CiiiciiniaficDi and Lexington Fossils 35 



scl"-Ool house. A single loose specimen of Cata::xga Jicadi was 

 found east of Concord, in Lewis county, Kentucky. Several speci- 

 mens have been found loose directly east of Wyoming, along the 

 southwestern edge of Fleming county. At both of these Ken- 

 tuckian exposures the specimens were found at the level of the 

 middle, or Clarksville division of the Waynesville bed. but may 

 easily have dropped from the base of the Blanchester division. 



Along Sewell run, immediately south of the pike from Clarks- 

 ville to Wilmington, in Clinton county, Ohio, Dr. George M. 

 Austin found a considerable number of specimens from 6 to 10 feet 

 below the lower Hchcrtclla insciilpta horizon, in the upper part of 

 the Clarksville division. Along Stony Hollow, northwest of 

 Clarksville, Cata::yga licadi occurs within two feet of the base of 

 the lower Hchcrtclla lusciilpta horizon, and a loose specimen occur- 

 red ten feel: lielow this base. Hall and Clarke figure a specimen 

 from the vicinity of \\'aynesville. Ohio. The species figured by 

 Meek in the Ohio Paleontology, vol. i, probablv came from Clinton 

 county. 



Cataj:yga Jicadi is listed from Richmond. Indiana, and probably 

 was obtained a considerable distance down the ri\er from this city. 

 It occurs north of Versailles, being listed as Glassia scJiitchcrtana 

 from this locality. At Madison, Indiana, Cata::;yga Jicadi occurs 

 along the Hitz road, directly west of the great railroad cut, yy feet 

 below the great Colninnaria reef, here forming the base of the 

 Saluda bed. Since the upper Hchcrtclla insciilpta layer, at the top 

 of the Waynesville bed, occurs along the Michigan road t,2 feet 

 below this Colninnaria layer, Catacyga Jicadi must belong about 45 

 feet below the upper Hchcrtclla insciilpta layer. Since the Blan- 

 chester division of the Waynesville bed is not known to exceed 

 20 feet in thickness at Canaan and at Moores Hill. Indiana, it seems 

 probable that at Madison Cata::xga Jicadi occurs in the upper part 

 of the Clarksville division. 



Judging from the i)receding notes, Cata::yga Jicadi occurs in 

 the u])per part of the middle or Clarksville division of the Waynes- 

 ville bed, and at the base of the upper or Blanchester division. In 

 its geogra])hical distribution, its range appears nearly coterminous 

 with the area within which StropJionicna ncglccta, the most widely 

 distributed fossil characteristic of the Blanchester division, has been 

 recognized. It has not been found, so far. south of \\"yoming. Ken- 

 tucky, and Madison. Indiana. 



