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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