2002-2003 North Cascades National Park Service Complex the Natural Resource Challenge R I He Popularity of National Parks Has Continued to A
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1 Recognising Glacial Features. Examine the Illustrations of Glacial Landforms That Are Shown on This Page and on the Next Page
1 Recognising glacial features. Examine the illustrations of glacial landforms that are shown on this C page and on the next page. In Column 1 of the grid provided write the names of the glacial D features that are labelled A–L. In Column 2 indicate whether B each feature is formed by glacial erosion of by glacial deposition. A In Column 3 indicate whether G each feature is more likely to be found in an upland or in a lowland area. E F 1 H K J 2 I 24 Chapter 6 L direction of boulder clay ice flow 3 Column 1 Column 2 Column 3 A Arête Erosion Upland B Tarn (cirque with tarn) Erosion Upland C Pyramidal peak Erosion Upland D Cirque Erosion Upland E Ribbon lake Erosion Upland F Glaciated valley Erosion Upland G Hanging valley Erosion Upland H Lateral moraine Deposition Lowland (upland also accepted) I Frontal moraine Deposition Lowland (upland also accepted) J Medial moraine Deposition Lowland (upland also accepted) K Fjord Erosion Upland L Drumlin Deposition Lowland 2 In the boxes provided, match each letter in Column X with the number of its pair in Column Y. One pair has been completed for you. COLUMN X COLUMN Y A Corrie 1 Narrow ridge between two corries A 4 B Arête 2 Glaciated valley overhanging main valley B 1 C Fjord 3 Hollow on valley floor scooped out by ice C 5 D Hanging valley 4 Steep-sided hollow sometimes containing a lake D 2 E Ribbon lake 5 Glaciated valley drowned by rising sea levels E 3 25 New Complete Geography Skills Book 3 (a) Landform of glacial erosion Name one feature of glacial erosion and with the aid of a diagram explain how it was formed. -
The Complete Script
Feb rua rg 1968 North Cascades Conservation Council P. 0. Box 156 Un ? ve rs i ty Stat i on Seattle, './n. 98 105 SCRIPT FOR NORTH CASCAOES SLIDE SHOW (75 SI Ides) I ntroduct Ion : The North Cascades fiountatn Range In the State of VJashington Is a great tangled chain of knotted peaks and spires, glaciers and rivers, lakes, forests, and meadov;s, stretching for a 150 miles - roughly from Pt. fiainier National Park north to the Canadian Border, The h undreds of sharp spiring mountain peaks, many of them still unnamed and relatively unexplored, rise from near sea level elevations to seven to ten thousand feet. On the flanks of the mountains are 519 glaciers, in 9 3 square mites of ice - three times as much living ice as in all the rest of the forty-eight states put together. The great river valleys contain the last remnants of the magnificent Pacific Northwest Rain Forest of immense Douglas Fir, cedar, and hemlock. f'oss and ferns carpet the forest floor, and wild• life abounds. The great rivers and thousands of streams and lakes run clear and pure still; the nine thousand foot deep trencli contain• ing 55 mile long Lake Chelan is one of tiie deepest canyons in the world, from lake bottom to mountain top, in 1937 Park Service Study Report declared that the North Cascades, if created into a National Park, would "outrank in scenic quality any existing National Park in the United States and any possibility for such a park." The seven iiiitlion acre area of the North Cascades is almost entirely Fedo rally owned, and managed by the United States Forest Service, an agency of the Department of Agriculture, The Forest Ser• vice operates under the policy of "multiple use", which permits log• ging, mining, grazing, hunting, wt Iderness, and alI forms of recrea• tional use, Hov/e ve r , the 1937 Park Study Report rec ornmen d ed the creation of a three million acre Ice Peaks National Park ombracing all of the great volcanos of the North Cascades and most of the rest of the superlative scenery. -
Upper Skagit
