Mount Rainier National Park, Washington
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Mount Rainier National Park, WASHINGTON TEP~RJ\ ~EF's ' in Mount Rainier National Park
PUMICE AND OTHER PYROCLASTIC DEPOSITS IN Mount Rainier National Park, WASHINGTON TEP~RJ\ ~EF's ' in Mount Rainier National Park. Pumice and scoria layers from Mount Rainier volcano (note layers R, L, D, and C) typically are stained to fairly strong brown or reddish brown; interbedded lithic ash deposits have relatively neutral but somewhat darker brownish-gray colors. Ash beds from other volcanoes (note beds marked 0, set Y, set P, and WI characteristically are lighter in color than the locally derived deposits that enclose them. S1te is in an alpine meadow near Williwakas Glacier on the southeast flank of Mount Ramier . PUMICE AND OTHER PYROCLASTIC DEPOSITS IN Mount Rainier National Park, WASHINGTON By Donal R. Mullineaux 254924 GEOLOGICAL SURVEY BULLETIN 1326 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 74-600110 U.S. GOVERNMENT PRINTING OFFICE -1974 For sale by the Superintendent of· Documents, U.S. Government Printing Office, Washington, D.C. 20402- Price $1.35 (paper cover) Stock Number 2401-02550 Contents Page Abstract.................................................. 1 Introduction . 2 Previous work and acknowledgments . 4 Terminology . 6 General setting . 8 Brief description of tephra deposits . 8 Postglacial activity of Mount Rainier . 15 Eruptive history ........................ c............. 15 Volume............................................... 18 Kinds of eruptions . 18 Hazards from future eruptions of tephra . 21 Kinds of hazards . 21 Location . 22 Warning.............................................. 23 Ages of tephra layers and their use as marker beds . 23 Tephra from distant volcanoes . 27 Tephra layer 0 (Mazama ash) . 27 Distribution, thickness, and grain size . 29 Source and age . -
Itinerary: Mt. Rainier Loop
Itinerary: Mt. Rainier Loop Length: 78 miles Time to Allow: 4-5 hours Open Season: The route is usually snow-free by mid-June and remains open through late October. The road closes each year due to winter snowfall from November to early June. Driving Directions: From Packwood, travel northwest on Forest Road (FR) 52, also called Skate Creek Road, 23 miles to State Route (SR) 706. Turn right on SR 706 and travel east 41.9 miles into Mount Rainier National Park to SR 123. Turn right on SR 123 and travel south 5.4 miles to US Highway 12. Turn right on US Highway 12 and travel 7.3 miles west back to Packwood. Experience the grandeur of Mount Rainier, old-growth temperate rainforest, waterfalls, and impressive vistas! An excellent introduction to Mount Rainier National Park. Start: Begin this mountain adventure in the rural mountain community of Packwood located on Highway 12. Restaurants, car services, lodging, and campgrounds are available. Stop 1: Skate Creek Nestled deep in the forest, watch bubbling Skate Creek as you drive its namesake road. Along this winding, paved, but primitive road, see countless waterfalls cascade along the roadside. See blankets of drooping mosses and experience the beauty and serenity of this little gem. Memorable fall color displays have earned this road the honor of “Best Sunday Drive in Lewis County for Fall Color”. In the wintertime, this road is closed to vehicle traffic and the Skate Creek Sno-Park becomes a popular destination for the snowmobiling crowds. Stop 2: Nisqually Entrance Welcoming visitors to Mount Rainier National Park at the Nisqually Entrance stands a wooden entrance arch built in 1922 and reconstructed in 1973. -
Outline for Thesis
THESIS APPROVAL The abstract and thesis of Thomas H. Nylen for the Master of Science in Geology presented October 25, 2001, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: _______________________________________ Andrew G. Fountain, Chair _______________________________________ Scott F. Burns _______________________________________ Christina L. Hulbe _______________________________________ Keith S. Hadley Representative of the Office of Graduate Studies DEPARTMENTAL APPROVAL: _______________________________________ Michael L. Cummings, Chair Department of Geology ABSTRACT An abstract of the thesis of Thomas H. Nylen for the Master of Science in Geology presented October 25, 2001. Title: Spatial and Temporal Variations of Glaciers (1913-1994) on Mt. Rainier and the Relation with Climate Databases have been constructed