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Field-Trip Guide to Volcanic and Volcaniclastic Deposits of the Lower Jurassic Talkeetna Formation, Sheep Mountain, South-Central Alaska
Field-Trip Guide to Volcanic and Volcaniclastic Deposits of the Lower Jurassic Talkeetna Formation, Sheep Mountain, South-Central Alaska U.S. Department of the Interior U.S. Geological Survey Open-File Report 2006-1124 Field-Trip Guide to Volcanic and Volcaniclastic Deposits of the Lower Jurassic Talkeetna Formation, Sheep Mountain, South-Central Alaska Amy E. Draut U.S. Geological Survey, Pacific Science Center, Santa Cruz, CA 95060 Peter D. Clift School of Geosciences, University of Aberdeen, AB24 3UE, U.K. Robert B. Blodgett U.S. Geological Survey–Contractor, Anchorage, AK 99508 U.S. GEOLOGICAL SURVEY Open-File Report 2006-1124 2006 U.S. Department of the Interior P. Lynn Scarlett, Acting Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 Revised and reprinted: 2006 Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government To download a copy of this report from the World Wide Web: http://pubs.usgs.gov/of/2006/1124/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. LIST OF FIGURES FIGURE 1. Regional map of the field-trip area. FIGURE 2. Geologic cross section through Sheep Mountain. FIGURE 3. Stratigraphic sections on the south side of Sheep Mountain. -
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. -
Lower Matanuska Valley Alaska
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOK BTTLI/ETIN 500 *- J 0 GEOLOGY AND COAL FIELDS OF THE LOWER MATANUSKA VALLEY ALASKA BY G. C. MARTIN AND F. J. KATZ WASHINGTON GOVERNMENT PRINTING OFFICE 1912 CONTENTS. Page. Preface, by Alfred H. Brooks.............................................. 7 Introduction....................;......................................... 9 Location.............................................................. 9 Account of investigations............................................... 9 Exploratory and reconnaissance surveys............................. 9 Detailed surveys.................................................. 10 General description of the district....................................... 10 Geography............................... .*. ........................ 10 Climate............................................................ 11 Vegetation......................................................... 13 Accessibility....................................................... 13 Commercial development........................................... 14 Outline of the geology of the Matanuska Valley.......................... 14 General features................................................... 14 Mica schists....................................................... 15 Gray wackes and slates of the Knik Eiver region..................... 16 Lower Jurassic rocks................................................ 17 Granitic rocks................................................... -
WINTEK VIEW of MOUNT Mckinley from the NORTHWEST. UNITED STATES DEPARTMENT of the INTERIOR Harold L
GEOLOGICAL SURVEY BULLETIN 907 FRONTISPIECE WINTEK VIEW OF MOUNT McKINLEY FROM THE NORTHWEST. UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 907 GEOLOGY OF THE ALASKA RAILROAD REGION BY STEPHEN R. CAPPS UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1940 For sale by the Superintendent of Documents. Washington, D. C. ..... Price $1.25 (paper) ft 3 -vu> CONTENTS Page Abstract. _._._.-._.._.___._______-_---.--_--__------_--..-.-.-__._ 1 Introduction.._.._..._..__-__-__-------l---_._-...--.-.---_-__.-_. 1 History., of, exploration. _..__._.._._-----..--_.___-____.-_-____.-__.. 4 Present report__....--..-__._-.--------.----...----_----_----.-._ 21 Geography.. .-...._-.___-_--.-------_------_-__--.-_-----___.._ 23- Geographic provinces._______----_--_----_-_._---.---_.--...._. 23' Chugach-Kenai Mountains._----_---_.__--_--_---.---...-.. 24 Talkeetna Mountains._-_-------_---__--._.____._-..._-._.. 25 Cook Inlet-Susitna lowland.-----_----__--_---.-_---_-,-_-__ 26 Copper-Susitna lowland._------------..___-..._.--_.-.-.-._ 27 Alaska Range.______.___------__----_-_-__--_-_-__________ 27 Tanana-Kuskokwim lowland.._-..__.__._.__._._____.__.____ 29 Yukon-Tanana'upland. __--_------------__--------------.-- 30 Climate. _-_-__-------_---_-_-----------_-----------._-_-_-_--_ 31 Vegetation... _._._.__._-:___-.._.---.___.--._----__-_-__--._-__ 33 Animal life.___-_---_-_--_----_-----------_-------__.-__.---._ 35 Population..................----.-.----I.-.-..--.-.-......... -
