U.S. Geological Survey
2016
Trackline navigation for multi-channel streamer seismic-reflection profiles collected in 2015 by the U.S. Geological Survey along the Delmarva Peninsula, MD and VA (Esri polyline shapefile, GCS WGS 84).
1.0
vector digital data
data release
DOI:10.5066/F7P55KK3
Woods Hole Coastal and Marine Science Center, Woods Hole, Massachusetts
U.S. Geological Survey, Coastal and Marine Geology Program
https://doi.org/10.5066/F7P55KK3
https://cmgds.marine.usgs.gov/data/field-activity-data/2015-001-FA/data/seismics/tracklines/2015-001-FA_MCS_tracks.zip
Edward M. Sweeney
Elizabeth A. Pendleton
Seth D. Ackerman
Brian D. Andrews
Wayne E. Baldwin
William W. Danforth
David S. Foster
E. Robert Thieler
Laura L. Brothers
2016
High-resolution geophysical data collected along the Delmarva Peninsula 2015, U.S. Geological Survey Field Activity 2015-001-FA
2.0
data release
DOI:10.5066/F7P55KK3
Reston, VA
U.S. Geological Survey
https://doi.org/10.5066/F7P55KK3
The Delmarva Peninsula is a 220-kilometer-long headland, spit, and barrier island complex that was significantly affected by Hurricane Sandy in the fall of 2012. The U.S. Geological Survey conducted cruises during the summers of 2014 and 2015 to map the inner continental shelf of the Delmarva Peninsula using geophysical and sampling techniques to define the geologic framework that governs coastal system evolution at storm-event and longer timescales. Geophysical data collected during the cruises include swath bathymetric, sidescan sonar, chirp and boomer seismic reflection profiles, grab sample and bottom photograph data. More information about the USGS survey conducted as part of the Hurricane Sandy Response-- Geologic Framework and Coastal Vulnerability Study can be found at the project website or on the WHCMSC Field Activity Web pages: https://woodshole.er.usgs.gov/project-pages/delmarva/, https://cmgds.marine.usgs.gov/fan_info.php?fan=2014-002-FA and https://cmgds.marine.usgs.gov/fan_info.php?fan=2015-001-FA. Data collected during the 2014 survey can be obtained here: https://doi.org/10.5066/F7MW2F60
This dataset contains trackline navigation for approximately 1,460 km of multi-channel streamer seismic-reflection profiles collected by the U.S. Geological Survey during cruise 2015-001-FA along the Delmarva Peninsula, MD and VA. This information can help spatially correlate the subbottom profiles with other data in the GIS.
20150610
20150617
ground condition
None planned.
-75.831103
-75.156956
37.606200
37.001644
None
U.S. Geological Survey
USGS
Woods Hole Coastal and Marine Science Center
WHCMSC
Coastal and Marine Geology Program
CMGP
shapefile
trackline navigation
survey line
boomer
S-boom
field activity number 2015-001-FA
multi-channel streamer
GeoEel
Geometrics
Applied Acoustics
Esri Shapefile
Marine Geology
ISO 19115 Topic Category
oceans
location
None
Atlantic Ocean
Delmarva Peninsula
Delaware
Maryland
Virginia
Assateague Island
Assateague Island National Seashore
Chincoteague Island
Chincoteague National Wildlife Refuge
Chincoteague Inlet
Chincoteague Bay
Wallops Island
Parramore Island
Cobb Island
Wreck Island
Ship Shoal Island
Myrtle Island
Smith Island
Fisherman Island
Hog Island
none
Public domain data from the U.S. Government are freely redistributable with proper metadata and source attribution. Please recognize the U.S. Geological Survey as the originator of the dataset.
