Washington Natural Areas Plan 2007
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2019 Oregon Administrative Rules Compilation
2019 OREGON ADMINISTRATIVE RULES COMPILATION CHAPTER 736 Parks and Recreation Department Published By DENNIS RICHARDSON Secretary of State Copyright 2019 Office of the Secretary of State Rules effective as of January 01, 2019 DIVISION 1 PROCEDURAL RULES 736-001-0000 Notice of Proposed Rules 736-001-0005 Model Rules of Procedure 736-001-0030 Fees for Public Records DIVISION 2 ADMINISTRATIVE ACTIVITIES 736-002-0010 State Park Cooperating Associations 736-002-0015 Working with Donor Organizations 736-002-0020 Criminal Records Checks 736-002-0030 Definitions 736-002-0038 Designated Positions: Authorized Designee and Contact Person 736-002-0042 Criminal Records Check Process 736-002-0050 Preliminary Fitness Determination. 736-002-0052 Hiring or Appointing on a Preliminary Basis 736-002-0058 Final Fitness Determination 736-002-0070 Crimes Considered 736-002-0102 Appealing a Fitness Determination 736-002-0150 Recordkeeping, Confidentiality, and Retention 736-002-0160 Fees DIVISION 3 WILLAMETTE RIVER GREENWAY PLAN 736-003-0005 Willamette River Greenway Plan DIVISION 4 DISTRIBUTION OF ALL-TERRAIN VEHICLE FUNDSTO PUBLIC AND PRIVATELY OWNED LANDMANAGERS, ATV CLUBS AND ORGANIZATIONS 736-004-0005 Purpose of Rule 736-004-0010 Statutory Authority 736-004-0015 Definitions 736-004-0020 ATV Grant Program: Apportionment of Monies 736-004-0025 Grant Application Eligibility and Requirements 736-004-0030 Project Administration 736-004-0035 Establishment of the ATV Advisory Committee 736-004-0045 ATV Operating Permit Agent Application and Privileges 736-004-0060 -
Washington Division of Geology and Earth Resources Open File Report
RECONNAISSANCE SURFICIAL GEOLOGIC MAPPING OF THE LATE CENOZOIC SEDIMENTS OF THE COLUMBIA BASIN, WASHINGTON by James G. Rigby and Kurt Othberg with contributions from Newell Campbell Larry Hanson Eugene Kiver Dale Stradling Gary Webster Open File Report 79-3 September 1979 State of Washington Department of Natural Resources Division of Geology and Earth Resources Olympia, Washington CONTENTS Introduction Objectives Study Area Regional Setting 1 Mapping Procedure 4 Sample Collection 8 Description of Map Units 8 Pre-Miocene Rocks 8 Columbia River Basalt, Yakima Basalt Subgroup 9 Ellensburg Formation 9 Gravels of the Ancestral Columbia River 13 Ringold Formation 15 Thorp Gravel 17 Gravel of Terrace Remnants 19 Tieton Andesite 23 Palouse Formation and Other Loess Deposits 23 Glacial Deposits 25 Catastrophic Flood Deposits 28 Background and previous work 30 Description and interpretation of flood deposits 35 Distinctive geomorphic features 38 Terraces and other features of undetermined origin 40 Post-Pleistocene Deposits 43 Landslide Deposits 44 Alluvium 45 Alluvial Fan Deposits 45 Older Alluvial Fan Deposits 45 Colluvium 46 Sand Dunes 46 Mirna Mounds and Other Periglacial(?) Patterned Ground 47 Structural Geology 48 Southwest Quadrant 48 Toppenish Ridge 49 Ah tanum Ridge 52 Horse Heaven Hills 52 East Selah Fault 53 Northern Saddle Mountains and Smyrna Bench 54 Selah Butte Area 57 Miscellaneous Areas 58 Northwest Quadrant 58 Kittitas Valley 58 Beebe Terrace Disturbance 59 Winesap Lineament 60 Northeast Quadrant 60 Southeast Quadrant 61 Recommendations 62 Stratigraphy 62 Structure 63 Summary 64 References Cited 66 Appendix A - Tephrochronology and identification of collected datable materials 82 Appendix B - Description of field mapping units 88 Northeast Quadrant 89 Northwest Quadrant 90 Southwest Quadrant 91 Southeast Quadrant 92 ii ILLUSTRATIONS Figure 1. -
Scientific Program Chair
Science Program 44th Annual Meeting of the Pacific Seabird Group 22-25 February, 2017 Daily Schedule Overview Tacoma Convention Center (TCC) Comments or questions, please contact Local Committee: [email protected] Tuesday, 21 February 2017 (pre-conference) Hotel Murano, Lido Boardroom 1300-1700 Short-tailed Albatross Recovery Team (START) Meeting – by invitation Wednesday, 22 February 2017 0730–1700 REGISTRATION DESK OPEN (TCC Lobby) Committee Meetings – all welcome, unless otherwise indicated. Boardroom N, Ballroom AB, Boardroom S, Commencement Bay N, 1 TCC TCC TCC CUW Aleutian Tern Tech 0900-1230 EXCO MAMU Tech Comm TUPU Tech Comm Comm 1230-1300 BREAK Seabird Monitoring SCMU and GUMU Tech 1300-1500 EXCO MAMU Tech Comm Comm Comm FWS Pacific Seabird SCMU and GUMU Tech 1500-1700 EXCO MAMU Tech Comm Program