MOUNT RAINIER NATIONAL PARK L/Lsajjiswujjarns
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
An Inventory of Fish in Streams in Mount Rainier National Park 2001-2003
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science An Inventory of Fish in Streams at Mount Rainier National Park 2001-2003 Natural Resource Technical Report NPS/NCCN/NRTR—2013/717.N ON THE COVER National Park staff conducting a snorkel fish survey in Kotsuck Creek, Mount Rainier National Park, 2002. Photograph courtesy of Mount Rainier National Park. An Inventory of Fish in Streams at Mount Rainier National Park 2001-2003 Natural Resource Technical Report NPS/NCCN/NRTR—2013/717.N Barbara A. Samora, Heather Moran, Rebecca Lofgren National Park Service North Coast and Cascades Network Inventory and Monitoring Program Mount Rainier National Park Tahoma Woods Star Rt. Ashford, WA. 98304 April 2013 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are 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 Technical Report Series is used to disseminate results of scientific studies in the physical, biological, and social sciences for both the advancement of science and the achievement of the National Park Service mission. The series provides contributors with a forum for displaying comprehensive data that are often deleted from journals because of page limitations. 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. -
FINAL Kimball 16-Page Marketing Piece.Indd
Kimball Welcomes You! As seen in the March/April 2008 issue of Nebraska Life MagazineKIMBALL. WELCOMES YOU School HOPE THAT THE FOLLOWING feature story, pictures and ads will be Superintendent of Schools helpful in familiarizing yourself with Kimball and our citizens. Since 1889, Troy L. Unzicker the town of Kimball has welcomed both travelers and settlers into the warm 901 S. Nadine St. embrace of its friendly and welcoming community nestled in the far southwestern Kimball, NE 69145 corner of Nebraska. (308) 235-2188 Safely secured under the brightest stars and the most spectacular sunsets, Kim- Fax: (308) 235-3269 ball has emerged as one of the most desirable destinations to live, work, raise a [email protected] family, retire and even start a business in the Great Plains. http://kimball.k12.ne.us Th ere’s so much to like about Kimball. Its natural, rural beauty. Close proximity to the Colorado Front Range, Interstate 80 and the future Heartland Expressway City make our location a huge attribute. City of Kimball Administrator Harold Farrar • Healthy living. 223 S. Chestnut St. Hospital University of • Top notch health care facilities. Kimball, NE 69145 Kimball Health Services Nebraska Extension • Assisted living and nursing home that are second to none. (308) 235-3639 or 235-2971 Julie Schnell - Chief Kimball-Banner Co. • Excellent schools. [email protected] Executive Offi cer Extension Offi ce • Welcoming churches. www.ci.kimball.ne.us 505 S. Burg St. 209 E. 3rd St. Kimball, NE 69145 • Unique shopping. Kimball, NE 69141-1401 (308) 235-1951 Hospital • Rich rail history and presence Economic (308) 235-3122 (308) 235-1966 Clinic (308) 235-3077 • Many dining options. -
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. -
Chambers Creek
Section 3 - Physical and Environmental Inventory 3.1 Chambers Creek – Clover Creek Drainage Basin 3.2 Puyallup River Drainage Basin 3.3 Sewer Service Basins in the Puyallup and White River Drainage Basins 3.4 Nisqually River Drainage Basin 3.5 Kitsap Drainage Basin 3.6 City of Tacoma - North End WWTP 3.7 Joint Base Lewis Mcchord Sewer System – Tatsolo Point WWTP Pierce County Public Works and Utilities – Sewer Utility Unified Sewer Plan Update Section 3 Section 3 – Physical and Environmental Inventory Section 3 documents the land-use and environmental tenants of the four major basins in Pierce County and are organized around those basins. Chambers Creek – Clover Creek Drainage Basin - Section 3.1 Puyallup River Drainage Basin – Section 3.2 Nisqually River Drainage Basin – Section 3.4 Kitsap Drainage Basin – Section 3.5 3.1 Chambers Creek – Clover Creek Drainage Basin