Skyharbour Resources Ltd. is a uranium and precious metal exploration company actively involved with the development of projects in one of the most active uranium exploration regions in the world, the Athabasca Basin, Saskatchewan.

The Company now owns a 100% interest in approximately 400,000 total acres of land between seven properties in the Athabasca Basin region in northern Saskatchewan. Six of the properties consisting of approximately 388,000 acres of prospective ground are strategically located near the Alpha Minerals (TSX-V: AMW) and Fission Energy (TSX-V: FIS) Patterson Lake South (PLS) uranium discovery area. The properties were acquired for their proximity to the PLS discovery and interpreted favourable geology for the occurrence of PLS style uranium mineralization. Skyharbour's land position is now one of the largest in the Patterson Lake area. The Athabasca Basin hosts the world's largest and richest high-grade uranium deposits accounting for approximately 20% of global primary uranium supply. There are still many areas in the region that are highly prospective and underexplored as illustrated by the new high-grade uranium discovery at the Patterson Lake South property.

The Patterson Lake area has received escalating exploration attention and claim acquisition activity as a result of the new, shallow discovery made by Alpha and Fission which includes the recently reported drill interval of 4.92% U3O8 over 34 metres in hole PLS13-038 (see Alpha / Fission News Release dated March 25). This mineralized zone is located approximately 400 metres to the northeast of discovery hole PLS12-024 which returned 2.49% U3O8 over 12.5 metres. These discoveries demonstrate the potential for high-grade uranium mineralization on the margins of the western side of the Athabasca Basin where significantly less exploration has been carried out compared to the eastern side of the Athabasca Basin With this significant land package, the Company is well positioned in this emerging area to the north, south and east of the recent high grade uranium discovery at the Patterson Lake South property. Other regional operators in the area include Cameco Corp., Areva, and Denison Mines.

Given the excellent supply-demand fundamentals underpinning uranium, Skyharbour intends to build upon its portfolio of uranium projects in the Athabasca Basin as well as in other prolific uranium districts.

Donald C. Huston
Position: Director, President and Chief Executive Officer

Don Huston is the President and Chief Executive Officer of Skyharbour Resources Ltd. He has been associated with the mineral exploration industry for over 25 years and has extensive experience as a financier and in-field manager of numerous mineral exploration projects in North America. He was born and raised in Red Lake, Ontario and spent 15 years as a geophysical contractor with C.D. Huston & Sons Ltd. as mineral exploration consultants in northern Ontario, Manitoba, and Saskatchewan. Mr. Huston serves as a Director of 5 Canadian public resource companies.

Amanda Chow, CMA
Position: Director

Amanda Chow serves as an independent Director of Skyharbour Resources Ltd. Ms. Chow is a Certified Management Accountant (CMA) and a graduate of Simon Fraser University where she earned her Bachelor of Business Administration degree. She began working with public companies in 1999.

James G. Pettit
Position: Director

Jim Pettit is a Director of Skyharbour Resources Ltd. Mr. Pettit is currently serving as a Director on the Boards of 6 public resource companies and offers 15 years experience within the industry specializing in finance, corporate governance, management, and compliance. He specializes in the early stage development of private, as well as public companies. His background over the past 15 years has been focused primarily within the resource sector where he has managed and directed junior resource companies through good times and bad.

Donald G. Myers
Position: Director

Don Myers serves as a Director of Skyharbour Resources Ltd. He has over twenty years of experience in public company management and corporate communications working with companies listed on the TSX Venture, NASDAQ, and Toronto Stock Exchanges. Mr. Myers background includes holding the position of Director and Officer of several junior public companies listed on the TSX Venture Exchange.

Nancy Ackerfeldt
Position: Corporate Secretary

Nancy Ackerfeldt has over twenty years of experience in public company administration and compliance, working primarily with junior public companies listed on the TSX Venture Exchange. From August 1995 to date, Ms. Ackerfeldt has been employed with 98 Corporate Group Resources Ltd., a private management and administrative services company which provides office space, accounting, legal, secretarial and support services to public companies.

Robert Marvin, P.Geo., CPG
Position: Exploration Manager and Qualified Person

Bob Marvin, P.Geo, CPG, Senior Project Geologist. Mr. Marvin has been involved in mineral exploration for and evaluation of gold, copper, zinc, and uranium deposits throughout the Americas as an employee and as an independent consultant. He graduated from the University of New Mexico with a Bachelor of Science degree in geology in 1984. Mr. Marvin is the Exploration Manager of the Company's operations.

