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Tuesday, July 14, 2020 | History

3 edition of Ground-water and surface-water elevations in the University of Alaska Fairbanks area, 1992-95 found in the catalog.

Ground-water and surface-water elevations in the University of Alaska Fairbanks area, 1992-95

Ground-water and surface-water elevations in the University of Alaska Fairbanks area, 1992-95

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Published by U.S. Dept. of the Interior, U.S. Geological Survey, Earth Science Information Services [distributor] in Fairbanks, Alaska, Denver, CO .
Written in English

    Subjects:
  • Water table -- Alaska -- Fairbanks Region

  • Edition Notes

    Other titlesGround water and surface water elevations in the University of Alaska Fairbanks area, 1992-95
    Statementby Melanie L. Jackson and Michael R. Lilly ; prepared in cooperation with the University of Alaska, Fairbanks
    SeriesU.S. Geological Survey open-file report -- 96-416
    ContributionsLilly, Michael R, University of Alaska, Fairbanks, Geological Survey (U.S.)
    The Physical Object
    FormatMicroform
    Pagination1 v
    ID Numbers
    Open LibraryOL18021126M

    Alaska's Changing Environment Documenting Alaska's physical and biological changes through observations Alaska has recently experienced profound environmental change related to extreme weather events and deviations from the historical climate. Sustained warmth, sea ice loss, coastal flooding, river flooding, and major ecosystem changes have impacted the daily lives of Alaskans . Main phone: Fax: After hours: Dial , which is forwarded to the University Dispatch Center (). Office hours: Monday - Friday, 8 AM - 5 PM.

    The University of Alaska Fairbanks is an AA/EO employer and educational institution and prohibits illegal discrimination against any individual: Learn more about UA's notice of nondiscrimination. Please report any problems or feedback concerning this website to [email protected] © Geophysical Institute, University of Alaska Fairbanks. United States Geological Survey (USGS). Ground-Water Atlas of the United States, Segm Alaska, Hawaii, Puerto Rico and the U.S. Virgin Islands. Published as USGS Hydrologic Investigations Atlas N. University of Alaska Fairbanks (UAF). Ground-Water and Surface-Water Interactions, Fort Wainwright, Alaska. Retrieved online at.

    Alaska’s changing environment: documenting Alaska’s physical and biological changes through observations. H. R. McFarland, Ed. International Arctic Research Center, University of Alaska Fairbanks. Longest growing season ( days) Bethel, Warmest month Yakutat, July Five warmest winters Utqiaġvik, – Flooding Dalton. Rural Surface Water Quality Testing. This is an archived copy of the catalog. To access the The University of Alaska Fairbanks is an AA/EO employer and educational institution and prohibits illegal discrimination against any individual.


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Ground-water and surface-water elevations in the University of Alaska Fairbanks area, 1992-95 Download PDF EPUB FB2

Ground-Water and Surface-Water Elevations in the University of Alaska Fairbanks Area, By Melanie L. Jackson and Michael R. Lilly Abstract The U.S. Geological Survey, in cooperation with the University of Alaska Fairbanks, col­ lected water-elevation data at 50 ground-water sites and 11 surface-water sites.

These data wereFile Size: 1MB. Get this from a library. Ground-water and surface-water elevations in the University of Alaska Fairbanks area, [Melanie L Jackson; Michael R Lilly; University of Alaska Fairbanks.; Geological Survey (U.S.)].

Ground-Water and Surface-Water Elevations in the University of Alaska Fairbanks Area, By Melanie L. Jackson and Michael R. Lilly Abstract The U.S. Geological Survey, in cooperation with the University of Alaska Fairbanks, col- lected water-elevation data at 50 ground-water sites and 11 surface-water sites.

These data were. Ground-water and surface-water elevation data were collected at 61 sites from to by the U.S. Geological Survey in cooperation with the Alaska Department of Transportation and Public Facilities, Fairbanks International Airport. Water-surface elevations were measured in 41 ground-water observation wells and at 20 surface-water sites to help characterize the geohydrology of the.

Water-Elevation, Stream-Discharge, and Ground-Water Quality Data in the Alaska Railroad Industrial Area Fairbanks, Alaska, May to May By Anne T. Kriegler and Michael R.

Lilly U.S. GEOLOGICAL SURVEY Open-File Report Prepared in cooperation with the ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF MINING AND WATER MANAGEMENTCited by: 1.