The Chambers Creek - Clover Creek Drainage Basin (Basin) is located in central Pierce County, between Puget Sound on the west and the ridge above the Puyallup River Valley on the east. Point Defiance and the southwest shore of Commencement Bay serve as the basin’s northern boundary, and the City of DuPont lies on the southern boundary. The basin encompasses approximately 104,258 acres (117 square miles) of land including the Cities of DuPont, including Northwest Landing, University Place, Lakewood, and Northwest Tacoma, Fircrest, the Towns of Ruston, and Steilacoom, as well as portions of Fort Lewis and McChord Military Reservations, and the unincorporated communities of South Hill, Frederickson, Mid County, Graham, Parkland, and Spanaway. 3.1.1 Topography Lowland topography is generally flat to gently rolling. -
Tahoma News Summer 2007
November 2006 Flood Makes History The flood of November 6 and 7, 2006 was an previous records. Record amounts fell throughout up here, washing it away there changing course, historical, natural event unlike any other that has other regions of the park. seeking the easiest path through the debris. This been recorded in Mount Rainier National Park’s is why glacial riverbeds are wide and rocky, with 108 year history. The snow levels during the storm stayed above the river itself braided into constantly changing 10,000 feet in elevation, with the majority of the channels. Long before National Park status, debris flows precipitation falling as rain. Some existing snow traveled from Mount Rainier to the Puget Sound. above 7,000 feet melted, adding to the runoff in the Recent research at Mount Rainier National Park Areas near Tacoma and Seattle are formed of rivers. has measured aggradation in most park rivers prehistoric debris from the mountain. to occur at a rate of 6 to 14 inches per decade. As the rain flowed down mountain-sides and In comparison, during the November flood, the In more recent park history (1946-47), a series roads to the main watersheds, it caused extreme riverbed where Tahoma Creek flows under the of heavy snowstorms caused extreme damage to soil erosion and slides. It uprooted large areas of Nisqually Road rose more than four feet. facilities. For two weeks, the main entrance to the trees that eventually caused log jams that redirected park was closed to the public due to the danger of water. -
2010 CENSUS - CENSUS TRACT REFERENCE MAP: Lewis County, WA 121.217411W LEGEND Emmons Glacier
46.862203N 46.867049N 121.983702W 2010 CENSUS - CENSUS TRACT REFERENCE MAP: Lewis County, WA 121.217411W LEGEND Emmons Glacier Y P SYMBOL DESCRIPTION SYMBOL LABEL STYLE South Mowich Fryingpan Glacier A I Glacier E K R I C M Federal American Indian Puyallup Glacier E A Reservation L'ANSE RES 1880 0 Bumping Lk Ingraham Glacier 5 0 3 7 7 Off-Reservation Trust Land, Hawaiian Home Land T1880 Tahoma Glacier Oklahoma Tribal Statistical Area, Alaska Native Village Statistical Area, KAW OTSA 5340 Tribal Designated Statistical Area State American Indian W Tama Res 4125 ilson Glacier Reservation Kautz Glacier South Tahoma Glacier Nisqually Glacier Cowlitz Glacier State Designated Tribal Statistical Area Lumbee STSA 9815 Alaska Native Regional Corporation NANA ANRC 52120 State (or statistically equivalent entity) NEW YORK 36 County (or statistically Mount Rainier Natl Pk equivalent entity) ERIE 029 Minor Civil Division (MCD)1,2 Bristol town 07485 123 PIERCE 053 Consolidated City MILFORD 47500 S LEWIS 041 d R lley 1,3 Va e Incorporated Place s Davis 18100 i rad Pa Census Designated Place (CDP) 3 Incline Village 35100 ns Cany e on v e R t d S Census Tract 33.07 706 DESCRIPTION SYMBOL DESCRIPTION SYMBOL Interstate 3 Water Body Pleasant Lake W o l d 706 706 r o 2 R 2 F 1 U.S. Highway 0 e Cre d t at ek a d Swamp or Marsh Okefenokee Swamp Sk N N R R i v d sq e N u D ally Riv State Highway 4 Glacier Bering Glacier 4 Marsh Ln 4 Other Road N d D a R e t v F v or Na e R t D d F 4WD Trail, Stairway, 0 o r 1 r o 2 F Military Fort Belvoir D e t Alley, Walkway, -
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 -
Kimball Nebraska!
