Backyard Beauty in Snohomish County, Washington
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USGS Geologic Investigations Series I-1963, Pamphlet
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-1963 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE SKYKOMISH RIVER 30- BY 60 MINUTE QUADRANGLE, WASHINGTON By R.W. Tabor, V.A. Frizzell, Jr., D.B. Booth, R.B. Waitt, J.T. Whetten, and R.E. Zartman INTRODUCTION From the eastern-most edges of suburban Seattle, the Skykomish River quadrangle stretches east across the low rolling hills and broad river valleys of the Puget Lowland, across the forested foothills of the North Cascades, and across high meadowlands to the bare rock peaks of the Cascade crest. The quadrangle straddles parts of two major river systems, the Skykomish and the Snoqualmie Rivers, which drain westward from the mountains to the lowlands (figs. 1 and 2). In the late 19th Century mineral deposits were discovered in the Monte Cristo, Silver Creek and the Index mining districts within the Skykomish River quadrangle. Soon after came the geologists: Spurr (1901) studied base- and precious- metal deposits in the Monte Cristo district and Weaver (1912a) and Smith (1915, 1916, 1917) in the Index district. General geologic mapping was begun by Oles (1956), Galster (1956), and Yeats (1958a) who mapped many of the essential features recognized today. Areas in which additional studies have been undertaken are shown on figure 3. Our work in the Skykomish River quadrangle, the northwest quadrant of the Wenatchee 1° by 2° quadrangle, began in 1975 and is part of a larger mapping project covering the Wenatchee quadrangle (fig. 1). Tabor, Frizzell, Whetten, and Booth have primary responsibility for bedrock mapping and compilation. -
Wednesday, March 25, 2009
8 TFW -16B-90-0 11 EVALUATION OF TIlE TFW STREAM CLASSIFICATION SYSTEM: STRATIFICATION OF PHYSICAL HABITAT AREA AND DISTRIBUTION By T. J. Beechie and T. H. Sibley TIMB~:R &WILDLIFE July 1990 EVALUATION OF THE TFW STREAM CLASSIFICATION SYSTEM: STRATIFICATION OF PHYSICAL HABITAT AREA AND DISTRIBUTION. FINAL REPORT 1988,1990 Prepared by T. J. Beechie and T. H. Sibley Center for Streamside Studies (AR-lO) and Fisheries Research Institute (WH-10) University of Washington Seattle, W A. 98195 Submitted to: TimberIFishlWildlife Ambient Monitoring Steering Committee and State of Washington. Department of Natural Resources (EL-03) Olympia, W A. 98504 July, 1990 TABLE OF CONTENTS List of Tables IV List of Figures v Executive Summary vm 1. Introduction 1 1.1 Stream Classification Review 1 1.2 Proposed Classification System 4 1.3 Objectives 5 2. Approach 7 2.1 Problems in Variable Definition 7 2.2 The Problem of Spatial Scale 11 2.3 The Problem of Time 11 2.4 Addressing Sources of Variability 12 2.5 Recent Evaluations and Their Implications 15 2.6 Variables Used in this Study 15 3. Methods 19 3.1 Data Collected 19 3.2 Code Definitions 20 3.3 Field Procedures 21 3.4 Visual Estimation Procedure 22 3.5 Statistical Analyses 23 3.6 Study Area 23 4. Results and Discussion 33 4.1 Reference Sites 33 Summary of site characteristics 33 Variation channel unit areas with changes in discharge 36 Relative importance of several physical factors in predicting the percentage of summer pools 40 Discharge-area relationships 42 Large organic debris as obstructions 42 ii Page 4.2 South Fork Stillaguamish River Basin Sites 44 Percentages of summer pool surface area in paired segments 46 Comparison of spawning gravel percentages 48 Distributions of channel unit types 50 Cluster Analysis 50 Discriminant analysis 53 4.3 Multiple Watershed Sites 55 Spawning gravel distribution 55 Discriminant analysis 58 Percentages of pools 58 Physical factors affecting pool area 61 5. -
2015 Removal Action Appendices
