Chapter 11. Mid-Columbia Recovery Unit Yakima River Basin Critical Habitat Unit
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The Washington Climate Change Impacts Assessment
The Washington Climate Change Impacts Assessment Evaluating Washington’s Future in a Changing Climate ........................................................................................................ A report by The Climate Impacts Group University of Washington Climate Science June 2009 in the Public Interest Recommended citation: Climate Impacts Group, 2009. The Washington Climate Change Impacts Assessment, M. McGuire Elsner, J. Littell, and L Whitely Binder (eds). Center for Science in the Earth System, Joint Institute for the Study of the Atmosphere and Oceans, University of Washington, Seattle, Washington. Available at: http://www.cses.washington.edu/db/pdf/wacciareport681.pdf Front cover satellite image credit: http://visibleearth.nasa.gov/view_rec.php?vev1id=4786 NASA - National Aeronautics and Space Administration Visible Earth: A catalog of NASA images and animations of our home planet Provided by the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE The Pacific Northwest is cloud-free in this SeaWiFS image. Multihued phytoplankton blooms are visible off of Washington's Olympic coast. Also visible in this image are: Fraser River outflow, snowcapped peaks of Mt. Olympus, Mt. Rainier, Mt. Adams, Mt. Hood, Mt. Jefferson, the Three Sisters, the North Cascades, and the Columbia and Snake River watersheds. Metadata * Sensor OrbView-2/SeaWiFS * Visualization Date 2000-09-26 * The Visible Earth is part of the EOS Project Science Office located at NASA Goddard Space Flight Center. Small images credits: Wheat: © 2009 www.photos.com Coast; Seattle skyline: © J. Martin Grassley McNary Dam: courtesy Bonneville Power Administration Salmon: courtesy University of Washington News and Information Forest: courtesy Climate Impacts Group, University of Washington Report design: Beth Tully, Edit-Design Center, University of Washington The Washington Climate Change Impacts Assessment Evaluating Washington’s Future in a Changing Climate ........................................................................................ -
Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington by Wes Hildreth and Judy Fierstein
Prepared in Cooperation with the Water Resources Program of the Yakama Nation Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington By Wes Hildreth and Judy Fierstein Pamphlet to accompany Scientific Investigations Map 3315 Photograph showing Mount Adams andesitic stratovolcano and Signal Peak mafic shield volcano viewed westward from near Mill Creek Guard Station. Low-relief rocky meadows and modest forested ridges marked by scattered cinder cones and shields are common landforms in Simcoe Mountains volcanic field. Mount Adams (elevation: 12,276 ft; 3,742 m) is centered 50 km west and 2.8 km higher than foreground meadow (elevation: 2,950 ft.; 900 m); its eruptions began ~520 ka, its upper cone was built in late Pleistocene, and several eruptions have taken place in the Holocene. Signal Peak (elevation: 5,100 ft; 1,555 m), 20 km west of camera, is one of largest and highest eruptive centers in Simcoe Mountains volcanic field; short-lived shield, built around 3.7 Ma, is seven times older than Mount Adams. 2015 U.S. Department of the Interior U.S. Geological Survey Contents Introductory Overview for Non-Geologists ...............................................................................................1 Introduction.....................................................................................................................................................2 Physiography, Environment, Boundary Surveys, and Access ......................................................6 Previous Geologic -
Indian Artifacts of the Columbia River Priest
