Geology of the continenal terrace off the central coast of Oregon

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Frequently-anticipated questions:


What does this data set describe?

Title:
Geology of the continenal terrace off the central coast of Oregon
Abstract:
No formal abstract is available. "This thesis deals with the geology of the continental terrace off the central coast of Oregon. The study includes the area bounded on the east by the shore line (124 04' W to 124 10' W), on the west by the base of the continental slope, at about 125 20' W, on the south by latitude 43 50' N, and on the north by latitude 44 40' N."
Supplemental_Information:
Data digitized by the USGS for inclusion into usSEABED (<http://walrus.wr.usgs.gov/usseabed>); Some data overlaps with Maloney & Byrne, 1964 and Runge, 1966; overlapping data are decommissioned in those reports and are not included in usSEABED.
  1. How should this data set be cited?

    Maloney, Neil Joseph , 1965, Geology of the continenal terrace off the central coast of Oregon: Oregon State University, Corvallis, OR.

    Other_Citation_Details: PhD. thesis

  2. What geographic area does the data set cover?

    West_Bounding_Coordinate: -127.905
    East_Bounding_Coordinate: -124.087
    North_Bounding_Coordinate: 44.747
    South_Bounding_Coordinate: 43.804

  3. What does it look like?

    Maloney_PhD_1965 (JPG)
    Screen grab of sample distribution, coastline, and bathymetry

  4. Does the data set describe conditions during a particular time period?

    Beginning_Date: 1960
    Ending_Date: 1963
    Currentness_Reference: Publication date

  5. What is the general form of this data set?

    Geospatial_Data_Presentation_Form: Paper

  6. How does the data set represent geographic features?

    1. How are geographic features stored in the data set?

      This is a Vector data set. It contains the following vector data types (SDTS terminology):

      • Point (386)

    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 0.00167. Longitudes are given to the nearest 0.00167. Latitude and longitude values are specified in Decimal degrees.

  7. How does the data set describe geographic features?

    Point
    SDTS point (Source: Source report)

    Sample number
    Sample number (Source: Oregon State University)

    Alpha numeric code based on year, month, sample number, and subcore information.

    Lithologic description
    Lithologic description (Source: Source report)

    Description of rocks and sediment, including color

    Gravel
    Amount of gravel in sample (Source: Wentworth 1938)

    No gravel sediment recorded, but is mentioned in the text, as are shells.

    Sand
    Amount of sand in sample (Source: Wentworth 1938)

    Range of values
    Minimum:0
    Maximum:100
    Units:Percent
    Resolution:1.0

    Silt
    Amount of silt in sample (Source: Wentworth 1938)

    Range of values
    Minimum:0
    Maximum:80
    Units:Percent
    Resolution:1.0

    Clay
    Amount of clay in sample (Source: Wentworth 1938)

    Range of values
    Minimum:0
    Maximum:69
    Units:Percent
    Resolution:1.0

    Median
    Median grainsize (Source: None)

    Range of values
    Minimum:0.48
    Maximum:9.04
    Units:Phi
    Resolution:0.0001

    Mean
    Mean grainsize (Source: Inman 1952)

    Range of values
    Minimum:-2.7
    Maximum:9
    Units:Phi
    Resolution:0.0001

    Standard deviation
    Standard deviation of grainsize (Source: Inman 1952)

    Range of values
    Minimum:0.16
    Maximum:5.55
    Units:Phi
    Resolution:0.01

    Skewness
    First skewness of grainsize distribution (Source: Inman, 1952)

    Range of values
    Minimum:-1.45
    Maximum:6.96
    Units:Unitless
    Resolution:0.01

    Skewness
    First skewness of grainsize distribution (Source: Inman, 1952)

    Range of values
    Minimum:-1.45
    Maximum:6.96
    Units:Unitless
    Resolution:0.01

    Kurtosis
    Kurtosis of grainsize distribution (Source: Inman, 1952)

    Range of values
    Minimum:0.1974
    Maximum:6.92
    Units:Unitless
    Resolution:0.0001

    Standard deviation
    Standard deviation of grainsize (Source: Trask, 1932)

    Range of values
    Minimum:1.0985
    Maximum:10.5224
    Units:Phi
    Resolution:0.01

    Skewness
    Skewness of grainsize distribution (Source: Trask, 1932)

    Range of values
    Minimum:0.1544
    Maximum:2.5154
    Units:Unitless
    Resolution:0.01

    Kurtosis
    Kurtosis of grainsize distribution (Source: Trask, 1932)

    Range of values
    Minimum:0.0199
    Maximum:0.3639
    Units:Unitless
    Resolution:0.01

    Rk
    Rock fragments in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:42
    Units:Percent
    Resolution:1.0

    Mica
    Mica in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:26
    Units:Percent
    Resolution:1.0

    Detrital
    Detrital grains in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:100
    Units:Percent
    Resolution:1.0

    Spic
    Spicules in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:86
    Units:Percent
    Resolution:1.0

    Diat
    Diatoms in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:48
    Units:Percent
    Resolution:1.0

    Foram
    Foraminfera in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:42
    Units:Percent
    Resolution:1.0

    Rad
    Radiolaria in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:65
    Units:Percent
    Resolution:1.0

    Glauc
    Glauconite in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:100
    Units:Percent
    Resolution:1.0

    Pyrite
    Pyrite in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:40
    Units:Percent
    Resolution:1.0

    Other
    Other grains in the sand fraction (Source: Source report)

    Range of values
    Minimum:0
    Maximum:5
    Units:Percent
    Resolution:1.0


Who produced the data set?

