as shorelines of statewide significance. The mainstem BOGACHIEL (RM 0 – 17.6) contains no reach breaks under the current SMP. The portion of the Bogachiel that flows through the Forks Urban Growth Area (FUGA) extends from approximately RM 8.9 to 10.1. Tributary reaches include the following: BEAR‐BOGACHIEL (RM 0‐4.2); DRY‐BOGACHIEL (RM 0‐.5); MAXFIELD 10 (RM 0‐2.7); MAXFIELD 20 (RM 2.7‐4.4); MILL (RM 0 – 1.3); MURPHY 10 (RM 0‐ 1.7); MURPHY 20 (RM 1.7‐ 2.1); and DRY‐BOGACHIEL (RM 0‐ .5). The portion of MILL CR that is within the FUGA extends from RM .8‐ 1.3. The creek flows outside of FUGA and then returns into FUGA boundaries (RM .1) upstream of its confluence with the Bogachiel. The portion of Mill Creek that is outside of FUGA extends from RM 0.1 ‐ .8. Physical Environment The headwaters of the Bogachiel River lie outside the current planning area in the steep terrain of the Olympic National Park. As it enters the planning unit, it flows in a northwesterly direction with several miles in close proximity to US 101. West of the Forks UGA, its largest tributary, the Calawah River, flows into the Bogachiel. Downstream of the confluence, the River widens and meanders in a westward direction through a broad alluvial valley. Beds of Pleistocene clay, sand, and gravel WRIA 20 Draft ICR June 30, 2011 10 | Page overlie the older rocks throughout most of this region. -
Catch Record Cards & Codes
Catch Record Cards Catch Record Card Codes The Catch Record Card is an important management tool for estimating the recreational catch of PUGET SOUND REGION sturgeon, steelhead, salmon, halibut, and Puget Sound Dungeness crab. A catch record card must be REMINDER! 824 Baker River 724 Dakota Creek (Whatcom Co.) 770 McAllister Creek (Thurston Co.) 814 Salt Creek (Clallam Co.) 874 Stillaguamish River, South Fork in your possession to fish for these species. Washington Administrative Code (WAC 220-56-175, WAC 825 Baker Lake 726 Deep Creek (Clallam Co.) 778 Minter Creek (Pierce/Kitsap Co.) 816 Samish River 832 Suiattle River 220-69-236) requires all kept sturgeon, steelhead, salmon, halibut, and Puget Sound Dungeness Return your Catch Record Cards 784 Berry Creek 728 Deschutes River 782 Morse Creek (Clallam Co.) 828 Sauk River 854 Sultan River crab to be recorded on your Catch Record Card, and requires all anglers to return their fish Catch by the date printed on the card 812 Big Quilcene River 732 Dewatto River 786 Nisqually River 818 Sekiu River 878 Tahuya River Record Card by April 30, or for Dungeness crab by the date indicated on the card, even if nothing “With or Without Catch” 748 Big Soos Creek 734 Dosewallips River 794 Nooksack River (below North Fork) 830 Skagit River 856 Tokul Creek is caught or you did not fish. Please use the instruction sheet issued with your card. Please return 708 Burley Creek (Kitsap Co.) 736 Duckabush River 790 Nooksack River, North Fork 834 Skokomish River (Mason Co.) 858 Tolt River Catch Record Cards to: WDFW CRC Unit, PO Box 43142, Olympia WA 98504-3142. -
North Pacific Coast (WRIA 20) Salmon Restoration Strategy (2021 Edition)
North Pacific Coast (WRIA 20) Salmon Restoration Strategy (2021 Edition) North Pacific Coast Lead Entity University of Washington, Olympic Natural Resources Center 1455 South Forks Avenue, P.O. Box 1628, Forks, WA 98331 Approved by the North Pacific Coast Lead Entity Public Review Draft - Pending April 2021 final approval 2021 North Pacific Coast (WRIA 20) Salmon Restoration Strategy Table of Contents Page - Table of Contents i - List of Figures ii - List of Tables ii - Acronyms iii - Glossary iv - Executive Summary xi - Acknowledgements xii Section 1: Project Prioritization and Application Processes 1.1 Goals and Objectives. 1 1.1.1 Incorporating Climate Change 2 1.1.2 Education and Outreach 3 1.2 Project Prioritization Method. 4 1.2.1 Descriptions of Prioritization Categories: 7 1.3 Review Process (Project application procedure, explanation of evaluation process). 