Edward M. Sweeney
U.S. Geological Survey
Physical Scientist
mailing and physical address
384 Woods Hole Road
Woods Hole
Massachusetts
02543-1598
USA
508-548-8700 x2256
508-457-2310
emsweeney@usgs.gov
https://cmgds.marine.usgs.gov/data/field-activity-data/2015-001-FA/data/seismics/tracklines/2015-001-FA_MCS_tracks_browse.jpg
Thumbnail image of multichannel seismic-reflection tracklines for Delmarva Peninsula.
JPEG
Elizabeth A. Pendleton
Seth D. Ackerman
Wayne E. Baldwin
William W. Danforth
David S. Foster
E. Robert Thieler
Laura L. Brothers
2015
High-resolution geophysical data collected along the Delmarva Peninsula 2014, U.S. Geological Survey Field Activity 2014-002-FA
3.0
webpage
data release
DOI:10.5066/F7MW2F60
Reston, VA
U.S. Geological Survey
https://doi.org/10.5066/F7MW2F60
These seismic reflection profile data were collected in a grid at roughly 3.2 kilometer line spacing. Most of the alongshore tracklines were acquired roughly parallel to the orientation of Assateague Island, with crosslines lines running roughly perpendicular to the coast. Line numbering begins at line 1 and ends at line 39. Any spurious data points were removed during processing. For each seismic trackline there is one seismic-profile image that is hyperlinked by the field 'image'. No duplicates exist.
Sections of tracklines where navigation was recorded but no seismic data were logged are not included such as some turns and transits. There is no line l6f1.
Differential Global Positioning System (DGPS) and Wide Area Augmentation System (WAAS) GPS navigation data were acquired with a Proflex and a Hemisphere receiver, which were both recorded using HYPACK software (version 14.0.9.47) (www.hypack.com). The DGPS antenna was located on the port-side of the acquisition van. DGPS horizontal positional accuracy is estimated to be within 3-5 m; WAAS enable GPS is estimated to be less than 2 m.
The applied acoustics S-Boom source was towed 20-m (lines 1-14) and 25-m (lines 15-39) astern of the M/V Scarlet Isabella. The 100-m long GeoEel 16-channel streamer was towed from the starboard side of the M/V Scarlett Isabella on a 4.82 m boom with 20 m (lines 1-18f1, 37 and 38) and 15 m (lines 18f2-36, 39) of tow cable and 10 m of isolation in front of the start of the active channel. The Geometrics CNT-1 seismic acquisition software (version 5.361) logged the navigation coordinates (in arc seconds) to individual trace headers using the Proflex receiver (JD 161-162) and the Hemisphere receiver (JD 162-168). Layback distance between the GPS antenna and the acoustic source and receiver were calculated in post processing. Although horizontal accuracy of navigation positioning is assumed to be within 2 m, inaccuracies likely exceed this value in the seismic reflection data due to uncertainty of azimuths calculated in the layback correction (described in the processing steps).
U.S. Geological Survey
Unpublished Material
raw MCS trackline data
vector digital data
disc
20150610
20150617
ground condition; data were not collected on 20150628 (transition between Legs 1 and 2 of the survey).
raw MCS data
MCS seismic data were collected using S-Boom source and a 100-m long GeoEel 16-channel streamer. The applied acoustics S-Boom source was towed astern of the M/V Scarlet Isabella at a power level of 400 joules. The Geometrics GeoEel, 16-channel liquid filled digital streamer was towed from the starboard side of the vessel, and the center of the first channel of the active section was 10 to 20 m aft of the boomer source. The streamer had a group interval of 3.25 m connected to Geometrics Streamer Power Supply Unit (SPSU). Data were acquired in Geometrics SEG-D format on Windows PC controller system using Geometrics CNT-1 software. The fire rate was 1 s, the record length was 250 ms and the sample interval was 0.25 ms.
