2 edition of Quaternary and engineering geology in the central part of the Alaska Range. found in the catalog.
Quaternary and engineering geology in the central part of the Alaska Range.
|Contributions||Black, Robert Foster, 1918-|
|LC Classifications||QE75 .P9 no. 293|
|The Physical Object|
|Pagination||viii, 118 p. :|
|Number of Pages||118|
|LC Control Number||gs 58000240|
Quaternary Geology Description. Quaternary Geology is ,scale data that illustrates the geologic features formed in Connecticut during the Quaternary Period, which spans from ± million years ago to the present and includes the Pleistocene (glacial) and Holocene (postglacial) Epochs. Reger, R.D., , Reconnaissance geology of the Talkeetna-Kashwitna area, Susitna River basin, Alaska: Alaska Division of Geological and Geophysical Surveys Alaska Open-File Report AOFa, 1 sheet, scale International Association for Quaternary Research; Symposium on Cold Climate Environments and Processes; ( ; Fairbanks, Alaska) Contents: The Periglacial Environment / Troy L. Pewe--Factors Influencing Discontinuous Permafrost in Canada / R.J.E. Brown--Underground ice in the Quaternary Deposits of the Yana-Indigirka Lowland as a Genetic. Professional Summary My research and teaching focuses on understanding the nature and dynamics of Quaternary paleoenvironmental change and landscape evolution, environmental geology, natural hazards, and geochronology.
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Plate 1, Map of the Alaska Range between longitude degrees 30 minutes and degrees and 00 minutes west, showing bedrock geology, scale( M) Plate 2, Geologic map of parts of Healy D-4 and Healy D-5 quadrangles, Alaska, showing Pleistocene deposits along.
Quaternary geology of the Nenana River Valley and adjacent parts of the Alaska Range. Engineering geology along part of the Alaska Railroad. Geologic map and sections of the Moody Landslide area, along the Nenana river, Alaska.
Geologic map of parts of Healy D-4 and D-5 quadrangles, Alaska, showing Pleistocene deposits along the Nenana River. This book summarizing the Quaternary geology of central and south-central Alaska and containing descriptions of localities between Fairbanks and Anchorage was prepared in for Field Conference F of the VII Congress of the International Association for Quaternary Manufacturer: State of Alaska.
Quaternary geology of the Nenana River valley and adjacent parts of the Alaska Range; Engineering geology along part of the Alaska Railroad Professional Paper A,B. The Geology of Alaska is the largest publication produced in the Decade of North American Geology program, a fitting tribute to this magnificent area.
Geology of part of east-central Alaska. Author(s) Quaternary volcanism in the Alaska Peninsula and Wrangell Mountains, Alaska. Author(s). Permafrost and marine, fluvial, lacustrine, glacial, eolian, and periglacial deposits of Quaternary age that are widespread in the central and southern parts of Alaska are forming today.
Glaciers are common in mountainous areas, and the forces of glacial action that formerly shaped much of the world's land area can be directly observed today in southern Alaska. Quaternary geology of Alaska: Series title: Professional Paper: Series number: DOI: /pp Edition-Year Published: Language: ENGLISH: Publisher: U.S.
Govt. Print. Off., Description: p.; 1 plate and 2 tables in pocket: Google Analytic Metrics: Metrics page: Part or all of this report is presented in Portable Document.
Wahrhaftig, Clyde, and Black, R.F.,Engineering geology along part of the Alaska Railroad, in Wahrhaftig, Clyde, and Black, R.F., Quaternary and engineering geology in the central part of the Alaska Range: U.S.
Geological Survey Professional Paperp. Publication Products. This publication is part of a larger work. PP / Wahrhaftig, C. and Black, R. / QUATERNARY AND ENGINEERING GEOLOGY IN THE CENTRAL PART OF THE ALASKA RANGE, A. Quarternary Geology of the Nenana River Valley and adjacent parts of the Alaska Range, B.
Engineering Geology along part of the Alaska Railroad,pb, pages, 10 plates (in pocket), 58 figs., 8 tables, $ The three major sections of this volume include six chapters describing the regional Quaternary geology of Canada, two describing the Quaternary geology and climatic history of Greenland, and six that review applied Quaternary geology in Canada, including chapters on paleobotanical analysis, geodynamics, geomorphic processes, terrain geochemistry, Quaternary resources, and the influence of the.
Quaternary and Engineering geology in the Central Part of the Alaska Range: U.S. Geological Survey Professional Paper I have used other books in the "Roadside Geology" series for previous trips.
