Show the composite crystalline mass colm pricing t the lie granite gra tilte of if lone peak and little cottonwood cotton wood banyon lorile tit at tile the heade of joiy and little cottonwood onn conyous american fork and creek provo aud add ihla limrite tit the heads of jig big cottonwood fast conyon and snake creek creck with its extensions northeast through the park city district in the form I 1 of if dikea iii ia the dominant hictor in the greater g reater geological of tile the middle the ill uses ilges ant the relation leip of thase gratt intrusive have not yet been completely established in it a ahro broad id structural tience the bodice may bereza crded ua as i i fe mi ait composite t ju it tula light the 1 ing tf nf tilt lita normal structure iun if if ahe be I 1 wa Wn 4 atch aach and the I 1 narken sit SHI dip in ahio immediate b become e significant the Algo tildan on the west tho cambrian to ajic on oil the torl forth the llie on oil ulf east and atie Carbon to on oil tile the south deppin away from thita caun 1 me ale spen aeck to bo h the ot or 11 i att abc hil colit colithia hla dome this fritkin feature fea iture tuve cupl hy 1110 Ile e corded forded hy by the intrusive hitri jivu of thiv hetu eau th the e s anddie and llie elastics ly by thy the and of the adjacent coun ay 11 iy Y roc kand by the lie orail unusually complete series of typical contact Is conclusive aa to HH part this intrusive mass hila in ilie history ol of tile iho r floii J JM al boutwell in contributions to ei economic geology 1903 1902 the above JK Is not published because of its usefulness to the he wining frater olty but as hn of the efforts the US geological J rm survey is making to benefit uio the ruining mining industry BHO and Incident Iv ed educate licate t the he miner atud prope clor in the indications of mineral mine e ral aft after er rending the f foregoing ore going clipping ull all lint tile the prospector need do in order to find it a large larga brood of bonan bonanzas zag is to go out almost a anywhere tit in the hilla hill and wand hid find a with buu dip 11 and then dig in plain english park city and vicinity is a great domelike dome like eley elevation aaion composed of tilted beds of lime shale and aad quartzite with beds of gra granite tilie porphyry and other eruptive rocks which from the apex of the dome dip in all directions i |