Richard Kusmirski, P.Geo, M.Sc.
Position: Head of Advisory Board

Rick Kusmirski, P.Geo, M.Sc., Head of Advisory Board, has over 40 years of exploration experience in North America and overseas, and has actively participated in the discovery of a number of uranium, gold and base metal deposits. For several years, in his capacity as Exploration Manager, he directed Cameco Corporation's (TSX: CCO) uranium exploration projects in the Athabasca Basin. In 1999, Rick joined JNR Resources becoming Vice President of Exploration in 2000. Subsequently, he directed the exploration program that led to the discovery of the Maverick Zone on the Moore Lake uranium joint venture in the Athabasca Basin in Saskatchewan with partner Kennecott Canada. Rick became JNR's President and CEO in January of 2001. In February of 2013, Denison Mines Corp. (TSX: DML) successfully acquired all of the outstanding shares of JNR by way of a friendly all-share take-over bid.

Skyharbour Resources has acquired six uranium properties in the Patterson Lake region totaling 388,000 acres, making it one of the largest land positions in the area. Two of these properties, North Patterson and RY, are strategically located approximately 27 km and 35 km respectively to the north of Alpha Minerals (TSX-V: AMW) and Fission Energy (TSX-V: FIS) Patterson Lake South discovery area claim boundary and cover prospective geology within the Athabasca Basin sandstones including NE-SW regional structural trends.

Six of the properties consisting of approximately 388,000 acres of prospective ground are strategically located near the Alpha Minerals (TSX-V: AMW; "Alpha") and Fission Energy (TSX-V: FIS; "Fission") Patterson Lake South (PLS) uranium discovery area. The properties were acquired for their proximity to the PLS discovery and interpreted favourable geology for the occurrence of PLS style uranium mineralization. Skyharbour's land position is now one of the largest in the Patterson Lake area. The Athabasca Basin hosts the world's largest and richest high-grade uranium deposits accounting for approximately 20% of global primary uranium supply. There are still many areas in the region that are highly prospective and underexplored as illustrated by the new high-grade uranium discovery at the Patterson Lake South property.

Recent acquisition includes additional ground tied onto the Company's South Patterson Property located approximately 15 km to the south of Fission / Alpha's Patterson Lake South project claim boundary. The claims are accessible by road with primary access from the all-weather Highway 955, which runs north through the Patterson Lake South discovery to the former Cluff Lake mine where over 60 million pounds of uranium was produced. The highway also passes through the UEX-Areva Shea Creek discoveries to the north which are currently under active exploration and development. Skyharbour's newly acquired sixth property in the Patterson Lake area, the West Patterson Property, is located approximately 18 km to the southwest of Fission / Alpha's Patterson Lake South project claim boundary. This property is on strike with the W-SW to E-NE mineralized trend being delineated at the PLS uranium discovery zones. Other regional operators in the area include Cameco Corp., Areva, and Denison Mines.

The Patterson Lake area has received escalating exploration attention and claim acquisition activity as a result of the new, shallow discovery made by Alpha and Fission which includes the recently reported drill interval of 4.92% U3O8 over 34 metres in hole PLS13-038 (see Alpha / Fission News Release dated March 25). This mineralized zone is located approximately 400 metres to the northeast of discovery hole PLS12-024 which returned 2.49% U3O8 over 12.5 metres. These discoveries demonstrate the potential for high-grade uranium mineralization on the margins of the western side of the Athabasca Basin where significantly less exploration has been carried out compared to the eastern side of the Athabasca Basin.

Skyharbour has acquired its entire land package at acquisition cost plus the issuance of one million common shares of the Company at a deemed price of six cents per share. The share issuance is subject to the acceptance of the TSX Venture Exchange. Roughly 115,000 acres of the total land position was staked directly by the Company while the other approximately 285,000 acres were staked by an arms-length party and are subject to a 2% NSR.

With roughly $900,000 in the treasury, Skyharbour will now examine and compile all available historic and related mineral exploration data associated with the acquired properties in anticipation of uranium exploration work programs this year. Given the excellent supply-demand fundamentals underpinning uranium, Skyharbour will continue to evaluate uranium projects for potential acquisition in the Athabasca Basin as well as in other prolific uranium districts.

