USGS

Preliminary Conceptual Models of the Occurrence, Fate, and Transport of Chlorinated Solvents in Karst Regions of Tennessee

Table 4. Distributions of selected geomorphic variables among karst regions of Tennessee

[p10, 10th percentile; p50, median; p90, 90th percentile; p100, maximum; %, percent; <, less than; >, greater than]

 

Depth to bedrock, in meters 1

Land-surface slope, in degrees2

Streamflow recession index, in days per log cycle3

Percent of region in various sinkhole-density classes4

Reported cave entrances per 1,000 square kilometers5

Region

p10

p50

p90

Number of wells

p10

p50

p90

p100

p10

p50

p90

<1% sinkholes

1-10% sinkholes

>10% sinkholes

 

Inner Central Basin

0.9

2.4

7.3

2,544

0

0

2

14

32

32

32

50.2

46.1

3.7

10

Outer Central Basin

1.5

3.7

13.7

3,920

0

2

7

26

35

35

50

94.1

5.9

0

18

Eastern Highland Rim

3.7

14.6

25.0

3,347

0

0

5

22

50

65

140

70.2

23.3

6.5

20

Pennyroyal Plateau

4.9

11.0

18.3

529

0

0

1

9

50

80

80

31.8

52.0

16.2

10

Western Highland Rim

3.0

15.2

35.1

4,703

0

1

4

13

50

120

140

97.4

2.5

0.1

6

Coves and escarpments of the Cumberland Plateau

.9

8.2

25.9

745

1

8

14

34

32

50

100

87.8

7.8

4.4

63

Valley and Ridge

3.4

12.8

38.4

8,925

0

2

8

36

50

80

120

62.1

34.9

3.0

9

Western toe of the Blue Ridge

5.2

19.2

42.7

357

0

3

11

28

75

109

120

73.9

25.1

1.0

30


1. Data from private-well logs maintained by Tennessee Department of Environment and Conservation, Division of Water Supply.

2. U.S. Geological Survey digital elevation model, scale 1:250,000.

3. Distribution based on streamflow recession areas delineated by Bingham (1986) subdivided into 500 x 500 meter cells distributed among karst regions.

4. Crawford and Veni, 1986; based on U.S. Geological Survey topographic quadrangle maps, scale 1:24,000.

5. Cave-entrance locations from Barr (1961) and Matthews (1971).



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