From May to Maythe U.S. Geological Survey in cooperation with the Alaska Department of Natural Resources, Division of Mining and Water Management collected data on ground-water and surface-water elevations, stream discharge, and ground-water quality in the Alaska Railroad Industrial area in Fairbanks, Alaska.

The data- collection efforts were coordinated with environmental efforts. Jackson, M.L., and Lilly, M.R.,Ground-water and surface-water elevations in the University of Alaska, Fairbanks area, U.S. Geological Survey Open-File Reportp. PDF Noll, R.S.,Hydrologic evaluation of the unconfined aquifer in Last Chance Basin, Juneau, Alaska: Alaska Division of Geological & Geophysical.

TRANSIENT GROUNDWATER AND SURFACE-WATER INTERACTIONS AT FORT WAINWRIGHT, ALASKA A THESIS Presented to the Faculty of the University of Alaska Fairbanks in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE By Matthew Aaron Wegner, B.S.

Fairbanks, Alaska December File Size: 1MB. Notice - The USGS Water Resources Mission Area's priority is to maintain the safety and well-being of our communities, including providing critical situational awareness in times of flooding in all 50 U.S. states and additional territories. Our hydrologic monitoring stations continue to send data in near real-time to NWISWeb, and we are continuing critical water monitoring activities to.

The USGS annually monitors groundwater levels in thousands of wells in the United States. Groundwater level data are collected and stored as either discrete field-water-level measurements or as continuous time-series data from automated recorders. Data from some of the continuous record stations are relayed to USGS offices nationwide through telephone lines or by satellite transmissions.

Not Ranked: %: %: %: VALDEZ GLACIER R AT VALDEZ GLACIER LK NR VALDEZ AK: ft: ft 3 /s. The area of the vapor barrier, then, is about. 3, ft. 2, allowing 10 percent of floor area for doors and windows. means. time. UNIVERSITY OF ALASKA FAIRBANKS. EEM UNIVERSITY OF ALASKA FAIRBANKS. January in Fairbanks.

Let the inside RH be 40 percent and the outside be 70 percent. The table of vapor pres. Review: Groundwater in Alaska (USA) Article (PDF Available) in Hydrogeology Journal 21(1) February with 1, Reads How we measure 'reads'. Claar, D.V., and Lilly, M.R.,Ground-water and surface-water elevations in the Fairbanks International Airport Area, Alaska, U.S.

Geological Survey. PDF GROUND-WATER DATA FOR THE STERLING AREA, ALASKA, by Mary A. Maurer and Roy R. Ireland, Octoberp. PDF PRESENTATION OF GROUND WATER AND SOIL INFORMATION COLLECTED IN PREVIOUS SITE INVESTIGATIONS, RAILROAD INDUSTRIAL AREA, FAIRBANKS, ALASKA, by Mary A.

Maurer, Roy Ireland, and Jim Vohden, Septemberp. The University of Alaska Fairbanks is an AA/EO employer and educational institution and prohibits illegal discrimination against any individual. Learn more about the university's notice of nondiscrimination. For questions or comments regarding this website, contact @ Sincerest thanks and appreciation are extended to our local, state, and federal cooperative partners at Anchorage Water and Wastewater Utility, City of Unalaska Department of Public Works and Utilities, Kenai Peninsula Borough, Alaska Department of Fish and Game, University of Alaska - Fairbanks, Alaska Department of Environmental Conservation, Alaska Department of Transportation and Public.

Statewide Streamflow Table. Current data typically are recorded at to minute intervals, stored onsite, and then transmitted to USGS offices every 1 to 4.

of 5 tolike most Alaska soil, the organic mat-ter holds negative charges, which contribute to the ability of a soil to hold nutrients with positive charges, such as NH. 4 +, Cu. 2+, Zn. 2+, Ca. 2+, Mg. 2+, etc.

In addition to the original plant and animal residues, soil organic matter contains complex compounds relatively resistant to decay. The State of Alaska, Drinking Water Program, does not sample, test, or regulate the construction of private drinking water wells.

In fact, the only local governments that regulate and have established standards for private water wells are the Municipality of Anchorage and the City of North Pole. For program information, contact Alaska Sea Grant, PO BoxFairbanks, Alaska, @, () Alaska Sea Grant is part of the College of Fisheries and Ocean Sciences at the University of Alaska Fairbanks and part.

The new Arctic digital elevation model maps show a much more precise picture of the Interior. This map of the Fairbanks area is rendered to show .Department of Transportation and Public Facilities, Ground-water and surface-water elevations in the Fairbanks International Airport area, Alaska,and selected geohydrologic report references by .