Denali Wilderness Character Narrative NPS PHOTO/ KENT MILLER
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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. -
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. -
Yukon River Nulato Hills Lime Hills Alaska Range Yukon River Lowlands Seward Peninsula Yukon-Kuskokwim Delta Ray Mountains Ahklu
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Chapter Four
Chapter Four South Denali Visitor Center Complex: Interpretive Master Plan Site Resources Tangible Natural Site Features 1. Granite outcroppings and erratic Resources are at the core of an boulders (glacial striations) interpretive experience. Tangible resources, those things that can be seen 2. Panoramic views of surrounding or touched, are important for connecting landscape visitors physically to a unique site. • Peaks of the Alaska Range Intangible resources, such as concepts, (include Denali/Mt. McKinley, values, and events, facilitate emotional Mt. Foraker, Mt. Hunter, Mt. and meaningful experiences for visitors. Huntington, Mt. Dickey, Moose’s Effective interpretation occurs when Erratic boulders on Curry Ridge. September, 2007 Tooth, Broken Tooth, Tokosha tangible resources are connected with Mountains) intangible meanings. • Peters Hills • Talkeetna Mountains The visitor center site on Curry Ridge maximizes access to resources that serve • Braided Chulitna River and valley as tangible connections to the natural and • Ruth Glacier cultural history of the region. • Curry Ridge The stunning views from the visitor center site reveal a plethora of tangible Mt. McKinley/Denali features that can be interpreted. This Mt. Foraker Mt. Hunter Moose’s Tooth shot from Google Earth shows some of the major ones. Tokosha Ruth Glacier Mountains Chulitna River Parks Highway Page 22 3. Diversity of habitats and uniquely 5. Unfettered views of the open sky adapted vegetation • Aurora Borealis/Northern Lights • Lake 1787 (alpine lake) • Storms, clouds, and other weather • Alpine Tundra (specially adapted patterns plants, stunted trees) • Sun halos and sun dogs • High Brush (scrub/shrub) • Spruce Forests • Numerous beaver ponds and streams Tangible Cultural Site Features • Sedge meadows and muskegs 1. -
Nos Cook Inlet Operational Forecast System: Model Development and Hindcast Skill Assessment
NOAA Technical Report NOS CS 40 NOS COOK INLET OPERATIONAL FORECAST SYSTEM: MODEL DEVELOPMENT AND HINDCAST SKILL ASSESSMENT Silver Spring, Maryland September 2020 noaa National Oceanic and Atmospheric Administration U.S. DEPARTMENT OF COMMERCE National Ocean Service Coast Survey Development Laboratory Office of Coast Survey National Ocean Service National Oceanic and Atmospheric Administration U.S. Department of Commerce The Office of Coast Survey (OCS) is the Nation’s only official chartmaker. As the oldest United States scientific organization, dating from 1807, this office has a long history. Today it promotes safe navigation by managing the National Oceanic and Atmospheric Administration’s (NOAA) nautical chart and oceanographic data collection and information programs. There are four components of OCS: The Coast Survey Development Laboratory develops new and efficient techniques to accomplish Coast Survey missions and to produce new and improved products and services for the maritime community and other coastal users. The Marine Chart Division acquires marine navigational data to construct and maintain nautical charts, Coast Pilots, and related marine products for the United States. The Hydrographic Surveys Division directs programs for ship and shore-based hydrographic survey units and conducts general hydrographic survey operations. The Navigational Services Division is the focal point for Coast Survey customer service activities, concentrating predominately on charting issues, fast-response hydrographic surveys, and Coast Pilot -
Little Susitna River FY 2014 Final Report
Clean Boating on the Little Susitna River FY 2014 Final Report Prepared for: Alaska Department of Environmental Conservation Alaska Clean Water Action Grant #14-03 July 1, 2013—June 30, 2014 Cook Inletkeeper is a community-based nonprofit organization that combines advocacy, outreach, and science toward its mission to protect Alaska’s Cook Inlet watershed and the life it sustains. Report prepared by: Rachel Lord Outreach & Monitoring Coordinator Cook Inletkeeper 3734 Ben Walters Ln. Suite 201 Clean Boating on Big Lake Homer, AK 99603 (907) 235-4068 FY14 Final Report www. inletkeeper.org 2 Cook Inletkeeper ● www.inletkeeper.org TABLE OF CONTENTS Introduction 4 Launch Host Program 7 Boater Survey Results 9 Community Outreach 12 Future Work 15 Acknowledgements 16 Appendix A. FY14 Little Su Clean Boater Surveys Appendix B. Media Excerpts Appendix C. Clean boating resources Protecting Alaska’s Cook Inlet watershed and the life it sustains since 1995. 3 INTRODUCTION The Little Susitna River is located in the densely as impacts from high turbidity levels around the populated Southcentral region of Alaska. It sup- Public Use Facility (PUF, river mile 25). This pol- ports salmon and trout populations, making it a lutant loading is associated with busy, high use popular fishing destination for many in the An- times of the summer when Chinook salmon (May chorage and Mat-Su Borough area. In addition to -June) and Coho salmon (July –September) are fishing, people come to the ‘Little Su’ during running in the river. More information on the summer months for recreational boating, hunt- ADEC efforts at the Little Su can be found ing, picnics and camping. -
The Little Susitna River— an Ecological Assessment
