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Elevation-Derived Hydrography READ Rules: Underground Conduit

A set of naturally occurring subsurface drainage channels formed from the dissolution of soluble rocks in karst terrain or in terrain similar to karst but formed in non-soluble rocks, as by melting of permafrost or ground ice, collapse after mining, and by outflow of liquid lava from beneath its solidified crust (Figure 73).

Media
Imagery and a map depicting a conduit feature.
Figure 73. Example of an Underground Conduit feature, Fayette County, Kentucky. Note how the surface topography does not provide information or clues as to the direction of groundwater flow within the underground conduit. The flow direction was determined by dye-tracing and provided to the USGS Hydrography program.

Delineation

The limit of Underground Conduit is the virtual line connecting two nonadjacent network segments where the NHD has previously placed an underground conduit, or other data sources have mapped the subsurface flowpath between surface water features in karst terrain. Underground Conduit may also be placed in locations where there is evidence of subsurface flowpath between surface water features in thermokarst terrain.

NOTE: A Sink point feature must be placed at the start of an Underground Conduit.  

Representation Rules

Delineate features as points, lines, or polygons based on their area or length along different axes (Table 33).
 

Table 33. Underground Conduit Representation Rules.
Kind of feature object                                       AreaShortest AxisLongest Axis
0-dimensional (point)------
1-dimensional (line)--greater than 0--
2-dimensional (polygon)------
Special Conditions

None.

Data Extraction

Capture Conditions

If Underground Conduit is required to identify a known or highly probable groundwater flowpath with verified outflow location,

then capture.

Attribute Information

FClass 1—Hydrography feature defined within the collection criteria of the elevation-derived hydrography specifications.
FCode 42002—Underground Conduit: Indefinite (a set of naturally occurring subsurface drainage channels formed from the dissolution of soluble rocks in karst terrain or in terrain similar to karst but formed in non-soluble rocks, as by melting of permafrost or ground ice (thermokarst), collapse after mining, and by outflow of liquid lava from beneath its solidified crust).
EClass 0— Not used to create elevation derivatives.

Source Interpretation Guidelines

The following conditions indicates when and why the capture of Underground Conduit is required:

•    When Underground Conduit is part of a network that is represented as being connected. 
•    When there is a previously existing groundwater dataset, or other data indicating the presence of karst, thermokarst, mining systems, volcanic terrain, or similar groundwater terrain types disrupting the hydrographic network.

Special Conditions

None.

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