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THIS NEWS RELEASE IS NOT INTENDED FOR DISTRIBUTION TO UNITED STATES NEWSWIRE SERVICES OR FOR DISSEMINATION IN THE UNITED STATES AND DOES NOT CONSTITUTE AN OFFER OF THE SECURITIES DESCRIBED HEREIN
VANCOUVER, British Columbia, March 19, 2019 (GLOBE NEWSWIRE) — Riverside Resources Inc. (“Riverside” or the “Company”) (RRI.V) is pleased to announce it has closed its previously announced private placement. The placement was over-subscribed and the Company issued 17,488,875 units at a price of $0.16 per unit for gross proceeds of $2,798,220 instead of the 9,375,000 units ($1,500,000) originally contemplated.
Each unit consists of one common share and one whole common share purchase warrant (“Unit”). Each common share purchase warrant is exercisable into one common share for a period of two (2) years from closing at a price of $0.22 (“Warrant”). If, at any time after July 20, 2019, the closing price of the common shares on the TSX Venture Exchange (“TSX-V”) trades at a VWAP equal or greater than $0.45 for 10 consecutive trading days, the Company may accelerate the expiry date of the Warrants by disseminating a press release announcing the new expiry date whereupon the Warrants will expire on the 30th trading day after the date on which such press release is disseminated.
Management and insiders subscribed for 845,000 Units for $135,200 in total proceeds to the Company.
With respect to a portion of the funds raised in the private placement, the Company paid finders’ fees of $87,312 to Sprott Global Resource Investments Ltd., $20,076.80 and 12,000 Units to Haywood Securities Inc., 16,000 Units to Canaccord Genuity, and $1,280 to PI Financial Corp.
All securities issued pursuant to the private placement and as finders’ fees will be subject to a four-month hold period expiring on July 20, 2019.
The Company will use the proceeds of the financing to fund a focused drill program at the Cecilia Gold Project, additional project acquisitions and further target refinement on existing projects to advance towards new partnerships.
The securities being offered have not been and will not be registered under the U.S. Securities Act of 1933, as amended, and may not be offered or sold in the United States or to, or for the account or benefit of, U.S. persons without United States federal and state registration or an applicable exemption from registration requirements.
About Riverside Resources Inc.:
Riverside is an exploration company driven by value generation and discovery. The company has fewer than 65M shares issued and a strong portfolio of gold-silver and copper assets in North America. Riverside has extensive experience and knowledge operating in Mexico and leverages its large database to generate a portfolio of prospective mineral properties. In addition to Riverside’s own exploration spending, the Company also strives to diversify risk by securing joint-venture and spin-out partnerships to advance multiple assets simultaneously and create more chances for discovery. Riverside has additional properties available for option, with more information available on the Company’s website at www.rivres.com.
ON BEHALF OF RIVERSIDE RESOURCES INC.
“John-Mark Staude”
Dr. John-Mark Staude, President & CEO
For additional information contact:
| John-Mark Staude President, CEO Riverside Resources Inc. info@rivres.com Phone: (778) 327-6671 Fax: (778) 327-6675 Web: www.rivres.com |
Raffi Elmajian Corporate Communications Riverside Resources Inc. relmajian@rivres.com Phone: (778) 327-6671 TF: (877) RIV-RES1 Web: www.rivres.com |
Certain statements in this press release may be considered forward-looking information. These statements can be identified by the use of forward-looking terminology (e.g., “expect”,” estimates”, “intends”, “anticipates”, “believes”, “plans”). Such information involves known and unknown risks — including the availability of funds, the results of financing and exploration activities, the interpretation of exploration results and other geological data, or unanticipated costs and expenses and other risks identified by Riverside in its public securities filings that may cause actual events to differ materially from current expectations. Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this press release.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

