Observed and Projected Climate Changes
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GLACIERS Glacial Ice Is One of the Foremost Scenic and Scientific Values of Olympic National Park
OLYMPIC NATIONAL PARK Glaciers MOUNT OLYMPUS GLACIERS Glacial ice is one of the foremost scenic and scientific values of Olympic National Park. There are about sixty glaciers crowning the Olympics peaks; most of them are quite small in contrast to the great rivers of ice in Alaska. The prominent glaciers are those on Mount Olympus covering approximately ten square miles. Beyond the Olympic complex are the glaciers of Mount Carrie, the Bailey Range, Mount Christie, and Mount Anderson. In the company of these glaciers are perpetual snowbanks that have the superficial appearance of glacial ice. Because they are lacking in the criteria below, they are (aerial view) not true glaciers. True glaciers are structurally three layered bodies of frozen water. The top layer is snow; the middle neve, or mixed snow and ice; and the bottom layer is of pure ice, which is quite plastic in nature. Crevasses or deep cracks in the glaciers form as the ice is subjected to uneven flow over alpine terrain. Another structural feature is the bergschrund, which is a prominent crevasse-like opening at the head of the glacier where the ice has been pulled away from the mountain wall. The rate of glacial flow is quite variable, and Olympic glaciers are "slow-moving" in contrast to some in Alaska which occasionally move at the rate of several hundred feet per day for short periods of time. There is no great advance of Olympic glaciers today, but there is not a rapid melting back of the ice either. Forward surges in glacial flow often occur after a number of very heavy winters and cool summers, but such activity has been relatively infrequent with Olympic glaciers in recorded time. -
History of the Club from a to Z
, . THE KLAHHANE CLUB GOLDEN ANNIVERSARY 1965 founded in 1915 I DEDICATION To the men and women who founded this Club our sincere appreciation To future members may this Club give you the same deep contentment in the outdoors and the same abiding friendships that it has granted to its members both past and present II PREFACE The desire to explore remote places, to enjoy the out-of-doors, to conquer difficult terrain, and to share these triumphs with congenial souls, has been the motivating force behind the formation of many an outdoor club. So it has been with the Klahhane Club. From the enjoyment of our heritage of mountain, sea, and forest, comes renewed strength and a spirit of delight which carries over into our workaday world. This is an enthusiasm which may be aroused in early childhood or later in life, but once aroused, it continues to delight throughout life, even after hiking days are done. May I conclude with a quotation from Mr. Thomas Gupthill, who wrote in the first Klahhane Annual of 1918, "Favored is he who is privi- leged to join that charmed circle of congenial spirits who find inspiration and recreation in unfrequented aisle and far reaches." by Primrose Bred! III PRESIDENT'S REMARKS Klahhane or good-times-out-of-doors has meant more to me during my fifty years of membership than any other organization. Being president (usually when no one else would take it) has been only a small part of it. There is some- thing inexplainable about its lure. You leave your safe comfortable home to go and climb a mountain. -
Flattery Rocks National Wildlife Refuge
