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Last C$0.16 CAD
Change Today 0.00 / 0.00%
Volume 0.0
EVM On Other Exchanges
Symbol
Exchange
Venture
OTC US
Frankfurt
As of 11:27 AM 04/28/15 All times are local (Market data is delayed by at least 15 minutes).

evrim resources corp (EVM) Snapshot

Open
C$0.16
Previous Close
C$0.16
Day High
C$0.16
Day Low
C$0.16
52 Week High
07/31/14 - C$0.45
52 Week Low
12/30/14 - C$0.16
Market Cap
6.0M
Average Volume 10 Days
1.5K
EPS TTM
C$-0.06
Shares Outstanding
37.8M
EX-Date
--
P/E TM
--
Dividend
--
Dividend Yield
--
Current Stock Chart for EVRIM RESOURCES CORP (EVM)

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evrim resources corp (EVM) Details

Evrim Resources Corp. explores mineral properties in Canada and Mexico. The company explores for copper, silver, gold, molybdenum, iron, and precious and base metal deposits. It owns interest in various projects located in Sonora, Durango, and Sinaloa states in Mexico. The company was formerly known as Avaranta Resources Ltd. and changed its name to Evrim Resources Corp. in December 2010. Evrim Resources Corp. is headquartered in Vancouver, Canada.

10 Employees
Last Reported Date: 04/14/15

evrim resources corp (EVM) Top Compensated Officers

Chief Executive Officer, President and Direct...
Total Annual Compensation: C$180.0K
Chief Financial Officer
Total Annual Compensation: C$70.4K
Vice President of Technical Services
Total Annual Compensation: C$145.0K
Compensation as of Fiscal Year 2013.

evrim resources corp (EVM) Key Developments

Evrim Resources Corp. Acquires the Ball Creek Project in British Columbia

Evrim Resources Corp. announced that it has signed an agreement with Paget Minerals Corp. to acquire a 100% interest in the Ball Creek project in northwest British Columbia. Ball Creek is an early stage exploration target covering 52,442 hectares of ground prospective for copper-gold-molybdenum porphyry and epithermal gold-silver deposits. The Ball Creek project is a significant land package straddling sections of the regionally significant Jurassic Eskay Rift and contains several separate porphyry copper-gold-molybdenum and epithermal gold-silver systems associated with the Jurassic intrusives of the Texas Creek plutonic suite. Prominent gossanous alteration zones occur over an area of 20 square kilometres within the property. The Ball Creek porphyry system contains at least four distinct mineralized zones with extensive potassic, phyllic and propylitic alteration indicating a multi-phase and substantial hydrothermal system. Drilling in the Main zone by previous operators intersected 231 metres grading 0.21% copper and 0.54 g/t gold in drill hole BC07-12 and including 15.24 metres grading 0.42% copper and 1.11 g/t gold. The zones remain open in several directions and at depth, and there is significant potential to expand the area of mineralization to the south at the Cliff, Goat, and ME zones, which have seen very limited exploration to date.

Evrim Resources Corp. Acquires the Ardmore Copper Porphyry Property in Arizona

Evrim Resources Corp. announced that it has acquired the Ardmore property in Pinal County, Arizona. Ardmore is an early stage exploration target covering 696 hectares of ground prospective for copper-molybdenum porphyry and gold deposits. The project was identified through the Company's generative programs in 2014 and acquired through staking. The Ardmore project is favorably situated at the intersection of a major northwest belt of porphyry copper deposits (Ray, Miami/Globe, Superior, Resolution) and a northeast belt of similar style deposits (San Manuel/Kalamazoo, Silver Bell, Lakeshore, Safford, Morenci), approximately 60 kilometres north of Tucson. The project is road accessible with no communities nearby. The Company has also consolidated additional prospective ground in the Ardmore area through a separate agreement with local landowners. Geology on the property consists of porphyritic Proterozoic monzogranite to granite and Laramide porphyritic dykes with zones of quartz-sericite alteration. Alteration is truncated by Tertiary andesites and conglomerates of an upper detachment plate, which is mapped as a shallow thrust by the United States Geological Survey. Gold mineralization is coincident with a combination of steep and flat lying structures along the thrust front. The propylitic to phyllic alteration may represent the margin of a porphyry system beneath the overriding upper thrust plate. The project has never been drill tested for concealed porphyry targets and has seen only limited exploration. Mapping and geochemical sampling will be undertaken to determine vectors towards a potential mineral center.

Evrim Resources Corp. Announces Gold-Silver Mineralization Discovered at Ermitano Project, Mexico

Evrim Resources Corp. and exploration partner SilverCrest Mines Inc. announced initial results of nine drill holes on the Company's Ermitaño project in Sonora, Mexico. The 2,656 meter drill program successfully identified the presence of near surface gold and silver mineralization at the El Durazno target. The Ermitaño project is located within the same trend of mineralization that is currently being mined at SilverCrest's Santa Elena mine and comprises an estimated 16,526 hectares. The defined corridor is approximately 10 kilometres by 20 kilometres along a NW-SE trend. The concessions contain Late Cretaceous andesite and rhyolite volcanic rocks which host the vein structures controlling the Santa Elena low sulphidation epithermal mineralization. An exploration program completed in 2014 has tested widespread epithermal mineralization in four defined main targets. The El Durazno target comprises two parallel east-west trending corridors of veining and stockwork mineralization with thickness ranging from 4 meters to 50 meters for a defined cumulative strike length of approximately 900 meters. The first corridor is defined by outcropping of veins and stockwork in an area of 400 meters along strike and 50 meters wide with a total of 86 surface channel samples averaging 1.28g/t gold. The second corridor is defined by outcropping of vein and stockwork in an area of 500 meters along strike and 50 meters wide with 129 surface channel samples averaging 0.34g/t gold. Surface channel samples in the two corridors range from 0.4 meters to 2.0 meters in width and average 1.50 meters in width. Evidence based on epithermal textures and more detailed mineralogical studies suggest a shallower level exposure in a low sulphidation epithermal environment compared to Santa Elena. The interpreted shallow level of exposure presents an excellent opportunity to discover additional mineralization at depth. Ermitaño West contains a network of low sulphidation east–west trending epithermal veins and stockwork within an area of 1,200 meters long and 600 meters wide with 546 surface channel samples averaging 0.17g/t gold over widths ranging from 0.3 meters to 2.0 meters and averaging 1.3 meters. Vein textures suggest a shallower level of exposure in the low sulphidation epithermal environment compared to Santa Elena. Ermitano East is an east–west trending galena-bearing silver vein system with indications of two different levels of epithermal exposure (deep and shallow). Surface sampling returned significant silver grades with 554 channel samples with an average width of 1.60 meters and an average grade of 14 g/t silver, including 6 samples that exceeded 300 g/t silver. Veta Valentina hosts a 1.2 kilometre long and 10 meter wide east-west trending structural corridor with low sulphidation epithermal veining.

 

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Price/Sales 45.7x
Price/Book 1.5x
Price/Cash Flow NM Not Meaningful
TEV/Sales 21.5x
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