The Little Susitna River— An Ecological Assessment Jeffrey C. Davis and Gay A. Davis P.O. Box 923 Talkeetna, Alaska (907) 733.5432. www.arrialaska.org July 2007 Acknowledgements This project was completed with support from the State of Alaska, Alaska Clean Water Action Plan program, ACWA 07-11. Laura Eldred, the DEC Project Manger provided support through comments and suggestion on the project sampling plan, QAPP and final report. Nick Ettema from Grand Valley State University assisted in data collection. ARRI—Little Susitna River July 2007 Table of Contents Summary............................................................................................................................. 2 Introduction......................................................................................................................... 3 Methods............................................................................................................................... 4 Sampling Locations ........................................................................................................ 4 Results................................................................................................................................. 6 Riparian Development .................................................................................................... 6 Index of Bank Stability ................................................................................................... 7 Chemical Characteristics and Turbidity......................................................................... -
Floods of October 1986 in Southcentral Alaska
FLOODS OF OCTOBER 1986 IN SOUTHCENTRAL ALASKA " » U.S. GEOLOGICAL SURVEY OPEN- FILE REPORT 87-391 REVISED 1988 Prepared in cooperation with the: ALASKA DEPARTMENT OF TRANSPORTATION AND PUBLIC FACILITIES ALASKA DIVISION OF EMERGENCY SERVICES FEDERAL HIGHWAY ADMINISTRATION FLOODS OF OCTOBER 1986 IN SOUTHCENTRAL ALASKA by Robert D. Lamke and Bruce P. Bigelow U.S. GEOLOGICAL SURVEY Open-File Report 87-391 REVISED 1988 Prepared in cooperation with the: ALASKA DEPARTMENT OF TRANSPORTATION AND PUBLIC FACILITIES ALASKA DIVISION OF EMERGENCY SERVICES FEDERAL HIGHWAY ADMINISTRATION Anchorage, Alaska 1988 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Books and Open-File Reports Section Water Resources Division Federal Center 4230 University Drive, Suite 201 Box 25425 Anchorage, Alaska 99508-4664 Denver, Colorado 80225 11 CONTENTS Page Abstract .............................................................. 1 Introduction .......................................................... 1 Purpose and scope ................................................ 1 Acknowledgements ................................................. 3 Precipitation ......................................................... 3 Discharge data ........................................................ 7 Peak stage and discharge table ................................... 7 Discharge data for October -
Talkeetna Airport, Phase II
Talkeetna Airport, Phase II Hydrologic/ Hydraulic Assessment Incomplete Draft January 2003 Prepared For: Prepared By: URS Corporation 301 W. Northern Lights 3504 Industrial Ave., Suite 125 Blvd., Suite 601 Fairbanks, AK 99701 CH2M Hill Anchorage, AK 99503 (907) 374-0303 TABLE OF CONTENTS Section Title Page 1.0 Introduction..........................................................................................................................1 2.0 Background Data .................................................................................................................4 2.1 Airport Construction ................................................................................................4 2.2 Past Floodplain Delineations ...................................................................................6 2.3 Past Suggestions for Floodplain Mitigation.............................................................7 2.4 Historical Floods......................................................................................................8 3.0 Flood-Peak Frequency .......................................................................................................12 3.1 Talkeetna River at its Mouth..................................................................................12 3.2 Susitna River Above and Below the Talkeetna River ...........................................13 3.3 Summary................................................................................................................15 4.0 Flood Timing ....................................................................................................................16 -
MOUNT Mckinley I Adolph Murie
I (Ie De/;,;;I; D·· 3g>' I \N ITHE :.Tnf,';AGt:: I GRIZZLIES OF !MOUNT McKINLEY I Adolph Murie I I I I I •I I I II I ,I I' I' Ii I I I •I I I Ii I I I I r THE GRIZZLIES OF I MOUNT McKINLEY I I I I I •I I PlEASE RETURN TO: TECHNICAL INfORMATION CENTER I f1r,}lVER SiRV~r.r Gs:t.!TER ON ;j1,l1uNAl PM~ :../,,;ICE I -------- --- For sale h~' the Super!u!p!u]eut of Documents, U.S. Goyernment Printing Office I Washing-ton. D.C. 20402 I I '1I I I I I I I I .1I Adolph Murie on Muldrow Glacier, 1939. I I I I , II I I' I I I THE GRIZZLIES I OF r MOUNT McKINLEY I ,I Adolph Murie I ,I I. I Scientific Monograph Series No. 14 'It I I I U.S. Department of the Interior National Park Service Washington, D.C. I 1981 I I I As the Nation's principal conservation agency, the Department of the,I Interior has responsibility for most ofour nationally owned public lands and natural resources. This includes fostering the wisest use ofour land and water resources, protecting our fish and wildlife, preserving the environmental and cultural values of our national parks and historical places, and providing for the enjoyment of life through outdoor recre- I ation. The Department assesses our energy and mineral resources and works to assure that their development is in the best interests of all our people. The Department also has a major responsibility for American Indian reservation communities and for people who live in Island Ter- I ritories under U.S.