A GUIDE TO PEOPLE AND PLACES OF THE UPPER SKAGIT BOB MIERENDORF AND GERRY COOK NORTH CASCADES NATIONAL PARK SERVICE COMPLEX NORTH CASCADES INSTITUTE JULY 22–25 2010 1 CLASS FIELD DAYS ITINERARY PEOPLE AND PLACES OF THE UPPER SKAGIT RIVER JULY 22–25, 2010 FRIDAY 9 am Drive from ELC to Ross Dam Trailhead parking lot 9:15–10:00 Hike to Ross Lake (end of haul road) – Brief stop on trail at a Ross Dam overlook – Load ourselves and gear on the Mule 10:30 am Welcome to the Wild Upper Skagit – Rules of the Mule and other safety matters – Instructor and participant introductions Noon Lunch on the Mule near Big Beaver Creek 2:45 pm Second stop near May Creek (no rest rooms here) 6 pm Arrive at Lightning Horse Camp (our base camp for two nights) 7 pm Potluck dinner SATURDAY 7 am Breakfast 8 am–Noon Ethnobotany hike along Eastbank Trail – About a two mile hike, rolling terrain – Gerry will pick us up with the Mule – Lunch on the Mule 1 pm Quick rest room stop at Boundary Bay Campground 3 pm Arrive at International Boundary 3:15 pm Stop at Winnebago Flats – There are toilets here – Get drinking water and fill water jugs 3:45 pm Depart Winnebago Flats on return trip 5 pm Arrive back at our camp 6:30 pm Potluck dinner SUNDAY ABOUT THE COVER 7 am Breakfast U.S. Forest Service, Mt. Baker 8 am Break camp and load Mule Ranger District, 1931 oblique 9 am Depart on Mule aerial facing 182o (south), of pre-impoundment Skagit River 10 am Arrive at Big Beaver Campground flood plain; Skymo Creek canyon – There are rest rooms here in lower right, Devil’s Creek canyon – Hike up Big Beaver to old growth cedar grove emerging from middle left. -
Helmy Beckey, 1925 – 2019 Helmut Fritz Beckey, Known As Helmy, Was Born in Seattle and Died in Munich, Germany, at Age 93
AAC Publications Helmy Beckey, 1925 – 2019 Helmut Fritz Beckey, known as Helmy, was born in Seattle and died in Munich, Germany, at age 93. In his youth, he established first ascents and new routes throughout the Cascades and elsewhere. Helmy learned the basics of climbing as a member of the Mountaineers, where his aptitude was recognized early. In 1940, he and his brother Fred, who was two years older, made two extensive excursions into the Picket Range. The teenagers climbed the west ridge of Mt. Thompson and made the first ascents of Forbidden Peak, Phantom Peak, Whatcom Peak, Mt. Challenger, Crooked Thumb, Luna Peak, Mt. Fury’s East Peak, McMillan Spire’s West Spire, and Inspiration Peak. In 1941, along with the numerous first ascents and new routes in the North Cascades he did with Fred, Helmy joined Lloyd Anderson, Lyman Boyer, and Tom Campbell in the Bugaboos of British Columbia, where they completed the first ascent of the South Tower of Howser Spire. In the summer of 1942, Helmy and Fred embarked on a six-week expedition into the Coast Mountains of British Columbia. Here, the teenage brothers famously climbed the remote and challenging Mt. Waddington. It was only the second ascent of the peak, which had repelled a multitude of summit attempts. Fred Beckey wrote in the 1943 AAJ about the descent: “Helmy was hit on the knee by one of a flurry of rocks that sped down the mountain side. All hope of reaching camp that night was gone because of a heavily bleeding cut. This was Helmy’s 17th birthday present, donated by Mt. -
Washington State's Scenic Byways & Road Trips
waShington State’S Scenic BywayS & Road tRipS inSide: Road Maps & Scenic drives planning tips points of interest 2 taBLe of contentS waShington State’S Scenic BywayS & Road tRipS introduction 3 Washington State’s Scenic Byways & Road Trips guide has been made possible State Map overview of Scenic Byways 4 through funding from the Federal Highway Administration’s National Scenic Byways Program, Washington State Department of Transportation and aLL aMeRican RoadS Washington State Tourism. waShington State depaRtMent of coMMeRce Chinook Pass Scenic Byway 9 director, Rogers Weed International Selkirk Loop 15 waShington State touRiSM executive director, Marsha Massey nationaL Scenic BywayS Marketing Manager, Betsy Gabel product development Manager, Michelle Campbell Coulee Corridor 21 waShington State depaRtMent of tRanSpoRtation Mountains to Sound Greenway 25 Secretary