A SIOSEIS seismic processing software script (sio_geom) was used as follows:
1. The raw SEG-D shot files were read with the process SEGDDIN specifying the geometrics format; the process HEADER was used to insert time of day into the header based on the start and end times recorded in HYPACK files and from the cruise survey log entries. The process GEOM was used to describe the shot and streamer geometries and to calculate the reflection point (RP) numbers used to gather (sort traces) the seismic line. The process GEOM also set the shot-receiver distance in the trace header of every trace. GEOM type 9 was used for all lines (except for lines 2 to 6 and l30f1) to calculate distances between shots from shot point locations in the SEG-D headers and to bin traces as common RP's (reflection points). GEOM type 6 was specified for lines 2 to 6 (because positions were absent or bad in the header), which computes a distance from last shot (DFLS) for each shot based on the shot time in the header and the navigation from an ASCII file containing time and position. The ASCII navigation file was derived from the HYPACK data and merged with RP files with the Unix join command. The process GATHER was used to sort the shot order traces by the RP numbers (computed by GEOM). A normal move out (NMO) applied a travel time correction to each trace based on time offset and a velocity of 1530 m/s. Lastly, the shot ordered trace gathers were written with the process DISKOX in SEG-Y rev. 1, IEEE floating point format. This step and all subsequent steps were completed by Dave Foster.
2. A SIOSEIS script (sio_gather) was used to sort traces into RP order trace gathers using the RP values calculated by the SIOSEIS process GEOM. RP ordered navigation coordinates to be used in process step 3.
3. A SIOSEIS script (sio_nmo) was used to apply a normal moveout to the RP gathers from step 2. Moveout velocities of 1510 to 1540 m/s were used.
4. A shell script (layback_stack) read the navigation output created in step 2 and extracted the navigation coordinates for channel 1 within each RP. The result was read by a Python script (layback_rp.py), which applied a layback correction (offset from the GPS antenna source and to the midpoint from the source to the first active channel). The script calculated easting and northing differential values between trace positions. Headings between consecutive traces were calculated using the arctangent function (arctan2(dy,dx)), and reciprocal back bearings were determined using a lookup table. Back bearings were smoothed along track using a moving median function. Layback easting and northing offsets were calculated by multiplying the layback distance by the sine and cosine of the smoothed back bearing, respectively. Offset values were then added to the original coordinates to produce layback positions. The script (layback_stack) then called a SIOSEIS script (siostackpop) which stacked the RP gathers and applied a bandpass filter. The process DISKIN read the RP sorted SEG-Y file. The process STACK was used to sum traces, compute the average amplitude for each trace sample, and write the computed samples to one trace. The trace header values of the first trace in the gather were used for the stacked trace. The process FILTER applied a zero-phase bandpass frequency domain filter between 350 and 1800 Hz with a slope of 48 decibel per octave slope. The process HEADER was used to populate the SEG-Y headers with the layback corrected RP coordinates. The processed stacked traces were written to disk with the process DISKOX in SEG-Y rev. 1, IEEE floating point format. The script layback_stack used AWK to format navigation files with unique RP positions and positions for every 100 reflection points in CSV format, which contains attributes for layback corrected UTM Zone 18 coordinates, layback corrected geographic coordinates, line (file) name, year, day, RP number, and fold. Finally, a Python script (GBrptoSQL15001.py) written by Wayne Baldwin, imported the CSV files to the Spatialite (version 3.0.1) enabled SQLite (version 3.7.9) database. Esri shape polyline and shot point files were exported directly from the SQLite database.
20150714
Dave Foster
U.S. Geological Survey
Geologist
mailing and physical address
384 Woods Hole Rd.
Woods Hole
MA
02543-1598
(508) 548-8700 x2271
(508) 457-2310
dfoster@usgs.gov
Vector
Entity point
61
0.000001
0.000001
Decimal degrees
D_WGS_1984
WGS_1984
6378137.000000
298.257224
2015-001-FA_MCS_tracks
Multichannel seismic-reflection tracklines for survey 2015-001-FA along the Delmarva Peninsula.
U.S. Geological Survey
FID
Internal feature number.