Uranium mineralization is associated with granitic plutons, stocks, pegmatites and other felsic gneiss of the Archean basement rocks of the Athabasca Basin in this region. The uranium is trapped in both pre-Paleozoic sandstones and carbonaceous units of the Manitiou Falls Formation (like Cigar Lake on the Eastern Flank of the Basin) and within younger Cretaceous age silty sandstones within and on the flanks of the Basin (like the high grade Patterson Lake South uranium discovery). Skyharbour has at least two target types on its recently acquired land in the Patterson Lake region including pegmatite hosted uranium as well as silty sandstone hosted mineralization in the McMurray formation.

Uranium is a very dense metal, which can be used as an abundant source of concentrated energy. On a scale arranged according to the increasing mass of their nuclei, uranium is the heaviest of all the naturally occurring elements (hydrogen is the lightest).

Uranium has various military and civilian uses. The largest significant commercial usage of uranium is in nuclear power reactors, but it also has usage in the construction industry, medical appliances and medicine, and even agriculture.

The Uranium (U3O8) deposits of Saskatchewan, Canada are arguably the richest in the world.

The Athabasca Basin is an ancient sedimentary basin which hosts the World's most significant uranium mines and produces almost 30% per cent of the current world uranium production of 108 million pounds U3O8. Athabasca uranium deposits also have grades substantially higher than the world average grade of about 0.2% U3O8. The two dozen or so known uranium deposits within the Athabasca Basin have average grades of more than 3.0% U3O8. The two largest deposits, Cigar Lake and McArthur River have average grades of 20% and 24% U3O8 respectively. The near surface uranium mines in the Cluff Lake mine area produced more than 60 million pounds of uranium with gold as a by-product.

The Athabasca Basin is host to unconformity-associated type Uranium deposits. Mineralization occurs at, above or below the unconformity which separates the Proterozoic Athabasca Sandstone Group from the underlying metamorphosed gneissic rock. Uranium mineralization within the Athabasca Basin is primarily hosted by meta-sediments including pelites and calc-silicates and by sandstone of the Athabasca formation. The pelites are commonly graphitic (free carbon) which may have acted as a chemical reductant, fixing uranium from water circulated by large hydrothermal systems. Some Athabasca uranium deposits are associated with faults and these faults may cause displacements of the basal unconformity.

In the eastern portion of the Athabasca Basin (underlain by the basement zone called the Wollaston Domain), there are two types of uranium deposits found - one which has uranium, nickel, cobalt and arsenic (Polymetallic) and a second which is primarily uranium (Monometallic). The Polymetallic deposits have a high grade core which lies just below the unconformity and a lower grade envelope which can extend well up into the Athabasca sediments. The Monometallic deposits lie completely within the basement along faults within graphitic gneiss. The characteristics of the deposition of these deposits provide exploration tools in the search for other deposits - for Polymetallic deposits the presence of the other metals and large alteration zones which can extend to or near the Athabasca surface and for Monometallic deposits the presence of faults and graphite. Typically the alteration increases as the deposit is approached.

The three primary characteristics sought today by explorers in the Athabasca Basin are:
1.  The target area of the Athabasca sandstone/basement contact.
2.  There should be graphitic rocks.
3.  There should be clay alteration in the upper basement or lower Athabasca sediments.

Skyharbour's 11,769 acre Wheeler Project is located in the Eastern Flank of the Athabasca Basin and has three uranium showings on the property. Initially, a northeast-trending train of radioactive boulders was located which was traced to the source mineralized outcrop. Grab sample assay values range from 10 ppm to 0.495% U3O8. The mineralization is contemporaneous with the formation of the pegmatoid rocks and uranium mineralization is scattered uraninite grains enclosed in fresh and weakly altered biotite, quartz and feldspar.

The Wheeler project has two obvious targets for immediate exploration. First, the known, outcropping, pegmatite hosted uranium mineralization mentioned above, and second, Cigar Lake style uranium mineralization hosted at the regional, unconformable contact between the Archean age pegmatites and overlying basin fill sedimentary units.