Matanuska River Watershed Plan
1 Matanuska River Watershed Plan Prepared by: U.S. Department of Agriculture Natural Resources Conservation Service Palmer Field Office 1700 E. Bogard, Suite 203 Wasilla, AK 99654 JUNE 2006 2 TABLE OF CONTENTS Approval of the Plan Acknowledgements Planning Signatures and Initiating Government Letters of Approval TABLE OF CONTENTS EXECUTIVE SUMMARY 1.0 INTRODUCTION AND PLANNING FRAMEWORK 1.1 Background and historical information 1.2 Studies and Reports: past and present 1.3 Purpose of the Plan 1.4 Limitations 2.0 WATERSHED CHARACTERIZATION 2.1 Natural Environment 2.1.1 Geography & Climate 2.1.2 Soils 2.1.3 Hydrology and Geohydrology 2.1.4 Biology 2.2 Human Environment 2.2.1 Land Use and Demographics 2.3 Tributaries 2.3.1 Overview 2.4 Water Resources 2.4.1 Water Quality 2.4.2 Water Quantity 3.0 RESOURCE CONCERNS 3.1 Critical Residential Area of concern 3.2 Habitat Conditions 4.0 IMPLEMENTATION AND RECOMMENDATIONS 4.1 Structural 4.2 Non-structural 5.0 COST BENEFIT COMPARISON 6.0 APPENDICES (Figures & Tables) 3 ACKNOWLEDGEMENTS The planning team consisted of NRCS staff with input from the Matanuska River Watershed Coalition group. The planning effort is the result of over ten years of ongoing erosion impacted-structures and public pressure to address the loss property. The following people participated in the Watershed Planning process. Initiating Governments Matanuska Susitna Borough (MSB) NRCS Watershed Coalition Team Author: Michelle Schuman, USDA, Natural Resources Conservation Service, District Conservationist, Palmer Field Office Review: -
Hawkwatch Is in South-Central One Would Expect Spring Migrants in North Amer - Alaska (See Map, P
Paul Fritz Cecily Fritz Palmer, Alaska Urbana, Maryland [email protected] [email protected] 30 BIRDING • JANUARY 2011 nless you are an avid hawk watcher or you follow Alaska birding, you prob - ably have never heard of the Gunsight Mountain Hawk Watch. Although relatively unknown, Gunsight’s spring hawk migration has grabbed the at - tention of an increasing number of raptor enthusiasts because of the rich array of Red-tailed and Rough-legged hawk plumages it offers. And from an Alaskan per - spective, Gunsight is likely the most reliable spot in the state to see Swainson’s Hawks, rare in Alaska. Gunsight is the only known site in the state where Swain - son’s is seen often enough to garner a “rare” status as opposed to “casual” or “accidental.” What makes the area even more enticing is the percentage of reflected light (albedo) from the consistent snow cover. With new snowfall, albedo can exceed 90%, although it’s more generally in the 40–50% range—still wonderful lighting conditions, considering that other surfaces reflect 10% or less of the sunlight. Even on a cloudy day, watchers and photographers enjoy excel - lent conditions for observation of fine details and for raptor-in-flight pho - tography. WWW.ABA.ORG 31 GUNSIGHT MOUNTAIN whereas, for instance, in the Himalayas and other mountainous areas, the plateau is relatively high. In 1995, the well-known mountain climber Gerry Roach reported seeing Denali from the summit of Mt. Sanford, an astounding distance of more than 225 miles. Gunsight nfrequent Alaskan hawk counts have Mountain is the been conducted north of Gunsight, place to see a Harlan’s but only two regularly staffed hawk Hawk . -
Geology of the Northern Chugach Mountains, Southcentral Alaska
GEOLOGY OF THE NORTHERN CHUGACH MOUNTAINS, SOUTHCENTRAL ALASKA BY L.E.Burns, G.H.Pessel, T.A. Little, T.L. Pavlis, R.J. Newberry, G.R. Winkler, and John Decker Professional Report 94 Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DMSION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Alaska Department of NATURAL RESOURCES GEOLOGY OF THE NORTHERN CHUGACH MOUNTAINS, SOUTHCENTRAL ALASKA BY L.E. Burns, G.H. Pessel, TA. Little, T.L. Pavlis, R.J. Newberry, G.R. Winkler, and John Decker Cover: View looking east into valley of a tributary of Coal Creek in the Anchorage C-4 Quadrangle. Photo shows Mesozoic schist (Mzsh) and a very mixed unit of Jurassic diorite-quam diorite (Jdqd) inmdcd by Creraceow rrondhjemite (Kt). A smaU fault-bounded sliver of Jurassic gabbroic rocks (Jgu) is imbedded in the rrondhjemite. A mkture of Jurassic plutonic rocks, including compositionsfrom