W [[.1,1 A MS 
KINDLE 
VN " | KENTUCKY SECTIONS. 23 
Five miles northeast of Clermont the blue clay shale of the knob 
•stone " has been extensively denuded of soil and vegetation by 
"washes" on the slope of Deerlick Knob, exposing the following 
section: 
Section 1368 C, at Deerlick Knob, Bullitt I bunty, Ken/nek;/. 
Feet, 
5. Blue clay shale 35 
4. Thin-bedded crinoidal limestone 5 
3. Black shale 15 
2. Covered 1 5 
1. Limestone 3 
73 
Faunule of zone 5 of section 1368 ( ', at Deerlick Knob, Knit nek;/. 
[a, abundant; e, common; r, rare.] 
1. Zaphrentis dalei (a). 
2. Chonetes illinoisensis (r). 
3. Productus semireticulatus (c). 
4. Dielasma cf. bovidens (r). 
5. Spirifer marionensis (r). 
6. S. mortonanus (c). 
7. S. sp. (r). 
8. Athyris lamellosa (a). 
The blue-clay shales containing this faunule are similar in lithologic 
as well as faunal characters to the New Providence shale of southern 
Indiana, of which they are the southern continuation. 
The thin limestone of this section, at the top of the black shale, is 
of particular interest because it occupies the same stratigraphic hori- 
zon as the Rockford limestone 30 miles to the northwest, while it car- 
ries the lower "knob" (New Providence shale) fauna, which is entirely 
unlike that of the Rockford limestone. The following species were 
obtained at Deerlick Knob, Ky. : 
Faunule of zone 4 of section 1368 C, at Deerlick Knob, Kentucky. 
1. Rhipidomella oweni (abundant). I 3. S. suborbicularis (common). 
2. Spirifer mortonanus (common). 
NEW HAVEN, NELSON COUNTY, KY. 
The Devonian limestone was not seen at New Haven and, if present 
there, is very thin. The following section is exposed just west of the 
town, on the bank of Rolling Fork: 
Section 1371 A, at Neir Haven, Ky. 
Feet. 
3. Black shale 5 
2. Covered 4 
1. Dolomitie limestone 7 
The dolomitie limestone, 1 of the above section, furnished the 
following Niagara species: 
Faunule of zone 1 of section 1371 A, near New Haven, Kentucky. 
I. Calymene niagarensis (common). | 2. Dalmanites verrucosus (rare). 
