Draft Lake Chelan Subbasin Summary
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Stehekin River Classification
Stehekin Wild & Scenic River Eligibility Report FINAL DRAFT May 2002 Acknowledgments . The National Park Service gratefully acknowledges the support and assistance of the U.S. Forest Service Wenatchee and Okanogan National Forests – their assistance was critical in this report’s development. Special thanks also to the staff at the North Cascades National Park for helping to make the field work a very pleasant and informative experience. Executive Summary This study report evaluates the eligibility and classification of the Stehekin River watershed, located in the North Cascades Mountains of Washington State, as a component of the National Wild and Scenic Rivers System (National System). This evaluation is done partially in settlement of a cause of action brought by the North Cascades Conservation Council1, but primarily as a Department of the Interior requirement for normal management planning processes. The Stehekin River and its tributaries constitute a comparatively small watershed. Most of the natural and cultural resources found in the watershed are dependent not just on the main stem of the Stehekin River, but also on its tributaries. There is also no clear demarcation between most resources throughout the watershed. For these reasons, it is appropriate to consider the entire Stehekin River system as a single unit for the purposes of this evaluation, with the exception of classifying segments of the river as described later. Under the Wild and Scenic Rivers Act (Act), the river must meet physical requirements (eligibility). These physical requirements are: 1) the river must be free-flowing; and 2) the river must have at least one resource important or unique to the region or nation. -
The Mountaineer Annual
The Mountaineer Annual 1991-1992 The MountaineerAnnual 1991-1992 Volume 79 Published August, 1993 2 TheMountaineer Annual Beargrass on Mt. Rainier Steve Johnson The Mountaineers Purposes To explore and study the mountains, forests and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of Northwest America; To make expeditionsinto theseregions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor life. Ascending Eldorado Royce Conrad 4 The Mountaineer Annual The MountaineerAnnual The continuing spirit of The Mountaineers shines through in this newest edition of The Mountaineer Annual. Thank you to all the creative people who so willingly gave their time and talent in producing this book. EditorialCommittee Judi Maxwell- Editor; Production Manager; Layout Ann Marshall -Assistant Editor Steve Johnson -Computer Editor; Mailing Fran Troje -Advertising Manager Mike Buettner- Editorial Committee George Potratz- Desktop Publishing (Communications Manager) Helen Cherullo and Marge Mueller- Production Consultants (Mountaineers Books) Virginia Felton - Executive Director Katrina Reed-Administrative Assistant Eileen Allen - Accounting Manager Steve Costie -Member Services Manager Cover Design: Judi Maxwell and Helen Cherullo Cover Photographs: Front -Ascent of Eldorado © Photo by John Roper Back- Friends in High Places © Photo by Julie Smith © 1993 by The Mountaineers All Rights Reserved Published by The Mountaineers 300Third Avenue West Seattle, Washington 98119 Printedin the United States of America Printed on recycled paper Contents The Mountaineers Purposes 3 Foreword 8 Don Heck Vision for the Twenty-First Century 11 Dianne Hoff Development of a Wilderness Ethics Policy 14 Edward M. -
The Wild Cascades
THE WILD CASCADES October-November 1969 2 THE WILD CASCADES FARTHEST EAST: CHOPAKA MOUNTAIN Field Notes of an N3C Reconnaissance State of Washington, school lands managed by May 1969 the Department of Natural Resources. The absolute easternmost peak of the North Cascades is Chopaka Mountain, 7882 feet. An This probably is the most spectacular chunk abrupt and impressive 6700-foot scarp drops of alpine terrain owned by the state. Certain from the flowery summit to blue waters of ly its fame will soon spread far beyond the Palmer Lake and meanders of the Similka- Okanogan. Certainly the state should take a mean River, surrounded by green pastures new, close look at Chopaka and develop a re and orchards. Beyond, across this wide vised management plan that takes into account trough of a Pleistocene glacier, roll brown the scenic and recreational resources. hills of the Okanogan Highlands. Northward are distant, snowy beginnings of Canadian ranges. Far south, Tiffany Mountain stands above forested branches