nacortes-Friday H A arbor Ferry Pe ar P oi FFrriiddaayynt Harbor y Harbor Ba r e n t a n m e r C e h s i F AAnnaaccoorrtteess 124°0'0"W 123°0'0"W n Tillicum k i l 1a a c pl 17 nd k U a ³² 1a a s c Belmont ³² r b P k a ³² p Glen J Park m y u Lake Ba * H " Luxton West Bay Y Colwood T Braemar James A Happy N Heights VViiccttoorriiaa D Bay Iceberg Valley A U t 1 Poin ³² N O S A C C Chibahdehl N Tatoosh Mushroom Slant Rocks Kydikabbit A Island U Rock Rock MIIDDWAAYY Point Koitlah British Columbia British Columbia J y Cr a Point anb Sah-da-ped-thl Warmhouse err B N y L Look- t a n k t Titacoclos CLASSET Beach Waadah i A e Through Rock CLASSET Po Albert ne Falls Island S or Cape r Head C Fuca t e Kan Archawat t gar Pillar Flattery First t oo Peak O in NEEAH Beach Second s (1308'') Bahokus re t o V C ek BAY Beach h Troxell il lage BAY Third n Peak i c W d Beach o t (1380'') R P e a B Av S A N J Y a y a w y M U A N C O U N T t r y Vie k c e c o Y IS h t T L A N C r R N D C O U N T Y t S U a ucket o O Y e d o T r l E ke C N e 14 ell ape F C N U Trox k C ³² A O re J U C e N O N W WAAAATTCCHH k S A R S d hi d Waatch F E N dbey Isla n Point E F n AS ad Hobuck J r ost Y F Beach Hobuck k a u r o Lake T e e C L C o l A y Bahobohosh r Y C A N N L A a Point L D T S T Waatch n A M A U ek a k N e O r Peak e C t ml re O Y n l M a C U T U C i Strawberry (1350') a d N C (1350') ka In u e h J N U n e T O O Fakkema B Rock R on s a Shipwreck Y N C T Y g es ati n N N e v C n r s s A e U n i U e u Point J C O d O u l N M S an J u an I sla nd s Silver Lake Sooes -
ABSTRACT SHINPAUGH, JOSHUA ERIK. Geochemical Signatures
ABSTRACT SHINPAUGH, JOSHUA ERIK. Geochemical Signatures of Potential Sediment Sources to Lake Quinault, Washington. (Under the direction of Dr. Elana Leithold). Over centennial to millennial time scales, sediment production in mountainous areas of the world is typically dominated by episodic events such as earthquakes and storms, which commonly trigger widespread mass wasting. As streams carry these sediments out of the affected catchments, downstream sites of sediment accumulation, such as lakes and continental margins, have the potential to record these erosional processes. Widespread deep- seated landsliding should produce sediments with geochemical properties similar to those of bedrock while shallow landslides should produce sediment with geochemistry reflecting larger components of soil and vegetation. Lake Quinault, on the western side of the Olympic Peninsula, sits in a landslide-prone region atop the Cascadia Subduction Zone (CSZ). Evidence for great subduction earthquakes along the CSZ with a typical recurrence interval of 300-500 years has been documented. The lake, formed behind a glacial moraine between 20,000 and 29,000 years ago, has the potential to record the geomorphic response to these events. The goal of this study was to examine recent sources of sediment in the lake’s catchment and to establish geochemical criteria by which this response might be reconstructed. Sources, including bedrock, soils, river terrace, and paleo-lacustrine sediments were sampled and their inorganic and organic geochemical signatures characterized. Stream samples were also gathered and analyzed to test applicability of source geochemistry in the determination of stream sediment derivation. Chemical Index of Alteration (CIA) and Weathering Index of Parker (WIP) values were calculated from inorganic geochemical data. -
Major Revisions to the Basic Climbs Guide for 2010
Major revisions to the Basic Climbs Guide for 2010. ¾ Jurisdiction web site links added ¾ Guide book references updated and new guide books added. Please remember… your safety depends on your preparedness and your ability and willingness to make good decisions! Here is the list of references: Cascade Alpine Guide, vols. I (2000), II (2003) & III (2008) - Becky Selected Climbs in the Cascades vol. I (2003) & *vol. II (2000) – Nelson/Potterfield Olympic Mountains: A Climbing Guide, 4th ed (2006). (This is a revision of “Climber’s Guide to the Olympic Mountains” (1988).) – Olympic Mountain Rescue Classic Climbs of the Northwest (2002) - Kearney *Summit Routes – Washington’s 100 Highest Peaks (2004) – Stephenson/Bongiovanni *Mt Rainier: a climbing guide (2005) - Gauthier (head climbing ranger at MRNP.) *Washington’s Highest Mountains – Basic Alpine & Glacier Routes (2004) – Goldman (This guide has GPS waypoints.) *Alpine Select – Climbs in SW British Columbia and N Washington (2001) - McLane * These references are new to the Basic Climbs Guide. ¾ Route Descriptions revisions: Mt Anderson/Anderson Glacier: 1) changed back to glacier route for Basic Course credit. Anderson glacier is way down but this route travels on the Eel Glacier also. 2) Mileage added to approach due to road washout. Description altered to a 3-day trip. Mt Constance approach has mileage added due to road washout. Mt Hood/South Side: conditions just above the hogsback have deteriorated. The “old chute” route is now listed. Slippery Slab: The approach listed here-to-fore -
