Along the Altsetnaey Nalcine Trail
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Technical Paper No. 421 Harvest and Use of Wild Resources In
Technical Paper No. 421 Harvest and Use of Wild Resources in Northway, Alaska, 2014, with special attention to nonsalmon fish by Anna R. Godduhn and Marylynne L. Kostick November 2016 Alaska Department of Fish and Game Division of Subsistence Symbols and Abbreviations The following symbols and abbreviations, and others approved for the Système International d'Unités (SI), are used without definition in the reports by the Division of Subsistence. All others, including deviations from definitions listed below, are noted in the text at first mention, as well as in the titles or footnotes of tables, and in figure or figure captions. Weights and measures (metric) General Mathematics, statistics centimeter cm Alaska Administrative Code AAC all standard mathematical signs, symbols deciliter dL all commonly-accepted and abbreviations gram g abbreviations e.g., alternate hypothesis HA hectare ha Mr., Mrs., base of natural logarithm e kilogram kg AM, PM, etc. catch per unit effort CPUE kilometer km all commonly-accepted coefficient of variation CV liter L professional titles e.g., Dr., Ph.D., common test statistics (F, t, χ2, etc.) meter m R.N., etc. confidence interval CI milliliter mL at @ correlation coefficient (multiple) R millimeter mm compass directions: correlation coefficient (simple) r east E covariance cov Weights and measures (English) north N degree (angular ) ° cubic feet per second ft3/s south S degrees of freedom df foot ft west W expected value E gallon gal copyright greater than > inch in corporate suffixes: greater than or equal to ≥ mile mi Company Co. harvest per unit effort HPUE nautical mile nmi Corporation Corp. -
Mount Sanford…Errrr, Mount Jarvis. Wait, What?? Mount Who?? It Was Roughly Around Thanksgiving 2016 and the Time Had Come Fo
Mount Sanford…errrr, Mount Jarvis. Wait, what?? Mount Who?? It was roughly around Thanksgiving 2016 and the time had come for me to book my next IMG adventure. With two young children at home and no family close by, I had settled into a routine of doing a big climb every other year. This year was a bit different, as I normally book my major climbs around September for an April or May departure the following year. However, due to a Mt. Blackburn (Alaska) trip falling through, I had to book another expedition. In 2015, I was on an IMG team that summitted Mt. Bona from the north side, not the original plan (jot that down – this will become a theme in Alaska), and really enjoyed the solitude, adventure, physical challenge, small team, and lack of schedule the Wrangell & St Elias Mountains had to offer. So, I hopped on IMG’s website, checked out the scheduled Alaskan climb for 2017, which was Mt. Sanford, and peppered George with my typical questions. Everything lined up, so I completed the pile of paperwork (do I really have to sign another waiver?!?), sent in my deposit (still no AMEX, ugh…), set my training schedule, and started Googling trip reports about Mt. Sanford. Little did I know that READING about Mt. Sanford was the closest I would ever get to it! Pulling from my previous Alaskan climbing experience, I was better prepared for this trip than for Mt Bona in 2015. Due to our bush pilot’s inability to safely land us on the south side of Bona two years prior, we flew up, around, and over the mountain and landed on the north side. -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
P1616 Text-Only PDF File
A Geologic Guide to Wrangell–Saint Elias National Park and Preserve, Alaska A Tectonic Collage of Northbound Terranes By Gary R. Winkler1 With contributions by Edward M. MacKevett, Jr.,2 George Plafker,3 Donald H. Richter,4 Danny S. Rosenkrans,5 and Henry R. Schmoll1 Introduction region—his explorations of Malaspina Glacier and Mt. St. Elias—characterized the vast mountains and glaciers whose realms he invaded with a sense of astonishment. His descrip Wrangell–Saint Elias National Park and Preserve (fig. tions are filled with superlatives. In the ensuing 100+ years, 6), the largest unit in the U.S. National Park System, earth scientists have learned much more about the geologic encompasses nearly 13.2 million acres of geological won evolution of the parklands, but the possibility of astonishment derments. Furthermore, its geologic makeup is shared with still is with us as we unravel the results of continuing tectonic contiguous Tetlin National Wildlife Refuge in Alaska, Kluane processes along the south-central Alaska continental margin. National Park and Game Sanctuary in the Yukon Territory, the Russell’s superlatives are justified: Wrangell–Saint Elias Alsek-Tatshenshini Provincial Park in British Columbia, the is, indeed, an awesome collage of geologic terranes. Most Cordova district of Chugach National Forest and the Yakutat wonderful has been the continuing discovery that the disparate district of Tongass National Forest, and Glacier Bay National terranes are, like us, invaders of a sort with unique trajectories Park and Preserve at the north end of Alaska’s panhan and timelines marking their northward journeys to arrive in dle—shared landscapes of awesome dimensions and classic today’s parklands. -
