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1922 Elizabeth T
co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St. -
Geomorphic Character, Age and Distribution of Rock Glaciers in the Olympic Mountains, Washington
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1987 Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington Steven Paul Welter Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Geomorphology Commons Let us know how access to this document benefits ou.y Recommended Citation Welter, Steven Paul, "Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington" (1987). Dissertations and Theses. Paper 3558. https://doi.org/10.15760/etd.5440 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. For more information, please contact [email protected]. AN ABSTRACT OF THE THESIS OF Steven Paul Welter for the Master of Science in Geography presented August 7, 1987. Title: The Geomorphic Character, Age, and Distribution of Rock Glaciers in the Olympic Mountains, Washington APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Rock glaciers are tongue-shaped or lobate masses of rock debris which occur below cliffs and talus in many alpine regions. They are best developed in continental alpine climates where it is cold enough to preserve a core or matrix of ice within the rock mass but insufficiently snowy to produce true glaciers. Previous reports have identified and briefly described several rock glaciers in the Olympic Mountains, Washington {Long 1975a, pp. 39-41; Nebert 1984), but no detailed integrative study has been made regarding the geomorphic character, age, 2 and distribution of these features. -
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 -
1968 Mountaineer Outings
The Mountaineer The Mountaineer 1969 Cover Photo: Mount Shuksan, near north boundary North Cascades National Park-Lee Mann Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during June by The Mountaineers, P.O. Box 122, Seattle, Washington 98111. Clubroom is at 7191h Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. EDITORIAL STAFF: Alice Thorn, editor; Loretta Slat er, Betty Manning. Material and photographs should be submitted to The Mountaineers, at above address, before Novem ber 1, 1969, for consideration. Photographs should be black and white glossy prints, 5x7, with caption and photographer's name on back. Manuscripts should be typed double-spaced and include writer's name, address and phone number. foreword Since the North Cascades National Park was indubi tably the event of this past year, this issue of The Mountaineer attempts to record aspects of that event. Many other magazines and groups have celebrated by now, of course, but hopefully we have managed to avoid total redundancy. Probably there will be few outward signs of the new management in the park this summer. A great deal of thinking and planning is in progress as the Park Serv ice shapes its policies and plans developments. The North Cross-State highway, while accessible by four wheel vehicle, is by no means fully open to the public yet. So, visitors and hikers are unlikely to "see" the changeover to park status right away. But the first articles in this annual reveal both the thinking and work which led to the park, and the think ing which must now be done about how the park is to be used. -
The Brothers Wilderness Air Quality Report, 2012
The Brothers Wilderness Air Quality Report Wilderness ID: 241 Wilderness Name: The Brothers Wilderness The Brothers Wilderness Air Quality Report National Forest: Olympic National Forest State: WA Counties: Jefferson General Location: Olympic Peninsula Acres: 16,337 Thursday, May 17, 2012 Page 1 of 4 The Brothers Wilderness Air Quality Report Wilderness ID: 241 Wilderness Name: The Brothers Wilderness Wilderness Categories Information Specific to this Wilderness Year Established 1984 Establishment Notes 99-635, Washington State Wilderness Act of 1984 Designation Clean Air Act Class 2 Administrative Olympic National Forest Unique Landscape Features The Brothers Wilderness is located on the eastern flanks of the Olympic National Forest just South of Buckhorn Wilderness and north of Mt. Skokomish Wilderness. Between moss- and fern-laden banks, the Dosewallips and Hamma Hamma Rivers run cold and clear north and south, respectively, of the borders of The Brothers Wilderness. At 6,866 feet, The Brothers is the highest peak in the area, with a distinct double summit that ranks among the most popular climbs in the Olympics. Through the center of the Wilderness the Duckabush River splashes down a wide and lovely glacier-carved valley shadowed by tall hemlock, fir, and cedar. From the Duckabush the terrain rises steeply into a mazelike network of forested ridges that peak on The Brothers to the south and 5,701-foot Mount Jupiter to the north. In the rain shadow of the Olympic Mountains, the area collects about 80 inches of precipitation each year, and temperatures stay temperate, rarely rising above 80 degrees Fahrenheit and seldom freezing along the river. -
The Story of Three Olympic Peaks
