Eminent Railway Builders Nijipalities in L'euticto
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Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
USGS Topographic Maps of California
USGS Topographic Maps of California: 7.5' (1:24,000) Planimetric Planimetric Map Name Reference Regular Replace Ref Replace Reg County Orthophotoquad DRG Digital Stock No Paper Overlay Aberdeen 1985, 1994 1985 (3), 1994 (3) Fresno, Inyo 1994 TCA3252 Academy 1947, 1964 (pp), 1964, 1947, 1964 (3) 1964 1964 c.1, 2, 3 Fresno 1964 TCA0002 1978 Ackerson Mountain 1990, 1992 1992 (2) Mariposa, Tuolumne 1992 TCA3473 Acolita 1953, 1992, 1998 1953 (3), 1992 (2) Imperial 1992 TCA0004 Acorn Hollow 1985 Tehama 1985 TCA3327 Acton 1959, 1974 (pp), 1974 1959 (3), 1974 (2), 1994 1974 1994 c.2 Los Angeles 1994 TCA0006 (2), 1994, 1995 (2) Adelaida 1948 (pp), 1948, 1978 1948 (3), 1978 1948, 1978 1948 (pp) c.1 San Luis Obispo 1978 TCA0009 (pp), 1978 Adelanto 1956, 1968 (pp), 1968, 1956 (3), 1968 (3), 1980 1968, 1980 San Bernardino 1993 TCA0010 1980 (pp), 1980 (2), (2) 1993 Adin 1990 Lassen, Modoc 1990 TCA3474 Adin Pass 1990, 1993 1993 (2) Modoc 1993 TCA3475 Adobe Mountain 1955, 1968 (pp), 1968 1955 (3), 1968 (2), 1992 1968 Los Angeles, San 1968 TCA0012 Bernardino Aetna Springs 1958 (pp), 1958, 1981 1958 (3), 1981 (2) 1958, 1981 1981 (pp) c.1 Lake, Napa 1992 TCA0013 (pp), 1981, 1992, 1998 Agua Caliente Springs 1959 (pp), 1959, 1997 1959 (2) 1959 San Diego 1959 TCA0014 Agua Dulce 1960 (pp), 1960, 1974, 1960 (3), 1974 (3), 1994 1960 Los Angeles 1994 TCA0015 1988, 1994, 1995 (3) Aguanga 1954, 1971 (pp), 1971, 1954 (2), 1971 (3), 1982 1971 1954 c.2 Riverside, San Diego 1988 TCA0016 1982, 1988, 1997 (3), 1988 Ah Pah Ridge 1983, 1997 1983 Del Norte, Humboldt 1983 -
Calgary Climber Brian Greenwood
100 NEW ROUTE ON THE GRAND PILlER D'ANGLE II am. Suddenly we have a wide view of the south side of Mont Blanc-weare on the top of the frontal face of the Grand Pilier d'Angle. A light plane dives straight towards us. Photos. A sip of tea. Pitons are thrown away-for luck ... and to lighten the burden. Our crampons dig into the softened ice. Wefeel the weight of the snow balling on them. The last rocks become an island for castaways. Six hours of drift in the warmed slush. The sun dips behind Mont Blanc de Courmayeur; the snow hardens. We force the pace to the limit. Over a cornice I reach the top of the ridge. It is 9 pm. The sun is just above the horizon. A fabulous play of colours. An overpowering red in every crystal of snow. Secret dark blue valleys. Distant grey-green. I had to share this. I pull the rope violently, telling them to hurry. Sixty metres is a long way. The blazing ball is sinking. They are just in time! At 10 pm we were in the longed-for"\ allot hut. SUMMARY Mont Blanc, South-east face of Grand Pilier d'Angle by new route to the left of the Bonatti-Gobbi route 15-20 July 1969. E. Chrobak, T. Laukajtys, A. Mroz. ED 250 pitons. Technical note p 137. 64 Howse Peak (left) and Chephren Peak showing the East faces. Photo: W. R. Joyce Calgary climber Brian Greenwood Canada is a very big country, but, being a climber, I wouldn't really care if a line running slightly west of north were drawn through Calgary and that part to the east were cast adrift. -
ICEFIELDS PARKWAY Driving Guide
ICEFIELDS PARKWAY driving guide an eBook from Parkways of the Canadian Rockies, the region’s original and most comprehensive driving guide | by Brian Patton CONTENTS 2 Herbert Lake .................................................................................................................. 4 Crowfoot Glacier ....................................................................................................... 6 Bow Lake ........................................................................................................................... 7 Peyto Lake ........................................................................................................................ 9 Upper Waterfowl Lake ........................................................................................ 