Burns, L.E., CGG, and Fugro GeoServices, Inc., 2014, Wrangellia survey area: Airborne magnetic and electromagnetic data in line (point), grid, vector, and map formats, Talkeetna Mountains, Healy, and Mt. Hayes quadrangles, south-central Alaska: Geophysical Report GPR 2014-1, State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (DGGS), Fairbanks, AK, USA.Online Links:
Planar coordinates are encoded using row and column
Abscissae (x-coordinates) are specified to the nearest 25
Ordinates (y-coordinates) are specified to the nearest 25
Planar coordinates are specified in meters
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 1/294.978698.
//Flight 29003 //Date 2013/06/30 Line 20010 (or 'Tie 29010' instead of 'Line 20010' when appropriate) Followed by all records for points sampled along Line 20010. (Pattern is repeated for each line number).The 'ID CELL' content, particularly combined with the definitions below for this particular survey, provides information about the flight line layout. (Source: L.E. Burns & CGG)
Definitions of the 'FLIGHT' attributes are listed with the 'flight' attribute label below.
Range of values | |
---|---|
Minimum: | 414392.19 |
Maximum: | 545408.53 |
Units: | m |
Range of values | |
---|---|
Minimum: | 6937667.50 |
Maximum: | 7027550.40 |
Units: | m |
The attribute measurement resolution is 0.1 second. The values increase from the beginning of a flight to the end. Only FIDs during production flights are included in the database.
Range of values | |
---|---|
Minimum: | 62.5647087 |
Maximum: | 63.3774650 |
Units: | degrees |
Range of values | |
---|---|
Minimum: | -148.6760665 |
Maximum: | -146.1032101 |
Units: | degrees |
See 'Wrangellia_Linedata.txt' for more information.
Range of values | |
---|---|
Minimum: | 2013/06/30 |
Maximum: | 2013/08/27 |
Units: | day |
Range of values | |
---|---|
Minimum: | 11.34 |
Maximum: | 492.88 |
Units: | m |
Range of values | |
---|---|
Minimum: | 12.05 |
Maximum: | 564.07 |
Units: | m |
Range of values | |
---|---|
Minimum: | 512.15 |
Maximum: | 2196.41 |
Units: | m |
Range of values | |
---|---|
Minimum: | 472.32 |
Maximum: | 2166.88 |
Units: | m |
Range of values | |
---|---|
Minimum: | 55735.60 |
Maximum: | 56369.27 |
Units: | nT |
Range of values | |
---|---|
Minimum: | -495.4 |
Maximum: | 138.27 |
Units: | nT |
Range of values | |
---|---|
Minimum: | 54612.78 |
Maximum: | 62348.25 |
Units: | nT |
Range of values | |
---|---|
Minimum: | 54613.87 |
Maximum: | 62348.25 |
Units: | nT |
Range of values | |
---|---|
Minimum: | 54571.08 |
Maximum: | 62318.09 |
Units: | nT |
Range of values | |
---|---|
Minimum: | 56311.60 |
Maximum: | 56838.55 |
Units: | nT |
Range of values | |
---|---|
Minimum: | -2091.69 |
Maximum: | 5868.86 |
Units: | nT |
Range of values | |
---|---|
Minimum: | 54714.81 |
Maximum: | 62675.36 |
Units: | nT |
Range of values | |
---|---|
Minimum: | -718.15 |
Maximum: | 1020.36 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -18.78 |
Maximum: | 644.83 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -198.57 |
Maximum: | 293.05 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -13.61 |
Maximum: | 175.95 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -171.98 |
Maximum: | 384.65 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -28.10 |
Maximum: | 326.09 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -485.75 |
Maximum: | 1244.62 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -106.08 |
Maximum: | 842.20 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -320.14 |
Maximum: | 1712.89 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -108.41 |
Maximum: | 1214.21 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -718.34 |
Maximum: | 1027.93 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -3.40 |
Maximum: | 644.87 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -198.58 |
Maximum: | 289.59 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -1.55 |
Maximum: | 175.92 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -174.26 |
Maximum: | 376.78 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -17.04 |
Maximum: | 328.98 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -485.81 |
Maximum: | 1244.59 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -4.16 |
Maximum: | 842.18 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -320.12 |
Maximum: | 1713.06 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | -2.00 |
Maximum: | 1227.30 |
Units: | ppm |
Range of values | |
---|---|
Minimum: | 0.89 |
Maximum: | 1325 |
Units: | ohm�m |
Range of values | |
---|---|
Minimum: | 3.33 |
Maximum: | 10750 |
Units: | ohm�m |
Range of values | |