First pass drill program returns encouraging results
TSX VENTURE SYMBOL: FUU
KELOWNA, BC, March 20, 2019 /CNW/ – FISSION 3.0 CORP. (“Fission 3” or “the Company“) is pleased to announce results from the first pass drill program at its Key Lake South properties (Karpinka Lake and Hobo Lake projects) in the south-east Athabasca Basin region of Saskatchewan, Canada. A total of ~1300m was drilled in eight completed holes, all of which encountered variably intense hydrothermal alteration and six holes with anomalous radioactivity. Of note, holes KL19-005, KL19-006 and KL19-007, drilled in the northern part of the extensive land package, encountered the most significant hydrothermal alteration and paleoweathering, which are considered important factors for hosting high-grade uranium mineralization and will be prioritized for follow up. With $6M in the treasury, Fission 3 is well poised to continue to explore on its extensive property portfolio.
Ross McElroy, COO, and Chief Geologist for Fission, commented,
“The drill program at Key Lake is the latest step in the ongoing exploration of our prospective uranium projects. With radioactivity and strong alteration in multiple holes, we are looking at very encouraging first pass results that warrant follow up drilling. The winter program will now progress with a ground geophysics DC resistivity survey on our Cree Bay property in the northeast basin area, as we focus on developing high-priority drill targets to be tested during the summer exploration program.”
About Key Lake South: The Key Lake area is an important historic mining district. The Key Lake operations is owned by Cameco Corp. (83%) and Orano Canada Inc. (17%) and hosted the former Key Lake mine, which produced 208 million pounds of uranium between 1975 to 1997 and is home to one of the largest uranium mills in the world. The Key Lake mill processed ore from the McArthur River uranium deposit, until Cameco announced in 2018 that McArthur River mining would be suspended indefinitely due to low uranium prices. The area is considered highly prospective to discover significant new uranium occurrences.
The 100% owned Key Lake South Projects consist of two projects (Karpinka Lake and Hobo Lake) covering 19,377 ha in 42 mineral claims. The properties are located approximately 40km south of the historic Key Lake mine. The projects are geologically situated within the extremely prolific Wollaston-Mudjatic Transition Zone “WMTZ”, notable for hosting the majority of the major high-grade uranium deposits on the eastern side of the Athabasca Basin. To the north, the Key Lake Deposit is hosted within the northern portion of northeast-southwest trending litho-structural feature known as the Key Lake Shear Zone “KLSZ”. The KLSZ continues southward through the Karpinka Lake and Hobo Lake projects. Together the properties cover approximately 50km of trend of the KLSZ, where a number of geochemical uranium anomalies have been discovered and where a network of EM conductors exhibit structural complexity including off-sets, breaks, folding and other geophysical features such as gravity and resistivity lows. These features are often associated with uranium mineralization occurrences.
Key Lake South Projects – Drilling Summary
Table 1: Winter 2019 Key Lake South Drill Hole Summary
| Property | Target | EM Conductor | Hole ID | Collar | * Down-hole Radiometric Highlights with Mount Sopris 2PGA-1000 Natural Gamma Probe |
Overburden Depth (m) |
Total Depth (m) |
||||
| Azimuth | Dip | From (m) | To (m) | Width (m) | CPS Peak | ||||||
| Karpinka Lake |
Key Lake Shear Zone | FOR-B-2220 | KL19-001 | 79 | -75 | 99.9 | 100.2 | 0.3 | 743 | 18.0 | 149.0 |
| 111.3 | 111.9 | 0.6 | 884 | ||||||||
| 114.9 | 115.3 | 0.4 | 984 | ||||||||
| 126.5 | 126.8 | 0.3 | 948 | ||||||||
| 129.4 | 131.8 | 2.4 | 1431 | ||||||||
| FOR-2 | KL19-002 | 274 | -50 | 53.5 | 53.8 | 0.3 | 1344 | 2.1 | 101.0 | ||
| 79.1 | 80.2 | 1.1 | 985 | ||||||||
| FOR-B-2220 | KL19-003 | 257 | -63 | 217.2 | 218.1 | 0.9 | 1492 | 15.3 | 251.0 | ||
| 220.3 | 220.6 | 0.3 | 693 | ||||||||
| KAR-3160 | KL19-004 | 277 | -54 | 69.1 | 70.0 | 0.9 | 1302 | 37.6 | 125.0 | ||
| KL19-005 | 86 | -61 | No anomalous radioactivity | 39.0 | 128.8 | ||||||
| KL19-006 | 90 | -52 | No anomalous radioactivity | 57.0 | 101.0 | ||||||
| KL19-007 | 86 | -67 | 113.7 | 114.3 | 0.6 | 840 | 29.0 | 152.0 | |||
| 118.7 | 119 | 0.3 | 595 | ||||||||
| N/A | KL19-008 | 271 | -55 | 212.3 | 212.5 | 0.2 | 550 | 7.3 | 293.0 | ||
| TOTAL | 1300.8 | ||||||||||
KL19-001
KL19-001 was an angled drill hole oriented parallel to the intermittent, weak, calc-silicate hosted radioactivity intersected in historic hole RO-01. The purpose of KL19-001 was to test the radioactive calc-silicate from the top of bedrock down to a depth of approximately 150m. Bedrock was intersected at a depth of 18.0m down hole and was comprised of variably clay, hematite, graphite and chlorite altered schist, cataclasite and calc-silicate. A strongly hematized calc-silicate was cored from 126.8m to 132.5m down hole which returned weak radioactivity up to 590 cps on a RS-125 handheld scintillometer. No other anomalous radioactivity was intersected, and the hole was terminated at a depth of 149.0m in weakly altered graphitic schist.
KL19-002
KL19-002 was an angled drill hole targeting the Key Lake Shear zone (KLSZ) approximately 950m south of KL19-001. Bedrock was intersected at a depth of 43.0 m down hole and was comprised of weakly altered orthogneiss and calc-silicate gneiss to a depth of 72.9m. From 72.9m to 80.3m a strongly sheared biotite-garnet gneiss was cored with a central 5.2mwide graphitic brittle-ductile fault zone. The hole was terminated at a depth of 101.0m in fresh orthogneiss.
KL19-003
KL19-003 was an angled drill hole targeting the weakly radioactive calc-silicate approximately 75m below that intersected in KL19-001. The drill hole aimed to assess the variability in previously intersected calc-silicate thickness and radioactivity with depth, and to test for parallel radioactive calc-silicate lenses. Bedrock was intersected at a depth of 15.3m down hole and was comprised of a thick sequence of biotite schist to a depth of 182.5m where a sheared, graphitic schist was intersected. A weakly radioactive calc-silicate lens was cored from 222.2m to 224.5m which returned up to 410 cps on a RS-125 handheld scintillometer. The hole was terminated at a final depth of 251.0m in fresh orthogneiss.
KL19-004
KL19-004 was an angled drill hole testing the southern extent of a large left stepping electromagnetic conductor trace ~7km north of KL-001. This flexure is interpreted to reflect a dilational zone in the KLSZ caused by sinistral strike-slip movement. Bedrock was intersected at a depth of 37.0m down hole and was comprised primarily of weakly hematite altered orthogneiss. An intercalacted sequence of weakly graphitic biotite-garnet schist and cataclasite was cored from 42.7m to 66.9m down hole. No anomalous radioactivity was intersected, and the hole was terminated at a depth of 125.0m in fresh orthogneiss.
KL19-005
KL19-005 was an angled drill hole testing the same large, left stepping KLSZ VTEM conductor trace as KL19-004, approximately 1 km further to the north. Bedrock was intersected at a depth of 39.0m down hole as was comprised of moderately to extremely bleached, clay, hematite, chlorite and graphite altered orthogneiss. A strongly graphitic, clay and chlorite altered cataclasite was intersected from 85.5m to 94.5m down hole. Thin limonitic fractures in the graphite altered orthogneiss at approximately 78m down hole returned elevated radioactivity up to 200 cps on the RS-125 handheld scintillometer. The hole was lost due to ground conditions at a depth of 128.8m in strongly chlorite and graphite altered orthogneiss.
KL19-006
KL19-006 was an angled drill hole testing the up-dip projection of the graphitic cataclasite in hole KL19-005. Bedrock was intersected at depth of 56.0m down hole and was comprised of weakly clay and chlorite altered orthogneiss. The drill hole is interpreted to have overshot the graphitic cataclasite which down-dropped the bedrock surface to the east (normal faulting). No anomalous radioactivity was intersected and the hole was terminated at a depth of 101.0m in weakly chlorite and clay altered orthogneiss.
KL19-007
KL19-007 was an angled drill hole testing the down-dip projection of the structural damage zone and strong alteration in KL19-005. Bedrock was intersected at a depth of 29.0m down hole and was comprised of extremely clay and chlorite altered graphitic cataclasite, variably altered graphitic schist, biotite schist and orthogneiss. Weak elevated radioactivity up to 160 cps was recorded on the RS-125 handheld scintillometer at 119.0m hosted in intercalated quartzitic and graphitic schist. Apart from the upper cataclasite no structural damage zone was intersected below KL19-005 and the hole was terminated at a depth of 152.0m in fresh orthogneiss.
KL19-008
KL19-008 was an angled drill hole testing for the northern extension of the historic DD-Zone where previous historic drilling returned up to 0.78% U3O8 over 0.5m. Bedrock was intersected at a depth of 7.3m down hole and was comprised of a thick intercalated sequence of graphite altered amphibolite and calc-silicate to a depth of 136.8m. Below 136.8m, the hole encountered weakly altered to fresh biotite-garnet schist and graphitic schist. A 0.20m granite intrusion at 90.5 m depth returned elevated radioactivity up to 540 cps. The hole was terminated at a depth of 293.0m in fresh biotite-garnet schist.
Natural gamma radiation in drill core that is reported in this news release was measured in counts per second (cps) using a Mount Sopris PGA-1000 Natural Gamma Probe and a hand-held RS-125 Scintillometer manufactured by Radiation Solutions. The reader is cautioned that scintillometer readings are not directly or uniformly related to uranium grades of the rock sample measured and should be used only as a preliminary indication of the presence of radioactive materials.
Samples from the drill core are split in half sections on site. Where possible, samples are standardized at 0.5m down-hole intervals. One-half of the split sample will be sent to SRC Geoanalytical Laboratories (an SCC ISO/IEC 17025: 2005 Accredited Facility) in Saskatoon, SK. Analysis will include a 63 element ICP-OES, and boron.
All depth measurements reported, including radioactivity and mineralization interval widths are down-hole, core interval measurements and true thickness are yet to be determined.
Cree Bay Exploration: In 2017 a ground DC Resistivity survey was completed in 2 separate grids centered on sections of strong conductivity interpreted from a historic airborne GEOTEM electromagnetic survey on what was then the Cree Bay property. Fission 3 subsequently staked additional ground to cover the most conductive part of this anomaly. The winter 2019 exploration work will thus continue to extend the ground geophysics survey over the anomaly, to determine the highest priority drill targets. The program will consist of a winter 21 line-km ground DC Resistivity survey and 2 lines of Moving Loop TDEM survey will be conducted during April to cover the most geophysically prospective area identified from a historic GEOTEM electromagnetic survey.
About Cree Bay: The Cree Bay property, located 20km south of the town of Stony Rapids, consists of 16 claims totaling 14,080 ha and sits on the inside edge of the north-eastern Athabasca Basin. The property is located along the major SW-NE trending Virgin River Shear Zone. Locally the conductive corridor is bound by the Black Lake Fault to the north and East Channel Fault to the south. The historic Nisto uranium mine, is located ~7.5km to the northeast, along the Black Lake fault.
The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and reviewed on behalf of the company by Ross McElroy, P.Geol. Chief Geologist and COO for Fission 3.0 Corp., a qualified person.
About Fission 3.0 Corp.
Fission 3.0 Corp. is a Canadian based resource company specializing in the strategic acquisition, exploration and development of uranium properties and is headquartered in Kelowna, British Columbia. Common Shares are listed on the TSX Venture Exchange under the symbol “FUU.”
ON BEHALF OF THE BOARD
“Ross McElroy”
Ross McElroy, COO
Cautionary Statement: Certain information contained in this press release constitutes “forward-looking information”, within the meaning of Canadian legislation. Generally, these forward-looking statements can be identified by the use of forward-looking terminology such as “plans”, “expects” or “does not expect”, “is expected”, “budget”, “scheduled”, “estimates”, “forecasts”, “intends”, “anticipates” or “does not anticipate”, or “believes”, or variations of such words and phrases or state that certain actions, events or results “may”, “could”, “would”, “might” or “will be taken”, “occur”, “be achieved” or “has the potential to”. Forward looking statements contained in this press release may include statements regarding the future operating or financial performance of Fission 3.0 Corp. which involve known and unknown risks and uncertainties which may not prove to be accurate. Actual results and outcomes may differ materially from what is expressed or forecasted in these forward-looking statements. Such statements are qualified in their entirety by the inherent risks and uncertainties surrounding future expectations. Among those factors which could cause actual results to differ materially are the following: market conditions and other risk factors listed from time to time in our reports filed with Canadian securities regulators on SEDAR at www.sedar.com. The forward-looking statements included in this press release are made as of the date of this press release and Fission 3 Corp. disclaim any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as expressly required by applicable securities legislation.
SOURCE Fission 3.0 Corp.
Matt Gili the CEO, President, and Director of Nevada Copper (TSX: NCU | OTC: NEVDF) sits down with Maurice Jackson of Proven and Probable to discuss the value proposition of Nevada Copper, which is on target for U.S. production in Q4 2019. Mr. Gili, provides updates on the flagship Pumpkin Hollow Project, which hosts both an underground and open-pit deposits. We provide an overview on the supply an demand fundamentals on Copper, where a prudent speculator may position themselves to take advantage of the copper supply deficit.
Matt Gili, CEO of Nevada Copper, talks with Maurice Jackson of Proven and Probable about his company’s progress in beginning copper production by the end of the year.