Skyharbour Resources Ltd. has a 20% interest in the 5,100-acre McKenzie Island Property with Cypress Development Corp. owning the other 80%. This property is located to the west and adjacent to Goldcorp’s Cochenour / Bruce Channel Deposit. The McKenzie Island property is also on strike with the Goldcorp (TSX: G) Red Lake and Campbell mines seven kilometres to the east.

In addition to the Bruce Channel deposit, the Western Discovery Zone is yet another gold zone that has been found on Goldcorp's Cochenour / Bruce Channel Deposit property and is located on the western side of the property close to Skyharbour's McKenzie Island project. This zone has a strike length of over one kilometre in an east-west direction and has a width of 350 metres from north to south. The Cypress Development / Skyharbour Resources joint venture is of the opinion that there is potential for the extension of the Western Discovery Zone onto the McKenzie Island property.

Past Exploration and Drilling Completed on the McKenzie Island Property

An initial exploration program was completed on the property in 2002 by Skyharbour. This program consisted of data compilation, mapping, and geochemical and geophysical testing. This identified the highly prospective McAndrew gold / alteration trend extending across the centre of Skyharbour's McKenzie Island property - a comparable geological environment to the McKenzie Island Mine which historically produced 650,000 ounces of gold. As a result of this initial exploration phase, a first phase of drilling consisting of 13 holes totaling 6,828 feet (2,100 metres) to test targets identified during the 2002 exploration program was completed. In addition, overburden drilling totaling 2,990 feet tested the basal till at 133 sites in two areas on the property to identify new targets. Gold values were encountered along the McAndrew Trend on McKenzie Island as well as along the contact between the volcanics and sediments on the north part of McKenzie Island.

In May of 2004, the Company added an integral claim block to its existing land package. This acreage is situated in the middle of the held ground and now allows the Company to continue to follow another mile strike length of the known McAndrew geological trend.

In early 2005, 14 reconnaissance holes (approximately 3,300 metres) were also completed during Phase I and Phase II (February and April of 2005) diamond drill programs on the St. Paul's Bay region on the southern most portion of the McKenzie Island property to explore a district-scale W-NW trending structure known as the "D2" Structure.

Significant zones of gold mineralization were discovered. The new zones were located in diamond drill holes M05-3 through to M05-7. In reconnaissance drill hole M05-3, visible gold was identified within several centimetre-scale quartz veinlets with sample results showing numerous multi-gram intercepts with a high value of 23.8 g/t gold over 0.2 metres. In reconnaissance drill hole M05-4, highly anomalous gold values up to 850 ppb were intercepted over 60 metres. In reconnaissance drill hole M05-7, a 10-metre wide zone of gold mineralization was intersected in a zone hosted by quartz-sulfide veining and silica flooding within a strongly sericite altered felsic intrusive.

All of the intercepted zones of gold mineralization lie within a large (1000+ metres by 150+ metres) envelope of quartz-sericite-chlorite alteration, which appears to be controlled by a district-scale, W-NW trending D2 deformation zone. The strike length of the altered system has not been limited by the 2005 drill programs. The Company is encouraged with the results of the 2005 Phase I & II drill programs on the south portion of its McKenzie Island property.

Drill testing of 2 prospective target areas on the eastern portion of the Skyharbour's McKenzie Island claim group, adjacent to Goldcorp's Cochenour / Bruce Channel property, were completed in the winter of 2006. Three diamond drill holes were completed in areas where a significant angular unconformity has been projected. This unconformity appears to exert a strong regional influence on gold deposition including past gold produced from the McKenzie Red Lake Gold Mine and the Gold Eagle Mine east of Skyharbour's property. The geologic corridor flanking this known unconformity is considered to be very prospective for gold deposition in the Red Lake gold camp.

Skyharbour Resources Ltd. has a 24.5% interest in the Baird Property with Bayfield Ventures Corp. (TSX.V: BYV) (24.5%) interest, and Goldcorp (TSX: G) now owns the remaining (51%) interest. The Baird property lies in the central Red Lake gold belt adjacent to the Claude Resources property on the south, to the Goldcorp Parvus Project on the north and east, and to Goldcorp's Humlin property on the west. The Baird property is six kilometres north of the Madsen Mine and fourteen kilometres southwest of the Goldcorp Red Lake Mine.

