Twilite Gold Property
The Twi-lite property, lies along the western margin of the Botwood Basin, central Newfoundland, It is situated approximately 30 kms southwest of the Moosehead gold prospects and has similar potential for epithermal gold mineralization.

The two major structural elements within the survey area are NE-NNE and NW faults. These two directions are well represented within the Discovery showing and have been noted as being associated with gold mineralization. The regional depth calculations, carried out using the Source Parameter Imaging Technique indicates that two major “graben” type structures may occur within the area; one striking NW-SE along the Victoria Lake-Badger Group overlap and the other along the Badger Group-Botwood Group NE striking fault contact. Through the central portion of the area, immediately east of the Discovery showing, major N-S faults are evident on the processed magnetic maps. At the southern end these N-S structures control eastern boundary of the Victoria Lake Group and in the north they appear to form the eastern edge of the Lemotte’s Ridge Sequence.

Some results to date:
The Discovery Prospect: Zone of quartz veining and associated silicification, high of 202 g/t Au (Visible Gold).
The Spring Pit prospect: bedded pyrite/mafic fault gouge (high of 14.9 g/t).
The 320 Vein: zone of quartz veining and quartz breccias (high of 16.6 g/t).
The Paddy’s Pitt prospect: silicified and brecciated siltstone (high of 23.80 g/t).

Twilite- Exploration Results- Click Here