Geoscience Resources of Newfoundland and...

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001L/14/0273

FIFTH AND EIGHTH YEAR ASSESSMENT REPORT, Geochemistry and Examination of Old Trenches

Licenses 21055M, 21479M, AND 22121M NTS 1L/14.

ST. LAWRENCE AREA, NFLD. ALEX HARRIS, B. Sc.

Work performed March, 2014 to, January 2015 For: NEWFOUNDLAND FLUORSPAR EXPLORATION LTD.

Total Expenditures: $16,887.68 Total Number of claims 57.

January 5, 2015 Allocation by License: 21055M 2,237.85 21479M 7,696.62 22121M 6,953.21 TOTAL $16,887.68

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TABLE OF CONTENTS page INTRODUCTION 4 LOCATION AND ACCESS 4 PREVIOUS EXPLORATION AND MINING 4 GEOLOGY 5 REGIONAL SETTING 5 REGIONAL GEOLOGY & MINERALIZATION AT ST. LAWRENCE 5 FLUORITE VEINS 6 TAREFARE - GRASSY GULCH VEIN 7 BLACK DUCK VEIN 8 LAWN ROAD VEIN 9 BOX HEATER VEIN 9 RYAN MOUNTAIN-SALMON HOLE VEIN 9 RYAN FLATS TRENCHES 10 CRANBERRY BOG 11 MINE COVE VEIN 11 LITTLE LAWN HARBOUR OCCURRENCE 12 FLUORSPAR PROSPECTING TECHNIQUES 12 NEWFLUOREX 2014 EXPLORATION RESULTS 14 TRENCHING AT LITTLE ST. LAWRENCE 14 SOIL GEOCHEMISTRY 14 HYDROGEOCHEMISTRY 15 RECOMMENDATIONS 16 REFERENCES CITED 17 APPENDIX 1 Maps: SL 14-1 Location of Project SL 14-2 Key of Map sheets SL 14-3 Diamond Drilling Locations 1:50,000 SL 14-4 2014 Water and Soil sample locations and traverses, 1:25,000

SL 14-5, 2014 Water Sampling, Proposed HLEM Survey, Bedrock Geology Licence 21055M, 1:25,000

SL 14-6 2014 Fluoride in Water Licence 21479M South, 1:10,000 SL 14-7 2014 Fluoride in Water Licence 21479M North, 1:10,000 SL 14-8 2014 Fluoride in Water Licence 21057M, 1:10,000 SL 14-9 2014 Fluoride in Water Licence 21479M, 1:5,000

SL 14-10 2014 Soil Sample Values, proposed HLEM AMT survey, Licence 21479M, 1:10,000

SL 14-11 Little St. Lawrence Water and Soil sample values, 1:2,000 SL 14-12 Cranberry Bog Area Historical Trenching Overlay 2014 GPS Points, 1:5,000.

SL 14-13 Tarefare Vein Extension Diamond Drill Hole 1:5,000 SL 14-14 Little St. Lawrence Proposed Drilling Locations 1:5,000 SL 14-15 Proposed Diamond Drill Holes and as-drilled LSL-1 Section, 1:2,000 SL 14-16 Diamond Drilling Specifications

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APPENDIX 2 Certificates of Analysis APPENDIX 3 GPS Data Listing APPENDIX 4. Statement of Expenditures APPENDIX 5 List of Personnel

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INTRODUCTION Grubstake Management (Nfld.) Ltd., acquired Licence17062M in the St. Lawrence Area, Newfoundland, NTS sheet 1L/14 late in 2009. Early in 2010 this Licence was transferred to Newfoundland Fluorspar Exploration Ltd. (Newfluorex). Later in 2010, 17832M was staked by Newfluorex; 16461M, 17055M, and 17982M were optioned from Golden Dory Resources (Now Sokoman Iron Corp.). Early in 2011 Blocks 17062M and 17832M were reduced and grouped as Licence 18753M and Licence 17982 was split into 2 Licences, 18749 retained by Newfluorex under option from Golden Dory Resources while remaining Licence (Now 020098M) was returned to Golden Dory. Licences 16461M and 17055M were combined as new Licence 19839M early in 2012. Licences 18749M and 19839M were further reduced early in 2013 as 21055M and 21057M and transferred to Newfluorex on completion of terms of option agreement. Licence 18753M was further reduced mid-2013 to Licence 21479M. Licence 21057M was reduced to Licence 22121M in March, 2014. Claim locations are shown in Appendix 1 LOCATION AND ACCESS St. Lawrence is located at 46° 45' North Latitude and 55° 20' West Longitude. Maps 14-1 to 14-3 show location of Project. Claims are accessible from Provincial Highway 220 and by ATV trails. The harbour at St. Lawrence is ice-free all winter allowing for shipping in all seasons. PREVIOUS EXPLORATION AND MINING Harris (1996) reviewed the previous exploration and mining history of the St. Lawrence Area in detail for Burin Minerals Ltd. Subsequent work by Burin Minerals/Canada Fluorspar (Agnerian, 2009) has concentrated on drill testing of Blue Beach North and Tarefare Deposits in preparation for resumption of Fluorspar Mining. Exploration North of the Burin Minerals/Canada Fluorspar properties by Golden Dory Resources in 2007-2009 (Evans & Vatcher, 2007; Vatcher & Evans, 2009; Evans & Vatcher, 2009) has focused on Uranium exploration. Harris (2010) reported on Hydrogeochemical survey and prospecting, compiled Geological and Hydrogeochemical information and recommended a diamond drilling program. Harris (2011) reported on further Geochemical Surveys and Diamond Drilling. Harris (2013) included a 43-101 report prepared by Tim Froude, P. Geo. Harris (2014) reported on examination of old trenches in Ryan Hill and Ryan Flats Areas and soil geochemical work in Loo Pond Area. The St. Lawrence area hosts numerous fluorite-bearing veins, which range to 2 km in length and, in some cases, exceed 30 m in thickness. Fluorspar mining began in 1933. Development was by two companies, Newfoundland Fluorspar Ltd., and The St. Lawrence Corporation, both of which eventually came under the control of Alcan. After 44 years of mining, 4.2 million tonnes of ore had been produced when Alcan closed the mines in 1977. Production of about 440,000 tonnes of ore was reported between 1986 and 1991 by St. Lawrence Fluorspar (Minworth).

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Canada Fluorspar Inc. holds Licences and Mining Leases adjacent to Newfluorex property and is attempting to resume mining of Blue Beach North and Tarefare veins. They have (News Release Dec. 4, 2013) announced results of Diamond Drilling on the AGS Vein (Formerly Grebe’s Nest Vein) and Director Vein, including an inferred resource of 7,090,000 Tonnes on the AGS vein. GEOLOGY The fluorspar veins are spatially and genetically associated with the Carboniferous St, Lawrence Granite and related porphyry dikes. The veins are complex structures along fault zones, which have had multiple episodes of movement. Typically, vein has a high grade core and irregular amounts of mineralized granite breccia along one or both sides. Three major groups of veins are recognized: "North-South" veins, "East-West" veins and "Outer" veins which typically have some barite. REGIONAL SETTING O'Driscoll et. al. (1988) have described the regional setting of the Avalon Zone in the eastern portion of the Appalachian mountain system. This zone is separated from other zones by major faults. O’Driscoll et. al. (Ibid.) discuss the General Geology of the Avalon Zone in considerable detail. They describe the zone as characterized by thick, widespread, dominantly subaerial volcanic rocks and marine to terrestrial clastic sedimentary rocks of Late Precambrian age, locally overlain by shallow marine, sedimentary and minor volcanic rocks of Cambrian age, these sequences are locally overlain with angular unconformity by Devonian and Carboniferous sediments and volcanics. The zone is intruded by several Late Precambrian and Late Devonian to Carboniferous granites. Van Alstine (1944) noted that folding and thrust faulting (of Cambrian and older units) preceded intrusion of the St. Lawrence Granite. REGIONAL GEOLOGY AND MINERALIZATION AT ST. LAWRENCE The fluorspar deposits are spatially and genetically associated with the St. Lawrence Granite which has been described by Teng and Strong ( 1976), as a high level, peralkaline, Carboniferous pluton intruding volcanic and sedimentary rocks of Late Precambrian and Cambrian age. Grain size decreases progressively towards its contact. Miarolitic structures are seen within a few meters of the contacts. Tuffisites are common, consisting of discrete angular to rounded fragments of the granite in a finely commuted matrix. Related pink quartz-feldspar porphyry dikes are common outside its western margin. The St. Lawrence Granite and associated rocks are unique in eastern Newfoundland, in that they contain aegirine and riebeckite. Smith (1957) notes that the granite has three pronounced sets of jointing, one parallel to the north-south elongation of the batholith, another at right angles to the elongation, and a third horizontal set of joints. The most recent detailed regional geological mapping of the area was reported by Strong et. al. (1978) in the central and eastern portions of the district, while the western portion of the district was mapped by O'Brien et. al.(1977). Many writers, including Van Alstine (1944) have noted that in general, the hornfels and slate adjacent to the St. Lawrence Granite is considered to be a poor host rock for fluorspar veins.

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FLUORITE VEINS Smith (1957) reported that within an area of about 60 square miles there are 39 known fluorspar veins, some of which have been more thoroughly outlined by exploration than others. Tilsley (1972b) has produced good quality compilation maps with locations of those veins which are within a 5km radius of the Town of St. Lawrence. Strong et. al. (1978) show approximate locations of many of these veins and most of the outlying veins. The largest production has been from Director, Tarefare, and Blue Beach veins. Almost all of the veins are within the granite or the related porphyry dikes. The 2013 discovery by Canada Fluorspar Inc. of significant fluorite mineralization in the AGS Vein (known previously as Grebes Nest Vein), within metasedimentary rocks is the first discovery of mineralizarion outside the granite. The veins are fissure fillings located in cracks which developed from regional stress and contraction during the cooling of the granite (Smith 1957). Smith (1957) points out that there has been shearing movement, predominantly horizontal, along the fissures, and brecciation of the wallrocks which were cemented by fluorite probably before the vein itself was formed. Veins vary from a few hundred meters to well over 2 km long and tend to pinch and swell in both horizontal and vertical directions. Van Alstine (1948) notes that no vein has been followed to its terminations. Smith (1957) notes that cross veins and parallel veins are fairly common. The veins at St. Lawrence are not simple tabular bodies, but complex structures along fault zones which have had multiple episodes of movement before and during vein formation. Three major groups of fluorite veins are recognized: 1. The low grade veins are widest, averaging 7m, and longest, with CaF, grades in 35-70% range. Although strike varies from 135 to 160, those were locally known as "North-South" veins. Examples are Tarefare and Blue Beach veins. 2. High grade veins have an average width of 1 m or less, and are characterized by grades averaging 95%. Strike varies from 60 to 115 and they are locally known as "East-West" veins. Examples are Iron Springs and Black Duck veins. 3. The "Outer" veins in the peripheral region of the district typically have significant barite intergrown with fluorite. Examples are Lunch Pond, and Clam Pond veins. Fluorite is mostly massive and coarsely crystalline, filling veins from wall to wall. Close to the vein walls the fluorite is commonly finely banded, suggesting rhythmic deposition. In the larger veins, fluorite surrounds sharp fragments of granite, the fragments being frequently of very considerable size (Smith, W.S., 1938). Fluorite occurs in a wide variety of colours. Garrison (1927) stated that the color of fluorspar is due to the presence of hydrocarbons oxidized at the time of its crystallization. Tilsley (1975) suggests that colour in fluorite is caused by atomic disorder in the crystal rather than chemical impurities. He reports that coloured crystals may dissolve in water as much as two and a half times as rapidly as the clear variety. Vugs and openings are commonly lined with well formed crystals of fluorite, commonly as cubes which may reach 35 cm along an edge. In plan some vugs measure 3 feet by 20 feet, and some extend for a vertical distance of more than 100 feet (Van Alstine, 1944),

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The most common gangue mineral is quartz, occurring in the material locally known as "blastonite", brecciated fluorite cemented by a mixture of microcrystalline quartz and fluorite. Nodular forms of fluorite and calcite around fragments of country rock or older fluorite fragments are common in the larger veins, mainly along the footwall of veins. Williamson (1956) describes a typical cross section of a vein as: wall rock, massive fluorspar, massive white quartz, blastonite, a narrow width of fluorspar, wall rock. Calcite occurs in nearly all the fluorite veins. Barite, galena, sphalerite and hematite are common while chalcopyrite, pyrite, covellite, bornite and chalcocite have also been noted. Van Alstine (1948) notes that most veins in the district have sections that are considerably richer in sulphides, and when fluorspar from such sections is being milled, a marketable lead and zinc concentrate probably could be made. Williamson (1956) suggests that sulphides (mainly galena and sphalerite) are more abundant near the granite contacts or where the vein crosses into country rocks; veins lying well within the granite carry comparatively little sulphides, although this is where chalcopyrite is best developed. Smith (1957) states that in no case has a vein been moved by post mineral faulting. Collins (1984) reported results of studies indicating that boiling of fluids, causing an increase in pH, was a major control in fluorite deposition. He reported two cycles of temperature and salinity variations for the samples he examined. TAREFARE - GRASSY GULCH VEIN House et. al. (l983) indicate that the Tarefare - Grassy Gulch vein system has been traced on surface for approximately 2.5 km, striking 150° and dipping almost vertically. At the north end it dips steeply east and parallels the contact between the St. Lawrence Granite and the adjacent Inlet Group (composed mainly of siltstone). There are three closely adjacent parallel veins in this area, the Tarefare, Blowout and Hope veins, all of which are accessible from the underground Tarefare workings. Several cross veins striking 060° and dipping steeply northwest contained mineable widths of >90% CaF2 in the 70 m between the Tarefare and Hope veins. Tarefare vein contains abundant blastonite accompanied by crystalline, locally banded massive fluorite with gangue of quartz and calcite with lesser amounts of sulfides. Smith (1957) noted that the tendency to pinch suddenly, displayed by the Blowout Vein, contrasts with the Tarefare Vein which tapers gradually. Alcan archive records indicate reserves at Tarefare at cessation of operations on 1 October 1976 totaling 2,585,900 tons at 54%. A total of 79,530 tonnes were mined by St. Lawrence Fluorspar by open pit in 1987-89, Collins (1985) included plans for open cut at Tarefare South. Canada Fluorspar Inc. currently has indicated resource at Tarefare of 4.7 million tones at 44.7% with additional inferred resource of 595,000 tonnes at 31.8% at the adjacent Blowout Vein. The Tarefare Vein is open to the North and appears to be plunging at about 10. It is expected to plunge beneath Licence 21055M which Newfluorex acquired from Golden Dory Resources. A new Diamond Drill Hole NSL-101-2 completed in September, 2011 encountered granite at a down-hole depth of 283m near the SouthEast corner of 21055M.

