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What does this data set describe?

Title:
Geophysical data of field activity W-1-67-MX in Mexico from 11/07/1967 to 12/15/1967
Abstract:
Chief Scientists: Fred Spiess, B. Luyendyk. Geophysical data (LoranC, magnetics, airgun) of field activity W-1-67-MX in Mexico from 11/07/1967 to 12/15/1967, <http://walrus.wr.usgs.gov/infobank/w/w167mx/html/w-1-67-mx.meta.html>.
Supplemental_Information:

Equipment Used -
LoranC Loran, but not sure if A or C
magnetics Varian MFD Proton-Precession magnetometer
airgun 40 cu. in. airgun, Gifft recorder
Notes -
Scripps Institution of Oceanography
Publications -
Normark, William R., and Curray, Joseph R., 1968, Geology and structure of the
tip of Baja California, Mexico: Geological Society of America Bulletin, v. 79,
no. 11, p. 1589-1600.<BR>
<HR>
Normark, W.R., Loughridge, Michael S., and Spiess, F.N.,
1968, Detailed channel morphology of the La Jolla submarine fan valley:
American Geophysical Union Transactions, v. 49, no. 1, p. 212.<BR>
<HR>
Normark, W.R., and Piper, D.J.W., 1969, Deep-sea fan
valleys, past and present: Geological Society of America Abstracts Cordilleran
Section, v. pt. 3, p. 49.<BR>
<HR>
Normark, William R., 1969, Erosional deep sea fan valleys:
Geological Society of America Abstracts Rocky Mountain Section, v. pt. 5, p.
59.<BR>
<HR>
Normark, W.R., Allison, E.C., and Curray, J.R., 1969, The geology of the Pacific
continental margin of the peninsula of Baja California: Geological Society of
America Abstracts, Annual Meeting, v. pt. 7, p. 163.<BR>
<HR>
Normark, W.R., and Spiess, F.N., 1969, Active channel system of the San Lucas
submarine fan at the tip of Baja California: Geological Society of America
Special Paper, p. 220-221.<BR>
<HR>
Normark, William R., 1970, Growth patterns of deep-sea fans: The American
Association of Petroleum Geologists Bulletin, v. 54, no. 11, p. 2170-2195.<BR>
<HR>
Normark, William R., 1970, Growth patterns of deep-sea fans: The American
Association of Petroleum Geologists Bulletin, v. 54, no. 11, p. 2170-2195. <BR>
<HR>
Normark, W.R., 1971, Transfer of lower Baja California, Mexico, from North
American to Pacific lithospheric plates: Geological Society of America Abstracts
with Programs, v. 3,
no. 2, p. 172.<BR>
<HR>
Mudie, John D., Normark, William R., and Klitgord, Kim D., 1971, Some more
magnetic lineations observed near the ocean floor in the northeast Pacific and
possible implications on Gilbert geomagnetic chronology: American Geophysical
Union Eos, Transactions, v. 52, no. 4, p. 194.<BR>
<HR>
Normark, William R., 1969, Growth patterns of deep-sea fans: San Diego, La
Jolla, CA, University of California, dissertation.
<HR>
Normark, William R., 1970, Growth Patterns of Deep-Sea Fans: San Diego, CA,
University of California, Scripps Institution of Oceanography Contributions, v.
40, pt. 2, no. 2, p. 1488-1513.<BR>
<HR>
Normark, William R., 1971, Mini-topography of deep-sea fans; geometric
considerations for facies interpretations in turbidites, in Geologic guide
book--Newport Lagoon to San Clemente, Orange County, California: Tulsa, OK,