IINNDDIIAANN AARRTTIIFFAACCTTSS OOFF TTHHEE CCOOLLUUMMBBIIAA RRIIVVEERR PPRRIIEESSTT RRAAPPIIDDSS TTOO TTHHEE CCOOLLUUMMBBIIAA RRIIVVEERR GGOORRGGEE IIIDDDEEENNNTTTIIIFFFIIICCCAAATTTIIIOOONNN GGGUUUIIIDDDEEE VVVOOOLLLUUUMMMEEE 111 DDDaaavvviiiddd HHHeeeaaattthhh Copyright 2003 All rights reserved. This publication may only be reproduced for personal and educational use. SSSCCCOOOPPPEEE This document is used to define projectile point typologies common to the Columbia Plateau, covering the region from Priest Rapids to the Columbia Gorge. When employed, recognition of a specified typology is understood as define within the body of this document. This document does not intend to cover, describe or define all typologies found within the region. This document will present several recognized typologies from the region. In several cases, a typology may extend beyond the Columbia Plateau region. Definitions are based upon research and records derived from consultation with; and information obtained from collectors and authorities. They are subject to revision as further experience and investigation may show is necessary or desirable. This document is authorized for distribution in an electronic format through selected organizations. This document is free for personal and educational use. RRREEECCCOOOGGGNNNIIITTTIIIOOONNN A special thanks for contributions given to: Ben Stermer - Technical Contributions Bill Jackson - Technical Contributions Joel Castanza - Images Mark Berreth - Images, Technical Contributions Randy McNeice - Images Rodney Michel -
The Teanaway: Geologic & Physical Geographic Patterns
Ellensburg Chapter Ice Age Floods Institute The Teanaway: Geologic & Physical Geographic Patterns Field Trip Leader: Dr. Karl Lillquist Geography Department Central Washington University 29 September 2013 1 Preliminaries Field Trip Overview: Itinerary: The State of Washington is in the 11:00 am Depart CWU process of purchasing ~50,000 acres of 11:30 Stop 1—Lambert Road private forest lands in the Teanaway River Watershed. This Eastern Cascade 12:15 pm Depart drainage contains prime fish and 12:30 Stop 2—Ballard Hill Road wildlife habitat, and is a key piece of 1:00 Depart the Yakima River Basin water puzzle. 1:15 Stop 3—Cheese Rock 2:45 Depart We will explore the geology and 3:00 29 Pines CG Toilet Stop physical geography of the soon-to-be purchased lands as well as private and 3:15 Depart adjacent U.S. Forest Service lands in 3:30 Stop 4—Teanaway Grd Stn the Teanaway River Watershed. Our 4:00 Depart focus will be on the different bedrock 4:15 Stop 5—Iron Peak Trail and landforms of the watershed. Columbia River basalts, Roslyn 5:00 Depart sandstone, Teanaway basalt, Swauk 6:00 Arrive at CWU sandstone, and Ingalls Tectonic Complex are all found in the area. These varied lithologies have been shaped by unique Eastern Cascade weather and climate patterns resulting in river processes, weathering, landslides, and glaciers over time. 2 En route to Stop 1 Our route to Stop 1: Fans (Waitt, 1979; Tabor et al, 1982). Drive south on D street to University Over time, these fans became stable Way, then west on University Way to (perhaps because of slowing tectonic WA 10. -
Naches Watershed Washington
Washington Naches Watershed HUC: 17030002 Rapid Watershed Assessment This assessment involves the collection of quantitative and qualitative information to develop a watershed profile, sufficient analysis of that information to make qualitative statements as to resource concerns and conditions, and the generation of information with which to make decisions about conservation needs and recommendations. These assessments are conducted through the use of Geographic Information System (GIS) technology and by conservation planning teams working within the watershed, meeting with landowners and conservation groups, inventorying agricultural areas, assessing current levels of resource management, identifying conservation recommendations and, making qualitative estimates of the impacts of conservation on local resource concerns. October 2, 2006 1 Naches Watershed Introduction 717,048 Total Acres HUC# 17030003 The Naches Watershed is located in the Yakima River drainage in on the east side of the Cascade Mountain range. The Naches 8-Digit Hydrologic Unit Code (HUC) subbasin is approximately 717,048 acres in size. The watershed is 20% privately owned and 80% publicly owned. The majority of the watershed is forest and cropland. Cropland is located mostly in the lower elevations. Agricultural enterprises include hay and pasture, orchards and small beef operations. The city of Naches makes up the largest urban area in the watershed. The majority of the watershed is located in Yakima County. Major resource concerns are soil erosion from forest roads, streambank erosion, impaired water quality, forest health issues, invasive weeds, and poor pasture condition. Primary natural resource technical assistance is provided by the Yakima NRCS Field Office, North Yakima Conservation District and the South Central Resource Conservation and Development Area. -
