Isostatic gravity map of Yukon Flats, east-central Alaska

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What does this data set describe?

Title: Isostatic gravity map of Yukon Flats, east-central Alaska
Abstract:
An isostatic gravity map of Yukon Flats at a scale of 1:500,000 was prepared using all know publicly available gravity data. The data were gridded at 0.25 x 0.25 km interval and contoured at 5 mGal interval.
The principal facts (gravity measurements and supporting survey data) are provided along with the printable map.
  1. How might this data set be cited?
    Morin, R.L., 2002, Isostatic gravity map of Yukon Flats, east-central Alaska: U.S. Geological Survey Open-File Report 02-322, U.S. Geological Survey, Menlo Park, California.

    Online Links:

  2. What geographic area does the data set cover?
    West_Bounding_Coordinate: -152.000
    East_Bounding_Coordinate: -141.000
    North_Bounding_Coordinate: 68.000
    South_Bounding_Coordinate: 65.000
  3. What does it look like?
    http://geo-nsdi.er.usgs.gov/metadata/open-file/02-322/browse.png (PNG)
    Reduced-size image of the map sheet, 725x483 pixels, 114k bytes
    http://pubs.usgs.gov/of/2002/0322/pdf/of02-322.pdf (PDF)
    Printable version of the map sheet, 1.5 megabytes
  4. Does the data set describe conditions during a particular time period?
    Calendar_Date: 2002
    Currentness_Reference:
    publication date
  5. What is the general form of this data set?
    Geospatial_Data_Presentation_Form: map
  6. How does the data set represent geographic features?
    1. How are geographic features stored in the data set?
      This is a point data set.
    2. What coordinate system is used to represent geographic features?
      Horizontal positions are specified in geographic coordinates, that is, latitude and longitude. Latitudes are given to the nearest 0.01 minute. Longitudes are given to the nearest 0.01 minute. Latitude and longitude values are specified in Degrees and decimal minutes. The horizontal datum used is North American Datum of 1927.
      The ellipsoid used is Clarke 1866.
      The semi-major axis of the ellipsoid used is 6378206.4.
      The flattening of the ellipsoid used is 1/294.98.
      Vertical_Coordinate_System_Definition:
      Altitude_System_Definition:
      Altitude_Datum_Name: National Geodetic Vertical Datum of 1929 (NGVD29)
      Altitude_Resolution: 0.1
      Altitude_Distance_Units: feet
      Altitude_Encoding_Method: attribute values
  7. How does the data set describe geographic features?
    table1.doc
    Principal facts (gravity observations)
    (stname)
    station identifier (text, 4 characters) identifier without scientific significance
    auxname
    (text, 4 characters) identifier without scientific significance
    latdeg
    degrees of latitude (integer)
    Range of values
    Minimum:64
    Maximum:67
    Units:degrees
    Resolution:1
    latmin
    minutes of latitude (number, 2 places to right of decimal)
    Range of values
    Minimum:0.00
    Maximum:59.90
    Units:minutes
    Resolution:0.01
    londeg
    degrees of longitude (integer)
    Range of values
    Minimum:141
    Maximum:151
    Units:degrees
    Resolution:1
    lonmin
    minutes of longitude (number, 2 places to right of decimal)
    Range of values
    Minimum:0.00
    Maximum:59.95
    Units:minutes
    Resolution:0.01
    elevft
    Elevation in feet
    Range of values
    Minimum:154.2
    Maximum:4722.0
    Units:feet
    Resolution:0.1
    obsgrav
    Observed gravity
    Range of values
    Minimum:981929.03
    Maximum:982383.30
    Units:mgal
    Resolution:0.01
    locsrc
    Location source code
    ValueDefinition
    Agood location, modern published maps, scale 1:63,360
    Bpoor location, modern published maps, scale 1:63,360
    Fgood location, old or unpublished maps, scale 1:63,360
    Gpoor location, old or unpublished maps, scale 1:63,360
    Itransfer from smaller-scale field map, old or unpublished maps, scale 1:63,360
    Kgood location, modern 1:250,000 scale maps
    Lpoor location, modern 1:250,000 scale maps
    gravsrc
    Gravity source code
    ValueDefinition
    ALaCoste & Romberg Geodetic meters: 3 ties within 0.1 mGal
    BLaCoste & Romberg Geodetic meters: other multiple ties
    CLaCoste & Romberg Geodetic meters: ties or drift loops lasting 6 hours
    DLaCoste & Romberg Geodetic meters: ties or drift loops lasting 6-24 hours
    ELaCoste & Romberg Geodetic meters: ties or drift loops lasting 1-4 days
    FLaCoste & Romberg Geodetic meters: ties or drift loops lasting > 4 days
    GWorden or World-Wide meters (loop drift control): 3 ties within 0.1 mGal
    HWorden or World-Wide meters (loop drift control): other multiple ties
    IWorden or World-Wide meters (loop drift control): ties or drift loops lasting 6 hours
    JWorden or World-Wide meters (loop drift control): ties or drift loops lasting 6-24 hours
    KWorden or World-Wide meters (loop drift control): ties or drift loops lasting 1-4 days
    LWorden or World-Wide meters (loop drift control): ties or drift loops lasting > 4 days
    MWorden or World-Wide meters (other drift control): 3 ties within 0.1 mGal
    NWorden or World-Wide meters (other drift control): other multiple ties
    OWorden or World-Wide meters (other drift control): ties or drift loops lasting 6 hours
    PWorden or World-Wide meters (other drift control): ties or drift loops lasting 6-24 hours
    QWorden or World-Wide meters (other drift control): ties or drift loops lasting 1-4 days
    RWorden or World-Wide meters (other drift control): ties or drift loops lasting > 4 days
    SWorden or World-Wide meters (no drift control): 3 ties within 0.1 mGal
    TWorden or World-Wide meters (no drift control): other multiple ties
    UWorden or World-Wide meters (no drift control): ties or drift loops lasting 6 hours