Esri
Sequential unique whole numbers that are automatically generated.
Shape
Feature geometry.
Esri
Coordinates defining the features.
LineName
Name of the trackline along which MCS data were collected in the format: line number (i.e. 'l1') + file number (i.e. 'f1').
U.S. Geological Survey
Character set
Image
Name of the PNG image file associated with the MCS survey line. The appended '_stack' in the file name indicates that a stack filter had been applied to the subbottom data.
U.S. Geological Survey
Character set
RP_init
Reflection point at the start of the line.
U.S. Geological Survey
92
96
reflection point
1
RP_end
Reflection point at the end of the line.
U.S. Geological Survey
883
43703
reflection point
1
Year
Year the survey was conducted (YYYY).
U.S. Geological Survey
2015
2015
year
1
JD_init
Julian day at the start of the survey line (DDD). Julian day is the integer number (although recorded here in text string format) representing the interval of time in days since January 1 of the year of collection.
U.S. Geological Survey
161
168
Julian day
1
JD_end
Julian day at the end of the survey line (DDD).
U.S. Geological Survey
161
168
Julian day
1
SurveyID
WHCMSC field activity identifier (e.g. "2015-001-FA" where 2015 is the survey year, 001 is survey number of that year, and FA is Field Activity).
U.S. Geological Survey
Character set
VehicleID
Survey vessel name.
U.S. Geological Survey
Character set
DeviceID
Sonar device used to collect MCS data in the format: source (AA S-Boom)/receiver (GeoEel).
U.S. Geological Survey
Character set
Length_km
Length of MCS data line in kilometers (UTM Zone 18N, WGS 84).
U.S. Geological Survey
1.278
70.097
kilometers
0.001
Edward M. Sweeney
U.S. Geological Survey
Physical Scientist
mailing and physical address
384 Woods Hole Road
Woods Hole
Massachusetts
02543
USA
508-548-8700 x2256
508-457-2310
emsweeney@usgs.gov
USGS data release 2015-001-FA MCS data from the Delmarva Peninsula area (2015-001-FA_MCS_tracks.zip). The zip file contains a folder with the following shapefile: 2015-001-FA_MCS_tracks.shp, a browse graphic (2015-001-FA_MCS_tracks_browse.jpg) and Federal Geographic Data Committee (FGDC) Content Standards for Digital Geospatial Metadata (CSDGM) metadata files (2015-001-FA_MCS_tracks.xml) in four standard formats are also included in the zip file.
Neither the U.S. Government, the Department of the Interior, nor the USGS, nor any of their employees, contractors, or subcontractors, make any warranty, express or implied, nor assume any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, nor represent that its use would not infringe on privately owned rights. The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the USGS in the use of these data or related materials. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Shapefile
Spatialite version 3.0.1
Shapefile
The WinZip (version 14.0) file contains a shapefile of MCS tracklines collected by the U.S. Geological Survey - Woods Hole Coastal and Marine Science Center along the Delmarva Peninsula, MD and VA and the associated metadata.
Use WinZip, 7zip, Peazip or pkUnzip
5
https://cmgds.marine.usgs.gov/data/field-activity-data/2015-001-FA/data/seismics/tracklines/2015-001-FA_MCS_tracks.zip
https://doi.org/10.5066/F7P55KK3
https://cmgds.marine.usgs.gov/data/field-activity-data/2015-001-FA/
Data can be downloaded via the Internet
none
This zip file contains data available in shapefile format. The user must have software capable of reading shapefile format to use these data.
20170419
Edward M. Sweeney
U.S. Geological Survey
Physical Scientist
mailing and physical address
384 Woods Hole Road
Woods Hole
Massachusetts
02543
USA
508-548-8700 x2256
508-457-2310
emsweeney@usgs.gov
FGDC Content Standards for Digital Geospatial Metadata
FGDC-STD-001-1998
local time