10 1.4 Annual Project List. 10 1.5 Eligibility for the Annual Project Round 11 Section 2: Priority Projects by Geographic Section 2.0 All WRIA 20 Basins System-wide 12 2.1 Hoh River Basin: 2.1.1 Hoh Watershed Background. 13 2.1.2 Hoh River Watershed Priority Projects. 18 2.2 Quillayute River Complex: 2.2.1 Quillayute Basin Background. 21 2.1.1.1 Climate Change Forecasts 23 2.2.2 Quillayute Basin Prioritized Projects: 24 2.2.2.0 Quillayute Basin-Wide Priority Projects. 24 2.2.2.1 Quillayute Main Stem Priority Projects. 25 2.2.2.2 Dickey River Watershed Priority Projects. 27 2.2.2.3 Bogachiel River Watershed Priority Projects. 28 2.2.2.4 Calawah River Watershed Priority Projects. -
2016 State of Our Watersheds Report Quillayute River Basin Quileute Tribe
2016 State of Our Watersheds Report Quillayute River Basin abitat projects are vital to restoring the Hsalmon fishery. We have successfully partnered on projects in the past but we need many more into the future. - MEL MOON, NATURAL RESOURCES DIRECTOR QUILEUTE TRIBE Quileute Tribe The Quileute Tribe is located in La Push, on the shores of the Pacific Ocean, where tribal members have lived and hunted for thousands of years. Although their reservation is only about 2 square miles, the Tribe’s original territory stretched along the shores of the Pacific from the glaciers of Mount Olympus to the rivers of rain forests. Much has changed since those times, but Quileute elders remember the time when the Seattle people challenged Kwalla, the mighty whale. They also tell the story of how the bayak, or ra- ven, placed the sun in the sky. 178 Quileute Tribe Large Watershed Has Significant Subbasins The Quileute Tribe’s Area of Concern co-managed with the state of Washington, includes the northern portion of WRIA 20, and the Quileute Tribe has a shared Usual from Lake Ozette to the Goodman Creek and Accustomed area with the Makah Tribe Watershed. The largest basin in the area in the Lake Ozette basin. The Lake Ozette is the Quillayute, with four major sub-ba- sockeye is listed as threatened under the sins: the Dickey, Sol Duc, Calawah and Endangered Species Act. Bogachiel rivers. This part of the coastal The area is heavily forested with rela- region is a temperate rainforest with abun- tively infrequent impervious cover caused dant waterfall and an annual rainfall that by development and small population cen- can reach 140 inches. -
WRIA 20 ICR Calawah River System
The Calawah River System The Calawah River is the largest tributary of the Bogachiel River and is formed by the confluence of the north and south forks of the Calawah. The two forks of the Calawah, CALAWAH N 10 and 20 (20 miles long) and CALAWAH S 10 (6 miles relevant to this report) originate in the Olympic Mountains. All but one mile of the South Fork Calawah within the SMP study area flows exclusively through federal and state commercial forest lands; a one mile stretch near the mouth serves as an eastern boundary of the Forks Urban Growth Area (FUGA) (RM 0‐1). The Calawah’s North Fork is 20 miles long and flows through a mix of private and public commercial forest lands before it empties into the mainstem at the FUGA boundary. Two relatively short tributaries— ALBION (.9 miles) and PISTOL (2.2 miles), flow into the north fork. The Calawah’s south fork is fed by more numerous and significant tributaries including HYAS (3.8 miles) Creek and the SITKUM system which in turn includes the mainstem river (12.7 miles), SITKUM N (2.3 miles) and RAINBOW (RM 0‐.6). LOST (2.3 miles), also a tributary of the South Fork, flows in and out of the Olympic National Park. The segment from RM 1.5 to 2.3 is included in the study area. The mainstem reaches‐‐ CALAWAH 10 (RM 4.9‐ 6.9), CALAWAH 20 (RM 6.9 to 10) and CALAWAH 30 (RM 10 to 10.9), and a segment of its tributary, Elk Creek‐‐ pass alongside or through the (FUGA). -
The Bogachiel System