APPENDICES Appendix A. Health and Safety Plan Appendix B. Updated HELP Model Simulations Appendix C. MCMA Repository Run-on Control Drain Appendix D. Technical Specifications and Construction Quality Assurance Plan Appendix E. Biological Monitoring Plan Appendix F. Cultural Resources Monitoring and Treatment Plan Appendix G. MCMA 2015 Removal Action Proposed Schedule Appendix H Modified XRF Protocol for Field Screening Appendix A. Health and Safety Plan Health and Safety Plan 2015 Removal Action Monte Cristo Mining Area Mt. Baker-Snoqualmie National Forest Snohomish County, Washington April 2015 Cascade Earth Sciences 3511 Pacific Blvd SW Albany, OR 97321 Ph. (541) 926-7737 Fax (541) 967-7619 www.cascade-earth.com Health and Safety Plan 2015 Removal Action Monte Cristo Mining Area Mt. Baker-Snoqualmie National Forest Snohomish County, Washington EMERGENCY PHONE NUMBERS Medical Emergency/Ambulance .......................................................................................... 911 Police.......................................................................................................................................... 911 Fire .............................................................................................................................................. 911 National Poison Control Center ...................................................................... (800) 222-1222 CES Corporate Safety Officer (Ellen Crawford) ............................................ (541) 812-6620 US Forest Service, Snoqualmie National -
WDFW Wildlife Program Bi-Weekly Report August 1-15, 2020
Wildlife Program – Bi-weekly Report August 1 to August 15, 2020 DIVERSITY DIVISION HERE’S WHAT WE’VE BEEN UP: 1) Managing Wildlife Populations Fishers: Fisher reintroduction project partners from Washington Department of Fish and Wildlife, the National Park Service, Conservation Northwest, Calgary Zoo, and United States Forest Service recently initiated a genetic analysis of fishers to predict the effect of augmenting ten new fishers to Olympic National Park. One main goal of the analysis is to determine how the success of the augmentation could differ depending on whether the fishers came from British Columbia versus; two genetically different source-populations. Using existing genotypes from British Columbia and Alberta fishers, this analysis will provide insights into the best source population of fishers to use for the planned augmentation to the Olympic National Park, where 90 fishers from British Columbia were reintroduced from 2008 to 2010. A 2019 genetic analysis of fishers on the Olympic Peninsula (based on hair samples collected at baited hair-snare and camera stations from 2013-2016) indicated that genetic diversity of the Olympic fisher population had declined slightly and would be expected to decline further in the future, which could put that population at risk. An augmentation of new fishers could restore this genetic diversity and this new analysis of the effects of releasing more British Columbia versus Alberta fishers into this population will help us decide the best source population and the best implementation approach. 2) Providing Recreation Opportunities Nothing for this installment. 3) Providing Conflict Prevention and Education Nothing for this installment. 4) Conserving Natural Areas Nothing for this installment. -
Structure and Petrology of the Deer Peaks Area Western North Cascades, Washington
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Winter 1986 Structure and Petrology of the Deer Peaks Area Western North Cascades, Washington Gregory Joseph Reller Western Washington University, [email protected] Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Reller, Gregory Joseph, "Structure and Petrology of the Deer Peaks Area Western North Cascades, Washington" (1986). WWU Graduate School Collection. 726. https://cedar.wwu.edu/wwuet/726 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. STRUCTURE AMD PETROLOGY OF THE DEER PEAKS AREA iVESTERN NORTH CASCADES, WASHIMGTa^ by Gregory Joseph Re Her Accepted in Partial Completion of the Requiremerjts for the Degree Master of Science February, 1986 School Advisory Comiiattee STRUCTURE AiO PETROIDGY OF THE DEER PEAKS AREA WESTERN NORTIi CASCADES, VC'oHINGTON A Thesis Presented to The Faculty of Western Washington University In Partial Fulfillment of the requirements for the Degree Master of Science by Gregory Joseph Re Her February, 1986 ABSTRACT Dominant bedrock mits of the Deer Peaks area, nortliv/estern Washington, include the Shiaksan Metamorphic Suite, the Deer Peaks unit, the Chuckanut Fontation, the Oso volcanic rocks and the Granite Lake Stock. Rocks of the Shuksan Metainorphic Suite (SMS) exhibit a stratigraphy of meta-basalt, iron/manganese schist, and carbonaceous phyllite. Tne shear sense of stretching lineations in the SMS indicates that dioring high pressure metamorphism ttie subduction zone dipped to the northeast relative to the present position of the rocks. -
