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Chapter 4: Destinations – Utilitarian And
Jefferson County Non-Motorized Transportation and Recreational Trails Plan 2010 Chapter 4: Destinations – Utilitarian and Recreational 2010 Plan Update: Chapter 4 Destinations provides a broad picture of Jefferson County: where people live, work, go to school, shop, and recreate and the locations of tourist facilities and significant public facilities. This information is intended to inform decisions about connecting these destinations with non-motorized transportation facilities. It is not intended as an up-to-date guide. While Chapter 4 has not been updated, it still performs its intended function. This chapter has been retained in the original 2002 Plan format. County, City, Port, School District, State, Federal, and private enterprises have developed an extensive number of commercial, employment, business, educational, recreational, and other public facilities within the County. This extensive array of facilities is of interest to non-motorized transportation and recreational trail users. This chapter describes the most significant destinations. 4.1 Schools The Brinnon, Chimacum, Port Townsend, Queets-Clearwater, Quilcene, Quillayute Valley, and Sequim School Districts provide educational services to Jefferson County residents. Brinnon School District The school district collects students by bus within the district’s service area – which includes all of Brinnon and the areas along US-101 from the Mason County line to Mt Walker and transports them to the central school site. Upper grade students are bused to Quilcene High School. The district operates 6 school bus routes beginning at 6:35-9:00 am and ending at 3:46-4:23 pm for the collection and distribution of different school grades and after school programs. -
South Puget Sound Community College Year Three Mid-Cycle Evaluation
South Puget Sound Community College Year Three Mid-Cycle Evaluation Dr. Timothy Stokes President September, 2014 Table of Contents Report on Year One Recommendation ......................................................................................................... 1 Mission .......................................................................................................................................................... 1 Part I .............................................................................................................................................................. 1 Mission Fulfillment .................................................................................................................................... 1 Operational Planning ................................................................................................................................ 2 Core Themes, Objectives and Indicators .................................................................................................. 3 Part II ............................................................................................................................................................. 4 Rationale for Indicators of Achievement .................................................................................................. 5 Increase Student Retention (Objective 1.A) ......................................................................................... 5 Support Student Completion (Objective 1.B) ...................................................................................... -
Jefferson County Hazard Identification and Vulnerability Assessment 2011 2
Jefferson County Department of Emergency Management 81 Elkins Road, Port Hadlock, Washington 98339 - Phone: (360) 385-9368 Email: [email protected] TABLE OF CONTENTS PURPOSE 3 EXECUTIVE SUMMARY 4 I. INTRODUCTION 6 II. GEOGRAPHIC CHARACTERISTICS 6 III. DEMOGRAPHIC ASPECTS 7 IV. SIGNIFICANT HISTORICAL DISASTER EVENTS 9 V. NATURAL HAZARDS 12 • AVALANCHE 13 • DROUGHT 14 • EARTHQUAKES 17 • FLOOD 24 • LANDSLIDE 32 • SEVERE LOCAL STORM 34 • TSUNAMI / SEICHE 38 • VOLCANO 42 • WILDLAND / FOREST / INTERFACE FIRES 45 VI. TECHNOLOGICAL (HUMAN MADE) HAZARDS 48 • CIVIL DISTURBANCE 49 • DAM FAILURE 51 • ENERGY EMERGENCY 53 • FOOD AND WATER CONTAMINATION 56 • HAZARDOUS MATERIALS 58 • MARINE OIL SPILL – MAJOR POLLUTION EVENT 60 • SHELTER / REFUGE SITE 62 • TERRORISM 64 • URBAN FIRE 67 RESOURCES / REFERENCES 69 Jefferson County Hazard Identification and Vulnerability Assessment 2011 2 PURPOSE This Hazard Identification and Vulnerability Assessment (HIVA) document describes known natural and technological (human-made) hazards that could potentially impact the lives, economy, environment, and property of residents of Jefferson County. It provides a foundation for further planning to ensure that County leadership, agencies, and citizens are aware and prepared to meet the effects of disasters and emergencies. Incident management cannot be event driven. Through increased awareness and preventive measures, the ultimate goal is to help ensure a unified approach that will lesson vulnerability to hazards over time. The HIVA is not a detailed study, but a general overview of known hazards that can affect Jefferson County. Jefferson County Hazard Identification and Vulnerability Assessment 2011 3 EXECUTIVE SUMMARY An integrated emergency management approach involves hazard identification, risk assessment, and vulnerability analysis. This document, the Hazard Identification and Vulnerability Assessment (HIVA) describes the hazard identification and assessment of both natural hazards and technological, or human caused hazards, which exist for the people of Jefferson County. -
