Compliance Energy Corp. reported the assay results of 9 diamond drill holes from the company's drilling program at the Camp Lake project, approximately 25 kilometres west of Campbell River, British Columbia. Highlights of the 2011 drilling program includes hole 11-CL-08, which returned an 8.9 metre (29 foot) intercept of 58.36% magnetic iron, and 1151 ppm (0.1151%) Cu and hole 11-CL-06, which returned an 8.4 metre (26 foot) intercept of 41.35 % magnetic iron, 695 ppm (0.0695%) Cu (copper) and 522 ppm (0.0522%) Zn (Zinc). During 2011, company completed 9 holes totaling 644 metres of diamond drilling testing the Spur Magnetite and Junction Copper showings. Company also completed prospecting, geological mapping and soil and rock geochemistry on the Camp Lake property including 466 soil and 20 rock samples. Much of the property remains unexplored. Prospecting and grid-based geochemistry work completed at Camp Lake in 2011 included the discovery of two new copper-silver showings in outcrop, and three new areas of multi-element soil geochemistry anomalies. One of the soil anomaly areas contains elevated values in silver, arsenic, cobalt, copper and zinc over a 250 metre diameter area, similar in size and geochemical signature to the Spur Magnetite target. The two other soil anomaly areas contain elevated values of silver, copper, molybdenum and/or zinc. Possible bedrock sources of these soil anomalies have yet to be located. The Camp Lake Property covers 3,442 hectares and is situated on the flank of an intense circular aeromagnetic high measuring 10 kilometres in diameter. This aeromagnetic high is centered on a granodiorite stock of the Jurassic Island Intrusive Suite, which intrudes a NW-SE trending graben structure containing a preserved, gently NE-dipping Triassic to Cretaceous volcano-sedimentary sequence, which includes the Triassic Quatsino limestone unit. Along the western side of the intrusive stock sits a pendant of Jurassic Bonanza volcanics, underlain by Triassic Quatsino limestones. Dikes and sills of the Eocene Mount Washington Intrusive Suite may also be present. This geological setting is considered ideal for porphyry copper-molybdenum and related polymetallic magnetite-copper-zinc skarn mineralization on Vancouver Island. The Spur Magnetite Zone is exposed, mapped and sampled in outcrop and delineated by diamond drilling over an area of 250 metres by 75 metres, and is open both to the south and the east. The Zone appears to be gently south dipping, is partially eroded and ranges in thickness from approximately 2 to 9 metres. Mineralization is described as a black, yellow and brown, highly magnetic and zoned magnetite-copper-zinc skarn containing disseminated to massive magnetite, with variable garnetite, actinolite, quartz-calcite stringers, and sulphide stringers and clusters mainly pyrite, pyrrhotite, chalcopyrite and sphalerite. All core samples, along with geochemical blanks and standards, as well as all rock and soil samples taken in 2011 from the Camp Lake Property were transported in batches by bonded transport carriers from Campbell River, BC or Nanaimo, BC to Inspectorate Mining and Exploration Service Ltd.'s facility in Richmond, BC where they were received, prepared, and analyzed using their 50-4A-UT ICP multi-element and Au-1AT-AA gold methods. All samples with greater than 10% iron (Fe) from ICP analyses were re-analyzed by Inspectorate using the Davis Tube method to determine magnetic iron %.