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Engineering Aspects of Karst

Engineering Aspects of Karst

Metadata also available as - [Outline] - [Parseable text] - [XML] - [DIF]

Frequently-anticipated questions:


What does this data set describe?

Title: Engineering Aspects of Karst
Abstract:
These data are a digital version of U.S. Geological Survey Open File Report 2004-1352, Engineering Aspects of Karst. The open-file report is a map with accompanying explanatory text that shows areas containing distinctive surficial and subterranean features developed by solution of carbonate and other rocks and characterized by closed depressions, sinking streams, and cavern openings. These areas are commonly referred to as karst. Included on the map are areas of "features analogous to karst" also called pseudokarst, which is karst-like terrain produced by processes other than the dissolution of rocks. Also included are lines indicating areas in which extensive historical subsidence has occurred.

When used in its broadest sense, the term karst encompasses many surface and subsurface conditions that give rise to problems in engineering geology. Most of these problems pertain to subterranean features that affect foundations, tunnels, reservoir tightness, and diversion of surface drainage. Subterranean openings may be the habitat of unique and, in some cases, endangered fauna.

Supplemental_Information:
The data set for Engineering Aspects of Karst consists of two map layers. The map layer karst0p075 contains information on karst regions. The map layer karst0l075 contains information on the extent of areas of subsidence. The map layers are distributed and should be used together.

These map layers are intended to provide users with a national scale karst data coverage to use for graphic and demonstration purposes until a new, improved map layer is developed. These data are not intended for and should not be used for site-specific research.

  1. How should this data set be cited?

    Tobin, B.D., and Weary, D.J., 200506, Engineering Aspects of Karst: National Atlas of the United States, Reston, VA.

    Online Links:

  2. What geographic area does the data set cover?

    West_Bounding_Coordinate: -171
    East_Bounding_Coordinate: -67
    North_Bounding_Coordinate: 70
    South_Bounding_Coordinate: 19

  3. What does it look like?

    <http://pubs.usgs.gov/of/2004/1352/data/USA_karst.pdf> (PDF)
    The U.S. Geological Survey Open File Report 2004-1352, Engineering Aspects of Karst. The open-file report consists of a map with accompanying explanatory text. The file is approximately 9.4 Mb.

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

    Calendar_Date: 1984
    Currentness_Reference: Publication date of source material

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

    Geospatial_Data_Presentation_Form: Vector digital data

  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):

      • GT-polygon composed of chains (1464)
      • String (14)

    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 0.000278. Longitudes are given to the nearest 0.000278. Latitude and longitude values are specified in Decimal degrees.

      The horizontal datum used is North American Datum of 1983.
      The ellipsoid used is GRS1980.
      The semi-major axis of the ellipsoid used is 6378137.000000.
      The flattening of the ellipsoid used is 1/298.257222.

  7. How does the data set describe geographic features?

    Karst polygons (described by karst0p075.dbf)
    Areas containing distinctive surficial and subterranean features developed by solution of carbonate and other rocks and characterized by closed depressions, sinking streams, and cavern openings. (Source: U.S. Geological Survey)

    Shape
    The representation of the entity in the data. (Source: National Atlas of the United States)

    ValueDefinition
    Polygon2-dimensional element

    Area
    The size of the shape in square coverage units. In the distributed file, coverage units represent square decimal degrees. (Source: National Atlas of the United States)

    Range of values
    Minimum:0.00000
    Maximum:12.18929

    Perimeter
    The perimeter of the shape in coverage units. In the distributed file, coverage units represent decimal degrees. (Source: National Atlas of the United States)

    Range of values
    Minimum:0.00533
    Maximum:51.71492

    Karst0p075
    Internal feature number. (Source: National Atlas of the United States)

    Range of values
    Minimum:2
    Maximum:1465

    Objectid
    Internal identification number. (Source: U.S. Geological Survey)

    Range of values
    Minimum:0
    Maximum:1670

    K_type
    The abbreviation of the karst type. (Source: U.S. Geological Survey)