Ross McElroy the COO and Chief Geologist for Fission 3.0 (TSX.V: FUU | OTCQB: FISOF) sits down with Maurice Jackson of Proven and Probable to discuss the value proposition of Fission 3.0 and their Property Bank. In this interview Mr. McElroy provides the macro economics for uranium and how one may allocate their uranium holdings in a Uranium Project Generator with a Property Bank with projects located in high-grade uranium districts, with proven management and technical team that has a 20 year history of delivering success to shareholders.
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Original Source: https://www.streetwisereports.com/article/2019/03/16/prospect-generator-in-position-for-uranium-turnaround.html
Maurice Jackson: Joining us for a conversation is Ross McElroy, the COO and chief geologist for Fission 3.0 Corp. (FUU:TSX.V; FISOF:OTC.MKTS): A Uranium Project Generator and Property Bank. Ross McElroy, glad to have you back on the program to share the value proposition of Fission 3.0. Before we begin, Ross, I’d like to begin with some basic fundamentals regarding uranium. For someone new to the uranium sector, what is uranium, and where is it used?
Ross McElroy: Uranium is really all about energy. The way we use uranium is for nuclear fuel. That’s basically the fuel that runs reactors.
Globally nuclear power constitutes between 15% and 20% of the electrical requirements. That’s really where the majority of the uranium is used. There is some uranium that’s used for strategic purposes on a country by country basis, more for the Department of Defense reasons. But really, the vast, vast majority of uranium is used to fuel nuclear reactors.
Maurice Jackson: Provide us with some metrics on how abundant uranium is in the Earth’s crust, and correlate that to the average grade that is found versus the grade that is needed to define an ore deposit in a future mine?
Ross McElroy: Well, uranium is actually one of the most abundant elements in the Earth. It’s kind of ubiquitous. You’ll see it throughout the Earth’s crust; there is trace amounts of uranium present primarily in volcanic and igneous rocks and sedimentary rocks.
On a deposit level, there’s actually a number of uranium deposits around the world, in every continent on the planet and in many countries. On a global basis, the average grade of a uranium deposit worldwide is around 0.1 to 0.15% U308.
Now, if you compare that to say, the deposits in Canada, they’re orders of magnitude higher grade in Canada. We’re talking orders of magnitude that are 10 to 20 times that of the global grade.
Although I’ve given you the average grade, most of those deposits at those lower grades, the average grades are really uneconomic deposits. We need grades that are generally much higher than the 0.1%–0.15% if it’s going to be an economic deposit. And that’s what Canada has. Canada has very high-grade deposits, so the economic metrics are just that much more attractive in Canada.
Maurice Jackson: Now that we’ve identified uranium’s utility, what can you share with us from a supply and demand perspective?

Ross McElroy: Well, it’s fairly simple to understand what the demand for nuclear energy is, in other words, uranium. We can just multiply the number of reactors around the world that are currently operating, and the known fuel consumption rate for a 1000 megawatt reactor is just under 500,000 pounds of uranium a year. If we look at the global reactors, there are around 450 reactors around the world. You can see that the need for uranium on an annual basis is around the realm of almost 200 million pounds of uranium.
Maurice Jackson: How does the nuclear plant in Fukushima, Japan, fit into this narrative?
Ross McElroy: Japan historically, up until the Fukushima event in 2011, was one of the main users on a country basis worldwide. Japan I think consumed almost 20% of the world’s nuclear power, in other words, 20% of the world’s annual production of uranium was used to run the Japanese reactors.
In 2011, of course, we had the magnitude 9 earthquake followed by a tsunami, and that’s what damaged the Fukushima facility. Interestingly enough, even with that magnitude of an earthquake and the soon-to-follow tsunami, the reactor still did not breach. The housing that surrounded the reactor was damaged, and this is where some of the radiation leaks came from, but the reactor itself actually held, and so the damage was actually very, very limited and manageable.
What happened is overnight, Japan shut down all of its nuclear reactors, in other words, all 52 reactors I think they had working at that time, went offline. That caused disruption to the supply/demand situation globally.
What’s happened since then is Japan is slowly coming back on. Japan’s alternatives for power are pretty limited as the country doesn’t have very much of its own resources, if any at all. It imports whatever energy that it needs, be it in natural gas now, in nuclear.
It’s important for Japan to be able to operate these factories that they’re running. I mean, it’s an exporting country around the world, so it does have high energy requirements. It also has the requirements for inexpensive power.
Japan is coming back on to the scene as far as nuclear power. There are eight reactors that are currently back up and operating, and 17 reactors that are in the near-term licensing for approval to get them restarted again.
I think the bottom line is, prior to Fukushima, Japan depended on nuclear energy for at least 25% of its electricity demands. I think by the time 2030 approaches, Japan is supposed to be right back up to those same levels. The country is coming back on, it has always been an important major consumer of nuclear power. I think we’ll see it right back to the equation again in the very near future.
Maurice Jackson: Uranium, next to gold, is known as the other yellow metal, and here’s why. Ross, let’s step back to the bull market in uranium. If one was selective with the uranium holdings, they would’ve had generational changes in their portfolio. What was the spot price during the last bull market?

Ross McElroy: Well, in 2002, uranium was around, I don’t know, about $15 a pound. This is on the spot market. That’s what uranium was trading for.
In 2003–2004, we really saw the lift off of the price of uranium. In fact, it peaked at 2007 to around $140 a pound. It went almost a 10-fold increase in the price of the commodity between 2003 and 2007. The peak at 140 didn’t last particularly long, but it had a slower decline until about 2008—2009, it stabilized, and then it peaked back up again.
Really, it was holding steady. I guess this is the point I would want to make, is that we were starting to see a steady state price of between $50 to $70 a pound, and then the Fukushima event hit that we talked about in 2011, and that really threw the whole pricing structure right out the window. We’ve been working on our recovery ever since.
Maurice Jackson: What is the spot price for uranium today?
Ross McElroy: Currently we’re about $28 a pound for uranium. It has recovered; we’re off the bottoms of $17, $18 a pound just a couple of years ago. Uranium is making its way back.
Maybe the important point here to note is we’re still at prices that the majority of mines around the world are not profitable. Even the lowest cost producers are really not operating in an environment where they can make money with uranium prices what they’re at right now.
What we’ve seen is that the supply is starting to be restricted as the producers are taking a lot of that uranium off market; they’re not supplying it to the utilities at this cheap price, because it’s not a working business model to lose money in the long run on the mining of the commodity.
We are seeing an improvement in the price of uranium, and it’s been about a year and a half in the making. It’s gone up from the $18 that I mentioned to about $28 a pound, but it certainly has a lot more room to move upwards even before we can start to get production back online to meaningful levels.
Maurice Jackson: What is that spot price that companies right now, uranium companies I should say, for them to earn their cost of capital? Is the number around $60 for a spot price of uranium?