Observations of Migrating Golden Eagles (Aquila Chrysaetos) in Eastern Interior Alaska Offer Insights on Population Size and Migration Monitoring
J. Raptor Res. 50(3):254–264 Ó 2016 The Raptor Research Foundation, Inc. OBSERVATIONS OF MIGRATING GOLDEN EAGLES (AQUILA CHRYSAETOS) IN EASTERN INTERIOR ALASKA OFFER INSIGHTS ON POPULATION SIZE AND MIGRATION MONITORING 1 CAROL L. MCINTYRE Denali National Park and Preserve, 4175 Geist Road, Fairbanks, AK 99709 U.S.A. STEPHEN B. LEWIS U.S. Fish and Wildlife Service, 3000 Vintage Boulevard, Suite 201, Juneau, AK 99801 U.S.A. ABSTRACT.—Migratory Golden Eagles (Aquila chrysaetos) from Alaska winter across a vast region of western North America, much of which is undergoing rapid change from a diversity of indirect and direct human activities. To address recent conservation concerns, we are studying the year-round movements of migratory Golden Eagles from interior and northern Alaska to identify and evaluate potential risks to their survival. We are also developing new survey techniques to estimate population size and trends. As part of our ongoing studies, we observed migrating Golden Eagles in spring and autumn 2014 during field investigations to locate Golden Eagle capture sites in eastern interior Alaska, and in spring 2015 during capture activities. We observed large numbers of Golden Eagles in both spring and autumn, suggesting that the Mentasta Mountains are an important migration corridor for this species. Further, our observations, including 1364 migrating Golden Eagles in October 2014, suggested that the Alaska Golden Eagle population is much larger than is reflected in the only currently available statewide population estimate of 2400 eagles. In combination with historical and contemporary tracking studies, our observations in the Mentasta Mountains provide important new information about Golden Eagle migration in Alaska and stimulate interest in answering fundamental questions about using counts of migrating Golden Eagles to estimate, and detect change in, the population size of Alaska’s migratory Golden Eagles. -
Historical Crossroads of Alaska Neil Hannan Photo
Wrangell-St. Elias National Park & Preserve National Park Service U.S. Department of the Interior Wrangell-St. Elias National Park & Preserve 2009 Visitor Guide Richardson Highway, Milepost 88 Historical Crossroads of Alaska Neil Hannan photo THE 13.2 MILLION ACRES WHICH COMPRISE traditional subsistence hunting and fishing, but many others Wrangell-St. Elias National Park and Preserve have for centuries who visit our largest national park come for recreation or to Inside: served as a crossroads of human activity. Russians began to enter learn. They come to face wilderness challenges, such as the area in the late 1700s. The subsequent United States purchase fording glacial stream or topping an ice-clad mountain. They of Alaska in the 1800s further spurred expeditions, but all come to monitor species of concern, such as Kittlitz's Welcome ..................................... 2 of these endeavors came long after people became murrelets or Mentasta caribou. They come to see active in this region 8,000 years ago. the largest glaciers in North America, or to Visitor Centers ........................... 3 study evidence of past human activity along Humans were drawn here to trade with other their receding margins. They come to What To Do? .............................. 4 groups for materials unavailable in their own experience the Kennecott Mill Town, which territories and by dreams of fur trapping, mineral once extracted the world's richest copper ore, Early Explorers ........................... 6 riches, and rivers teeming with salmon. They initially to follow in the footsteps of early stampeders were lured into this wild country of jagged peaks and along the Richardson Highway, or to feel the quiet Safety ........................................ -
North America Summary, 1968
