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Field Notes in Support of a Revision of Hawaiian Carabidae
Field Notes in Support of a Revision of Hawaiian Carabidae James K. Liebherr* Cornell University Ithaca, NY, U.S.A. * Curator (Ret.) Cornell University Insect Collection, and Professor Emeritus 23 August 2021 Field Notes in Support of a Revision of Hawaiian Carabidae © 2021 by James K. Liebherr is licensed under Attribution-NonCommercial-NoDerivatives 4.0 International. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/4.0/ Cornell University Insect Collection John H. and Ann B. Comstock Hall Cornell University Ithaca, NY 14853-2601 U.S.A. ii Table of Contents Foreword ……………………………………………………………….…………………………. iv 00.—Introduction …………………………………………………………………..………….. 1 01.—Kauaˋi; 9-22 March, 10-16 May 1991 ……..…………………………...….... 7 02.—Hawaiˋi Island; 23 March-5 April 1991 ..…………………………..…….… 21 03.—Haleakalā; 8-13 April 1991, 29 April–9 May 1991 …………….…….… 27 04.—Oˋahu; 20–23 April, 18 May 1991 ………………………..……….…..….…..41 05.—Molokaˋi; 24-27 April 1991 …………………………………….……..….………45 06.—West Maui, 11-15 May 1992; Molokaˋi, 15-16 May 1992 ...……… 50 07.—Maui Nui, 29 April-21 May 1993 (Lānaˋi, Molokaˋi, West Maui, Haleakalā) ……………….………………………………………………………………….…….61 08.—Oˋahu, 1-15 May 1995 .………………………………….……………………..…. 89 09.—Kauaˋi, 16-22 May 1995 ………………….………………..…………..………. 104 10.—Maui + Molokaˋi 20-31 May 1997 …..……………………………………... 114 11.—Hawaiˋi Island—1–6 June 1997 …..………………………..……………….. 134 12.—Hawaiˋi Island—9–17 October 1997 …..……………………….…….….. 138 13.—Haleakalā, Maui—30 April–15 May 1998 ….…………………………... 145 14.—Haleakalā and West Maui—15–23 May 2001 …….………….………. 167 15.—Hawaiˋi Island—23–27 May 2001 …………………..…………..…………. 179 16.—Haleakalā, Maui, 14–20 May 2003 …………………………………………. 184 17.—Hawaiˋi Island, 21–25 May 2003 ………………..………………………….. 192 18.—Lānaˋi, Molokaˋi, West Maui, 10–28 May 2004 …..……..….………. -
Geologic Maps of the Eastern Alaska Range, Alaska, (44 Quadrangles, 1:63360 Scale)
Report of Investigations 2015-6 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units by Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner Southeastern Tanana Basin Southern Yukon–Tanana Upland and Terrane Delta River Granite Jarvis Mountain Aurora Peak Creek Terrane Hines Creek Fault Black Rapids Glacier Jarvis Creek Glacier Subterrane - Southern Yukon–Tanana Terrane Windy Terrane Denali Denali Fault Fault East Susitna Canwell Batholith Glacier Maclaren Glacier McCallum Creek- Metamorhic Belt Meteor Peak Slate Creek Thrust Broxson Gulch Fault Thrust Rainbow Mountain Slana River Subterrane, Wrangellia Terrane Phelan Delta Creek River Highway Slana River Subterrane, Wrangellia Terrane Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS 2015 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner COVER: View toward the north across the eastern Alaska Range and into the southern Yukon–Tanana Upland highlighting geologic, structural, and geomorphic features. View is across the central Mount Hayes Quadrangle and is centered on the Delta River, Richardson Highway, and Trans-Alaska Pipeline System (TAPS). Major geologic features, from south to north, are: (1) the Slana River Subterrane, Wrangellia Terrane; (2) the Maclaren Terrane containing the Maclaren Glacier Metamorphic Belt to the south and the East Susitna Batholith to the north; (3) the Windy Terrane; (4) the Aurora Peak Terrane; and (5) the Jarvis Creek Glacier Subterrane of the Yukon–Tanana Terrane. -
2020 January Scree