gabbroic to quom diontic, crops our in the background. Foreground is composed of a rock glacier (Qrg) and glacier (Qg). Photo by G.H. Pessel, 1983. Professional Report 94 Division of Geological & Geophysical Surveys Fairbanks, Alaska 1991 STATE OF ALASKA Walter J. Hickel, Governor DEPARTMENT OF NATURAL RESOURCES Harold C. Heinze, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Thomas E. Smith, Acting Director and State Geologist DGGS publications may be inspected at the following locations. Address mail orders to the Fairbanks office. Alaska Division of Geological & Geophysical Surveys 794 University Avenue, Suite 200 400 Willoughby Avenue, 3rd floor Fairbanks, Alaska -
Gypsiferous Deposits on Sheep Mountain Alaska
Gypsiferous Deposits on Sheep Mountain Alaska GEOLOGICAL SURVEY BULLETIN 989-C GYPSIFEROUS DEPOSITS ON SHEEP MOUNTAIN, ALASKA By RICHARD A. ECKHART ABSTRACT Gypsum-bearing rocks crop out in Gypsum and Yellow Jacket Gulches, on Sheep Mountain, which is about 90 miles northeast of Anchorage, Alaska. The gypsiferous rock occurs in deposits of irregular shape in the greenstone. Both the gypsiferous rock and the greenstone are hydrothermal alteration products of the volcanic rocks of Jurassic age which comprise the bulk of the mountain. Near-surface samples of the gypsiferous rock contained an average of 25 to 30 percent gypsum; some contained as much as 50 percent. Quartz, alunite, clay, sericite, and pyrite are contaminating constituents of the ore. Six of the largest and most accessible of the gypsum deposits were mapped and calculations show that three of the deposits contain an aggregate of approximately 311,000 short tons of indicated gypsiferous rock and four of the deposits contain 348,000 short tons of inferred gypsiferous rock. INTRODUCTION Gypsiferous deposits occur on the south side of Sheep Mountain (see fig. 12), 112 miles northeast of Anchorage via the Glenn Highway. Sheep Mountain is a high east-trending ridge, approximately 10 miles long and 3 miles wide. It is bordered on the west by Caribou Creek and on the east by Tahneta Pass. To the north it is separated from the Talkeetna Mountains by the valley of Caribou and Squaw Creeks and from the Chugach Mountains, to the south, by the valley of the Matanuska River. Two creeks, Gypsum and Yellow Jacket, have incised V-shaped gulches 1,500 to 2,000 feet deep in the area of the gypsiferous deposits. -
Birding in Mat-Su
!"#$"%&'"%'()*+,-' ' PALMER HAY FLATS STATE GAME REFUGE Where: Primary access is from Hayfield Road via Knik-Goose Bay Rd. From Wasilla take Knik -Goose Bay Rd 4.1 mile. Turn left on Fairview Loop Rd. Go 1.9 miles. Go straight ahead onto Hayfield Rd From the Parks Hwy: Take the Hyer Rd exit to Fairview Loop Road. (From the west - Wasilla area turn right onto E. Fireweed Lane, then take first left onto Fairview Loop Rd. Coming from Anchorage/Palmer area turn left onto Hyer Rd, go under the Parks Highway, turn right onto E. Fireweed Rd, then take the first left onto Fairview Loop Rd). Continue 9 miles. Turn left onto Hayfield Rd. Follow Hayfield Road about 1.3 miles. You will see Lucy Lake Road ion the right, the Hay Flats access road on the left, and a Palmer Hay Flats Refuge sign on the right. Drive 0.4 miles down the access road to the parking lot. What: This estuary is one of the most productive waterfowl stopover and nesting areas accessible in south central Alaska. It is an important migratory stopover for large numbers of ducks, geese, swans and Sandhill Cranes, as well as shorebirds. A variety of raptors such as Northern Harrier, Rough- legged Hawk and Short-eared Owl can be seen regularly during migration with some nesting as well. Warblers, sparrows, longspurs, thrushes and other songbirds also frequent the area. Some species that occur in the Hay Flats have special conservation status including Trumpeter Swan and Rusty Blackbird. International BirdLife and National Audubon Society nominated the Refuge as an Important Bird Area (IBA). -
Paul Fritz Cecily Fritz Palmer, Alaska Urbana, Maryland [email protected] [email protected]