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Newfluorex proposes to test the feasibility of using the audio-magnetotelluric (AMT) ground geophysical method as a means to delineate vein structure at depth, with a survey line crossing the projected strike of the Tarefare vein (Map SL-13-9). Newfluorex considers the Tarefare Vein to be a high-priority exploration target. A 620 m long drill hole NSL-101-3 is proposed to test the projected vein structure. BLACK DUCK VEIN Howse et. al. (1983) note that the Black Duck vein strikes 060°, and was mined along a strike length of approximately 285 m. Average grades were approximately 90%. Fluorite ranged in color from amber to red to green and purple. Characteristic pinches and swells were prevalent. Howse (1937) reported that Black Duck Vein has been worked to a depth of 140 feet and shows no signs of narrowing or petering out. Van Alstine (1939) describes this vein as varying from 3 inches to 7 feet in width and extending to depth of 250 feet. Smith (1957) mentions that the vein is cut off by a diabase dyke at the west end. Farrell (1967) reports total production from Black Duck Mine at 46,000 tons during the period 1933 to 1941. Smith (1957) describes a vein of fluorspar located on Claim No. 80 which was thought to be an extension of the Black Duck Vein. A shaft was sunk to a depth of about 100 feet and a drift eastward about 150 feet was in high grade ore about 4 feet wide similar to Black Duck ore. Ground conditions were poor and workings caved in. Farrell (1967) provides more detail about this working, which he describes as extending over an overall length of approximately 550 ft. He states that no trenching or diamond drilling was done in this area. A total of about 2,000 tons of fluorspar were recovered. They commented that ore still remained in the bottom and that this area deserves more work. They also reviewed the unsuccessful development efforts at the New Black Duck Vein about 1500 ft. to the southeast where bad ground conditions resulted in caving, and the discovery of fluorspar float when the local football field was leveled. They suggest that this system has the earmarks of a major vein system with the possibility of large tonnages. Alcan archive records show reserve estimates at Black Duck No. I as of 1 Nov., 1975 at 14,800 tons probable, and 32,200 tons possible for a total of 47,000. At Black Duck No. 2 they estimate 5,700 tons probable plus 6,900 possible for a total of 12,600. Newfoundland Fluorspar Works (1976) file includes log for hole No. I on Black Duck Vein collared 1000 ft. West of Black Duck No. 1. At depth of 314.2-317.5 in inclined (45) hole a 3.3 ft, intersection assayed 95.1% (66.6%/5.3ft.). A second hole 300 ft, further west did not intersect any mineralization or any evidence of vein structure. Locations of these holes are shown on Map14-6.

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LAWN ROAD VEIN Van Alstine (1939) describes this vein as purple and green fluorite with calcite, chalcedony and granite observed over strike length of 75 feet and varying in width from 6 to 16 inches. BOX HEATER VEIN The Box Heater Vein located immediately north of the highway west of St. Lawrence is a filling in a fault fissure within the St. Lawrence granite. The vein reportedly strikes N80E and was traced on surface for approximately 137 meters, and reportedly has a width of 0.9 to 3 meters (MODS report 001L/14/FL 042). The fluorite is multi-coloured. Associated gangue minerals include barite, calcite and galena. Past work included a shaft to depth of 52 feet, and a 35 ft long southward cross cut. Two underground diamond drill holes were completed 100 and 252 ft long, which did not intersect any appreciable fluorite mineralization, although a 9 ft long cave-in was encountered in one hole which was said to possibly represent an unrecoverable vein structure. Although old trench work was observed during Newfluorex’s 2010 hydrogeochemical program, the heavy overgrowth by trees up to 10 cm diameter, and bush did not allow for confirmation of vein dimensions without extensive clearing and excavating (Harris, 2010). Due to narrow width of this vein, Newfluorex regards this vein as having a low potential for minable tonnage and therefore does not plan, at this time, to undertake future exploration efforts on the Box Heater Vein. RYAN MOUNTAIN-SALMON HOLE VEIN Prevous reports (Smith 1957; Farrell, 1967) have suggested that the Ryan Mountain (Hill) Vein is the western continuation of the Salmon Hole Vein, about 600 meters apart from each other. Smith (1957) reports that the vein was trenched over a length of 600 feet and had widths up to 4 ft., tapering gradually to 1 foot on both ends. A trenching map included in Smith’s report shows the central part of Ryan Mountain Vein extending over 180 ft. along strike with a width of over 3.5 ft. The fluorite mineralization was mentioned being “good quality”, about 90% CaF2. The vein is hosted in the St. Lawrence Granite, traced eastward from the slate-granite contact and then cut off on the east by a diabase dike. Exploratory drilling east of the diabase dike did not intersect the vein, but trenching exposed 6 ft. of low grade ore (Smith, 1957). At least two drill holes, 60 ft and 200 ft long, were completed in 1946 (Smith, 1946a). Geological progress reports (Smith 1945, 1946c) describing work undertaken in the mid-1940s, mention overburden ranging from 8 to 20 ft deep, increasing to the east. Test pits required extensive lagging for protection and water ingress was a problem.

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A search of Alcan archive records, by Harris (1996b), showed that reserve estimates at Ryan Mountain as of 01 November, 1975 at 6,100 tons possible. However no grade was provided with the estimate. Newfluorex personnel found about half of the Ryan Hill trenches and pits during a site reconnaissance in July 2013. Trenches and pits found were readily correlated with trenching plan from Smith (1957). The area is extensively overgrown with dense low forest and alder, such that workings were almost undiscernible from a few meters distance. The Salmon Hole Vein occurs on Newfluorex property licence 21057M.Van Alstine (1939) describes the Salmon Hole vein as tan colloform fluorite with calcite and lamprophyre observed over a strike length of 200 feet and varying in width from 3 inches to 2 feet. It occurs within a lamprophyre dyke in the granite. At Salmon Hole on the Little St. Lawrence Brook, there is an open cut on the western bank of the brook where the vein outcrops 3 feet wide. The south wall here is diabase and the ore is about half lime and half fluorspar. David S. Robertson and Associates (1974) have mapped two VLF-EM conductors East of Salmon Hole towards Mount Margaret. The northern of the two structures is interpreted as being the extension of the Salmon Hole fluorspar vein. Geochemical results indicate that both structures are mineralized. Diamond drilling and Trenching was recommended. Mason (1974) refers to “A target selected for and presently being drilled for Alcan”, clearly referring to this area, and Buller(1974) stated “The Alcan test drilling turned out to be negative. Newfluorex considers the Ryan Mountain /Salmon Hole Vein to be a higher-priority exploration target for a geophysical survey to determine presence of a fault / shear structure beneath overburden. Test work should be focused outside of the St. Lawrence Water Supply Area. RYAN FLATS TRENCHES The Ryan Flat showing is located on Newfluorex property license 21479M. Exploration was carried out on the Ryan Flats claim group during the mid to late 1940s (Gummer, 1945; Smith, 1946a, 1946b, 1947). In 1945, a large trench cut (visible today) was made in a valley across a 50 ft wide zone of strongly fractured granite described as soft and kaolinized. Several veinlets of siliceous fluorite up to 6-inches wide were reported. A nearby 26 ft deep shaft was sunk on the most pronounced zone of kaolinized fracturing, but said to be unmineralized with fluorite. Strong iron staining was present in the kaolinized rock. By 1946, the well-timbered shaft had been deepened to 38 ft. From the shaft, a 22 ft long westward and a 30 ft eastward crosscut were completed. No fluorite mineralization was encountered in the shaft or crosscuts, although kaolinization was persistent and accompanied by quartz mineralization and narrow veinlets of “flint”. Another test pit, 25 ft deep, was located 25 ft east of the shaft. This pit was completed into fairly

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solid granite without finding any fluorite (Smith, 1947) Newfluorex personnel located the former Ryan Flat workings during a site visit in July 2013. The large trench cut, with high embankments of muck rock, is readily visible. Near the western end of the cut is a concrete cap, believed to mark the former shaft. On top and along sides of the 15 m high knobby hill immediately west of the cut and capped shaft are several shallow (less 1 m deep) rubble partially infilled trenches. No further work is recommended at Ryan Flats. CRANBERRY BOG The Cranberry Bog showing is located on property license 21479M, wholly held by Newfluorex. At Cranberry Bog, sometime during 1944, a 6 ft. by 6 ft. timbered shaft was sunk to 30 feet on a vein 1 ft. wide (Smith, 1957). Trenching traced a vein for 600 feet, but widths continued narrow. The vein was hosted in the St. Lawrence Granite, striking 030o and dipping steeply southeast. Smith (1957) reported the “ore is of very good grade with only a little intergrown calcite”. About 100 ft. from the shaft another fluorite vein occurs, striking 330o and dipping steeply southwest. This second vein varied from a few inches to 18 inches width, hosted in a 3 ft wide fracture zone. Galena and magnetite occur with the fluorite. Although a test pit was sunk on the intersection point of the two veins, Smith mentions that encouraging mineralization was not found on the northwest trending vein. A surface exploratory drill hole (unknown date) at the shaft did not cut any parallel veins. Old trench locations were observed in 2014 field work correlating closely with historical survey record as shown on Map SL 14-12. Notes on field observations and GPS coordinates are included in Appendix 3. Newfluorex considers the Cranberry Bog Vein to be a low priority exploration target since a previous prospecting shaft and a surface drill hole failed to intersect mineralization. MINE COVE VEIN The Mine Cove showing, initially explored for lead-silver, on the east shore of Little Lawn Harbour is located on Newfluorex’s property license 21055M. In 1870, Alexander Murray and James Howley visited Little Lawn and reported on the Mine Cove vein (Murray and Howley, 1871). The vein was described by Van Alstine (1939) as a green and purple fluorite vein with galena, sphalerite, and quartz occurring within slate and rhyolite porphyry over an observed length of 250 ft. and varying in width from 1 to 18 inches. According to Smith (1957) the vein was worked prior to 1870 by means of a small tunnel about 50 ft. long, searching for silver . The vein was traced eastward until the vein so narrowed that it could no longer be followed (Smith, 1957). DeZoysa (1966) has commented on the presence of galena and fluorite veins, but also notes there were no accompany assay data in the historical record. Newfluorex considers the Mine Cove area to have a high priority for additional exploration due to the discovery by Canada Fluorspar Inc. in 2013 of significant fluorite mineralization in the

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AGS Vein (known previously as Grebes Nest Vein), located 1 km south of the Mine Cove Vein, within metasedimentary rocks (siltstones and shale). Historically, the major fluorspar veins in the St. Lawrence area were hosted in the St. Lawrence Granite and not the widespread metasedimentary rock into which the granite intrudes. Newfluorex plans to undertake a reconnaissance HLEM ground geophysics survey line to determine whether the Mine Cove Vein structure extends eastward (inland) beneath the overburden, and to identify locations for possible drill testing of any identified structure. A hydrogeochemical survey is also recommended. LITTLE LAWN HARBOUR OCCURRENCE There is sparse information about the Little Lawn Harbour occurrence listed in the on-line MODS report 001L/14/Fl 042. The vein is listed as a map reference in which it is described as “a mineral showing in bedrock”, the St. Lawrence Granite. Radex Minerals Limited was the first to note this showing, as a result of their 1969-1971 exploration programs (Pearse, 1971). Golden Dory (Froude, T, 2012) noted several occurrences of fracture filled purple fluorite in the same vicinity. Newfluorex proposes a reconnaissance HLEM ground geophysics survey to determine if a potential fluorite-bearing fault / shear zone is responsible for the Little Lawn Harbour Occurrence, which appears to be hosted in metasedimentary rock. The previously mentioned off-property AGS Vein is situated about 1.5 km south of the Little Lawn Harbour Occurrence. FLUORSPAR PROSPECTING TECHNIQUES From description in Smith's (1957) report of prospecting activity in the area, it is obvious that thorough surface prospecting with extensive hand digging and trenching in search for fluorspar float has been completed on the lands which were held by Newfoundland Fluorspar Ltd. (Alcan). Farrell's (1967) report indicates that prospecting of the St. Lawrence Corporation properties was much less thorough and systematic. Van Alstine (1948) notes that in most places the vein material is less resistant to erosion than the host rock, and the vein may be expressed topographically as a notch in the sea shore or as a small gully. Boulders and pebbles of fluorite are in places found within glacial drift - ice moved in a southerly direction in the area. Van Alstine (1948) also points out that in the vicinity of a vein, granite and rhyolite porphyry generally show extensive development of breccia cemented with purple fluorite. He recommends that areas near the contacts of granite or rhyolite porphyry with hornfels are especially worthy of further prospecting, as are irregular borders of intrusives, especially embayments of granite into hornfels.

