Mount Rainier : a Record of Exploration
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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 . -
Climate Change Impacts on Water Management in the Puget Sound Region, Washington, USA Julie A
Climate Change Impacts on Water Management in the Puget Sound Region, Washington, USA Julie A. Vano1, Nathalie Voisin1, Lan Cuo1,2, Alan F. Hamlet1,2, Marketa McGuire Elsner2, Richard N. Palmer3, Austin Polebitski1, and Dennis P. Lettenmaier1,2 Abstract limate change is projected to result, on average, in earlier snowmelt and reduced summer flows, patterns that are not well represented in the historical observations used for planning and reliability analyses by water utilities. CWe extend ongoing efforts in the Puget Sound basin cities of Everett, Seattle, and Tacoma to characterize differences between historic and future streamflow and the ability of the region’s water supply systems to meet future demands. We use future streamflow simulations for the 2020s, 2040s, and 2080s from the Distributed Hydrology-Soil- Vegetation Model (DHSVM), driven by climate simulations archived by the 2007 Fourth Assessment Report (AR4) of the Intergovernmental Panel on Climate Change (IPCC). We use ensembles of streamflow predictions produced by DHSVM forced with multiple downscaled ensembles from the IPCC climate models as inputs to reservoir system models for the Everett, Seattle, and Tacoma water supply systems. Over the next century, under average conditions all three systems are projected to experience a decline and eventual disappearance of the springtime snowmelt peak in their inflows. How these shifts impact water management depends on the specifics of the reservoir system and their operating objectives, site-specific variations in the influence that reductions in snowmelt have on reservoir inflows, and the adaptive capacity of each system. Without adaptations, average seasonal drawdown of reservoir storage is projected to increase in all of the systems throughout the 21st century. -
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 -
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. -
Mount Rainier NATIONAL PARK
Mount Rainier NATIONAL PARK . WASHINGTON THE SEASONS Curving mountain roads demand careful driving. at Cougar Rock Campground. Camping through Observe posted speeds; drive defensively. Use out the park is allowed at designated sites only. From mid-June through October, the experi lower gears for steep hills. Help prevent traffic Also, for back-country camping, you will need a enced visitor comes prepared for cool and rainy jams by using turnouts and parking areas while back-country use permit, which is available at days as well as for those that are warm and sunny. observing wildlife or scenery. any ranger station. Build fires only in places where From November through May, heavy snowstorms fires are permitted. Dead and down wood only Motorcycles and motorbikes must be licensed, and are frequent. Annual snowfall at Paradise (5,420 may be used. Do not leave fires unattended; ex riders must comply with Washington State laws. feet) may total 80 feet; snow may lie as deep as tinguish them completely with water. Report un They are not allowed on park trails. 30 feet; 5 to 14 feet of snow may remain on the attended fires to a ranger. ground into June, and even 3 to 8 feet into July. Stop at overlooks marked "POINT OF INTEREST To keep bears and other animals from your food, AHEAD" for grand views and exhibits on Mount Wildflowers in the high meadows begin to blos you must store it in your car or suspended high in Rainier's features. som in mid-June in places where the snow has a tree. -
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). -
Mount Rainier National Park, Washington
NATIONAL PARK . WASHINGTON MOUNT RAINIER WASHINGTON CONTENTS "The Mountain" 1 Wealth of Gorgeous Flowers 3 The Forests 5 How To Reach the Park 8 By Automobile 8 By Railroad and Bus 11 By Airplane 11 Administration 11 Free Public Campgrounds 11 Post Offices 12 Communication and Express Service 12 Medical Service 12 Gasoline Service 12 What To Wear 12 Trails 13 Fishing 13 Mount Rainier Summit Climb 13 Accommodations and Expenses 15 Summer Season 18 Winter Season 18 Ohanapecosh Hot Springs 20 Horseback Trips and Guide Service 20 Transportation 21 Tables of Distances 23 Principal Points of Interest 28 References 32 Rules and Regulations 33 Events of Historical Importance 34 Government Publications 35 UNITED STATES DEPARTMENT OF THE INTERIOR • Harold L. Ickes, Secretary NATIONAL PARK SERVICE Arno B. Cammerer, Director UNITED STATES GOVERNMENT PRINTING OFFICE • 1938 AN ALL-YEAR PARK Museums.—The park museum, headquarters for educational activities, MOUNT RAINIER NATIONAL PARK may be fully enjoyed throughout the and office of the park naturalist are located in the museum building at year. The summer season extends from early June to early November; the Longmire. Natural history displays and wild flower exhibits are main winter ski season, from late November well into May. All-year roads make tained at Paradise Community House, Yakima Park Blockhouse, and the park always accessible. Longmire Museum. Nisquaiiy Road is open to Paradise Valley throughout the year. During Hikes from Longmire.—Free hikes, requiring 1 day for the round trip the winter months this road is open to general traffic to Narada Falls, 1.5 are conducted by ranger naturalists from the museum to Van Trump Park, miles by trail from Paradise Valley. -