Final Mountain Loop Road Repair Environmental Assessment
Figure 1-Vicinity Map, Location of Damage Forest-wide, 2003 Flood i Table of Content Chapter 1 –Need for Action ....................................................................................................... 1 Introduction ......................................................................................................................................... 1 Mountain Loop History, Desired Road Condition ............................................................................................. 1 October 2003 Flood Event ................................................................................................................................. 3 Need for Action .................................................................................................................................... 6 Proposed Action................................................................................................................................... 7 Proposed Repair at Milepost 33.1 (T30N, R11E, Section 29) ........................................................................... 7 Proposed Repair at Milepost 33.6 (T30N, R11E, Section 29) ......................................................................... 11 Proposed Repair at Milepost 34.8 (T30N, R11E, Section 28) ......................................................................... 16 Proposed Repair at Milepost 35.6 (T30N, R11E, Section 21) ......................................................................... 18 Project Scope..................................................................................................................................... -
Structure and Petrology of the Grandy Ridge-Lake Shannon Area, North Cascades, Washington Moira T
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Winter 1986 Structure and Petrology of the Grandy Ridge-Lake Shannon Area, North Cascades, Washington Moira T. (Moira Tracey) Smith Western Washington University, [email protected] Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Smith, Moira T. (Moira Tracey), "Structure and Petrology of the Grandy Ridge-Lake Shannon Area, North Cascades, Washington" (1986). WWU Graduate School Collection. 721. https://cedar.wwu.edu/wwuet/721 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. MASTER'S THESIS In presenting this thesis in partial fulfillment of the requirements for a master's degree at Western Washington University, I agree that the Library shall make its copies freely available for inspection. I further agree that extensive copying of this thesis is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without my written permission . Bellin^hum, W'Mihington 9HZZS □ izoai aTG-3000 STRUCTURE AND PETROLOGY OF THE GRANDY RIDGE-LAKE SHANNON AREA, NORTH CASCADES, WASHINGTON By Moira T. Smith Accepted in Partial Completion of the Requirements for the Degree Master of Science aduate School ADVISORY COMMITEE: Chairperson MASTER’S THESIS In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Western Washington University, I grant to Western Washington University the non-exclusive royalty-free right to archive, reproduce, distribute, and display the thesis in any and all forms, including electronic format, via any digital library mechanisms maintained by WWU. -
Distribution and Abundance of Mountain Goats Within the Ross Lake Watershed, North Cascades National Park Service Complex
