CARROLL COUNTY. 1 
Osa CLO MALLO MGR a cha eee eo a le cheers te beak iets meloiolae wit ticle dm ets 0.61 
IHRE We So es Ae OE os COROT RCT Ie Ne a Siete teal tre Sree a eee SL eee a Bes 
MA BITNOMA oooc00 a600 S000 Goes 400050 Dog 800 6500 809000005066 2650 bn00 conG808 0.07 
Potash oy i  CENRD ER NG RORY EP IETS ana Peat ae Lal amenity Ath bes | 0.65 
Soda 
TENG tists PRPs AT ent D Pepe gh ose My ATU a UP ue RRL Uae tA) ae Slit dA RY 99,92 
The gray limestone overlying Coal No. 4 comes to the surface at only 
one point within the county. It was seen in the banks of Sandy Creek, 
just at the Tuscarawas line. It is compact, about two feet thick, and 
quite fossiliferous. Blocks brought out from the shaft on the Trumbull 
Company’s property showed fine specimens of Productus semi-reticulatus 
and Spirifer lineatus. 
Coal No. 4, immediately underlying the gray limestone, crops out at no 
locality within the county. Messrs. Tod, Stambaugh & Co. ine it by 
means of a shaft on the Trumbull Company’s property, Rose »wnship, 
two miles south-west from Magnolia. The works are in char of Mr. 
John Young, to whose intelligent observation I am indebted fi many 
important and interesting facts which otherwise could not hay been 
obtained. The shaft by which this coal is reached was sunk almost 
directly on the summit of the anticlinal already referred to, and the ex- 
hibition in the entry is well worthy of note. The general section, as 
seen in the mine, is: 
FT. IN 
PM CRLAVAIIINES TONG Rae en Aa Ne err stn 2) Roan We es) Mie olathe ew, 2 6 
Up: IBIBO GOR Ks Bae Se ABR A Bac eens Atay eee ats age Po arene Dae aay eS neg 0 4 
Bo! ACORN ise os bites ie hs Bice s ES ts ee pe gee eB tie Ean LE O° ail 
FRAT ONY Oper ates isis hata sina ata SS stil os sais el ale uie oar alels: clecinteicte elas « 0) 
Syn © Oat etree peat nr atere te Ieee mrt poate Nae aia shan at Shale aie Othe one 1 8 
OC Lenya UNA Os Sapa arch ola oth ata aia tare cite etree aid! dinltclaateerete Bs BOG 0 2-3 
ee lackaslatenomslatyacoalene: somuves,© sass cera ass.2e des cae cisisisce oso Sie 0 2-7 
Sh.) LOXDE ML ese Gy cad eis SST ge LS feat SS a BU Ge ae Rg PC Pe oe Re Op O 
DLE INR eae Sh SS6. 62 Sere BEE ODORS SEI HA CRC OT en rss Caeara apne ame ores 0 1 
NOs COR Ge Sec BSA SO ene Ee ene Se Se ea ae eee 0 10 
Ike © TENTS CHAE Ges eS IS te ee er ee Pi See Eee 5 0 
NMC ODI MNO On) ee ee hse eles nein ce tains se ectaee Csi aces amuin’s werg wenie 2a 2 0 
The evidences of disturbance are well marked in the entry for one 
hundred yards from the shaft, after which, the summit of the anticlinal 
having been passed, the south-easterly dip is resumed, and the coal be-. 
comes compact, with a sound roof. At many points along this hundred: 
yards the limestone roof is broken, showing fissures from six to twelve 
inches wide. Two of these extend well into the sandstone above, where 
they became enlarged so as to form reservoirs for water, which, in pass-. 
13 