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Smith (1957) does not attach much importance to the "embayment" theory, pointing out that apparent embayments are often accidental and due to glacial planation of slate. Williamson (1956) notes that "Lean Showings", which trenching and stripping has shown to consist only of impregnations and the absence of a vein structure, nearly always consist of purple fluorspar. Van Alstine (1948) also recommends that locations with slight changes in strike of a vein should be investigated as a possible location of a lens of workable fluorspar. He also notes that parallel and branch veins have been located by cross-cutting from drifts and by drilling. Van Alstine (1948) also notes that veins associated with lamprophyre dykes could be traced by a magnetometer survey. Tilsley (1972) cautions that the interpretation of the significance of a geochemical anomaly must include determination of the depth of overburden and, if possible, the position of the water table. Anomalies may be "transported" by groundwater as much as 3000 feet from source. Tilsley (1972b) obtained hydrogeochemical anomalies from most of the know veins, the exceptions being those structures which lie on high ground or under more than 10 feet of saturated overburden. He recommended additional work in four selected areas: Shoal Cove Pond, Mount Margaret Pond, Clarke Pond, and Tarefare Road. He noted more than a dozen smaller anomalies which are related to unknown fluorine sources which should be reappraised. All hydrogeochemical data have been compiled on maps COMP1 – COMP12 in Appendix 1. Tilsley (1972e) reports that the depth of cover through which 'frost heaving' of mineralized material may take place is in the order of 4 feet or less. Since most known fluorspar-bearing structures in the St. Lawrence area were discovered as outcropping veins or through tracing of float short distances, he concluded that it is probable that there are few undiscovered veins in areas of shallow overburden cover. Tilsley (1973) notes that approximately 70% of the mineralized structures at St. Lawrence are more or less conductive and can be detected by VLF-EM Surveys. He observes that conductivity varies along a structure with changes in intensity of alteration along strike. Tilsley (1973c) presented a large amount of geochemical and geophysical data for the "Lanes Pond Area", and the "Mt. Margaret Area". All hydrogeochemical data have been compiled on maps COMP1 – COMP12 in Appendix 1. Tilsley (1974) notes that the primary signal used for VLF-EM surveys is normally supplied by military navigational beacons. In the St. Lawrence area, the signal from only one such beacon (NAA, Cutler, Maine) can be adequately received for survey purpose East-West structures can be readily detected, but those which strike nearly north-south do not develop secondary electromagnetic fields. He describes test work with a portable VLF signal generator which was effective within 2 miles of the generator. He considers VLF-EM surveying using both

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military and portable signal sources to be an indispensable tool in fluorspar exploration in this area. Tilsley (1974) reports that the typical exploration program can be divided into four stages: a. Reconnaissance hydgogeochemistry, interpretation of airborne magnetic and VLF-EM data, geological mapping and prospecting. b. Detailed hydrogeochemistry, ground magnetic and VLF-EM surveys. c. Deep overburden sampling and fluorine analysis along axes of fault structures defined by geophysical surveys, d. Trenching or, more usually, diamond drilling. David S. Robertson and Associates (1974) note that an impervious 'placon' layer has been noted in the soil profile in most areas where the water table is above bedrock. This 'placon' prohibits the movement of groundwater to the surface and thus prevents any surface expression of an underlying fluorspar vein, Experimentation showed the basal till horizon to be the most indicative of a nearby source of fluorine, Basal till samples are also less susceptible to surface contamination. Tilsley (1972) discussed fluorspar exploration techniques and fluorine geochemistry. He indicated that solubility of CaF2 decreases rapidly from 8.76 mg/kg H2O at 23C toward near zero at the freezing point. Waters examined from the St. Lawrence Area ranged from less than 0.2 ppm to maximum of 2.8 ppm. He stated “a fluorine anomaly is defined as a group of samples which show … a fluoride content which exceeds the regional background by a factor of at least 2. Background values … usually range between 0.05 and 0.30 ppm fluorine.” NEWFLUOREX 2014 EXPLORATION RESULTS TRENCHING AT LITTLE ST. LAWRENCE On Licence 22121M, (Maps 14-4, 14-11) a 110-m flag and compass line was established along a natural gully. Using a mattock, Ten small (0.3-1m square) openings were made into gully sidewalls to search for bedrock. No bedrock was exposed due to presence of granite boulders. Five soil samples (SSL-200-204) were collected. Openings were backfilled with the hand-excavated soil. SOIL GEOCHEMISTRY Ten soil samples were collected on Licence 021479M in a line crossing a topographic lineament. Two samples were collected at each of five sites, one at top of mineral soil horizon and one at deepest penetration with auger. Since there was very little difference in sampling depths (maximum 22 cm.), deepest samples were analyzed for total fluoride content and shallower samples were dried and retained for possible future analysis. Five soil samples were also collected on Licence 22121M as noted in above paragraph. Sample locations are shown on Map 14-4 and results on Maps 14-10 and 14-11. Three values on Licence 21479M were above threshold value of 150 ppm (Maximum 180 ppm) and one value of 330 ppm on Licence 22121M. Complete Data Listing is in Appendix 2.

15

HYDROGEOCHEMISTRY Three water samples were collected on Licence 22121M and seven on Licence 21055M. Sample locations are shown on Map 14-4 and results, together with historical values are shown on Maps 14-5, 6, 7, 8, 9, and 11. Two highly anomalous values above 1 ppm are located on 22121M. Five values on 21055M were below detection limit and two were slightly below threshold value of 0.3 ppm. Location of these two samples in close proximity to trend of the Director Vein Structure may indicate some significance. These two samples were from separate seepages emitting from a small knoll. Frost heaved rock was observed on the knoll. Additional prospecting is recommended in this area.

16

RECOMMENDATIONS Cut 2 short lines at Little St. Lawrence as shown on Maps 14-11 and 14-14, collect soil samples at 25m intervals and strip moss at 2 locations shown on Map 14-11 to expose bedrock. Collect soil samples on 21479M on Lines 50-m North, 50-m South, and 100-m South of 2014 soil samples to better define anomalous area (Map 14-10). Area with anomalous fluoride in water and soil near intersection of a linear feature and a VLF-EM conductor near Loo Pond in Northwest corner of Licence 21479 may warrant future drill testing. Complete an audio-magnetotelluric (AMT) ground geophysical test survey on line connecting proposed collar of NSL-101-3 and NSL-101-2 extending 300m each side of projected position of Tarefare vein, with readings taken every 25 m. Location of test survey line is shown on map SL 14-13. Establish grid as shown on Map 14-5, complete HLEM survey, complete Hydrogeochemical survey 3 areas of 21055M as shown on Map 14-5. Complete an AMT test survey along ATV trail to Loo Pond extending 300m each side of projected strike of Ryan Hill Vein. Complete Preliminary HLEM survey along ATV trail to Loo Pond from 5199350N to 5200850N (Map SL-14-10). An additional 6 Diamond Drill Holes are recommended at this time for a total depth of 1,020 meters. 1 drill hole will test for extension of the Tarefare Vein (Map 14-13). 4 drill holes will test continuity of the recently discovered Little St. Lawrence Vein and 1 drill hole to investigate a topographic linear structure parallel to Little St. Lawrence Vein (Maps 14-14, -15). Drill hole specifications are summarized on Map 14-16. Projecting all-inclusive costs of proposed drilling program is $200,000. Respectfully Submitted January 5, 2015 Alex Harris, B. Sc.

17

REFERENCES CITED: Agnerian, H., 2009: Technical Report on the St. Lawrence Fluorspar Project, St. Lawrence, Newfoundland and Labrador, updated 43-101 Report for Canada Fluorspar Inc., available at Canada Fluorspar Website. Buller, A.E., 1974: Report on Cera Fluorite Project on Nalco Lot 4 in the Mount Margaret Area of the St. Lawrence Area, Newfoundland. NF Miner. Dev. Div. Assess. File 001L14/0052. Collins, C.J.; 1984: Genesis of the St. Lawrence Fluorite Veins, as indicated by Fluid Inclusion and Trace Element Data from three selected veins. BSC Thesis, Memorial University of Newfoundland, 117 pages. GSB # 001L/0088. Collins, CJ., 1985: Geological, Engineering and Metallurgical Study of the St. Lawrence Fluorspar Deposits. NF Miner. Dev. Div. Assess. File 001 L14/0095. David S. Robertson & Associates Ltd.; 1974: Report on Ground EM and Hydrogeochemical Surveys in the Mount Margaret Area of the St. Lawrence Area, Newfoundland. NF Miner. Dev. Div, Assess. File 1L/14/0068. Evans, D., and Vatcher, S.V., 2007, First Year Assessment Report on Magnetic & Radiometric Survey & Prospecting, Burin Property, Lawn Project: Licences 013251M, 013085M, 013119M, 013091M, 013118M, 013084M, 013086M, 013090M, 012704M, 013083M, 012703M, Grand Beach Project: Licences 013587M, 013388M, 010652M, 013092M, 010651M, and Salmonier Hill Project: Licence 013252M. NTS 1L/13, 1L/14, 1M/3 and 1M/4. Confidential Assessment Report supplied by Golden Dory Resources Ltd. Evans, D., and Vatcher, S.V., 2009, First Second and Third Year Assessment, Burin Project: Licences 012704M, 013091M, 013119M, 013821M, 015455M, 016336M, 016461M, 016649M, 017055M, 017057M, 017060M, 017093M, NTS 1L/13, 1L/14, 1M/3 and 1M/4. Confidential Assessment Report supplied by Golden Dory Resources Ltd. Farrell, H., 1967: Report on Mining Properties of St. Lawrence Corporation. NF Miner. Dev, Div. Assess. File 1L/14/0084. Froude, T., 2012: National Instrument 43-101 Qualifying Report For the St. Lawrence Property, Licence #s: 013095M, 018749M, 018753M and 019839M, NTS 1L/14, Burin Peninsula, Southern Newfoundland. Unpublished Report for Newfoundland Fluorspar Exploration Ltd.; Included as Appendix 5 in Harris, 2013. Garrison, F. Lynwood, 1927: Fluorspar Deposits at Great St. Lawrence and Little Lawn, Placentia Bay, Newfoundland. In Alcan archive files.

18

Gummer, W.K.,1945: Prospecting and Mapping 1944 for Newfoundland Fluorspar Limited, General Technical Department, Aluminum company of Canada Limited, Arvida, Quebec, 31 January 1945, p.46-47, 49 Harris, A., 1996: First Year Assessment Report on Licences 4591, 4610, 4611, 4612, 4613, 4669M, 4747, 4748, 4790, on NTS 1L/13, 1L/14, and 1M/13. NF Miner, Dev. Div. Assess. File Nfld. /2608. Harris, A., 2010: First and Forth Year Assessment Report, Hydrogeochemical Survey and prospecting, compilation of Geological and Hydrogeochemical Information, Drilling Recommendations, Licences 13095M, 16461M, 17055M, 17062M, 17832M, and 17982M, NTS 1L/14. St. Lawrence Area, Nfld., Confidential Assessment Report for Newfoundland Fluorspar Exploration Ltd. Harris, A., 2011: Second And Fifth Year Assessment Report, Geochemical Surveys, Prospecting, and Diamond Drilling Licenses 13095m, 16461m, 17055m, 18749m And18753m, NTS 1L/14. St. Lawrence Area, Nfld., Confidential Assessment Report for Newfoundland Fluorspar Exploration Ltd. Harris, A., 2013: Third And Sixth Year Assessment Report, 43-101 Report and Resource Estimate, Licenses 13095M, 19839M, 18749M AND 18753M, NTS 1L/14.St. Lawrence Area, Nfld., Confidential Assessment Report for Newfoundland Fluorspar Exploration Ltd. Harris, A., 2014: Fourth And Seventh Year Assessment Report, 43-101 Report and Resource Estimate, Licenses 21055M, 21057M, 21479M AND, NTS 1L/14.St. Lawrence Area, Nfld., Confidential Assessment Report for Newfoundland Fluorspar Exploration Ltd. Howse, A.; Dean, P.; Swinden, S.; Kean, B.; Morrisey, F.;1983: Fluorspar Deposits of the St. Lawrence Area, Newfoundland: Geology and Economic Potential. NF Miner. Dev, Div., Rep. 83 -09, 23 pages, (GSB# 00 1 L/009 1) Howse, C.K.; 1937: The Fluorspar Industry at St. Lawrence, Newfoundland, NF. Miner. Dev, Div., Intern. Rep. (GSB#1L14/003) Mason, R.J.; 1974: Cera Nalco Lot 4 Proposed Exploration, Fluorspar Concession, Aug. 6, 1974, appended to Buller (1974). Newfoundland Fluorspar Works; 1976: Diamond Drilling Logs and Plans for Holes drilled in 1976 on Meadow Wood Vein and Doctors Pond Area in the St. Lawrence Area, Newfoundland. NF, Miner. Dev. Div., Assess. File 001L/14/0059. O'Brien, SI; Strong, P.G.; and Evans, J.L,; 1977: The Geology of the Grand Bank (1 M/4) and Lamaline (1 L/13) Map Areas, Burin Peninsula, Newfoundland, NF Miner. Dev. Div. Rep. 77-7, 16 pages.

19

O'Driscoll, C.F.; Collins, C.J.; and Tuach, J.T.; 1988: Volcanic-hosted, high-alumina, epithermal environments and the St. Lawrence fluorite deposit in the Avalon Zone, eastern Newfoundland. GAC/MAC/CSPG Field Trip Guidebook A-5, 76 pages. Pearse, G.H.K.; 1971: Exploration report on Nalco lot 4, mainly in the north Lawn area, Newfoundland. Unpublished report Radex Minerals Limited and Newfoundland and Labrador Corporation Limited. Newfoundland and Labrador Geological Survey, Assessment File NFLD/0901, 30 pages. Smith, W.S.;1938: Report on St. Lawrence Fluorspar. NF. Miner, Dev. Div., Intern Rep. (GSB# 001L/14/005) Smith, W.S., 1945: Geological Progress Report for the Period 1-30 July, 1945, Newfoundland Fluorspar Limited, St. Lawrence, Newfoundland, 14 August 1945, p. Smith, W.S.; 1946a: Geological Progress Report for July-1946, Newfoundland Fluorspar Limited, St. Lawrence, Newfoundland, 31 August 1946, p. 3, 4 Smith, W.S.; 1946b: Geological Progress Report for August and September-1946, Newfoundland Fluorspar Limited, St. Lawrence, Newfoundland, 29 October 1946, p.2 Smith, W.S.;1946c: Geological Progress Report for May-1946, Newfoundland Fluorspar Limited, St. Lawrence, Newfoundland, 18 June 1946, p.4 Smith, W.S.;1947: Geological Progress Report January through May 1947, Newfoundland Fluorspar Limited, St. Lawrence, Newfoundland, 2 June 1947, p.8 Smith, W.S. 1957: Fluorspar at St. Lawrence, Newfoundland. Newfoundland Fluorspar Ltd.; NF. Miner. Dev, Div., Assess. File 00 1 U 14/0016. Strong, D.F ; O'Brien, S.J. ; Taylor, S.W.; Strong, P.G,; and Wilton, D.H.; 1978: Geology of the Marystown (I M/3) and St. Lawrence (I L/ 14) Map Areas, Newfoundland. NF, Miner. Dev. Div., Rep. 77-8, 81 pages. Teng, H. C . and Strong, D, F.; 1976: Geology and geochemistry of the St. Lawrence peralkaline granite and associated fluorite deposits, southeast Newfoundland. Can. J. Earth Sci , v. 113, p.1374-1385, (GSB# NFLD/1 121) Tilsley, J,E,. 1971 Exploration for Fluorspar, An Explanation of Techniques and Discussion of Fluorine Geochemistry. NF. Miner. Dev, Div., Assess. File 001L/14/0067, Tilsley, J,E.; 1972b Hydrogeochemical Reconnaissance Survey on Property of the Newfoundland Fluorspar Ltd on The St. Lawrence Area, Newfoundland. NF. Miner. Dev, Div . Assess File 001 L/ 14/0069,