' I ; q£ 04. & 9) -~o3 Distribution and Abundance of Mountain Goats within the Ross Lake Watershed, North Cascades National Park Service Complex Final Report to Skagit Environmental Endowment Commission Sarah J. Welch Robert C. Kuntz II Ronald E. Holmes Roger G. Christophersen North Cascades National Park Service Complex 2105 State Route 20 Sedro-Woolley, Washington 98284-9314 December 1997 1997 SEC #10 . ' Table of Contents I. Introduction 1 2. Study Area 3. Methods 3 4. Results. 4 5. Discussion 5 6. Recommendations 6 7. Literature Cited 7 List of Figures 1. Figure 1: Mountain goat study area in Ross Lake watershed, North Cascades National Park Service Complex (1996-1997) 2 List of Tables 1. Table l: Mountain goat observations. 4 2. Table 2: Habitat characteristics where mountain goats were observed 5 Distribution and Abundance of Mountain Goats within the Ross Lake Watershed, North Cascades National Park Service Complex Introduction Mountain goats (Oreamnus americanus) are native to northwestern North America and can be found throughout the North Cascades National Park Service Complex (NOCA). Their habitat requirements are quite specific and suitable habitat is patchily distributed across the landscape. During a11 seasons, mountain goat habitat is characterized by steep, rocky terrain. Summer habitat is generally above 1525 m (5000 ft) elevation, and features rock outcrops in or near subalpine meadows and forest (Welch, 1991; Holmes, 1993; Schoen and Kirchoff, 1981; NCASI, 1989; Chadwick, 1983; Benzon and Rice, 1988). Many mountain goat populations in Washington have declined during the last 20 years. Although specific causes have not been identified, several factors may have contributed to the regional decline. -
Redacted for Privacy Dr
AN ABSTRACT OF THE THESIS OF PETER TREADWELL MILNES for the degree of Master of Science in Geology presented on October 22, 1976 Title: STRUCTURAL GEOLOGY AND METAMORPHIC PETROLOGY OF THE ILLABOT PEAKS AREA, SKAGIT COUNTY, WASHINGTON Abstract approved: Redacted for Privacy Dr. Robert Lawrence The Illabot Peaks area is composed of several essentially homo- clinal eastward dipping thrust blocks of Shuksan Schist which are comprised of olivine-free calc-alkaline basalt that has been meta- morphosed under greenschist to blueschist facies conditions.The structurally lower portions of the Shuksan Schist are occupied by a soda amphibole-bearing rock that probably originated from intercala- tions of high Po and high ferric iron content.The blocks of Shuksan 2 Schist rest upon ductile mega-shear zones of lower greenschist facies quartz-muscovite-graphite phyllite that have been tentatively corre- lated with the Darrington Phyllite.The Shuksan Schist and Darrington Phyllite, forming the Shuksan metamorphic suite, were syntecton- ically metamorphosed in the late Permian to early Triassic.The primary foliation, the amphibole lineations, and the intrafolial F 1 folds were formed at this time. The blocks of Shuksan Schist were emplaced during the Middle to early Late Cretaceous by movements on the large displacement Shuksan thrust.The thrust system in the Illabot Peaks area dips in a concave upward manner tothe east, has a large westward displace- ment, and is highly imbricated.Small lenticular pods of brecciated blueschist fragments and meta-igneous basement rock slivershave been tectonically emplaced along the margins of the thrust.The blueschist pods, retrogressively metamorphosed, are possibleindi- cators of a rock unit at depth of a higher faciesthan the typical Shuksan Schist. -
North Stillaguamish Valley ECONOMIC REDEVELOPMENT PLAN October, 2015 ACKNOWLEDGEMENTS
North Stillaguamish Valley ECONOMIC REDEVELOPMENT PLAN October, 2015 ACKNOWLEDGEMENTS The strength of the North Stillaguamish Economic Redevelopment Plan lies in the people who have crafted it, who live and work in the valley and who will continue to shape its future. The project team is honored to have worked with this enthusiastic group of stakeholders. Office of Senator Maria Cantwell Town of Darrington Sally Hintz, Northwest Washington Director Dan Rankin, Mayor Snohomish County Councilman Ken Klein, Snohomish County Council District 1 Washington State University Sean Connell, Trade and Economic Development Director Curtis Moulton, Snohomish County Director, WSU Extension Annique Bennett, Tourism Promotion Area Coordinator Bradley Gaolach, Director, Western Center for Metropolitan Extension & Research Linda Neunzig, Agricultural Project Coordinator Martha Aitken, Senior Associate for Metropolitan Extension Judy Pendergrass, Extension Coordinator City of Arlington Barbara Tolbert, Mayor Workforce Snohomish Paul Ellis, City Administrator Erin Monroe, CEO Reid Shockey, Consultant Mary Houston, Director of Service Delivery PROJECT TEAM Economic Alliance Snohomish County Troy McClelland, President