Paul Fritz Cecily Fritz Palmer, Alaska Urbana, Maryland [email protected] [email protected] 30 BIRDING • JANUARY 2011 nless you are an avid hawk watcher or you follow Alaska birding, you prob - ably have never heard of the Gunsight Mountain Hawk Watch. Although relatively unknown, Gunsight’s spring hawk migration has grabbed the at - tention of an increasing number of raptor enthusiasts because of the rich array of Red-tailed and Rough-legged hawk plumages it offers. And from an Alaskan per - spective, Gunsight is likely the most reliable spot in the state to see Swainson’s Hawks, rare in Alaska. Gunsight is the only known site in the state where Swain - son’s is seen often enough to garner a “rare” status as opposed to “casual” or “accidental.” What makes the area even more enticing is the percentage of reflected light (albedo) from the consistent snow cover. With new snowfall, albedo can exceed 90%, although it’s more generally in the 40–50% range—still wonderful lighting conditions, considering that other surfaces reflect 10% or less of the sunlight. Even on a cloudy day, watchers and photographers enjoy excel - lent conditions for observation of fine details and for raptor-in-flight pho - tography. WWW.ABA.ORG 31 GUNSIGHT MOUNTAIN whereas, for instance, in the Himalayas and other mountainous areas, the plateau is relatively high. In 1995, the well-known mountain climber Gerry Roach reported seeing Denali from the summit of Mt. Sanford, an astounding distance of more than 225 miles. Gunsight nfrequent Alaskan hawk counts have Mountain is the been conducted north of Gunsight, place to see a Harlan’s but only two regularly staffed hawk Hawk . -
Mountaineering Club of Alaska August 2013
the SCREE Mountaineering Club of Alaska August 2013 Volume 56 Number 8 Monthly meeting: 6:30 p.m., Wednesday, August 21 Program: "Tibet, Bhutan, and Yunnan: In search of the Himalayan Iceworm" presented by Roman Dial Contents Peakbagging in the Saint Elias Mountains Mount Laurens “Somewhere between the bottom of Bold Peak the climb and the summit is the an- Peak 4738 Raven Peak swer to the mystery why we climb.” Kings Mountain -Greg Child Peak of the Month: Peak 1950 Scree – August 2013 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." Join us for our club meeting at 6:30 p.m. on August 21 at the BP Energy Center, 1014 Energy Court, Anchorage, Alaska. http://www.alaskageology.org/graphics/meetingmap.gif Contents Cover Photo Peakbagging in the Saint Elias Mountains Joe Chmielowski working his way up to the north ridge of Mount Laurens Kings Mountain. Photo by Todd Kelsey. Bold Peak Peak 4738 Raven Peak Kings Mountain Peak of the Month: Peak 1950 Article Submission Text and photography submissions for the Scree can be sent as attachments to [email protected]. Articles should be submitted by the 25th of each month to appear in the next issue of the Scree. Do not submit material in the body of the email. Do not submit photos embedded in the text file. Send the photo files separately. -
Selected Quotes from Shem Pete's Alaska 2016 Proto-Dene Lex Loci P
selected quotes from Shem Pete's Alaska 2016 Proto-Dene Lex Loci p. 14 xii p. 14 MAP 9 Hydronymic districts in Northern Athabascan languages. River is at Delta River and Goodpaster River. Kari 1996a:463: ‡The hydronymic district was the first key concept for Kari’s “the na’/ niq’ innovation is only one piece of evidence of the theory of Dene prehistory “The Proto-Dene Lex Loci” (‘word/ gradual westward/ downstream expansion of the Athabaskans law of location’, or PDLL) that is introduced on pp. 144–147. into western and Southcentral Alaska. The Tanana River, with Some concepts presented in Kari 1996a, 1996c, and 2010b that four [to five] smallish language areas gives every indication of are central to the PDLL theory are hydronymic districts (seven having been the ancient center of Northern Athabaskan culture.” regional terms for ‘stream’ in Northern Dene languages), reverse Also introduced on p. 144 is the PDLL term watershed tenure hydronymns (use of a minor hydronymn to highlight streams such that includes hydronymic districts and several other pragmatic/ as -niq’ instead of -na’ in Western Alaska), and oronymic districts intentional place naming devices that are detectable in Alaska (where PA *dz ł ‘mountain’ shifts to *d ghilayi south and west of Dene place names. the Alaska Range, see. 7.61). The hydronym niq’ literally means ‘on MAP BY JAMES KARI AND DIXON JONES the upstream’. The na’/ niq’ hyronymn boundary on the Tanana INTRODUCTION 39 ‡Introducing the Proto-Dene Lex Loci with Selected Dene Place Names South and West of the Alaska Range by James Kari For further study on PDLL refer to discussions and examples on pages xii, 14, 39, 141, 154, 214–215, 217, 221–222, 227–229, and 309.