Peregrine Diamonds Ltd. Discovers Kimberlite At Chidliak, Baffin Island; Estimated Kimberlite Size: Six Hectares

July 23, 2008 PDF version
Mr. Brooke Clements, President and Mr. Eric Friedland, Chief Executive Officer of Peregrine Diamonds Ltd. (“Peregrine” or “the Company”) are pleased to report the discovery of a new kimberlite on the Chidliak property (“Chidliak”), Baffin Island, Nunavut, Canada. A kimberlite outcrop was discovered within a circular magnetic anomaly selected from an airborne geophysical survey that commenced on July 17, 2008. The anomaly has an estimated surface expression of six hectares. The outcrop was discovered in an area with high concentrations of kimberlite indicator minerals (“KIMs”). As reported in a news release on February 19, 2008, many of these indicator minerals have geochemical compositions that imply their kimberlite source contains diamonds. Chidliak is situated approximately 150 kilometres northeast of Iqaluit, capital of Nunavut. The proximity to the capital provides the Chidliak project with better infrastructure support than is available in other more remote regions of Nunavut.

A sample of approximately 200 kilograms collected from the kimberlite outcrop has been shipped to Saskatchewan Research Council Geoanalytical Laboratories for microdiamond recovery by caustic fusion. Results of the analyses are expected in August.

Mr. Peter Holmes, Peregrine’s Vice President, Exploration stated “This is a significant discovery in a brand new area; the nearest known kimberlites are approximately 700 kilometres to the east in Greenland. The fact that the discovery was made after only the fourth day of the airborne geophysical survey provides optimism that this is the first of many kimberlite discoveries to be made. We have now proven that there is good tonnage potential in this new district and the encouraging mineral chemistry on the property suggests that some of the kimberlites could be significantly diamondiferous.”

Brooke Clements, President of Peregrine stated “This discovery, coupled with the discovery of a new diamond district on the Nanuq property in the eastern Arctic region of Nunavut in July 2007, puts Peregrine in a unique position among junior diamond explorers in the world. Peregrine currently controls 100% interests in Nanuq and Chidliak and it is truly early days in the evaluation of the diamond potential of these two new districts. We look forward to continued encouraging results. The discoveries at Nanuq and Chidliak are the result of the hard work, dedication and technical expertise of the Peregrine staff and the efforts of many contractors.”

Description of Kimberlite Discovery and 2008 Chidliak Work Program
On July 17, 2008, Fugro Airborne Surveys Corporation initiated a 9,000 line kilometre heli-borne magnetic/electromagnetic survey flown at a 100 metre line spacing. The survey was designed to cover the most prominent KIM anomalies that have been identified on the property. The three distinct and well-defined KIM anomaly areas on Chidliak are situated 20 to 30 kilometres apart and are referred to as the Southern Anomaly, the Northern Anomaly and the Eastern Anomaly. Peregrine’s geophysicist, Maiko Sell is in the field interpreting the survey data on a real-time basis. On July 20, 2008, after the fourth day of surveying, a large circular magnetic anomaly, approximately 250 metres in diameter, was selected from the survey data for follow-up on the ground. Mr. Sell and Project Manager Hugo Grenon visited the anomaly and immediately discovered an outcrop of weathered kimberlite measuring three metres by five metres. Abundant kimberlite cobbles are present in the soil away from the outcrop within the boundaries of the anomaly. The kimberlite from the outcrop is described as being magmatic with abundant olivine macrocrysts, some up to 10 mm in size. Abundant mauve-colored pyrope garnet and chrome diopside are present and both ilmenite and chromite were tentatively identified. An altered peridotite xenolith was also observed.

Three maps, an image showing the encouraging garnet mineral chemistry from Chidliak, and several photographs of the kimberlite discovery are available