Society of Economic Paleontologists and Mineralogists, Pacific Section.<BR>
<HR>
Klitgord, Kim D., Mudie, John D., and Normark, William R., 1972, Magnetic
Lineations Observed Near the Ocean Floor and Possible Implications on the
Geomagnetic Chronology of the Gilbert Epoch: The Geophysical Journal of the
Royal Astronomical Society, v. 28, no. 1, p. 35-48.<BR>
<HR>
Normark, William R., 1972, Submarine canyons and fan-valleys; factors affecting
growth processes of deep-sea fans (abst.), in A conference on modern and ancient
geosynclinal sedimentation: Madison, WI, University of Wisconsin National
Science Foundation.<BR>
<HR>
Normark, W.R., 1976, Growth patterns of deep-sea fans, in Whitaker, J.H., ed.,
Submarine canyons and deep-sea fans; modern and ancient: Stroudsburg, Pa.,
Dowden, Hutchinson and Ross, Inc.<BR>
<HR>
Chase, T.E., Normark, W.R., and Wilde, P., 1976, Compilations of marine geologic
and oceanographic data off the West Coast of the United States: Geological
Society of America Abstracts with Programs, v. 8, no. 6, p. 809. <BR>
<HR>
Chase, T.E., Holmes, M.L., Wilde, P., and Normark, W.R., 1977, Compilation of
marine geologic and oceanographic data off the western United States; Cascadia
Sheet: Geological Society of America Abstracts with Programs, v. 9, no. 7, p.
926. <BR>
<HR>
Normark, W.R., 1977, Neogene basins and transform motion within the Pacific
continental margin of Baja California: Offshore Technology Conference, no. 9, v.
3, Preprints, p. 93-100.<BR>
<HR>
Normark, W.R., Hess, G.R., and Spiess, F.N., 1978, Mapping of small scale
(outcrop-size) sedimentological features on modern submarine fans: Offshore
Technology Conference Proceedings, no. 10, v. 1, p. 593-598.<BR>
<HR>
Spencer, J.E., and Normark, W.R., 1979, The Neogene Tosco-Abreojos strike-slip
fault within the Pacific margin of southern Baja California, Mexico: Geological
Society of America Abstracts with Programs, v. 11, no. 3, p. 129.<BR>
<HR>
Spencer, J.E., and Normark, W.R., 1979, Tosco-Abreojos fault zone; a Neogene
transform plate boundary within the Pacific margin of southern Baja California,
Mexico: Boulder, CO, Geology, v. 7, no. 11, p. 554-557.<BR>
<HR>
Chase, T.E., Normark, W.R., Thomas, J.A., Holmes, M.L., and Wilde, P., 1979,
Compilation of marine geologic and oceanographic data off the western United
States; southern California continental borderland: Geological Society of
America Abstracts with Programs, v. 11, no. 7, p. 400. <BR>
<HR>
Hess, G.R., and Normark, W.R., 1980, Possible geometries of sandstone bodies as
reflected by geomorphic features on modern submarine fans: American Association
of Petroleum Geologists Bulletin, v. 64, no. 5, p. 722-723. <BR>
<HR>
Normark, William R., Spencer, Jon E., and Ingle, James C., Jr., 1987, Geology
and Neogene history of the Pacific continental margin of Baja California Sur,
Mexico, in Scholl, David W., Grantz, Arthur, and Vedder, John G., eds., Geology
and resource potential of the continental margin of western North America and
adjacent ocean basins, Beaufort Sea to Baja California: Circum-Pacific Council
for Energy and Mineral Resources, Earth Science Series, v. 6, p. 449-472.<BR>

