Baltz, Christopher J. and Madonna Ledford (Gray & Paps Cultural Resources Consultants, Cincinnati)

THE ARCHAEOLOGY OF THE MOGAN RIDGE AREA OF THE HOOSIER NATIONAL FOREST


General Survey Description

A cultural resources survey of a 6,280-acre parcel of land in the Mogan Ridge area of the Tell City District, Hoosier National Forest was conducted by Gray & Pape Cultural Resources Consultants of Cincinati, Ohio in late 1989. The project area is located in Union and Leopold Townships of Perry County, Indiana, just northwest of Derby. The Mogan Ridge area is the largest contiguous parcel of land in the Tell City District of the Hoosier National Forest. This area encompasses the Rockhouse Hollow rockshelters, 12 Pe 98 and 12 Pe 100, which are listed in the National Register of Historic Places.

A total of 118 previously undocumented prehistoric and historic archaeological sites were recorded by the survey using shovel testing and walk-over survey techniques. Of the 118 sites, 101 were prehistoric sites or site components. These sites comprised 26 rockshelters and 75 open prehistoric sites. In addition, 25 historic sites or site components were also discovered during this survey. Most of these components consisted of homesteads or farmsteads.

Unusual historic features found during the survey induded a lookout tower, an apparently isolated stacked stone springhouse, a stone bridge or culvert, and a rockshelter that was apparently used as a root cellar. The entrance to this shelter was partially closed by one mortared and one unmortared stone wall.

The amount of information gathered during the survey was not sufficient to recommend any of the 118 sites for inclusion on the National Register of Historic Places. However, further work was recommended for 46 sites. Recommendations included additional work at 21 rockshelter and 7 open prehistoric sites, and further archival research for 17 historic homestead and farmstead sites as well as for the tower site.

The survey of the Mogan Ridge project area produced a higher density of prehistoric sites than several other surveys in the Tell City District of the Hoosier National Forest. The rockshelter density of the Mogan Ridge area is somewhat, but not significantly higher than that of several other areas of the forest. It certainly does not compare with the Branchville area, the focus of Edward Smith's I9X2 rockshelter survey (for the Indiana Historical Society). On the other hand, the density of open prehistoric sites is significantly higher in the Mogan Ridge area. Three possible reasons for this difference are: 1) the screening of shovel tests during the Mogan Ridge survey, 2) the proximity of the project area to major water sources, namely Oil Creek and the Ohio River, and 3) the availability of Derby chert. Apparently, the proximity to water and chert resources were more important than the screening of shovel tests, since few open sites were found in the western portion of the project area, away from the water and chert resources. In the 1989 Cultural Resource Overview of the Hoosier National Forest, Ellen Sieber and her colleagues found that screened and unscreened shovel test techniques discovered open prehistoric sites at approximately the same rate.

A total of 26 rockshelters was recorded during the survey. Several contained bedrock mortars, and, of course, many showed evidence of looting. Three of these shelters were particularly interesting.

Site 12 Pe 810 lies at the head of, and is probably the source of, the Ash House Branch. It has been extensively looted over the years. The spring in the shelter attracted heavy prehistoric occupation which is evidenced by the midden-like soil in the shelter. Outside of the shelter, in the creek below, a variety of artifacts, including several nutting stones were found.

Site 12 Pe 841 is located 150 meters south of the Rockhouse Hollow shelters. This shelter is one of five looted rockshelters that has been included in the Forest Service's experimental looting behavior study. This program, initiated by Forest Service archaeologist Ruth Brinker, consists of the mapping of sites by volunteers, screening of backdirt, and backfilling the looters's holes. Thereafter, these sites are monitored periodically by Forest Service personnel for evidence of new looting.

The third rockshelter of interest is probably unique in the Hoosier National Forest. Site 12 Pe 843 is a "floating" shelter; it is located on a large sandstone block that is in float on the hillside. A small sheltered area is located on the eastern end of a boulder, which is stacked upon a larger boulder. Within the sheltered area are numerous chert flakes. The site lies near an outcrop of Derby chert, and was probably the periodic locus of chert knapping.

Chert Resources

Another interesting aspect of this survey was the location of several bedrock, near bedrock, and residual outcrops of Derby chert. Derby chert was encountered in various forms throughout much of the project area. The historic springhouse noted above was made primarily of poor quality chert blocks.

There has been much discussion over the past few years about the source of Derby chert.

Sources that have been proposed include the Kincaid limestone, which contains chert in some locations in Illinois; the Vienna limestone, which is also reported to contain chert in Illinois; and the Glen Dean limestone. The Vienna limestone appears to be the most likely source, based on a geologic study of the general area.

In his descriptions of the Buffalo Wallow Group, of upper Mississippian rocks, Henry Gray includes the Koohns hill section, which is located within the project area near an outcrop of the Derby chert. Although Gray's description does not include chert, it does note a discontinuity in the column where the Mansfield formation sandstone cuts through the Kincaid, apparently ruling it out. The outcrop of chert is well above the Glen Dean limestone at this point, and at the approximate stratigraphic location of the Vienna limestone. This identification is tentative, and further research is necessary to support this proposition.

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Created: July 25, 1996
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