of Toats Coulee Our gang became aware of Chopaka on the Creek. Close to the west is the Pasayten Fourth of July weekend of 1968 while explor Wilderness Area, dominated here by Windy ing Horseshoe Basin -- now protected (except Peak, Horseshoe Mountain, Arnold Peak — from Emmet Smith's cattle) within the Pasay the Horseshoe Basin country. Farther west, ten Wilderness Area. We looked east to the hazy-dreamy on the horizon, rise summits of wide-open ridges of Chopaka Mountain and the Chelan Crest and Washington Pass. were intrigued. To get there, drive the Okanogan Valley to On our way to Horseshoe Basin we met Wil Tonasket and turn west to Loomis in the Sin- lis Erwin, one of the Okanoganites chiefly lahekin Valley. -
Review Article Magma Loading in the Southern Coast Plutonic Complex, British Columbia and Washington
GeoScienceWorld Lithosphere Volume 2020, Article ID 8856566, 17 pages https://doi.org/10.2113/2020/8856566 Review Article Magma Loading in the Southern Coast Plutonic Complex, British Columbia and Washington E. H. Brown Department of Geology, Western Washington University, USA Correspondence should be addressed to E. H. Brown; [email protected] Received 2 May 2020; Accepted 22 September 2020; Published 10 November 2020 Academic Editor: Tamer S. Abu-Alam Copyright © 2020 E. H. Brown. Exclusive Licensee GeoScienceWorld. Distributed under a Creative Commons Attribution License (CC BY 4.0). The southen end of the 1800 km long Coast Plutonic Complex (CPC), exposed in the Harrison Lake area of British Columbia and in the North Cascades of Washington, bears a record of great crustal thickening -20 to 40 km in localized zones during Late Cretaceous times. During this period, the CPC was positioned at the continental margin during collision/subduction of the Farallon plate. Arc magmatism and regional orogenic contraction were both active as potential crustal thickening processes. Magmatism is favored in this report as the dominant factor based on the delineation of four spatially and temporally separate loading events, the close association of the loaded areas with emplacement of large plutons, and a paucity of evidence of deep regional tectonic contraction. The timing and spatial location of crustal loading events are documented by the following: zircon ages in plutons; an early event of low pressure in pluton aureoles evidenced by andalusite, now pseudomorphed by high- pressure minerals; high pressures in country rock in pluton aureoles measured by mineral compositions in the assemblages garnet-biotite-muscovite-plagioclase and garnet-aluminum silicate-plagioclase; high pressures recorded in plutons by Al-in- hornblende barometry; and uplift ages of plutons derived from K-Ar and Ar-Ar ages of micas and hornblende in plutons. -
A Geochemical Study of the Riddle Peaks Gabbro, North Cascades: Evidence for Amphibole Accumulation in the Mid-Crust of an Arc
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship 2014 A geochemical study of the Riddle Peaks gabbro, North Cascades: evidence for amphibole accumulation in the mid-crust of an arc Angela C. Cota Western Washington University Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Cota, Angela C., "A geochemical study of the Riddle Peaks gabbro, North Cascades: evidence for amphibole accumulation in the mid-crust of an arc" (2014). WWU Graduate School Collection. 362. https://cedar.wwu.edu/wwuet/362 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]. A GEOCHEMICAL STUDY OF THE RIDDLE PEAKS GABBRO, NORTH CASCADES: EVIDENCE FOR AMPHIBOLE ACCUMULATION IN THE MID CRUST OF AN ARC By Angela C. Cota Submitted for Partial Completion Of the Requirements for the Degree Master of Science Kathleen L. Kitto, Dean of the Graduate School ADVISORY COMMITTEE Chair, Dr. Susan DeBari Dr. Elizabeth Schermer Dr. Robert Miller 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 nonexclusive 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. I represent and warrant this is my original work, and does not infringe or violate any rights of others. -
Lake Chelan Basin Overview View ‘Up-Lake’ of 90 Km (50 Mile) Long, 453 M (1486 Ft.) Deep Lake Chelan