Ross McElroy: I believe you are correct. We’re seeing prices that globally, they have to be in the $60 to $70 a pound really to bring on any meaningful production.
One of the clues that I look at when we look at the best uranium mines out there, the lowest cost producers, those would be McArthur River deposit in Canada’s Athabasca Basin in Northern Saskatchewan. That is one of the best uranium mines in the world, certainly the largest highest-grade operating mine. Cameco took that offline because of the prices of uranium where they were at, they weren’t making any money on the mining of this deposit.
There are some indications that Cameco won’t turn that mine back on into being a producer until the price of uranium is somewhat north of $40, maybe $45. Something in that realm.
I don’t have an exact number there, but it does tell you that if you’re going to even bring back the best of those deposits, you really need prices that are something of $40 to $45. As we mentioned earlier, the price for many of the other deposits around the world are probably closer to $60 or $70. You can see, there’s still lots of room for improvement.
Maurice Jackson: The current price of uranium does not support the fundamentals. What correlations do you see today that may exceed the returns from the last bull market?
Ross McElroy: Well, it’s sort of an elastic situation. I think that the longer that we keep depressed prices, yet the demand is still there and growing, reactors are being built, the need to fuel these reactors, that’s not stopping.
In fact, it’s growing. You have the primary suppliers of uranium, i.e., the mines that are not supplying it, the longer that the prices are low, the more rapid that climb will be in the price of uranium when it does correct.
I think there’s a possibility, as I’ve heard some analysts call it, a violent reaction upwards to the price of uranium. I think we’re going to see some substantial price increases within some short vision of time, maybe a year or two or three. Something in that realm that I think will be quite meaningful.
We’ll see what happens, but the longer it stays depressed, the more likely and quicker the rise will be when it does come.
Maurice Jackson: Ross, you’ve provided a compelling case on the fundamentals for uranium. I know readers may be asking, how will all of this demand for uranium be met? Mr. McElroy, please introduce us to Fission 3.0.
Ross McElroy: Fission 3.0 is a uranium explorer. This is a company that we spun out of Fission Uranium Corp. (FCU:TSX; FCUUF:OTCQX; 2FU:FSE), our larger company, back in 2014 when we bought out our partner on the Patterson Lake project, and in so doing with that process from that arrangement, we spun out our non-core assets, the more grassroots exploration projects.
We’ve been able to build up an exploration portfolio, primarily focused in the Athabasca Basin. Remember, the Athabasca Basin is Canada’s only producing uranium field. That’s where the McArthur River deposit is, this is where Fission Uranium has the Triple R deposit. There’s some fantastic deposits out there.
That’s what we’re exploring for in Fission 3.0. We’re looking for the next high-grade uranium deposit in the Athabasca Basin.
Maurice Jackson: You referenced that you’re a project generator. There’s a lot of ambiguity regarding project generators. Please share the virtues and why Fission 3.0 took on the project generator business model?
Ross McElroy: Project generators are really all about sharing the risk. In our case, what we do very well is pick ground. We’ve been able to strategically stake ground in the Athabasca Basin, we’ve made discoveries on two of our properties, the first one in the company called Fission Energy that we made the discovery at our Waterbury Lake property, and later on in Fission Uranium Corp on our PLS property.
That have been situations where we’ve had joint-venture partners sharing the risks, sharing the costs with others. To use the model, what we do is we use our brands and other peoples’ money. That’s really what we’re good at, that’s basically the model that we have.
We have a very highly trained technical team that’s exceptional at picking out high-quality projects. We attract other people who are looking to get into the uranium business, looking to partner up with a team such as ours and join us for the ride to make a discovery.
It’s really all about sharing risk. That’s really what the project generator model does. It’s our land, and we partner with good quality people that can fund a project, and that’s how they earn into it as well.
Maurice Jackson: Do you currently have a joint-venture partner? If yes, who and what are the terms of the relationship?
Ross McElroy: We have had joint-venture partners in the past, and very successful ones. As I mentioned earlier on our Waterbury project, we had a partner with the Korean utility called KEPCO. It earned in by spending a certain amount of money on the property each year over the course of a three-year period.
What we did with that, we were able to make a discovery, using the money in that project, we made a discovery, built up the resource estimate on there, and eventually sold that asset. That was how our shareholders were able to take advantage of our monetizing on the property.
I guess we could say the same at the PLS project, which we now own 100% of it, but that was also a partnership. We shared in the risk early on and in the money early on with our partner. We eventually bought them out in 2014. That was another example of a successful joint venture partnership.
Each one of the deals would be a little bit different from each other. It is a model that we think works very well. I will note that in our property down in Peru as well, we have a partnership that we’re still looking to finalize the deal. This is one where another group has approached us, said it’s interested in the potential of a property down in Peru. It will spend a significant amount of money having us as the operator. Hopefully we’ll make a discovery down in Peru as well.
Maurice Jackson: Well, you’ve just alluded to my next question. Fission 3.0 has 18 projects in its project bank. Now, it is strategically located in premier, high-grade uranium districts in Canada and Peru. Mr. McElroy, introduce us to the Fission 3.0 Project Bank (click here).

Ross McElroy: We have 18 properties in the Athabasca Basin. Our properties, we think that everywhere in the Athabasca Basin has the potential to host high-grade uranium projects.
One of the keys that we seek to identify are deposits that will be shallow. In other words, the closer a deposit is to surface, the easier it is to build a case that this could be a project that could go into production. It’s an easier mine to develop the closer it is to the surface.

Really deep deposits are challenging. They still exist, but they’re challenging. Eventually they cost more money to find and cost more money to get out of the ground. They’re just another level of challenge.
If you look at our 18 properties, they’re all in and around the edge of the Athabasca Basin, where we’ve had a great deal of success finding near-surface mineralization.
Our PLS project that hosts the Triple R deposit in Fission Uranium is a great example of a near-surface deposit. The mineralization starts at 50 meters below the surface, so 150 feet below the present-day surface is where the high-grade mineralization starts. That makes it a potentially open-pit deposit, which is generally low cost and gives you a lot of flexibility.
This is the sort of thing that we’re looking for in Fission 3.0. We’ve got very good properties that are in known mining districts, conversely, we have a good portfolio of ground around the southwest side of the basin where our PLS project in Fission Uranium is hosted, and also NexGen’s Arrow deposit, it’s all in that same area. We have the significant land package that surrounds that area.

We also have a good strategic land package in and around the Key Lake area on the southeast side of the basin. This has been, and still currently is the hot bed of uranium mining in Canada right now. This is the side of the basin where the McArthur River and Cigar Lake deposits are located.

McArthur shut down for economic reasons waiting for higher uranium prices. It was an operating mine up until about a year ago, and Cigar still is in operation. You’ve also got the Key Lake mine.
It’s a strategic area to have a good land package. We think there’s lots of opportunities in and around land in that area to make a new discovery.

And probably third for us is the land package that’s up in the northwest side of the basin, in the old uranium city Beaverlodge district where uranium mining in Saskatchewan first got started back in the 1950s and was the going concern back in the ’50s and the ’60s, I think there were about 52 operating mines up in that area, pretty small scale most of them, but still lots of high-grade uranium. That’s an area where we think that there’s still plenty of exploration potential.
Between all those areas, we’re going to be active and we’re going to be looking for the next high-grade uranium deposit in Saskatchewan.
Maurice Jackson: Speaking of being active, is there active drilling going on right now in these projects?
Ross McElroy: There is active drilling. We did drill in the southwest side of the basin. We were drilling in January on our PLN project. That project is just immediately north of Fission Uranium’s PLS project.
You’re really talking about the same area where the latest discoveries have been found, where you’ve got the Triple R deposit, you’ve got NexGen’s Arrow deposit. These are two of the best new deposits that have been found in the Athabasca Basin in the last 15 years.
We have a package around there called PLN, and we did drill six holes in there earlier this year. It has the potential to host another one of these fantastic deposits, so we are going to continue looking there. We see all the signs present that tell us that this is where we’ll make that discovery.
As we’re speaking right now, we’re drilling over in the Key Lake area that I described earlier. This is over on the southeast side of the basin, about 200 kilometers to the east of the PLS drilling. That is a program where we’ll drill probably eight or nine holes, just south of the Key Lake Mill and the old historical Key Lake deposits. There’s areas of activity there. We’ll continue drilling throughout the rest of 2019 on a number of our projects.
Fission 3.0 is active. We were able to raise some significant money early in the year, in late 2018. We’re going to be active. This is how we’ve been successful in the past, is by being aggressive, looking in places where people probably haven’t looked for a while or never even thought to look, and putting our technical team to work. Yes, you’ll see pretty good news flow out of Fission 3 this year.
Maurice Jackson: Ross, let’s expand the narrative on the project bank portfolio and go south into Peru. What can you share with us there?

