Laserfiche WebLink
1' <br />- The preserrE main corking level of this group is through the i9lkado tiuvnel. <br />r <br />. fa tumnel is owr(ed bg cams parties and has been driven into the mountain a dir- <br />f; <br />anee of 1S?5 !'bet. The objective pout area the Tomboy vein, new supposed to bo <br />t a fear hundred Yeet beyorxl the breast of the tunnel. The strength of this <br />ein together with the general strike as demonstrated in TomboyWBalaont-}fountain <br />feY claims, Fund the topography of the country would tend to strengthen t}nia be- <br />ief. This territory on surface where this vein is supposed to pees thrcugh is <br />overall deeply with heavy elide. In this elide rock however, cues be found pieosa <br />f quartz or float that aprear the came as that found in elide rock belrns the <br />Toppings of the Tomboy-Bslaront. Rbova a aarLain line none oP this float could <br />fo•.1ad. .,ear the northern part of the ridge embracing Tfiddia Darin amineral- <br />zed zone or gap, supposed to be the point this vein passed through, !s quite <br />ticeable+ All things considered it appears more than probablo that thin vain <br />oea extend through thls aectlon+ Its value, if it exists, 1a problematical until <br />c+.ually irnterseeted and exploited. Thip tsYnnal enters cover at a point where <br />he Cross vain cute through the south-vest side line of the Japan ;to. 2. <br />The first vein enevurnterod in the property described is the iThala~ of <br />hich rrentioa has already been made. This vein has been apenad from surface and <br />3 cut in the upper workings of shat is knows as the Climax tunnel, nbout 1c~0 <br />set south-west of the Ifikado tunnel. Here a drift has boon driven on the vein <br />bout Ski fast long. This drift diaclosea a quartz vain from ?, to 6 inches wide, <br />ryina; golds soma of which, in choice speclraens, fs observable ir. free for[n. <br />The next vair_ encountered, and which is cut by the ffikzdo and Climax <br />m,alsn la the Sapan~ vhieh has been quite extensively developed. The outcrop <br />-. f this vain on surface is observable in many places and rxxy ba traced the full <br />ength at several olaima. 67}nere the vain is cut by tumtel a <br />fi <br />r <br />!~ <br />`: <br />i1 <br />3 <br />,, <br />t <br />i,', <br />i <br />,r. <br />i <br /> <br />i <br />s; ';i <br />i <br />;, <br />Sa <br />i' <br />4,. <br />.- <br />it <br />