the SCREE Mountaineering Club of Alaska January 2020 Volume 63, Number 1 Contents Mount Anno Domini Peak 2330 and Far Out Peak Devils Paw North Taku Tower Randoism via Rosie’s Roost "The greatest danger for Berlin Wall most of us is not that our aim is too high and we Katmai and the Valley of Ten Thousand Smokes miss it, but that it is too Peak of the Month: Old Snowy low and we reach it." – Michelangelo JANUARY MEETING: Wednesday, January 8, at 6:30 p.m. Luc Mehl will give the presentation. The Mountaineering Club of Alaska www.mtnclubak.org "To maintain, promote, and perpetuate the association of persons who are interested in promoting, sponsoring, im- proving, stimulating, and contributing to the exercise of skill and safety in the Art and Science of Mountaineering." This issue brought to you by: Editor—Steve Gruhn assisted by Dawn Munroe Hut Needs and Notes Cover Photo If you are headed to one of the MCA huts, please consult the Hut Gabe Hayden high on Devils Paw. Inventory and Needs on the website (http://www.mtnclubak.org/ Photo by Brette Harrington index.cfm/Huts/Hut-Inventory-and-Needs) or Greg Bragiel, MCA Huts Committee Chairman, at either [email protected] or (907) 350-5146 to see what needs to be taken to the huts or repaired. All JANUARY MEETING huts have tools and materials so that anyone can make basic re- Wednesday, January 8, at 6:30 p.m. at the BP Energy Center at pairs. Hutmeisters are needed for each hut: If you have a favorite 1014 Energy Court in Anchorage. -
Melt Regimes, Stratigraphy, Flow Dynamics and Glaciochemistry of Three Glaciers in the Alaska Range
Journal of Glaciology, Vol. 58, No. 207, 2012 doi: 10.3189/2012JoG10J238 99 Melt regimes, stratigraphy, flow dynamics and glaciochemistry of three glaciers in the Alaska Range Seth CAMPBELL,1,2 Karl KREUTZ,1 Erich OSTERBERG,3 Steven ARCONE,2 Cameron WAKE,4 Douglas INTRONE,1 Kevin VOLKENING,5 Dominic WINSKI1 1Climate Change Institute and Department of Earth Sciences, University of Maine, Orono, ME, USA E-mail: [email protected] 2US Army Cold Regions Research and Engineering Laboratory, Hanover, NH, USA 3Department of Earth Sciences, Dartmouth College, Hanover, NH, USA 4Complex Systems Research Center, Institute for the Study of Earth, Oceans and Space, University of New Hampshire, Durham, NH, USA 5Department of Chemical and Biological Engineering, Montana State University, Bozeman, MT, USA ABSTRACT. We used ground-penetrating radar (GPR), GPS and glaciochemistry to evaluate melt regimes and ice depths, important variables for mass-balance and ice-volume studies, of Upper Yentna Glacier, Upper Kahiltna Glacier and the Mount Hunter ice divide, Alaska. We show the wet, percolation and dry snow zones located below 2700 m a.s.l., at 2700 to 3900 m a.s.l. and above 3900 m a.s.l., respectively. We successfully imaged glacier ice depths upwards of 480 m using 40–100 MHz GPR frequencies. This depth is nearly double previous depth measurements reached using mid-frequency GPR systems on temperate glaciers. Few Holocene-length climate records are available in Alaska, hence we also assess stratigraphy and flow dynamics at each study site as a potential ice-core location. Ice layers in shallow firn cores and attenuated glaciochemical signals or lacking strata in GPR profiles collected on Upper Yentna Glacier suggest that regions below 2800 m a.s.l. -
Post-Monsoon in the Nepal Himalaya. in the Post-Monsoon in The