So, although I worked in Alaska many times over the past 40 years, I decided to buy a used copy of "Roadside Geology of Alaska" from Amazon for my first RV trip up the Alaska by: Engineering geology along part of the Alaska Railroad, in Wahrhaftig, C. and Black, R.F., eds., Quaternary and engineering geology in the Quaternary and engineering geology in the central part of the Alaska Range.
book part of the Alaska Range. US Geological Survey Professional Paper pp. 69– Summary of Quaternary geology of the Municipality of Anchorage, Alaska Henry R. Schmoll*, Lynn A. Yehle, Randall G. Updike U.S. Geological Survey, Box MSDenver, COUSA Abstract Quaternary geology of the Upper Cook Inlet region is dominated by deposits of glacier retreats that followed repeated advancesFile Size: 1MB.
Quaternary geology of the Arctic Coastal Plain, northern Alaska John Blandford O'Sullivan Iowa State University Follow this and additional works at: Part of theGeology Commons This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State.
Holocene Climate Inferred from Oxygen Isotope Ratios in Lake Sediments, Central Brooks Range, Alaska - Volume 55 Issue 3 - Lesleigh Anderson, Mark B. Abbott, Bruce P. FinneyCited by: More than t Au were r ecovered from placer operations in the F airbanks district, east-central Alaska.
A) A) Hydraulic mining below a 45 m high bank of loess on Cripple Creek, J Late Quaternary glaciation and equilibrium line altitude variations of the McKinley River region, central Alaska Range.
JASON M. DORTCH 1, LEWIS A. OWEN 1 CAFFEE, M. and BREASE, P. (), Late Quaternary glaciation and equilibrium line altitude variations of the McKinley River region, central Alaska Range. Boreas, – doi: pp / wahrhaftig, c.
and black, r. / quaternary and engineering geology in the central part of the alaska range, a. quarternary geology of the nenana river valley and adjacent parts of the alaska range, b.
engineering geology along part of the alaska railroad,pb, pages, 10 plates (in pocket), 58 figs., 8 tables, $ A 14, yr paleoenvironmental record from Windmill Lake, central Alaska: Lateglacial and Holocene vegetation in the Alaska range. Quaternary Science Reviews, 20 Cited by: 4.
Wahrhaftig, C.,Quaternary geology of the Nenana River valley and adjacent parts of the Alaska Range, in Quaternary and engineering geology in the central part of the Alaska Range: U.S. Geological Survey Professional Paperp. Quaternary and engineering geology in the central part of the Alaska Range Wahrhaftig, Clyde, [ Book, Government publication: ].
Péwé, T.L. Guidebook to the Quaternary Geology of Central and South-Central Alaska INQUA Guidebook for Field Conference F Lincoln Nebraska Academy of Sciences Péwé, T.L. Quaternary Stratigraphic Nomenclature in Unglaciated Central Alaska U.S. Geological Survey Professional Paper Cited by: The timing and direction of climate variability indicated by the oxygen isotope time series from Meli and Tangled Up lakes are consistent with previously established late Holocene glacier advances at ∼ cal yr B.P.
in the central Brooks Range, and high lake-levels at Birch Lake since ∼ cal yr by: Gravel Spread Far North of the Alaska Range. The long distance transport of cobbles and boulders seems to be a common theme.
around many mountains ranges of the Earth. In this chapter, I will document the long distance spread of gravel north of the Alaska Range into central Alaska.
The Alaska Range. The Alaska Range (Figure ) is an arc. Fourth international conference on permafrost, Fairbanks, Alaska, July, Guidebook to permafrost and Quaternary geology along the Richardson and Glenn Highways between Fairbanks and Anchorage, Alaska: Division of Geological and Geophysical Surveys, Department of Natural Resources, Fairbanks, Alaska, p.
1 sheet, scaleBIBLIOGRAPHY OF QUATERNARY GEOLOGY, COPPER RIVER BASIN AND ADJACENT AREAS, SOUTH-CENTRAL ALASKA by Oscar J. Ferrians, Jr.1 U.S. Geological Survey Open-File Report A This report is preliminary and has not been reviewed for conformity with U.S.
Geological Survey editorial standards. Any use of trade, product, or firm names is for descriptiveAuthor: Oscar J. Ferrians. This interactive map displays locations and relative activity of Alaska’s Quaternary faults and folds.
Display MP and MP (pre-Quaternary) overlays together for the most accurate view. The map offers zoom and scroll options, and multiple base map layers.