Tacoma‐Pierce County Board of Health
Tacoma‐Pierce County Board of Health Regular Meeting Agenda 3629 South D Street, Tacoma, WA 98418 January 20, 2021 Board of Health Clerk, (253) 798‐2899 3 ‐ 5 p.m. Board Members Remote Attendance Only Keith Blocker Dial in: 253 215 8782 Marty Campbell Meeting ID: 992 6138 9468 Bruce Dammeier William Hirota, MD Passcode: 575390 Patricia Johnson Dave Morell Catherine Ushka I. CALL TO ORDER Derek Young II. ROLL CALL III. ELECTION OF BOARD OF HEALTH (BOH) OFFICERS Motion for 2021 BOH Chair Motion for 2021 BOH Vice Chair IV. COMMENTS BY THE PUBLIC The Board will consider written and oral public comments. Submit written comments any time prior to when a Board of Health meeting adjourns at [email protected]. Written comments we receive prior to noon on the date of a Board of Health meeting will go to Board members before the meeting. For the duration of the declared public health emergency, make oral comments when you join the meeting by phone with the number, meeting ID, and passcode at the top of the agenda. Press *9 to raise your hand and signal you wish to make a comment. You will be announced by your name or the last four digits of your phone number. Comments unrelated to specific agenda items have a two‐minute limit per person. The Chair has the authority to change the time limits as deemed necessary. All written and oral comments will become part of the meeting record. V. COVID‐19: Update [Anthony L‐T Chen, Director of Health] [Nigel Turner, Incident Commander] [Kayla Scrivner, Public Health Nurse] VI. -
Geologic Map of the Coupeville and Part of the Port Townsend North 7.5
WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-58 Geologic Map of the Coupeville and Part of the Port Townsend North R1W R1E 42¢30² 122°45¢ 40¢ 122°37¢30² 48°15¢ 48°15¢ Qgtv Qco Qb Qgoge Qco Qgdp 7.5-minute Quadrangles, Island County, Washington Qml 1 Qco schematic section Qgog Qgd 5 e Qcw from top to Qgav; Qgav Qgdme elev. 197 ft schematic section elev. 160 ft measured section Qgdp Qml Qgav Qgoge elev. 150 ft Qs <10 ft sand by Michael Polenz, Stephen L. Slaughter, and Gerald W. Thorsen ~10 ft below Qgav Qd active dune sand Qp Qs 110,124,182 6 to 12 ft 5 ft Qs sand Qgdm 18 ft sand and gravel Qgdm Qco silt and clay e Qgav 7 ft Qgdm diamict e Qb liquefaction features e Qgdme Qml Qc 15 ft silt 9 ft Qgd diamict Qcw o and small shears in Qd Qgoge Qgd 9 ft Qgt till 188 p 10 ft silt and clay silt and sand at ~100 ft June 2005 v Qgtv <75 ft Qgoge 11 ft Qgav sandy gravel Qcw Qp Qmw 177,178 gravel with ~30 ft mixed deposits—sand, Qmw silt boulders silt, and minor gravel Qgd Qp Qgomee? Qm Qgdmels? ~20 ft lahar runout (Table 2, samples 188 and 182*) GEOLOGIC SETTING AND DEVELOPMENT We suggest that this sediment source is partly documented by a high-energy outwash Deposits of the Fraser Glaciation (Pleistocene) alluvial facies reflect ancestral Skagit River provenance. Sparse, local Glacier REFERENCES CITED channel deposits— Qgomee Qcw Qgd 79 ft p clean sand with Qls Qb Qcw ~15 ft channel deposits—sand and minor gravel gravel unit (unit Qgoge), which locally grades up into Partridge Gravel, and which we Peak dacite and pumice pebbles, such as those found to the east of Long Point very sparse gravel Like most of the Puget Lowland, the map area is dominated by glacial sediment and lacks Armstrong, J. -
Development of a Hydrodynamic Model of Puget Sound and Northwest Straits
PNNL-17161 Prepared for the U.S. Department of Energy under Contract DE-AC05-76RL01830 Development of a Hydrodynamic Model of Puget Sound and Northwest Straits Z Yang TP Khangaonkar December 2007 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor Battelle Memorial Institute, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof, or Battelle Memorial Institute. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. PACIFIC NORTHWEST NATIONAL LABORATORY operated by BATTELLE for the UNITED STATES DEPARTMENT OF ENERGY under Contract DE-AC05-76RL01830 Printed in the United States of America Available to DOE and DOE contractors from the Office of Scientific and Technical Information, P.O. Box 62, Oak Ridge, TN 37831-0062; ph: (865) 576-8401 fax: (865) 576-5728 email: [email protected] Available to the public from the National Technical Information Service, U.S. Department of Commerce, 5285 Port Royal Rd., Springfield, VA 22161 ph: (800) 553-6847 fax: (703) 605-6900 email: [email protected] online ordering: http://www.ntis.gov/ordering.htm This document was printed on recycled paper. -