Comm 1700-1830 KIMU Tech Comm 1800-2100 WELCOME RECEPTION (Hotel Murano, Venice Ballroom) 1 Center for Urban Waters (CUW), 326 East D St. Tacoma WA 98421. https://www.urbanwaters.org 1 Thursday, 23 February 2017 0730–1700 REGISTRATION DESK OPEN (TCC Lobby) Ballroom AB Meeting Room 315 Meeting Room 316 0830-0900 Welcome and Opening Remarks PLENARY: P. Dee Boersma (Ballroom AB) 0900-1000 Natural History and Long-Term Studies Are Fundamental to Science 1000-1030 Coffee Break SPS 2: Sound to Sea: 1030-1200 Marine Birds Across the Population Biology Tools and Techniques Salish Sea Lunch (on your own) and Meetings 1200-1330 NOAA Fisheries Seabird Workgroup (1200, Boardroom N) – by invitation Former Chairs Meeting (1215-1320, -
Periodically Spaced Anticlines of the Columbia Plateau
Geological Society of America Special Paper 239 1989 Periodically spaced anticlines of the Columbia Plateau Thomas R. Watters Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, D. C. 20560 ABSTRACT Deformation of the continental flood-basalt in the westernmost portion of the Columbia Plateau has resulted in regularly spaced anticlinal ridges. The periodic nature of the anticlines is characterized by dividing the Yakima fold belt into three domains on the basis of spacings and orientations: (1) the northern domain, made up of the eastern segments of Umtanum Ridge, the Saddle Mountains, and the Frenchman Hills; (2) the central domain, made up of segments of Rattlesnake Ridge, the eastern segments of Horse Heaven Hills, Yakima Ridge, the western segments of Umtanum Ridge, Cleman Mountain, Bethel Ridge, and Manastash Ridge; and (3) the southern domain, made up of Gordon Ridge, the Columbia Hills, the western segment of Horse Heaven Hills, Toppenish Ridge, and Ahtanum Ridge. The northern, central, and southern domains have mean spacings of 19.6,11.6, and 27.6 km, respectively, with a total range of 4 to 36 km and a mean of 20.4 km (n = 203). The basalts are modeled as a multilayer of thin linear elastic plates with frictionless contacts, resting on a mechanically weak elastic substrate of finite thickness, that has buckled at a critical wavelength of folding. Free slip between layers is assumed, based on the presence of thin sedimentary interbeds in the Grande Ronde Basalt separating groups of flows with an average thickness of roughly 280 m. -
Flood Basalts and Glacier Floods—Roadside Geology
u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1. -
Analysis of Dishman Hills Structure and Hydrogeology
Eastern Washington University EWU Digital Commons Geosciences Student Work Geosciences 2021 Analysis of Dishman Hills Structure and Hydrogeology Cole R. McGregor Eastern Washington University, [email protected] Follow this and additional works at: https://dc.ewu.edu/geosci_student Part of the Earth Sciences Commons, and the Mathematics Commons Recommended Citation McGregor, Cole R., "Analysis of Dishman Hills Structure and Hydrogeology" (2021). Geosciences Student Work. 1. https://dc.ewu.edu/geosci_student/1 This Poster is brought to you for free and open access by the Geosciences at EWU Digital Commons. It has been accepted for inclusion in Geosciences Student Work by an authorized administrator of EWU Digital Commons. For more information, please contact [email protected]. Analysis of Dishman Hills Structure and Hydrogeology Cole McGregor Eastern Washington University, Department of Geology Abstract: The structural and hydrogeology of Dishman Hills Conservation Area was interpreted to gain a better picture of its interaction with the Spokane Valley-Rathdrum Prairie aquifer. The rock in this area is Precambrian Ravalli Group with granitic migmatites. This is due to Figure 9: exhumation causing decompression melting in between the bed layers. Other rocks such as amphibolite, gneiss, schist, quartzite, and phyllite are seen along with granitic dikes (WSDNR). This rock type covers all of the Dishman area and is Precambrian in age. Due to The image shows areas of water ponding that don’t tectonic forces in the Spokane area, fractures have also formed within the Precambrian rock. Water will concentrate in fracture zones, enter the aquifer as green polygons. These seem to be known to be areas of groundwater drainage. -
Preserving Trails and Providing Solutions May-June
