2016 GEOLOGICAL REPORT ON THE NAZKO PROPERTY CARIBOO MINING DIVISION BRITISH COLUMBIA
BCGS MAPS 093B.082 AND 093B.092 LATITUDE 52° 55’ 32.3” N AND LONGITUDE 123° 44’ 10.8” W STATEMENT OF WORK EVENT: 5611358
Prepared for: CANLAVA Mining Corp. 203 – 1312 Ketch Court Coquitlam, B.C. V3K 6W1
Prepared by: R. A. (Bob) Lane, P.Geo. Plateau Minerals Corp.
Date: June 30, 2016
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
TABLE OF CONTENTS
1 EXECUTIVE SUMMARY ...... 1 2 INTRODUCTION ...... 2 2.1 LOCATION AND ACCESS ...... 2 2.2 PHYSIOGRAPHY AND CLIMATE ...... 2 2.3 PROPERTY STATUS AND OWNERSHIP ...... 2 2.4 DEVELOPMENT AND EXPLORATION HISTORY ...... 6 3 REGIONAL GEOLOGY ...... 6 4 PROPERTY GEOLOGY ...... 7 5 MINERALIZATION ...... 9 6 2016 EXPLORATION PROGRAM ...... 10 6.1 BEDROCK MAPPING AND PROSPECTING ...... 10 7 SAMPLING METHOD AND APPROACH ...... 13 8 SAMPLE PREPARATION, ANALYSES AND SECURITY ...... 13 9 INTERPRETATION AND CONCLUSIONS ...... 17 10 RECOMMENDATIONS ...... 17 11 ITEMIZED COST STATEMENT – NAZKO PROPERTY ...... 18 12 REFERENCES ...... 19 13 STATEMENTS OF QUALIFICATIONS ...... 21
LIST OF TABLES TABLE 1: NAZKO PROPERTY – LIST OF MINERAL TENURES ...... 4 TABLE 2: 2016 ROCK SAMPLE LOCATIONS, DESCRIPTIONS AND RESULTS ...... 14
LIST OF FIGURES FIGURE 1: NAZKO PROPERTY - LOCATION ...... 3 FIGURE 2: NAZKO PROPERTY - MINERAL TENURE ...... 5 FIGURE 3: NAZKO AREA - REGIONAL GEOLOGY ...... 8 FIGURE 4: NAZKO PROPERTY – LOCAL GEOLOGY ...... 15 FIGURE 5: BEDROCK GEOLOGY, SAMPLE LOCATIONS AND RESULTS – SOUTHERN NAZKO PROPERTY...... 16
LIST OF PLATES PLATE 1: VIEW OF THE NAZKO CINDER CONE AND CANLAVA’S LAVA ROCK QUARRY OPERATION...... 11 PLATE 2: GREY WEATHERING ‘SPOTTED’ ANDESITE OF THE OOTSA LAKE GROUP ...... 12 PLATE 3: FRACTURE-CONTROLLED IRON AND MANGANESE STAINING OF COARSE-GRAINED SANDSTONE THAT UNDERLIES THE VOLCANIC STRATIGRAPHY...... 12 PLATE 4: IRON AND MANGANESE-STAINED RHYOLITE BRECCIA, OOTSA LAKE GROUP...... 13
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APPENDICES APPENDIX A – TABULATED WEIGH POINT DATA APPENDIX B – LABORATORY CERTIFICATES
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1 EXECUTIVE SUMMARY The Nazko property is located approximately 80 km west of Quesnel, British Columbia, and 10 km west of the village of Nazko, in the Cariboo Mining Division. The property is centered at 52°55’32.3” N and 123°44’10.8” W (NAD83), between Fishpot Lake to the west and Marmot Lake to the east. The Nazko property covers parts of BCGS maps 093B.082 and 093B.092. The Nazko property consists of two contiguous mineral leases that cover 400.00 hectares (ha) of land that are encompassed by six mineral claims that cover 1676.20 ha. The leases and claims that comprise the Nazko property are 100% owned by CANLAVA Mining Corp. (CANLAVA).
Access to the property is west from Quesnel via the paved Nazko Road to the village of Nazko, then west along the well-travelled gravel 4000 Road to the Nazko cone and approximate centre of the property. The Nazko property covers the Recent Nazko cinder cone where scoria and tephra is currently being mined and processed on mining leases into finished product by owner- operator CANLAVA. Underling rocks include prospective Eocence Ootsa Lake Group rhyolitic volcanic rocks and Cretaceous Skeena Group fine to coarse-grained siliciclastics.
The Nazko property has only recently been the subject of exploration for precious metals. Geochemical surveys have outlined several anomalies that warranted follow-up work.