20

Tilsley, J E., 1972e Fluorspar Exploration Proposal St. Lawrence, Newfoundland Property, Aluminium Company of Canada. Alcan Archive records. Tilsley, J.E 1 1973. Report on Ground EM and Geochemical Surveys in the Shoal Cove Pond Area of the St Lawrence Area, Newfoundland. NF, Miner. Dev. Div., Assess. File 001L/14/0065. Tilsley, J,E.. 1973c Report on geological, geophysical and geochemical surveys and DDH records of Cera-Nalco Lot 4 in the St, Lawrence Area, Newfoundland. NF, Miner. Dev. Div , Assess. File Nfld/0900, Tilsley, J.E.', 1974: Report on CERA-NALCO Fluorspar Exploration Program from 1971 to 1974 on Nalco Lot 4 on the Burin Peninsula, Newfoundland. NF. Miner. Dev. Div., Assess, File NFLD/0898. Tilsley, J.E.; 1975: Application of geophysical, geochemical and deep overburden sampling techniques to exploration for fluorspar in glaciated terrain; pp. 126-133 in Prospecting in areas of Glaciated Terrain 1975; Jones, M.J. (editor). (GSB# Nfld/0900) Van Alstine, R. E., 1939: Summary Field Report, St, Lawrence Area, Newfoundland. NF Miner. Dev. Div, Intern. Rep. (058# 1L/14/007) Van Alstine, R. E. , 1944: The Fluorspar Deposits of St. Lawrence, Newfoundland. Econ, Geol., Vol, 39, No. 2, pp. 109-132, (GSB#001L/14/0009) Van Alstine, R, E.; 1948: Geology and Mineral Deposits of the St. Lawrence Area, Burin Peninsula, Newfoundland. Nfld. Geol. Surv. Bull. No. 23, 73 pages. (GSB# 1014/10) Vatcher, S.V., and Evans, D., 2009, First and Second Year Assessment Report Burin Project: Licences 010689M, 013251M, 012703M, 012704M, 013083M, 013084M, 013085M, 013086M, 013090M, 013091M, 013095M, 013118M, 013119M, 013120M, 013121M, 013231M, 013253M, 013821M, 013870M, 013871M, 013876M, 013880M, 013902M, 013903M, 013904M, 013965M, 013906M, 014529M, 015455M, 015496M, 014002M, 014003M, 014004M, 014007M, 014008M, 014009M, 014010M, NTS 1L/13, 1L/14, 1M/3 1M/4 and 1M/15. Confidential Assessment Report supplied by Golden Dory Resources Ltd. Williamson, D.H.; 1956: The geology of the fluorspar district of St. Lawrence, Burin Peninsula, Newfoundland (12 maps), NF Min. Res. Div. Internal Rep. (GSB# 1L/14/15)

Burin Minerals Ltd. Geology December 18, 1995.

APPENDIX 1 Maps: (Base maps and Digital Air Photos from Dept. of Environment and

Conservation, Surveys and Mapping Division)

Newfoundland Fluorspar Exploration Ltd.St. Lawrence Claims

NewFluorEx.com Dec 12, 2014 SL14-1

Location ofProject

Drafting by: G. Stefanuk


NewFluorEx.com Dec 12, 2014 SL14-2

1:25,000 Scale Maps

SL14-4

SL14-5

Key ofMap Sheets

1:10,000 Scale Maps

SL14-6

SL14-8

Legend

SL14-7

1:2,000 Scale Map1:5,000 Scale Maps

20000 2000

Scale: 1 : 150,000

1000

SL14-9SL14-14

SL14-13

SL14-11

SL14-12

SL14-10

LSL-2 to LSL-6

22121M

21055M

21479M

NSL-103

Legend

As-Drilled Locations Diamond Drilling Locations

Drafting by: G. StefanukNewFluorEx.com Dec 12, 2014 Map SL14-3

Program by: Alex Harris, B. Sc.

Map: SL14-2 Diamond Drilling LocationsMap: SL14-13 Tarefare Vein ExtensionMap: SL14-14 Little St. LawrenceMap: SL14-15 Little St. Lawrence SectionMap: SL14-16 Diamond Drilling Specifications

Approx. Locationof Wind Turbines

Highw

ay #220

Proposed Drilling Locations

Town ofSt. Lawrence

Approx. Location of Wind Turbines

Newfoundland FluorsparExploration Ltd.

0 1 km

Scale: 1 : 50,000

SL14-14

SL14-13

5198

000m

N51

9900

0m N

5200

000m

N52

0100

0m N

622000m E 623000m E620000m E 624000m E

NTS Map Reference: St. Lawrence 1L/14UTM Zone 21, Nad 27

LegendMineral Licence Boundary

Historical Diamond Drill HoleDDH

Axis of Conductor

Fluorite Mineral OccurrencesLinear Structure From Air Photo

500m0 250

Scale: 1 : 25,000

Soil Samples & Observations 2014SSL203

Water Sample Locations 2014WSL106 Previous Trenches

Trench

DDH-A2

O

LittleSt. LawrenceOccurrence

SalmonHoleVein

Doctors Pondand Scrape Vein

Ryan HillVein

y 220To n of

DDH

DDH 72-20

DDH-BD2DDH-BD1

DDHTrench

Cranberry BogVeinH

ighway

220

Lawn Road Veins

New Black DuckVein

BoxheaterVein

Ryan FlatsTrenches

PreviousTrenching

Old Road

Black DuckVein

Church Vein

Licence:21479M

Licence: 22121M

BrecciaSSL200

SSL201

SSL202

SSL203

SSL204

SSL206SSL208

SSL210SSL212

SSL214

Tr11Tr4 to Tr10

TrATrB

TrQ

TrR to TrZ

WSL100

WSL101

WSL102WSL103

WSL104

WSL105

WSL106 WSL107

WSL108

WSL109

Hospital

Newfoundland FluorsparExploration Ltd.Licence Numbers:

22121M, 21479M,21055M


NewFluorEx.com Dec 14, 2014 Map: SL14-4

2014 Water and Soil SampleLocations and Traverses


621000m E619000m E618000m E

Licence:21055M

Fault Line

Exploration Traverse Location

2014 Water Sampling,Proposed HLEM Survey and,

Bedrock Geology, Licence 21055M

Mine CoveVein

Renamed AGSVein

HistoricalGrebes Nest

Vein Mine Lease

TS-20

TS-36

TS-18

TS-9

TarefareVein Mine

Lease

BlakesBrookVeins

Trail

Highw

ay

220

Old Road

TarefareVein

HopeVein

TarefareShaft 2

3+50

W

Base 0

+0

8+50

W

23+5

0W

28+5

0W

32+0

1.6W

Little Lawn HarbourOccurrence

Licence:21055M

0.210.30

0.180.12

0.31

0.220.21

0.12

0.27

0.22

0.31

0.300.310.13

0.160.11

0.190.13

0.31

0.130.23

0.21 0.27

0.09

0.20

0.110.22

0.080.19

0.18

0.170.38

0.090.10

0.12 0.10

0.330.11

0.210.55

0.30

0.150.19

0.410.26

0.220.45

0.300.30

0.220.27

0.19

0.310.51

0.480.110.19

0.10

0.30

0.20

0.29

0.390.14

0.19 0.18 0.080.120.35

0.250.29

0.110.4

0.050.270.060.21

0.200.28

0.090.28

0.080.390.05

0.060.10

0.10

0.100.12

0.25

0.13

0.34

0.330.07

0.130.26

0.18

0.06 0.26

0.31

0.27 0.29

0.250.310.19

0.04 0.110.01 0.100.09

0.400.52

0.500.120.18

NSL-101-2

-ND

-ND

0.20

0.26

-ND

-ND

-ND

0.30

5195

000m

N

618000m E 619000m E

5196

000m

N

Axis of ConductorFault LineHistorical Diamond Drill HolesTS-36

Mineral Licence BoundaryCFI Mining Lease


5198

000m

N

617000m E616000m E

5197

000m

N

Marine Siliciclastic SedimentsSt. Lawrence Granite

5199

000m

N

Proposed HLEM Survey Line

Previous Newfluorex Drill Holes



NTS St. Lawrence 1L/14UTM Zone 21, Nad 27

Legend

Fluorite Mineral Occurrences

Linear Structure From Air Photo

500m0 250

Scale: 1 : 25,000


Topographic Lineament

2014Water Sample Fluorine ppm0.2

Exploration Traverse LocationProposed HydrochemichalSampling Location

Fluorine In Water Anomaly >= 0.3 mg/L

Historical Water Sample ppm1.14


Drafting by: Gordon StefanukProgram by: Alex Harris, B. Sc.

