WASHINGTON COUNTY. 479 
5. Blossom of coal, Cumberland or Bear Creek seam. oe 
GMO HHO XP OSCC er ean reir c mere NU eps eilenevauceairiissdtie debe asses sisavetees cess 50 0 
7. Limestone (not measured). 
SHPN OME DOSe Cairne treme ee Nonene Aue HaeaUin sive esuteasecevelosice tt ete scises swnenoes 10 0 
DRM CAV ASANOSLOM CME et Noe td cccdecest eet e a ua saae cats sulesarcecaniecinmniwe'n soc josibe se luet/ss 25 0 
10. Coal below bed of stream, once dug a little. 
Bear Creek. (See Map XI., No. 17.) 
On the hill, back of the house of B F. Dyar, section 7, in this town- 
-ship, we find the Hobson coal exposed. It has in two and one-half miles 
from the place of the last section dipped about sixty feet. Mr. Dyar’s 
section is as follows: 
1, Dt, 
1. Nodules of iron ore, hematite. 
Ao alesyamdsamdStOmes| ey ..ccr-\eccacsec-\cecesnes) ccortcer) eeeneriesrtsiesvesemociev ees 34. (0 
SMES AUG SLOME SMC IN Etl yearns tae en sacue eden whee v osu nua drecekseted eouecdu mecunatanss 200 
ANNO tREXPOSEC yee seeviceccae teiesswcees HU ees bc A Tdare ANS A LAA Laie MID en) 
Ha Oatletlsl OO SOME Se alii memes ander Ulta ALU a CCR tn Lie hur MUh aes ani aiha alana ORES 
By i ile sy sees et rire ea Pig alae Be a A ae aT LAPP UA PN AR 0 2 
7. Coal ef SPLURGE SAE BSR ee RENT ARESSO LO ACBAE EEOC IPE Ran an EMM ee pee eaiid IM 
Sue Win denclayire races Woatucdd es. 0 
©.) Chrtunan| oy rays Images tRoyaNey he cicadas nomial cane roncecesetoeedaen ocHanoaune ca rinicdaececdbal e-yiee) 
NO REmMNObrexeo Ose Cipine cect odeuremne oie yun nent lc Me Ne rune eee We eae LA) GQ 
TLS: DA GGVeSIONNG 6 pod aabies Gua HAO HORC ES AGA ECE aon DESO EEE cane ae eee Tarr enna ren orae AMA ie uhad 0 
IZ eelnaterval limon secentoy Mis kao til MATVEI ss .cclne tastes ccenaracssesmedeeee cence, [0D 10 
(See Map XI., No. 24.) 
A section was taken on the north side of March Run hill to obtain the 
interval between a thin seam of coal once mined by Frank Norman, and 
the heavy limestone deposit near the foot of the hill. This was found to 
be ninety-seven feet. The limestone, with the shales between the lay- 
ers, is nine feet thick. Underneath are four feet of shale. A composition 
section showing all the strata on both sides of the hill is as follows: 
Ft. In. 
1. Red shales on top of slate. 
yy, (Onnonamlolbharse Ihhnaversiconane) yavel 01 2a csores Bedods 350 dood ea atts Ui ten ano 2 0 
OM VLOS Elias Me mement ce MeL SMe nsceesrndaiecestinsletedssawueaieciece nec ecedealenoaces dl 0 
ANSE SAIN SUOTLCMeR RCIA sere ieby dua MLN CS SU AU 2 TAL Ua del Uneldalede's ae batedlberalacleculeasue nore O 
EeMmaLwe lis neal Gia rte nenansgeain', GN RAG iSraulsalsist wecde mete ewasericeh agers snap dee meemeas 36 0 
6. Coal once dug, now covered. 
7.) Elardvlimestone near the! top, rest UNSeen «20.6.6: veces ses coeseseccces 20 O 
MSM SAL S LOMCM apap MMI E cumnilN Aa alin Wadia haeumiuatcmemaeussarccde sent, LOU 1 O 
SeoliMsieclaymvithwanlaveronimodules (Ol Ore.csnecectsthecrendscec. estes LOO 
TOY) SLAB ONVEKSHIOY OVS) copa codossiea Bede be Heo HEN ROM Rae ELIE HO FET ne GAN REICH er Se es ee OR 8 
IEC avmshiale menue a hate nied mba uh MUA Yael lo. Bi) 
MOAI S LOM casanenccatetedceeeaer ats ttilen cle soseseéalcoesle sons) efeaanes ante ysis sees seasics 4 0 
