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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 . -
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. -
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. -
NATURAL RESOURCES (Updated Excerpt from Jo Daviess Comprehensive Plan Baseline Data)
ATTACHMENT F: NATURAL RESOURCES (Updated excerpt from Jo Daviess Comprehensive Plan Baseline Data) The natural resources in Jo Daviess County are unique relative to the rest of the state and much of the mid-west because the county is part of the Wisconsin Driftless Region bypassed by continental glaciers of the Ice Age. This region covers parts of southern Minnesota and Wisconsin, Northwestern Illinois and Northeastern Iowa. Glaciated areas were leveled, strewn with glacial debris or "drift" and dotted with lakes and ponds. The driftless areas, on the other hand, have bedrock close to the surface into which deep valleys have been carved by millions of years of weather and erosion. In Jo Daviess County, streams are numerous and the only two lakes are man-made. The relief from the higher ridges to the valley floors is typically 300 feet or more creating a rugged and scenic landscape. Ecosystems can be found in this landscape that are older than those found in glaciated areas. Geology The topography of Jo Daviess County is characterized by rugged relief unique to most of Illinois. Our county, located in the far northwestern corner of the state, is in an area spared by the major glaciations of the last two million years. It is, accordingly, called the "Driftless Area" by geologists, the term "drift" referring to material deposited by glacial activity. The visible landscape that we see today began during the Paleozoic Era (570 to 245 million years ago) when shallow seas repeatedly inundated the interior of the continent. Shells of marine animals, along with muds, silts and sands from eroding highlands, were periodically deposited in those sea bottoms. -
Encounters with the Early Highpointers by Charles
SOME CLOSE (AND NOT SO CLOSE) ENCOUNTERS WITH THE EARLY HIGHPOINTERS BY CHARLES FERIS Many stories can be told of how we got our first inspiration to pursue this hobby of ours, this highpointing. We’ve been inspired in a hundred ways; mine arose during a period of boredom, while in college. Seeking something other than study, I took out a Rand McNally road atlas, and looked at a map of my native state of Illinois, noting the little red dot in the northwest corner of the state. Wow, something neat to do. So while the other kids were off to Florida, off to Charles Mound I went during spring break 1961. Then it hit me; I had already done Mt. Whitney the year before, so why not do all the states. Now I was really excited. The next few years saw me collecting 13 more highpoints in the Midwest and southeast. I went my merry way, never realizing that others might be crazy enough to be pursuing the very same project. At this point I was not aware of the tiny fraternity of early highpointers who were already years before me. I had no idea of the remarkable people I was about to meet. Then in August 1965 a Sierra Club friend of mine in Chicago told me about C. Rowland Stebbins. I had found a kindred soul, one who had already completed the 48. I phoned him immediately. Soon my wife and I were off on the four hour drive to Lansing, Michigan. We arrived to an expansive mansion on Moore’s River Drive atop a bluff overlooking the Grand River. -
Mountain Ear MONTHLY Newslettep of the ROCKY MOUNTAINEERS
Mountain Ear MONTHLY NEWSLETTEp OF THE ROCKY MOUNTAINEERS _, _- . August , 1.99 3 MEETING a Time and Place: The Club does not hold meetings during the summer. The next meeting will be on Wednesday, September 8. The program in September will be the traditional. retrospective slide show of Club trips during the previous year, so start choosing your favorite slides, TRIP CALENDAR Tuesday Niqht Mount Sentinel '~ikes: If you're bored with the stair machine at the club, meet in the Mount Sentinel parking lot at 5:30 p.m. each'Tuesday for a more interesting climb. Thursdav eveninqs and Saturdays,' Rock Climbinq, If you ' re interested in beginning, intermediate or advanced rock climbing at Kootenai Canyon, Blodgett Canyon or Lolo Pass on Thursday evenings or Saturdays, call ~eraldOlbu at 549-4769, A report on-last month's climbs is set forth below, Kayakins and raftinq, A lot of the rivers in the region are pooping out, but there is still whitewatef to be found. If you are interested in kayaking and/or rafting trips, call Peter Dayton at 728-8101 or Art Gidel at 543-6352. Sunday, Auwst 8, Turauoise Lake, Easy to moderate 7-mile hike to Turquoise Lake in the Mission Mountains from the Swan Valley side, Turquoise Lake is the most beautiful of the large lakes in the Missions- It will be apparent why it's called "~urquoise"Lake. Call Gerald Olbu at 549-4769 for details, Sundav, Ausust 15, Lucifer Lake, Turquoise Peak, Mountaineer Peak. Hike and climb in the Mission Mountains near St, Ignatius. -