NewFluorEx.com Dec 14, 2014 Map: StL14-6

2014 Fluoride in WaterLicence 21479M South

2014 Water Sample Fluorine mg/LMineral Licence Boundary


Diamond Drill HoleDDH

Axis of Conductor


Linear Structures From Air Photos

Fault Line

1.14

Fluorine In Water Anomaly >=0.3 mg/L

107 m

122 m

137 m152 m

61 m

0.020.29

0.21

0.71

0.16

0.15

0.21

0.70.180.17

00.3

0.900.100.09

0.29

DDH-BD2DDH-BD1

-ND

0.16

0.25

0.07

0.07

0.03

0.010.05

0.16

0.18

0.03 0.09

0.05 0.07

0.12

1.00

0.55

0.70

0.95

0.25

0.19

0.25

0.21

0.20

-ND-ND

-ND

-ND

0.200.50

0.60

-ND

-ND

-ND-ND

-ND

-ND

0.20

0.01

0.45

0.62

0.22

0.22

0.150.31

0.330.30

0.190.19

0.19

0.19

0.500.35

0.61

0.210.20

0.82

0.71

CranberryBog Vein

wn RoadVeins

BlacV

NewBlack Duck

Vein

BoxheaterVein

Ryan FlatsTrenching

PreviousTrenching

Licence:21479M

See Detail WaterDrawing StL14-9

Power

Lin

e


5199

000m

N51

9950

0m N

5200

000m

N51

9850

0m N

622500m E621000m E 621500m E 622000m E

NTS Map Reference:St. Lawrence 1L/14

UTM Zone 21, Nad 27

Legend

0 250m

Scale: 1 : 10,000

125

ProposedHydrochemichalSampling Location

Historical Trenching

5199

000m

N

5199

500m

N

624000m E

5200

000m

N52

0100

0m N




2014 Fluoride in WaterLicence 21479M North

91 m107 m

122 m

137 m152 m

76 m

0.20

0.10

-ND

-ND

0.62

0.90

0.18

0.52

0.01

0.20

0.401.01

0.15

0.13

0.200.14

0.500.24

0.07

ND

Vein

Ryan HillVein

0.05 0.13

-ND

0.16

0.25

0.25

0.12

0.07

0.14

0.10

0.16

0.12

0.08

0.09 0.20

0.07

0.03

0.010.05

0.15

0.40

0.230.16

0.13

0.18

0.03 0.090.10

0.05 0.070.03

0.12

-ND

0.31 0.15

0.18

0.18

0.25 0.150.09

0.15

0.20

-ND-ND

Ryan FlatsTrenching

Licence:21479M

Power

Lin

e52

0050

0m N

620500m E 621000m E 621500m E 622000m E




Axis of Conductor



Fault Line

1.14




UTM Zone 21, Nad 27

Legend

0 250m

Scale: 1 : 10,000

125



622500m E 623000m E 623500m E 624000m E




2014 Fluoride in WaterLicence 21057M

Trench

15 m

76 m

61 m

Trenches

DDH-A2

Strip2Strip1

0.30

0.60

0.96

0.500.98

0.81 0.990.52

1.151.62

0.36 1.62

0.510.21

0.30

1.211.92

0.652.70

1.110.18

0.490.50 0.32

0.37

0.411.07

1.070.60

1.000.74 0.45

0.900.82

1.08

0.440.410.70

1.12

0.97

3.300.5

0.35

0.55

0.60

0.300.300.60

0.600.10

1.200.20

-ND0.300.16

0.701.31 1.03

0.28

0.591.38

0.780.52

0.90 1.16

1.45

0.89

1.19

0.38

0.200.39

0.39

0.20

0.301.120.48

0.17

0.200.230.18

0.10 0.11

0.09

0.14 0.13

0.130.80

1.41

1.80See DetailDrawing LSL14-11

LittleSt. LawrenceOccurrence

Salmon HoleVein

-ND

1.31.9

0.020.29

0.21

0.71

0.16

0.15

0.21

1.17

0.710.180.17 0.30

0.120.38

0.10

0.90

0.13 0.21

0.100.09

0.320.29

1

DDH-BD2DDH-BD1 Black Duck

Vein

Licence:22121M

1.141.60

1.210.57

Power

Lin

e

LSL-1

5199

000m

N51

9950

0m N

5200

000m

N52

0100

0m N

5200

500m

N




Axis of Conductor



Fault Line

1.14




UTM Zone 21, Nad 27

Legend

0 250m

Scale: 1 : 10,000

125






2014 Fluoride in WaterLicence 21479M

2014 Water Sample Fluorine ppmMineral Licence Boundary



Axis of Conductor



Fault Line

1.14

Fluorine In Water Anomaly > 0.3

0.25

0.19

0.25

0.21

0.20

-ND-ND

-ND

-ND

-ND

-ND-ND

-ND

-ND

0.20

0.01

0.45

0.62

0.22

0.22

0.150.31

0.330.30

0.190.19

0.19

0.19

0.500.35

0.61

0.210.20

0.82

0.71

Lawn RoadVeins

BoxheaterVein

CranberryBog Vein


5198

000m

N51

9850

0m N

621000m E 621500m E


UTM Zone 21, Nad 27

Legend


0

Scale: 1 : 5,000

100m


5199

500m

N


NewFluorEx.com Dec 27, 2014 Map SL14-10

120

BDLBDL

120 220

BDL110

100

6xNS

4xNSNS

210

Vein

Ryan HillVein

Ryan FlatsTrenching

Licence:21479M

Power

Lin

e

N/A160N/A

180N/ABDLN/A160

N/A13052

0000

0m N

5200

500m

N52

0100

0m N

621000m E 621500m E620500m E

Mineral Licence Boundary

Axis of ConductorLinear Structures From Air Photos

Fault Line


2014 Total Fluoride (F) mg/kg130

2011&13 Total Fluoride (F) mg/kg130

2014 Soil Sample Values,Proposed HLEM, AMT Survey

622000m E

5199

000m

N

Proposed Diamond Drill HoleLP-01



Legend Fluorite Mineral OccurrencesPrevious TrenchesPublic Water Supply Area

Proposed HLEM Survey Line

0 250m

Scale: 1 : 10,000

125

Projected Line of Ryan Hill Vein

2014 GPS Traverse Location

Proposed AMT Test Line

Fluorine In Siol Contour Int. 150 mg/kg

Historical TrenchingProposed Soil SamplesNote: NS = No Sample Obtained

NTS St. Lawrence 1L/14UTM Zone 21, Nad 27

0 50m

Scale: 1 : 2,000

Little St. LawrenceWater and Soil Sample Values

5199

000m

N51

9910

0m N

623400m E

15 m

15 m46

m

30 m

Strip2

Strip1

1.14

1.60

LSL-3

LSL-5

LSL-4

LSL-2

LSL-6

BDL

BrecciaBDL

130330BDL-ND

1.3

1.9


NewFluorEx.com Dec 14, 2014 Map:LSL14-11

LSL-1 Previous Newfluorex Drill Holes

Axis of Conductor


Fault Line



St. Lawrence 1L/14 UTM Zone 21, Nad 27

Legend


Exploration Traverse Location

623500m E 623600m E

5198

900m

N

2014 Water Sample Fluorine ppm

Historical Water Sample ppm

0.2

1.14

220 2014 Total Fluoride (F) mg/kg

623300m E

Proposed Cut Line & Sampling

Proposed Diamond Drill HoleLSL-6

Propposed Stripping LocationStrip1

Soil Sample Contour 150 mg/kgAs Drilled Diamond Drill HoleLSL-1

5199

000m

N51

9850

0m N

621500m E 622000m E





Overlay of Geofile MapReference, 001L_0075_ST_A_1079

Cranberry Bog Area HistoricalTrenching Overlay 2014 GPS Points

Legend

Historical Claim BoudaryPrevious Trenching Locations

2014 GPS Location NAD27Tr#

Axis of ConductorLinear Structures From Air Photos

Fault Line

Fluorine In Water Anomaly > 0.3 mg/L

0

Scale: 1 : 5,000

100m

Topgraphic Lineament

5196

000m

N51

9650

0m N

618500m E618000m E

Axis of Conductor



Fault Line

Mineral Licence Boundary



Tarefare Vein Extension PorposedDiamond Drill Hole

Proposed Diamond Drill HoleNSL-NSL- Previous Newfluorex Drill Holes

0 100m

Scale: 1 : 5,000



Legend

Propopsed AMT test Location

Fluorine In WaterAnomaly >= 0.3 mg/kg

0 100m

Scale: 1 : 5,000

Little St. LawrenceProposed Drilling Locations

5199

500m

N51

9900

0m N

623000m E 623500m E

LittleSt LawrenceOccurrence

6.0m BrecciaCaF2 to 40%

LSL-3

LSL-5

LSL-4

LSL-2

LSL-6

LSL-1

Proposed Diamond Drill HoleLSL-6



LSL-1 Previous Newfluorex Drill HolesMineral Licence Boundary

Axis of Conductor


Fault Line

Fluorine In Water Anomaly > 0.3 mg/L



Legend


2013 GPS Traverse Location

Proposed Cut Line

Proposed Diamond Drill HolesAnd As-Drilled LSL-1 Section

C/L

Lin

ear

Str

uctu

re(3

25 D

eg. A

zim

uth)

0 m (Sea Level)

-200m Elev

Ground Elevation100m 0

m

100m

Gra

nite

Bre

ccia

St. L

awre

nce

Riv

er

-100m Elev

St. Lawrence Granite Vein Structure - Dominantly blastonite and

granite breccia with minor purple fluorite

St. Lawrence Granite

Overburden

DrillstringTest Results: Mag. N. Grid N.Depth Dip Azimuth Azimuth130 43.6 262.8 240.3

LSL-1From To Length(m) %CaF2 Smpl#117.75 118.75 1.00 21.8 1000118.75 119.75 1.00 24.0 1001119.75 120.45 0.70 13.6 1002120.45 120.95 0.50 11.4 1003120.95 121.52 0.57 17.2 1004121.52 122.25 0.73 11.1 1005122.25 123.00 0.75 7.0 1006123.00 124.00 1.00 3.4 1007

200m

LS

L-1

As-

Dri

lled

Pro

pose

dL

SL

-6

Pro

pose

dL

SL

-2 &

LSL

-3


NewFluorEx.com Dec 14, 2014 Section: SL14-15

Licence UTM E UTM N Azimuth Dip Deg. Depth mHole #LSL-1 235 -45 130

UTM Coordinate System NAD 27Azimuth based on Grid NorthSection Facing: 325 degrees (C/L Linear Structure)

22121M

0 50m

Scale: 1 : 2,000

623541 5198947

Drafting by: G. StefanukProgram by: Alex Harris, B. Sc.

UTM Coordinate System NAD 27, Azimuth to Grid North

Licence UTM E UTM N Azimuth Dip Deg. Depth mLSL-1 235 -45 1305198947623541

NSL-101-2 235 -80 6015196146618164

Hole #

21055M

22121M



Licence UTM E UTM N Azimuth Dip Deg. Depth mLSL-2 235 -45 45623418 5198985LSL-3 235 -70 805198985623418

LSL-4 235 -45 455199067623360

Hole #

22121M

22121M

22121M

Drilling Completed 2011

Proposed Drilling

LSL-5 235 -70 80623360 5199067LSL-6 55 -45 1505198947623541

NSL-101-3 50 -55 620519601361781721055M

22121M

22121M


Diamond DrillingSpecifications

APPENDIX 2 Certificates of Analysis

METHOD SUMMRY Total Fluoride in Soil The soil sample is fused with sodium hydroxide and then extracted. The fluoride in extract is determined potentiometrically using a combination-specific ion fluoride electrode containing a silver/silver chloride reference electrode. The agent used for the extraction is NaOH, DI Water, and concentrated HCl. __________________________________________________________________________ Fluoride in Water SOP #: ATL SOP 43 Reference: Standard Methods, 20th ed. Method 4500 - F- C, 1998 1. Scope and Application This method is applicable for the determination of fluoride in water matrices. Total Fluoride requires distillation prior to analysis to meet USEPA wastewater discharge requirements. Some difficulty is encountered with samples that are highly basic/acidic or samples that have dissolved solids above 10,000 mg/L. The Reporting Detection Limit (RDL) is 0.10 mg/L for water samples. 2. Summary of Method An ion specific electrode is used to measure fluoride concentration. The fluoride electrode measures the ion activity of fluoride in solution rather than concentration. Fluoride ion activity depends on the solution rather than the concentration. Fluoride ion activity depends on the solutions total ionic strength and pH, and on fluoride complexing species. Adding an appropriate buffer provides uniform ion strength background, adjusts pH, and breaks up complexes so in effect, the electrode measures concentration. 3. Quality Assurance Reagent blanks, standard reference materials, and method spikes are analyzed in the same manner as mentioned above for the samples. Spiking of samples at a level appropriate to the matrix is performed at a frequency of 5%. Duplicate samples are also analyzed at a frequency of 5 %.

Your Project #: DB4F5084

Attention: BEDFORD CLIENT SERVICEMAXXAM ANALYTICS200 BLUEWATER ROAD, SUITE 105BEDFORD, NSCANADA B4B 1G9

Report Date: 2014/09/21Report #: R1646462

Version: 1

CERTIFICATE OF ANALYSIS

MAXXAM JOB #: B476654Received: 2014/08/29, 08:57

Sample Matrix: Soil# Samples Received: 10

Date DateAnalyses Quantity Extracted Analyzed Laboratory Method Analytical MethodTotal Fluoride 10 N/A 2014/09/20 AB SOP-00051 / AB SM 22 4500 F-C m

SOP-00005

* RPDs calculated using raw data. The rounding of final results may result in the apparent difference.

Encryption Key

Please direct all questions regarding this Certificate of Analysis to your Project Manager.

Sherlyne Sim, B.Eng, Project ManagerEmail: [email protected]# (780) 577-7113

====================================================================Maxxam has procedures in place to guard against improper use of the electronic signature and have the required "signatories", as per section5.10.2 of ISO/IEC 17025:2005(E), signing the reports. For Service Group specific validation please refer to the Validation Signature Page.

Total cover pages: 1

Maxxam Analytics International Corporation o/a Maxxam Analytics Edmonton: 9331 - 48th Street T6B 2R4 Telephone(780)577-7100 Fax(780)450-4187

Page 1 of 5

MAXXAM ANALYTICSMaxxam Job #: B476654 Client Project #: DB4F5084Report Date: 2014/09/21

Sampler Initials: PAF

RESULTS OF CHEMICAL ANALYSES OF SOIL

Maxxam ID K M 2 6 9 7 K M 2 6 9 7 K M 2 6 9 8 K M 2 6 9 9 K M 2 7 0 0Sampling Date 2014/08/22 2014/08/22 2014/08/22 2014/08/22 2014/08/22

13:20 13:20 13:25 13:55 14:45 U N I T S XH2622-01R XH2622-01R XH2623-01R XH2624-01R XH2625-01R RDL QC Batch

\ SSL 200 \ SSL \ SSL 201 \ SSL 202 \ SSL 203200 Lab-Dup

ANIONS

Total Fluoride (F) mg/kg <100 <100 130 330 <100 100 7646807

RDL = Reportable Detection Limit

Maxxam ID K M 2 7 0 1 K M 2 7 0 2 K M 2 7 0 3 K M 2 7 0 4 K M 2 7 0 5Sampling Date 2014/08/22 2014/08/23 2014/08/23 2014/08/23 2014/08/23

15:05 10:10 10:15 12:20 13:30 U N I T S XH2626-01R XH2627-01R XH2628-01R XH2629-01R XH2630-01R RDL QC Batch

\ SSL 204 \ SSL 206 \ SSL 208 \ SSL 210 \ SSL 212

ANIONS

Total Fluoride (F) mg/kg <100 160 180 <100 160 100 7646807


Maxxam ID K M 2 7 0 6Sampling Date 2014/08/23

14:00 U N I T S XH2631-01R RDL QC Batch

\ SSL 214

ANIONS

Total Fluoride (F) mg/kg 130 100 7646807


Page 2 of 5

MAXXAM ANALYTICSMaxxam Job #: B476654 Client Project #: DB4F5084Report Date: 2014/09/21


Package 1 2.0°CEach temperature is the average of up to three cooler temperatures taken at receipt

General Comments

Results relate only to the items tested.

Page 3 of 5

MAXXAM ANALYTICSAttention: BEDFORD CLIENT SERVICE Client Project #: DB4F5084P.O. #: Site Location:

Quality Assurance ReportMaxxam Job Number: EB476654

QA/QC DateBatch AnalyzedNum Init QC Type Parameter yyyy/mm/dd Value Recovery UNITS QC Limits

7646807 CH7 Matrix Spike[KM2697-01] Total Fluoride (F) 2014/09/20 83 % 75 - 125QC Standard Total Fluoride (F) 2014/09/20 93 % 75 - 125Spiked Blank Total Fluoride (F) 2014/09/20 97 % 75 - 125Method Blank Total Fluoride (F) 2014/09/20 <100 mg/kgRPD [ K M 2 6 9 7 - 0 1 ] Total Fluoride (F) 2014/09/20 NC % 35

Duplicate: Paired analysis of a separate portion of the same sample. Used to evaluate the variance in the measurement.Matrix Spike: A sample to which a known amount of the analyte of interest has been added. Used to evaluate sample matrix interference.QC Standard: A sample of known concentration prepared by an external agency under stringent conditions. Used as an independent check of methodaccuracy.Spiked Blank: A blank matrix sample to which a known amount of the analyte, usually from a second source, has been added. Used to evaluate methodaccuracy.Method Blank: A blank matrix containing all reagents used in the analytical procedure. Used to identify laboratory contamination.NC (Duplicate RPD): The duplicate RPD was not calculated. The concentration in the sample and/or duplicate was too low to permit a reliable RPDcalculation (one or both samples < 5x RDL).

Maxxam Analytics International Corporation o/a Maxxam Analytics Edmonton: 9331 - 48th Street T6B 2R4 Telephone(780)577-7100 Fax(780)450-4187

Page 4 of 5

Validation Signature Page

Maxxam Job #: B476654

The analytical data and all QC contained in this report were reviewed and validated by the following individual(s).

Maryse Maurice, Scientific Specialist

====================================================================Maxxam has procedures in place to guard against improper use of the electronic signature and have the required "signatories", as per section 5.10.2 ofISO/IEC 17025:2005(E), signing the reports. For Service Group specific validation please refer to the Validation Signature Page.

Page 5 of 5

MAXXAM JOB #: B4F5084Received: 2014/08/26, 10:43

CERTIFICATE OF ANALYSIS

Report Date: 2014/09/22Report #: R3164088

Version: 2

Attention:Alex Harris

NewFluorEx5-1035 Boychuk DrSaskatoon, SKCANADA S7H5B2

Your C.O.C. #: B 156956, B 156957

ST. LAWRENCESite Location:

Sample Matrix: Water# Samples Received: 10

ReferenceLaboratory MethodDateAnalyzed

DateExtractedQuantityAnalyses

SM 22 4500-F- C mATL SOP 000432014/09/02N/A10Fluoride (1)

* RPDs calculated using raw data. The rounding of final results may result in the apparent difference.

(1) This test was performed by Maxxam Bedford

Encryption Key

Please direct all questions regarding this Certificate of Analysis to your Project Manager.Heather Macumber, Project ManagerEmail: [email protected]# (902)420-0203 Ext:226==================================================================== Maxxam has procedures in place to guard against improper use of the electronic signature and have the required "signatories", as per section 5.10.2 of ISO/IEC 17025:2005(E), signing the reports. For Service Group specific validation please refer to the Validation Signature Page.

Total Cover Pages : 1Page 1 of 6

Maxxam Analytics International Corporation o/a Maxxam Analytics 49-55 Elizabeth Ave, Suite 101A, St.John's, NL, Canada A1A 1W9 Tel: 709-754-0203 Toll Free: 888-492-7227 Fax: 709-754-8612 www.maxxamanalytics.com

Maxxam Job #: B4F5084Report Date: 2014/09/22

NewFluorEx



RESULTS OF ANALYSES OF WATER

ND = Not detected

MAC: Guideline - Summary of Guidelines for Canadian Drinking Water Quality (SGCDWQ), Health Canada, Aug. 2012.