Ross McElroy: Peru is a really interesting area. Where our projects are is called the Macusani Plateau, located in southern Peru, near the Bolivian border. The Macusani Plateau has shown at least over 100 million pounds in near-surface uranium deposits.

There’s a company down there that’s quite dominant called Plateau Energy. Plateau has been able to stake a lot and consolidate a land package in the area, and consolidated all these old deposits. It has amassed around 100 million pounds of uranium in these uranium deposits.

However, even more significant, Plateau made a discovery of high-grade lithium in the same area, and in fact, that’s within five kilometers of our southern property boundary on our Macusani plains. Not only do we have the potential now to host near-surface uranium deposits, and we have shown in fact that we do have mineralization on our property for uranium, we’ve mapped it, we’ve drilled, we’ve trenched and found high-grade uranium, but now the potential’s there for hosting high-grade lithium.
This is really a new dimension that we have down in that area, that we wouldn’t have had say, two or three years ago when we were last down drilling. You’ve got uranium, and now we have lithium. It’s a very interesting up-and-coming area as well.
Maurice Jackson: Switching gears, Fission 3.0 has the right projects in the right place at the right time. But that’s only part of the story. Equally important are the people that are responsible for increasing shareholder value. Mr. McElroy, please introduce us to your board of directors.
Ross McElroy: Thank you, and I appreciate that. We do have a very successful team. Our founder of Fission 3.0 is also the same CEO and founder of Fission Uranium, and previously Fission Energy before that, and Strathmore.
Dev Randhawa has been involved in this company right from the get-go in its first iteration back in 1996, and also heading up Fission 3.0. Dev is the longest running CEO in the uranium sector.
Myself, I’ve been involved with Dev 12, 13 years now. We’ve had a great successful relationship. We’re able to raise money, raise attention, put that money to work, make discoveries, and basically build shareholder value right from the bottom up.
This is the group that I think, we’ve been able to deliver in the past, and we’re going to be able to deliver shareholder value as we move forward in this much improving uranium sector.
A lot of the same players that we’ve had all the way along, still keep also in the Fission 3 group.
Maurice Jackson: Who is on your management team?

Ross McElroy: The management team is composed of our CEO Dev Randhawa and chairman. I am the chief operating officer, and also the chief geologist. We have maintained the same structure that we have in Fission Uranium, is the same that we have in Fission 3.0. It’s a fairly lean team. Phil Morehouse is president of Fission 3.0. We kept a pretty lean mean machine in Fission 3.
Don’t forget, we’ve had up until just recently in the last six months, it’s been a very quiet company, there hasn’t been a lot of exploration activities in the uranium sector. I think as we start to ramp up, with our level of activity increasing, we’ll start to draw more and more people into roles and developing roles within the company as we begin to be active, get out and start marketing the story more, get on the ground and back that up with real results, we’re going to continue to build our team.
Maurice Jackson: Before we move on to your impressive technical team, in the natural resource basis, why is it wise to follow proven winners? Ross, you alluded to it earlier, you and CEO Dev Randhawa have a proven pedigree of success. How were shareholders rewarded as far as returns for their loyalty to sticking with your team?
Ross McElroy: Well, if you owned the original company at the beginning, which would’ve been Strathmore Minerals, and you’d held on it to all the way throughout, over the last 20 years since about 1996, 97, you’d probably own about five different companies right now.
What’s happened is we’ve moved on to a new phase, we’ve made discoveries, advanced projects, sold different projects to different groups. What we’ve been able to do is form new companies, split off new companies in what they call a butterfly transaction.
You have shares in the new company, still maintain your shares in the old company, so you would’ve received essentially what would look like dividends in the way of different shares for five different companies since that time. The shareholders that have been loyal and sticking with us would’ve succeeded quite handsomely all the way along.
Maurice Jackson: Your technical team is exceptional. I had an opportunity to meet them in the summer of 2016 at the site visit there. Please, introduce us to them.
Ross McElroy: We’re very, very proud of this group. This has been the team we’ve had, the same core group of people with us since 2010. With that same group, we were able to make our discovery on the Waterbury Lake project, and then followed up in 2012 with the discovery of PLS. It’s the same group that is very core and important to us in Fission 3.0.
I do head up the team and the technical group, so I would be the team leader or chief geologist for the technical team. My right hand guy is Raymond Ashley, he’s the VP of exploration. Ray is an excellent geoscientist who I’ve had the pleasure to work with for over 30 years in this sector, so we’ve been working pretty close together. Definitely a proven mine finder.
We’ve basically held the same group of people together on the project managers, all the structural scientists, geochemists. We’ve kept the same core group together over the last almost 10 years or so.
To me, that’s really the key. You want a team that works together well, good chemistry with each other, the ability and the environment to think outside of the box. Really, the goal for each and every one of us is to responsibly make world-class discoveries. That’s what we’re all about.
We’ve got an excellent team. All the key people are listed on the website. You’ll be able to go there and see the roles of the various groups there in the technical team, but there’s about seven or eight of us that have been able to be what I consider the core team for the last decade or so.
Maurice Jackson: Let’s get into some numbers. Please share your capital structure.