of transportation, Paula Hammond director, highways and Local programs, Kathleen Davis Stevens Pass Greenway 29 Scenic Byways coordinator, Ed Spilker Strait of Juan de Fuca - Highway 112 33 Byway leaders and an interagency advisory group with representatives from the White Pass Scenic Byway 37 Washington State Department of Transportation, Washington State Department of Agriculture, Washington State Department of Fish & Wildlife, Washington State Tourism, Washington State Parks and Recreation Commission and State Scenic BywayS Audubon Washington were also instrumental in the creation of this guide. Cape Flattery Tribal Scenic Byway 40 puBLiShing SeRviceS pRovided By deStination -
Toolstone Geography in the Northern Cascades of Washington and Adjacent Areas
CHAPTER 6 Toolstone Geography in the Northern Cascades of Washington and Adjacent Areas Robert R. Mierendorf National Park Service (Retired), U. S. Department of Interior, 810 SR 20, Sedro Woolley, WA 98284- 1239 ([email protected]); Kevin E. Baldwin 1014 151st Ave SE, Bellevue WA 98007 ([email protected]) Background to the Study of North Cascades Toolstone The northern Cascade Mountain Range, or North 1986). The park and its immediately adjacent lands Cascades, extends 220 km from northeast of the encompass the core area of a distinctive toolstone town of Hope, British Columbia, to Snoqualmie landscape whose rich suite of rock types offered a Pass in Washington State. The geographic center of variety of utilitarian options to pre-contact the North Cascades is within the North Cascades populations. Reflecting for the most part National Park Service Complex (the park) and geographic variation in bedrock lithology, this suite adjacent lands. The park (Figure 6-1) takes in of toolstone types differs from the variety of remote alpine terrain comprising the most heavily toolstone used in the foothill, lower riverine valley, glaciated portion of the range in the convergent and littoral landscapes that surround the North headwaters of the three largest regional rivers - the Cascades. Even within the North Cascades interior, Columbia, the Fraser, and the Skagit. Park lands on the abundance and type of toolstone in the western slopes extend from the border with archaeological assemblages vary significantly Canada, south along the upper Skagit River; park within and between watersheds. land extends east across the Cascade crest to Archaeological evidence indicates that, hardly include the upper end of Lake Chelan. -
1968 Mountaineer Outings
The Mountaineer The Mountaineer 1969 Cover Photo: Mount Shuksan, near north boundary North Cascades National Park-Lee Mann Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during June by The Mountaineers, P.O. Box 122, Seattle, Washington 98111. Clubroom is at 7191h Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. EDITORIAL STAFF: Alice Thorn, editor; Loretta Slat er, Betty Manning. Material and photographs should be submitted to The Mountaineers, at above address, before Novem ber 1, 1969, for consideration. Photographs should be black and white glossy prints, 5x7, with caption and photographer's name on back. Manuscripts should be typed double-spaced and include writer's name, address and phone number. foreword Since the North Cascades National Park was indubi tably the event of this past year, this issue of The Mountaineer attempts to record aspects of that event. Many other magazines and groups have celebrated by now, of course, but hopefully we have managed to avoid total redundancy. Probably there will be few outward signs of the new management in the park this summer. A great deal of thinking and planning is in progress as the Park Serv ice shapes its policies and plans developments. The North Cross-State highway, while accessible by four wheel vehicle, is by no means fully open to the public yet. So, visitors and hikers are unlikely to "see" the changeover to park status right away. But the first articles in this annual reveal both the thinking and work which led to the park, and the think ing which must now be done about how the park is to be used. -