APNW-50 Tr' ORTH (4 -66
low AMC U. S. FOREST SERVICE tr ORTH (4 -66 EST FOREST AND RANGE EXPERIMENT STATION • U.S. DEPARTMENT OF AGRICULTURE • PORTLAND, OREGON APNW-50 March 1967 C PRIMARY MICROBIOLOGICAL SUCCESSION ON A LANDSLIDE cL OF ALPINE ORIGIN AT MOUNT RAINIER CD O by W. B. Bollen, Principal Soil Microbiologist CD a= K. C. Lu, Microbiologist 1--- CD J. M. Trappe, Principal Mycologist 77 R. F. Tarrant, Principal Soil Scientist CD 4 J. F. Franklin, Plant Ecologist In December 1963, immense masses of rock and debris broke loose from the north face of Little Tahoma Peak on the shoulder of Mount Rainier (Crandell and Fahnestock 1965).1/ Originating from a zone roughly 9,000 to 11,000 feet above sea level, the resulting series of avalanches swept down Emmons Glacier to deposit an estimated 14 million cubic yards of debris over 2 square miles of the glacier and the sparsely vegetated outwash valley below (fig. 1). Deposits reach thicknesses of about 100 feet in the valley, whose original elevation ranged from about 4,500 to 5,500 feet. Figure 1.--Northeast slope of Mount Rainier with Little Tahoma Peak on left-center skyline and avalanche de- posit in valley. 1/ — Names and dates in parentheses refer to Litera- ture Cited, p. 7. This nearly virgin, alpine "soil," laid in a valley surrounded by montane forest, presents superb opportunity for studies of soil development, plant succession, and distribution of pesticides and other environmental pollutants, especially when coupled with concur- rent observations of nearby terminal moraines left from recent recession of Emmons Glacier. -
Cascades Volcano Observatory
U.S. GEOLOGICAL SURVEY—REDUCING THE RISK FROM VOLCANO HAZARDS Mount Rainier—Living Safely With a Volcano in Your Backyard ajestic Mount Rainier M soars almost 3 miles (14,410 feet) above sea level and looms over the expanding suburbs of Seattle and Tacoma, Washington. Each year almost two million visitors come to Mount Rainier National Park to admire the volcano and its glaciers, alpine meadows, and forested ridges. However, the volcano’s beauty is deceptive— U.S. Geological Survey (USGS) research shows that Mount Rainier is one of our Nation’s most dangerous volcanoes. It has been the source of countless eruptions and volcanic mudflows (lahars) that have surged down valleys on its flanks and buried broad areas now densely populated. To help people live more safely with the volcano, USGS scientists are working closely with local communities, emergency managers, and the National Park Service. Mount Rainier, an active volcano currently at rest between eruptions, is the highest peak in the Cascade Range. Its edifice, capped by snow and 25 glaciers, has been built up by untold eruptions over the past 500,000 years. It last erupted in 1894–95, when small summit explosions were reported by observers in Seattle and Tacoma. Mount Rainier’s next eruption The flat floor of the Puyallup River valley near Orting, Washington, is formed by deposits of the 500-year-old might be of similar or larger size and Electron lahar, which surged down from Mount Rainier (in background). Lahars, or volcanic mudflows, are rapidly flowing slurries of mud and boulders that destroy or bury most manmade structures in their paths. -
Arcuser Magazine Summer 2014 Issue
Summer 2014 ArcUser The Magazine for Esri Software Users It Can’t Wait 16 We’re All Storytellers Now 26 It’s All about Collaboration 36 What if your entire organization could share geospatial knowledge? Sharing can be a challenge. Especially when your workforce is scattered across geographic locations, and they all have different methods for accessing the geospatial information they need. ENVI for ArcGIS® allows everyone from your organization to use geospatial imagery and data, such as SAR and LiDAR, to enhance their GIS applications. And, since ENVI products are fully integrated with ArcGIS, whether your team is analyzing imagery from a desktop computer, or they need to share the latest advanced image analysis tool with their colleagues via ArcGIS for Server we have the imagery software to suit your needs. Now with ENVI, sharing just got a little easier. Information from Imagery Attending the Esri UC? Means a Better GIS. Stop by booth #1311 to see our solutions! ® ® › For more information about ENVI for ArcGIS , visit www.exelisvis.com/ArcUser ©2014, Exelis Visual Information Solutions, Inc. All rights reserved. Exelis, ENVI, and IDL are registered trademarks of Exelis Inc. All other marks are the property of their respective owners. Esri trademarks provided under license from Esri. Contents Summer 2014 Vol. 17 No. 3 Focus 16 It Can’t Wait Making communities more resilient to climate change now 16 Feature 22 Audit Ready USCG validates real property assets 24 Saving Space and Time with Mosaic Datasets 24 Special Section 38 ArcGIS Pro Helps You Get Work Done Faster 40 How Quick It Is… Developing web apps with ArcGIS 42 Ready-to-Use Native App for Mobile Devices 42 esri.com Summer 2014 au 3 Deciding a Better Future ArcUser Summer 2014 Vol. -