Ross McElroy: In Fission 3.0, we have 142 million shares outstanding. We were able to raise a significant amount. We have just under $7 million in the treasury right now, that’ll allow us to be active over the next two years or so.
Maurice Jackson: What is your burn rate?
Ross McElroy: The burn rate, because it’s exploration, it’s pretty discretionary spending. We have $7 million that we have in the treasury right now, that’ll certainly carry us over the next two to three years of pretty aggressive exploration spending on our key projects. We can dial that kind of number up, and we can dial it back as conditions warrant. That’s the benefit of being in exploration.
The burn rate is actually pretty minimal. In other words, we run a pretty lean shop as far as the number of management and corporate costs. Really, the majority of the costs are exploration spending, which is really entirely discretionary.
Maurice Jackson: How much debt do you have?
Ross McElroy: We have no debt. We’ve not taken on any debt. Basically, the money that we raise have been through equity share offerings. No debt in Fission 3.0.
Maurice Jackson: Who are your major shareholders? What is their level of commitment?
Ross McElroy: When we spun off Fission 3.0 back in December of 2014, it was the same shareholders that were shareholders of Fission Uranium, were the same shareholders in Fission 3.0. We would’ve had a lot of the same loyal, large shareholders, including JP Morgan, even investment from others that we’ve had along the way. It’s been the same loyal group.
We have significant new shareholders now with the financing that we did back in 2018, which was led by the Sprott Global Resources Group out of California. I think we have some new players back to the game, but we have a lot of shareholders that have been with us over the long haul.
These are people that have a good vision of the uranium sector. They know that the good times are around the corner. It’s a point that we believe really strongly, and we think that the sector is improving a great deal.
This is how our loyal shareholders are going to be rewarded, by being a much better market with an aggressive team like Fission 3.0, and the new shareholders will probably be long term loyal shareholders too if we’re successful and able to build value for them as well.
Maurice Jackson: What is the float?
Ross McElroy: Fully diluted, we have 227 million shares. We’ve got shares outstanding, we’ve got options and warrants that we’re a part of financing as well, so 227 million shares out in total. We trade around 240,000 shares a day, I think that’s our average volume.
Maurice Jackson: Multi-layered question. What is the next unanswered question for Fission 3.0? When can we expect a response? What determines success?
Ross McElroy: Well, we are going to be successful through work. We know that a better market should buoy the price up of everybody involved in the nuclear sector. They’re starting to get some life back in the exploration world.
Really, we’ve always built value by our success. We’ve been successful with making discoveries. We now have the money, we have the team, we’re putting them to work. I would look to us as being one of the most dynamic uranium explorers out there. That’s something that I think people can follow, they can see our news release cycle, they’ll see how we’re marketing our story, and just look at the results. I think they’ll speak for themselves.
We’re looking at our projects, we’ll be active throughout the calendar year. I think the news flow will be very strong and steady. People that are interested in following the company will always see that there’s a continuing narrative out there. We want to take advantage of this and improve the uranium market, the fact that we are well financed, and we have the properties that we want to explore. I think there’s a very good opportunity for readers to look at Fission 3.0 as a sector leader in the uranium exploration business.
Maurice Jackson: Mr. McElroy, last question. What did I forget to ask?
Ross McElroy: I think we’ve covered a lot of ground here, and a lot of important ground. One of the takeaways that I want readers to know is we really do believe in the nuclear sector. We think that we have turned the corner and that conditions are improving.
If people are looking to invest in the uranium sector, I think it’s important for them to look at a group that has done it before. Your track record is very indicative of what your future has the potential to look like. I always find myself, when I’m investing, I like to back teams with a proven track record.
We have that in our group. We’ve got an exceptional management team. We’ve done it before. We’ve been able to capitalize on our discoveries by selling assets. We have a unique technical team that has the ability to make discoveries.
So better sector, very good team. Strong management. Those are the ingredients we need to be successful.
Maurice Jackson: Ross, for someone listening that wants to get more information about Fission 3.0, please share the website address.
Ross McElroy: Our website address is www.fission3corp.com.
Maurice Jackson: For direct queries email ir@fission3corp.com, or you may call (778) 484-8030. Fission 3.0 trades on the TSX:V, symbol FUU, and on the OTC, symbol FISOF.
For audience, we’ve been proud shareholders of Fission 3.0 since 2014. Last but not least, please visit our website, provenandprobable.com, for mining insights and bullion sales. You may reach us at contact@provenandprobable.com.
Ross McElroy of Fission 3.0, thank you for joining us today on Proven and Probable.
Maurice Jackson is the founder of Proven and Probable, a site that aims to enrich its subscribers through education in precious metals and junior mining companies that will enrich the world.
Disclosure:
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TSX VENTURE SYMBOL: FUU
KELOWNA, BC, March 13, 2019 /CNW/ – Fission 3.0 Corp. (“Fission 3” or the “Company“) is pleased to announce that, further to its news release on August 16, 2018, it has entered into a binding agreement (the “Earn-In Agreement“) with Rhyolite Lithium Corp. (“Rhyolite“), pursuant to which Rhyolite can earn up to an 80% interest in Fission 3’s mining concessions located in Peru (the “Peruvian Assets“) by spending up to C$22 million over a five-year period (the “Earn-In“).
Pursuant to the Earn-In Agreement, Rhyolite is required to spend a minimum of C$5.5 million prior to December 31, 2020 to earn a 50% interest in the Peruvian Assets (“Stage One“), and has the option to spend a further C$16.5 million over the following three years to earn an additional 30% interest in the Peruvian Assets (“Stage Two“). If Rhyolite does not complete Stage One, Rhyolite will earn no interest in the Peruvian Assets, and if it elects to begin, but does not complete, Stage 2, it will only be granted a portion of the additional 30% interest.
In connection with the entrance into the Earn-In Agreement, and as consideration for the Earn-In, Fission 3 was issued 19.9% of the issued and outstanding shares of Rhyolite and was granted a right to participate, on a pro rata basis, in all future financings of Rhyolite to maintain its proportionate interest in Rhyolite.
Fission 3 will remain the operator of the Peruvian Assets until the completion of Stage One.
CEO Dev Randhawa commented,
“The Macusani area has shown strong potential for both uranium and lithium resources, as demonstrated by the recent results of operators in the nearby and surrounding area. We are pleased to partner with Rhyolite Lithium, which has strong financial backers with the equity needed to fund important work programs on the Macusani Project. We believe that by working with Rhyolite we will unlock value for Fission 3 shareholders.”
About Fission 3’s Macusani Project
Macusani, Peru, is an emerging uranium and lithium district in a mining-friendly jurisdiction. The area is host to multiple uranium deposits that are large scale, near-to-surface and potentially heap-leachable – giving them a strong economic case. The region also hosts several near-surface lithium occurrences associated with uranium mineralization in the Yapamayo Member formation as well as higher-grade lithium in the underlying Sapanuta Member formation.
Fission 3 holds titles to 9 concessions totaling 5,100 ha in the Macusani district. The property is surrounded by Plateau Energy Metals Inc.’s land package including the Falchani high-grade lithium discovery located less than 5km to the south. The Macusani concessions are easily accessed by a series of paved roads from the City of Puno to the town of Macusani, which connects to the Interoceanic Highway, a two-lane, paved highway that passes 14km north-east of the property.
About Fission 3.0 Corp.
Fission 3.0 Corp. is a Canadian based resource company specializing in the strategic acquisition, exploration and development of uranium properties and is headquartered in Kelowna, British Columbia. Common Shares are listed on the TSX Venture Exchange under the symbol “FUU.”
ON BEHALF OF THE BOARD
“Dev Randhawa”
Dev Randhawa, CEO
Fission 3.0 Corp.
Cautionary Statement: Fission 3.0 Corp.