North Cascades National Park I Mcallister Cutthroat Pass A
To Hope, B.C. S ka 40mi 64km gi t R iv er Chilliwack S il Lake v e CHILLIWACK LAKE SKAGIT VALLEY r MANNING - S k a g PROVINCIAL PARK PROVINCIAL PARK i PROVINCIAL PARK t Ross Lake R o a d British Columbia CANADA Washington Hozomeen UNITED STATES S i Hozomeen Mountain le Silver Mount Winthrop s Sil Hoz 8066ft ia ve o Castle Peak 7850ft Lake r m 2459m Cr 8306ft 2393m ee e k e 2532m MOUNT BAKER WILDERNESS Little Jackass n C Mount Spickard re Mountain T B 8979ft r e l e a k i ar R 4387ft Hozomeen Castle Pass 2737m i a e d l r C ou 1337m T r b Lake e t G e k Mount Redoubt lacie 4-wheel-drive k r W c 8969ft conditions east Jack i Ridley Lake Twin a l of this point 2734m P lo w er Point i ry w k Lakes l Joker Mountain e l L re i C ak 7603ft n h e l r C R Tra ee i C i Copper Mountain a e re O l Willow 2317m t r v e le n 7142ft T i R k t F a e S k s o w R Lake a 2177m In d S e r u e o C k h g d e u c r Goat Mountain d i b u i a Hopkins t C h 6890ft R k n c Skagit Peak Pass C 2100m a C rail Desolation Peak w r r T 6800ft li Cre e ave 6102ft er il ek e e Be 2073m 542 p h k Littl 1860m p C o Noo R C ks i n a Silver Fir v k latio k ck c e ee Deso e Ro Cree k r Cr k k l e il e i r B e N a r Trail a C To Glacier r r O T r C Thre O u s T e Fool B (U.S. -
VACATION LAND the National Forests in Oregon
VACATION LAND The National Forests in Oregon High up in the mountains, where the timber is scarce and stunted and the only means of transportation is by horseback United States Department of Agriculture::Forest Service 1919 WELCOME TO THE ATIONAL PORESTS U.S.DEPARTVENT OFAGRICULTURE FOREST SIEIRVICE UNITED STATES DEPARTMENT OF AGRICULTURE DEPARTMENT CIRCULAR 4 Contribution from the Forest Service HENRY S. GRAVES. Forester DIRECTORY OF NATIONAL FORESTS IN OREGON. George H. Cecil, District Forester. District Office, Post Office Building, Portland, Oreg. NATIONAL FOREST. FOREST SUPERVISOR. HEADQUARTERS. Cascade C. R. Seitz Eugene, Oreg. 2- Crater H B Rankin Medford, Oreg. Deschutes N. G. Jacobson Bend, Oreg. H Fremont...... Gilbert D. Brown Lakeview, Oreg. -Maiheur Cy J. Bingham John Day, Oreg. L-Milaam R. M. Evans.... Baker, Oreg. - Ochoco.. V. V. Harpham Prineville, Oreg. Oregon H. Sherrard...... Portland, Oreg. Santiam C. C. Hall.. Albany, Oreg. -Siskiyou.... N. F. Macduff Grants Pass, Oreg. Siuslaw R. S. Shelley Eugene, Oreg. \-Umati1la W. W. Cryder Pendleton, Oreg. 13 .Umpqua C. Bartrum Roseburg, Oreg. j Wallowa H. W. Harris Wallowa, Oreg. S'Wenaha J. C. Kulins Walla Walla, Wash. l,Whitman R. M. Evans.... Baker, Oreg. The view on page s of the cover is a reprodtction from a photograph of Mount Jefferson, Sautiam National Forest, showing forest and snow peak. THE NATIONAL VACATION 1 ANDESTS IN OREGON AN IDEAL VACATION LAND HEN, tired of the daily grind, you say to yourself, "I need a vacation," your first thought is to get away from civili- zation and its trammels.Your next is to find interest- ing and health-giving recreation.In the National For- ests in Oregon you may find both, and much besides. -
Glaciers and Glacial Erosional Landforms
GLACIERS AND GLACIAL EROSIONAL LANDFORMS Dr. NANDINI CHATTERJEE Associate Professor Department of Geography Taki Govt College Taki, North 24 Parganas, West Bengal Part I Geography Honours Paper I Group B -Geomorphology Topic 5- Development of Landforms GLACIER AND ICE CAPS Glacier is an extended mass of ice formed from snow falling and accumulating over the years and moving very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of accumulation, as in continental glaciers. • Ice Cap - less than 50,000 km2. • Ice Sheet - cover major portion of a continent. • Ice thicker than topography. • Ice flows in direction of slope of the glacier. • Greenland and Antarctica - 3000 to 4000 m thick (10 - 13 thousand feet or 1.5 to 2 miles!) FORMATION AND MOVEMENT OF GLACIERS • Glaciers begin to form when snow remains Once the glacier becomes heavy enough, it in the same area year-round, where starts to move. There are two types of enough snow