Naches River Basin Field Trip
Ice Age Floods Institute—Ellensburg Chapter Naches River Basin Field Trip Field Trip Leaders: Karl Lillquist, Geography Department, CWU Nick Zentner, Geology Department, CWU Sunday 25 September 2011 Route & Itinerary 11:00 Depart from CWU’s Hebeler Hall 12:00 Arrive Stop 1—Sanford Pasture Landslide 12:30 Depart for Stop 2 12:45 Arrive Stop 2—Nile Landslide (up close) 1:45 Depart for Stop 3 2:00 Arrive at Stop 3—Nile 5 Landslide (big picture) 2:30 Depart for Stop 4 4 2:45 Arrive at Stop 4—Edgar Rock Volcano 3:15 Depart for Stop 5 3 3:30 Arrive at Stop 5—Boulder 2 Cave 1 4:30 Depart for Ellensburg 6:00 Arrive in Ellensburg 1 Trip Overview Our field trip will take us from the Columbia Plateau to the South Cascades. Our story begins with volcanism—effusive and explosive that resulted in lava flows, lahars, dikes, and stratovolcanoes. Over time, weathering as well as erosion by glaciers, rivers, and landslides have shaped the volcanics. Recent landslides and floods have dramatically altered this area. Stops will include the early Pleistocene? Sanford Pasture landslide, the October 2009 Nile Valley landslide, Miocene Edgar Rock Volcano, and Quaternary Boulder Cave–all in the middle Naches River Valley. 2 Enroute to Stop 1 • On I-82, we go over three prominent NW-SE trending up-folds or anticlines—Manastash Ridge, North Umtanum Ridge, and South Umtanum Ridge. These folds, and some associated thrust faulting, are the result of ~N-S compression. • If the weather is clear, note Mount Rainier and Mount Adams, the towering stratovolcanoes that dominate the South Cascades. -
Suggested Fishing Destinations in Central Washington the Yakima
Suggested Fishing Destinations in Central Washington Always refer to the WDFW Fishing Regulation Pamphlet prior to fishing any of these streams. Most of these are within an easy drive of Red’s Fly Shop, or even a day trip from the Puget Sound area. The east slopes of the Cascades are regarded as the best small stream fishing in Washington State and a GREAT place to start as a beginner! Most of the fisheries here offer small trout in abundance, which is great adventure and perfect for learning the art of fly fishing. The Yakima River Canyon The Canyon near Red’s Fly Shop is best wade fished when the river flows are below 2,500 cfs. September and October are the best months for wading, but February and March can offer great bank access as well. Spring and summer are more challenging but still possible. Yakima County Naches River – Trout tend to be most abundant upstream from the Tieton River junction. The best wade fishing season is July – October Tieton River – It runs fairly dirty in June, but July – mid August is excellent. Rattlesnake Creek – This is a great hike in adventure and offers wonderful small stream Cutthroat fishing for anyone willing to get off the beaten path. Little Naches River – Easy access off of USFS Road 19, July – October is the best time. American River/Bumping Rivers – These are in the headwaters of the Naches drainage. Be sure to read the WDFW Regulations if you fish the American River. Ahtanum Creek – Great small stream fishing. June – October Wenas Creek – Small water, small fish, but a great adventure. -
Restoring Sockeye Salmon to the Yakima River Basin. Mark V