WRIA 16 Final Report.Doc
Hydrogeologic Study of the Lower Dosewallips/Brinnon Area Prepared for: WRIA 16 Planning Unit Funding Source: WRIA 16 Base Grant, Department of Ecology Grant #G9900020 As pectconsulti ng IN-DEPTH PERSPECTIVE 179 Madrone Lane North 811 First Avenue #480 Bainbridge Island, WA 98110 SeaUle, WA 98104 (206) 780-9370 (206)-328-7443 Project No. 0301 16-001-05 - March 30, 2005 HYDROGEOLOGIC STUDY OF THE LOWER DOSEWALLIPS/BRINNON AREA Prepared for: WRIA 16 Planning Unit Funding Source: WRIA 16 Base Grant, Department of Ecology Grant #G9900020 Project No. 030116-001-05 • March 30, 2005 Aspect Consulting, LLC Erick W. Miller tEXP1REs 02J011or- Erick W. Miller, LHG Joseph S. Lubischer, P.E. Senior Associate Hydrogeologist Project Engineer [email protected] [email protected] W:\030116 WRIA 16\FinaJ Report\WRIA 16 Final Report.doc ~79 Madrone Lane North •• ASPECT CONSULTING Contents Executive Summary........................................................................................... 1 1 Introduction ................................................................................................ 3 1.1 Background .................................................................................................. 3 1.2 Overview of Dosewallips Basin.................................................................... 3 1.3 Purpose and Scope...................................................................................... 5 2 Geologic Conditions and Basin Glaciation .............................................. 6 2.1 Previous -
PGST Climate Impact Assessment Report 0518 FINAL
E PORT GAMBLE S’KLALLAM TRIBE | CLIMATE CHANGE IMPACT ASSESSMENT ACKNOWLEDGMENTS PAGE 2 PORT GAMBLE S’KLALLAM TRIBE | CLIMATE CHANGE IMPACT ASSESSMENT ACKNOWLEDGMENTS PAGE 3 PORT GAMBLE S’KLALLAM TRIBE | CLIMATE CHANGE IMPACT ASSESSMENT ACKNOWLEDGMENTS This assessment would not have been possible without the tremendous contributions of many individuals, listed below. Project team Paul McCollum, Natural Resources Director Hans Daubenberger, Principal Habitat Biologist Samuel Phillips, Environmental Scientist Special thanks to the following Tribal staff and partners Roma Call, Environmental Program Manager Ahmis Loving, Loving Engineering & Consulting, P.S. Inc. Laurie Mattson, Interim Health Director Kerstin Powell, Health Services Manager Joe Sparr, Planning Director Sam White, Police Chief Josh Wisniewski, Anthropologist Tim Cullinan, Thom Johnson, Ryan Murphy, Cynthia Rossi, and Austin Paul from the Point No Point Treaty Council We are also grateful for the contributions of our expert reviewers and interviewees Tim Beechie Tim Cullinan Lisa Crozier Joth Davis Austin Paul David Peterson Thanks to the following for their regional coordination efforts around these issues Eliza Ghitis, Northwest Indian Fisheries Commission Kathy Lynn, Tribal Climate Change Project Prepared for the Port Gamble S’Klallam Tribe by Cascadia Consulting Group University of Washington Climate Impacts Group Recommended Citation Format Port Gamble S’Klallam Tribe Natural Resources Department. 2016. Climate Change Impact Assessment. A collaboration of the Port Gamble -
Voice of the Wild Olympics, Winter 2014
