326 GEOLOGY OF OHIO. 
Marysville) (with, Bellefontaine eet ees) seeee rennet aa eagen iced tes seaaras 325 ft 
New @alitormiapenpeeec see tenes SEE ee PRCA Eaton as SOAS Rico’ suooss ola) 
EL MeastlotiNe wei Calidorinia os ey seo nn te eR LIe e eeR 395“ 
ey Edainw City sence WAU ctor yards galvct «cu vila'e cia isised ge Uuactaels DAM ae Ob Ie SLM 226, “ 
Hills westiot Marysvilles.ctc. uinccsccce ccedecsescescennsetcccsmeutucnmeatec st snenniene 1 BaD) 
POOP ae Ne ee eaten wecuiecesceseniveseceleed muetues AR NCO etna 410 ‘ 
ING WiLOTTS ier ee aedha cc als aaa va data tas UUs era Aba an Ca Caan Pl eg RE 460 ‘ 
Flat one-fourth mile east of East Liberty, Logan county............ 0.006. 490 “ 
Top of hill two miles west of Kast Liberty, . aldacay sae stesbeamen 805 “ 
Top of hill two and a half miles west of East Liberty, Logan county.. 880 “ 
Suntaceon vad kun, Zanesield muogany cOumbyamsteweerccisdeen sere steeeee OOOMm 
Divide between Mad Run and Goose Creek, near Zanesfield............ G0. 
Water in) Goose reeks Zanestield seen s eee men een anneal eNO GOH aS 
Divide between Goose Creek and McKee’s Creek, Zanesfield............ 915 * 
Surface of MeKee’s Creek, east of Bellefontaine....... ian eu a en alee 765) 
Divide between McKee and Blue Jacket creeks...............cccses ccoeeess 845“ 
Surface of Blue Jacket Creek, east of Bellefontaine......... ......... 0000 680 ‘‘ 
Depot C. C. C. and I. R. R., Bellefontaine (railroad profile).............. 640 
St. John’s, Auglaize county, hill south of village...............05 essscense oes AQ] “* 
St. John’s, street in front of Bitler House.................. Ue Lae SER le 430 “ 
St. John’s, suriace of little stream west of Village.............csscees secosceee 390 “ 
[The last three points, when connected with Wapakoneta, gave, respectively, 504 
feet, 443 feet, and 405 feet. | 
RharisburgmUniOnCOUmbyscumsaicrcsrceslatesee suocecy se areas nincan sete ecensat 304 ft. 
Essex, EOD) PERG cattle ALR SOs AN CE AU oN, dre acm Ane ea a 309 * 
North-east corner Washington township...... .......0. scsces ssc cec scree esense Rew) 
WY ON Cente ties siveras seh leita uns Ana a totes Nee uicetarc Macatee ste ee chia tnd nen Amt iene ae) 
IDES illest, IOAN, COLL 555000 cocnd0d! ashie00de Dorgaoada Gaghos donsooconmnasaanoags LEE) 
Mad dle bUneics.cincccclsceibassensaorecuoacuecues steams race ce tacnan cae aeenen aaa Tatenines 625 “ 
Survey No. 5,270, Allen township, Union county................-26- sessore A485 * 
WANT ens COnten reer teck dave te cece cee ece ee rela Sat tate reenter ae eT mR Bea aR 435 “ 
Milford: Center (ices sorb ese eS A ES AE EA OR ON AEN SPAT eean ales old * 
Soil and Timber.—The soil is one derived entirely from the Drift, and 
may be denominated in general a gravelly clay. It exhibits the well- 
known characteristics of fertility and endurance that mark all the Drift 
soils of north-western Ohio. It shows a very fair sprinkling of stones 
and bowlders, but in some places is very fine and heavy. It is only 
along the immediate river banks, on the bottom lands, that the sandy 
element prevails, and it is then confined to the alluvium. 
The trees of the county consist of the usual deciduous varieties. The 
following species were noted : 
Acer saccharinum—Sugar Ma] iiraies ch cea canlsue sce jensmeuta eaneucescteetuatamne Wang. 
Hacus Merny cineca Beech uacssconavserssenseclecocessusnecseseccteneersescentes Ait. 
Wilmaus PAmarericana— Elna (oli laity) Mesectosceecsssescicoseeceeccea cauenoasterses Willd. 