A= Maximum Acceptable Concentration (MAC) - established for substances that are known or suspected to cause adverse effects on health.

AO= Aesthetic Objectives (AO) - apply to characteristics of drinking water that can affect its acceptance by consumers or interfere with practices forsupplying good quality water.

Note 1 Turbidity guideline value of 0.3 NTU based on conventional treatment system. For slow sand or diatomaceous earth filtration 1.0 NTU and formembrane filtration 0.1 NTU.Note 2 Aluminium guideline value of 0.1 mg/L is for treatment plants using aluminium-based coagulants, 0.2mg/L applies to other types of treatmentsystems.

QC Batch = Quality Control Batch


37322370.100.260.20NDNDND1.31.91.5mg/LDissolved Fluoride (F-)

Inorganics

QC BatchRDLWSL 106WSL 105WSL 104WSL 103WSL 102WSL 101WSL 100MACUnits

B 156957B 156957B 156957B 156957B 156957B 156957B 156957COC Number

2014/08/24 10:27

2014/08/24 10:05

2014/08/24 09:50

2014/08/24 09:35

2014/08/22 14:00

2014/08/22 13:00

2014/08/22 09:45

Sampling Date

XH2639XH2638XH2637XH2636XH2635XH2634XH2633Maxxam ID

Page 2 of 6



NewFluorEx



RESULTS OF ANALYSES OF WATER

ND = Not detected

MAC: Guideline - Summary of Guidelines for Canadian Drinking Water Quality (SGCDWQ), Health Canada,Aug. 2012.

A= Maximum Acceptable Concentration (MAC) - established for substances that are known or suspected tocause adverse effects on health.

AO= Aesthetic Objectives (AO) - apply to characteristics of drinking water that can affect its acceptance byconsumers or interfere with practices for supplying good quality water.

Note 1 Turbidity guideline value of 0.3 NTU based on conventional treatment system. For slow sand ordiatomaceous earth filtration 1.0 NTU and for membrane filtration 0.1 NTU.Note 2 Aluminium guideline value of 0.1 mg/L is for treatment plants using aluminium-based coagulants,0.2mg/L applies to other types of treatment systems.

QC Batch = Quality Control Batch


37322440.10ND3732237NDND1.5mg/LDissolved Fluoride (F-)

Inorganics

QC BatchRDLWSL 109QC BatchWSL 108WSL 107MACUnits

B 156957B 156957B 156957COC Number

2014/08/24 11:21

2014/08/24 11:10

2014/08/24 10:50

Sampling Date

XH2642XH2641XH2640Maxxam ID

Page 3 of 6



NewFluorEx



GENERAL COMMENTS

Each temperature is the average of up to three cooler temperatures taken at receipt

21.6°CPackage 1

Results relate only to the items tested.

Page 4 of 6



NewFluorEx



QUALITY ASSURANCE REPORT

QC LimitsUnits RecoveryValueDate

AnalyzedParameterQC TypeInitQA/QCBatch

80 - 120%992014/09/02Dissolved Fluoride (F-)Matrix SpikeKMC373223780 - 120%1022014/09/02Dissolved Fluoride (F-)Spiked BlankKMC3732237

mg/LND ,RDL=0.10

2014/09/02Dissolved Fluoride (F-)Method BlankKMC3732237

25%NC2014/09/02Dissolved Fluoride (F-)RPDKMC373223780 - 120%1032014/09/02Dissolved Fluoride (F-)Matrix SpikeKMC373224480 - 120%1062014/09/02Dissolved Fluoride (F-)Spiked BlankKMC3732244

mg/LND ,RDL=0.10

2014/09/02Dissolved Fluoride (F-)Method BlankKMC3732244

25%NC2014/09/02Dissolved Fluoride (F-)RPDKMC3732244

NC (Duplicate RPD): The duplicate RPD was not calculated. The concentration in the sample and/or duplicate was too low to permit a reliable RPDcalculation (one or both samples < 5x RDL).

Method Blank: A blank matrix containing all reagents used in the analytical procedure. Used to identify laboratory contamination.

Spiked Blank: A blank matrix sample to which a known amount of the analyte, usually from a second source, has been added. Used to evaluate methodaccuracy.

Matrix Spike: A sample to which a known amount of the analyte of interest has been added. Used to evaluate sample matrix interference.

Duplicate: Paired analysis of a separate portion of the same sample. Used to evaluate the variance in the measurement.

Page 5 of 6



NewFluorEx



VALIDATION SIGNATURE PAGE

The analytical data and all QC contained in this report were reviewed and validated by the following individual(s).

Kevin MacDonald, Inorganics Supervisor

Maxxam has procedures in place to guard against improper use of the electronic signature and have the required "signatories", as per section 5.10.2 of ISO/IEC17025:2005(E), signing the reports. For Service Group specific validation please refer to the Validation Signature Page.

Page 6 of 6


APPENDIX 3 GPS Data Listing

Fluoride in Water (F) mg / Litre

2014 (WSL) and Historical (HWS) Grid: UTM

St. Lawrence Datum: NAD27 Canada

Name Type mg / L Date Time Zone UTM East North Elev. Units

Licence: 22121M

WSL100 Surface 1.9 22‐Aug‐14 09:45AM 21 T 623483 5198912 5 m


WSL102 Surface ND 22‐Aug‐14 14:00PM 21 T 623450 5198886 27 m

Licence: 21055M

WSL103 Surface ND 24‐Aug‐14 09:35AM 21 T 618402 5198685 89 m







ND = Not Detected

St. Lawrence

www.NewFluorEx.com

1 of 1

Fluoride in Water (F) mg / Litre Licences: 22121M and 21479M

2010 ‐ 2011 (WSL) and Historical (HWS) Grid: UTM



2011 Water Samples

WSL100‐11 Surface ND 27‐Jun‐11 2:16PM 21 T 620744 5200873 100 m

WSL101‐11 Well 3 28‐Jun‐11 10:39AM 21 T 622672 5201619 90 m

WSL102‐11 Surface 0.5 15‐Jul‐11 2:49PM 21 T 623471 5199817 22 m

WSL103‐11 Well 3.3 01‐Sep‐11 9:00AM 21 T 623541 5198948 1 m

2010 Water Samples





WSL005 Surface ND 05‐Aug‐10 9:32AM 21 T 621401 5198163 m














WSL020 Surface 0.1 05‐Aug‐10 12:14PM 21 T 614695 5201258 65 m












WSL032 Surface 0.3 06‐Aug‐10 9:13AM 21 T 622990 5199507 m

WSL033 Surface ND 06‐Aug‐10 9:17AM 21 T 623116 5199529 m


ND = Not Detected

St. Lawrence

www.NewFluorEx.com

1 of 8



























WSL057 Surface 1 12‐Aug‐10 8:07AM 21 T 624035 5198534 5 m


















ND = Not Detected

St. Lawrence

www.NewFluorEx.com

2 of 8





Historical Water Samples

HWS012 Surface 0.9 1972‐74 21 T 623873 5198581 m

HWS013 Surface 1.16 1972‐74 21 T 624000 5198583 m

HWS015 Surface 0.52 1972‐74 21 T 623878 5198683 m

HWS016 Surface 0.78 1972‐74 21 T 623854 5198709 m

HWS069 Surface 1.41 1972‐74 21 T 623644 5199010 m

HWS070 Surface 0.57 1972‐74 21 T 623550 5199016 m

HWS071 Surface 1.21 1972‐74 21 T 623508 5199000 m

HWS072 Surface 1.14 1972‐74 21 T 623335 5199136 m

HWS073 Surface 1.6 1972‐74 21 T 623307 5199163 m

HWS074 Surface 1.38 1972‐74 21 T 623321 5199253 m

HWS075 Surface 0.59 1972‐74 21 T 623600 5199322 m

HWS076 Surface 1.19 1972‐74 21 T 623300 5199393 m

HWS077 Surface 1.12 1972‐74 21 T 623493 5199415 m

HWS078 Surface 0.3 1972‐74 21 T 623529 5199390 m

HWS079 Surface 0.48 1972‐74 21 T 623513 5199430 m

HWS080 Surface 0.17 1972‐74 21 T 623548 5199486 m

HWS081 Surface 0.7 1972‐74 21 T 623270 5199516 m

HWS082 Surface 0.2 1972‐74 21 T 623524 5199582 m

HWS083 Surface 0.2 1972‐74 21 T 623526 5199611 m

HWS084 Surface 0.38 1972‐74 21 T 623521 5199654 m

HWS085 Surface 0.39 1972‐74 21 T 623522 5199667 m

HWS086 Surface 0.39 1972‐74 21 T 623569 5199688 m

HWS087 Surface 0.89 1972‐74 21 T 623510 5199686 m

HWS088 Surface 0.09 1972‐74 21 T 623927 5199536 m

HWS089 Surface 0.16 1972‐74 21 T 622841 5199523 m

HWS090 Surface 0.13 1972‐74 21 T 623894 5199566 m

HWS091 Surface 0.13 1972‐74 21 T 623869 5199572 m

HWS092 Surface 0.1 1972‐74 21 T 623812 5199567 m

HWS093 Surface 0.14 1972‐74 21 T 623839 5199605 m

HWS094 Surface 0.18 1972‐74 21 T 623874 5199667 m

HWS095 Surface 0.49 1972‐74 21 T 623915 5199739 m

HWS096 Surface 0.23 1972‐74 21 T 623870 5199734 m

HWS097 Surface 0.32 1972‐74 21 T 623831 5199749 m

HWS098 Surface 0.35 1972‐74 21 T 623783 5199729 m

HWS099 Surface 0.5 1972‐74 21 T 623761 5199748 m

HWS100 Surface 0.3 1972‐74 21 T 623603 5199758 m

HWS101 Surface 0.21 1972‐74 21 T 623594 5199786 m

HWS102 Surface 0.51 1972‐74 21 T 623561 5199801 m

ND = Not Detected

St. Lawrence

www.NewFluorEx.com

3 of 8





HWS103 Surface 1.62 1972‐74 21 T 623461 5199749 m

HWS104 Surface 0.36 1972‐74 21 T 623438 5199770 m

HWS105 Surface 1.62 1972‐74 21 T 623442 5199791 m

HWS106 Surface 0.55 1972‐74 21 T 622812 5199468 m

HWS107 Surface 0.38 1972‐74 21 T 622709 5199520 m

HWS108 Surface 0.2 1972‐74 21 T 623752 5199659 m

HWS109 Surface 0.11 1972‐74 21 T 623930 5199567 m

HWS110 Surface 3.3 1972‐74 21 T 623475 5199817 m

HWS111 Surface 1.15 1972‐74 21 T 623414 5199820 m

HWS112 Surface 1.21 1972‐74 21 T 623506 5199858 m

HWS113 Surface 1.11 1972‐74 21 T 623551 5199866 m

HWS114 Surface 0.18 1972‐74 21 T 623586 5199860 m

HWS115 Surface 2.7 1972‐74 21 T 623536 5199876 m

HWS116 Surface 1.92 1972‐74 21 T 623440 5199919 m

HWS117 Surface 0.65 1972‐74 21 T 623551 5199946 m

HWS118 Surface 0.12 1972‐74 21 T 622660 5199576 m

HWS119 Surface 0.41 1972‐74 21 T 623474 5200009 m

HWS120 Surface 0.44 1972‐74 21 T 623688 5200024 m

HWS121 Surface 0.41 1972‐74 21 T 623685 5200047 m

HWS122 Surface 0.7 1972‐74 21 T 623699 5200077 m

HWS123 Surface 1.08 1972‐74 21 T 623615 5200057 m

HWS124 Surface 1.07 1972‐74 21 T 623554 5200060 m

HWS125 Surface 1.21 1972‐74 21 T 623772 5200181 m

HWS126 Surface 0.97 1972‐74 21 T 623859 5200275 m

HWS127 Surface 1.07 1972‐74 21 T 623531 5200111 m

HWS128 Surface 0.6 1972‐74 21 T 623521 5200139 m

HWS129 Surface 1 1972‐74 21 T 623504 5200220 m

HWS130 Surface 0.37 1972‐74 21 T 623316 5200238 m

HWS131 Surface 0.74 1972‐74 21 T 623538 5200270 m

HWS132 Surface 0.45 1972‐74 21 T 623572 5200276 m

HWS133 Surface 0.9 1972‐74 21 T 623494 5200354 m

HWS134 Surface 0.82 1972‐74 21 T 623437 5200346 m

HWS135 Surface 0.52 1972‐74 21 T 623207 5200235 m

HWS136 Surface 0.99 1972‐74 21 T 623211 5200273 m

HWS137 Surface 0.96 1972‐74 21 T 623245 5199825 m

HWS138 Surface 1.45 1972‐74 21 T 623276 5199584 m

HWS139 Surface 1.03 1972‐74 21 T 623108 5199461 m

HWS140 Surface 0.8 1972‐74 21 T 623152 5199571 m

HWS141 Surface 1.31 1972‐74 21 T 622970 5199485 m

HWS142 Surface 0.28 1972‐74 21 T 623016 5199594 m

HWS143 Surface 1.17 1972‐74 21 T 622688 5199600 m

ND = Not Detected

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HWS144 Surface 0.3 1972‐74 21 T 622669 5199625 m

