Show the wyno group during the latter part of last itt week and first of this week reuben dewitt his son john andt and mr fugitt have been work working ing on the wyno group near bear oak springs a couple of miles or so south of tenmile tensile creek the ore is principally gold and occurs in bl black ackiron iron oxide the matrix of which is slightly iron stained quartz on the wyno vein a shaft is down about ISO feet and while the vein vein is small at the surface it holds its width to bottom of shaft where there are about 12 inches of bf ore that samples ten dollars per ton in gold there are other veins one of which can be traced a distance of feet and is a large vein carrying good milling val values lues it is rumored that a prospective deal is pending feromone Fr omone of our townsmen who recently spent several days looking over the oak springs locality it is learned tl th at t keo geologically logically the region is singularly interest interesting ingi our informant is of the I 1 opinion ion that the maze of eruptive foothills mark tile the trend of the sevier pault fault ian on jl its course to the t that they are ire ot of recent origin our informant says adys that the eruptive material of the hills is charged with a radish brown shale hale and occasionally quartzite qu artrite trite bowld ers highly altered are present in ole ia erupt ives which are generally iron stained and that it proves that volcanic forces after afir the building of the main range forced the eruptive material up through ahe atan other he found a dike of peculiar peculia r material in bottom of a wash and th that at the dyke disappears under the erupt ives on each side of the wash these facts said our informant prove beyond question that quartzite and shale or limestone perhaps both occupy bedded fissured fissure dand and faulted positions beneath the eruptive hills and at no no great distance beneath the vein droppings crop pings it does not appear to be a poor mans country said our informant but if men with ample means will undertake the development of that region there is not the slightest doubt that great beds and veins of the precious metals will be found in the underlying sediment laries bartz ite limestone and shale |