Similar information is available for thousands of other USGS/CMG-related Activities.
If known, available are Activity-specific navigation, gravity, magnetics, bathymetry, seismic, and sampling data; track maps; and equipment information; as well as summary overviews, crew lists, and information about analog materials.
If available, access to physical samples is described in the "WR CMG Sample Distribution Policy" at: <http://walrus.wr.usgs.gov/infobank/programs/html/main/sample-dist-policy.html>
Primary access to the USGS/CMG Information Bank's digital data, analog data, and metadata is provided through... <http://walrus.wr.usgs.gov/infobank/>
This page accomodates a variety of search approaches (e.g., by platform, by region, by scientist, by equipment type, etc.).
  1. How should this data set be cited?

    U.S. Geological Survey (USGS) <http://www.usgs.gov/>, Coastal and Marine Geology Program (CMGP) <http://marine.usgs.gov/>, 20131030, Geophysical data of field activity W-1-67-MX in Mexico from 11/07/1967 to 12/15/1967: U.S. Geological Survey (USGS) <http://www.usgs.gov>, Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>, Menlo Park, CA.

    Online Links:

  2. What geographic area does the data set cover?

    West_Bounding_Coordinate: -116.92480
    East_Bounding_Coordinate: -109.80100
    North_Bounding_Coordinate: 31.82960
    South_Bounding_Coordinate: 22.45920

  3. What does it look like?

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

    Beginning_Date: 07-Nov-1967
    Ending_Date: 15-Dec-1967
    Currentness_Reference: ground condition

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

  6. How does the data set represent geographic features?

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

      Indirect_Spatial_Reference: Mexico
      This is a Point data set. It contains the following vector data types (SDTS terminology):
      • Point

    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 0.00001. Longitudes are given to the nearest 0.00001. Latitude and longitude values are specified in Decimal degrees.

      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:
      Depth_System_Definition:
      Depth_Datum_Name: Local surface
      Depth_Resolution: 0.1
      Depth_Distance_Units: meters
      Depth_Encoding_Method: Attribute values


  7. How does the data set describe geographic features?

    Entity_and_Attribute_Overview:
    Magnetics with Time Stamp <http://walrus.wr.usgs.gov/infobank/programs/html/definition/mag.html>
    Entity_and_Attribute_Overview:
    Navigation with Time Stamp <http://walrus.wr.usgs.gov/infobank/programs/html/definition/nav.html>


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?

    Fred Spiess (Chief Scientist, Scripps); B. Luyendyk (Chief Scientist, Scripps)

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

    U.S. Geological Survey (USGS) <http://www.usgs.gov>, Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>
    Attn: Clint Steele <http://walrus.wr.usgs.gov/staff/csteele.html>
    InfoBank Group Leader <http://walrus.wr.usgs.gov/staff/csteele.html>
    USGS, MailStop 999, 345 Middlefield Road
    Menlo Park, CA 94025-3561
    USA

    (650) 329-5055 (voice)
    (650) 329-5190 (FAX)
    infobank@octopus.wr.usgs.gov <mailto:infobank@octopus.wr.usgs.gov>


Why was the data set created?

These data and information are intended for science researchers, students from elementary through college, policy makers, and general public.


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: 30-Jan-1998 (process 1 of 2)
    Navigation Data
    01/30/1998 clint w-1-67-mx.050
    /bear/programs/ngdc/unrefngdc/unrefngdc
    Integrated navigation (SINS) data
    
    

    Person who carried out this activity:

    U.S. Geological Survey (USGS) <http://www.usgs.gov>, Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>
    Attn: Clint Steele <http://walrus.wr.usgs.gov/staff/csteele.html>
    InfoBank Group Leader <http://walrus.wr.usgs.gov/staff/csteele.html>
    USGS, MailStop 999, 345 Middlefield Road
    Menlo Park, CA 94025-3561
    USA

    (650) 329-5055 (voice)
    (650) 329-5190 (FAX)
    infobank@octopus.wr.usgs.gov <mailto:infobank@octopus.wr.usgs.gov>

    Date: 20-Jun-2012 (process 2 of 2)
    Magnetics Data
    06/20/2012 carolyn w-1-67-mx.221_050
    
    Reprocessed using subroutines from Susan Macmillan's
    IGRF SYNTHESIS PROGRAM <http://www.ngdc.noaa.gov/IAGA/vmod/igrf11.f>
    with IGRF-11 coeffiecients integrated into the source code.
    /infobank/programs/mag/magred1111/magred1111.for
    Using geodetic coordinate system (Earth shape approximated by spheriod)
    with altitude 0.0 km (for sea level).
    
