The 1658 ha Davies Property is located approximately 146 km northwest of Mackenzie and 60 km north-northwest of the community of Manson Creek, along the south side of the Osilinka River valley. The property is prospecive for Mississippi Valley Type ("MVT") critical-metal deposition and is accessible via a network of mainline logging roads from either Mackenzie or Fort St. James BC. while secondary FSR’s provide access to the mineral showings themselves.

The claims are 100% owned by Eagle Plains with no underlying royalties or encumbrances.

The Donna Property is located in south central British Columbia approximately 63 km east of Vernon and is accessed by a network of well-maintained logging roads.  The 12,364 ha project was acquired in 2016 by way of agreement with ALX Uranium Corp. and is 100% controlled by Eagle Plains with an underlying 2% NSR.  In July 2020, Eagle Plains added significantly to the gold exploration potential of the property by purchasing 4 crown grants located in the NW portion of the property that are host to the past producing St. Paul and Morgan mines.

The Elsiar Property is located in western British Columbia  approximately 45 kms northwest of Terrace. The 558ha project is 100% controlled by Eagle Plains with an underlying 2% NSR held by Eagle Royalties containing a 1% buy-back clause. The claims were acquired in 2003 based on regional research and a similar geologic environment as the Kalum property, 10 km to the south. The project area is accessed by a network of logging roads.

The 11,287 ha Findlay Property is located approximately 30 km north of the city of Kimberley in south-east B.C. The claims were staked in anticipation of an airborne geophysical survey conducted in the fall of 1995 by the Geological Survey of Canada (GSC), and the British Columbia Geological Survey (BCGS).

Geology

The Mount Haskins property lies within the northern extension of the Omineca lithotectonic domain, underlain by the sedimentary Cassiar Platform of the Cariboo/Cassiar terrane, which has been intruded by Eocene granitic stocks. The platform is made up of the Cambrian-Ordivician Kechika Group and Lower Cambrian Atan Group of clastic sediments. Regional structural trends of folding and faulting are dominantly northwesterly, with local secondary northeast-trending faulting.