J. Riedel Contributions to the 2018 Pacific Northwest Friends of the Pleistocene Field Conference Stop 1.2: Lake Chelan Basin Overview View ‘up-lake’ of 90 km (50 mile) long, 453 m (1486 ft.) deep Lake Chelan. There are three basins comprising Lake Chelan separated by bedrock sills: Stehekin, Lucerne, and Wapato (Figure 2). The Lucerne Basin is the deepest and longest, with relief of > 3200 m (10,660 000 ft.) from the bedrock floor of the valley to the summit of Bonanza Peak (2900 m) on its west valley wall (Figure 2). The shallower Wapato Basin is in part dammed by glacial drift south of Chelan (Stop 1.4; Runner 1921). Figure 1. Location of Lake Chelan in north-central Washington. Blue arrows at top indicate Fisher and Rainy passes, where Cordilleran Ice Sheet entered Chelan watershed. Waitt (2017) noted the ice sheet was 760 m thick over Rainy Pass. Figure 2. Longitudinal profile of the bottom of Lake Chelan (top) and seismic profiling of sub-bottom (UW and NPS unpublished). The Lucerne and Stehekin basins are superimposed on resistant Skagit Gneiss and Tertiary igneous bedrock. The upper part of the valley is cut into resistant gneiss, which allows the canyon walls to stand near vertically along the upper lake. The deepest part of Lake Chelan occurs in the Lucerne Basin in The Straits near Falls Creek, where the bedrock changes from gneiss to erodible volcanic rocks and schist. The lower two basins are separated at the Narrows, an accumulation of landslide debris from Slide Ridge on the south shore, and bedrock on the north shore (Whetten, 1967). -
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. -
Lower Stehekin River Cutthroat and Rainbow Trout Spawning Surveys, 2009
National Park Service U.S. Department of the Interior Natural Resource Program Center Lower Stehekin River cutthroat and rainbow trout spawning surveys, 2009 Natural Resource Data Series NPS/NOCA/NRDS—2010/111 ON THE COVER Surveyor stands by a Rainbow Trout Redd. Photograph by: North Cascades National Park Lower Stehekin River cutthroat and rainbow trout spawning surveys, 2009 Natural Resource Data Series NPS/NOCA/NRDS—2010/111 Hugh Anthony and Reed Glesne North Cascades National Park Service Complex 810 State Route 20 Sedro-Woolley, WA. 98284 November 2010 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics 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 Data Series is intended for timely release of basic data sets and data summaries. Care has been taken to assure accuracy of raw data values, but a thorough analysis and interpretation of the data has not been completed. Consequently, the initial analyses of data in this report are provisional and subject to change. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. This report received informal peer review by subject-matter experts who were not directly involved in the collection, analysis, or reporting of the data. -
Low Impact Hydropower Institute Re-Certification Application Lake
Low Impact Hydropower Institute Re-certification Application Lake Chelan Hydroelectric Project (FERC No. 637) Public Utility District No. 1 of Chelan County August 30, 2018 1 Contents Part 1. Facility Description ............................................................................................................. 3 The Lake Chelan Hydroelectric Project, FERC Project No. 637. .................................................. 3 Part 2. Standards Matrices ............................................................................................................ 15 2.1 Zone of Effect 1 – Lake Chelan .......................................................................................... 15 Table 1 – Zone of Effect 1 ..................................................................................................... 15 2.2 Zone of Effect 2 – Reaches 1, 2, and 3 of the Chelan River ............................................... 28 Table 2 – Zone of Effect 2 ..................................................................................................... 28 2.3 Zone of Effect 3 – Reach 4 of the Chelan River ................................................................. 39 Table 3 – Zone of Effect 3 ..................................................................................................... 39 2.4 Zone of Effect 4 – Lake Chelan Project Tailrace ................................................................ 51 Table 4 – Zone of Effect 4 .................................................................................................... -
GEOLOGIC MAP of the CHELAN 30-MINUTE by 60-MINUTE QUADRANGLE, WASHINGTON by R