    VOld LaCoste & Romberg or other thermostated meters: 3 ties within 0.1 mGal
    WOld LaCoste & Romberg or other thermostated meters: other multiple ties
    XOld LaCoste & Romberg or other thermostated meters: ties or drift loops lasting 6 hours
    YData from other agencies
    ZUnstated reasons to expect errors
    elevsrc
    Elevation source code
    ValueDefinition
    Abench marks
    Bhighway and railway surveys
    Csea level
    Dspecial surveys
    EUS Weather Bureau, FAA, and U-Wisconsin surveys
    Fblack map elevations
    Gbrown map elevations
    Hblue map elevations
    Ielevations from unpublished maps
    Jriver gradient interpolation, contour interval 0-50 ft
    Kriver gradient interpolation, contour interval 100 ft
    Lriver gradient interpolation, contour interval 200 ft
    Mgood contour interpolation, contour interval 0-50 ft
    Ngood contour interpolation, contour interval 100 ft
    Ogood contour interpolation, contour interval 200 ft
    Ppoor contour interpolation, contour interval 0-100 ft
    Qpoor contour interpolation, contour interval 200 ft
    RAltimetry, good repeated readings, base distance < 15 miles
    SAltimetry, good repeated readings, base distance 15-70 miles
    TAltimetry, alticorder or other good base control, base distance < 15 miles
    UAltimetry, alticorder or other good base control, base distance 15-70 miles
    VAltimetry, poor control, base distance < 15 miles
    WAltimetry, poor control, base distance 15-70 miles
    XAltimetry, poor control, base distance > 70 miles
    YAltimetry involving special adjustments
    ?no data
    @Elevation from nearby bench marks
    $Elevation from differential GPS
    %Elevation from GPS
    sbaacc
    simple bouguer anomaly accuracy code
    ValueDefinition
    1gravity anomaly accuracy, milligals 0.01 Local surveys with special gravity meters and leveling
    2gravity anomaly accuracy, milligals 0.02 Multiple readings with LaCoste & Romberg meters on hard, surveyed surfaces
    3gravity anomaly accuracy, milligals 0.05 Average LaCoste & Romberg data at stable bench marks
    4gravity anomaly accuracy, milligals 0.10 Average LaCoste & Romberg or Worden data at sea level or frost-affected bench marks
    5gravity anomaly accuracy, milligals 0.2 Worden or LaCoste & Romberg data with poor drift or closure errors, or average data at vertical angle bench marks
    6gravity anomaly accuracy, milligals 0.5 Data from loops with closure errors this large, or good data using river gradients, good photogrammetric elevations or well controlled altimetry
    7gravity anomaly accuracy, milligals 1.0 Most surveys based on reasonable altimetry
    8gravity anomaly accuracy, milligals 2.0 Data using moderate-distance altimetry in variable weather or spot elevations on 100-ft contour interval maps
    9gravity anomaly accuracy, milligals 5.0 Data using long-range altimetry in bad weather or contour interpolation on 200-ft contour interval maps
    0gravity anomaly accuracy, milligals >5.0 Data from surveys using long-distance altimetry or altimetry with control failures or errors or some 500-ft contour interval reconnaissance maps
    faa
    free-air anomaly (mgal)
    Range of values
    Minimum:-75.08
    Maximum:117.11
    Units:mgal
    Resolution:0.01
    sba
    simple bouguer anomaly (mgal)
    Range of values
    Minimum:-98.67
    Maximum:18.11
    Units:mgal
    Resolution:0.01
    iztc
    inner-zone terrain correction from station to 0.39 km to 0.01 milligal
    Range of values
    Minimum:0.00
    Maximum:0.00
    Units:mgal
    tc
    terrain correction from 0.39 km to 166.7 km to 0.01 milligal
    Range of values
    Minimum:-0.23
    Maximum:25.37
    Units:mgal
    Resolution:0.01
    cba
    complete bouguer anomaly
    Range of values
    Minimum:-88.99
    Maximum:18.75
    Units:mgal
    Resolution:0.01
    ia
    isostatic anomaly
    Range of values
    Minimum:-39.74
    Maximum:62.08
    Units:mgal
    Resolution:0.01
    dataset
    text of 4 characters matching a value from the dataset table (table 2) identifier without scientific significance
    datum
    Datum code
    ValueDefinition
    (no value) 
    N1967 ellipsoid and conversion of Barnes Alaska datum to IGSN-71 datum
    elev2ft
    second elevation in whole feet
    Range of values
    Minimum:0
    Maximum:4694
    Units:feet
    Resolution:1
    elev2src
    Second elevation source code (same meanings as for elevation source code)
    sba2elev
    simple Bouguer anomaly based on second elevation to 0.1 milligal
    Range of values
    Minimum:-91.5
    Maximum:78.5
    Units:mgal
    Resolution:0.1
    iacode
    isostatic anomaly code
    ValueDefinition
    ISOisostatic correction made from station to 166.7 km.
    ISOWisostatic correction made for the whole earth
    table2.doc
    Data set
    dscode
    Data set code (text of 8 characters) identifier without scientific significance
    project
    Abbreviation (10 character) for name of project in which data set was created identifier without scientific significance
    traverse
    Abbreviation (15 character) for the traverse on which observations were collected identifier without scientific significance
    dsdate
    Date the data set was created coded dates, as MM/DD/YYYY where MM is the month, DD the day, YYYY the 4-digit year, leading zeros retained
    meter
    Gravity meter used identifier without scientific significance
    metertyp
    meter type
    ValueDefinition
    0 
    1 
    2 
    factor
    Meter factor
    Range of values
    Minimum:0.00000
    Maximum:1.00252
    Resolution:0.00001
    gmt
    local time offset from GMT
    Range of values
    Minimum:8
    Maximum:11
    Units:hours
    Resolution:0.00001
    chief
    Name of project chief carrying out survey surnames
    obsrvrs
    Names of people involved in surveying (14 characters) surnames separated by commas, sometimes truncated