    Input was...
    10/31/1998  /tiger/w/w167mx/mag/w-1-67-mx.220_050
    /bear/programs/edit/automerge/automerge
    
    01/30/1998 clint w-1-67-mx.220
    /bear/programs/ngdc/unrefngdc/unrefngdc
    Edited magnetics data
    
    01/30/1998 clint w-1-67-mx.050
    /bear/programs/ngdc/unrefngdc/unrefngdc
    Integrated navigation (SINS) data
    
    time, lat, long, time(sec) to nearest nav fix, data values
    

    Person who carried out this activity:

    U.S. Geological Survey (USGS) <http://www.usgs.gov>, Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>
    Attn: Clint Steele <http://walrus.wr.usgs.gov/staff/csteele.html>
    InfoBank Group Leader <http://walrus.wr.usgs.gov/staff/csteele.html>
    USGS, MailStop 999, 345 Middlefield Road
    Menlo Park, CA 94025-3561
    USA

    (650) 329-5055 (voice)
    (650) 329-5190 (FAX)
    infobank@octopus.wr.usgs.gov <mailto:infobank@octopus.wr.usgs.gov>

  3. What similar or related data should the user be aware of?

    U.S. Geological Survey (USGS) <http://www.usgs.gov>, Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>, Unknown, USGS/CMG Information Bank <http://walrus.wr.usgs.gov/infobank/>: U.S. Geological Survey (USGS) <http://www.usgs.gov> Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>, Menlo Park, CA.

    Online Links:

