EXTRA HIGH Project
EXTRA HIGH
Country Canada 
Province British columbia
Close to Kamloops
Status EARLY DISCOVERY 
Surface 11 km² / 2,656 acres
Latitude / Longitude 51 N 08 / 119 W 50
Legends
Valorisation
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Produces
Develops
Explores for Copper - Gold - Lead - Silver - Zinc -
Last updated on 7/20/2010 - Terms of Use
Risk and valuation analysis of the EXTRA HIGH Project
Status Risk : Early discovery
Country Risk : Very Low
Title(s) of the EXTRA HIGH Project
Colt Resources Inc.
Interest: 67%
Company website
TitleCompany ProfileAll ProjectsCompany websiteCompany project page
On January 23, 2008, Colt entered into an Option Agreement with Zab Resources Inc. ("Zab"), a related company, whereby Colt has the right and option to acquire, in two separate equal tranches, Zab's 66% undivided interest in the Extra High Property ( more...
Zab Resources Inc.
Owner: 33%
Company ProfileAll Projects
TitleCompany ProfileAll ProjectsCompany websiteCompany project page
Colt is the Operator of the Property and owns a 67% interest while Zab owns the remaining 33% interest in the Property. Colt has the right to acquire Zab’s 33% interest in the Property by making a cash payment of $250,000 to Zab on or before December 31, 2008.
Location of the EXTRA HIGH Project
The Extra High property is located 60 km north from Kamloops B.C. and / or 22 km east from the town of Barriere B.C. via the paved Agate Bay road from Highway 5. Access to the property is then by good gravel logging roads to the 1,450 metre elevation. The main area of interest lies immediately south from the past producing Samatosum Mine.
 
History of the EXTRA HIGH Project
Zab Resources Inc (hereinafter referred to as Zab) acquired 10 Extra High claims in March, 2004 from the late Mr. R. Wells of Kamloops B.C. Subsequently, an additional 25 mineral claims were acquired and became part of the option agreement. These 3 more...
 
Geology of the EXTRA HIGH Project
The Extra High property lies on the Adams Plateau which is located on the western edge of the Ominica Belt. In this area, the belt is comprised of a Lower Paleozoic succession of clastic metasediments, carbonate and mafic volcanic rocks, and an overlying Devonian - Mississipian succession of felsic to intermediate metavolcanics and clastic metasediments, termed the Eagle Bay Assemblage.
 
Location
Data last updated on : 7/20/2008
Disclaimer
All information on this page comes from internal and external sources deemed reliable. This information might not be up to date, so please perform due diligence before making any conclusion or making any action. Do contact us should any information be missing or incorrect.
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