In 2016 a limited program of bedrock mapping, prospecting and rock geochemical sampling was conducted over the southern half of the property. It identified a previously unrecognized window through the young volcanic cover to older rocks. The window exposes locally iron and manganese-altered chert pebble conglomerate and coarse-grained sandstone of the Skeena Group that occurs mainly on the western edge of the claim group. It is in contact to the west with hematite-altered rhyolite breccia of the Ootsa Lake Group. Select grab samples from the altered sandstone and conglomerate returned background levels of pathfinder elements, while two samples of rhyolite breccia returned weakly anomalous values for Zn, but background values for the other pathfinder elements. Despite weak analytical results, further examination of the area west of the claim boundary to more fully evaluate the rhyolite breccia is warranted.
It is recommended that CANLAVA consider staking the open ground located immediately west of the existing claim block to cover areas underlain by the altered Ootsa Lake Group rhyolitic rocks. Should new claims be added, a suggested budget for a 1-week follow-up program of detailed mapping and prospecting is an estimated $13,000.00.
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2 INTRODUCTION This assessment report has been prepared at the request of CANLAVA Mining Corp. (CANLAVA) to summarize results of a bedrock mapping and prospecting program conducted in mid-May of 2016 on its Nazko property. This assessment report was prepared by independent Qualified Person R.A. (Bob) Lane, P.Geo.
2.1 LOCATION AND ACCESS The Nazko property is located approximately 80 km west of Quesnel, British Columbia, and 10 km west of the village of Nazko, in the Cariboo Mining Division. The property is centered at 52°55’32.3” N and 123°44’10.8” W (NAD83), between Fishpot Lake to the west and Marmot Lake to the east. The Nazko property covers parts of BCGS maps 093B.082 and 093B.092.
Access to the property is west from Quesnel via the paved Nazko Road to the village of Nazko, then west along the well-travelled gravel 4000 Road to the Nazko cone and approximate centre of the property. Several tertiary roads, some of which are decommissioned, provide 4x4 and ATV access to several large clear cuts. Recent clear cut logging and associated road development south of Nazko cone provide good access to areas of thin overburden cover where road cuts expose previously hidden bedrock.
2.2 PHYSIOGRAPHY AND CLIMATE The Nazko property area is characterized by low rolling hills, with elevations ranging between 1090 and 1305 m above sea level (asl). Uniform glacial till generally less than 10 m thick covers bedrock. Exposed bedrock accounts for less than 10% of the property area; outcrop exposures generally limited to north- and west-facing hillsides and man-made road cuts. Much of the property has been logged since the mid-1980s. Forested areas contain a mixture of pine and spruce with minor alder undergrowth in low-lying areas.
The climate is typical of a moderate continental setting at this latitude. Relatively cold winter conditions occur from November through March, and temperate summer conditions occur between June and September.
2.3 PROPERTY STATUS AND OWNERSHIP The Nazko property consists of two contiguous mineral leases that cover 400.00 hectares (ha) of land that are encompassed by six mineral claims that cover 1676.20 ha (Table 1 and Figure 2). The tenures cover parts of BCGS maps 093B.092 and 093B.082. The leases and claims that comprise the Nazko property are 100% owned by CANLAVA Mining Corp. (client ID 275848).
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Figure 1: Nazko Property - Location
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Table 1: Nazko Property – List of Mineral Tenures
Title Title Map Area Title Number Claim Name Owner Sub Status Type Number (ha) Type 275848 316265 (100%) Mineral Lease 093B092 GOOD 200.00 275848 329933 (100%) Mineral Lease 093B092 GOOD 200.00 275848 552589 LAVA 7 (100%) Mineral Claim 093B GOOD 233.78 275848 552591 (100%) Mineral Claim 093B GOOD 233.78 275848 552592 LAVA 8 (100%) Mineral Claim 093B GOOD 409.31 275848 552593 LAVA 9 (100%) Mineral Claim 093B GOOD 155.90 275848 552594 LAVA 10 (100%) Mineral Claim 093B GOOD 487.41 CANLAVA 275848 1041719 Mineral Claim 093B GOOD 156.02 SOUTHWEST (100%)
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Figure 2: Nazko Property - Mineral Tenure
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2.4 DEVELOPMENT AND EXPLORATION HISTORY The Nazko property covers the Recent Nazko cinder cone where scoria and tephra is currently being mined and processed on mining leases into finished product by owner-operator CANLAVA Mining Corp. The mine has been an intermittent producer since 1991 when it was under the control of Canada Pumice Corporation (CPC). In 2004, CPC became a subsidiary of Crystal Graphite Corporation, but the companies soon encountered financial difficulties and were placed into receivership. Early in 2006, Pricewaterhouse Coopers Inc. was appointed Receiver-Manager of both companies. In June 2012 the mine was purchased by CANLAVA.