HWS145 Surface 0.71 1972‐74 21 T 622642 5199657 m

HWS146 Surface 0.18 1972‐74 21 T 622607 5199629 m

HWS147 Surface 0.71 1972‐74 21 T 622588 5199620 m

HWS148 Surface 0.17 1972‐74 21 T 622580 5199634 m

HWS149 Surface 0.21 1972‐74 21 T 622524 5199429 m

HWS150 Surface 0.16 1972‐74 21 T 622518 5199510 m

HWS151 Surface 0.21 1972‐74 21 T 622489 5199496 m

HWS152 Surface 0.02 1972‐74 21 T 622499 5199442 m

HWS153 Surface 0.29 1972‐74 21 T 622475 5199465 m

HWS154 Surface 0.9 1972‐74 21 T 622617 5199722 m

HWS155 Surface 0.1 1972‐74 21 T 622590 5199726 m

HWS156 Surface 0.09 1972‐74 21 T 622577 5199767 m

HWS157 Surface 0.29 1972‐74 21 T 622537 5199790 m

HWS158 Surface 0.32 1972‐74 21 T 622574 5199815 m

HWS159 Surface 0.1 1972‐74 21 T 622641 5199836 m

HWS160 Surface 0.21 1972‐74 21 T 622440 5199886 m

HWS161 Surface 0.13 1972‐74 21 T 622318 5199903 m

HWS162 Surface 0.6 1972‐74 21 T 622431 5200336 m

HWS163 Surface 0.98 1972‐74 21 T 622626 5200383 m

HWS164 Surface 0.81 1972‐74 21 T 622648 5200255 m

HWS166 Surface 0.15 1972‐74 21 T 622382 5199250 m

HWS168 Surface 1 1972‐74 21 T 621965 5198178 m

HWS169 Surface 0.55 1972‐74 21 T 621968 5198411 m

HWS170 Surface 0.95 1972‐74 21 T 621879 5198454 m

HWS171 Surface 0.7 1972‐74 21 T 621824 5198586 m

HWS172 Surface 0.62 1972‐74 21 T 621433 5198101 m

HWS173 Surface 0.45 1972‐74 21 T 621418 5198095 m

HWS174 Surface 0.19 1972‐74 21 T 621371 5198156 m

HWS175 Surface 0.19 1972‐74 21 T 621356 5198154 m

HWS176 Surface 0.19 1972‐74 21 T 621357 5198168 m

HWS177 Surface 0.19 1972‐74 21 T 621349 5198177 m

HWS178 Surface 0.5 1972‐74 21 T 621349 5198189 m

HWS179 Surface 0.21 1972‐74 21 T 621312 5198154 m

HWS180 Surface 0.2 1972‐74 21 T 621306 5198168 m

HWS181 Surface 0.61 1972‐74 21 T 621321 5198169 m

HWS182 Surface 0.61 1972‐74 21 T 621328 5198185 m

HWS183 Surface 0.82 1972‐74 21 T 621325 5198200 m

HWS184 Surface 0.71 1972‐74 21 T 621342 5198200 m

HWS185 Surface 0.35 1972‐74 21 T 621335 5198218 m

HWS186 Surface 0.3 1972‐74 21 T 621316 5198272 m

ND = Not Detected

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HWS187 Surface 0.33 1972‐74 21 T 621304 5198276 m

HWS188 Surface 0.31 1972‐74 21 T 621299 5198289 m

HWS189 Surface 0.15 1972‐74 21 T 621304 5198307 m

HWS190 Surface 0.22 1972‐74 21 T 621259 5198300 m

HWS191 Surface 0.22 1972‐74 21 T 621251 5198313 m

HWS192 Surface 0.25 1972‐74 21 T 621232 5198330 m

HWS193 Surface 0.25 1972‐74 21 T 621213 5198341 m

HWS194 Surface 0.21 1972‐74 21 T 621202 5198355 m

HWS195 Surface 0.19 1972‐74 21 T 621193 5198376 m

HWS196 Surface 0.2 1972‐74 21 T 621168 5198401 m

HWS224 Surface 0.32 1972‐74 21 T 624284 5200912 m

HWS225 Surface 0.53 1972‐74 21 T 624240 5200914 m

HWS226 Surface 0.22 1972‐74 21 T 624317 5200933 m

HWS227 Surface 0.7 1972‐74 21 T 620469 5198436 m

HWS228 Surface 0.31 1972‐74 21 T 620407 5198453 m

HWS229 Surface 0.5 1972‐74 21 T 620214 5198488 m

HWS230 Surface 0.18 1972‐74 21 T 620167 5198482 m

HWS231 Surface 0.38 1972‐74 21 T 619926 5198474 m

HWS232 Surface 0.09 1972‐74 21 T 619988 5198453 m

HWS233 Surface 0.3 1972‐74 21 T 619944 5198487 m

HWS234 Surface 0.4 1972‐74 21 T 619895 5198542 m

HWS235 Surface 0.51 1972‐74 21 T 620071 5198490 m

HWS236 Surface 0.22 1972‐74 21 T 620358 5198511 m

HWS237 Surface ND 1972‐74 21 T 620249 5198536 m

HWS238 Surface 0.54 1972‐74 21 T 620245 5198605 m

HWS239 Surface 0.22 1972‐74 21 T 620353 5198689 m

HWS240 Surface 0.22 1972‐74 21 T 620282 5198753 m

HWS241 Surface 0.05 1972‐74 21 T 620152 5198635 m

HWS242 Surface 0.06 1972‐74 21 T 620017 5198591 m

HWS243 Surface 0.19 1972‐74 21 T 619998 5198642 m

HWS244 Surface 0.87 1972‐74 21 T 619899 5198650 m

HWS245 Surface 0.1 1972‐74 21 T 620110 5198754 m

HWS246 Surface 0.1 1972‐74 21 T 620218 5198680 m

HWS247 Surface 0.29 1972‐74 21 T 620345 5198797 m

HWS248 Surface 0.26 1972‐74 21 T 620243 5198872 m

HWS249 Surface 0.1 1972‐74 21 T 620139 5198937 m

HWS250 Surface 0.16 1972‐74 21 T 620197 5198934 m

HWS251 Surface 0.1 1972‐74 21 T 620312 5198859 m

HWS252 Surface 0.23 1972‐74 21 T 620405 5198858 m

HWS253 Surface 0.04 1972‐74 21 T 620407 5198908 m

HWS254 Surface 0.28 1972‐74 21 T 620372 5198969 m

ND = Not Detected

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HWS261 Surface 0.23 1972‐74 21 T 620637 5199072 m

HWS262 Surface 0.16 1972‐74 21 T 620918 5199029 m

HWS263 Surface 0.18 1972‐74 21 T 620999 5199122 m

HWS264 Surface 0.12 1972‐74 21 T 620900 5199122 m

HWS265 Surface 0.1 1972‐74 21 T 620685 5199164 m

HWS266 Surface 0.13 1972‐74 21 T 620578 5199209 m

HWS267 Surface 0.03 1972‐74 21 T 620716 5199224 m

HWS268 Surface 0.05 1972‐74 21 T 620846 5199237 m

HWS269 Surface 0.07 1972‐74 21 T 620968 5199228 m

HWS270 Surface 0.03 1972‐74 21 T 621047 5199219 m

HWS271 Surface 0.09 1972‐74 21 T 621149 5199225 m

HWS272 Surface 0.07 1972‐74 21 T 621322 5199423 m

HWS273 Surface 0.16 1972‐74 21 T 620812 5199482 m

HWS274 Surface 0.14 1972‐74 21 T 620718 5199480 m

HWS275 Surface 0.25 1972‐74 21 T 620568 5199422 m

HWS276 Surface 0.4 1972‐74 21 T 620502 5199554 m

HWS277 Surface 0.25 1972‐74 21 T 620841 5199615 m

HWS278 Surface 0.12 1972‐74 21 T 620511 5199641 m

HWS279 Surface 0.1 1972‐74 21 T 620463 5199780 m

HWS280 Surface 0.1 1972‐74 21 T 620506 5199875 m

HWS281 Surface 0.09 1972‐74 21 T 620710 5199857 m

HWS282 Surface 0.2 1972‐74 21 T 620778 5199881 m

HWS283 Surface 0.03 1972‐74 21 T 621554 5199694 m

HWS284 Surface 0.01 1972‐74 21 T 621692 5199759 m

HWS285 Surface 0.07 1972‐74 21 T 621111 5199762 m

HWS286 Surface 0.12 1972‐74 21 T 621371 5199881 m

HWS287 Surface 0.08 1972‐74 21 T 621347 5199959 m

HWS288 Surface 0.2 1972‐74 21 T 621271 5200107 m

HWS289 Surface 0.15 1972‐74 21 T 621101 5200155 m

HWS290 Surface 0.09 1972‐74 21 T 621094 5200276 m

HWS292 Surface 0.15 1972‐74 21 T 620503 5200038 m

HWS293 Surface 0.16 1972‐74 21 T 620621 5200053 m

HWS294 Surface 0.18 1972‐74 21 T 620672 5200133 m

HWS295 Surface 0.25 1972‐74 21 T 620771 5200176 m

HWS296 Surface 0.18 1972‐74 21 T 620594 5200195 m

HWS297 Surface 0.15 1972‐74 21 T 620945 5200184 m

HWS298 Surface 0.15 1972‐74 21 T 620768 5200341 m

HWS299 Surface 0.31 1972‐74 21 T 620614 5200338 m

HWS300 Surface 0.18 1972‐74 21 T 620606 5200389 m

HWS301 Surface 0.52 1972‐74 21 T 620594 5200467 m

HWS302 Surface 0.9 1972‐74 21 T 620572 5200583 m

ND = Not Detected

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HWS303 Surface 0.24 1972‐74 21 T 620753 5200468 m

HWS304 Surface 0.2 1972‐74 21 T 621076 5200540 m

HWS305 Surface 0.62 1972‐74 21 T 620711 5200532 m

HWS306 Surface 1.01 1972‐74 21 T 620744 5200706 m

HWS307 Surface 0.4 1972‐74 21 T 620825 5200688 m

HWS308 Surface 0.15 1972‐74 21 T 620878 5200797 m

HWS309 Surface 0.13 1972‐74 21 T 620867 5200843 m

HWS310 Surface 0.07 1972‐74 21 T 621352 5200764 m

HWS311 Surface 0.19 1972‐74 21 T 620457 5201044 m

HWS312 Surface 0.14 1972‐74 21 T 620638 5200997 m

HWS313 Surface 0.18 1972‐74 21 T 620768 5201017 m

HWS314 Surface 0.2 1972‐74 21 T 620871 5200947 m

HWS315 Surface 0.01 1972‐74 21 T 621333 5200989 m

HWS318 Surface 0.5 1972‐74 21 T 622333 5200420 m

HWS330 Surface 0.05 1972‐74 21 T 622011 5199874 m

HWS331 Surface 0.05 1972‐74 21 T 622028 5199813 m

ND = Not Detected

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Historical Water Samples (HWS) East of 21055M Geofile 001L_0069 map sheet 4 & 9

Fluoride in Water (F) mg / Litre (ppm) Grid: UTM



HWS400 Surface 0.06 1972‐74 21 T 618778 5198861

HWS401 Surface 0.26 1972‐74 21 T 619029 5198886

HWS402 Surface 0.28 1972‐74 21 T 618798 5198792

HWS403 Surface 0.09 1972‐74 21 T 618746 5198724

HWS404 Surface 0.39 1972‐74 21 T 618767 5198723

HWS405 Surface 0.08 1972‐74 21 T 618922 5198745

HWS406 Surface 0.06 1972‐74 21 T 618590 5198623

HWS407 Surface 0.05 1972‐74 21 T 618621 5198587

HWS408 Surface 0.27 1972‐74 21 T 618712 5198629

HWS409 Surface 0.21 1972‐74 21 T 618704 5198581

HWS410 Surface 0.28 1972‐74 21 T 618695 5198561

HWS411 Surface 0.06 1972‐74 21 T 619019 5198679

HWS412 Surface 0.10 1972‐74 21 T 619002 5198610

HWS413 Surface 0.10 1972‐74 21 T 618898 5198549

HWS414 Surface 0.12 1972‐74 21 T 618848 5198470

HWS415 Surface 0.40 1972‐74 21 T 618656 5198491

HWS416 Surface 0.20 1972‐74 21 T 618744 5198486

HWS417 Surface 0.11 1972‐74 21 T 618616 5198458

HWS418 Surface 0.31 1972‐74 21 T 618659 5198372

HWS419 Surface 0.18 1972‐74 21 T 618730 5198380

HWS420 Surface 0.10 1972‐74 21 T 619000 5198391

HWS421 Surface 0.34 1972‐74 21 T 618904 5198325

HWS422 Surface 0.27 1972‐74 21 T 618678 5198193

HWS423 Surface 0.29 1972‐74 21 T 618782 5198180

HWS424 Surface 0.33 1972‐74 21 T 618856 5198164

HWS425 Surface 0.07 1972‐74 21 T 618958 5198215

HWS426 Surface 0.25 1972‐74 21 T 618722 5198088

HWS427 Surface 0.31 1972‐74 21 T 618751 5198042

HWS428 Surface 0.26 1972‐74 21 T 618795 5198009

HWS429 Surface 0.13 1972‐74 21 T 618900 5198096

HWS430 Surface 0.19 1972‐74 21 T 618742 5197973

HWS431 Surface 0.13 1972‐74 21 T 619002 5197968

HWS432 Surface 0.04 1972‐74 21 T 618695 5197810

HWS433 Surface 0.11 1972‐74 21 T 618701 5197770

HWS434 Surface 0.01 1972‐74 21 T 618708 5197742

HWS435 Surface 0.10 1972‐74 21 T 618703 5197705

HWS436 Surface 0.09 1972‐74 21 T 618696 5197653

HWS437 Surface 0.40 1972‐74 21 T 619038 5197817

HWS438 Surface 0.52 1972‐74 21 T 619079 5197732

HWS439 Surface 0.50 1972‐74 21 T 619046 5197693

HWS440 Surface 0.12 1972‐74 21 T 619060 5197625

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HWS441 Surface 0.18 1972‐74 21 T 619060 5197603

