Show A DISUIVKIU hlhIN HCel I leers of flooil aid lIon toeool alI Itcplli of Urrr a llunlrnl toil I lu Sjupftr limo A Allrtd of Katrvlow I one of Iho many oillrri who came Into llm JtyrunM rIfle bait week tayt Hint ar lo look at llu myilirlout rock rtctully liken from 1211th llran dont wrll Air AllroJ 1 report I lhal hc hmjuil flnlihtj a well ou Joieh Ilnigge I lace near Mill urn Iho depth booIng ISO feel 1 At Ul I fool been luntereda Iwo or Ihro foot layer of Ceinihlt and travel lu which wai lm > bedded a number of pluoei of llmbt of lr M tmall tllckv bilk etc coon of Iho lice i being four out lIeu luchet long Cud In a rooted condition but coomowoet tolldlfled ai Iliouth pairIng Ililoa pelrlMed or uatbou atati rim full oIIlh of Ihu Ktllronllnued Ibrough Ihuiinmiihiraoler uf ground which ovldoiuly had trot washed down Iroiu luo mountain choIr iliuliij mitt foci I All tlm ground un Ihu Wool tide of Htuilo valley I of llm tame char acluraud wella lu Ihli city lo llm dublIn 01 11KI feel havu nOt retolmd Ibe limit of llm waibed gravel atidilano bjuU etc cod cmoll Whet pruceii of nature na-ture inca created thu soIl directly uu durntalh many of our Htnpele townt to It I ouu of lho unexlalntd 1 1 1 rnyt bob the ttudy of nhlth will ptihir alwaytconlluuuto balllo k tucceitlul olnlluu rim molt Ituklb e theory It tbat lloodi have from time lo lime carried he4vyaiilerudipo > IU from tIne mountain moun-tain tiki and with Ibm whatever of plaul llfu may have burr wllliln In > 4th IhMehavu gradually 1111 up unlll 1 Jii Hi uf a hundred feet or moo Ito boo accululIJ |