11 Lower Waterfowl Lake ........................................................................................ 11 Mistaya Canyon ........................................................................................................... 12 David Thompson Highway ............................................................................... 14 Rampart Creek ............................................................................................................. 15 Graveyard Flats ............................................................................................................ 15 Weeping Wall ............................................................................................................... 16 Big Bend ............................................................................................................................ -
HIGHWAY North America, but Certainly One of the Most Access WHY ARE GLACIERS RECEDING ? to Support a Tremendous Weight
THE COLUMBIA ICE-FIELD mass of ice in the valley reaches lower altitudes CARRYING POWER ATHABASCA GLACIER melting takes place during the summer months, CANADA'S The Columbia Ice-field, centre of the greatest One of the most interesting characteristics of a forming glacial streams. The Athabasca Glacier has been receding rapidly CANADA'S ICE-FIELD known accumulation of ice in the Rocky Mountains, glacier is its carrying power. Although it is in motion in recent years. Records of the Water Resources is not only one of the most interesting ice-fields in like a plastic substance, it is solid and strong enough Division of the Engineering and Water Resources HIGHWAY North America, but certainly one of the most access WHY ARE GLACIERS RECEDING ? to support a tremendous weight. Debris torn from Branch, Department of Northern Affairs and National ible. Near the Highway, it lies astride the British the mountainside obscures its edge, so that often The present glaciers are the remnants of the con Resources, show that the average yearly recession Columbia-Alberta boundary and at the dividing line one may walk 50 yards out before the ice can be tinental ice-cap which once covered a large part of (1945-1949) has been 102 feet. It has well-defined between Banff and Jasper National Parks. seen. This fringe of broken rock carried on the edge HI-FI ELD the northern half of this continent. In earlier times and apparently recently formed terminal and mar Scenic beyond adequate description, this spectac of the glacier is called a marginal moraine. -
TG 2018 ODM PRINT FINAL 2018-12-06.Pdf;1 Cockscomb Mountain Southwest Lyell Glaciers Ego Mountain Lens Mountain Sullivan River
Cockscomb Mountain Ego Mountain Southwest Lyell Glaciers Lens Mountain Sullivan River Prattle Creek Sir James Glacier Waterfowl La Clytte Mountain Division Mountain Lakes Vertebrae Ridge Epaulette Mountain Kemmel Mountain Mons Glacier Noyes Creek North Glacier East Glacier Waterfowl Mount Forbes Mount Chephren Waputik Mountains Stovepipe Mountain Mons Icefield Lakes Alpland Creek Lyell Creek West Glacier South Glacier Banff White Pyramid Ladylove Mountain Rocky Mountains Icefall Lodge Mons Peak Lid Mountain Golden Eagle Peak Chephren Lake 93 Mons Icefield Mount David Thompson National Sophist Mountain Poker Mountain Bush River Howse Peak Bush Mountain Cambrai Mountain Cirque Silverhorn Creek Garrett Creek Icefall Peak Mons Creek Messines Mountain Forbes Creek Aiguille Peak Kitchen Range Vertebrae Ridge Goat Peak Lake Mount Weed Park Mount Synge Midway Peak Bush Peak Solitude Mountain Freshfield Waputik Mountains Stairway Peak Rostrum Peak Icefall Brook Creek Mistaya River Aries Peak This is a Motorized Corridor Bush Mountain Valenciennes Mountain Caribou Creek Chatter Creek Through Non-Motorized Terrain. Arras Mountain Ebon Peak Capricorn Silverhorn Mountain Conway Creek Ebon Creek Lake Stay On The Road Marmot Mountain Dolomite Creek Vertebrae Ridge Breaker Mountain Conway Group Snowbird Glacier Zillebeke Mountain Niverville Glacier Glacier Lake Observation Peak Game Creek Capricorn Glacier Mount Conway Mount Patterson OUTDOOR DISCOVERY MAP Nixon Creek Chatter Creek Lodge Navy Creek Breaker Creek Parapet Glacier Barbette Glacier Corsair -
