Yukon Prospect:
Rostock Ventures has acquired what management feels is a high impact gold prospect located in the Yukon, Canada. The property is approximately 3200 contiguous acres and has similar 
geological characteristics as recent gold discoveries in close proximity to this new prospect. This prospect lies within the globally prolific mining region call the Tintina Gold Belt. The Tintina Gold Belt hosts world-class deposits including Donlin Creek (29.3 M ozs Au Proven & Probable reserves), Fort Knox (3.8 M ounces P & P), Pogo (3.6 M ozs P & P), Dublin Gulch (2.7 M ozs Indicated resource); as well as past producers with remaining resources such as Brewery Creek (approximately 278,484 ozs produced, 145,000 ozs Indicated + 143,000 ozs Inferred Resources) and several advanced staged exploration projects including Freegold Mountain and Underworld’s White Gold. Underworld Resources Inc. and Kinross Gold Corporation announced March 11th 2010 that their respective Boards of Directors have approved a business combination by way of a friendly offer by Kinross to acquire 100% of the outstanding common shares of Underworld not already owned by Kinross.
According to Underworld, the culmination of the 2008 and 2009 drill programs is the first resource estimation for the Golden Saddle and Arc Deposits. 1,004,570 ounces at a grade of 3.2 g/t Au in an indicated category were identified for Golden Saddle with an additional 407,413 ounces of inferred resources at an average grade of 2.5 g/t Au. At the Arc Zone, the initial resource was 170,470 ounces at an average grade of 1.2 g/t Au in the inferred category.
The Golden Saddle Deposit which has a footprint of 580 m along strike and up to 560 m down dip remains open to expansion along strike to the northeast, and down dip to the northwest. Strength of alteration and mineralization increases in intensity to the northeast. The most northeasterly and deepest holes completed to-date include holes WD09-101, which intersected 4.86 g/t Au over 23.38 meters and WD09-103 which intersected 5.07 g/t Au over 25.38 meters. The Arc deposit is open in all directions.
At Golden Saddle, gold mineralization is hosted by metamorphosed felsic intrusive units, as well as felsic and mafic metavolcanic rocks, and is associated with quartz veins, stockworks, and breccia zones, as well as pyrite disseminations that form NE striking and moderately NW dipping (±50o) tabular bodies of gold mineralization. Comprehensive metallurgical testing indicates that a 92% or better gold recovery can be expected with a conventional plant at Golden Saddle, with 6% to 9% of contained gold reporting to a gravity concentrator prior to cyanidation. Recent metallurgical testing on Arc deposit mineralization shows recoveries of up to 85% achievable following flotation.
Nevada Prospect: Phase I
The Phase I exploration program on the McVicar Lode Mining Claim as outlined in the writer’s report Dated December 26, 2007 has been completed. The work was performed by Multi Metal Mining Corp. and consisted of trenching and sampling over the known mineral zones on the McVicar Lode Mining Claim.
The McVicar Lode Mining Claim is comprised of one claim with an area of 30 acres located in the Goodsprings (Yellow Pine) Mining District situated within the southwestern corner of the State of Nevada, USA. The McVicar Lode Mining Claim covers some former exploratory workings on a mineral showing.
The McVicar Lode Mining Claim is also situated on the easternmost portion of the Yellow Pine Mining District southern Nevada. Although less famous than many of the other mining districts of the Great Basin it nevertheless ranks second only to Tonopah in total Nevada lead and zinc production. During World War I this district was one of the most productive in the west, but by the end of World War II only a few mines remained in operation.
The region is known for its historic production of lead, silver and gold.
The favorable host rock for the indicated mineralization on the McVicar Lode Mining Claim is indicated to be a limestone. Although information on the mineralization of the McVicar mine is not known, the mineralization at the Root Mine within one mile to the northeast is reported as hydrozincite, calamine, and cerussite; galena occurs as residual pods in masses of cerussite. Production from the Root mine is reported as 3,896,057 LB zinc, 858,055 LB lead, 20,783 oz silver 44,002 lb copper and 27 oz gold.
As recommended in the writer’s December 26. 2006 report on the McVicar Lode Mining Claim, the objective of the Phase I exploration program was to trench and sample the known mineral zone to determine the geological controls and the nature of the mineralization. The trenching and the sampling were successfully complete by Multi Metal Mining Corp. whereupon the writer was provided with the exploration results upon which this report is based.