The property lies within the highly prospective Balmer assemblage volcanic rocks and exhibits structural and alteration systems typical of the Goldcorp Red Lake and Campbell mines. Drilling in the 1980's by United Reef on Baird returned assay values of 172 g/t gold over 1.2 metres and 19 g/t gold over 1.8 metres. These showings were the focus of Skyharbour's initial drill program. The intent was to gain a greater understanding of the geologic setting where these historical grades were present.

Skyharbour completed a 1,600 metre drill program on the Baird Property in the summer of 2002 with gold intersections of up to 10 g/t gold over 1.0 metre encountered in what is known as the North Shear Zone. The 2002 drill program also identified a potential South Shear Zone. The results from Skyharbour's 2002 drill program were the catalyst needed to convince Placer Dome to option the Baird Property and initiate a major drill program. Placer Dome funded 7,043 metres of drilling in 3 drill programs, which has identified a large fold structure which contains the shear zones in it.

The goal of this extensive drill program was to identify and confirm the existence of this major structural hinge (fold) feature that contained within it the North Shear Zone and the South Shear Zone. A Structure of this type is of major significance to the discovery of gold in the Red Lake camp.

Placer Dome earned their 51% interest in the property, which Goldcorp acquired and became the operator. The 3 drill programs were carried out with the guidance and assistance of Placer Dome, which operated the high-grade Campbell Gold Mine in Red Lake. For a three year period following the formation of this 51% / 49% (Skyharbour / Bayfield) joint venture, Goldcorp will have the right to increase its interest to 65% by electing to complete a feasibility study. Should either party elect not to participate in an approved program following the formation of the joint venture, the interest of the non-participating party will be subject to dilution based on a standard formula. Should either party dilute to a 10% interest, its interest will automatically convert to a 1% NSR, half of which can be purchased at any time for $1 million.

Skyharbour Resources holds a 100% interest in 3,200 acres of land that includes the former Selco South Bay copper-zinc-silver mine.  The South Bay property is located in the Dent, Mitchell, and Agnew Townships, 80 kilometres east-northeast of Red Lake in northwestern Ontario.

The former South Bay Mine, located on the Company's 123498 claim block, produced approximately 1.6 million tons of 2.3% copper, 14.5% zinc, and 3.5 oz/ton silver to a vertical depth of 410 metres, and explored to a vertical depth of 600 metres, between 1970 and 1982. The South Bay deposit is a classic Archean Volcanic associated Massive Sulfide (VMS) deposit that is hosted in an area known as the Confederation Belt.

Skyharbour Resources believes that with current geophysical survey methods allowing exploration to depths in excess of 1,000 metres, there is significant potential to identify new, highly prospective precious and base metal settings on the South Bay property.

In preparation for a drill program, Skyharbour Resources completed a Quantec "Titan-24" geophysical survey over the its South Bay property in Feb. 2007. A total of 22 line kilometres were surveyed. The primary objective of the "Titan-24" survey was to identify Direct Current, Induced Polarization (DCIP) and Magnetotelluric (MT) anomalies, which may represent copper-zinc Volcanic Massive Sulfide (VMS) mineralization similar to the South Bay copper-zinc-silver deposit. The "Titan-24" survey responses over the South Bay Mine deposit were used as a "Calibration Model" for prioritizing anomalies in the area.

Three dimensional modeling of the geophysical responses and known diamond drilling show that most of the targets have not been tested at all or were very poor tests of the Titan 24 anomalies.

On April 3rd, 2008 Skyharbour announced it made what appeared to be a significant discovery of volcanogenic massive sulphide (VMS) mineralization, in an area that has never been drill tested in the past, approximately 500 metres to the southwest of the former South Bay Mine shaft.

While drill testing Titan 24 geophysical anomalies on the Company's South Bay property, Skyharbour identified massive sulphide zones. The mineralization consists of fine grained, massive to finely bedded phyrrotite with visible zinc sulphides (sphalerite) and visible copper sulphides (chalcopyrite). These new VMS zones are approximately 500 metres to the southwest of the former South Bay mine shaft operated by Selection Trust of London (Selco. 1970 - 1982).

The discovery of VMS style zinc mineralization in a totally unexplored portion of the South Bay stratigraphy is highly significant. It is too early in the exploration process to have identified the principle vent(s) and more strongly mineralized areas. Subsequent pressure and folding of the mineralization has resulted in thinning and thickening of the sulphides and buried to depth with concentrations expected to be both of lower and higher grade. Concentrations most likely will be found in both pods and lenses with lower and higher grade sections. The possibility of parallel zones is also a potential. Exploration is currently focused on expanding the area of mineralization to identify richer portions of the system.