VOICE of the WILD OLYMPICS Olympic Park Associates Founded in 1948 Volume 22 Number 1 Winter 2013-2014 Contents Book Reviews: Ascendance 3 Katie Gale 11 Remembrances: 4 Patrick Goldsworthy Phil Zalesky Update: Wild Olympics Campaign 5 Ancient Temperate Rainforest in the South Quinault Ridge Proposed Wilderness, Olympic National Forest. Wilderness Gifts: Water 6 Photo from Wild Olympics Campaign Olympic National Park’s Vanishing Glaciers 7 Olympics Bill Introduced in Congress Citizen Science: Marmot Survey 8 Senator Murray and Representative Kilmer Update: Team Up to Protect Olympic Wildlands & Rivers Spotted Owls Decline 9 In January OPA joined conservationists Popular roadless areas that would receive OPA’s New Trustees 10 across the Northwest celebrating the intro- wilderness protection in the legislation include: duction of the Wild Olympics Wilderness Deer Ridge, Lower Graywolf, Upper Dunge- Celebrate and Wild and Scenic Rivers Act of 2014. ness, Mount Townsend North, Dosewallips Wilderness Act’s 50th The bill, similar to the one introduced and Jupiter Ridges, Mounts Ellinore and with Great Old Broads 10 by Senator Murray and Representative Washington, South Fork Skokomish River, Dicks in 2012, would permanently pro- Moonlight Dome, South Quinault Ridge, Rug- Federal Closures: tect more than 126,000 acres of new Impacts on Peninsula 11 wilderness in Olympic National Forest. ged Ridge, and Gates of the Elwha. OPA and In addition, it would also protect 19 Wild our sister conservation organizations have Poem: and Scenic Rivers in the national forest and been working to protect most of these areas Plunging into the Wild 12 the national park, the first ever designated for decades. -
GLACIERS Glacial Ice Is One of the Foremost Scenic and Scientific
GLACIERS Glacial ice is one of the foremost scenic and the Mount Olympus complex of glaciers scientific values of Olympic National Park. which receive the full impact of Pacific storms. The average annual precipitation is There are about sixty glaciers crowning the about two hundred inches; most of the mois Olympics peaks; most of them are quite ture coming in the form of snow. Snow nur small in contrast to the great rivers of ice in tures the glaciers in the accumulation zone Alaska. The prominent glaciers are those or at the origin of the ice. Most of the melt on Mount Olympus covering approximately ing or ablation occurs near the termini or ten square miles. Beyond the Olympic com snouts of the glaciers. As with human plex are the glaciers of Mount Carrie, the finance management, glaciers work with a Bailey Range, Mount Christie, and Mount budget and expenditure plan. A vigorous Anderson. In the company of these glaciers glacier will be maintained by a heavy ac are perpetual snowbanks that have the su cumulation of snow in the winter and only perficial appearance of glacial ice. Because average melting during the summer. The they are lacking in the criteria below, they freezing point in late spring and precipita are not true glaciers. tion in early fall appear to be critical items in relation to this gain and loss. Excessive True glaciers are structurally three layered melt before and after the normal melt bodies of frozen water. The top layer is season would result in an impoverished snow; the middle neve, or mixed snow and budget for the following year. -
References Cited
References Cited Abercrombie, W.R., 1900, Supplementary expedition into the Armentrout, J.M., 1983, Glacial lithofacies of the Neogene Yakata- Copper River Valley, Alaska, in Compilation of narratives of ga Formation, Robinson Mountains, southern Alaska, Coast explorations in Alaska, part A: Washington, D.C., Government Range, in Molnia, B.F., ed., 1981, Glacial-marine sedimenta- Printing Office, 169 p. tion: New York, Plenum Press, p. 629–665. Aðalgeirsdóttir, G., Echelmeyer, K.A., and Harrison, W.D., 1998, Bagley, J.W., 1917, The use of the panoramic camera in topograph- Elevation and volume changes on the Harding Icefield, Alaska: ic surveying: U.S. Geological Survey Bulletin 657, 88 p. Journal of Glaciology, v. 44, 148, p. 570–582. Bahr, D.B., 1997, Global distributions of glacier properties: A sto- Allen, C.R., and Smith, G.I., 1953, Seismic and gravity investiga- chastic scaling paradigm: Water Resources Research, v. 33, tions on the Malaspina Glacier, Alaska: Transactions, Ameri- no. 7, p. 1669–1679. can Geophysical Union, v. 34, no. 5, p. 755–760. Bahr, D.B. and Meier, M.F., 2000, Snow patch and glacier size dis- Allen, H.T., 1887, Report of an expedition to the Copper, Tanana, tribution: Water Resources Research, v. 36, no. 2, p. 495–501. and Koyukuk Rivers, in the Territory of Alaska, in the year Bailey, Palmer, Fleisher, P.J., Mankoff, Evan, and Senglaub, Mi- 1885, for the purpose of obtaining all information which will chael, 2000, An evolving ice-contact proglacial lake, Sheridan be valuable and important, especially to the military branch of Glacier, Alaska [abs.]: Geological Society of America, Ab- the government: Washington, D.C., Government Printing Of- stracts with Programs, v. -
