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Worthington Bell Property

May 8, 2007 press release (URSA Major Minerals initiates exploration program on nickel targets at Worthington Bell Property, Worthington Offset Dike, Sudbury area, Ontario)

In late 2006, URSA Major signed an option agreement to acquire a 100% interest in a nickel-copper exploration property on the Worthington offset dike, located in Lorne Township, 40 km west of Sudbury, Ontario. URSA Majors’ Worthington Bell option covers 1.2 kilometers of strike length of the Worthington offset dike. This dike extends for approximately 12 kilometers from the Sudbury Igneous Complex and is the host to several nickel-copper mines and deposits. Most notably, the Totten Mine Extension, owned by CVRD-Inco is located approximately 6 kilometers northeast of URSA’s property on the Worthington offset dike. The Totten Mine Extension contains approximately 10 million tonnes of 1.50% nickel, 2.0% copper and 4.8 grams per tonne of palladium and platinum.

 

The Worthington Bell property is located in an area of excellent infrastructure and is accessible from paved roads. The Worthington Bell property was previously known as the Mystery Offset Dike. The central portion of the dike is an inclusion-bearing quartz diorite that is similar to other mineralized offset dikes in the Sudbury district. Continuous zones of pyrrhotite, chalcopyrite and pentlandite mineralization are present on URSA Major’s Worthington offset dike property. On the property, shallow drilling by previous operators returned several mineralized intersections including a 2.62 meter intersection grading 1.26% nickel, 0.45% copper and 13.43 g/t platinum group metals plus gold. The approximately 102 ha (250 acre) patented mining property is being optioned for payments totaling $150,000 and 60,000 shares over a two year period, with a final payment of $187,500. URSA Major is required to complete a $500,000 exploration program within 2 years. The property is subject to a 2% NSR which is held by third parties.

At Worthington Bell, as announced on October 5, 2007, URSA Major completed 2 diamond drill holes to depths of 977 metres and 725 metres respectively. Both holes intersected the highly favourable rock fragment-bearing quartz diorite phase of the offset dike with disseminated sulphide mineralization and localized sulphide veins. The 2 holes completed by URSA Major, as well as holes drilled by previous operators, were probed with Lamontagne Geophysics Ltd.’s down hole UTEM system. This survey identified an EM conductor at a depth of approximately 500 meters and a potential EM conductor near below the deepest hole. The first conductor was drill tested and did not yield significant mineralization. The Company currently has plans to drill test the deeper anomaly.

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