THE COLUMBIA ICE-FIELD That the Athabasca and Nearby Dome Glaciers Were Ice-Falls and Transverse Crevasses—Passing Over Joined at One Time
CANADA'S ICE-FIELD THE COLUMBIA ICE-FIELD that the Athabasca and nearby Dome Glaciers were Ice-falls and transverse crevasses—Passing over joined at one time. an uneven bed, the body of a glacier is first bent in CANADA'S one direction and then in the other. When the slope HIGHWAY The Columbia Ice-field, centre of the greatest known The present glaciers are remnants of the immense increases, great openings are formed across the glacier accumulation of ice in the Rocky Mountains, is not continental ice-cap which once covered a large part which are known as transverse crevasses, as they only one of the most interesting ice-fields in North of the northern half of this continent. usually occur almost at right angles to the direction of America but also one of the most accessible. Near the Although in general glaciers are shrinking, it will the flow. The ice at this point may form in great steps Defying description, this spectacular highway ranks highway it straddles the British Columbia-Alberta be centuries before these mighty fortresses of ice give with crevasses between them. This is known as an among the great "highroads" of the world. Its entire border and lies across the boundary of Banff and up their claim on the Rocky Mountains. ice-fall. Iffi-FI ELD Jasper National Parks. length of 142 miles commands some of the most Glacier tables—Medium-sized rocks, a few feet breath-taking and majestic scenery in the Canadian With its outlet glaciers, the Columbia Ice-field covers Glacier Formation and Recession across, called glacier tables, are left standing on Rockies. -
California Quad Search
NORTHERN CALIFORNIA QUAD SEARCH Brookings Mount Emily Fourth of July Creek Biscuit Hill Buckskin Peak O'Brien Takilma Oregon Caves Grayback Mountain Carberry Creek Squaw Lakes Dutchman Peak Siskiyou Peak Mount Ashland Siskiyou Pass Soda Mountain Parker Mountain Mule Hill Chicken Hills Hamaker Mountain Worden Lost River Merrill Malin Bryant Mountain Langell Valley Brady Butte Antler Point Strawberry Butte Dog Lake Fitzwater Point West Side Crane Creek Crane Mountain Collins Rim May Lake Smith River High Divide High Plateau Mountain Shelly Creek Ridge Broken Rib Mountain Polar Bear Mountain Deadman Point Figurehead Mountain Kangaroo Mountain Dutch Creek Condrey Mountain Buckhorn Bally Cottonwood Peak Hornbrook Iron Gate Reservoir Copco Secret Spring Mountain Sams Neck Dorris Sheepy Lake Lower Klamath Lake Hatfield Tulelake Newell Carr Butte Sagebrush Butte Steele Swamp Weed Valley Beaver Mountain Pease Flat West of Willow Ranch Willow Ranch Mount Bidwell Lake Annie Barrel Springs Crescent City OE W Crescent City Hiouchi Gasquet Hurdygurdy Butte Devils Punchbowl Preston Peak Happy Camp Slater Butte Seiad Valley Hamburg Horse Creek McKinley Mountain Badger Mountain Hawkinsville Bogus Mountain Dewey Gulch Panther Rock MacDoel Sheep Mountain Red Rock Lakes Mount Dome Captain Jacks Stronghold The Panhandle Copic Double Head Mountain Pinnacle Lake Pothole Valley Hager Basin Del Norte South Mountain McGinty Reservoir McGinty Point Sugar Hill Fort Bidwell Larkspur Hills Crooks Meadow Sister Rocks Childs Hill Cant Hook Mountain Ship Mountain Prescott -
The Story of the Mountains in Banff National Park
THE STORY OF THE MOUNTAINS IN BANFF NATIONAL PARK By Helen R. Belyea GEOLOGICAL SURVEY OF CANADA TNI STORY OF THE MOUNTAINS BANFF NATIONAL PARK Issued by GEOLOGICAL SURVEY OF CANADA Department of Mines and Technical Surveys Ottawa Price: .75 85261-6—1 THE QUEEN'S PRINTER AND CONTROLLER OF STATIONERY OTTAWA. 