The Bogachiel System Within the Bogachiel system, a number of stream reaches qualify as shorelines of statewide significance. The mainstem, BOGACHIEL (RM 0 – 17.6) contains no reach breaks under the current SMP. The portion of the Boagchiel that flows through the Forks Urban Growth Area (FUGA) extends from approximately RM 8.9 to 10.1. Tributary reaches include the following: BEAR-BOGACHIEL (RM 0-4.2); DRY-BOGACHIEL (RM 0-.5); MAXFIELD 10 (RM 0-2.7); MAXFIELD 20 (RM 2.7-4.4); MILL (RM 0 – 1.3); MURPHY 10 (RM 0- 1.7); MURPHY 20 (RM 1.7- 2.1); and DRY-BOGACHIEL (RM 0- .5). The portion of MILL CR that is within the FUGA extends from RM .8- 1.3. The creek flows outside of FUGA and then returns into FUGA boundaries (RM .1) upstream of its confluence with the Bogachiel. The portion of Mill Creek that is outside of FUGA extends from RM 0.1 - .8. Physical Environment The headwaters of the Bogachiel River lie outside the current planning area in the steep terrain of the Olympic National Park. As it enters the planning unit, it flows in a northwesterly direction with several miles in close proximity to US 101. As the river turns to the northwest, it passes through Bogachiel State Park. West of the Forks UGA, its largest tributary, the Calawah River, flows into the Bogachiel. Downstream of the confluence, the River widens and meanders in a westward direction through a broad alluvial valley. Beds of Pleistocene clay, sand, and gravel overlie the older rocks throughout most of this region. -
Clallam County SMP WRIA 20 Restoration Plan
Draft WRIA 20 Restoration Plan Prepared by Miranda Wecker and Rebekah Gentry UW Olympic Natural Resources Center May 30, 2011 Table of Contents Watershed Overview Watershed Overview ................................................................................................................................................ 1 Recommended Restoration Actions by River System The Bogachiel River System Bogachiel Reference Map ......................................................................................................................................... 2 General Restoration Needs and Recommendations ................................................................................................. 2 Known Restoration Needs and Projects ................................................................................................................... 3 Protection ................................................................................................................................................................. 4 The Calawah River System Calawah Reference Map ........................................................................................................................................... 5 General Restoration Needs and Recommendations ................................................................................................ 5 Restoration Recommendations ............................................................................................................................... 5 Known Restoration Needs and -
Quinault, Queets, Hoh, and Quillayute River Basins
95 124°30’ 124° 123°30’ STRAIT OF JUAN DE FUCA British Columbia 48° 15' CANADA Ozette Lake . k F t s k e River r W o r, t F e as , North Fork v E r i e k iv R uc h R y d alawa ke le C ic So D 12043000 South Fork Forks er Quillayute Bogachiel Riv River r CLALLAM ve Mount Ri Olympus JEFFERSON So. oh Fork H H 12041200 oh River 47° r 45' ive R River r ate rw ts a ee e Qu Cl 12040500 r Quinault Rive Queets Lake GRAYS HARBOR 12039500 Quinault nault Qui PACIFIC OCEAN MASON Taholah GRAYS HARBOR 47° 15' EXPLANATION REAL-TIME SURFACE-WATER STATION WASHINGTON 010515 20 MILES 01015520 25 30 KILOMETERS Figure 12. Location of surface-water stations in the Quinault, Queets, Hoh, and Quillayute River Basins. 