24 CONTRIBUTIONS TO DEVONIAN PALEONTOLOGY. [bull.244. 
About 5 miles south of New Haven the following section is exposed 
along the pike at Muldrows Hill: 
Section 1371 /»', at Muldrows Hi/I, Kentucky. 
Feet 
9. Covered 10 
8. Shaly limestone and shale 20 
7. Shale •- 3-5 
6. Limestone 20 
5. Sandstone 9 
4. Limestone 18 
3. Bluish sandstone weathering shaly 40 
2. Blue shaly sandstone 15 
1. Shaly sandstone and shale 15 
The above section shows the interpolation of the Harrodsburg 
("Lower Carboniferous ") limestone beds in the Knobstone sandstone. 
The following section shows a similar interstratification of the lime- 
stone and Knobstone sandstone, 2 miles southwest of New Haven: 
Section 1371 <\ % miles south of New Haven, Ky. 
Ft. In. 
7. Shaly sandstone 8 
6. Limestone 1 8 
5. Gray sandy shale 10 
4. Limestone and shale 18 
3. Covered (mostly shale) 10 
2. Iron-ore concretions 4 
1. Black shale 10 
It may be noted that the limestone at the top of the black shale in 
the Deerlick section (1368 C4) is represented in the above section 
only by a band of ferruginous concretions (1371 C2). No fossils 
were seen in the blue clay shale above the black shale except crinoid 
stems. 
RILEY, MARION COUNTY, KY. 
The Ordovician limestone outcrops about 100 yards northwest of 
Riley station with a dip of 10° to 15° southwest. The black shale is 
exposed in the cut at the station. A short distance northwest of the 
cut the shale rests unconformably on rocks which are probably of 
Niagara age. No fossils were found in them. The Ordovician out- 
crops northwest of Riley station (section 1372 A) afforded the following 
fossils: 
1. Platystrophia erassa (rare). 
'2. V. lynx (common). 
Faunule of section 1372 A, northwest of Riley station. 
3. Murchisonia sp. (common). 