and CEO Glenn Coil, Senior Manager, Public Policy & Research Community Attributes Inc. Funded by Chris Mefford, President and CEO U.S. Department of Commerce Economic Development Administration Alison Peters, Research Principal Award # 07-79-07116 Elliot Weiss, Project Manager Tim Degner, Graphic Designer Economic Adjustment Assistance Program under 42 U.S.C. §3149, Section 290 Mark Goodman, Planning Analyst of the Public Works and Economic Development Act of 1965 (Public Law 89- 136), as amended by the Economic Development Administration Reauthoriza- Yolanda Ho, Planning Analyst tion Act of 2004 (Public Law 108-373) Bryan Lobel, Senior Planning Analyst North Stillaguamish Valley ECONOMIC REDEVELOPMENT PLAN 808 134th St. -
Geologic Map of Washington - Northwest Quadrant
GEOLOGIC MAP OF WASHINGTON - NORTHWEST QUADRANT by JOE D. DRAGOVICH, ROBERT L. LOGAN, HENRY W. SCHASSE, TIMOTHY J. WALSH, WILLIAM S. LINGLEY, JR., DAVID K . NORMAN, WENDY J. GERSTEL, THOMAS J. LAPEN, J. ERIC SCHUSTER, AND KAREN D. MEYERS WASHINGTON DIVISION Of GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 •• WASHINGTON STATE DEPARTMENTOF 4 r Natural Resources Doug Sutherland· Commissioner of Pubhc Lands Division ol Geology and Earth Resources Ron Telssera, Slate Geologist WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere, State Geologist David K. Norman, Assistant State Geologist GEOLOGIC MAP OF WASHINGTON NORTHWEST QUADRANT by Joe D. Dragovich, Robert L. Logan, Henry W. Schasse, Timothy J. Walsh, William S. Lingley, Jr., David K. Norman, Wendy J. Gerstel, Thomas J. Lapen, J. Eric Schuster, and Karen D. Meyers This publication is dedicated to Rowland W. Tabor, U.S. Geological Survey, retired, in recognition and appreciation of his fundamental contributions to geologic mapping and geologic understanding in the Cascade Range and Olympic Mountains. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 Envelope photo: View to the northeast from Hurricane Ridge in the Olympic Mountains across the eastern Strait of Juan de Fuca to the northern Cascade Range. The Dungeness River lowland, capped by late Pleistocene glacial sedi ments, is in the center foreground. Holocene Dungeness Spit is in the lower left foreground. Fidalgo Island and Mount Erie, composed of Jurassic intrusive and Jurassic to Cretaceous sedimentary rocks of the Fidalgo Complex, are visible as the first high point of land directly across the strait from Dungeness Spit. -
Mt. Baker-Snoqualmie Campground Prospectus
United States Forest Mt. Baker- 2930 Wetmore Ave/ Suite 3A Department of Service Snoqualmie Everett, Washington, 09201 Agriculture National Forest File Code: 2730-1 Date: September 1, 2017 Route To: (2720) Subject: Forest-wide Campground Concession To: Dear Interested Parties REPLY DUE OCTOBER 2, 2017 Dear Interested Parties: Thank you for your interest in providing visitor services at various recreation sites within the Mount Baker-Snoqualmie National Forest (MBS). The Prospectus (solicitation for offers) is now available for review and download on the Forest website (address below). Detailed information on this business opportunity, Forest Service concession program and policies, special use permit, application and post-selection requirements are available in the Prospectus. This website will also serve as the main source for all Prospectus related information and updates throughout this solicitation and selection process. If requested by applicants, a single site visit may be scheduled in Fall 2017. All applicants will be encouraged to attend this on-site visit to review the facilities when and if it is scheduled. Applications submitted in response to this Prospectus are subject to cost recovery pursuant to 36 CFR 251.58(c)(3)(iii). Applicants must submit an application fee of $400.00 to cover the cost of the Prospectus and review of the application. Additionally, the selected applicant will be responsible for the cost of preparing and issuing the permit and conducting a Financial Ability Determination (FAD), unless the Forest Service has conducted a FAD on the applicant within the past year. Payments due the United States for this application must be paid in the form of a bank draft, money order, or cashier’s check payable to the USDA- Forest Service.