Restoring Sockeye Salmon to the Yakima River Basin. Mark V. Johnston1,David E. Fast1, Brian Saluskin1, William J. Bosch1, and Stephen J. Grabowski2. 1 2 Sockeye at Roza Dam, Yakima R., July 17, 2002 Stan Wamiss Yakama Nation – Yakima/Klickitat Fisheries Project, Toppenish, WA. U.S. Bureau of Reclamation, Boise, ID. Abstract Returns of sockeye salmon to the upper Columbia Basin have In a January 2007 memorandum discussing the role of large extirpated areas in Current Restoration Effort numbered 50,000 or fewer in 14 of the past 22 years. Dam counts indicate recovery, the Interior Columbia Technical Recovery Team noted that “Snake As part of water storage improvements under Section 1206 of the 1994 that sockeye are declining by an average of 830 fish per year. Of the historic River sockeye are currently restricted to a single extant population. The Yakima River Basin Water Enhancement Project Act, Title XII of Public Law sockeye nursery lake habitat in the Upper Columbia, only about 4% is probability of long-term persistence of the [evolutionarily significant unit] ESU 103-434, the Yakama Nation, with the cooperation of the U.S. Bureau of presently utilized with only two (Wenatchee and Osoyoos) of 12 historic will be greatly enhanced with additional populations. In fact, the ESU cannot Reclamation, is now actively pursuing the restoration of anadromous fish nursery lakes presently producing fish. Four nursery lakes in the Yakima meet the minimum ESU biological viability criteria established by the TRT passage above Cle Elum Dam. The BOR estimated sockeye smolt River Basin, which historically produced an estimated annual return of about without multiple viable populations.” production potential of 400,000 to 1.6 million fish in the Cle Elum Lake 200,000 sockeye, were removed from production in the early 1900s when watershed (Fig. -
Cle Elum Lake Anadromous
April 2000 CLE ELUM LAKE ANADROMOUS SALMON RESTORATION FEASIBILITY STUDY: SUMMARY OF RESEARCH THIS IS INVISIBLE TEXT TO KEEP VERTICAL ALIGNMENT THIS IS INVISIBLE TEXT TO KEEP VERTICAL ALIGNMENT THIS IS INVISIBLE TEXT TO KEEP VERTICAL ALIGNMENT THIS IS INVISIBLE TEXT TO KEEP VERTICAL ALIGNMENT THIS IS INVISIBLE TEXT TO KEEP VERTICAL ALIGNMENT THIS IS INVISIBLE TEXT TO KEEP VERTICAL ALIGNMENT Final Report 2000 DOE/BP-64840-4 This report was funded by the Bonneville Power Administration (BPA), U.S. Department of Energy, as part of BPA's program to protect, mitigate, and enhance fish and wildlife affected by the development and operation of hydroelectric facilities on the Columbia River and its tributaries. The views of this report are the author's and do not necessarily represent the views of BPA. This document should be cited as follows: Flagg, Thomas A., T. E. Ruehle, L. W. Harrell, J. L. Mighell, C. R. Pasley, A. J. Novotny, E. Statick, C. W. Sims, D. B. Dey, Conrad V. W. Mahnken - National Marine Fisheries Service, Seattle, WA, 2000, Cle Elum Lake Anadromous Salmon Restoration Feasibility Study: Summary of Research, 2000 Final Report to Bonneville Power Administration, Portland, OR, Contract No. 86AI64840, Project No. 86-045, 118 electronic pages (BPA Report DOE/BP-64840-4) This report and other BPA Fish and Wildlife Publications are available on the Internet at: http://www.efw.bpa.gov/cgi-bin/efw/FW/publications.cgi For other information on electronic documents or other printed media, contact or write to: Bonneville Power Administration Environment, Fish and Wildlife Division P.O. -
Wenatchee National Forest
United States Department of Agriculture Forest Service Wenatchee National Forest Pacific Northwest Region Annual Report on Wenatchee Land and Resource Management Plan Implementation and Monitoring for Fiscal Year 2003 Wenatchee National Forest FY 2003 Monitoring Report - Land and Resource Management Plan 1 I. INTRODUCTTION Purpose of the Monitoring Report General Information II. SUMMARY OF THE RECOMMENDED ACTIONS III. INDIVIDUAL MONITORING ITEMS RECREATION Facilities Management – Trails and Developed Recreation Recreation Use WILD AND SCENIC RIVERS Wild, Scenic And Recreational Rivers SCENERY MANAGEMENT Scenic Resource Objectives Stand Character Goals WILDERNESS Recreation Impacts on Wilderness Resources Cultural Resources (Heritage Resources) Cultural and Historic Site Protection Cultural and Historic Site Rehabilitation COOPERATION OF FOREST PROGRAMS with INDIAN TRIBES American Indians and their Culture Coordination and Communication of Forest Programs with Indian Tribes WILDLIFE Management Indicator Species -Primary Cavity Excavators Land Birds Riparian Dependent Wildlife Species Deer, Elk and Mountain Goat Habitat Threatened and Endangered Species: Northern Spotted Owl Bald Eagle (Threatened) Peregrine Falcon Grizzly Bear