PONDEROSA BACK COUNTRY HORSEMEN OF WASHINGTON Preserving Trails and Providing Solutions May-June 2018 VOLUNTEER HOURS DUE BY MAY 25! Please be sure to turn in your volunteer hours to Carol Klar by May 25! Any time you spend working on BCH stuff (phone calls, trail clearing, work parties, paperwork, whatever) counts towards your volunteer hours. If you have questions, give Carol a call. BCHA Annual Board Meeting By Ken Carmichael The BCHA board meeting was held in Airway Heights Washington April 23-25. This annual event is hosted by a different state each year. It is a time to be very proud of being a BCHW member. The team that put on the event did a great job. Our national directors Darrell Wallace and Jason Ridlon had the event brought to Washington and helped arrange for the nice facilities. Alternate Director Bill McKenna coordinated all of the volunteers. BCHW President Kathy Young and many volunteers were on site to help. Among those was PBCH member Doug Bailey helping with registration and other duties. BCHW Executive Director Nicole Sedgwick provided the other states with an update on the status of the Your Membership program and I spoke about the Membership Development Program. Darrell is also Vice President of BCHA. BCHW member Mike McGlenn was elected to the Executive Committee of BCHA. BCHW continues to be a leader among the states. This board meeting provided many opportunities for sharing information among the states and committees. A new feature was a break out into 4 regions to discuss issues. Then each region had the opportunity to discuss these issues with the BCHA 10 standing committees. -
Feature Web 05-04
the Centers for Disease Control, only 15 percent of the Healthy Hiking U.S. adult population is getting enough physical activity. “Our goal,” says Julie CHIEFELBEIN Gerberding, Director of the S AVE CDC, “is to help people D understand that even modest activity such as walking or gardening is a step in the right direction.” According to the American Hiking Society, the benefits of hiking or walking just 30 minutes a day are impressive: ⌧Decreased cholesterol ⌧Lowering of blood pressure ⌧Releasing of calming endorphins ⌧Preventing osteoporosis ⌧Relieving back pain ⌧Reducing insulin needed by diabetics Detailed info on these Getting fit on studies are available at www.americanhiking.org. the trail is For those of us who already hike, none of this is terribly surprising. easy, fun, and “It’s a great break from the routine,” says Debra Gore, a good for you. family practice doctor with Group Health in Spokane. “It’s a great stress relief from the hassles of sitting in front of a computer all day.” And for those who want to get out more and enjoy these benefits, there’s good news: you don’t have to be a buff mountain By Andrew Engelson years later, he’s still getting up into the climber to get started. It’s easy. backcountry. He and other hikers his As with any exercise program, if Julian Ansell is evidence that hiking age are as good a case as any for the you’re just beginning, consult your is good for you. physical and emotional benefits of doctor or medical provider first to The retired physician and Washing- hiking. -
Grays Harbor Juvenile Fish Use Assessment: 2012 Annual Report
Grays Harbor Juvenile Fish Use Assessment: 2012 Annual Report Prepared for the Chehalis Basin Habitat Work Group February, 2013 Prepared by: Todd Sandell, James Fletcher, Andrew McAninch and Micah Wait Setting the net in Half Moon Bay, Grays Harbor Estuary, 2012 Sculpin displaying in a Wild Fish Conservancy “photarium”, April 2012 Table of Contents Executive Summary .................................................................................................... 1 Section 1: Introduction ................................................................................................ 7 1.1 Purpose and Objectives ................................................................................................7 1.2 Study Area ...................................................................................................................8 Specific Hypotheses: ......................................................................................................... 10 Section 2: Methods ................................................................................................... 12 2.1 Habitat Inventory/ Sample Site Selection.................................................................... 12 2.2 Field Sampling Methodology ....................................................................................... 15 Data Recording/Water Quality Measures ............................................................................................ 17 2.3 Age Class Assignments .............................................................................................. -