240 CLIMBS A~D REGIONAL ?\OTES North America Summary, 1968. Climbing activity in both Alaska and Canada subsided mar kedly from the peak in 1967 when both regions were celebrating their centen nials. The lessened activity seems also to have spread to other sections too for new routes and first ascents were considerably fewer. In Alaska probably the outstanding climb from the standpoint of difficulty was the fourth ascent of Mount Foraker, where a four-man party (Warren Bleser, Alex Birtulis, Hans Baer, Peter Williams) opened a new route up the central rib of the South face. Late in June this party flew in from Talkeetna to the Lacuna glacier. By 11 July they had established their Base Camp at the foot of the South face and started up the rib. This involved 10,000 ft of ice and rotten rock at an angle of 65°. In the next two weeks three camps were estab lished, the highest at 13,000 ft. Here, it was decided to make an all-out push for the summit. On 24 July two of the climbers started ahead to prepare a route. In twenty-eight hours of steady going they finally reached a suitable spot for a bivouac. The other two men who started long after them reached the same place in ten hours of steady going utilising the steps, fixed ropes and pitons left by the first party. After a night in the bivouac, the two groups then contin ued together and reached the summit, 17,300 ft, on 25 July. They were forced to bivouac another night on the return before reaching their high camp. -
The Keltaeni
National Park Service U.S. Department of the Interior Park News + The Offcial Guide of Wrangell-St. Elias National Park and Preserve The K’ełt’aeni Volume 2019 OTHER PAGES YOU MIGHT LIKE: 3 Park Visitor 5 North District/ 8 South District/ Centers Nabesna Area Kennecott Area Activities & Itineraries 2 Bear Safety 4 The park has several visitor contact stations Picturesque scenery and mountain An adventure awaits the traveler who where you can get park information and viewing awaits the traveler who ventures ventures down the McCarthy Road to Nabesna Road Guide 6-7 down the Nabesna Road. Information historic McCarthy and the Kennecott Mill orientation from park rangers, as well as about the area and a road guide helps Town. Information about the area and a McCarthy Road Guide 10-11 view exhibits and the park flm. a traveler discover the mysteries of road guide helps a traveler discover the Nabesna. secrets of McCarthy-Kennecott. Information and Services 12 New Interpretive Exhibits at the Kennecott New Waysides at the Wrangell-St. Elias Mines National Historic Landmark Visitor Center in Copper Center The immersive exhibits include The interpretive waysides are personal stories of the workers located at the park entrance, and the families that lived in along the bluff trail and on Kennecott during the mining the Boreal Forest trail. The operation years from 1911 to outside panels describe the 1938. The displays include many scenic views of the Wrangell artifacts from the site that are on Mountains, the historic Valdez loan from local people or from Trail, an archeological site, the the park’s collection. -
Wrangell-St. Elias Alaska
Wrangell - St. Elias National Park Service National Park and National Preserve U.S. Department of the Interior Wrangell-St. Elias Alaska The wildness of Wrangell-St. Elias National Park The Alaska National Interest Lands Conservation vest harbor seals, which feed on fish and In late summer, black and brown bears, drawn and Preserve is uncompromising, its geography Act (ANILCA) of 1980 allows the subsistence marine invertebrates. These species and many by ripening soapberries, frequent the forests awe-inspiring. Mount Wrangell, namesake of harvest of wildlife within the park, and preserve more are key foods in the subsistence diet of and gravel bars. Human history here is ancient one of the park's four mountain ranges, is an and sport hunting only in the preserve. Hunters the Ahtna and Upper Tanana Athabaskans, and relatively sparse, and has left a light imprint active volcano. Hundreds of glaciers and ice find Dall's sheep, the park's most numerous Eyak, and Tlingit peoples. Local, non-Native on the immense landscape. Even where people fields form in the high peaks, then melt into riv large mammal, on mountain slopes where they people also share in the bounty. continue to hunt, fish, and trap, most animal, ers and streams that drain to the Gulf of Alaska browse sedges, grasses, and forbs. Sockeye, Chi fish, and plant populations are healthy and self and the Bering Sea. Ice is a bridge that connects nook, and Coho salmon spawn in area lakes and Long, dark winters and brief, lush summers lend regulati ng. For the species who call Wrangell the park's geographically isolated areas. -
The Glenn Highway EMBODIES ALL SIX QUALITIES of a SCENIC BYWAY