1950 Cat. No. M40-2160 Figure 1. View from top of Sulphur Mountain. Ranges of mountains and intermontane valleys trend in a northwesterly direction. Bow River, the highways and railway line cut across the mountains 3,500 feet below and Banff nestles in the valley between Tunnel and Sulphur Mountains. The grey limestone cliffs consist of sediments deposited during the Palaeozoic, the time of ancient life. The layers of rock dip west off the peaks into the valleys. Younger rocks of the Mesozoic, the time of medieval life, underlie the valleys between the ranges. The older Palaeozoic rocks of the mountains were pushed from the west along thrust faults over the Mesozoic rocks of the valleys. The thrust faults are located approximately at the base of the grey rocks on the east face of each mountain range. The lower slopes of the mountains were smoothed by glaciers during the Ice Age but the jagged peaks projected above the ice. Numerous cirques and hanging valleys are visible from here. The following letters refer to the ages of the rock formations: C - Cambrian; O - Ordovician; D - Devonian; M - Mississippian; Me - Mesozoic. 85261-6—H CONTENTS Page The Rocks 4 The Building of the Mountains 12 Mountain Sculpture 13 Drainage Patterns 17 Glossary -
Download Escaladarocosascanadienses.Pdf
ROCOSAS :Plantilla Pyrenaica 6/8/08 18:42 Página 156 Escalada ROCOSAS CANADIENSES “OBSESIONADOS POR LAS AGUAS HELADAS” Jonatan Larrañaga ITUADAS a lo largo de la frontera entre Alberta y la parar el coche y catalejo en mano poder Columbia Británica, las Montañas Rocosas observar esas columnas y rayas de hielo, Canadienses, están localizadas dentro de dos efímeras, que cuelgan del Monte Rundle, S estaban finas y alguna de ellas no llegaba al imponentes Parques Nacionales : el de Banff, al Sur, que fue suelo, así que habría que estudiarlas mas el primer santuario oficial de la vida salvaje en Canadá y el detalladamente y hablar con los locales. de Jasper al Norte, mas inexplorado que el primero. Los primeros días fueron de toma de contacto, de hacer kilómetros con el Estamos a primeros de febrero de 2008, tercera incursión en la zona y que ha coche y vichear posibles líneas escal- después de escalar varias vías alpinas por tenido la oportunidad de escalar casi todo ables. Abrimos la libreta con Némesis, en los Pirineos y pasar algo de miedo debido lo bueno y difícil de las Rockies. El segundo el Stanley Valley (Uno de los valles con al calor y a la caída de proyectiles de hielo, es, Jordi Corominas, que también le gusta más potencial, de vías alpinas de hielo y nos decantamos por cruzar el charco y ver lo de estar a -20ºC, abrir huella y escalar mixto de entre 3 y 5 largos). Dani y Jordi, si tenemos más éxito por las Rocky Moun- largos verticales que no se acaban nunca. -
The Coast Range of British Columbia
1 THE ALASKAN PANHANDLE and NORTH BRITISH COLUMBIA: A CLIMBER’S GUIDE. By Earle R. Whipple and Steven C. Gruhn Even today, the Alaskan Panhandle and the Coast Range (Coastal Ranges) of British Columbia are two of the wildest and most unknown ranges in the world. It is a land of high mountains, long distances, difficult access, long fjords (inlets), big inland lakes, large glaciers and icefields, powerful rivers and deep valleys with undergrowth. When measured from north-northwest to south-southeast, British Columbia is 1600 km (1000 miles) long, up to 800 km wide in the north, but narrower in the south, and is endowed with several cordilleras, of which the Coast Range and the Canadian Rockies are the longest. Only a relatively few areas are routinely visited by mountaineers in Alaska and the northern Coast Range. There is excellent technical climbing in the Taku Group on the Mendenhall Towers. The Stikine Group has outstanding summits such as Oasis Peak, the Devil’s Thumb, Cat’s Ears Spire and the Witch’s Tits, all on excellent rock and formidable. Numbers of traverses, both for summer and winter, abound. There are many easy summits and, along the coast, easy summits rise a bit above tree line with marvellous views not only of mountains but of the channels and islands. The Groups have inlets (fjords) and channels from the ocean, and climbers often approach their favourite peaks by boat, securing their craft against the coming tides. The famous American conservationist John Muir ascended the Snow Dome (Takhinsha Group) in 1888. The border between Alaska and British Columbia is long and the formal determination of the border produced much government- sponsored exploration and climbing by the United States and Canada in the years just before and after 1900.