CHARAY GOLD PROPERTY, SINALOA, MEXICO

LOW SULPHIDATION GOLD PROPERTY

The Charay Property (also known as “La Mina Del Padre”) is comprised of three concessions totaling 380 hectares, and is located in northern Sinaloa, Mexico, approximately one hour by road from the city of Los Mochis.

EXPLORATION TO DATE

Limited exploration has been conducted on the structure.
In 1996 Empresa Cambior collected 80 samples on surface from a zone of silicification on the south side of the eastern known extent of the vein. Several samples contained anomalous amounts of gold, up to 5g/T. In 1999 Empresa International Northair collected 21 surface chips on the property.

In 2005, Vane Minerals Group drilled 27 shallow holes on the Property, totalling 1,576 meters. Eight drill holes targeted large zones of intense alteration in search of large-tonnage, low-grade disseminated mineralization. Nineteen drill holes targeted and intersected mineralized quartz vein/structure along as strike length of approximately 240 meters.

Vane Minerals estimated an approximate 37,000 tonnes of material along the 240 meter drill tested strike length of the structure across a width of 1.14 meters, and to a depth of 50 meters, which averaged 18.75 g/T Au and 120.15 g/T Ag. The mineralized structure remains open along strike with mineralization appearing to increase with depth. Due diligence on the property has consisted of re-logging and quarter sampling of the 2005 drill core. The new samples were assayed by Chemex Laboratories located in Vancouver, BC, Canada. There was an excellent correlation with previously reported results, however, the previous data has not been sufficiently verified by a qualified person under National Instrument 43-101 to be classified as a current resource estimate. Journey is not treating the estimate as a current resource estimate and therefore, this data should not be relied upon.




The Charay Property is accessible by road, with most of the property covered with thin overburden. A 100m X 25m soil geochemistry grid is planned to define the surface trace of the El Padre vein and try and locate parallel structures. The existing vein is open to the east and to depth, it has the potential to be larger resource than is currently defined.
Journey is in the process of mobilizing the company owned drill rig to the property to complete a Phase 1 drill program designed to test the mineralized depth and extension of the known structure.