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Lost River - Karst Information Portal

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2007 NSS Convention Guidebook<br />

170<br />

Figure 60. The True Rise of <strong>Lost</strong> <strong>River</strong>. Photo by Byrd and Strunk, 1992.<br />

Figure 61. Cross-section of the True Rise of <strong>Lost</strong><br />

<strong>River</strong>. From Steve Maegerlein, about 1978.<br />

long east to west, 30 feet wide north to south,<br />

and 11 feet deep confined by mud banks on<br />

the east side of the <strong>Lost</strong> <strong>River</strong>. An underwater<br />

opening near the east end of the channel is a<br />

nearly vertical slot that allows divers to descend<br />

to a depth of 160 feet. Most of the water rises<br />

in this slot-like passage, as yet unexplored, at<br />

about the same stratigraphic position of the<br />

gypsum beds in the lower part of the St Louis<br />

Limestone. Chemical analyses indicate higher<br />

sulfate percentages. The True Rise is available<br />

for visitation by smaller field trip parties. An<br />

old iron bridge over the dry bed of <strong>Lost</strong> <strong>River</strong><br />

limits bus traffic. See Figures 60 and 61.<br />

Travel to State Road 56 and<br />

French Lick<br />

From the Orangeville Rise, travel westerly<br />

and southerly almost 5 miles through the <strong>Lost</strong><br />

<strong>River</strong> Valley and Crawford Upland to the<br />

intersection of County Road 725W with State<br />

Road 56 just east of Prospect. This drive allows<br />

reexamination of the topographic transition<br />

from the Crawford Upland to the Mitchell<br />

Plain, the general Chester Escarpment and

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