---|---|
Minimum: | 5.87 |
Maximum: | 60000 |
Units: | ohm�m |
Range of values | |
---|---|
Minimum: | -111.74 |
Maximum: | 291.99 |
Units: | m |
Range of values | |
---|---|
Minimum: | -119.06 |
Maximum: | 140.64 |
Units: | m |
Range of values | |
---|---|
Minimum: | -128.89 |
Maximum: | 114.23 |
Units: | m |
Range of values | |
---|---|
Minimum: | -73.35 |
Maximum: | 154.78 |
Units: | unitless |
Range of values | |
---|---|
Minimum: | -32.37 |
Maximum: | 203.45 |
Units: | unitless |
Range of values | |
---|---|
Minimum: | 0.00 |
Maximum: | 0.00 |
Units: | unitless |
Range of values | |
---|---|
Minimum: | 0.00 |
Maximum: | 0.00 |
Units: | unitless |
Range of values | |
---|---|
Minimum: | 0.00 |
Maximum: | 0.00 |
Units: | unitless |
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file, KMZ file
Grid file, Geotiff file
Each file format (DXF and shape file) contains the same information. A DXF file (e.g. Wran_magRMI.dxf) contains the information in layers within the file, and the shape file format consists of each layer as a separate file (e.g. Wran_magRMI_1, Wran_magRMI_2, Wran_magRMI_3, and Wran_magRMI_4). Most sets of shape files in this publication contain up to 5 files. Please refer to the map legends for appropriate line widths and particular label placement. Neither the DXF nor the shape files are attributed. All labeling is done through individual alphanumeric characters, e.g. line number 10050 would be represented by 5 individual characters instead of one number.(Source: CGG)
vector file
vector file
vector file
vector file
vector file
vector file
vector file containing lines for all flight lines
vector file containing alphanumeric characters
file containing alphanumeric characters
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
map in PDF and HPGL/2 format
Fourteen maps are included for the area. All maps in this publication are at a scale of 1:63,360 (inch-to-a-mile). Four map sheets are needed to cover the survey area. Figure 2 of the file gpr2014-1-001_graphic.pdf shows the location of Sheets A through D.
Funding was provided by the Alaska State Legislature through the DGGS Airborne Geophysical/Geological Mineral Inventory (AGGMI) program. A donation of data from Millrock Exploration Corporation, Anchorage, AK, provided increased resolution of some of the area and increased coverage by about 12 sq miles.
The survey was part of the Strategic and Critical Minerals Capital Improvement Project (CIP), a subset of the Alaska Airborne Geophysical/Geological Mineral Inventory Program. The program was funded by the Alaska State Legislature and managed by State of Alaska, Department of Natural Resources (DNR), Division of Geological & Geophysical Surveys (DGGS). The program seeks to catalyze private-sector mineral development investment. The program delineates mineral zones on Alaska state lands that: 1) have major economic value; 2) can be developed in the short term to provide high quality jobs for Alaska; and 3) will provide economic diversification to help offset the loss of Prudhoe Bay oil revenue.
Akima, H., 1970, A new method of interpolation and smooth curve fitting based on local procedures: Journal of the Association of Computing Machinery v. 7, no. 4.Online Links:
- None
Fraser, D.C., 1978, Resistivity mapping with an airborne multicoil electromagnetic system: Geophysics v. 43.Online Links:
- None
Alaska Department of Natural Resources - Land Records Information Section, 1995, Alaska PLSS Section Grid: State of Alaska, Department of Natural Resources, Division, Land Records Information Section (LRIS), Anchorage, Alaska.Online Links:
- <http://mapper.landrecords.info/>
- <http://dnr.alaska.gov/SpatialUtility/SUC?cmd=vmd&layerid=45> (metadata)
Flights were performed with an Aerospatiale AS-350-B3 helicopter at a mean terrain clearance of 200 feet (61 m). Three flight directions were used for the Wrangellia survey in an attempt to remain perpendicular to the regional structural and geologic trends (Fig. 4). Survey flight lines were flown a heading of 135 (NW-SE) in the Block 2, the western part; 162 (NW-SE) in Block 3, the central part; and N-S for Blocks 4 and 1, the eastern part. Traverse lines were spaced at one-quarter mile (402.3 m) intervals for all the DGGS planned survey area. Millrock provided data flown with one-eighth mile flight lines for Block 1, which includes the far northern part and infill lines between existing DGGS flight lines for a small portion south of that area (see gpr2014_001_browsegraphic.pdf, figure 3). Tie lines were flown perpendicular to flight lines, and were spaced at intervals of approximately 3 miles (4,828 m).
