Show INTERESTING STUDY OF GOLDFIELD FORMATION Rich Ore Shoots Are Segregations Segregations Segre Segre- gatons Within Masses of Quartz v BIG LODES CONTINUOUS Developments Show Much Milling Miling Ore Riches Ore Riches at Great Depth I S Former r General Manager Finch of the Consolidated Mines company com cons pany puny In making a summary of tho the ore on- bodies as they prevail at on this compan company's com corn pan pans pany's ground ss says In tho the Mohawk wk No 0 2 the bonanza ores have been heen found from Crom time the south endline northward for fora foru a u distance of nearl nearly 00 feet Cel alon along the claim and complete development promises to show their connection with Ih similar bodies recently discovered red In Inthe II the tho Kuus Kalfus lease GOO COO feet away In fact it i now begins to appear that tho the series of or remarkably rich ore oro bodies lodies In Ih the Combination January Combination Combi nation Fraction Mohawk Jumbo and andRed Red Het Top 01 will wi soon be definitely correlated corre corre- hated as an articulated system m of or veins due to the same causes and together forming a 8 stem Strict Strictly speaking the time bonanza ore are shoots are only extraordinarily rich segregations within greater masses o of 01 quartz deposits which range from a few feet to mol more than feet in hi width commonly called caled ledges Millions of cubic feel feet of such material have been developed in the tho breccia zones which er e everywhere where contain gold old values Such bodies are tho time great veins of and 1101 when hen company milling Is fully instituted a great grat portion of these masses will wi ho milled to good gool goot profit profit Such Ruch Is their extent that clint u a supply I of mill mil ore oie is assured for a period of or many years ars after the rich ores hn have ha been extracted Uninterrupted The un underground developments and geological eolo study of oC the past year ba says s 's a statement issued In behalf bohal of th Ow company have ha only served sel to render ron ren tel der more definite the conception of or these veins ns as above t expressed and to articulate their parts still sti more clOsely as great grent lodes mulo up LIP or of im immense 11 mi- mense elongated masses of oC qua or material in breccia fissures of great width surrounding lar large e irregular lar har horses of C porphyry yet Cl nowhere so far Car as ns developed d Interrupted In their 1 continuity as a I fissure system I The Mohawk anil the Jumbo lotie JOllo 8 system now nr to c und nt become distinct nn on In tl-lr tl strikes but lint thin tho r unite northward In th the tho Mohawk No 2 nn l Top claims r 11 I p nn Regarding t rf the IUS bodies a ns ax the thu member antI and the tile main Mohawk Mohawk Mo Mo- 10 hawk quartz quart mass us its the hanging wall wail wal I member there is on the Mohawk wk No I claim a great lode fully COO feet Ceol Wile wide wite uniform In dip on both bolh walls wals and I regular In form and hc be- be iween tween the Mohawk and Ish Ishi Ih shaft continuously vein eln material from wall wal to wall wal This body boily Is ia all al eolo l- l ally cally cly eln eln material but hul not u of f course commercial re It I is how however hower er the llio class of or material In iii which development may may at al an any point discover Ir valuable ore bodies The Th new west body In the tho Hell fled Top and the lon tr known bodies in th time the theold old ihl workings stand in the Lime tl same relation as time the Mohawk hotl bodies also alyo the Combination Combi nation laton January and l'- l' February quartz holIes bodies mo may ho bo rl regarded ar as the southward southward south south- ward continuation of the time same lode None one of tile the quartz bodies holies on the hanIng hanging liming hang ing hug or oi sll side or 01 the Iho connecting masses be between could he be isolated or defined for any great rat distance as separate separate sepa sepa- rate I vein In n deposits Taken together they form a system of fissures anti and aOI a n system system tem tern of vein eln deposits due tue to the time same saro causes acting OVer time the same geological periods Tho The low grade distributed values for great widths In ih the quartz bo bodies les also the time ramifying Internal bands of high grade and the larger bonanza sc segregations segregations seg seg- as 07 O in time the Mohawk are arc ore the result of continuously operating operating ralIn ral- ral In ing and Int Intensely active solutions which naturally affected the time st precipitation in the thc more open parts of oC the thc lode lote On account of or thc re recent recent recent re- re cent deposition of thc Lime lodes loties erosion has b been cn ani only moderate II It J Is probable that time outcrops have not been heen re reduced reduced re- re re-I re inert than O feet feel below their I original position Only a relative relatively small part of the ore or deposits have therefore been removed and dissipated dissipated- over the plains surrounding the ills dis Ils- Ils t A All ll 1 these considerations are arc e evidence evi ovi- i- i dence that hint mining la may be lie hI pursued to great ret depths and ami this I is 61 also 0 assured I h by the Iho visible promise shown In lh time the deepest developments do Sufficient underground underground unter un un- un- un ter round work has been heon accomplished already to make male It positive e that thai the district is essentially a deep mining section I |