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Arizona Gold & Silver Discovers 10 Metre Epithermal Quartz Vein Within 35.37 Metre Mineralized Quartz Vein Breccia at Philadelphia Project, Arizona
(TheNewswire) Vancouver, British Columbia – TheNewswir...
About this update from Arizona Gold & Silver Inc.
[{"type":"text","content":"Arizona Gold & Silver Discovers 10 Metre Epithermal Quartz Vein Within 35.37 Metre Mineralized Quartz Vein Breccia at Philadelphia Project, Arizona\n\n\n (TheNewswire)\n \n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n Vancouver, British\nColumbia –\n \n\n\n\n TheNewswire -\n \n\n\n\n August 14, 2025\n–\n \n\n\n\n Arizona Gold & Silver Inc.\n \n\n\n\n (TSXV: AZS)\n \n\n\n\n (\n \n\n\n\n OTCQB:AZASF\n \n\n\n\n ) announces further positive results from the\non-going core drilling program at the Philadelphia Project in Arizona.\nCore hole PC25-156 has intersected\n \n\n\n\n approximately 10 metres (“m”) of unbrecciated banded and massive\nvein quartz within a 35.7m intercept\n \n\n\n\n of quartz vein and quartz vein breccia.  This is the first\ntime a drill hole has been deep enough to intersect intact vein with\nthe classic epithermal vein textures typical of the high grade\ndeposits known in the nearby Oatman mining camp, 10 kms south of the\nproperty.  Furthermore the new drill intercept represents a 59%\nincrease in true thickness over drill hole PC25-155 that cut the zone\n60m up dip (see News Release dated August 6, 2025).\n \n\n\n\n\n\n\n\n\n Click Image To View Full Size\n \n\n\n\n\n Crenulation banding\nin yellow and brown quartz\n \n\n\n\n\n\n Greg Hahn, VP Exploration reports: “\n \n\n\n\n This drill hole confirms our geological\nmodelling.  My understanding of this low sulphidation  epithermal\nsystem predicted that with depth the system would be wider and\npotentially much higher grade as we penetrate the “boiling zone”\nof the system. We continue to see a decrease in bladed calcite and an\nincrease in quartz replacement of bladed calcite.\n \n\n\n\n\n\n “In addition, the interior of the unbrecciated\nvein displays classic epithermal textures including finely layered\nbanding of colloform layering and thin alternating compositional\nbanding. Yellow quartz dominates the upper part of the intercept and\ngreen, gray, and brown quartz dominate the lower portion of the vein\nintercept.  This is also a feature we have never witnessed in drill\ncore before.  In short we believe the vein system has the potential\nto rapidly open up into high-grade zones capable of delivering\nsubstantially increased grades.\n \n\...