The Glenn Highway EMBODIES ALL SIX QUALITIES OF A SCENIC BYWAY. Scenic Historic Cultural Natural Recreational Archaeological This resource This resource Evidence and Those features of Outdoor Those offers a heightened encompasses expressions of the the visual recreational characteristics of visual experience legacies of the past customs or environment that activities are the scenic byways derived from the that are distinctly traditions of a are in a relatively directly associated corridor that are view of natural associated with distinct group of undisturbed state. with and physical evidence and man made physical elements people. Cultural These features dependent upon of historic or elements of the of the landscape, features include, predate the arrival the natural and prehistoric human visual environment whether natural or but are not limited of human cultural elements life or activity that of the scenic man made, that to crafts, music, populations and of the corridor’s are visible and byway corridor. are of such dance, rituals, may include landscape. capable of being The characteristics significance that festivals, speech, geological The recreational inventoried and of the landscape they educate the food, special formations, fossils, activities provide interpreted. The are strikingly viewer and stir an events, vernacular landform, water opportunities for scenic byway distinct and offer a appreciation of the architecture, etc. bodies, vegetation, active and passive corridor’s pleasing and most past. The historic and are currently and wildlife. There recreational archaeological memorable visual elements reflect practiced. The may be evidence of experiences. They interest, as experience. All the actions of cultural qualities of human activity but include, but are not identified through elements of the people and may the corridor could the natural features limited to downhill ruins, artifacts, landscape – include buildings, highlight one or reveal minimal skiing, rafting, structural remains landform, water, settlement more significant disturbances. -
Alaska Range and Environs
Research Paper THEMED ISSUE: Geologic Evolution of the Alaska Range and Environs GEOSPHERE Stitch in the ditch: Nutzotin Mountains (Alaska) fluvial strata and a dike record ca. 117–114 Ma accretion of Wrangellia with western GEOSPHERE, v. 16, no. 1 North America and initiation of the Totschunda fault https://doi.org/10.1130/GES02127.1 Jeffrey M. Trop1, Jeffrey A. Benowitz2, Donald Q. Koepp1, David Sunderlin3, Matthew E. Brueseke4, Paul W. Layer2, and Paul G. Fitzgerald5 18 figures; 3 tables; 1 set of supplemental files 1Department of Geology and Environmental Geosciences, Bucknell University, 701 Moore Avenue, Lewisburg, Pennsylvania 17837, USA 2Geophysical Institute and Geochronology Laboratory, University of Alaska–Fairbanks, Fairbanks, Alaska 99775, USA 3 CORRESPONDENCE: [email protected] Department of Geology and Environmental Geosciences, Lafayette College, Easton, Pennsylvania 18042, USA 4Department of Geology, Kansas State University, Manhattan, Kansas 66506, USA 5Department of Earth Sciences, Syracuse University, Syracuse, New York 13244, USA CITATION: Trop, J.M., Benowitz, J.A., Koepp, D.Q., Sunderlin, D., Brueseke, M.E., Layer, P.W., and Fitzgerald, P.G., 2020, Stitch in the ditch: Nutzotin ABSTRACT clasts. Deposition was occurring by ca. 117 Ma and following the subduction of intervening oceanic Mountains (Alaska) fluvial strata and a dike record ceased by ca. 98 Ma, judging from palynomorphs, lithosphere is a fundamental process in plate ca. 117–114 Ma accretion of Wrangellia with west- ern North America and initiation of the Totschunda The Nutzotin basin of eastern Alaska consists the youngest detrital ages, and ages of crosscut- dynamics and the growth of Earth’s continents. The fault: Geosphere, v. -
Mount Wrangell District, Alaska
A, Economic Qeol y, 25 Rofeasional Paper No. 15 Series{ B, Dwmiptins Q&, 80 DEPARTMENT OF THE INTERIOR UNlTED S'l'hTES GEOLOGICAL SURVEY CHARLES U. \flALCOTT, I)IRECTOR THE MINERAL RESOURCES OF THE MOUNT WRANGELL DISTRICT, ALASKA BY WALTER C, MENDENHALL AND FRANK C, SCHRADER WASHINGTON GOVERNMENT PRINTING OFFICE 1903 .I MOUNT WRANGELL. VIFW t-keri frnm thi, Giivr,~nment im1 above To~is~iaBr~iloe 41 mles from tire sumtnit of tits maunin,~ I; NkDlNA RIVER BARS, Mnunt Drum in backgniuncl. Page . Introduction ................................................................................ 9 Copper ................................................................................... 13 Southern area ......................................................................... 13 Location ................................................................ ., ....... 13 Routes and trails ................................................................. 13 Geologic sketch .................................................................. 14 Nikolai greenstone ............................................................. 14 Chitistone limestone .......................................................... 14 Triassic shales and limestones ............................ .. .......... 15 Kennicott formation .......................................................... 15 Intrusive rocks ............................................................... 15 Copper occurrences ............................................................... 16 General statement ...........................................................