Blind Creek Resources Ltd., Annual General Meeting, Nov 26, 2012., at 10:00 Pacific Daylight. Location: 675 West Hastings Street. Agenda: To receive the audited financial statements of the company for the year ended November 30, 2011 together with the auditor's report on those statements; to set the number of directors for the ensuing year at three; to elect directors of the company for the ensuing year; to re-appoint BDO Canada LLP, Chartered Accountants as auditors for the company and to authorize the directors of the company to fix the auditor's remuneration; to approve stock option plan for the company; and to transact such other business as may properly come before the meeting and any adjournment thereof.

Blind Creek Resources Ltd. reported that the Blind Creek exploration team is finding visible mineralization on Table Mountain in the Atlin-Tagish region, 15-20 km Northwest of the historic Atlin Gold Camp in Northwest British Columbia, and 43 kilometres south of the Yukon border. Since 1910 and the initiation of Minfiles, Table Mountain records show almost no mineral exploration activity. Scattered over an area of 4 square kilometres, the Blind Creek team has now found a zone of individual gossans in addition to two undocumented adits within very steep cliff faces and gullies on Table Mountain. The first adit intersects a composite quartz vein system 50 cm wide at approximately 350 metres above Graham Inlet, and the second adit is located in a gossan zone approximately 1,000 metres to the northeast. These adits are estimated at 110 years old. The first adit intersects an east-west striking composite quartz vein dipping steeply north into Table Mountain, and is part of a geochemical anomaly found in 2011 by the Blind Creek team. This composite quartz vein is visible for 10 metres before covered either by talus at one end and tapering out at the other end; visible mineralization consists of strongly pervasive malachite, associated azurite, strongly disseminated galena, disseminated chalcopyrite and a lesser mineral identified as sphalerite. Down slope towards Graham Inlet trains of similar mineralized float rock are traceable for 350 metres. The second adit hosts lesser malachite staining. Generally, but not always, precious metals are associated with similar galena-sphalerite-chalcopyrite-malachite-azurite mineralization in the Atlin-Tagish Lake region. Eighty soil samples, forty-two mineralized rock samples, and two pan concentrate samples from Table Mountain will be delivered to a Whitehorse prep-laboratory by 16 July. Elsewhere in the Atlin camp, results from a Blind Creek magnetometer survey initiated in April 2012, suggest previous drilled gold bearing geology on Dominion Creek, but it has not been traced on Blind Creek's property and is as yet undrilled on the Company's tenures. This magnetometer survey will be followed-up this fall and winter to enhance future Blind Creek drilling target selection. Dominion Creek is adjacent and leads into Spruce Creek, historically one of the richest placer creeks in British Columbia, therefore Dominion Creek geology has long been suspect as a potential source to Spruce Creek gold placers. Within the Yukon Carlin Trend and Keno Silver projects near Mayo, Yukon, analytical results from June 2012 submitted samples have not been encouraging. Analyses from Blende-Ocelot mineralized chalcopyrite rock samples in addition to soil samples collected in June 2012 are still pending.

Blind Creek Resources Ltd. reported that it is in the final stages of completing stage 1 of its 2012 field program in the Mayo Mining District, Yukon. As previously reported, Blind Creek crews in June 2011 found mineralized gossan rock float hosting malachite - azurite as well traces of copper sulphides, within the Blende-Ocelot claim block which is adjacent to the ATAC claim block, Mayo Mining District, Yukon. Two rock float samples delivered to the laboratory then, returned 287 ppm and 468 ppm silver, 0.569 ppm and 0.969 ppm gold, 4380 ppm and 8700 ppm copper, as well as 247 and 506 ppm arsenic. Between 12th-19th June 2012 similar but more persistent copper sulphide-carbonate mineralization has been identified within a 5 metre wide north-south shear zone traceable over 1000 metres. These copper sulphides are interpreted to be skarn related, hosted within a Triassic (or older) complex of sills, dikes and intrusions of variable diorite composition.