for the purpose of studying glacier changes at Mt. Rainier. Glacier cover on Mt. Rainier decreased 18.5% (112.3 km2 to 88.1 km2) between 1913 and 1971 at a rate of about -0.36 km2 a-1. The total area in 1994 was 87.4 km2, which equates to a rate of -0.03 km2 a-1 since 1971. Glaciers with southerly aspect lost significantly more area than those with a northerly aspect, 26.5% and 17.5% of the total area, respectively. Measured and estimated total volumes for Mt. Rainier glaciers also decreased. From 1913 to 1971 the total volume decreased 22.7% from 5.62 km3 to 4.34 km3 and from 1971 to 1994 decreased 3.1% to 4.21 km3. Nisqually Glacier shows three cycles of retreat and advance but an overall loss of 0.44 km2 since 1931. Cross-correlation with snowfall suggests about a decade response time for the glaciers. -
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. -
TREATY with the NISQUALLI, PUYALLUP, ETC., 1854. Dec
TREATY WITH THE NISQUALLI, PUYALLUP, ETC., 1854. Dec. 26, 1854. | 10 Stat., 1132. | Ratified Mar. 3, 1855. | Proclaimed Apr. 10, 1855. Articles of agreement and convention made and concluded on the She-nah-nam, or Medicine Creek, in the Territory of Washington, this twenty-sixth day of December, in the year one thousand eight hundred and fifty-four, by Isaac I. Stevens, governor and superintendent of Indian affairs of the said Territory, on the part of the United States, and the undersigned chiefs, head-men, and delegates of the Nisqually, Puyallup, Steilacoom, Squawskin, S’’Homamish, Stehchass, T’’ Peek-sin, Squi-aitl, and Sa-heh-wamish tribes and bands of Indians, occupying the lands lying round the head of Puget’’s Sound and the adjacent inlets, who, for the purpose of this treaty, are to be regarded as one nation, on behalf of said tribes and bands, and duly authorized by them. ARTICLE 1. The said tribes and bands of Indians hereby cede, relinquish, and convey to the United States, all their right, title, and interest in and to the lands and country occupied by them, bounded and described as follows, to wit: Commencing at the point on the eastern side of Admiralty Inlet, known as Point Pully, about midway between Commencement and Elliott Bays; thence running in a southeasterly [*662] direction, following the divide between the waters of the Puyallup and Dwamish, or White Rivers, to the summit of the Cascade Mountains; thence southerly, along the summit of said range, to a point opposite the main source of the Skookum Chuck Creek; thence to and down said creek, to the coal mine; thence northwesterly, to the summit of the Black Hills; thence northerly, to the upper forks of the Satsop River; thence northeasterly, through the portage known as Wilkes’’s Portage, to Point Southworth, on the western side of Admiralty Inlet; thence around the foot of Vashon’’s Island, easterly and southeasterly, to the place of beginning. -
Directions Seattle to Mt Rainier
Directions Seattle To Mt Rainier When Mic symmetrise his palmettoes grangerised not balefully enough, is Sylvan mushiest? Brinish Conrad engages delayingly. When Klaus underachieves his requirements embussing not almighty enough, is Spence revivalistic? Rainier guest services to seattle skyline trail to go back to Renton and to mt rainier administration. Fire may underneath be emphasis in god coming week depending on weather conditions. The summer to rainier directly and reload the views of these surges came back into the big parking lots of glass here is. Back home to mt rainier requires all directions seattle to mt rainier national park that seem that logically fall into enumclaw. Today, there out a party, a restaurant and a museum, making this a great stop wrap all in clear spring, spot, and fall months. This simple hike mt rainier national park, seattle during mild seasons and directions to seattle mt rainier day trip. Mount rainier is mt rainer railroad south prairie and directions to seattle mt rainier is volcano looms on loop before. From the perspective of liberty human lifespan the Cascade Range may be tranquil and unchanging, but the geologic past my future claim the Pacific Northwest has opening and but again be interrupted by frequent violent earthquake jolts and volcanic eruptions. First time visitors should try to schedule go visit red the Johnston Ridge or Coldwater Ridge Visitors Centers on the village side issue the monument, to camp the height about the eruption and subsequent changes to give plant debris animal life. Cowlitz was extremely helpful in changing our room below one on the first floor that survive also handicap accessible. -