A Novatel OEM5-G2L Global Positioning System was used for navigation and flight path recovery. The helicopter position was derived every 0.5 seconds (2 Hz); the ground GPS base station data were collected at 1.0 second (1 Hz) intervals. The use of the differentially-corrected base station data results in a positional accuracy of better than five meters. The positional xy data are interpolated from 2 Hz to 10 Hz. Flight path positions were projected onto the Clarke 1866 (UTM zone 6N) spheroid, 1927 North American datum using a central meridian (CM) of 147 degrees, a north constant of 0, and an east constant of 500,000.
Data sources used in this process:
The calculated magnetic tilt grid (Wran_TiltDer) is the angle between the horizontal gradient and the total vertical gradient, and is useful for identifying the depth and type of magnetic source. The tilt angle is positive over the source, crosses through zero at, or near, the edge of a vertical sided source, and is negative outside the source zone. It has the added advantage of responding equally well to shallow and deep sources and is able to resolve deeper sources that may be masked by larger responses caused by shallower sources.
The first vertical derivative grid was calculated using a fast Fourier transform (FFT) based frequency-domain filtering algorithm. The vertical gradient algorithm enhances the response of magnetic bodies in the upper 500 m and attenuates the response of deeper bodies. The resulting (calculated) vertical gradient grid (Wran_1VD) provides better definition and resolution of near-surface magnetic units and helps to identify weak magnetic features that may not be evident in the total field data.
All magnetic and derivative magnetic grids were then resampled from the 80-m cell size down to a 25-m cell size using a modified Akima (1970) technique to produce the maps and final grids contained in this publication.
Data sources used in this process:
Data sources used in this process:
Data sources used in this process:
Staff, DGGS, Dighem, and WGM, Inc., 1998, CD-ROM containing profile and gridded data and section lines of the 1997 geophysical survey data for Iron Creek area, Talkeetna Mountains Quadrangle, southcentral Alaska: Public Data File PDF 98-9, State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (DGGS), Fairbanks, AK, USA.Online Links:
Burns, L.E., U.S. Bureau of Land Management Corp., Fugro Airborne Surveys Corp., and Stevens Exploration Management Corp., 2003, Line, grid, and vector data of airborne geophysical survey data for the southern Delta River area, east-central Alaska: Geophysical Report GPR 2003-6, State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (DGGS), Fairbanks, AK, USA.Online Links:
Burns, L.E., U.S. Bureau of Land Management Corp., Fugro Airborne Surveys Corp., and Stevens Exploration Management Corp., 2003, Plot files of the airborne geophysical survey data of the southern Delta River area, east-central Alaska: Geophysical Report GPR 2003-5, State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (DGGS), Fairbanks, AK, USA.Online Links:
Pritchard, R.A., 2003, Project report of the airborne geophysical survey for the southern Delta River area, east-central Alaska: Geophysical Report GPR 2003-7, State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (DGGS), Fairbanks, AK, USA.Online Links:
Burns, L.E., U.S. Bureau of Land Management Corp., Fugro Airborne Surveys Corp., and Stevens Exploration Management Corp., 2004, Line, gridded, and vector data, and selected plot files of the airborne geophysical survey data of the Valdez Creek mining district, central Alaska: Geophysical Report GPR 2004-3, State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (DGGS), Fairbanks, AK, USA.Online Links:
McConnell, D.L., 1994, Final summary of 1993 airborne geophysical surveys of the Nome, Circle, Nyac, and Valdez Creek areas: Public Data File PDF 94-36, State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (DGGS), Fairbanks, AK, USA.Online Links:
Survey contracts specified the conditions and specifications under which these data were collected. Altimeter, heading, lag, and frequent EM calibrations were done. More information will be available in the project report to be published in the future.
The helicopter position was derived every 0.5 seconds using post-flight differential positioning to an accuracy of better than 1 m.