Phylogenetic Taxonomy of Artemisia L. Species from Kazakhstan Based On
PROCEEDINGS OF THE LATVIAN ACADEMY OF SCIENCES. Section B, Vol. 72 (2018), No. 1 (712), pp. 29–37. DOI: 10.1515/prolas-2017-0068 PHYLOGENETIC TAXONOMY OF ARTEMISIA L. SPECIES FROM KAZAKHSTAN BASED ON MATK ANALYSES Yerlan Turuspekov1,5, Yuliya Genievskaya1, Aida Baibulatova1, Alibek Zatybekov1, Yuri Kotuhov2, Margarita Ishmuratova3, Akzhunis Imanbayeva4, and Saule Abugalieva1,5,# 1 Institute of Plant Biology and Biotechnology, 45 Timiryazev Street, Almaty, KAZAKHSTAN 2 Altai Botanical Garden, Ridder, KAZAKHSTAN 3 Karaganda State University, Karaganda, KAZAKHSTAN 4 Mangyshlak Experimental Botanical Garden, Aktau, KAZAKHSTAN 5 Al-Farabi Kazakh National University, Biodiversity and Bioresources Department, Almaty, KAZAKHSTAN # Corresponding author, [email protected] Communicated by Isaak Rashal The genus Artemisia is one of the largest of the Asteraceae family. It is abundant and diverse, with complex taxonomic relations. In order to expand the knowledge about the classification of Kazakhstan species and compare it with classical studies, matK genes of nine local species in- cluding endemic were sequenced. The infrageneric rank of one of them (A. kotuchovii) had re- mained unknown. In this study, we analysed results of sequences using two methods — NJ and MP and compared them with a median-joining haplotype network. As a result, monophyletic origin of the genus and subgenus Dracunculus was confirmed. Closeness of A. kotuchovii to other spe- cies of Dracunculus suggests its belonging to this subgenus. Generally, matK was shown as a useful barcode marker for the identification and investigation of Artemisia genus. Key words: Artemisia, Artemisia kotuchovii, DNA barcoding, haplotype network. INTRODUCTION (Bremer, 1994; Torrel et al., 1999). Due to the large amount of species in the genus, their classification is still complex Artemisia of the family Asteraceae is a genus with great and not fully completed. -
Analysis of Runoff from Small Drainage Basins in Wyoming
Analysis of Runoff from Small Drainage Basins in Wyoming GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2056 Prepared In cooperation with the Wyoming Highway Department and the U.S. Department of Transportation, Federal Highway Administration Analysis of Runoff from Small Drainage Basins in Wyoming By GORDON S. CRAIG, JR., and JAMES G. RANKL GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2056 Prepared in cooperation with the Wyoming Highway Department and the U.S. Department of Transportation, Federal Highway Administration UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1978 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Catalog-card Number 78-600090 For sale by the Superintendent of Documents, U. S. Government Printing OfEce Washington, D. C. 20402 Stock Number 024-001-03106-0 CONTENTS Page Symbols_________________________________________ V Abstract_________________________________________ 1 Introduction ________________________________________ 1 Purpose and scope _______ ____________________________ 1 Limitations of study _______________________________ 5 Acknowledgments ________________________________________ 5 Use of metric units of measurement ________________________ 6 Data collection ____________________________________ 6 Description of area __________________________________ 6 Instrumentation __________________________________ 7 Types of records _________________________________________ 7 Station frequency analysis _________________________________ 9 Runoff -
Artemisia Borealis Var. Wormskioldii, Miller Island, Washington