Post-Monsoon in the Nepal Himalaya. In the post-monsoon in the Nepal Himalaya, the sum mer monsoon rains and snowfall continued throughout September and into early October, several weeks beyond the normal end of the rainy season, only to be followed by a few mid- October days of more heavy snowfall resulting from a cyclone nearby in India. Many teams on Cho Oyu, Ama Dablam, Baruntse and other mountains with very limited time at their dis posal had to retreat from what they considered unsafe avalanche conditions or simply from snow too deep to manage to get through. There was very little success on Nepal’s eight 8000ers. Even on Cho Oyu, where success rates are often high, 21 expeditions did some climbing but just nine of them sent anyone to the top and all followed the normal route on the northwest side. The other 12 teams—includ ing cautiously-led commercial ones—withdrew well below the summit because of dangerous snow conditions. And those who were successful were able to reach the summit only from September 26-October 1 ; before and after those dates, snow conditions were very bad. One Japanese mountaineer, Toshiyuki Kitamura, tried to solo Cho Oyu’s seldom-climbed southwest face but had to abandon his attempt at 7400 meters in soft snow under a hot sun that defeated him. He moved over to the standard route and followed teammates to the top five days after their ascent. No one even attempted Annapurna I. Only one team out of seven (a predominantly American group that included Ginette Harrison; see below) had any summiters on Dhaulagiri I. -
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. -
Scaling the World's Most Challenging Summits Is Dangerous to Some. To
SCALING THE WORLD’S MOST CHALLENGING SUMMITS IS DANGEROUS TO SOME. TO DAVE HAHN, IT’S JUST A MATTER OF WALKING UPHILL A LITTLE LONGER THAN USUAL. KING SHEER FEAR OF THE HILLBY MICHAEL HAEDERLE photo: matthew turley matthew photo: 74 discovery channel magazine.com september 2009 75 WAS A LONG, COLD NIGHT IN After this first and most harrow- ROUTE TO THE TOP MAY 1994. CROUCHED ALONE ing success, Hahn went on to climb Hahn grew up in Kingston, New York, IIN A SNOWTSTORM 8,500 Everest a further ten times, more where his father, a former climber in than any other non-Sherpa, estab- Yosemite National Park, took him METRES UP ON THE NORTHEAST lishing himself as one of the world’s camping in the nearby Catskill and RIDGE OF MOUNT EVEREST leading high-altitude climbers. The Adirondack Mountains. As a teenag- lanky 47-year-old has also conquered er he visited his mother’s hometown – without oXYgen – DAVE the 4,897-metre Vinson Massif, the of Albuquerque, New Mexico, and HAHN HUNG ON FOR FIRST highest peak in Antarctica, a record scaled the craggy 3,255-metre Sandia LIGHT, DESPERATELY WILLING 26 times. Add to that 18 ascents of Crest. He returned to New Mexico af- Mount McKinley (also known as De- ter college to work as a ski instructor, HIMSELF TO STAY AWAKE AFTER nali) in Alaska and more than 250 but had an epiphany in 1985 when he 48 HOURS OF CONTINUOUS scalings of Mount Rainier in the US enrolled in a mountaineering course state of Washington and you have run by the Mount Rainier guide ser- CLIMBING. -
Yukon River Nulato Hills Lime Hills Alaska Range Yukon River Lowlands Seward Peninsula Yukon-Kuskokwim Delta Ray Mountains Ahklu
New Allakaket !! er !! iv !! H R k a e Alatna o z e l t r l a y g C k I o y n C e H r r e g k n e r Allakaket e k t Cre r e v r e Asiksa e i u e e C H K R k r P k a a a s C h h R n n s u i K v Kotzebue Sound Lowlands z i k e u k o r P e h r r t r k i r k k Selawik National u e k e i e e R ek u v u e H k il r i re Cr l C i C a u G v n u C n k R t i o s e la n k h a e ha r i k h r t il i i C e S g t C in u nu C Wildlife Refuge e h w H a r K r k S a e e l reek k e e o C e e ltlinkh h k Ta k r e S g r k W e k u e C h e e v o i n e r r e l e e e r C S R m l e k v o i C Deering k k r e L C e d x ! c u C r R r ! i o e C o D a r m Kada e k f R e ina C l f s re K Kobuk Ridges and Valleys e e K ek k i t o l p k s l o k S g e a lat p c ta ht a e n o i C u D k t k E r oha Creek na a r Al C C Cre a r e C e k C k e r r k k t e r e e ek e e l ek e o e i e r r v r k v C k k i C