Certain information contained in this press release constitutes “forward-looking information”, within the meaning of Canadian legislation. Generally, these forward-looking statements can be identified by the use of forward-looking terminology such as “plans”, “expects” or “does not expect”, “is expected”, “budget”, “scheduled”, “estimates”, “forecasts”, “intends”, “anticipates” or “does not anticipate”, or “believes”, or variations of such words and phrases or state that certain actions, events or results “may”, “could”, “would”, “might” or “will be taken”, “occur”, “be achieved” or “has the potential to”. Forward looking statements contained in this press release may include statements regarding the future operator of the Peruvian Assets, the characteristics, benefit, economics and mineralization of the Macusani region, the benefits of the earn-in agreement to Fission 3 shareholders and future operating or financial performance of Fission 3.0 Corp. which involve known and unknown risks and uncertainties which may not prove to be accurate. Actual results and outcomes may differ materially from what is expressed or forecasted in these forward-looking statements. Such statements are qualified in their entirety by the inherent risks and uncertainties surrounding future expectations. Among those factors which could cause actual results to differ materially are the following: Fission 3’s performance as operator of the Peruvian Assets, the Macusani region having different characteristics, economics or mineralization than currently expected, Rhyolite’s decision to fund expenditures on the Macusani Project pursuant to the Earn-In Agreement, market conditions and other risk factors listed from time to time in our reports filed with Canadian securities regulators on SEDAR at www.sedar.com. The forward-looking statements included in this press release are made as of the date of this press release and Fission 3.0 Corp. disclaim any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as expressly required by applicable securities legislation.
Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
SOURCE Fission 3.0 Corp.
Results Highlights
Ross McElroy, President, COO, and Chief Geologist for Fission, commented,
“We are very pleased with the results and current progress of the winter program at PLS. These drill holes accomplished the goals set out with respect to intersecting mineralization within the modeled high-grade domain and overall look to have expanded beyond the modeled domain. These important results highlight the potential for growth as the R780E zone is further delineated.”
Table 1: R780E Zone
| Hole ID | Zone | Collar | Hand-held Scintillometer Results On Mineralized Drillcore (>300 cps / >0.5M minimum) |
Lake Depth (m) |
Sandstone From – To (m) |
Basement Unconformity Depth (m) |
Total Drillhole Depth (m) |
|||||
| Grid Line | Az | Dip | From (m) | To (m) | Width (m) | CPS Peak Range | ||||||
| PLS19-PW-08 | R780E | 615E | 329 | – 70.9 | 121.0 | 146.5 | 25.5 | <300 – 15600 | 7.4 | NA | 62.0 | 407.0 |
| 151.5 | 157.0 | 5.5 | <300 – 15500 | |||||||||
| 162.0 | 165.5 | 3.5 | <300 – 8800 | |||||||||
| 178.0 | 179.5 | 1.5 | <300 – 410 | |||||||||
| 195.5 | 198.5 | 3.0 | <300 – 3600 | |||||||||
| 201.5 | 210.5 | 9.0 | <300 – 15700 | |||||||||
| 213.0 | 227.5 | 14.5 | <300 – 23600 | |||||||||
| 230.0 | 238.5 | 8.5 | <300 – 1200 | |||||||||
| 243.5 | 244.0 | 0.5 | 300 | |||||||||
| PLS19-PW-09 | R780E | 735E | 334 | – 68.5 | 130.0 | 130.5 | 0.5 | 400 | 7.4 | NA | 61.9 | 335.9 |
| 141.0 | 178.5 | 37.5 | <300 – 61115 | |||||||||
| 198.5 | 199.0 | 0.5 | 1200 | |||||||||
| 201.5 | 204.0 | 2.5 | 500 – 18100 | |||||||||
| PLS19-PW-10 | R780E | 990E | 330 | -71.2 | 108.0 | 109.5 | 1.5 | 400 – 2800 | 7.9 | NA | 65.6 | 372.5 |
| 129.5 | 131.0 | 1.5 | 320 – 530 | |||||||||
| 145.5 | 146.0 | 0.5 | 340 | |||||||||
| 149.0 | 149.5 | 0.5 | 480 | |||||||||
| 172.0 | 191.0 | 19.0 | <300 – 58300 | |||||||||
| 200.5 | 201.0 | 0.5 | 360 | |||||||||
| 210.5 | 215.0 | 4.5 | <300 -1000 | |||||||||
| 224.5 | 241.5 | 17.0 | <300 – 7100 | |||||||||
| 291.5 | 292.0 | 0.5 | 490 | |||||||||
| 313.5 | 315.5 | 2.0 | 500 – 30400 | |||||||||
Natural gamma radiation in drill core that is reported in this news release was measured in counts per second (cps) using a hand-held RS-121 Scintillometer manufactured by Radiation Solutions, which is capable of discriminating readings up to 65,535 cps. Natural gamma radiation in the drill hole survey that is reported in this news release was measured in counts per second (cps) using a Mount Sopris 2GHF-1000 Triple Gamma probe, which allows for more accurate measurements in high grade mineralized zones. The Triple Gamma probe is preferred in zones of high-grade mineralization. The reader is cautioned that scintillometer readings are not directly or uniformly related to uranium grades of the rock sample measured, and should be used only as a preliminary indication of the presence of radioactive materials. The degree of radioactivity within the mineralized intervals is highly variable and associated with visible pitchblende mineralization. All intersections are down-hole. All depths reported of core interval measurements including radioactivity and mineralization intervals widths are not always representative of true thickness. The orientation of the mineralized intervals tend to follow that of lithologic contacts, and generally dip steeply to the south. Within the Triple R deposit, individual zone wireframe models constructed from assay data and used in the resource estimate indicate that all 5 zones have a complex geometry controlled by and parallel to steeply south-dipping lithological boundaries as well as a preferential sub-horizontal orientation.
Samples from the drill core will be split in half sections on site and where possible, samples will be standardized at 0.5m down-hole intervals. One-half of the split sample will be sent to SRC Geoanalytical Laboratories (an SCC ISO/IEC 17025: 2005 Accredited Facility) in Saskatoon, SK for analysis which includes U3O8 (wt %) and fire assay for gold, while the other half remains on site for reference. All analysis includes a 63 element ICP-OES, uranium by fluorimetry and boron.
Further technical details
PLS19-PW-08 (line 615E)
PLS19-PW-08 targeted a low-grade gap between the middle and eastern R780E high-grade core models, and aimed to identify new high-grade mineralization outside of the current resource model. Moderate to strong radioactivity was intersected in the gap zone beginning at 121.0m down hole, returning a 25.5m wide main interval which included 0.7 m >10,000 counts per second (cps) on RS-121 handheld scintillometer. These results represent the strongest radioactivity on line 615E to date. Based on the current high-grade core model an interval of strong radioactivity was expected at approximately 140.0 m down hole which, as noted above, was instead intersected 19m higher up in the hole. A second zone of strong radioactivity was expected at approximately 152.0m which was successfully intersected and correlates well with the high-grade core model.
PLS19-PW-09 (line 735E)
PLS19-PW-09 targeted a large jog in the eastern high-grade core model where the high-grade core was interpreted to extend. A 37.5m wide zone of strong uranium mineralization was intersected, beginning at 141.0m down hole with a near continuous 3.72m interval of >10,000 cps occurring in the jog outside of the current high-grade core model. Based on the current high-grade core model the potential existed for a thin zone of strong radioactivity between 145m to 148m down hole. The hole actually intersected a 37.5m mineralized zone between 141m to 178.5m.
PLS19-PW-10 (line 990E)
PLS19-PW-10 targeted the interpreted extension of the R780E high-grade core approximately 120m east of the current high-grade resource. A 19m wide zone of strong uranium mineralization was intersected beginning at a depth of 172m with a total of 3.78 m >10,000 cps. No high-grade core model exists in the vicinity of PLS19-PW-10 but two vertical drill holes PLS14-180 (5.5m averaging 18.56% U3O8) and PLS14-158 (5.0m averaging 8.57% U3O8) are located approximately 4m and 8m to the east, respectively. The location of the strong radioactivity in PLS19-PW-10 correlates well with strong radioactivity in drill holes PLS14-180 and 158 and suggests potential exists to define additional high-grade domains east of the currently defined high-grade core.
PLS Mineralized Trend & Triple R Deposit Summary
Uranium mineralization of the Triple R deposit at PLS occurs within the Patterson Lake Conductive Corridor and has been traced by core drilling over ~3.18km of east-west strike length in five separated mineralized “zones” which collectively make up the Triple R deposit. From west to east, these zones are: R1515W, R840W, R00E, R780E and R1620E. Through successful exploration programs completed to date, Triple R has evolved into a large, near surface, basement hosted, structurally controlled high-grade uranium deposit. The discovery hole was announced on November 05, 2012 with drill hole PLS12-022, from what is now referred to as the R00E zone.
The R1515W, R840W and R00E zones make up the western region of the Triple R deposit and are located on land, where overburden thickness is generally between 55m to 100m. R1515W is the western-most of the zones and is drill defined to ~90m in strike-length, ~68m across strike and ~220m vertical and where mineralization remains open in several directions. R840W is located ~515m to the east along strike of R1515W and has a drill defined strike length of ~430m. R00E is located ~485m to the east along strike of R840W and is drill defined to ~115m in strike length. The R780E zone and R1620E zones make up the eastern region of the Triple R deposit. Both zones are located beneath Patterson Lake where water depth is generally less than six metres and overburden thickness is generally about 50m. R780E is located ~225m to the east of R00E and has a drill defined strike length of ~945m. R1620E is located ~210m along strike to the east of R780E, and is drill defined to ~185m in strike length.
Mineralization along the Patterson Lake Corridor trend remains prospective along strike in both the western and eastern directions. Basement rocks within the mineralized trend are identified primarily as mafic volcanic rocks with varying degrees of alteration. Mineralization is both located within and associated with mafic volcanic intrusives with varying degrees of silicification, metasomatic mineral assemblages and hydrothermal graphite. The graphitic sequences are associated with the PL-3B basement Electro-Magnetic (EM) conductor.
Patterson Lake South Property
The 31,039 hectare PLS project is 100% owned and operated by Fission Uranium Corp. PLS is accessible by road with primary access from all-weather Highway 955, which runs north to the former Cluff Lake mine and passes through the nearby UEX-Areva Shea Creek discoveries located 50km to the north, currently under active exploration and development.
The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and reviewed on behalf of the company by Ross McElroy, P.Geol., President and COO for Fission Uranium Corp., a qualified person.