The Wild Cascades
THE WILD CASCADES Fall, 1984 2 The Wild Cascades PRESIDENT'S MESSAGE ONCE THE LINES ARE DRAWN, THE BATTLE IS NOT OVER The North Cascades Conservation Council has developed a reputation for consistent, hard-hitting, responsible action to protect wildland resources in the Washington Cascades. It is perhaps best known for leading the fight to preserve and protect the North Cascades in the North Cascades National Park, the Pasayten and Glacier Peak Wilderness Areas, and the Ross Lake and Lake Chelan National Recreation Areas. Despite the recent passage of the Washington Wilderness Act, many areas which deserve and require wilderness designation remain unprotected. One of the goals of the N3C must be to assure protection for these areas. In this issue of the Wild Cascades we have analyzed the Washington Wilderness Act to see what we won and what still hangs in the balance (page ). The N3C will continue to fight to establish new wilderness areas, but there is also a new challenge. Our expertise is increasingly being sought by government agencies to assist in developing appropriate management plans and to support them against attempts to undermine such plans. The invitation to participate more fully in management activities will require considerable effort, but it represents a challenge and an opportunity that cannot be ignored. If we are to meet this challenge we will need members who are either knowledgable or willing to learn about an issue and to guide the Board in its actions. The Spring issue of the Wild Cascades carried a center section with two requests: 1) volunteers to assist and guide the organization on various issues; and 2) payment of dues. -
A G~Ographic Dictionary of Washington
' ' ., • I ,•,, ... I II•''• -. .. ' . '' . ... .; - . .II. • ~ ~ ,..,..\f •• ... • - WASHINGTON GEOLOGICAL SURVEY HENRY LANDES, State Geologist BULLETIN No. 17 A G~ographic Dictionary of Washington By HENRY LANDES OLYMPIA FRAN K M, LAMBORN ~PUBLIC PRINTER 1917 BOARD OF GEOLOGICAL SURVEY. Governor ERNEST LISTER, Chairman. Lieutenant Governor Louis F. HART. State Treasurer W.W. SHERMAN, Secretary. President HENRY SuzzALLO. President ERNEST 0. HOLLAND. HENRY LANDES, State Geologist. LETTER OF TRANSMITTAL. Go,:ernor Ernest Lister, Chairman, and Members of the Board of Geological Survey: GENTLEMEN : I have the honor to submit herewith a report entitled "A Geographic Dictionary of Washington," with the recommendation that it be printed as Bulletin No. 17 of the Sun-ey reports. Very respectfully, HENRY LAKDES, State Geologist. University Station, Seattle, December 1, 1917. TABLE OF CONTENTS. Page CHAPTER I. GENERAL INFORMATION............................. 7 I Location and Area................................... .. ... .. 7 Topography ... .... : . 8 Olympic Mountains . 8 Willapa Hills . • . 9 Puget Sound Basin. 10 Cascade Mountains . 11 Okanogan Highlands ................................ : ....' . 13 Columbia Plateau . 13 Blue Mountains ..................................... , . 15 Selkirk Mountains ......... : . : ... : .. : . 15 Clhnate . 16 Temperature ......... .' . .. 16 Rainfall . 19 United States Weather Bureau Stations....................... 38 Drainage . 38 Stream Gaging Stations. 42 Gradient of Columbia River. 44 Summary of Discharge -
San Juan Island National Historical Park Natural Resource Condition Assessment
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science San Juan Island National Historical Park Natural Resource Condition Assessment Natural Resource Report NPS/NRSS/WRD/NRR—xxxx ON THE COVER Looking east from the park, toward Lopez Island and Strait of Juan de Fuca. Photo by Peter Dunwiddie. San Juan Island National Historical Park Natural Resource Condition Assessment Natural Resource Report NPS/NRSS/WRD/NRR—xxx Paul R. Adamus Water Resources Science Program Oregon State University Corvallis, Oregon and Adamus Resource Assessment, Inc. Corvallis, Oregon Peter Dunwiddie University of Washington Seattle, Washington Anna Pakenham Marine Resource Management Program Oregon State University Corvallis, Oregon This report was prepared under Task Agreement P12AC15016 (Cooperative Agreement H8W07110001) between the National Park Service and Oregon State University September 2015 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with