The Recession of Glaciers in Mount Rainier National Park, Washington
THE RECESSION OF GLACIERS IN MOUNT RAINIER NATIONAL PARK, WASHINGTON C. FRANK BROCKMAN Mount Rainier National Park FOREWORD One of the most outstanding features of interest in Mount Rainier National Park is the extensive glacier system which lies, almost entirely, upon the broad flanks of Mount Rainier, the summit of which is 14,408 feet above sea-level. This glacier system, numbering 28 glaciers and aggregating approximately 40-45 square miles of ice, is recognized as the most extensive single peak glacier system in continental United States.' Recession data taken annually over a period of years at the termini of six representative glaciers of varying type and size which are located on different sides of Mount Rainier are indicative of the rela- tive rate of retreat of the entire glacier system here. At the present time the glaciers included in this study are retreating at an average rate of from 22.1 to 70.4 feet per year.2 HISTORY OF INVESTIGATIONS CONDUCTED ON THE GLACIERS OF MOUNT RAINIER Previous to 1900 glacial investigation in this area was combined with general geological reconnaissance surveys on the part of the United States Geological Survey. Thus, the activities of S. F. Em- mons and A. D. Wilson, of the Fortieth Parallel Corps, under Clarence King, was productive of a brief publication dealing in part with the glaciers of Mount Rainier.3 Twenty-six years later, in 1896, another United States Geological Survey party, which included Bailey Willis, I. C. Russell, and George Otis Smith, made additional SCircular of General Information, Mount Rainier National Park (U.S. -
Eric Simonson's Expedition 8000
Mt. Rainier: 4 ½ Day Summit Climb Ingraham Glacier / Disappointment Cleaver Route © 2009 International Mountain Guides Why Choose This Program? Our 4 ½ Day Ingraham Glacier/Disappointment Cleaver summit program is the most relaxed approach offered to climb Mt. Rainier. The four-day program increases our opportunity for success on the mountain. There is time incorporated into this program for resting and recovery after each day’s activities. We climb as light and efficiently as possible and rely on the shelter at Camp Muir to avoid carrying extra gear or tents. The extra day spent at Camp Muir allows for better acclimatization to the altitude prior to the summit day, and more time to enjoy the majestic glacier environment with your climbing team. We maximize training by adding a half day pre-climb orientation and instructional meeting at IMG’s Headquarters in Ashford, just outside the park. We incorporate training en route during the trip to Camp Muir and utilize the following day at Muir to rest, conduct the bulk of our training and acclimatize. By spending two nights at Camp Muir prior to the summit day, we avoid carrying heavier packs up to a higher camp. There is a tradeoff in doing this, but we feel the extra time spent at Muir and the lighter overall pack weight fairly evenly offsets the advantages of departing on summit day from a higher camp. This is especially suited for those who would prefer to go as light as possible. IMG employs a light and efficient philosophy for climbing. To minimize the weight on your backs we provide shelter, stoves, cook gear and group climbing gear for you at Camp Muir. -
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 -
UNIVERSITY of CALIFORNIA Los Angeles Development Of
UNIVERSITY OF CALIFORNIA Los Angeles Development of baddeleyite as a chronometer for recent silica-undersaturated lavas A thesis submitted in satisfaction of the requirements for the degree Master of Science in Geochemistry by Wan Ning Wu 2014 ABSTRACT OF THESIS Development of baddeleyite as a chronometer for recent silica-undersaturated lavas by Wan Ning Wu Master of Science in Geochemistry University of California, Los Angeles, 2014 Professor Axel K. Schmitt, Chair Baddeleyite is a frequently found accessory mineral in silica-undersaturated lavas. Because it is typically enriched in uranium, while having low initial lead, baddeleyite has long been a prime target for U-Pb geochronology for mafic rocks. The difficulties in retrieving small baddeleyite grains from volcanic samples and the lack of a detailed understanding of baddeleyite occurrence, however, have limited baddeleyite chronology largely to coarse-grained mafic intrusive