About Fission Uranium Corp.
Fission Uranium Corp. is a Canadian based resource company specializing in the strategic exploration and development of the Patterson Lake South uranium property – host to the class-leading Triple R uranium deposit – and is headquartered in Kelowna, British Columbia. Fission’s common shares are listed on the TSX Exchange under the symbol “FCU” and trade on the OTCQX marketplace in the U.S. under the symbol “FCUUF.”
ON BEHALF OF THE BOARD
“Ross McElroy”
Ross McElroy, President and COO
Cautionary Statement:
Certain information contained in this press release constitutes “forward-looking information”, within the meaning of Canadian legislation. Generally, these forward-looking statements can be identified by the use of forward-looking terminology such as “plans”, “expects” or “does not expect”, “is expected”, “budget”, “scheduled”, “estimates”, “forecasts”, “intends”, “anticipates” or “does not anticipate”, or “believes”, or variations of such words and phrases or state that certain actions, events or results “may”, “could”, “would”, “might” or “will be taken”, “occur”, “be achieved” or “has the potential to”. Forward looking statements contained in this press release may include statements regarding the future operating or financial performance of Fission and Fission Uranium which involve known and unknown risks and uncertainties which may not prove to be accurate. Actual results and outcomes may differ materially from what is expressed or forecasted in these forward-looking statements. Such statements are qualified in their entirety by the inherent risks and uncertainties surrounding future expectations. Among those factors which could cause actual results to differ materially are the following: market conditions and other risk factors listed from time to time in our reports filed with Canadian securities regulators on SEDAR at www.sedar.com. The forward-looking statements included in this press release are made as of the date of this press release and the Company and Fission Uranium disclaim any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as expressly required by applicable securities legislation.
SOURCE Fission Uranium Corp.
March 4, 2019
Vancouver, British Columbia, March 4, 2019 (TSX Venture: EMX; NYSE American: EMX) – EMX Royalty Corporation (the “Company” or “EMX”) is pleased to announce the execution of an exploration and option agreement (the “Agreement”) for the Røstvangen volcanogenic massive sulfide (“VMS”) property and Vakkerlien nickel-copper-cobalt property in Norway (collectively the “Project”) with Playfair Mining Ltd. (“Playfair”) (TSX Venture: PLY). The Agreement provides EMX with immediate share equity in Playfair, and upon Playfair’s completion of the option terms and other consideration, a 9.9% interest in Playfair, a 3% net smelter return (“NSR”) royalty on the Project, and advance royalty payments.
The Røstvangen property hosts a >30 kilometer long trend of geophysical anomalies and VMS-type mineralization, as well as the Kvikne copper deposits, that occur in one of Norway’s oldest mining districts. On the directly adjoining Vakkerlien property, nickel mineralization was discovered in the 1870s, and was the subject of drill campaigns from the 1970s through the early 2000s that led to the discovery of nickel-copper-cobalt mineralization.
Commercial Terms Overview. Pursuant to the Agreement, Playfair can earn 100% interest in the Project by the issuance of shares to EMX and performance of work during the one-year option period, as described below (all dollar amounts in CDN):
Upon exercise of the option, Playfair will issue to EMX an additional 3 million shares of Playfair stock, and EMX will receive a 3% NSR royalty on the properties comprising the Project. Within six years of the execution of the Agreement, Playfair may purchase 1% of the NSR royalty in 0.5% increments for a total of $3,000,000, leaving EMX with a 2.0% NSR royalty. EMX will also receive annual advance royalty (“AAR”) payments of $30,000 commencing on the second anniversary of the option exercise, with the AAR payments increasing by $5,000 per year until reaching $80,000 per year. AARs may be paid in cash or Playfair shares, subject to certain conditions.
After the exercise of the option, further conditions of the Agreement include:
The issuance of Playfair shares to EMX as set forth in the Agreement is subject to receipt of TSX Venture Exchange approval.
Overview of Project. The Røstvangen property is located approximately 300 kilometers north of Oslo, and hosts the “Kvikne Copper Works”, one of Norway’s oldest base metal mining districts. Copper mineralization was discovered at Kvikne in 1629, followed by 150 years of mineral production. The mineralization at Kvikne is VMS-type, with enrichments of copper and gold. The Kvikne deposits are positioned along a >30 kilometer long trend of geophysical anomalies and VMS-type mineral occurrences that form multiple parallel belts across the property. These belts have seen little modern exploration work, and only a few historic drill holes, despite the widespread VMS occurrences and historic mining activities.
The Vakkerlien nickel-copper-cobalt property directly adjoins the Røstvangen exploration licenses. Nickel was discovered on the property in the 1870s, when small scale mining was conducted in the district. Further exploration by Falconbridge Limited and Blackstone Ventures Inc. from 1975 through the early 2000s led to the drilling and discovery of nickel-copper-cobalt mineralization to the southeast of the historic workings. The mineralization is associated with, and hosted by, a mid-Proterozoic gabbroic intrusive complex, and is interpreted to be a magmatic sulfide deposit type. Gold and platinum group element (“PGE”) content remains poorly understood and in need of further assessment.
EMX and Playfair are planning to commence exploration programs in the upcoming spring and summer months, which will include property-scale sampling, reconnaissance mapping and geophysical surveys. The intent of the programs is to rapidly identify additional exploration targets for drill testing.
Dr. Eric P. Jensen, CPG, a Qualified Person as defined by National Instrument 43-101 and employee of the Company, has reviewed, verified and approved the disclosure of the technical information contained in this news release.
About EMX. EMX leverages asset ownership and exploration insight into partnerships that advance our mineral properties, with EMX receiving pre-production payments and retaining royalty interests. EMX complements its royalty generation initiatives with royalty acquisitions and strategic investments. Please see www.EMXroyalty.com for more information.
-30-
For further information contact:
David M. Cole
President and Chief Executive Officer
Phone: (303) 979-6666
Email: Dave@EMXroyalty.com
Scott Close
Director of Investor Relations
Phone: (303) 973-8585
Email:SClose@EMXroyalty.com
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
Forward-Looking Statements
This news release may contain “forward looking statements” that reflect the Company’s current expectations and projections about its future results. These forward-looking statements may include statements regarding perceived merits of properties, exploration results and budgets, mineral reserves and resource estimates, work programs, capital expenditures, timelines, strategic plans, market prices for precious and base metal, or other statements that are not statements of fact. When used in this news release, words such as “estimate,” “intend,” “expect,” “anticipate,” “will”, “believe”, “potential” and similar expressions are intended to identify forward-looking statements, which, by their very nature, are not guarantees of the Company’s future operational or financial performance, and are subject to risks and uncertainties and other factors that could cause the Company’s actual results, performance, prospects or opportunities to differ materially from those expressed in, or implied by, these forward-looking statements. These risks, uncertainties and factors may include, but are not limited to: unavailability of financing, failure to identify commercially viable mineral reserves, fluctuations in the market valuation for commodities, difficulties in obtaining required approvals for the development of a mineral project, increased regulatory compliance costs, expectations of project funding by joint venture partners and other factors.
Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this news release or as of the date otherwise specifically indicated herein. Due to risks and uncertainties, including the risks and uncertainties identified in this news release, and other risk factors and forward-looking statements listed in the Company’s MD&A for the nine month period that ended on September 30, 2018 (the “MD&A”), and the most recently filed Form 20-F for the year that ended on December 31, 2017, actual events may differ materially from current expectations. More information about the Company, including the MD&A, the 20-F and financial statements of the Company, is available on SEDAR at www.sedar.com and on the SEC’s EDGAR website at www.sec.gov.

In this action packed interview, Bob Moriarty the founder of 321gold and 321energy.com sits down with Maurice Jackson of Proven and Probable to discuss current events, companies that have your attention, and to discuss Amazon’s best-selling book right now, under Commodities Trading, which happens to be your book aptly entitled: “Basic Investing In Resource Stocks, the Idiot’s Guide”.
https://soundcloud.com/proven-and-probable/bob-feb-2019
Original Source: https://www.streetwisereports.com/article/2019/03/03/bob-moriarty-on-geopolitics-resource-companies-and-his-new-book.html
Source: Maurice Jackson for Streetwise Reports (3/3/19)

Bob Moriarty of 321 Gold sits down with Maurice Jackson of Proven and Probable and sounds off about the state of the world, resource companies he is paying attention to, and what readers will find in his new book.


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