  1. Who are the originators of the data set? (may include formal authors, digital compilers, and editors)

  2. Who also contributed to the data set?

    Neil Joseph Maloney at Oregon State University for the collection and analysis of data. For inclusion into usSEABED: Digitization: Monica Iglecia (USGS); Formatting corrections: Jane Reid (USGS) and Chris Jenkins (University of Colorado)

  3. To whom should users address questions about the data?

    College of Oceanic and Atmospheric Sciences, Oregon State University
    104 COAS Admin Bldg
    Corvallis, OR 97331-5503

    541-737-3504 (voice)


Why was the data set created?

No specific purpose is given in the dissertation.


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: Unknown (process 1 of 1)
    The settling tube (Emery 1938) was used for the analysis of most of the sand samples. Samples containing shells and pebbles and some of the samples containing appreciable quantities of glauconite were sieved using a set of standard Tyler screens. Samples containing more than four percent silt and clay were dispersed in 0.2 percent Calgon solution; filtered through a millipore filter to remove seawater, and the sediment residue then covered completely with the Calgon solution to exactly 1000 cc, completely dispersed, and hydrometer readings taking at 1, 2, 15, 30, 60, 120, and 1440 minutes after the dispersion. Following the hydrometer analysis, the sediment was wet sieved through a 0.062 mm screen. The sand fraction was then weighed, and if the sand fraction comprised more than four percent of the sample, it was analyzed using the settling tube. Cumulative curves and particle size statistics were calculated using IBM 1410 and IBM 1620 computers. A split of sand from each sample was spread over the grid on a micropaleontology slide and the composition of 150 to 250 grains were noted with the aid of a binocular microscope.

    Person who carried out this activity:

    College of Oceanic and Atmospheric Sciences, Oregon State University
    104 COAS Admin Bldg
    Corvallis, OR 97331-5503

    541-737-3504 (voice)

    Data sources used in this process:
    • Emery, 1938

    Data sources produced in this process:

    • Maloney_PhD_1965

  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?

    No estimate made for the accuracy of the data in the original report. Data digitized by the USGS and partners were visually compared to the source data, and corrected. Where appropriate, data were tested for completeness using MS Excel. Locations checked using GIS.

  2. How accurate are the geographic locations?

    Navigation probably by Loran-A and/or radar. Positions given to tenths of minutes.

  3. How accurate are the heights or depths?

    Depth determination by echosounder. Water depths recorded to nearest fathom; subsample depths given to nearest inch.

  4. Where are the gaps in the data? What is missing?

    Location, sample numbers, sampler type, simplistic rock and sediment descriptions, and water depth (Appendix 1), median grainsize, Trask statistics, Inman statistics, and percent sand, silt, clay (Appendix 2), the composition of the sediment sand fractions (Appendix 3), core descriptions (Appendix 4) were all completely digitized. Textural analyses of the rock samples (Appendix 5) and the more extensive rock sample description (Appendix 6) were not digitized and are not included in usSEABED.

  5. How consistent are the relationships among the observations, including topology?

    Data fall within normal ranges for the given parameters.


How can someone get a copy of the data set?

Are there legal restrictions on access or use of the data?

Access_Constraints: Thesis is available at the USGS library and at other libraries.
Use_Constraints:
Cite N.J. Maloney and Oregon State University as originators of the data.

  1. Who distributes the data set? (Distributor 1 of 2)

    College of Oceanic and Atmospheric Sciences, Oregon State University
    104 COAS Admin Bldg
    Corvallis, OR 97331-5503

    541-737-3504 (voice)

  2. What's the catalog number I need to order this data set?

    536 (285) M297g (USGS library only)

  3. What legal disclaimers am I supposed to read?

    Although this dataset has been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data. Users of the data should be aware of limitations of the data due to possible imprecision due to navigational inaccuracies and limitations of the statistical data.

  4. How can I download or order the data?


  1. Who distributes the data set? (Distributor 2 of 2)

    U.S. Geological Survey
    345 Middlefield Road
    Menlo Park, CA 94025

    650.329.5026 (voice)
    men_lib@usgs.gov

  2. What's the catalog number I need to order this data set?

    523 (285) M297g

  3. What legal disclaimers am I supposed to read?

    Although this dataset has been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data. Users of the data should be aware of the limitations of the data due to possible imprecision due to navigational inaccuracies, statistical limitations, and digitizing errors.

  4. How can I download or order the data?

  5. What hardware or software do I need in order to use the data set?

    None


Who wrote the metadata?

Dates:
Last modified: 2005
Metadata author:
U.S. Geological Survey
c/o Jane A. Reid
Geologist
400 Natural Bridges Drive
Santa Cruz, CA 95060

831-427-4727 (voice)
jareid@usgs.gov

Contact_Instructions: Email preferred
Metadata standard:
CSDGM Version 2 (FGDC-STD-001-1998)


Generated by mp version 2.8.17 on Tue May 16 21:58:18 2006