Uchi Belt Properties

Map of Uchi District Area Play Gold Exploration Project – Locations: North Western Ontario, Canada – Cross River Ventures

Cross River controls four early-stage properties within the Archean Uchi Greenstone Belt, located approximately 90km east of Red Lake. The claim groups from north to south are Shabu (gold), Dent-Jackson (gold and base metal); Maskootch (gold and base metal), and Ear Falls (gold).


The Shabu Lake claim block covers a narrow wedge of greenstone located along the northwest margin of the Uchi Belt.  The Ontario Mineral Database has four mineral occurrences on the claim block with exploration work ranging from the late 1930’s to 1980’s. The most significant occurrence is called Shabu (MDI 52N07SW 0002) and consists of a narrow (10-15cm wide) quartz vein crosscutting weakly altered gabbro and diorite.  A total of 6 drill holes were completed and each intersected a pyrite and chalcopyrite bearing (up to 2% copper) zone with hematite and epidote alteration. The best intersection was 1.065 ounce/ton gold over 15cm.  Despite the narrow nature of this zone, the high-grade values warrant a detailed evaluation and follow-up.  The Cross River technical team intends to undertake a structural desktop study of the claim block to aid with target generation.


The Maskootch claim block occurs along the southeastern margin of the Uchi Belt, approximately 100km east of Red Lake. The claims are underlain by a series of mafic to felsic volcanic rocks with narrow intervals of banded iron formation. Previous exploration has identified extensive alteration suggesting a high potential for base metal sulphide mineralization (VMS) as well as lode gold deposits. Two historical mineral occurrences are known on the property: Maskootch (copper) and Wenesaga (gold). The Maskootch copper occurrence has reported trench samples of 0.43% Cu over 1m from sampling completed in 1984 (MDI 52K16NW 00014). Subsequent diamond. drilling of airborne electromagnetic conductors in 2009 yielded weakly anomalous copper and gold from the sulphidic iron formation. The Wenesaga Road gold prospect was trenched in the late 1980’s in order to follow up reports of high-grade surface gold, however no assays are available (MDI 52K16NW 00006). A single drill hole is reported in the area from 1990 that yielded weakly anomalous gold values.

The technical content disclosed in this website was reviewed and approved by Dr. Rob Carpenter, P.Geo., Ph.D., a Qualified Person as defined under National Instrument 43-101.  Dr. Carpenter is independent of the Company.

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