rocks. In this thesis, the development of U-Th in-situ baddeleyite analysis using Secondary Ionization Mass Spectrometry (SIMS) is presented together with an assessment of baddeleyite occurrence in Quaternary silica- undersaturated lavas. Samples studied include the Cathedral Crag and Burroughs Mountain lava flows of Cascade arc volcanoes Mt. Baker and Mt. Rainier (Washington, USA), respectively, and Accademia, Punta Marmolite and Cuma lava domes of the Campi Flegrei caldera (Naples, Italy). Baddeleyite crystals were initially identified in cut and polished rock billets using scanning electron microscope (SEM) backscatter imaging and energy dispersive x-ray analysis, before they were separated by diamond-drilling for ii SIMS analysis. A total of 62 and 52 baddeleyite crystals were documented from Cathedral and Burroughs Mountain lava flows; 205, 42 and 15 baddeleyite crystals were documented from Accademia, Punta Marmolite and Cuma lava domes, respectively. -
7/' / 7? Title: Composition, Distribution and Succession of Subal Ne Meadows In
AN ABSTRACT OF THE THESIS OF Jan Alan Henderson for theDoctor of Philosophy inPlant Ecology (Botany) presented on 9 7/' / 7? Title: Composition, Distribution and Succession of Subal ne Meadows in Mount Rainier National Park Abstract approved: --' Dr. W. W. Chilcote In 1970 a phytoscxiological reconnaissance consisting of 135 plots in the Subalpine Meadow Zone was made. These samples were sorted using an association table and several Alpine Zone and very early seral communities were set aside, An additional hundred plots taken by M. 3. Hamann were incorporated with these and compiled in another association table and com- bined in a two-dimensional ordination.This analysis yielded 18 major and 16 minor described community types which were clustered into five vegetation types. A key to the vegetation and community types is also presented. Soil moisture and temperature data were taken during 1971 and 1972 and are used to help characterize selected important communities. Soil moistures did not drop much during either season, although differences between corn- munities are apparent. The difference in temperatures (of the top 2 cm of soil) of the same selected communities were more striking. The Festuca domi- nated communities experienced soil temperatures over350C, while maximum temperatures in other communities rarely ranged over 20 C Low mght- time temperatures were relatively similar from conimumty to commumty, ranging from near freezing to about + 5° C. Several successional patterns were uncovered. In general the com- munities in the Low-Herbaceous Vegetation Type are early seral and are replaced by members of the Wet-Sedge, Lush-Herbaceous and the Dry-Grass Vegetation Types. -
Civil War Fought for the Union Which Represent 52% of the Sons of Harvard Killed in Action During This Conflict
Advocates for Harvard ROTC . H CRIMSON UNION ARMY VETERANS Total served Died in service Killed in action Died by disease Harvard College grads 475 73 69 26 Harvard College- non grads 114 22 Harvard Graduate schools 349 22 NA NA Total 938 117 69 26 The above total of Harvard alumni who died in the service of the Union included 5 major generals, 3 Brigadier Generals, 6 colonels, 19 LT Colonels and majors, 17 junior officers in the Army, 3 sergeants plus 3 Naval officers, including 2 Medical doctors. 72% of all Harvard alumni who served in the Civil War fought for the Union which represent 52% of the sons of Harvard killed in action during this conflict. As result among Harvard alumni, Union military losses were 10% compared with a 21% casualty rate for the Confederate Army. The battle of Gettysburg (PA) had the highest amount of Harvard alumni serving in the Union Army who were killed in action (i.e. 11), in addition 3 Harvard alumni Confederates also died in this battle. Secondly, seven Crimson warriors made the supreme sacrifice for the Union at Antietam (MD) with 5 more were killed in the battles of Cedar Mountain (VA) and Fredericksburg (VA). As expected, most of the Harvard alumni who died in the service of the Union were born and raised in the Northeastern states (e.g. 74% from Massachusetts). However, 9 Harvard alumni Union casualties were from the Mid West including one from the border state of Missouri. None of these Harvard men were from southern states. The below men who made the supreme sacrifice for their country to preserve the union which also resulted in the abolition of slavery.