Chapter 3: Existing Facilities 2010 Plan Update: the Multi-Purpose Trail Inventory in the 2002 Plan Shows the Length of the Larry Scott Trail As 4.0 Miles
Jefferson County Non-Motorized Transportation and Recreational Trails Plan 2010 Chapter 3: Existing Facilities 2010 Plan Update: The multi-purpose trail inventory in the 2002 Plan shows the length of the Larry Scott Trail as 4.0 miles. This included both trail segments constructed to the County’s adopted standards and the existing “usage” trail on the railroad grade. Since the adoption of the 2002 Plan, Jefferson County has constructed additional trail segments. The constructed trail length is now 4.4 miles. Volunteers have developed additional segments that extend the trail to S. Discovery Road at the Discovery Bay Golf Course. These segments, while useable, are not constructed to the County’s standards and are not included in the current inventory. The remaining trail right-of-way has been acquired to the Milo Curry Road / S. Discovery Road intersection near Four Corners. Construction of the remaining trail segments is planned for substantial completion in 2011. The trail length will then be 7.6 miles. The remainder of this chapter was not revised for the 2010 Plan update. It has been retained in the original 2002 Plan format. Jefferson County, Port Townsend, Port Ludlow, Port of Port Townsend, Washington State, National Forest and Park Services, and other public and private agencies have assembled a significant inventory of non-motorized transportation and recreational trail systems within Jefferson County. These systems provide a variety of on and off-road opportunities for walking, hiking, bicycling, horse, and hand launch boat activities throughout the county. The 1998 County Comprehensive Plan provides a very limited description of the non-motorized transportation and recreational trail facilities in Jefferson County. -
Ground-Water Flooding in Glacial Terrain of Southern Puget Sound
science fora changing world Ground-Water Flooding in Glacial Terrain of Southern Puget Sound, Washington glacial lakes, and diverting drainage landforms and, in some places, eroded southward to the Chehalis River and then away sediments deposited during the west to the Pacific Ocean to create exten glacial advance. Coarse sediment, known sive outwash plains6' 7' 10. At its maximum as the Steiiacoom Gravel, was also extent, the glacier stretched from the deposited on the upland by water flowing Cascade Range to the Olympic Mountains through the intersecting channels and and extended south as far as Tenino, braided streams that further conveyed the Wash., in Thurston County, occupying all water away from the proglacial lake.2- 13 of the lowland area and lower mountain This gravel deposit is consistently coarse valleys. The glacier reached altitudes up over the central Pierce County upland to 4,000 feet along the mountain front10; area. Stones in the Steiiacoom Gravel are 6,000 feet near the present day United predominantly 1 inch in size and most do States-Canada border; 3,000 feet near not exceed 3 inches. 13 The thickness of Seattle; 2,200 feet near Tacoma; and less the gravel is generally 20 feet or less with than 1.000 feet near Olympia. 1' 4- 10 a maximum that rarely exceeds 60 feet. The resulting landscape is characterized T^\ ue to a global warming trend, the by many shallow, elongated depressions Figure 1. Proglacial Lake Puyattup and J ^Vashon Glacier began retreating and ice-contact depressions (kettles). The successive Lake Spillways (modified from its terminus about 17.000 years ago.7 larger and deeper depressions are occu from Thorson, 1979). -
Kitsap County Coordinated Water System Plan
Kitsap County Coordinated Water System Plan Regional Supplement 2005 Revision Kitsap County May 9, 2005 Coordinated Water System Plan Regional Supplement 2005 Revision Acknowledgements An undertaking of this magnitude is not possible without the efforts of numerous individuals and groups. This plan is a project of extensive input and a compilation of the recommendations of numerous special studies and related planning efforts. Those of us at the Kitsap County Water Utility Coordinating Committee (WUCC) and Economic and Engineering Services, Inc. (EES) would like to pay particular tribute to those agencies and individuals listed below: Morgan Johnson, Chair Water Utility Coordinating Committee Members of the Kitsap County Water Utility Coordinating Committee Kitsap Public Utility District Staff, Bill Hahn coordinating Kathleen Cahall, Water Resources Manager City of Bremerton Mike Means, Drinking Water Program Manager Kitsap County Health District Washington State Department of Health Staff z Denise Lahmann z Jim Rioux z Jared Davis z Karen Klocke Washington State Department of Ecology Staff Acknowledgements ii Kitsap County May 9, 2005 Coordinated Water System Plan Regional Supplement 2005 Revision Table of Contents Section Title Page Letter of Transmittal ........................................................................................................ Engineer's Certificate..................................................................................................... i Acknowledgements...................................................................................................... -