In completing the recommended Phase I program two trenches were established on the McVicar Lode Mining Claim in location of mineralization and as indicated on the accompanying map. The measurements of the Trench I and Trench II on the McVicar Lode Mining Claim are 30 feet long by three feet wide and two feet deep, and 35 feet long by three feet wide and two feet wide respectively.
Three grab samples were taken; one from the dump of an exploratory working of unknown dimensions, and one each from the two trenches. The samples were submitted for assay to Assayers Canada Laboratory in Vancouver, Canada. The samples were analyzed by a Multi-Element ICP-AES Analysis with the results.
Based on the results of the Phase I exploration program on the McVicar Lode Mining Claim, the writer concludes that the program was successful in that the mineralization and the sampling results from the dump of the McVicar Lode Mining Claim returned encouraging assay results that are indicative of potentially economic zones of mineralization. The dump sample showing mineral values of 10.25% Zn indicates a mineral zone with significant zinc values that was intersected by a tunnel. Lower zinc mineral zone samples taken from indicated mineral zones exposed by the two trenches suggest that parallel zones of structurally controlled mineral zones may occur in the area.
Phase II of the exploration program, as recommended in the writers December 26, 2006 report on the McVicar Lode mining Claim should be initiated and completed. This program of localized VLF-EM and geochemical surveys should assist in defining the structural trend and indicated mineral zones and provide information as to the location of the potentially economic mineral zones within the structures or within deep-seated intrusives.
McVicar Lode Mining Claim, Nevada. Phase II Exploration Program
The Phase II exploration program on the McVicar Lode Mining Claim as outlined in the writer’s report dated December 26, 2007 has been completed. The work was performed by New Zone Explorations and consisted of a magnetometer survey and a VLF-EM survey covering the entire McVicar Lode Mining Claim. The program was modified to substitute the geochemical survey, as originally proposed, to a VLF-EM survey. The modification was based on the surface rock exposure and limited soil horizons that would be required to provide an effective evaluation of soil analysis.
The McVicar Lode Mining Claim is comprised of one located claim with an area of 20 acres located in the Goodsprings (Yellow Pine) Mining District situated within the southwest corner of the State of Nevada, U.S.A. The McVicar Lode Mining Claim covers some former exploratory workings on a mineral showing.
The Yellow Pine Mining District, although less famous than many of the other mining districts of the Great Basin, nevertheless ranks second only to Tonopah in total Nevada lead and zinc production. During World War I this district was one of the most productive mineral producers in the west; but by the end of World War II only a few mines remained in operation. The region is also known for its historic production of lead, zinc, silver, and gold. The favorable host rock for the indicated mineralization on the McVicar Lode Mining Claim is indicated as a limestone. Although information on the mineralization at the McVicar Mine is not known, the mineralization at the Root Mine within one mile to the northeast is reported as hydrozincite, calamine, and cerussite; galena occurs as residual pods in masses of cerussite. Production from the Root Mine is reported as 3,896,057 pounds of zinc, 858,055 pounds of lead. Rostock Ventures Corp.
Phase II Exploration Program
Based on the field data accumulated from the completion of the Phase II exploration program on the McVicar Lode Mining Claim, five maps represented as Figures 3 to 7 in this report, were prepared. Figure 3 shows the magnetometer raw field data; Figure 4 shows the contoured raw field data; Figure 5 shows the VLF-EM survey raw data; Figure 6 shows the VLF-EM raw data as Fraser Filtered results; and Figure 7 shows the contoured Fraser Filtered results with the interpreted VLF-EM anomalous zones.
The result of the magnetometer survey as shown by Figure 4 indicates two magnetometer highs (HI); one in the south and one in the north of the McVicar Lode Mining Claim. The southern HI is specific and centrally localized in the grid bounded by 1100S to 1290S and 150E to 275E. The northern HI is general with localized HI’s in the grid bounded by 425S to 625S and 100E to 450E.
The results of the VLF-EM survey as shown on Figure 7 indicating the interpreted VLF-EM anomalies, three anomalies are indicated on the McVicar Lode Mining Claim; A, B, and C. Anomaly A is situated in the north and is comprised of two trends; an east-west trend and a northeasterly trend with an intersection at 425S, 125E. The intersection correlates with the area of the northern magnetometer HI.
Anomaly B is situated central in the Claim and is comprised of two west-northwest trends which may be one indicated structure offset by a northeast trending zone, which is not shown as an anomaly on the map but is indicated by the extended northeasterly eastern portion of Anomaly B. The main intersection could be at 750S, 310E within an area of magnetometer lows (LO) Anomaly C is situated in the south and is comprised of a west-northwest trending zone, open to the west, with a high (HI) at 1050S, 290E; the eastern end. The HI correlates with the upper portion of the southern magnetometer HI.