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-1661 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE CHELAN 30-MINUTE BY 60-MINUTE QUADRANGLE, WASHINGTON By R. W. Tabor, V. A. Frizzell, Jr., J. T. Whetten, R. B. Waitt, D. A. Swanson, G. R. Byerly, D. B. Booth, M. J. Hetherington, and R. E. Zartman INTRODUCTION Bedrock of the Chelan 1:100,000 quadrangle displays a long and varied geologic history (fig. 1). Pioneer geologic work in the quadrangle began with Bailey Willis (1887, 1903) and I. C. Russell (1893, 1900). A. C. Waters (1930, 1932, 1938) made the first definitive geologic studies in the area (fig. 2). He mapped and described the metamorphic rocks and the lavas of the Columbia River Basalt Group in the vicinity of Chelan as well as the arkoses within the Chiwaukum graben (fig. 1). B. M. Page (1939a, b) detailed much of the structure and petrology of the metamorphic and igneous rocks in the Chiwaukum Mountains, further described the arkoses, and, for the first time, defined the alpine glacial stages in the area. C. L. Willis (1950, 1953) was the first to recognize the Chiwaukum graben, one of the more significant structural features of the region. The pre-Tertiary schists and gneisses are continuous with rocks to the north included in the Skagit Metamorphic Suite of Misch (1966, p. 102-103). Peter Misch and his students established a framework of North Cascade metamorphic geology which underlies much of our construct, especially in the western part of the quadrangle. Our work began in 1975 and was essentially completed in 1980. -
Lake Chelan, Chelan River, Washington
Hydropower Reform Coalition Success Story LAKE CHELAN, CHELAN RIVER, WASHINGTON BALANCE IN LAKE CHELAN LEVELS Lake level management will protect against erosion at Stehekin Flats, control woody debris and riparian vegetation while maintaining local photo courtesy of recreation and tourism Chelan PUD industries NEW FLOWS IN THE CHELAN RIVER Minimum fl ows for fi sh habitat and special whitewater releases in the Chelan River photo courtesy of USGS A COMPREHENSIVE PLAN FOR LAKE CHELAN FISHERIES Watershed-wide improvements to Lake Chelan’s fi shery, including the removal of alluvium barriers in lake photo courtesy of tributaries and habitat National Park enhancements Service FERC PROJECT NUMBER: P-637 PROJECT OWNER: Chelan County PUD LAKE CHELAN PROJECT GENERATING CAPACITY: 59.2 MW PROJECT FIRST LICENSED: May 8, 1926 Chelan River, Washington SETTLEMENT ACHIEVED: October 8, 2003 CURRENT LICENSE ISSUED: November 6, 2006 LICENSE EXPIRATION DATE: October 31, 2056 Lake Chelan is a freshwater ord, a lake carved by ancient glaciers. At 1,500 feet deep and FEDERAL LANDS INUNDATED BY THE PROJECT: 361.4 55 miles long, it is the third deepest lake in the United States, and the longest and deepest acres (Wenatchee National Forest) and 104.1 acres lake in the state of Washington. The Chelan River, the lake’s outlet, fl ows four miles into the (Lake Chelan National Recreation Area of North Cascades National Park) Columbia River. Over a century ago, the Chelan River’s fl ows varied by a factor of ten: from 640 cfs in the winter to 6,400 cfs in late spring freshets. KEY SETTLEMENT SIGNATORIES AND SUPPORTERS: • Chelan County PUD (dam owner) Beginning in 1892, companies began to build dams at the outlet to raise and control Lake • Federal agencies: U.S. -
Geologic Map of the North Cascade Range, Washington by Ralph A
Prepared in cooperation with Washington State Division of Geology and Earth Resources, U.S. National Park Service, and U.S. Forest Service Geologic Map of the North Cascade Range, Washington By Ralph A. Haugerud and Rowland W. Tabor Nontechnical pamphlet to accompany Scientific Investigations Map 2940 Looking south from the North Klawatti Glacier [Mbse]. In the right foreground, the glacier breaks into a heavily crevassed icefall where it descends steeply. Rock in the foreground knob is Eldorado Orthogneiss (unit TKgo), a 90 million-year-old stitching pluton, which here includes numerous dikes of light- colored pegmatite. Mount Buckner on the left skyline and Mount Forbidden hidden in clouds are also eroded from the Eldorado Orthogneiss (photographed in 1987). 2009 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction.....................................................................................................................................................1 Using this report ....................................................................................................................................1 Map preparation ...................................................................................................................................1 Major sources of new data .................................................................................................................1 Acknowledgments ................................................................................................................................2