MALARTIC (H)

Location: North Western Québec, 8 km north east of Malartic in Cadillac Township Project Access: Gravel road from hyway 117 SNRC: 32D / 01 Land Description: 8 Mining claims 320 hectares Commodity: Gold Area Deposits: Black Cliff, Malartic Hygrade, Camflo Partners: Breakwater Resources inc & Twin Mining Resources Option: Option to acquire 51% interest.

REGIONAL GEOLOGY
The property is situated on the northern limb of the Malartic Syncline which is part of the Abitibi Orogenic Belt of the Superior Province. The Malartic "H" property hosts, from north to south, the upper 2 formations of the Malartic Group namely the Dubuisson Formation and the Jacola Formation. Regionally, these geological units strike NW-SE and dip vertically to sub-vertically. The Malartic Syncline structure was subsequently re-folded by EW (P2) deformation in a large "Z" fold structure occurring along the contact between the Malartic Group and the Kewagama Group. This structure hosts several gold deposits in the area northeast of the town of Malartic including the Black Cliff deposit (130,000 tonnes grading 8.23 g/t Au, 1987), the Malartic Hygrade Mine and the Camflo Mine.

Associated with the major fold structures are several secondary structural features also directly related to gold mineralization. The 2 most significant are the Norbenite/Norlartic shear zone which hosts the Kierens Zone (780,200 tonnes 7.54 g Au/t, 1989) and the Norlartic Mine and the Marbane Shear Zone which hosts the Marbane Mine and the Gold Hawk Mine. Another important setting for gold deposits is structurally controlled, chimney-like intrusive body, best exemplified by the Camflo Mine which to January 1989 had reached total production of 9,034,00 tonnes grading 6.4 g Au/t.

REGIONAL GEOLOGY
The property is situated on the northern limb of the Malartic Syncline which is part of the Abitibi Orogenic Belt of the Superior Province. The Malartic "H" property hosts, from north to south, the upper 2 formations of the Malartic Group namely the Dubuisson Formation and the Jacola Formation. Regionally, these geological units strike NW-SE and dip vertically to sub-vertically. The Malartic Syncline structure was subsequently re-folded by EW (P2) deformation in a large "Z" fold structure occurring along the contact between the Malartic Group and the Kewagama Group. This structure hosts several gold deposits in the area northeast of the town of Malartic including the Black Cliff deposit (130,000 tonnes grading 8.23 g/t Au, 1987), the Malartic Hygrade Mine and the Camflo Mine.

Associated with the major fold structures are several secondary structural features also directly related to gold mineralization. The 2 most significant are the Norbenite/Norlartic shear zone which hosts the Kierens Zone (780,200 tonnes 7.54 g Au/t, 1989) and the Norlartic Mine and the Marbane Shear Zone which hosts the Marbane Mine and the Gold Hawk Mine. Another important setting for gold deposits is structurally controlled, chimney-like intrusive body, best exemplified by the Camflo Mine which to January 1989 had reached total production of 9,034,00 tonnes grading 6.4 g Au/t.

MOUSKOR PROPERTY

Location: North Western Québec, 20 km west of Cadillac, Cadillac Township Project Access: Gravel road from hyway 117 SNRC: 32D / 02 Land Description: 17 Mining claims, 667 Hectares Commodity: Gold Area Deposits: Mouska, Doyon, Bousquet Partners: Breakwater Resources inc & Twin Mining Resources Option: Option to acquire 51% interest.

REGIONAL GEOLOGY
The Mouskor property is underlain by Archean metavolcanics and metasediments of the southern part of the Abitibi Greenstone belt, in the Superior Province of the Canadian Shield. The property is located on the northern flank of the Malartic Syncline (Gunning, 1941), an isoclinal series that shows an east-west trend and subvertical axial trace. The regional stratigraphy is divided into 6 geological groups of sedimentary and volcanic rocks which were metamorphosed from lower greenschist to lower epidote-amphiboles facies. They have been intruded by granitoid stocks and early Proterozoic diabase dykes.

The property is predominately underlain by the lower volcanic assemblage of the Blake River Group flanked to the north by the older Kewagama Group sediments. The Blake River Group consists of mainly mafic to intermediate volcanic flows and less abundant felsic volcanic flows, intercalated pyroclastic rocks, graphitic mudstones and narrow argillitic and conglomeratic horizons. The rocks dip steeply south and trend southeast. Based primarily on geophysical features, it is proposed that the lithological assemblage which forms an isoclinal series plunging to the west was disrupted by late north and north-east trending faults.

NORMAR PROPERTIES

Location: North Western Québec, 20 km west of Cadillac, Cadillac Township Project Access: Gravel road from hyway 117 SNRC: 32D / 02 Land Description: 81 Mining claims 1,323 hectares Commodity: Gold Area Deposits: Mouska, Doyon, Bousquet Partners: Breakwater Resources inc & Twin Mining Resources Option: Option to acquire 51% interest.

REGIONAL GEOLOGY
The property is situated on the southern limb of the Malartic Syncline which is part of the Abitibi Orogenic Belt of the Superior Province. The Normar property hosts from north to south, the Cadillac Group sediments and the sediments of the Pontiac Group. Regionally, these geological units strike east-west and dips vertically to subvertically. The Cadillac-Piche Group contact represents a high strain zone of deformation, regional in extend and known as the Cadillac Break. This crustal fracture is characterized by a broad assemblage of talcchloritecarbonate schists ranging from 30 metres to 150 metres wide.