Kitsap County Watershed Location Map Washington State Seems to Have an Abundance of Water
KITSAP COUNTY INITIAL BASIN ASSESSMENT October 1997 With the multitudes of lakes, streams, and rivers, Kitsap County Watershed Location Map Washington State seems to have an abundance of water. The demand for water resources, however, has steadily increased each year, while the water supply has stayed the same, or in some cases, appears to have declined. This increased demand for limited water resources has made approving new water uses complex and controversial. To expedite decisions about pending water rights, it is vital to accurately assess the quality and quantity of our surface and ground water. The Washington State Department of Ecology (Ecology) recognizes that water right decisions must be based on accurate scientific information. Ecology is working with consultants and local governments to conduct special studies called Initial What do we know about the Kitsap County Watershed or Basin Assessments throughout the Basin? State. The assessments describe existing water rights, streamflows, precipitation, geology, hydrology, Kitsap County encompasses almost 400 square miles and water quality, fisheries resources, and land use occupies a peninsula and several islands in Puget Sound. patterns. It is bounded on the east and north by Puget Sound and The assessments evaluate existing data on water which Admiralty Inlet, and on the west by Hood Canal. The will assist Ecology to make decisions about pending County is adjoined by Pierce and Mason Counties on the water right applications. The assessments do not affect south, Jefferson County -
Chapter 13 -- Puget Sound, Washington
514 Puget Sound, Washington Volume 7 WK50/2011 123° 122°30' 18428 SKAGIT BAY STRAIT OF JUAN DE FUCA S A R A T O 18423 G A D A M DUNGENESS BAY I P 18464 R A A L S T S Y A G Port Townsend I E N L E T 18443 SEQUIM BAY 18473 DISCOVERY BAY 48° 48° 18471 D Everett N U O S 18444 N O I S S E S S O P 18458 18446 Y 18477 A 18447 B B L O A B K A Seattle W E D W A S H I N ELLIOTT BAY G 18445 T O L Bremerton Port Orchard N A N 18450 A 18452 C 47° 47° 30' 18449 30' D O O E A H S 18476 T P 18474 A S S A G E T E L N 18453 I E S C COMMENCEMENT BAY A A C R R I N L E Shelton T Tacoma 18457 Puyallup BUDD INLET Olympia 47° 18456 47° General Index of Chart Coverage in Chapter 13 (see catalog for complete coverage) 123° 122°30' WK50/2011 Chapter 13 Puget Sound, Washington 515 Puget Sound, Washington (1) This chapter describes Puget Sound and its nu- (6) Other services offered by the Marine Exchange in- merous inlets, bays, and passages, and the waters of clude a daily newsletter about future marine traffic in Hood Canal, Lake Union, and Lake Washington. Also the Puget Sound area, communication services, and a discussed are the ports of Seattle, Tacoma, Everett, and variety of coordinative and statistical information. -
South Puget Sound Prairies the Nature Conservancy of Washington 2007 Conservation Vision
Conservation Action Planning Report for the SOUTH PUGET SOUND PRAIRIES The Nature Conservancy of Washington 2007 CONSERVATION VISION Successful conservation of the South Puget Sound Prairies will entail elements of protection, active land management and restoration, and integration of the full suite of partners working within the Willamette Valley - Puget Trough - Georgia Basin Ecoregion. The portfolio of protected conservation sites will contain a mosaic of habitats that support the full-range of prairie and oak woodland species. This portfolio will be a total of 20 protected sites, including at least six core areas. The core areas of the portfolio consist of protected sites embedded within a mosaic of land-use that complements prairie conservation and the protected conservation sites. The portfolio will take advantage of the wide-range of microclimates in the South Puget Sound, aimed at providing resiliency to the potential effects of climate change. The South Puget Sound will contribute to the conservation of rare species by promoting and implementing recovery actions throughout their historic range. Active management of the prairie maximizes the contribution to conservation of all portfolio sites. These management actions are coordinated and integrated across a range of partners and landowners. This integration ensures that information transfer is exemplary, that organizations are linked formally and informally and that sufficient resources are generated for all partners. The South Puget Sound Prairies will be a primary source for prairie-specific science and restoration techniques. It will similarly be a source concerning the science and conservation for fragmented natural systems. Prairie conservation in the South Puget Sound will be supported by a community that is actively engaged through a vigorous volunteer program and supports the financial and policy issues that affect prairies.