Show UTAH COAL the rh orant real alried or of emal eft conyon canyon am il 4 ansh vally eda tito formation or 01 country ot to the month of dry dj Sany ODi low 1 canyon silverado nd sou so lital lh mi is ill limestone this thin limestone lip appin pears everywhere forming strata nod and over lying tile ho lower radle th motion million is a series of ono on above aboto the other the iho place placa ot of which dips dip with the IOP ac abe hills wickwar a to lo the iho valley tho the course conno of thee taco 0 strata is i many ipacs interrupted ini and broken th thront routh lf tho the grot great upheaval through ilik seri of strata break dry canyon rest baal canyon and silver alo us as obaid cw formed through tho great courses upheavals and curvatures leaving tho the broken parts on either cither sido side ot of tho the channel each other to chow clearly which they occupied lvery v ono oco ti I 1 1 of 0 tho the gnat upheaval which tore rounder the 1 facing issing parts for if tho the fame mo thing appears on ot of every ean can yon the ibo boldly cropping out ot ion arc 1 ay opposite each other sod od oo on the bawo wo we see that it 11 these hills pressed pres sea back into their former position to a level with the val TI ey that bit all broken and dia lines would join equally to gether it will thus appear clearly UAL riuka TO rop ar 1 tho the country as aa tta horizontal P plop I 1 an was covered by a raws of over feet of limestone and when the bo hotho and terrible subterranean powers worked upwards choy broko broke kod find up heaved aho thoM bole bolo mass or of lim citone and at id for orned kited hilla boullosa bol llosa sod nd cady aoa ethey tt att hey bey appear rt it present the which ap appels peTs ion tho the cast slue iao of rush bush valley niona the mouths or of dry canyon E est east st OiD yoi aj silverado Silv orado different from ther the appears laureat more at tire held head of the cn can or more il it il is more compact my lime crowd all over v with ith I 1 Osle Path talent VOIDS and changes to well marl I 1 louail jQ tbt 1 l itono a bites find enla a gla pirus this la 16 formed kormod by marine manoo lai lacoco under this limestone appears the bealy 80 to ibs blakj rod below this the farill r accous shalo then a thin streak of fire clay I 1 bolow below ithmal the coal bej bed THIS COAL DED BED to tile lignite formation it is ia my cour b belief if that this coal will be round found good cooj anthracite the anthracite obar acter acler hao bad been laiti partog to the tha lignite by dykes of nt flo Oa Kinio material many ol of which occur deem oust of the coil coal crop P dingi 94 cabout feet cast cal of abo coal droppings crop cropp pings logs this coal is iii only opened oo on one place by an n incline about eig eighty aty fe feat roq and by it bat ninety feet deep it t wes firt by a mormon mornion former farmer about eight years ago through Tb to cho weather for eight year tho the coal haq lia or of course in its iti quality it is very probable pio bible that the eruptive ernp live r bavo anil and broken bialon through he abo anti and that large graor pro probably bibly and cite tho coil bas a gravity of 1 16 aso la ila burning it given a blue llimo game under intense lost boat I 1 ahe ht outcrops are very much moch broken and the iho coal it for a length inside ot of over fifty feet tabt greatly mixed with clay loj find shale too tuo bed has a thickness or of of over twenty feet no oiher doyel of any 07 malarial have this coil coal fiali which contemn severed thousand scree acres beyond beland the of coal IQ 10 ft 6 north and south lioe line of over four miles As A the ibo formation on the lie west vest tide kido of bush valley is the iho panic fame as 89 on the east side with the iho difference that the stratum dips aipa eastwards it is u my koplo lon ion that lh wo we lieve boro bore a coal burn bum which lias bag its ila point in J in or near the iha CENTER of RUSH VALLEY TAIL Zy the dips in an anglo of thir ty tafito civo degrees underlying tho the coil coal is old red sanda si bilious thal a and dark abide alternating with gray tand sandstone stone I 1 beveral species of from froia the tauda toro the sandstone la Is hard cootie coarse grained a ad h haitt cay bedded bcd dej it forms form in ia pieces a well T ridge running io in an amot direct cortti east sod bouth west lie aioo the great upheaval las ilia bro brought light to abo case of the coll crops in 61 lorian loria rock which boo fully foot feet below EO ahat the vertical displacements must mast be over lent below the ail arten rock rockie is metamorphosed east ortho of tho tho the aldge is not well wall donned defined as il the pebbles and nd red clay form the surface EAST or OF ACCE Sli the slopes ol of the hills bius in ia which tho the appear are re theold thickly y covered with yo yellow low and red pine piao and cedar bra beir all pieces we of ouy clay AO coes coby aby wagon boals and the utah railroad rail roid is ia rapidly approach lag fog completion the boil is il light and aad not dot suitable for except hero rod and thoro there a very limited patch in the ibo crock creek bottoms bol toan TUB CLIMATE I 1 is il healthy lit at every a ason aon the snow falls lia in I 1 tho he winter very light the mines at al tho the head bead of tho the canyons ire fire shipping out tho cho liter d day y wi SALT LARE LAKE cur CITY api april ia 1616 I 1 |