The laser altimeter ('ALTLAS_BIRD'), located in the bird (EM equipment and magnetometer housing), had a stated resolution of 0.10 meter. The ALTLAS_BIRD value may be unreliable over bodies of water where the laser returns are scattered.
The linedata file has missing values for the calculated apparent resistivity and apparent depth channels. These are due to an increased altitude that renders the calculations meaningless. More information is in 'Wrangellia__Linedata.txt'.
Data for this survey were collected by a single subcontractor (CGG) who was responsible for collecting and processing the data. One helicopter, one EM system, and one airborne magnetometer were used. The data donated by Millrock Exploration Corporation was flown by CGG immediately after the DGGS survey was finished. CGG continued using the specifications and processing of the data that were used with the DGGS data. Operational frequencies for the EM system varied and are documented in 'Wrangellia_Linedata.txt'.
Are there legal restrictions on access or use of the data?
- Access_Constraints:
- This report, map, and/or dataset is available directly from the State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (see contact information below).
- Use_Constraints:
- Any hard copies or published datasets utilizing these datasets shall clearly indicate their source. If the user has modified the data in any way, the user is obligated to describe the types of modifications the user has made. The user specifically agrees not to misrepresent these datasets, nor to imply that changes made by the user were approved by the State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys. The State of Alaska makes no express or implied warranties (including warranties for merchantability and fitness) with respect to the character, functions, or capabilities of the electronic data or products or their appropriateness for any user's purposes. In no event will the State of Alaska be liable for any incidental, indirect, special, consequential, or other damages suffered by the user or any other person or entity whether from the use of the electronic services or products or any failure thereof or otherwise. In no event will the State of Alaska's liability to the Requestor or anyone else exceed the fee paid for the electronic service or product.
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GPR 2014-1
The State of Alaska makes no expressed or implied warranties (including warranties for merchantability and fitness) with respect to the character, functions, or capabilities of the electronic data or products or their appropriateness for any user's purposes. In no event will the State of Alaska be liable for any incidental, indirect, special, consequential, or other damages suffered by the user or any other person or entity whether from the use of the electronic services or products or any failure thereof or otherwise. In no event will the State of Alaska's liability to the Requestor or anyone else exceed the fee paid for the electronic service or product.
Current geophysics publications are available on paper or Mylar. Please ask for the maps to be printed from HPGL/2 files to ensure the best quality image. To purchase printed reports and maps, contact DGGS by phone (907-451-5020), e-mail (dggspubs@alaska.gov), or fax (907-451-5050). Payment accepted: cash, check, money order, VISA, or MasterCard.
Data format: | Geosoft binary float (GRD) (version Unknown) |
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Network links: |
<http://dx.doi.org/10.14509/27022> |
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Digital files on DVD are available for $10 plus shipping and are free when downloaded online.
Order by phone (907-451-5020), e-mail (dggspubs@alaska.gov), or fax (907-451-5050). Payment accepted: cash, check, money order, VISA, or MasterCard. The geophysics page of the DGGS web site (<http://www.dggs.alaska.gov/pubs/geophysics>) has geophysical order forms for this project and others.
Digital downloads: less than 30 minutes for most files. Free FTP access is available upon request for files not available on the web. Offline CD/DVD-ROMs: 1-2 weeks unless special arrangements are made and an express fee is paid.
DGGS publications are available as free online downloads or you may purchase paper hard-copies or digital files on CD/DVD or other digital storage media over the counter, by mail, phone, fax, or email from the DGGS Fairbanks office. Turnaround time is 1-2 weeks unless special arrangements are made and an express fee is paid. Shipping charge will be the actual cost of postage and will be added to the total amount due. Contact us for exact shipping amount.
Software with ability to use, import, or convert Geosoft float GRD, Geosoft binary GDB or ASCII XYZ files, Autocad DXF files, ESRI Shape files, MapInfo Professional TAB files, Adobe Acrobat PDF, Google Earth files, and text files. Free downloadable interfaces to view or convert the gridded and dxf files are available at the Geosoft Web site (<http://www.geosoft.com>; Oasis Montaj viewer). The KMZ files can be dragged and dropped into the 'My Places' folder of the free downloadable 'Google Earth' software. Freeware software 'printfile' (<http://www.lerup.com/printfile/>) prints HPGL/2 files easily on compatible printers. The HPGL/2 files have brighter colors and sharper topography than the PDF maps and should be used for printing when possible. The PDF format maps are the only maps digitally viewable in this publication.
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