W ugh P ry i e R ar all g Slo C te e e le ic Lon s R r R k y i C C r k e C re M v e k e k r k k e a k e Map Area Extenitr B e e e r u r r D C K a i r B C h l e C o l v u k k c o y k i o H r m k g e A n e e a c e a u g H r R tla o e e e n C i o r k l n r a k a u R C n m e re n e a o k e y C o C c w b k o e r i a t a n C r k i r u a P e s I k Ca v o a H K M n h C C k e N d n i r oo e l Bb uckland C k u n ek it r l a e uk a re l o C h k ! C r e y C C e ! e L C ek a ree e r z na o E C u k e o r it a re h k C e z ol N s C y k N n s y e h K e i n e p e r n e ig k t i e y lo n k h s C G i ree e H ra o d M C k e o r l p K t d e n N O um e h k k o e z k J e ee k a ee e r Cr n K C B r e -
Glenn Highway Tok Cutoff (GJ-125 to GJ-0) to Milepost a 160
Map GLENN HIGHWAY • TOK CUTOFF Glenn Highway To Chicken and Eagle © The MILEPOST To Delta Junction (see TAYLOR HIGHWAY section) Key to mileage boxes ver (see ALASKA HIGHWAY section) Tanana Ri miles/kilometres G miles/kilometres Tanacross 5 from: la A L c A Swb T-Tok V-Valdez ia S K 2 Tok Map Location G-Glennallen ted A ® GJ-Gakona Junction A re A-Anchorage a R 2 A 1 Tetlin Junction J-Junction N HJ-Haines Junction Mount Kimball G T-0 a To Haines DJ-Delta Junction in 10,300 ft./3,139m E ch r w GJ-125/201km Junction Chisto cie G la A-328/528km (see ALASKA Principal Route Logged Key to Advertiser er HIGHWAY Services T iv DJ-108/174km C -Camping ok R section) Paved Unpaved R HJ-296/476km D -Dump Station iv ok Other Roads Logged d -Diesel er T G -Gas (reg., unld.) Tetlin I -Ice Lake Other Roads Scenic Byway L -Lodging M -Meals T Refer to Log for Visitor Facilities P -Propane Tok Cutoff ok Cu L R -Car Repair (major) na i Scale Sla R Mineral Lakes t iv t r -Car Repair (minor) e l 0 10 Miles r e S -Store (grocery) 0 10 Kilometres T -Telephone (pay) . t Cr t Bartell off (GJ-125 r Mentasta Lake e r e t T r. o v iv C i R Mentasta Lake S t ation k R Mentasta Summit n T-65/105km 2,434 ft./742m M a . i r E N d J-0 t C T A n e S I . -
Summary of Public Comment, Appendix B
Summary of Public Comment on Roadless Area Conservation Appendix B Requests for Inclusion or Exemption of Specific Areas Table B-1. Requested Inclusions Under the Proposed Rulemaking. Region 1 Northern NATIONAL FOREST OR AREA STATE GRASSLAND The state of Idaho Multiple ID (Individual, Boise, ID - #6033.10200) Roadless areas in Idaho Multiple ID (Individual, Olga, WA - #16638.10110) Inventoried and uninventoried roadless areas (including those Multiple ID, MT encompassed in the Northern Rockies Ecosystem Protection Act) (Individual, Bemidji, MN - #7964.64351) Roadless areas in Montana Multiple MT (Individual, Olga, WA - #16638.10110) Pioneer Scenic Byway in southwest Montana Beaverhead MT (Individual, Butte, MT - #50515.64351) West Big Hole area Beaverhead MT (Individual, Minneapolis, MN - #2892.83000) Selway-Bitterroot Wilderness, along the Selway River, and the Beaverhead-Deerlodge, MT Anaconda-Pintler Wilderness, at Johnson lake, the Pioneer Bitterroot Mountains in the Beaverhead-Deerlodge National Forest and the Great Bear Wilderness (Individual, Missoula, MT - #16940.90200) CLEARWATER NATIONAL FOREST: NORTH FORK Bighorn, Clearwater, Idaho ID, MT, COUNTRY- Panhandle, Lolo WY MALLARD-LARKINS--1300 (also on the Idaho Panhandle National Forest)….encompasses most of the high country between the St. Joe and North Fork Clearwater Rivers….a low elevation section of the North Fork Clearwater….Logging sales (Lower Salmon and Dworshak Blowdown) …a potential wild and scenic river section of the North Fork... THE GREAT BURN--1301 (or Hoodoo also on the Lolo National Forest) … harbors the incomparable Kelly Creek and includes its confluence with Cayuse Creek. This area forms a major headwaters for the North Fork of the Clearwater. …Fish Lake… the Jap, Siam, Goose and Shell Creek drainages WEITAS CREEK--1306 (Bighorn-Weitas)…Weitas Creek…North Fork Clearwater. -