Who produced the data set?

  1. Who are the originators of the data set? (may include formal authors, digital compilers, and editors)
    • Morin, R.L.
  2. Who also contributed to the data set?
  3. To whom should users address questions about the data?
    Robert L. Morin
    U.S. Geological Survey
    345 Middlefield Rd, MS 989
    Menlo Park, CA
    U.S.A.

    650-329-5320 (voice)
    morin@usgs.gov

Why was the data set created?

This map was produced to examine gravity anomalies associated with sedimentary basins in the area.

How was the data set created?

  1. From what previous works were the data drawn?
  2. How were the data generated, processed, and modified?
    Date: 1959 (process 1 of 3)
    The gravity data used to make this map were collected between 1959 and 1984. The data were collected by automobile, aircraft, and watercraft. Most of the data were collected as part of a U.S. Geological Survey (USGS) regional gravity data collection project. Some of the data were collected as part of other USGS local projects. One data set was collected by the NGS (National Geodetic Survey).
    Date: 2001 (process 2 of 3)
    data reviewed
    Date: 06-Aug-2003 (process 3 of 3)
    Creation of original metadata record Person who carried out this activity:
    Robert Morin
    U.S. Geological Survey
    USGS
    Menlo Park, CA
    USA

    650-329-5320 (voice)
    morin@usgs.gov
  3. What similar or related data should the user be aware of?

How reliable are the data; what problems remain in the data set?

  1. How well have the observations been checked?
    Observed gravity data are accurate to about 0.05 milligals.
  2. How accurate are the geographic locations?
    Accuracy of the data is about 18 m.
  3. How accurate are the heights or depths?
  4. Where are the gaps in the data? What is missing?
  5. How consistent are the relationships among the observations, including topology?
    Gravity anomalies were visually checked and reviewed at a scale of 1:500,000.
    This map was produced to be used at a map scale of 1:500,000.

How can someone get a copy of the data set?

Are there legal restrictions on access or use of the data?
Access_Constraints: none
Use_Constraints: none
  1. Who distributes the data set? (Distributor 1 of 1)
    U.S. Geological Survey
    345 Middlefield Road
    Menlo Park, CA
    USA

    1-888-ASK-USGS (voice)
  2. What's the catalog number I need to order this data set? USGS Open-File Report 02-322
  3. What legal disclaimers am I supposed to read?
    Although this digital spatial data has been subjected to rigorous review and is substantially complete, it is released on the condition that neither the USGS nor the United States Government may be held liable for any damage resulting from its authorized or unauthorized use.
  4. How can I download or order the data?

Who wrote the metadata?

Dates:
Last modified: 10-Jun-2016
Metadata author:
Peter N Schweitzer
USGS Midwest Area
Collection manager, USGS Geoscience Data Clearinghouse, http://geo-nsdi.er.usgs.gov/
Mail Stop 954
12201 Sunrise Valley Dr
Reston, VA
USA

703-648-6533 (voice)
703-648-6252 (FAX)
pschweitzer@usgs.gov
Metadata standard:
Content Standard for Digital Geospatial Metadata (FGDC-STD-001-1998)

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