HWS442 Surface 0.25 1972‐74 21 T 619087 5197461

HWS443 Surface 0.08 1972‐74 21 T 619137 5197432

HWS444 Surface 0.29 1972‐74 21 T 619071 5197418

HWS445 Surface 0.12 1972‐74 21 T 619062 5197381

HWS446 Surface 0.18 1972‐74 21 T 619040 5197349

HWS447 Surface 0.35 1972‐74 21 T 619063 5197323

HWS448 Surface 0.14 1972‐74 21 T 619055 5197290

HWS449 Surface 0.39 1972‐74 21 T 619024 5197263

HWS450 Surface 0.19 1972‐74 21 T 619013 5197305

HWS451 Surface 0.29 1972‐74 21 T 618998 5197312

HWS452 Surface 0.12 1972‐74 21 T 618967 5197324

HWS453 Surface 0.10 1972‐74 21 T 618966 5197288

HWS454 Surface 0.13 1972‐74 21 T 618913 5197262

HWS455 Surface 0.30 1972‐74 21 T 618892 5197291

HWS456 Surface 0.11 1972‐74 21 T 618871 5197281

HWS457 Surface 0.30 1972‐74 21 T 618804 5197296

HWS458 Surface 0.10 1972‐74 21 T 618740 5197321

HWS459 Surface 0.19 1972‐74 21 T 618771 5197270

HWS460 Surface 0.48 1972‐74 21 T 618884 5197176

HWS461 Surface 0.19 1972‐74 21 T 618927 5197176

HWS462 Surface 0.20 1972‐74 21 T 618959 5197198

HWS463 Surface 0.51 1972‐74 21 T 618914 5197145

HWS464 Surface 0.31 1972‐74 21 T 618933 5197093

HWS465 Surface 0.27 1972‐74 21 T 618985 5197103

HWS466 Surface 0.22 1972‐74 21 T 618967 5197043

HWS467 Surface 0.30 1972‐74 21 T 618885 5196854

HWS468 Surface 0.15 1972‐74 21 T 618845 5196827

HWS469 Surface 0.19 1972‐74 21 T 618926 5196780

HWS470 Surface 0.30 1972‐74 21 T 618969 5196774

HWS471 Surface 0.45 1972‐74 21 T 618976 5196746

HWS472 Surface 0.22 1972‐74 21 T 618989 5196727

HWS473 Surface 0.26 1972‐74 21 T 618961 5196704

HWS474 Surface 0.41 1972‐74 21 T 618946 5196685

HWS475 Surface 0.45 1972‐74 21 T 618955 5196675

HWS476 Surface 0.50 1972‐74 21 T 618922 5196676

HWS477 Surface 0.20 1972‐74 21 T 618927 5196661

HWS478 Surface 0.21 1972‐74 21 T 618924 5196635

HWS479 Surface 0.55 1972‐74 21 T 619017 5196600

HWS480 Surface 0.30 1972‐74 21 T 619059 5196631

HWS481 Surface 0.38 1972‐74 21 T 619035 5196552

HWS482 Surface 0.11 1972‐74 21 T 618610 5196728

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HWS483 Surface 0.33 1972‐74 21 T 618614 5196695

HWS484 Surface 0.10 1972‐74 21 T 618628 5196638

HWS485 Surface 0.09 1972‐74 21 T 618686 5196584

HWS486 Surface 0.10 1972‐74 21 T 618740 5196567

HWS487 Surface 0.12 1972‐74 21 T 618729 5196551

HWS488 Surface 0.17 1972‐74 21 T 619076 5196510

HWS489 Surface 0.19 1972‐74 21 T 619027 5196427

HWS490 Surface 0.08 1972‐74 21 T 618999 5196400

HWS491 Surface 0.18 1972‐74 21 T 619061 5196341

HWS492 Surface 0.23 1972‐74 21 T 618598 5196236

HWS493 Surface 0.13 1972‐74 21 T 618628 5196222

HWS494 Surface 0.21 1972‐74 21 T 618646 5196190

HWS495 Surface 0.21 1972‐74 21 T 618669 5196173

HWS496 Surface 0.27 1972‐74 21 T 618717 5196141

HWS497 Surface 0.20 1972‐74 21 T 618830 5196135

HWS498 Surface 0.09 1972‐74 21 T 618763 5196096

HWS499 Surface 0.22 1972‐74 21 T 618876 5196093

HWS500 Surface 0.11 1972‐74 21 T 618666 5196035

HWS501 Surface 0.13 1972‐74 21 T 618753 5196031

HWS502 Surface 0.11 1972‐74 21 T 618867 5196019

HWS503 Surface 0.16 1972‐74 21 T 618584 5196021

HWS504 Surface 0.10 1972‐74 21 T 618641 5195993

HWS505 Surface 0.13 1972‐74 21 T 618600 5195953

HWS506 Surface 0.19 1972‐74 21 T 618823 5195914

HWS507 Surface 0.31 1972‐74 21 T 618894 5195946

HWS508 Surface 0.30 1972‐74 21 T 618889 5195857

HWS509 Surface 0.31 1972‐74 21 T 618591 5195851

HWS510 Surface 0.12 1972‐74 21 T 618638 5195856

HWS511 Surface 0.18 1972‐74 21 T 618795 5195794

HWS512 Surface 0.31 1972‐74 21 T 618905 5195727

HWS513 Surface 0.22 1972‐74 21 T 619021 5195703

HWS514 Surface 0.31 1972‐74 21 T 618680 5195722

HWS515 Surface 0.21 1972‐74 21 T 618582 5195617

HWS516 Surface 0.30 1972‐74 21 T 618668 5195641

HWS517 Surface 0.30 1972‐74 21 T 618671 5195588

HWS518 Surface 0.21 1972‐74 21 T 618819 5195638

HWS519 Surface 0.22 1972‐74 21 T 618718 5195507

HWS520 Surface 0.12 1972‐74 21 T 618818 5195427

HWS521 Surface 0.27 1972‐74 21 T 618948 5195562

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St. Lawrence 2014

Fluoride in Soil mg / kg Grid: UTM

Datum: NAD27 Canada

Name mg / kg Depth, m. Date Time Zone UTM East North Elev. Units

SSL200 BDL 0.46 22‐Aug‐14 13:20AM 21 T 623448 5198896 11 m

SSL2000‐Dup BDL 0.46 22‐Aug‐14 13:20AM 21 T 623448 5198896 11 m

SSL201 130 0.46 22‐Aug‐14 13:25PM 21 T 623456 5198896 14 m

SSL202 330 0.30 22‐Aug‐14 13:55PM 21 T 623434 5198889 26 m

SSL203 BDL 0.51 22‐Aug‐14 14:45PM 21 T 623451 5198937 17 m

SSL204 BDL 0.25 22‐Aug‐14 15:05PM 21 T 623493 5198883 17 m

SSL206 160 0.36 23‐Aug‐14 10:10AM 21 T 621456 5199068 72 m

SSL208 180 0.28 23‐Aug‐14 10:15AM 21 T 621469 5199091 72 m

SSL210 BDL 0.51 23‐Aug‐14 12:20AM 21 T 621513 5199088 67 m

SSL212 160 0.30 23‐Aug‐14 13:30AM 21 T 621523 5199113 70 m

SSL214 130 0.41 23‐Aug‐14 14:00PM 21 T 621545 5199125 72 m

DBL = Below Detection Limit <100

Dup = Laboratoy Duplicate

NewFluorEx.com

St. Lawrence Project

St. Lawrence 2011 and 2013

Fluoride in Soil mg / kg Grid: UTM

Datum: NAD27 Canada

Name mg / kg Depth, m. Date Time Zone UTM East North Elev. Units

2011 Soil Samples

SSL01 120 27‐Jun‐11 1:50PM 21 T 621051 5200734 126 m

SSL02 BDL 27‐Jun‐11 1:59PM 21 T 621037 5200875 122 m

SSL03 BDL 27‐Jun‐11 2:07PM 21 T 621036 5201017 127 m

SSL04 BDL 27‐Jun‐11 2:24PM 21 T 620640 5200842 112 m

SSL06 110 13‐Jul‐11 11:33AM 21 T 624264 5199258 101 m

SSL07 110 13‐Jul‐11 11:38AM 21 T 624165 5199219 90 m

SSL08 120 13‐Jul‐11 11:46AM 21 T 624099 5199159 78 m

SSL11 110 16‐Jul‐11 4:25PM 21 T 624197 5199125 83 m

SSL12 BDL 16‐Jul‐11 4:32PM 21 T 624251 5199027 80 m

2013 Soil Samples

SSL20 120 0.52 6‐Jul‐13 11:32 AM 21 T 620709 5200607 106 m

SSL21 220 0.59 6‐Jul‐13 11:40 AM 21 T 620728 5200591 105 m

SSL22 BDL 0.67 6‐Jul‐13 11:48 AM 21 T 620741 5200572 106 m

SSL23 210 0.46 6‐Jul‐13 12:18 PM 21 T 620636 5200539 97 m

SSL23Dupl 210 0.46 6‐Jul‐13 12:18 PM 21 T 620636 5200539 97 m

SSL24 110 0.30 6‐Jul‐13 12:25 PM 21 T 620595 5200498 97 m

SSL25 100 0.29 6‐Jul‐13 12:52 PM 21 T 620766 5200371 100 m

DBL = Below Detection Limit <100NewFluorEx.com


St. Lawrence 2014

Observation Locations Grid: UTM

Datum: NAD27 Canada

Name Date Time Zone UTM East North Elev. Units

Licence 21057M

Tr3 24‐Aug‐14 2:50:14PM 21 T 621939 5198836 40 m

Tr4 24‐Aug‐14 3:06:48PM 21 T 621949 5198855 45 m

Tr5 24‐Aug‐14 3:14:53PM 21 T 621957 5198853 44 m

Tr6 24‐Aug‐14 3:19:44PM 21 T 621971 5198856 45 m

Tr7 24‐Aug‐14 3:24:48PM 21 T 621983 5198862 46 m

Tr8 24‐Aug‐14 3:30:26PM 21 T 622002 5198868 46 m

Tr9 24‐Aug‐14 3:38:42PM 21 T 622017 5198873 47 m

Tr10 24‐Aug‐14 3:46:12PM 21 T 622051 5198878 44 m

Tr11 24‐Aug‐14 3:54:33PM 21 T 622067 5198876 43 m

TrA 23‐Aug‐14 1:53:14PM 21 T 621919 5198851 35 m

TrB 23‐Aug‐14 2:21:08PM 21 T 621931 5198851 39 m

TrQ 24‐Aug‐14 2:15:38PM 21 T 621659 5198607 47 m

TrR 24‐Aug‐14 2:00:16PM 21 T 621678 5198642 41 m

TrS 24‐Aug‐14 1:50:17PM 21 T 621685 5198659 42 m

TrT 24‐Aug‐14 1:47:23PM 21 T 621694 5198673 43 m

TrU 24‐Aug‐14 1:41:59PM 21 T 621700 5198681 42 m

TrV 24‐Aug‐14 1:26:37PM 21 T 621729 5198745 39 m

TrW 24‐Aug‐14 1:17:06PM 21 T 621728 5198733 35 m

TrX 24‐Aug‐14 1:08:42PM 21 T 621716 5198717 36 m

TrY 24‐Aug‐14 1:03:56PM 21 T 621707 5198704 31 m

TrZ 24‐Aug‐14 12:57:22PM 21 T 621703 5198684 29 m

Hp1 24‐Aug‐14 2:22:50PM 21 T 621694 5198643 42 m

Licence 22121M

Breccia 22‐Aug‐14 1:53:42PM 21 T 623498 5198916 7 m

NewFluorEx.com


St. Lawrence 2014

Trench Observations Licence 21057M

Waypoint Dimensions (approx) Floor CommentsTr1 6-11m x 3.5 ft wide, 4 ft deep dry, solid Trench trends 340 degTr2 6 x 8 x 3 ft deep < 0.5 ft standing water Solid rubble floorTr3 25 x 25 ft, roughly squarish > 2 ft water, potentially deep Major excavation, blocky rock infilling, water flowing off gentle hillslope continuous infills trench and

then flows out to another trench-like feature (6 x 15 x 3 ft deep)Tr4 4 x 6 m < 1 ft standing water Not certain if trench or river washout, trench very close to stream in boulder filled boggy area

adjacent to streamTr5 10 x 10 x 2 ft deep dry, solid Poorly defined shape, big bermsTr6 6 x 10 x 2 ft deep dry, solid Uncertain if a trenchTr7 4m x 8m x 2 ft deep dry, solidTr8 6 x 10 x 3 ft deep dry, solid Poorly defined shape, big bermsTr9 8 x 25 x 4 ft deep damp, solidTr10 10 x 25 x >5 ft deep flooded Looks deepTr11 6 x 8 x 3 ft deep dry, solid Poorly defined shape, uncertain if trenchTrQ 5 x 20 x 2 ft deep dry, solid Narrow, possible trenchTrR 10-15 ft squarish depression, > 3 ft deep dry, solid Almost below powerline, rubble berms to north and south of pit, ingrown with raspberry bush, piece

large blast ? rock at pit bottom. Possible shaft. Potential trap hazard to ATV / snowmobiles.

TrS 6-8 x 15 x 4 ft deep dry, solidTrT 10 x 20 x 4 ft deep dry, solidTrU 8 x 18 x 5 ft deep dry, solidTrV 3 x 5 < 1 ft standing water Possible trench, no obvious bermTrW 10 x 10 x 3 ft deep < 1 ft standing water Solid rubble floorTrX 8 x 30 x 2 ft deep dry, solidTrY 8 x 25 x 4 ft deep dry, solidTrZ 10 ft long, 2 ft deep dry, solid Long, narrow

Observations Licence 22121M

Breccia Zone < 6 ft wide, 40 ft long.

exposed.

Trench Summary

brecciated granite at river edge, trends 305 deg, silicified areas, some small quartz veins, small (<1/2 inch)

blotches of purple fluorspar.

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APPENDIX 4 Statement of Expenditures Field Labour, 2014 $ 5,900.22 Lab costs 1,117.50 Hotels 300.00 Meals 255.13 Field Supply 82.00 ATV Rental and Gas 210.00 Personal Vehicles used at $0.50/km. 1,060.28 Airfare 433.07 Evaluation of Field Results Report Preparation, Research 2,220.00 Drafting and Data Processing, 3,075.00 Subtotal $14,684.94 15% Overhead Expense 2,202.74 TOTAL $16,887.68 Allocation by License: 21055M 2,237.85 21479M 7,696.62 22121M 6,953.21 TOTAL $16,887.68

APPENDIX 5 List of Personnel Alex Harris, B. Sc., Geologist, Saskatoon, Sk.

Research and Planning: Mar. 8, 12, 2014; Jun. 23,2014; Jul 26, 2014; Aug. 16, 21, 22, 23, 24, 25, 26, 28, 30, 2014. Report Preparation: Nov. 26, 30, 2014; Dec. 4, 13, 14, 20, 23, 2014.

Gordon Stefanuk, C. E. T., Draftsman, GIS and Data Processing, Lloydminster, AB.

Drafting, Data Processing etc. Mar. 1, 2, 3, 2014; Apr. 1, 5, May, 11, 2014; July 23, 25, 26, 2014; Aug. 1, 23, 2014; Sept. 3, 6, 2014; Oct. 4, 5, 10, 11, 12, 13, 14, 15, 18, 19, 20, 21, 23, 25, 26, 27, 30, 2014; Nov. 24, 25, 2014; Dec. 4, 5, 6, 7, 8, 9, 12, 14, 15, 16, 17, 18, 19, 20, 27, 2014

Bill Taylor, Prospector, Marystown, NL. Field Work: Aug. 20-25, 2014. Peter Fernberg, M. Sc., Geologist, Williamsburg, ON Field Work: Aug. 20-25, 2014.

Report Preparation: Dec. 23, 2014

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