Show thi PANAMA CANAL I 1 V II 11 concluded all ns vast and buo ouo already alluded to ri iho above captious cap tiou usually illy awakens interest nofa ony among contractors gunj angin acci s lait also which can nt bo at when we learn of uio geological which livo recently been made along tho panama canal and tho vari ous strain of earth and rock which have lccy so closely examined it has that very volcanic actions leavo place and si ns of submarine igno us action arc to be foaud m cicat variety granite enito anil m largo proportions aro als fo knolls eliat ex lend far baal aiuto alio isthmus linn alio llio banka of lie 0 i both bacs the alio llio has ao been aud that iii its bed inanc at well as callis cn llis also found at tho bottom of the river the rucks als havo a peculiar coloring which they aroi tho presence of peroxide of iron and the lodges near the central part of the abc said to havo been by submarine volcanic action timing tho tertiary gunod gray is y ii pablo station from which point also its ciny iks may to discover ld L d aliis ate contains ti achec of an Jiller ont sh arader aiom that bici is to lio round iu a radius of 25 miles rom ho fact that it contains no fossil ro auais lucli of ilia barru ain araugo is biado up t ind tiep formations at la techin here ii to bo fluid all 10 lo furu cr lamed locks bc dolo mintlo and othora chis las cular for it is at this p binl the heavy will bo oil pi lio aock of a canal is carried aiuto effect at the mouth of the rio grandc west of the of the city is a sti belt of sandstone containing no fossils and to belong to ho period it is upon a peninsula of for maciun thai llo city of panama is built while tho beautiful carro alo aubun aucun about muc distant stands upon a of tes t to ho geology of ui diio and has cost thousands of cullars 0 o b mado known alio isthmus and canal al r aro u staily and can lacarti i v bu as buch |