The stratigraphy hosting the discovery is a thick sequence of rhyolitic flows and flow breccias intruded by numerous porphyry bodies and sills. The mineralization may be within stratigraphy correlative with that hosting the South Bay mine. The area of the Skyharbour discovery is marked by a large and discrete sodium depletion zone in rocks that typically characterize VMS deposits.

The dominant mineral in the discovery is sphalerite (zinc) with minor chalcopyrite (copper). The zone is distinctly exhalite in origin and is very fine grained with very fine bedding and some chert beds. These features suggest the mineralization is on the apron, some distance (+/- 200 metres) from a potential vent area where zinc and copper grades are generally much higher. The deposit overlies an extensive rhyolitic flow breccia sequence with chlorite alteration in the matrix to the fragments.

The general area of the discovery has all the characteristics of a base metal camp. Typically a camp hosts a number of zinc-copper deposits with one or two larger deposits of 15 to 50 million tonnes and a range of much smaller deposits down to 0.5 million tonnes. The only significant deposit found to date is the South Bay Mine deposit and it is at the smaller end of the scale. This might suggest that larger deposits remain to be discovered.

The former South Bay Mine, located on the Company's 123498 claim block, produced approximately 1.6 million tons of 2.3% copper, 14.5% zinc, and 3.5 oz/ton silver to a vertical depth of 410 metres, and explored to a vertical depth of 600 metres, between 1970 and 1982.   The South Bay deposit is a classic Archean Volcanic associated Massive Sulfide (VMS) deposit that is hosted in an area known as the Confederation Belt.

VMS deposits are major sources of copper and zinc. Approximately 80% of the worlds VMS deposits occur in arc-related successions typical of many Archean greenstone belts. Archean and Phanerozic VMS deposits are typically hosted by rhyolite. VMS deposits tend to cluster in a favorable time stratigraphic interval. Two essential elements of most genetic models include strata bound mineralization and alteration pipes crosscutting rock types stratigraphically below mineralization. Stacking of mineralized bodies is common.

The South Bay deposit lies within a coalescing series of rhyolite domes and exhibits a small but distinct alteration zone in the footwall. Large scale litho geochemical sampling indicates the known deposit is related to a large zone of sodium depletion that terminates against a more mafic rock sequence in the hanging wall of the rhyolite dome complex. This setting is deemed exceptionally favorable and has not been systematically explored. Several surface geophysical targets and off-hole responses generated from down hole pulse electromagnetic surveys have yet to be tested.

Although the South Bay Mine was discovered at shallow depth, the best ore was subsequently identified at depths below 275 metres illustrating the concept of near-surface mineralization reflecting deeper-lying deposits. Many near surface zones have been identified but only South Bay has developed into a mine emphasizing the need to look deeper into the belt. A new, deeper penetration geophysical technique known as the "Titan-24" developed by Quantec Geoscience Inc. is being untilized by Skyharbour Resources.

VMS deposits are found within the massive or semi-massive sulphide accumulations typically formed above submarine volcanic centres, which are preserved as highly altered stockwork zones (and can themselves host ore-grade mineralization in sulphide-rich veins). While pyrite is ubiquitous and forms the bulk of the massive sulphide body, metal zoning of ore minerals can be seen with copper, in chalcopyrite form, typically giving way outwards to the more soluble sphalerite and galena and sometimes barite (barium sulphate). The outermost flanks will typically be more oxidized containing maganesse, hematite, chert and finally magnetite. In some cases at greater distance this lateral gradation culminates in iron or maganesse-rich massive oxide deposits, for example the Archean Algoma-type Banded Iron Formations, which can have great economic significance in their own right.

Due to the relatively small extent and therefore tonnage (0.1-10 Mt), major VMS copper-zinc mining camps usually correspond with deposit clusters. However, despite their small size, the high grade and bulk nature of these deposits mean they are often economically profitable to mine. Furthermore, exploration using geophysical techniques is aided by the high relative density and electro-magnetic properties of these bodies.

Projects throughout Canada, politically stable, mining friendly jurisdictions.

Shares Outstanding — 34.7 million shares

Fully Diluted — 61.2 million shares

Corporate Profile on Stockhouse

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