Searchlight Resources Inc. announced the results of the October 2018 prospecting on the 100% owned Cameron Cobalt Project located in Brigstocke Township approximately 20 kilometers southwest of the town of Cobalt, Ontario and 120 kilometers north of North Bay, Ontario. In October 2018 a team of prospectors spent 4 days prospecting and sampling the 100% owned Cameron cobalt target area at the north end of Brigstocke Lake. The team located and mapped the locations of 3 historic shafts, 4 pits and 7 trenches, with waste dumps near the workings. The area was largely over grown, and it is likely more features exist. See map 1 below. A total of 40 grab samples were collected from the area, the majority from waste dumps and outcrop exposed in shafts and pits. The results included a number of anomalous samples with selected samples shown in the table 1 below. The results include 1.35% Co in sample R318936 and 0.63% Co, 0.864% Ni, 341 ppb Au and >2,000 ppm Bi in sample R318939. The Cameron claim block consists of 64 claim units covering an area of 1,024 hectares in Brigstocke Township approximately 20 kilometers southwest of Cobalt, Ontario and 120 kilometers north of North Bay, Ontario. See Map 2 below. The claims are 100% owned by Searchlight with no royalties. The Cameron claims cover the past exploration pits and shafts of the Cameron target developed in the 1950's which is now closed. A grab sample collected in 1987 from the historical Cameron pits and analyzed by the Ontario Geological Survey returned assay values of 2.26% Co and 1.7 g/t Au. (Data Source is file MDI31M05SW00021 from the Ontario Mineral Deposit Inventory). Geologically the Cameron Cobalt property is located within the Cobalt Embayment in the Southern Province of the Canadian Shield where Huronian Supergroup sedimentary rocks lay unconformably overly Archean basement rocks. Both the Huronian sediments and Archean rocks have been intruded by Proterozoic-aged Nipissing diabase occurring as both sills and dykes. The Cameron property claims covers the contact between the Proterzoic sediments of the Lorrain and Gowganda formation of the Huronian Supergroup and the intrusion of the Nipissing Diabase. The mineralization model for the property is the "Five Element Vein" style of mineralization (Co-Ag-Ni-Bi-As), which is characteristically found with 250m of the diabase contact. This is the characteristic cobalt silver mineralization found throughout the Cobalt and Silver Centre mining camps.