    ValueDefinition
    absent_1Fissures, tubes, and caves generally absent; where present in small isolated areas, less than 50 ft (15 m) long; less than 50 ft (15 m) vertical extent; in crystalline, highly siliceous, intensely folded carbonate rock.
    absent_2Fissures, tubes, and caves generally absent; where present in small isolated areas, less than 50 ft (15 m) long; less than 50 ft (15 m) vertical extent; in moderately to steeply dipping beds of carbonate rock.
    absent_3Fissures, tubes, and caves generally absent; where present in small isolated areas, less than 50 ft (15 m) long; less than 50 ft (15 m) vertical extent; in gently dipping to flat-lying beds of carbonate rock.
    long_1Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in metamorphosed limestone, dolostone, and marble
    long_2Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in moderately to steeply dipping beds of carbonate rock.
    long_3Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in gently dipping to flat- lying beds of carbonate rock.
    long_4Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in gently dipping to flat- lying beds of carbonate rock beneath an overburden of noncarbonate material 10 ft (3 m) to 200 ft (60 m) thick.
    long_5Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in moderately to steeply dipping beds of gypsum.
    long_6Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in gently dipping to flat- lying beds of gypsum.
    no_geolThe area does not contain karst.
    pseudo_1Fissures and voids present to a depth of 250 ft (75 m) or more in areas of subsidence from piping in thick, unconsolidated material.
    pseudo_2Fissures and voids present to a depth of 50 ft (15 m) in areas of subsidence from piping in thick, unconsolidated material
    pseudo_3Fissures, tubes, and tunnels present to a depth of 250 ft (75m) or more in lava.
    pseudo_4Fissures, tubes, and tunnels present to a depth of 50 ft. (15 m) in lava.
    short_1Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in metamorphosed limestone, dolostone, and marble
    short_2Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in crystalline, highly siliceous, intensely folded carbonate rock.
    short_3Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in moderately to steeply dipping beds of carbonate rock.
    short_4Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of carbonate rock.
    short_5Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of carbonate rock beneath an overburden of noncarbonate material 10 ft (3 m) to 200 ft (60 m) thick.
    short_6Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in moderately to steeply dipping beds of gypsum
    short_7Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of gypsum.
    short_8Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of gypsum beneath an overburden of nongypsiferous material.
    short_9Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in carbonate zones in highly calcitic granite. Found in Alaska only.
    short_10Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in moderately to steeply dipping beds of carbonate rock with a thin cover of glacial till and frost derived residual soil. Found in Alaska only.

    Descript
    A full description of the karst type. (Source: U.S. Geological Survey)

    ValueDefinition
    Fissures and voids present to a depth of 250 ft (75 m) or more in areas of subsidence from piping in thick, unconsolidated materialPseudokarst areas as described.
    Fissures and voids present to a depth of 50 ft (15 m) in areas of subsidence from piping in thick, unconsolidated materialPseudokarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of carbonate rockKarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of carbonate rock beneath an overburden of noncarbonate material 10 ft (3 m) to 200 ft (60 m) thickKarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in carbonate zones in highly calcitic graniteKarst areas as described. Found in Alaska only.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in crystalline, highly siliceous, intensely folded carbonate rockKarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of gypsumKarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in gently dipping to flat- lying beds of gypsum beneath an overburden of nongypsiferous materialKarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in metamorphosed limestone, dolostone, and marbleKarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in moderately to steeply dipping beds of carbonate rockKarst areas as described.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in moderately to steeply dipping beds of carbonate rock with a thin cover of glacial till and frost derived residual soilKarst areas as described. Found in Alaska only.
    Fissures, tubes and caves generally less than 1,000 ft (300 m) long; 50 ft (15 m) or less vertical extent; in moderately to steeply dipping beds of gypsumKarst areas as described.
    Fissures, tubes, and caves generally absent; where present in small isolated areas, less than 50 ft (15 m) long; less than 50 ft (15 m) vertical extent; in crystalline, highly siliceous, intensely folded carbonate rockKarst areas as described.
    Fissures, tubes, and caves generally absent; where present in small isolated areas, less than 50 ft (15 m) long; less than 50 ft (15 m) vertical extent; in gently dipping to flat-lying beds of carbonate rockKarst areas as described.
    Fissures, tubes, and caves generally absent; where present in small isolated areas, less than 50 ft (15 m) long; less than 50 ft (15 m) vertical extent; in moderately to steeply dipping beds of carbonate rockKarst areas as described.
    Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in gently dipping to flat- lying beds of carbonate rockKarst areas as described.
    Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in gently dipping to flat- lying beds of carbonate rock beneath an overburden of noncarbonate material 10 ft (3 m) to 200 ft (60 m) thickKarst areas as described.
    Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in gently dipping to flat- lying beds of gypsumKarst areas as described.
    Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in metamorphosed limestone, dolostone, and marbleKarst areas as described.
    Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in moderately to steeply dipping beds of carbonate rockKarst areas as described.
    Fissures, tubes, and caves over 1,000 ft (300 m) long; 50 ft (15 m) to over 250 ft (75 m) vertical extent; in moderately to steeply dipping beds of gypsumKarst areas as described.
    Fissures, tubes, and tunnels present to a depth of 250 ft (75m) or more in lavaPseudokarst areas as described.
    Fissures, tubes, and tunnels present to a depth of 50 ft. (15 m) in lavaPseudokarst areas as described.
    no karstThe area does not contain karst.