THE STORY OF THREE OLYMPIC PEAKS The countless thousands who. from year to year. admire the three prominent peaks at the southeastern end of the Olympic Range would find themselves gazing at the wonderfully beautiful picture with even keener rapture if they but knew a part of the history interlocked with the names these peaks bear-Ellinor. The Brothers. and Constance. There are probably no other geographical features in the Pacific Northwest whose names involve a richer history. A beautiful and tender modesty screened the identity of the personalities behind those names. while a sin gle one of the four people survived. The last of the four was gathered to her fathers two years ago. and it is now possible to learn who were the people whose names have become so well known as geographical terms. In the first place let us see when and by whom the names were given to the mountains. The most accessible source is the Pacific Coast Pilot. which says: "When a vessel is going northward. and is clear of Vashon Island. the Jupiter Hills show over Blake Island. with Mount Constance to the southward. "1 A little further on the same work says; "Behind the Jupiter Hills is Mount Constance. 7777 feet elevation; Th~ Brothers. 6920 feet. and Mount Ellinor. estimated at 6500 feet. These great masses. rising so abruptly in wild, rocky peaks. are marks all over Admiralty Inlet and Puget Sound. but seem to overhang the main part of [Hood] Canal. The Brothers. a double peak. is less than seven miles from the water."2 Similar information is given in the reports made aI the time of the surveys. -
Environmental Assessment for the Dosewallips Engineered Log Jam Project
Environmental Assessment for the United States Department of Dosewallips Agriculture Forest Service Engineered Log Jam Pacific Northwest Project Region February 2013 Olympic National Forest The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, sex, religion, age, disability, political beliefs, sexual orientation, or marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice and TTY). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326-W, Whitten Building, 1400 Independence Avenue, SW, Washington, DC 20250-9410 or call (202) 720-5964 (voice and TTY). USDA is an equal opportunity provider and employer. i Environmental Assessment for the Dosewallips Engineered Log Jam Project Table of Contents CHAPTER 1 – INTRODUCTION ........................................................................................ 1 RELATIONSHIP TO THE FOREST PLAN AND OTHER MANAGEMENT DIRECTION ....................... 1 PROJECT LOCATION ............................................................................................................... 4 BACKGROUND ...................................................................................................................... 11 PURPOSE AND NEED ............................................................................................................ -
WRIA 18 Salmonid Habitat Limiting Factors Analysis
SALMON AND STEELHEAD HABITAT LIMITING FACTORS WATER RESOURCE INVENTORY AREA 18 WASHINGTON STATE CONSERVATION COMMISSION FINAL REPORT Donald Haring 12/27/99 ACKNOWLEDGEMENTS Completion of this report would not have been possible without the support and cooperation of the Technical Advisory Group (TAG). Their expertise and familiarity with the sub-watersheds within Water Resource Inventory Area (WRIA) 18, and their interest and willingness to share their knowledge, allowed us to complete this report. Two TAGs, one for the Dungeness Watershed (Bell Creek to Bagley Creek), and one for Morse Creek to the Elwha River, were utilized through much of the information collection phase of report development, with several of the members participating in both groups. The TAG participants from both groups are consolidated in the following list: Kevin Bauersfeld Department of Fish and Wildlife Lloyd Beebe Resident, owner of Olympic Game Farm Walt Blendermann Resident, City of Sequim John Cambalik North Olympic Lead Entity Coordinator Randy Cooper Department of Fish and Wildlife Pat Crain Elwha Klallam Tribe Steve Evans Department of Fish and Wildlife Joel Freudenthal Clallam County Dick Goin Resident, City of Port Angeles Mark Haggerty U.S. Forest Service Paul Hansen Clallam Conservation District Donald Haring Conservation Commission Randy Johnson Department of Fish and Wildlife Ray Johnson Department of Fish and Wildlife Eloise Kallin Protect the Peninsula’s Future Mike McHenry Elwha Klallam Tribe Cynthia Nelson Department of Ecology Linda Newberry -
Manganese Deposits of the Olympic Peninsula,· Washington