Climbs and Expeditions, 1988
Climbs and Expeditions, 1988 The Editorial Board expresses its deep gratitude to the many people who have done so much to make this section possible. We cannot list them all here, but we should like to give particular thanks to the following: Kamal K. Guha, Harish Kapadia, Soli S. Mehta, H.C. Sarin, P.C. Katoch, Zafarullah Siddiqui, Josef Nyka, Tsunemichi Ikeda, Trevor Braham, Renato More, Mirella Tenderini. Cesar Morales Arnao, Vojslav Arko, Franci Savenc, Paul Nunn, Do@ Rotovnik, Jose Manuel Anglada, Jordi Pons, Josep Paytubi, Elmar Landes, Robert Renzler, Sadao Tambe, Annie Bertholet, Fridebert Widder, Silvia Metzeltin Buscaini. Luciano Ghigo, Zhou Zheng. Ying Dao Shui, Karchung Wangchuk, Lloyd Freese, Tom Elliot, Robert Seibert, and Colin Monteath. METERS TO FEET Unfortunately the American public seems still to be resisting the change from feet to meters. To assist readers from the more enlightened countries, where meters are universally used, we give the following conversion chart: meters feet meters feet meters feet meters feet 3300 10,827 4700 15,420 6100 20,013 7500 24,607 3400 11,155 4800 15,748 6200 20,342 7600 24,935 3500 11,483 4900 16,076 6300 20,670 7700 25,263 3600 11,811 5000 16,404 6400 20,998 7800 25,591 3700 12,139 5100 16,733 6500 21,326 7900 25,919 3800 12,467 5200 17.061 6600 21,654 8000 26,247 3900 12,795 5300 7,389 6700 21,982 8100 26,575 4000 13,124 5400 17,717 6800 22,3 10 8200 26,903 4100 13,452 5500 8,045 6900 22,638 8300 27,231 4200 13,780 5600 8,373 7000 22,966 8400 27,560 4300 14,108 5700 8,701 7100 23,294 8500 27,888 4400 14,436 5800 19,029 7200 23,622 8600 28,216 4500 14,764 5900 9,357 7300 23,951 8700 28,544 4600 15,092 6000 19,685 7400 24,279 8800 28,872 NOTE: All dates in this section refer to 1988 unless otherwise stated. -
Region Forest Roadless Name GIS Acres 1 Beaverhead-Deerlodge
These acres were calculated from GIS data Available on the Forest Service Roadless website for the 2001 Roadless EIS. The data was downloaded on 8/24/2011 by Suzanne Johnson WO Minerals & Geology‐ GIS/Database Specialist. It was discovered that the Santa Fe NF in NM has errors. This spreadsheet holds the corrected data from the Santa Fe NF. The GIS data was downloaded from the eGIS data center SDE instance on 8/25/2011 Region Forest Roadless Name GIS Acres 1 Beaverhead‐Deerlodge Anderson Mountain 31,500.98 1 Beaverhead‐Deerlodge Basin Creek 9,499.51 1 Beaverhead‐Deerlodge Bear Creek 8,122.88 1 Beaverhead‐Deerlodge Beaver Lake 11,862.81 1 Beaverhead‐Deerlodge Big Horn Mountain 50,845.85 1 Beaverhead‐Deerlodge Black Butte 39,160.06 1 Beaverhead‐Deerlodge Call Mountain 8,795.54 1 Beaverhead‐Deerlodge Cattle Gulch 19,390.45 1 Beaverhead‐Deerlodge Cherry Lakes 19,945.49 1 Beaverhead‐Deerlodge Dixon Mountain 3,674.46 1 Beaverhead‐Deerlodge East Pioneer 145,082.05 1 Beaverhead‐Deerlodge Electric Peak 17,997.26 1 Beaverhead‐Deerlodge Emerine 14,282.26 1 Beaverhead‐Deerlodge Fleecer 31,585.50 1 Beaverhead‐Deerlodge Flint Range / Dolus Lakes 59,213.30 1 Beaverhead‐Deerlodge Four Eyes Canyon 7,029.38 1 Beaverhead‐Deerlodge Fred Burr 5,814.01 1 Beaverhead‐Deerlodge Freezeout Mountain 97,304.68 1 Beaverhead‐Deerlodge Garfield Mountain 41,891.22 1 Beaverhead‐Deerlodge Goat Mountain 9,347.87 1 Beaverhead‐Deerlodge Granulated Mountain 14,950.11 1 Beaverhead‐Deerlodge Highlands 20,043.87 1 Beaverhead‐Deerlodge Italian Peak 90,401.31 1 Beaverhead‐Deerlodge Lone Butte 13,725.16 1 Beaverhead‐Deerlodge Mckenzie Canyon 33,350.48 1 Beaverhead‐Deerlodge Middle Mtn.