Gray Wolf (Endangered) Canada Lynx (Threatened) Survey and Manage Species: Chelan Mountainsnail WATERSHEDS AND AQUATIC HABITATS Aquatic Management Indicator Species (MIS) Populations Riparian Watershed Standard Implementation Monitoring Watershed and Aquatic Habitats Monitoring TIMBER and RELATED SILVICULTURAL ACTIVITIES Timer Sale Program Reforestation Timber Harvest Unit Size, Shape and Distribution Insect and Disease ROADS Road Management and Maintenance FIRE Wildfire Occurrence MINERALS Mine Site Reclamation Mine Operating Plans GENERAL MONITORING of STANDARDS and GUIDELINES General Standards and Guidelines IV. FOREST PLAN UPDATE Forest Plan Amendments List of Preparers Wenatchee National Forest FY 2003 Monitoring Report - Land and Resource Management Plan 2 I. -
Northeastern Washington Forest Plan Revision
NORTHEASTERN WASHINGTON FOREST PLAN REVISION REVIEW OF POTENTIALLY ELIGIBLE WILD AND SCENIC RIVERS 6/22/2011 Historical Context The Wild and Scenic Rivers Act of 1968 provides federal protection for the most outstanding of our country’s free-flowing rivers; preserving them and their immediate environments for the use and enjoyment of present and future generations. Identifying rivers is a two-step process. First, eligibility is determined based on whether the river or stream is free flowing and has one or more outstandingly remarkable values. This creates an inventory of rivers. The second step is to determine suitability. Suitability examines a number of factors such as compatibility with resources uses, impacts on non-federal lands, and the costs of land acquisition. This information informs an agency decision on whether or not to recommend designation of a river. Wild and scenic rivers can be made official (designated) in two ways. The most common way is for Congress to pass a law designating the river. Rivers can also be designated by the Secretary of the Interior when a state has passed legislation and the governor has nominated the river. Determining Eligibility To be eligible a river must be free flowing and have one or more outstandingly remarkable values (ORV). The Wild and Scenic Rivers Act defines a river as “a flowing body of water or estuary or a section, portion, or tributary thereof, including rivers, streams, creeks, runs, kills, rills, and small lakes.” The Act also defines “free-flowing”. “Free-flowing”, as applied to any river or section of a river, means existing or flowing in a natural condition without impoundment, diversion, straightening, rip-rapping, or other modification of the waterway. -
Post-Glacial Fire History of Horsetail Fen and Human-Environment Interactions in the Teanaway Area of the Eastern Cascades, Washington
Central Washington University ScholarWorks@CWU All Master's Theses Master's Theses Winter 2019 Post-Glacial Fire History of Horsetail Fen and Human-Environment Interactions in the Teanaway Area of the Eastern Cascades, Washington Serafina erriF Central Washington University, [email protected] Follow this and additional works at: https://digitalcommons.cwu.edu/etd Part of the Environmental Education Commons, Environmental Monitoring Commons, Natural Resources and Conservation Commons, Other Environmental Sciences Commons, and the Sustainability Commons Recommended Citation Ferri, Serafina, "Post-Glacial Fire History of Horsetail Fen and Human-Environment Interactions in the Teanaway Area of the Eastern Cascades, Washington" (2019). All Master's Theses. 1124. https://digitalcommons.cwu.edu/etd/1124 This Thesis is brought to you for free and open access by the Master's Theses at ScholarWorks@CWU. It has been accepted for inclusion in All Master's Theses by an authorized administrator of ScholarWorks@CWU. For more information, please contact [email protected]. POST-GLACIAL FIRE HISTORY OF HORSETAIL FEN AND HUMAN-ENVIRONMENT INTERACTIONS IN THE TEANAWAY AREA OF THE EASTERN CASCADES, WASHINGTON __________________________________ A Thesis Presented to The Graduate Faculty Central Washington University ___________________________________ In Partial Fulfillment of the Requirements for the Degree Master of Science Resource Management ___________________________________ by Serafina Ann Ferri February 2019 CENTRAL WASHINGTON UNIVERSITY Graduate Studies