District Copper Corp. announced the results and interpretation of a 19.3km deep penetrating Induced Polarization survey on its Copper Keg porphyry copper project located approximately 55 kms west of Kamloops British Columbia. The property covers approximately 3,272 ha and is located at the north end of the Guichon Creek batholith.

Highlights of the program are: Highlights: Two positive chargeability anomalies have been located. The large anomaly is northwest trending, open ended, and measures 2,500m long by 1000m wide, hosted in Nicola Volcanics and the Guichon intrusive located on either side of the Barnes Creek Fault. The second positive anomaly is hosted in the Guichon Intrusive at the south end of the project, measures at least 1,500m long by 750m wide, and is open to the west.

The large chargeability anomaly exhibits a strong spatial correlation to the large area of intense argillic alteration and is interpreted to extend to the southeast under the Kamloops Group. The chargeability anomalies correlated with the two areas of coincident sporadic copper mineralization and intense argillic alteration defined by historical rock sampling programs. The Company also reported that field data collection for the recently announced airborne magnetometer survey over the entire property has now been completed by Precision GeoSurveys of Langley, BC. Interpretation of the data, including a Magnetic Vector Inversion, is underway.

The IP survey consisted of four, 500m spaced, north-south oriented lines covering 19.3 kms, contracted to Quantec Geoscience who used their Titan 24 system. The survey was completed using the dipole-pole-dipole configuration utilizing a 100 m dipole spacing. The objective of the survey was to map the chargeability and resistivity signature associated with the two areas of intense argillic alteration and associated sporadic copper mineralization.

The larger of the two chargeability anomalies is coincides with a large area of altered Nicola Volcanics and Guichon intrusives located along the trace of the Barnes Creek Fault. The chargeability signatures suggest that the Barnes Creek Fault and the intense argillic alteration could extend to the southeast under the Kamloops Group.