It is concluded that the results of the Phase II exploration program were successful in delineating correlative anomalous areas with an indication of potentially economical mineral controlling structures and/or mineralization. The magnetometer HI’s may indicate near surface intrusives creating the structures, as indicated by the VLF-EM anomalies, and providing the primary mineralization which is indicated as primary and altered secondary surface mineralization. The areas of the indicated intersecting VLF-EM anomalies/structures are the prime areas for locating potential economic mineral zones.
Management
Luis Carrillo, President
Luis Carrillo focuses his practice in the areas of corporation finance, corporate and business law, corporate governance, business transactions, and securities. He has significant experience representing buyers and sellers in the structuring and negotiation of complex mergers and acquisitions of both public and privately-held companies.
Luis has also worked closely with growth companies raising equity or debt capital in private placements and other transactions exempt from the registration requirements of the federal and state securities laws. These transactions have included the structuring and negotiation of rights, privileges, and preferences of common stock, preferred stock, convertible debt, warrants and other equity or debt arrangements (including preemptive rights, anti-dilution protections, liquidation and dividend preferences, registration rights, rights of first refusal, co-sale rights, puts, calls, voting rights and board representation, capital calls and other rights). Luis has represented companies in structuring and negotiating joint-venture, partnership and other strategic arrangements, licensing and development agreements, distribution and supply agreements, shareholder agreements, option and warrant agreements, employment and consulting agreements, and non-competition, nondisclosure and proprietary rights agreements.
Market Info
Could Gold Go To $2,000?
Well, you don't have to take my word for it, because like I said, analysts all over the world are saying that it is likely to! Why? One word - Inflation!
As the U.S. government waged war with recession, it was forced to pump trillions of dollars of new money into the syste. Ie. it was printing money. Long term this is likely to devalue the U.S. dollar. As the dollar's value declines it will inevitably result in inflation. Also, the Federal Reserve is keeping interest rates at historic lows to make money available at low rates to the market. This can also be an impetus to impact inflation as the market recovers. As inflation begins the Federal reserve will have to raise interest rates to combat inflation which will put a damper on economic recovery.
While some believe gold will take 2-4 years to jump to $2,000 per ounce, other believe it will be much sooner... but what they ALL believe is that the price of gold "WILL" go higher!
Here are some things to think about:
The respected founder of Goldcorp (GG), Rob McEwen even told Bloomberg how he sees gold rising to as high as $5,000 per ounce in the next four years.
As governments increase the money supply to combat recession, bullion will more than double to $2,000 an ounce by the end of next year.
While McEwen's prediction is bold and looks even outlandish now, look at how in history there were predictions of gold going to over $1,000 per ounce in 2001. Thinking back, it doesn't seem so outlandish now does it?
Also, given the confluence of extremely strong fundamentals, gold will likely rise to levels in the coming years that seem unthinkable today.
Also, CitiGroup believes gold will hit $2,000.... check out this article:
http://freundinvesting.com/2008/12/01/gold-to-2000-by-2009-citigroup-thinks-so/
So as you can see, we are not the only ones who believes gold is likely to hit $2,000 or more in the next two or so years!
Now, that means great things for ALL gold and precious metals mining stocks, but what about ROSV and its prospects?
A company means nothing without solid leadership to take it where it needs to go. A company with bad management is doomed and not even the most positive things within the company will be able to save it. ROSV's CEO, Luis Carrillo, has what it takes to lead the company in its mining and exploration efforts. He also has significant experience in negotiating and implementing mergers and acquisitions which might be in the cards for ROSV down the road.
A smart business professional always capitalizes on what is going on around them. This paradigm shift in gold price is something I believe he will capitalize on in a HUGE WAY with his expertise!
Keep ROSV on your immediate radar, and continue to do your own due diligence as it looks poised to shake the street in our opinion... We believe ROSV could possibly produce quick gains for OTCPicks.com members and amazing long term growth as well!
The ROSV chart is looking very robust lately. ROSV's share price is up more than 300% in the last month on a significant increase in daily trading volume. The stock is trending above both its 13 and 50 day moving average and both the MACD and Stochastics indicators are stongly bullish right now.
Put ROSV on your watchlist and do your due diligence asap as we believe this puppy still has more legs and can still pay dividends for OTCPicks.com members.
