Camp Bell

System Type:

Epithermal, high grade, banded, quartz veining, with scattered breccias and stockwork veining.

Strike-Length:

Camp Bell covers an area of 1,000 x 200 meters predominantly covered with a thin veneer of colluvium (gravel).

Resource:

None at this time.

Location:

The Camp Bell target is located immediately north of the Lost World target along the Gold Springs Wash on the Nevada side of the Gold Springs property.

Drilling:

None at this time.

Geophysics:

The Camp Bell target is located along a large +5-kilometre-long, north-south trending high resistivity anomaly identified with the airborne ZTEM geophysical survey, which encompassess the Camp Bell, Thor, and North Jennie target areas.

Geology:

The Camp Bell target is completely covered by colluvium with mineralized floats scattered throughout the 1,000 m x 200 m target area. Mineralized float consists of veins, breccia and stockwork some of which returned high-grade sample results >10 g/t gold. The target is defined by the Gold Springs Wash structural corridor which has a strike length of over 7 kilometres and runs north-south to north-east through the Camp Bell target area. This structural corridor is known to host mineralization at other target areas on the property.

Structural Geology:

The Camp Bell target is hosted along the Gold Springs Wash structural corridor. The corridor has a strike length of over 7 kilometers and runs north-south to north-east through the Camp Bell target. At the northern end of the Camp Bell target area the Gold Springs fault system jogs to the north-east for 3 kilometres before continuing north through the Juniper target where it is known to host mineralization.

Historical Mining:

There are few historic pits within the area. One USGS report from Perry 1976 describes a collapsed adit in the area. The Company attempted to uncover this at the described location, but it was never found.

Geochemistry:

Many high-grade samples have been collected by the Company from float consisting of veins, breccia and stockwork. These gold-barring samples range up to 145.68 g/t gold with 148.2 g/t silver and extend over an area of 1,000 x 200 meters. Recent surface sampling has produced the following results returning values greater than the resource cut-off grade of 0.25 g/t Au. Previous sample results obtained by the Company area also presented below:

Table: Rock Chip Sampling Results from the Camp Bell target

SAMPLE	Sample Type	Description	Au g/t	Ag g/t
33161	Float	Silicified rhyolite with bladed quartz	145.68	148.2
33182	Float	Bladed quartz-calcite-adularia	6.84	23.4
33183	Float	Banded, bladed quartz vein	0.67	7.9
33187	Float	Vuggy bladed quartz-adularia vein	12.73	75.4
33189	Float	Vuggy quartz vein	1.55	37.9
33228	Float	Vuggy quartz-adularia vein	0.66	45.5
33229	Float	Vuggy, bladed quartz-adularia vein	1.00	38.5
33230	Float	Brecciated andesite with quartz matrix	0.31	2.0
33232	Float	Banded quartz vein	5.12	70.5
33233	Float	Quartz-adularia vein	3.54	68.5
33235	Float	Andesite with quartz veining	0.43	40.5
33236	Float	Vuggy, bladed quartz-adularia vein	1.00	27.0
33237	Dump	Bladed quartz-adularia vein	3.30	111.0
33240	Float	Brecciated andesite with stockwork quartz veining	1.38	33.5
33244	Float	Brecciated andesite with quartz veining	17.45	165.1
33245	Float	Bladed quartz-calcite vein	6.74	40.5
33361	Float	Colloform quartz vein	0.55	14.7
224452	Float	Hydrothermal breccia with bladed textures	0.26	22.7
224453	Float	Banded quartz vein	2.24	65.7
224456	Float	Hydrothermal breccia with angular clay/sericite altered andesite clasts	0.41	<0.5
224457	Float	Silicified hydrothermal breccia in andesite host rock	1.07	95.0