WASHINGTON UNITED STATES Historic Events DEPARTMENT of the INTERIOR Olympic 1774 Juan Perez, Roving Spanish Sea Cap Harold L
0 NATIONAL PARK - WASHINGTON UNITED STATES Historic Events DEPARTMENT OF THE INTERIOR Olympic 1774 Juan Perez, roving Spanish sea cap Harold L. Ickes, Secretary tain, first white man to sight Olympic Mountains, which he named Santa OPEN NATIONAL PARK Rosalia. ALL WASHINGTON YEAR 1788 John Mears, British sea captain, named the highest peak Mount Olympus. WINDING HIGHWAY LAKE CRESCENT. NATIONAL PARK SERVICE Newton B. Drury, Director 1880 Earliest explorations made. LYMPIC NATIONAL PARK FORESTS coj\TEj\rs 1904 Bill to establish national park intro is a wilderness empire rich with duced in Congress, but failed of pas O One of the finest remaining areas of sage. evergreen forests, alpine mead virgin forest, Olympic National Park Mount Olympus (Photo by Wm. ows gaily sprinkled with fragrant wild- presents a splendid example of the flowers, snowcapped mountains, azure original forests of the Northwest in O. Thorniley) Cover lakes, lazily winding rivers, and ani 1909 President Theodore Roosevelt by proc the dense growth which covers the Forests 3 lamation established Mount Olympus mals which roam the forests and val mountain slopes and valley floors. National Monument of 620,000 acres. leys. "Rain Forests" 4 The region, extending from 300 to This unspoiled primeval wilderness 1,500 feet in elevation, is comprised of The Olympic Mountains . 4 is destined to be preserved as America's densely forested valleys. Most abundant 1912-1929 Area of monument reduced to "last frontier," yet it is easily accessible trees are Douglas fir, western hemlock, Wildlife Sanctuary .... 5 322,000 acres through withdrawals by Presidential proclamation. to the most inexperienced park visitor. -
Detrital Zircon Geochronology and Vitrinite Reflectance Analysis of the Cascadia Subduction Complex, Washington Peter Mahony
Detrital Zircon Geochronology and Vitrinite Reflectance Analysis of the Cascadia Subduction Complex, Washington Peter Mahony Advisor: Mark Brandon Second Reader: Alan Rooney May 2, 2018 A Senior Thesis presented to the faculty of the Department of Geology and Natural Geology, Yale University, in partial fulfillment of the Bachelors Degree. In presenting this thesis in partial fulfillment of the Bachelor’s Degree from the Department of Geology and Geophysics, Yale University, I agree that the department may make copies or post it on the departmental website so that others may better understand the undergraduate research of the department. 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 financial gain is not allowed without my written consent. Peter W. Mahony, 2 May 2018 1. Abstract: The Cascadia subduction zone, which presently spans some 1,300 km along the western continental margin of the Pacific Northwest, was initiated ~35 Ma ago. A subduction complex has grown above this subduction zone, due to convergence (30-40 km/Ma) and accretion of the ~2 km-thick sedimentary cover of the subducting offshore plate (Farallon/Juan de Fuca). The result has been a gradual uplift of the Pacific Northwest coast. The Olympic Mountains in Washington State was the first part of the Cascadia subduction complex to emerge above sea level and is the most deeply eroded part of the Cascadia subduction complex (Brandon et al. 1998). Thus, this region provides a unique opportunity to study the accretionary evolution of the Cascadia margin.