Zoo GEOLOGY OF OHIO. 
being obliquely beveled in consonance with the angle of the slope of the 
seam. On the other side of the seam the beds are conspicuously differ- 
ent from the above. The most of them are very thin, running from one 
inch to three inches, and the remainder, the lowest, are sometimes eight 
inches thick, varying from five inches. 
Diagram of the Bedding of the Rock at Mr. Steiner’s, 34 miles south-east of Cardington. 
SECTION AT THE Lert (SourH) END or STEINER’s QUARRY. 
IN Gayle Oe Hi ee rear eee na ae er EN ROME VEER OS cacao AL ti, (Bide 
far 2): oes 5) tO Sn CHES «4 sess .ccieedaeecodanes ik noe eee eee ee @G 
jton e DCds'S LO; 12 ANCHES: diss acsaeceom aca ote e eee ee ete renee Sie 
oc) Fae ear enor ncer een aentT Eady ace accu Aodccs obodod oabdbO000 essen gets) (Gen 
Section at THE Norra END or Mr. Strerner’s QUARRY. 
INCOM ce rat eae eRe hess ease tentarcet eos concen code deseo eee Cee ee ene A ft 
pee sar im abedsy(di-tod im Chies)wesntiesseclac cocsdee sec eee eae eee ee @ 
oon ebincker beds (6 to;Smnches) ee. aessscacesecae aerate eeremeeeees My NG Aba, 
Mote ad cam stata ae aes les ae aa aaa a Dette Ong 
SECTION AT Mr. Conarp’s QUARRY. 
Nowe (Hard= pan MDriit sc sscsihne Pare sea sees e sore ee eee eee ee eee eee een eee 3) Eb. 
(oc inimabedsiotlabout Zain esitaccsssecasnten eee een ee eee BM Gia 
ste oe o OOO SDT TCH OG cave i ewcecemetins wacaceel ee cs aun: Seaereae Cae ones eee Sree my 
MO tales bs Ne BRON OR a a Daas Sitges Giangy 
SECTION AT Mr. Brooxs’s QUARRY. 
Now rardepan ID ritti lin dean.e secebeccewsahoee salves ic aeeeinemenen cen noo iene eae: 1) aig 
20 “Sandstone (beds. 2:to4 inches. hh owe eee oeanb an enaa ia ama ners Sais 
13s) Sandstoney bedsi.S) tou 2 AMC eS veo. s sy .eeycseucnee wanbeeaaceee cece terse Orgs 
vi Ab Shale (reported )) ccf iicie.csues cone taweclleousne ta aeceeeeeeen carer sencnenpuetin I 
ROGAE Sse SUE See ee OSU AUTRE eT aE ER RO PAR 
Below No. 4 of the section at Mr. Brooks’s quarry, sandstone is said to 
occur again; but it is probably closely underlain by shale, and belongs 
10 Le ae beds seen in No. 4 of the general section at Mt. Gilead. 
It is noticeable that the most valuable portion of the Berea grit, viz., 
the heavy beds near its base, becomes much thinner in passing south 
into the central part of the State; that the whole becomes finer-grained, 
