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[Penny Roger$]

$PGVI ~ The Phil property is located within the southeastern portion of the Selwyn Basin, a thick sequence of shelf and off-shelf sedimentary and lesser volcanic strata deposited along the southern margin of the Ancient North American Platform. Strata were deposited from the late Proterozoic to early Triassic, and underlie much of central and southeastern Yukon north of the Tintina Trench. The property itself is located within a package of Cambro-Ordovician Rabbitkettle Formation limestone and shale overlying an extensive package of Neoproterozoic to Lower Cambrian Hyland Group sediments. The eastern margin of a package of Neoproterozoic to Lower Cambrian Vampire Formation clastic sediments underlies the western margin of the property.


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