NATURAL HERITAGE PROGRAM HERITAGE NATURAL Wormskiold’s northern wormwood (Artemisia borealis var. wormskioldii) Miller Island Conservation Plan WASHINGTON WASHINGTON Prepared for U.S. Fish and Wildlife Service Region 1 Prepared by Joseph Arnett September 20, 2010 Natural Heritage Report 2010-03 Wormskiold’s Northern Wormwood (Artemisia borealis var. wormskioldii) Miller Island Conservation Plan September 20, 2010 Prepared for The US Fish and Wildlife Service Western Washington Fish and Wildlife Office Through Section 6 funding, Region 1 Project 3E2, Segment 51 by Joseph Arnett Washington Natural Heritage Program Washington Department of Natural Resources PO Box 47014 Olympia, WA 98504-7014 ii Acknowledgements Many thanks to U.S. Forest Service staff who assisted with monitoring, including Robyn Beck, Robin Dobson, and Chuti Fiedler, and especially to Cathy Flick for all her help with logistics. Many volunteers also participated in the monitoring over the years; without their help the work would have been less successful and much less enjoyable: Nancy Allen, Kelly Amsberry, Robin Beck, Debi Budnick, Melissa Carr, Char Corkran, Kristin Currin, Rebecca Currin, Elizabeth Daniel, Kim Garner, Alison Henderson, Jurgen Hess, Susan Hess, Drew Merritt, Andrea Raven, Jamie Sheahan, Krista Thie, Jennifer Wade, Karen Whitlock, Carolyn Wright, and Sara Wu. The RareCare Program from the University of Washington provided training for many of the volunteers. Captain Jack LeFond, of Young’s Fishing Service, has transported us to the island and brought us back, and made our trips enjoyable as well as safe. Special thanks to Katie Birkhauser for her help revising the monitoring methodology in 2006. This work has been conducted with logistical support from the U.S. -
A Double Peak in the Seasonality of California's
Biogeosciences, 17, 405–422, 2020 https://doi.org/10.5194/bg-17-405-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. A double peak in the seasonality of California’s photosynthesis as observed from space Alexander J. Turner1,2,3, Philipp Köhler4, Troy S. Magney3,4,5, Christian Frankenberg3,4, Inez Fung1, and Ronald C. Cohen1,2 1Department of Earth and Planetary Sciences, University of California, Berkeley, CA 94720, USA 2College of Chemistry, University of California, Berkeley, CA 94720, USA 3Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA 4Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91226, USA 5Department of Plant Sciences, University of California, Davis, CA 95616, USA Correspondence: Alexander J. Turner ([email protected]) Received: 24 September 2019 – Discussion started: 26 September 2019 Revised: 16 December 2019 – Accepted: 6 January 2020 – Published: 29 January 2020 Abstract. Solar-induced chlorophyll fluorescence (SIF) has nia’s photosynthesis is due to two processes that are out of been shown to be a powerful proxy for photosynthesis and phase: grasses, chaparral, and oak savanna ecosystems show gross primary productivity (GPP). The recently launched an April maximum, while evergreen forests peak in June. TROPOspheric Monitoring Instrument (TROPOMI) features An empirical orthogonal function (EOF) analysis corrobo- the required spectral resolution and signal-to-noise ratio to rates the phase offset and spatial patterns driving the double retrieve SIF from space. Here, we present a downscaling peak. The EOF analysis further indicates that two spatiotem- method to obtain 500 m spatial resolution SIF over Cal- poral patterns explain 84 % of the variability in the SIF data. -
Artemisia Borealis Var. Wormskioldii, (Formerly Artemesia Campestris Ssp
U.S. FISH AND WILDLIFE SERVICE SPECIES ASSESSMENT AND LISTING PRIORITY ASSIGNMENT FORM SCIENTIFIC NAME: Artemisia borealis var. wormskioldii, (formerly Artemesia campestris ssp. borealis var. wormskioldii) COMMON NAME: Northern wormwood LEAD REGION: Region 1 INFORMATION CURRENT AS OF: March 29, 2007 STATUS/ACTION ___ Species assessment - determined we do not have sufficient information on file to support a proposal to list the species and, therefore, it was not elevated to Candidate status ___ New candidate X Continuing candidate __ Non-petitioned _X_ Petitioned - Date petition received: May 11, 2004 90-day positive - FR date: 12-month warranted but precluded - FR date: Did the petition request a reclassification of a listed species? NO FOR PETITIONED CANDIDATE SPECIES: a. Is listing warranted (if yes, see summary of threats below)? YES b. To date, has publication of a proposal to list been precluded by other higher priority listing actions? YES c. If the answer to a. and b. is “yes”, provide an explanation of why the action is precluded. We find that the immediate issuance of a proposed rule and timely promulgation of a final rule for this species has been, for the preceding 12 months, and continues to be, precluded by higher priority listing actions. During the past 12 months, almost our entire national listing budget has been consumed by work on various listing actions to comply with court orders and court-approved settlement agreements, meeting statutory deadlines for petition findings or listing determinations, emergency listing evaluations and determinations, and essential litigation- related, administrative, and program management tasks. We will continue to monitor the status of this species as new information becomes available.