    Other_Citation_Details:
    Normark, William R., and Curray, Joseph R., 1968, Geology and structure of the tip of Baja California, Mexico: Geological Society of America Bulletin, v. 79, no. 11, p. 1589-1600. Normark, W.R., Loughridge, Michael S., and Spiess, F.N., 1968, Detailed channel morphology of the La Jolla submarine fan valley: American Geophysical Union Transactions, v. 49, no. 1, p. 212. Normark, W.R., and Piper, D.J.W., 1969, Deep-sea fan valleys, past and present: Geological Society of America Abstracts Cordilleran Section, v. pt. 3, p. 49. Normark, William R., 1969, Erosional deep sea fan valleys: Geological Society of America Abstracts Rocky Mountain Section, v. pt. 5, p. 59. Normark, W.R., Allison, E.C., and Curray, J.R., 1969, The geology of the Pacific continental margin of the peninsula of Baja California: Geological Society of America Abstracts, Annual Meeting, v. pt. 7, p. 163. Normark, W.R., and Spiess, F.N., 1969, Active channel system of the San Lucas submarine fan at the tip of Baja California: Geological Society of America Special Paper, p. 220-221. Normark, William R., 1970, Growth patterns of deep-sea fans: The American Association of Petroleum Geologists Bulletin, v. 54, no. 11, p. 2170-2195. Normark, William R., 1970, Growth patterns of deep-sea fans: The American Association of Petroleum Geologists Bulletin, v. 54, no. 11, p. 2170-2195. Normark, W.R., 1971, Transfer of lower Baja California, Mexico, from North American to Pacific lithospheric plates: Geological Society of America Abstracts with Programs, v. 3, no. 2, p. 172. Mudie, John D., Normark, William R., and Klitgord, Kim D., 1971, Some more magnetic lineations observed near the ocean floor in the northeast Pacific and possible implications on Gilbert geomagnetic chronology: American Geophysical Union Eos, Transactions, v. 52, no. 4, p. 194. Normark, William R., 1969, Growth patterns of deep-sea fans: San Diego, La Jolla, CA, University of California, dissertation. Normark, William R., 1970, Growth Patterns of Deep-Sea Fans: San Diego, CA, University of California, Scripps Institution of Oceanography Contributions, v. 40, pt. 2, no. 2, p. 1488-1513. Normark, William R., 1971, Mini-topography of deep-sea fans; geometric considerations for facies interpretations in turbidites, in Geologic guide book--Newport Lagoon to San Clemente, Orange County, California: Tulsa, OK, Society of Economic Paleontologists and Mineralogists, Pacific Section. Klitgord, Kim D., Mudie, John D., and Normark, William R., 1972, Magnetic Lineations Observed Near the Ocean Floor and Possible Implications on the Geomagnetic Chronology of the Gilbert Epoch: The Geophysical Journal of the Royal Astronomical Society, v. 28, no. 1, p. 35-48. Normark, William R., 1972, Submarine canyons and fan-valleys; factors affecting growth processes of deep-sea fans (abst.), in A conference on modern and ancient geosynclinal sedimentation: Madison, WI, University of Wisconsin National Science Foundation. Normark, W.R., 1976, Growth patterns of deep-sea fans, in Whitaker, J.H., ed., Submarine canyons and deep-sea fans; modern and ancient: Stroudsburg, Pa., Dowden, Hutchinson and Ross, Inc. Chase, T.E., Normark, W.R., and Wilde, P., 1976, Compilations of marine geologic and oceanographic data off the West Coast of the United States: Geological Society of America Abstracts with Programs, v. 8, no. 6, p. 809. Chase, T.E., Holmes, M.L., Wilde, P., and Normark, W.R., 1977, Compilation of marine geologic and oceanographic data off the western United States; Cascadia Sheet: Geological Society of America Abstracts with Programs, v. 9, no. 7, p. 926. Normark, W.R., 1977, Neogene basins and transform motion within the Pacific continental margin of Baja California: Offshore Technology Conference, no. 9, v. 3, Preprints, p. 93-100. Normark, W.R., Hess, G.R., and Spiess, F.N., 1978, Mapping of small scale (outcrop-size) sedimentological features on modern submarine fans: Offshore Technology Conference Proceedings, no. 10, v. 1, p. 593-598. Spencer, J.E., and Normark, W.R., 1979, The Neogene Tosco-Abreojos strike-slip fault within the Pacific margin of southern Baja California, Mexico: Geological Society of America Abstracts with Programs, v. 11, no. 3, p. 129. Spencer, J.E., and Normark, W.R., 1979, Tosco-Abreojos fault zone; a Neogene transform plate boundary within the Pacific margin of southern Baja California, Mexico: Boulder, CO, Geology, v. 7, no. 11, p. 554-557. Chase, T.E., Normark, W.R., Thomas, J.A., Holmes, M.L., and Wilde, P., 1979, Compilation of marine geologic and oceanographic data off the western United States; southern California continental borderland: Geological Society of America Abstracts with Programs, v. 11, no. 7, p. 400. Hess, G.R., and Normark, W.R., 1980, Possible geometries of sandstone bodies as reflected by geomorphic features on modern submarine fans: American Association of Petroleum Geologists Bulletin, v. 64, no. 5, p. 722-723. Normark, William R., Spencer, Jon E., and Ingle, James C., Jr., 1987, Geology and Neogene history of the Pacific continental margin of Baja California Sur, Mexico, in Scholl, David W., Grantz, Arthur, and Vedder, John G., eds., Geology and resource potential of the continental margin of western North America and adjacent ocean basins, Beaufort Sea to Baja California: Circum-Pacific Council for Energy and Mineral Resources, Earth Science Series, v. 6, p. 449-472.



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

  1. How well have the observations been checked?

    Identified as best available version.