    Extent of extensive historical subsidence (described by karst0l075.dbf)
    The limits of areas of extensive historical surface subsidence (sinkhole development). Subsidence may be caused by alteration of ground-water conditions due to excessive pumping or diversion of surface drainage. (Source: U.S. geological Survey)

    Shape
    The representation of the entity in the data. (Source: National Atlas of the United States)

    ValueDefinition
    PolyLine1-dimensional element that may or may not surround a 2- dimensional element.

    Length
    The length of the line in coverage units. In the distributed file, coverage units represent decimal degrees. (Source: National Atlas of the United States)

    Range of values
    Minimum:0.54804
    Maximum:11.66906

    Karst0l075
    Internal feature number. (Source: National Atlas of the United States)

    Range of values
    Minimum:1
    Maximum:14

    Objectid
    Internal identification number. (Source: U.S. Geological Survey)

    Range of values
    Minimum:1
    Maximum:14


Who produced the data set?

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

    • B.D. Tobin
    • D.J. Weary

  2. Who also contributed to the data set?

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

    David Weary
    U.S. Geological Survey
    12201 Sunrise Valley Drive
    Reston, VA 20192
    USA

    703-648-6897 (voice)
    [email protected]


Why was the data set created?

These data are intended for geographic display and analysis at the national level, and for large regional areas. The data should be displayed and analyzed at scales appropriate for 1:7,500,000-scale data. No responsibility is assumed by the U.S. Geological Survey in the use of these data.


How was the data set created?

  1. From what previous works were the data drawn?

    KARST (source 1 of 2)
    Davies, W.E., J.H. Simpson, Ohlmacher, G.C., Kirk, W.E., and Newton, E.G., 1984, Engineering Aspects of Karst: U.S. Geological Survey, Reston, VA.

    Type_of_Source_Media: Stable-base material
    Source_Scale_Denominator: 7,500,000
    Source_Contribution: Spatial and attribute information

    Atlas-shore (source 2 of 2)
    National Atlas of the United States, 200206, State Boundaries of the United States: National Atlas of the United States, Reston, VA.

    Type_of_Source_Media: Online
    Source_Scale_Denominator: 2,000,000
    Source_Contribution: Spatial information

  2. How were the data generated, processed, and modified?

    Date: 2004 (process 1 of 2)
    Stable-base negatives of the map (KARST) were scanned 1:1 with the map scale at 600 dpi. The outlines of the karst polygons and the outlines of the areas of historical subsidence were vectorized and attributed in a GIS. The values of the polygons were queried in GIS software to check for empty or incorrect values and the polygons were checked visually against the original printed map for attribute and positional accuracy. The subsidence lines were checked visually against the original printed map for positional accuracy.

    Data sources used in this process:

    • KARST

    Date: 2004 (process 2 of 2)
    Shorelines in the karst file were checked against the shorelines in the National Atlas State boundaries file. Where the lines did not match, the lines from the karst file were replaced with the lines from the National Atlas file. Bogoslof Island, Alaska was deleted because it is smaller than the size limit applied to the National Atlas data.

    Data sources used in this process:

    • KARST
    • Atlas-shore

  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?

    All polygon attributes were manually checked for correct values against the original hard copy map.

  2. How accurate are the geographic locations?

    No tests for horizontal accuracy have been performed on these map layers.

  3. How accurate are the heights or depths?

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

    These map layers shows areas of karst and psuedokarst and the extent of historical subsidence in the fifty United States and the District of Columbia.

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

    These data are believed to be logically consistent, though no rigorous formal tests were performed. Polygon coverages were queried to screen for empty or inconsistent values. Line geometry is topologically clean.


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. Acknowledgment of the National Atlas of the United States of America and (or) the U.S. Geological Survey would be appreciated in products derived from these data.

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

    Earth Science Information Center, U.S. Geological Survey
    507 National Center
    Reston, VA 20192

    1-888-ASK-USGS (1-888-275-8747) (voice)

    Contact_Instructions:
    In addition to the address above there are other ESIC offices throughout the country. A full list of these offices is at <http://ask.usgs.gov/esic_index.html>.
  2. What's the catalog number I need to order this data set?

  3. What legal disclaimers am I supposed to read?

    Although these data have been processed successfully on a computer system at the U.S. Geological Survey, no warranty expressed or implied is made by the U.S. Geological Survey regarding the utility of the data on any other system, nor shall the act of distribution constitute any such warranty. No responsibility is assumed by the U.S. Geological Survey in the use of these data.

  4. How can I download or order the data?


Who wrote the metadata?

Dates:
Last modified: 21-Jun-2006
Metadata author:
Peg Rawson
National Atlas of the United States
12201 Sunrise Valley Drive
Reston, VA 20192

703-648-4183 (voice)
[email protected]

Metadata standard:
FGDC Content Standards for Digital Geospatial Metadata (FGDC-STD-001-1998)



 


Generated by mp version 2.9.1 on Mon Aug 21 14:55:47 2006