96 Dickey River Soleduck River Quillayute RM 6.51 RM River RM 6.5 1.3 RM RM Calawah River 10.2 North Fork 8.2 12043000 Calawah River RM 6.6 South Fork Calawah River Bogachiel River EXPLANATION Real-time surface-water station 12041200 RM RM 15.4 Hoh30.6 River 12041200 Station number RM 17.4 River mile Stream—Arrow shows direction of flow South Fork Hoh River PACIFIC OCEAN 12040500 Clearwater River RM 4.6 QueetsRM River 7.0 12039500 Quinault Quinault River RM 33.4 Lake Figure 13. Schematic diagram showing surface-water stations in the Quinault, Queets, Hoh, and Quillayute River Basins. QUINAULT RIVER BASIN 97 12039500 QUINAULT RIVER AT QUINAULT LAKE, WA ° ° 1⁄ 1⁄ LOCATION.--Lat 47 27'28", long 123 53'17", in SW 4NE 4 sec.25, T.23 N., R.10 W., Grays Harbor County, Hydrologic Unit 17100102, Quinault Indian Reservation, on left bank at outlet of Quinault Lake, 50 ft downstream from Olympic Highway bridge on U.S. -
The Quillayute River
The Quillayute River The Quillayute River is divided into two stream reaches. The downstream reach, QUILLAYUTE 10, flows entirely outside the planning unit from the Olympic National Park boundary to the river mouth within the Quileute Reservation. QUILLAYUTE 20 (RM 2.9‐5.3) is within the study area and extends from the Park Boundary at to the confluence of the Bogachiel and Sol Duc Rivers. Physical Environment The Quillayute River is the terminal mainstem of one of the largest and most productive river system networks on the Washington coast. The Quillayute River drainage encompasses over 800,000 acres and experiences some 120‐140 inches of rainfall per year. All of the contributing rivers have extensive tributary systems. The Quillayute mainstem is a low gradient and low velocity river, lacking in sinuosity and composed of long gravel bars. The flood plain for the mainstem is very wide throughout its length. Critical acquifer recharge areas occur throughout the mainstem channel, with one extensive recharge area located to the south of the channel between RM 3.6‐ 4. The mainstem channel is reported to flow over a landslide hazard area, portions of which extend out onto the north shoreline. Because the grade is gentle in this lowland portion of WRIA 20, tidal influence and measurable salinity can extend over five miles up to the confluence of the Sol Duc WRIA 20 Draft ICR June 30, 2011 55 | Page and Bogachiel Rivers at Three Rivers. This region is often exposed to high wind and heavy rainstorms resulting in peak flow events that cause sedimentation and velocity impacts in the Quillayute mainstem . -
The Quillayute River
The Quillayute River The Quillayute River is divided into two stream reaches. The downstream reach, QUILLAYUTE 10, flows entirely outside the planning unit from the Olympic National Park boundary to the river mouth within the Quileute Reservation. QUILLAYUTE 20 (RM 2.9-5.3) is within the study area and extends from the Park Boundary at to the confluence of the Bogachiel and Sol Duc Rivers. Physical Environment The Quillayute River is the terminal mainstem of one of the largest and most productive river system networks on the Washington coast. Four major rivers--the Bogachiel, Calawah, Sol Duc and Dickey-- combine to form the Quillayute River. The Quillayute River drainage encompasses over 800,000 acres and experiences some 120-140 inches of rainfall per year. All of the contributing rivers have extensive tributary systems. The Quillayute mainstem is a low gradient river, low velocity river, lacking in sinuosity and composed of long gravel bars. The flood plain for the mainstem is very wide throughout its length. Critical acquifer recharge areas occur throughout the mainstem channel, with one extensive recharge area located to the south of the channel between RM 3.6- 4. The mainstem channel is reported to flow over a landslide hazard area, portions of which extend out onto the north shoreline. Because the grade is gentle in this lowland portion of WRIA 20, tidal influence and measurable salinity can extend over five miles up to the confluence of the Sol Duc and Bogachiel Rivers at Three Rivers. This region is often exposed to high wind and heavy rainstorms resulting in peak flow events that cause sedimentation and velocity impacts in the Quillayute mainstem .