  2. How accurate are the geographic locations?

    Unspecified

  3. How accurate are the heights or depths?

    Unspecified

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

    Start and end date/times of data

    Navigation Data (w-1-67-mx.050 [SINS])
    YYYYMMDDHHMMSST    YYYYMMDDHHMMSST
    196711120645000    196711141107000
    196711141315000    196711141824000
    196711141845000    196711150028000
    196711150115000    196711150242000
    196711150315000    196711150322000
    196711150343000    196711150504000
    196711231004000    196711231244000
    196711231307000    196711231442000
    196711231506000    196711231532000
    196711231558000    196711231652000
    196711231719000    196711231859000
    196711231924000    196711240021000
    196711240044000    196711240848000
    196711240912000    196711241301000
    196711241334000    196711250717000
    196711250751000    196711251051000
    196711251115000    196711251145000
    196711251206000    196711251249000
    196711251326000    196711251326000
    196711251353000    196711252004000
    196711252025000    196711252133000
    196711252208000    196711260003000
    YYYYMMDDHHMMSST    YYYYMMDDHHMMSST
    Magnetics Data (w-1-67-mx.221_050)
    YYYYMMDDHHMMSST    YYYYMMDDHHMMSST
    196711120645000    196711120645000
    196711120701000    196711120736000
    196711120748000    196711120855000
    196711120907000    196711120949000
    196711121000000    196711121006000
    196711121018000    196711121031000
    196711121047000    196711121116000
    196711121136000    196711121429000
    196711121442000    196711121442000
    196711121508000    196711121508000
    196711121523000    196711121802000
    196711121813000    196711122036000
    196711122054000    196711122121000
    196711122139000    196711122213000
    196711122228000    196711122258000
    196711122312000    196711122316000
    196711122328000    196711122352000
    196711130007000    196711130035000
    196711130047000    196711130047000
    196711130101000    196711130135000
    196711130200000    196711130223000
    196711130237000    196711130252000
    196711130308000    196711130331000
    196711130343000    196711130400000
    196711130421000    196711130427000
    196711130507000    196711130512000
    196711130552000    196711130559000
    196711130612000    196711130622000
    196711130643000    196711130643000
    196711130702000    196711130702000
    196711130730000    196711130852000
    196711130905000    196711130950000
    196711131005000    196711131029000
    196711131058000    196711131058000
    196711131121000    196711131131000
    196711131147000    196711131147000
    196711131159000    196711131404000
    196711131415000    196711131419000
    196711131435000    196711131632000
    196711131644000    196711131752000
    196711131807000    196711131819000
    196711131834000    196711131903000
    196711131915000    196711131925000
    196711132002000    196711132113000
    196711132132000    196711132150000
    196711132231000    196711132231000
    196711132301000    196711132301000
    196711132336000    196711132346000
    196711132358000    196711140016000
    196711140037000    196711140109000
    196711140121000    196711140121000
    196711140132000    196711140146000
    196711140159000    196711140225000
    196711140247000    196711140247000
    196711140307000    196711140424000
    196711140440000    196711140535000
    196711140552000    196711140552000
    196711140613000    196711140705000
    196711140717000    196711140802000
    196711140816000    196711140816000
    196711140827000    196711140953000
    196711141006000    196711141011000
    196711141024000    196711141024000
    196711141039000    196711141049000
    196711141103000    196711141107000
    196711141315000    196711141322000
    196711141333000    196711141349000
    196711141400000    196711141413000
    196711141426000    196711141434000
    196711141448000    196711141510000
    196711141521000    196711141613000
    196711141627000    196711141634000
    196711141646000    196711141656000
    196711141708000    196711141824000
    196711141845000    196711142214000
    196711142227000    196711142251000
    196711142302000    196711150003000
    196711150017000    196711150028000
    196711150115000    196711150154000
    196711150209000    196711150227000
    196711150239000    196711150242000
    196711150315000    196711150322000
    196711150343000    196711150504000
    196711231004000    196711231014000
    196711231034000    196711231034000
    196711231048000    196711231053000
    196711231108000    196711231112000
    196711231130000    196711231244000
    196711231307000    196711231336000
    196711231348000    196711231355000
    196711231413000    196711231413000
    196711231424000    196711231442000
    196711231506000    196711231532000
    196711231558000    196711231558000
    196711231610000    196711231635000
    196711231649000    196711231652000
    196711231719000    196711231739000
    196711231756000    196711231802000
    196711231821000    196711231831000
    196711231845000    196711231859000
    196711231924000    196711231949000
    196711232000000    196711232052000
    196711232103000    196711232108000
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    YYYYMMDDHHMMSST    YYYYMMDDHHMMSST
    

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

    Unspecified


How can someone get a copy of the data set?

