Rocher Deboule Minerals Corp.
(RD:TSXV)
Snapshot of Rocher Deboule Minerals Corp. (RD)
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OPEN
C$0.22
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PREVIOUS CLOSE
C$0.21
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DAY HIGH
C$0.22
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DAY LOW
C$0.21
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52 WEEK HIGH
09/30/09 - C$0.32
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52 WEEK LOW
11/28/08 - C$0.07
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MARKET CAP
6.6M
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AVERAGE VOLUME 3 mo
48.1K
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DILUTED EPS TTM
--
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SHARES OUTSTANDING
32.3M
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RD Does Not Pay Dividends
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P/E TTM
NM
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| K = Thousands M = Millions B = Billions | ||
RD Details
Rocher Deboule Minerals Corp. engages in the acquisition, exploration, and development of mineral properties in Canada and the United States. The company explores for iron oxide, copper, gold, manganese, niobium, and magnesium. It holds interests in the Rocher Deboule property, the Lonnie Brent property, and the Canal Flats property, which are located in British Columbia. The company’s properties also include the Artillery Peak property located in Arizona; and the Black Prince, Junction Creek, and Olson properties in British Columbia. It was formerly known as Ameridex Minerals Corp. and changed its name to Rocher Deboule Minerals Corp. in September 2006. The company was incorporated in 1987 and is headquartered in White Rock, Canada.
RD Top Compensated Officers
Key developments for Rocher Deboule Minerals Corp. (RD)
Rocher Deboule Minerals Corp., Annual General Meeting, Jan 12, 2010 Location: 2A 15782 Marine Drive, White Rock, BC V4A 1E6,Canada.
Rocher Deboule Minerals Corp. announced the diamond drill has arrived on their 1,605 hectare (3.900 acre) rare earth niobium property located 7 km East of the community of Manson Creek in British Columbia. The focus of the drill program is to confirm surface values to depth and to identify the rare earth elements and strategic metals such as niobium, tantalum, titanium, lanthanum, neodymium, yttrium and gallium. Geology consists of a syenite-carbonatite complex of Upper Devonian to Lower Mississippian age which occurs in metasediments of the Proterozoic Ingenika Group. The metasediments consists of quartz hornblende gneiss, quartzite, sericitic schlst, feldspathic wacke and garnet-biotite-muscovite schlst. These rocks are metamorphosed to amphibolite phases and impose a penetrative fabric on the complex, concordant with that of the country rocks. The carbonatite appears fault bounded and may be within a mylonitized zone related to regional tectonism. The country rocks are variable fenitized for tens of meters around the complex. The Virgil carbonatite consists of syenite and biotite sovite which is composed of calcite, biotite and minor feldspar, apatite, zircon, columbite and pyrochlore. The zone which strikes 135 degrees and dips 50 degrees is 120 meters long and up to 40 meters wide. Sampling along the length assayed 0.19% Nb2O5 and 0.18% zirconium (assessment Report 10729). A chip sample along 56 meters assayed 0.15% TiO2, 0.05% lanthanum and 0.03% neodymium (Geology, Exploration and Mining British Columbia 1974). Pg 278-279. The Lonnie carbonatite is located on strike 4 km southwest of the Virgil. The Lonnie carbonatite zone has been traced by surface trenching for a length of approximately 650 meters with widths up to 50 meters grading 0.20% Nb2O5. It strikes 120 degrees and dips approximately 60 degrees southwest. A zone in the centre of the property averages 0.3% niobium (Nb2O5) across a width of 7.6 meters and a length of 240 meters. Diamond drilling will be located on the Lonnie carbonatite; results will be reported once they are received.
Rocher Deboule Minerals Corp. announced plans to drill their 1,605 hectare (3.900 acre) rare earth niobium property located 7.0 km Northeast of the community of Manson Creek in British Columbia. The Virgil carbonatite consists of syenite and biotite sovite which is composed of calcite, biotite and minor feldspar, apatite, zircon, columbite and pyrochlore. The zone which strikes 135 degrees and dips 50 degrees is 120 meters long and up to 40 meters wide. Sampling along the length assayed 0.19% Nb2O5 and 0.18% zirconium (assessment Report 10729). A chip sample along 56 meters assayed 0.15% TiO2, 0.05% lanthanum and 0.03% neodymium (Geology, Exploration and Mining British Columbia 1974). Pg 278-279. The Lonnie carbonatite is located on strike 4 km northwest of the Virgil. The Lonnie carbonatite zone has been traced by surface trenching for a length of approximately 650 meters with widths up to 50 meters grading 0.20% Nb2O5. It strikes 120 degrees and dips approximately 60 degrees southwest. A zone in the centre of the property averages 0.3% niobium (Nb2O5) across a width of 7.6 meters and a length of 240 meters (Open File 1987-17). Diamond drilling will be located on the Lonnie carbonatite, with particular emphasis on validating the historical assays on rare earths.
Stock Quotes
| Recently Viewed | |||
| RD (CA) | C$0.21 CAD | -0.005 | |
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| CRA | $6.29 USD | +0.04 | |
| BA | $52.63 USD | +0.93 | |
| NSOL | $0.03 USD | -0.001 | |
| CVS | $31.89 USD | +0.25 | |
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Industry Analysis
| Valuation | RD | Industry Range |
| Price/Earnings | NM | Not Meaningful |
| Price/Sales | -- | Not Meaningful |
| Price/Book | 3.5x |
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| Price/Cash Flow | NM | Not Meaningful |
| TEV/Sales | -- | Not Meaningful |
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RD transactions
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| No transactions in the last 6 months. | ||
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