Climbing America's
batical leave in Scandinavia, I finally reached the 5895m summit of Africa’s high- est mountain. In 1986, the year after I climbed Kilimanjaro, Dick Bass, Frank Wells, and Rick Ridgeway published Seven Summits, an account of Bass and Wells’ attempt to climb the highest peak on each of the world’s seven continents. I bought their book and devoured it. Inspired by it, I devised my own climbing goal—to climb at least ‘Three-and-a-Half Summits’: namely, at least three of the six highest of the Seven Summits plus Australia’s Mt Kosciuszko, which is a mere 2228m above sea level (i.e., less than half the height of Antarctica’s Vinson Massif, the sixth-lowest of the Seven Summits), and Kosciuszko can therefore, as a Kiwi I quipped, really only be regarded as a half-summit. I made reasonably quick progress towards achieving my goal. In August 1994, I climbed Russia’s Mt Elbrus, 5642m, the highest mountain in Europe. In December the same year, I summited 6962m-high Cerro Aconcagua in Argentina, the highest mountain in South America (which I like to tell people is ‘the highest mountain in the world outside Asia,’ and then hope their geography is so weak that they don’t realise how huge an exclusion clause those two words, ‘outside Asia’, are). I then decided to have a crack at climbing Denali, and on 6 July 1997 stood proudly on the 6194m-high summit of North America’s high- est peak and held up a t-shirt from Victoria University (which is where I taught political science for many years). -
Society Officers
Spring “The challenge goes on. There are other lands and rivers, other wilderness areas, to save and to share with all. March 2019 I challenge you to step forward to protect and care for the wild places you love best.” - Dr. Neil Compton Introducing Emily Roberts by David Peterson, Ozark Society President Please join me in welcoming Emily Foundation/Pioneer Forest in Salem, Roberts to the Ozark Society team! Mo. She has experience most Emily will be working on book, map, recently as a fire a biological science and other material sales for us and technician in the botany program at you can contact her at the Mt. Hood National Forest in [email protected]. Here is Dufur, Oregon; as a field technician some information about Emily. She for the Romance Christmas Tree has a Bachelor of Science degree in Farm in Romance, Arkansas; and as environmental science, with a an AmeriCorps member at the biology concentration, and is a Salmon-Challis Forest Training graduate of the Norbert O. Schedler Center in Challis, Idaho. her Honors College at UCA. Roberts was background. a crew member for the L-A-D Buffalo River Handbook 2nd Edition by Ken Smith by Janet Parsch, Ozark Society Foundation Chair Ken Smith has done it again. The description of the new 28-mile 150 miles of hiking trails. The second edition of his wonderfully segment of the Buffalo River Trail / Handbook is a comprehensive successful first edition of Buffalo River Ozark Highlands Trail from U.S. reference book for the history and Handbook is available for purchase. -
Final-Draft-Revied-1-17-2020-Copy
Final Review Draft Revised 1/17/2020 Revisions are shown in red L’Anse Township, MI MASTER PLAN Update 2019 L’Anse Township Master Plan Acknowledgements L’Anse Township Planning Commission Roy Kemppainen, Chair Dan Robillard, Secreatary Joan Bugni Craig Kent Joanne Pennock Buddy Sweeney Mike Roberts L’Anse Township Board Peter Magaraggia, Supervisor Kristin Kahler, Clerk Kristine Rice, Treasurer Shelley Lloyd, Trustee Buddy Sweeney, Trustee Consultant: We also wish to thank the many citizens who attended meetings, the Open House Event, and who provided input on the development of this Master Plan! Cover photo: 2nd Sand Beach by Jeffery Loman Patrick Coleman, AICP Acknowledgements Page 1 L’Anse Township Master Plan Table of Contents Page Acknowledgements 1 Chapter 1: Introduction 3 Chapter 2: Township Profile 10 Chapter 3: Housing 39 Chapter 4: Infrastructure and Community Facilities 44 Chapter 5: Land Use 53 Chapter 6: Transportation 69 Chapter 7: Economic Development 80 Chapter 8: Action Plan 86 Table of Contents Page 2 L’Anse Township Master Plan Chapter 1: Introduction This plan was undertaken to help the citizens of L’Anse Township make informed decisions and set priorities and goals to achieve a sustainable future. The plan contains recommendations and action strategies to assist the Township to organize efforts and resources for maximum potential. The plan will serve as a guide for future decisions about growth management and development, land-use regulation, and infrastructure. Authority and Purpose The purpose of the Master Plan is to guide the future of the Township and help the community develop sustainably through a realistic and well thought out approach.