State of Washington MON C. WALLGREN, Governor Department of Conservation and Development ART GARTON, Director DIVISION OF MINES AND MINING SHELDON L. GLOVER, Supervisor Report of Investigations . No. 7 Manganese Deposits of the Olympic Peninsula,· Washington By STEPHEN H. GREEN Olympia State Printing Plant 1945 For sale by Department of Conservation and Development, Olympia, Washington. Price, 25 cents. CONTENTS Page Foreword............................................................ 3 Introduction . 5 Fieldwork and acknowledgments. 6 Selected bibliography . 7 General production and uses of manganese. 8 Principal economic manganese minerals ............ ................. .. 10 Geology ............................................................. 11 Mineralogy . 15 Bementite . 16 Hausmannite . 17 Neotocite .................................................... 17 Inesite ...................................................... 17 Rhodochrosite .................................... : . 17 Rhodonite . 18 Minor manganese minerals. 18 Weathering products .......................................... 18 Associated minerals ....... ...... : . 18 Origin of deposits. 19 Beneficiation . 20 U.S. Government purchasing scheduLe, 1942 ............................. 24 Estimation of tonnage. 25 Distribution of known occurrences .......... : . 25 Clallam County .................................. ... ............ , 26 Pacific Coast to Lake Crescent vicinity. 26 Aw·ora Ridge area ....................................... ·..... 32 Storm King Mountain area. 33 Little -
Geologic Map of the Brinnon 7.5-Minute Quadrangle, Jefferson and Kitsap Counties, Washington
GEOLOGIC MAP OF THE BRINNON 7.5-MINUTE QUADRANGLE, JEFFERSON AND KITSAP COUNTIES, WASHINGTON by Michael Polenz, Eleanor Spangler, Logan A. Fusso, David A. Reioux, Ryan A. Cole, Timothy J. Walsh, Recep Cakir, Kenneth P. Clark, Jeffrey H. Tepper, Robert J. Carson, Domenico Pileggi, and Shannon A. Mahan WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Map Series 2012-02 December 2012 DISCLAIMER Neither the State of Washington, nor any agency thereof, 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 State of Washington or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the State of Washington or any agency thereof. INDEMNIFICATION Research supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program, under USGS award number G11AC20236. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. WASHINGTON STATE DEPARTMENT OF NATURAL RESOURCES -
WRIA 18: Elwha-Dungeness
ElWHA-DUNGENESS BASIN Water Resource Inventory Area 18 The Dungeness and Elwha rivers are the principal drain predominantly pool-riffle with few rapids and suitable ages within this basin. The Dungeness River with a total streambed for spawning and rearing of anadromous species. length of 31.9 linear miles and a watershed drainage of 198 The Elwha River originates deep in the Olympic Na square miles provides excellent spawning and rearing char tional Park from many glaciers and extends into a deep acteristics for both anadromous and resident fishes. The riv valley between the Bailey Range on the west and the Elk er's headwaters originate in the Olympic Mountains within Mountain, Mount Norton, Mount Christie, Mount Scott, national park boundaries. The mainstem Dungeness origi and Mount Barnes ranges on the east. Most of the tributary nates around the 4,000 foot level between Mount Constance headwaters originate at about the 4,000-foot elevation. De and Mount Deception and then flows northeast to the Strait spite the rugged headwater terrain, the river maintains of Juan de Fuca. The Greywolf River originates in the Nee mostly moderate gradient throughout much of its length dles Range between Mount Deception and Elk Mountain with excellent pool-riffle areas and occasional cascades and where Cameron Creek and Grand Creek also drain from ele rapids. The Elwha River contains 44.8 linear miles of total vations around 4,000 feet. The mainstem Dungeness flows stream length and 321 square miles of drainage area, but through a narrow valley and is characterized by many cas only 3.4 miles of main river above the mouth are accessible cades, falls, and rapids. -
June 2010 Penwicle
JUNE Ed Book Photography Monday, June 14, 7 pm 2010 Presented by: Ed Book Ed Book is a PWC member and past presenter, and was the PWC Artisan featured at the April PWC meeting. Ed will be sharing his photos of snow geese at the Skagit River delta in spring and the autumn oaks of Klickitat County (the best autumn color of Washington), just north of the Columbia River Gorge. The Skagit River delta serves as a wintering ground for hundreds of thousands of snow geese, trumpeter swans, and bald eagles. It's located at the north end of Puget Sound at the mouth of the Skagit River, which collects water from the northern Cascade Mountain Range and carries it to Puget Sound. Top: Snow geese wintering at Fir Island in the Skagit River delta fly in formation close to each other to reduce air resistance. Bottom: Snow geese wintering at Fir Island fly in the early morning with Whitehorse Mountain in the background. Photos courtesy of Ed Book, © edbookphoto.com Perry Avenue in East Bremerton. The public is cordially invited. is cordially The public Avenue Perry in East Bremerton. tsap Unitarian Universalist Fellowship on Fellowship Universalist Unitarian tsap Monday of every month at 7 pm at at every the month Ki Monday of Peninsula Club meets second Peninsula Wilderness on the Monthly MAP: Monthly Activity Planning Meeting & June Potluck Board Meeting Friday, June 25, 6:30 pm Thursday, June 10, 6 pm Board Meeting, 7 pm MAP Contact: Paul Dutky, 360-479-2683, [email protected] Contact: John & Ellen Knott, 360-710-1158 Visit with fellow PWCers at Paul’s home in Bremerton.