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

Access_Constraints:
Physical materials are under controlled on-site access.
If available, access to physical samples is described in the "WR CMG Sample Distribution Policy" at: <http://walrus.wr.usgs.gov/infobank/programs/html/main/sample-dist-policy.html>
Use_Constraints:
Please recognize the U.S. Geological Survey (USGS) as the source of this information.
Physical materials are under controlled on-site access.
Some USGS information accessed through this means may be preliminary in nature and presented without the approval of the Director of the USGS. This information is provided with the understanding that it is not guaranteed to be correct or complete and conclusions drawn from such information are the responsibility of the user.
This information is not intended for navigational purposes.
Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.

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

    U.S. Geological Survey (USGS) <http://www.usgs.gov>, Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>
    Attn: Clint Steele <http://walrus.wr.usgs.gov/staff/csteele.html>
    InfoBank Group Leader <http://walrus.wr.usgs.gov/staff/csteele.html>
    USGS, MailStop 999, 345 Middlefield Road
    Menlo Park, CA 94025-3561
    USA

    (650) 329-5055 (voice)
    (650) 329-5190 (FAX)
    infobank@octopus.wr.usgs.gov <mailto:infobank@octopus.wr.usgs.gov>

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

    Downloadable Data W-1-67-MX data set <http://walrus.wr.usgs.gov/infobank/w/w167mx/html/w-1-67-mx.meta.html>

  3. What legal disclaimers am I supposed to read?

    Please recognize the U.S. Geological Survey (USGS) as the source of this information.
    Physical materials are under controlled on-site access.
    Some USGS information accessed through this means may be preliminary in nature and presented without the approval of the Director of the USGS. This information is provided with the understanding that it is not guaranteed to be correct or complete and conclusions drawn from such information are the responsibility of the user.
    This information is not intended for navigational purposes.
    Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.

  4. How can I download or order the data?

    • Availability in digital form:

Data format: ASCII Size: 0.0
Network links: <http://walrus.wr.usgs.gov/infobank/w/w167mx/html/w-1-67-mx.nav.html>

Data format: ASCII Size: 0.1
Network links: <http://walrus.wr.usgs.gov/infobank/w/w167mx/html/w-1-67-mx.mag.html>

  • Cost to order the data: None


  • Who wrote the metadata?

    Dates:
    Last modified: 30-Oct-2013
    Metadata author:
    U.S. Geological Survey (USGS) <http://www.usgs.gov>, Coastal and Marine Geology (CMG) <http://walrus.wr.usgs.gov>
    Attn: Clint Steele <http://walrus.wr.usgs.gov/staff/csteele.html>
    InfoBank Group Leader <http://walrus.wr.usgs.gov/staff/csteele.html>
    USGS, MailStop 999, 345 Middlefield Road
    Menlo Park, CA 94025-3561
    USA

    (650) 329-5055 (voice)
    (650) 329-5190 (FAX)
    infobank@octopus.wr.usgs.gov <mailto:infobank@octopus.wr.usgs.gov>

    Metadata standard:
    FGDC Content Standards for Digital Geospatial Metadata <http://www.fgdc.gov/> (FGDC-STD-001-1998 <http://www.its.nbs.gov/nbs/meta/meta.html>)


    Generated by mp version 2.9.13 on Wed Oct 30 08:53:27 2013