. Outcrop in the valley floor on the western flank of the Reveille range. The iron-stained outcrop of quartz latite porphyry shows supergene leaching of sulfide rich sericite/illite alteration (potassium), stockworks of quartz veinlets with limonite after pyrite, and areas of local limonite cemented breccia. The alteration occurs in the northern part of the alteration halo to the core of the magnetic anomaly shown in Figure 1.
. Outcrop in the valley floor on the western flank of the Reveille range. The iron-stained outcrop of quartz latite porphyry shows supergene leaching of sulfide rich sericite/illite alteration (potassium), stockworks of quartz veinlets with limonite after pyrite, and areas of local limonite cemented breccia. The alteration occurs in the northern part of the alteration halo to the core of the magnetic anomaly shown in Figure 1.