accumulates to transform glacial movement, and most glacial into ice. Each year, new layers of snow bury movement is a mixture of both: and compress the previous layers. This Internal deformation, or strain, in glacier compression forces the snow to re- ice is a response to shear stresses arising crystallize, forming grains similar in size and from the weight of the ice (ice thickness) shape to grains of sugar. Gradually the and the degree of slope of the glacier grains grow larger and the air pockets surface. This is the slow creep of ice due to between the grains get smaller, causing the slippage within and between the ice snow to slowly compact and increase in crystals. -
GLACIATION in SNOWDONIA by Paul Sheppard
GeoActiveGeoActive 350 OnlineOnline GLACIATION IN SNOWDONIA by Paul Sheppard This unit can be used These remnants of formerly much higher mountains have since been independently or in Conwy conjunction with OS 1:50,000 eroded into what is seen today. The Bangor mountains of Snowdonia have map sheet 115. N Caernarfon Llanrwst been changed as a result of aerial Llanberis Capel Curig Snowdon Betws y Coed (climatic) and fluvial (water) HE SNOWDONIA OR ERYRI (Yr Wyddfa) Beddgelert Blaenau erosion that always act upon a NATIONAL PARK, established Ffestiniog T Porthmadog landscape, but in more recent SNOWDONIA Y Bala in 1951, was the third National NATIONAL Harlech geological times the effects of ice PARK Park to be established in England have had a major impact upon the and Wales following the 1949 Barmouth Abermaw Dolgellau actual land surface. National Parks and Access to the Cadair Countryside Act (Figure 1). It Idris Tywyn 2 Machynlleth Glaciation covers an area of 2,171 km (838 Aberdyfi 0 25 km square miles) of North Wales and Ice ages have been common in the British Isles and northern Europe, encompasses the Carneddau and Figure 1: Snowdonia National Park Glyderau mountain ranges. It also with 40 having been identified by includes the highest mountain in important to look first at the geologists and geomorphologists. England and Wales, with Mount geological origins of the area, as The most recent of these saw Snowdon (Yr Wyddfa in Welsh) this provides the foundation upon Snowdonia covered with ice as reaching a height of 1,085 metres which ice can act. -
Winter 2007-2008
THE WILD CASCADES THE JOURNAL OF THE NORTH CASCADES CONSERVATION COUNCIL WINTER 2007-2008 THE WILD CASCADES • Winter 2007-2008 THE NortH CASCADES THE WILD CASCADES Winter 2007-2008 ConSERVATIon CouncIL was formed in 1957 “To protect and In This Issue preserve the North Cascades’ scenic, 3 President’s Report — MARC BARDSLEY scientific, recreational, educational, and wilderness values.” Continuing 4 Stehekin River Corridor Implementation Plan: NCCC Perspective this mission, NCCC keeps government — DAVID FLUHARTY officials, environmental organizations, 6 Council Hires Executive Director and the general public informed about The Stehekin River Corridor Implementation Plan issues affecting the Greater North Cas- — CAROLYN MCCONNELL cades Ecosystem. Action is pursued 7 Wild Sky Wilderness Update through legislative, legal, and public Update: Granite Falls Motocross Park — BRUCE BARNBAUM participation channels to protect the 8 Big Dam Threatens Similkameen River — RICK MCGUIRE lands, waters, plants and wildlife. 11 Settlement Reached on Baker Salvage Appeal — KEVIN GERAGHTY Over the past third of a century the Collaboration? — For a seat at the negotiating table, they are jeopardiz- NCCC has led or participated in cam- ing their true role — ERICA ROSENBERG, LOS ANGELES TIMES paigns to create the North Cascades 12 Luna Cirque — TOM HAMMOND National Park Complex, Glacier Peak 15 Fifty Years of Research at South Cascade Glacier Wilderness, and other units of the — WENDELL TANGBORN National Wilderness System from the W.O. Douglas Wilderness north to the 19 Ski Area Mania Trashes Backcountry — MARK LAWLER, SIERRA CLUB Alpine Lakes Wilderness, the Henry M. CASCADE CHAPTER Jackson Wilderness, the Chelan-Saw- 20 In Memoriam: Bella Caminiti, Marion Hessey and William K.