Click individual fault and fold traces to view basic fault parameters: name, age. Wrangell-St. Elias is a wonderland of geology. Massive peaks, volcanoes, countless glaciers, and huge rivers set the stage for unsurpassed geologic exploration.
This diverse landscape attracts researchers from all over the world to investigate volcanism, glaciation, plate tectonics, and quaternary geology. Alaska Quaternary Center. AQC supports researchers who study the past two million years through its biology, climate, geology and human systems.
This time period is known as the Quaternary Period. Researchers with the center work on projects like helping to date archaeological sites or look at the landscape of Alaska during its last warming period. # Wahrhaftig C.
and Black R. QUATERNARY AND ENGINEERING GEOLOGY IN THE CENTRAL PART OF THE ALASKA RANGE 4to, wps with some spots on spine, some wear, contents vg with pp., 8 plts, 29 figs. Price: $ (stock#PP). This chapter was originally published in the book Developments in Quaternary Science, Vol, published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for noncommercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who know.
Synopsis General: The Denali fault is a major structural element in south-central Alaska, and accommodates a significant amount of the on-land deformation caused by the convergence between the northwestward-moving Pacific plate and the overriding North American plate. Underthrusting and subduction along the Aleutian Trench accommodates most of the plate convergence, but part of the.
The Alaska Range was formed in the Jurassic Age. In the axial part it is composed of intrusive rock (granodiorites); along the edges, of sedimentary rock.
The slopes are steep, rocky, and rugged. Railroads and highways have been built through the deep and sometimes rather broad valleys which cut through the Alaska Range.
Quaternary Science Reviews, 21(), CLIMAP Difference between modern sea surface temperature and estimated February sea surface temperature (in °C) at the last interglaciationyears ago." Image taken from text. Crowley, T.J. and North, G.R. Paleoclimatology - Oxford Monographs on Geology and Geophysics, Figurep Clyde A.
Wahrhaftig (December 1, – April 6, ) was an American geologist who worked for the United States Geological Survey and taught at the University of California at Berkeley. His research areas included Alaska, the Sierra Nevada, and the California Coast Ranges.
He is also known for his field guides to the geology of San Francisco and the Bay AreaAlma mater: Caltech (Bachelors degree). In a large proboscidean femur, probably Mammuthus sp., was found in situ in a bluff exposure at the mouth of the Tyone River in the northwestern part of the Copper River Basin, Alaska.
The regional setting, stratigraphy, radiocarbon chronology, flora, and implications of the fossil locality, which represents the first documented occurrence of Pleistocene terrestrial mammalian fauna in Cited by: Alaska geologic map data.
A GIS database of geologic units and structural features in Alaska, with lithology, age, data structure, and format written and arranged just like the other states. Info: Geologic field notes, geochemical analyses, and field photographs of outcrops and rock samples from the Big Delta B-1 quadrangle, east-central Alaska.
Lake Atna (/ ˈ ɑː t n ə /; also known as Lake Ahtna) was a prehistoric proglacial lake that initially formed approximately 58 ka (thousand years ago) in the Copper River Basin, an area roughly centered around km ( mi) northeast of modern-day Anchorage, lake formed and dispersed during the Wisconsin lake existed in several forms, with several prominent Coordinates: 62°17′04″N °45′00″W / °N.
Roddick, J., Redington, J., and Sorenson, S., Late Quaternary growth of thrust faults and associated folds in the eastern part of the Northern Foothills Fold and Thrust Belt, central Alaska Range, Alaska, AGU Chapman Conference on Active Tectonics and Seismic Potential of Alaska, Girdwood, Alaska.
Gold has also found throughout much of Alaska except in the vast uninhabitable swamps of the Yukon Flats and on the North Slope of the Arctic between the Brooks Range and the Beaufort Sea.
In the vast central uplands and plains and in the Pacific Mountains to the south, numerous gold, silver and massive sulfide deposits are : The Gem Hunter.Geology and assessment of undiscovered oil and gas resources of the Yukon Flats Basin Province, The hydrocarbon potential of the Yukon Flats Basin Province in Central Alaska was assessed in as part of an update to the National Oil and Gas Assessment.The Alaska Region represents a resource-rich, dynamic landscape shaped by volcanos, earthquakes, major rivers, and glaciers.
Here, we conduct research to inform management of Alaska’s extensive natural resources, inform national Arctic energy policy, and provide scientific information to help others understand, respond to, and mitigate impacts from natural hazards.