Kimball The High Point of Nebraska PC: Alisa Danae Photography Located at: 214 S Walnut St Kimball, Nebraska Phone: (308) 230-2111 Hours: Tuesday—Thursday (6:00 AM—2:00 PM) Friday & Saturday (6:00 AM— 8:00 PM) Karen’s Kitchen is a locally owned and operated family restaurant Offering Home cooked meals from the menu and daily specials. Karen’s Kitchen also offers pickup services. Table of Contents Quick Reference Phone Numbers Welcome Message History of Kimball Wheat Growers Hotel City of Kimball Government & Ordinances Agriculture in Kimball County Kimball Health Services Housing Utilities Education Oliver Reservoir State Recreation Area Four Winds Golf Course Gotte Park Panorama Point & Three State Corner Marker Plains Historical Museum Kimball Celebrations Kimball Organizations Transportation City of Kimball Map Kimball Businesses Quick Reference Phone Numbers Kimball City Offices…………………….308.235.3639 County Assessor………………...……….308.235.2362 County Attorney………………….....…..308.235.3678 County Clerk……………………………….308.235.2241 County Commissioners..……………....308.235.4056 County Court………..………………….....308.235.2831 County District Court………………...308.235.3591 County Highway Department……...308.235.2681 County Treasurer…………………...…..308.235.2242 District 10 Probation Office….…...308.235.4046 Fairgrounds………………………………...308.235.8886 Kimball Health Services……………..308.235.1952 Kimball Landfill...……………………….308.235.3540 Kimball Municipal Airport……........308.235.4008 Kimball Parks & Recreation…….....308.235.4241 Kimball Police Department..……....308.235.3608 -
1934 the MOUNTAINEERS Incorpora.Ted T�E MOUNTAINEER VOLUME TWENTY-SEVEN Number One
THE MOUNTAINEER VOLUME TWENTY -SEVEN Nom1-0ae Deceml.er, 19.34 GOING TO GLACIER PUBLISHED BY THE MOUNTAIN�ER.S INCOaPOllATBD SEATTLI: WASHINGTON. _,. Copyright 1934 THE MOUNTAINEERS Incorpora.ted T�e MOUNTAINEER VOLUME TWENTY-SEVEN Number One December, 1934 GOING TO GLACIER 7 •Organized 1906 Incorporated 1913 EDITORIAL BOARD, 1934 Phyllis Young Katharine A. Anderson C. F. Todd Marjorie Gregg Arthur R. Winder Subscription Price, $2.00 a Year Annual (only) Seventy-five Cents Published by THE MOUNTAINEERS Incorporated Seattle, Washington Entered as second class matter, December 15, 1920, at the Postofflce at Seattle, Washington, under the Act of March 3, 1879. TABLE OF CONTENTS Greeting ........................................................................Henr y S. Han, Jr. North Face of Mount Rainier ................................................ Wolf Baiter 3 r Going to Glacier, Illustrated ............... -.................... .Har iet K. Walker 6 Members of the 1934 Summer Outing........................................................ 8 The Lake Chelan Region ............. .N. W. <J1·igg and Arthiir R. Winder 11 Map and Illustration The Climb of Foraker, Illitstrated.................................... <J. S. Houston 17 Ascent of Spire Peak ............................................... -.. .Kenneth Chapman 18 Paradise to White River Camp on Skis .......................... Otto P. Strizek 20 Glacier Recession Studies ................................................H. Strandberg 22 The Mounta,ineer Climbers................................................ -
Mo44*Uiscutu&I
Mo44*UIscUtu&i NATIONAL PARK I UNITED STATES Historic Events DEPARTMENT OF THE MOUNT INTERIOR 1792 Capt. George Vancouver, of the Royal OPEN British Navy, first white man to re HAROLD L. ICKES, Secretary ALL RAINIER cord sight of "The Mountain," named YEAR it Mount Rainier in honor of his NATIONAL PARK friend, Admiral Peter Rainier. WASHINGTON l9 41 1833 Dr. William Fraser Tomlie entered NATIONAL PARK SERVICE northwest corner of what is now the NEWTON B. DRURY, Director park. First white man to penetrate ADMINISTRATION BUILDING AT LONGMIRE this region. CO^TE^TS OUNT RAINIER NATIONAL with cinders and steam-shredded parti 1857 Lt. A. V. Kautz and four companions M PARK was established by act of cles, lumps of lava, and occasional flows Congress, approved by President Mc- Wild Flowers Color the Alpine made first attempt to scale Mount of liquid lava that have solidified into Kinley, March 2, 1899- A subsequent Meadows Cover Rainier but did not reach summit. layers of hard andesite rock. Judging act, January 31, 1931, extended the east "The Mountain" 3 by the steep inclination of the lava and boundary to the summit of the Cascade cinder layers visible in its flanks, it is Flowers and Forests 4 Range, the boundary recommended by thought to have once attained an alti Mount Rainier Summit Climb . 4 1870 Hazard Stevens and P. B. Van Trump the original bill. The park embraces tude of 16,000 feet. In subsequent ex Winter Sports 4 made the first successful ascent via 377.78 square miles (241,782 acres).