Exploration of the mineral claims that encompass the mining leases is limited to a series of relatively recent government funded regional geochemical surveys and one property-specific silt sampling campaign (Jackaman, 2015). The surveys identified significant concentrations of path finder elements that are typical of gold-bearing mineralization, albeit elevated levels of gold itself have not been identified. The suite of elements may be indicative of an undiscovered precious metal epithermal vein system similar to that occurring on the Bob property less than 5 km to the east.
3 REGIONAL GEOLOGY The Nazko property is situated in the central part of the Intermontane Belt, and covers an area dominated by rocks of the Overlap Assemblage. These Cretaceous to Recent volcanic and sedimentary rocks are of variable thicknesses and cap the underlying basement geology of the Stikine Terrane which in the general area consists primarily of Jurassic volcanic rocks. The referenced rock descriptions provided below are taken from Angen et al. (2015).
Stikine Terrane Lower and Middle Jurassic Hazelton Group (Naglico Formation) Basalt - Pyroxene phyric mafic flows, tuff, and minor submarine sediments. Flows are dark green and rarely maroon basalt to andesite with 1-3 % augite phenocrysts and 1-35% plagioclase phenocrysts, less commonly aphanitic. Rare amygdules contain quartz, chlorite, and epidote. Pyroclastic rocks are green and red lapilli tuff with abundant plagioclase and chloritized mafics in both the matrix and lapilli. Rare interbedded sediments include arkosic arenite, siltstone, tuffaceous argillite, volcanic derived conglomerate, and minor limestone (Diakow et al., 1997).
Overlap Assemblage Lower Cretaceous Skeena Group Sandstone and conglomerate - Predominantly chert and quartz grain sandstone with chert pebble dominated conglomerate, minor maroon mudstone and dark grey siltstone. Rare maroon acitic and tan rhyolitic tuff. Chert clasts in conglomerate frequently contain quartz veins. Albian and Cenomanian to possibly Turonian palynological ages reported (Hunt, 1992; Riddell, 2011).
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Eocene Ootsa Lake Group Rhyolite to andesite flows and volcaniclastic rocks - White to beige to pale pink flow banded rhyolite, commonly with spherulites, <5% quartz, <3% feldspar, 7% magnetite phenocrysts; perlitic vitreous black dacite with <1% pyroxene and plagioclase phenocrysts; tan to pink hornblende dacite with <5% hornblende and <2% potassium feldspar phenocrysts; rhyolitic to dacitic lapilli tuff, locally welded. Minor amygdaloidal pyroxene or plagioclase phyric basalt, volcanic sandstone and conglomerate locally containing plutonic clasts (Bordet, 2014; Diakow et al., 1997).
Eocene to Oligocene Endako Group Basalt - Basaltic andesite and andesitic lava flows. Dark green-grey to black, columnar jointed to massive, fine grained to sparsely porphyritic flows with plagioclase phenocrysts and, less commonly, microphenocrysts of pyroxene and olivine (Haskin et al., 1998).
Miocene to Pliocene Chilcotin Group Basalt - Olivine basalt lava flows. Dark grey to black, crudely columnar jointed, flat-lying alkaline basalt flows with vesicle sheets and pipes, minor pillow basalts, and associated high level intrusions. Minor intercalated silicic tephra layers. Basalts are typically aphanitic or olivine microphyric (Bevier, 1983). The Cheslatta Lake Suite contains xenoliths of spinel peridotite and less common crustal xenoliths (gabbro, granite, anorthosite, and granulite) as well as megacrysts of olivine, clinopyroxene, plagioclase, and magnetite (Anderson et al., 2001). Rare, poorly consolidated polylithic conglomerate and sandstone with red-brown matrix.
Miocene to Holocene Anahim Volcanics Basalt - Basanites to basaltic trachyandesites and trachytes, phonolites, and rare rhyolites. Aphanitic to sparsely porphyritic with potassium feldspar, plagioclase, olivine, and pyroxene phenocrysts. Light grey to black and red, variably vesicular. Columnar jointed flows and pillow breccia are common. Scoria rarely preserved (Kuehn, 2014; Kuehn et al., 2015).
4 PROPERTY GEOLOGY The Nazko property is centered on the Recent Nazko cinder cone, a volcanic edifice that formed approximately 7,200 years ago. The cone and associated basalt lava flows occupy the majority of the claims. Eocene Ootsa Lake Group basalt flows cover the west and southern portions of the claim block and Cretaceous Skeena Group sedimentary rocks occupy the southeast corner of the property (Figure 4). Detailed descriptions of each unit are provided above in a regional context.
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Figure 3: Nazko Area - Regional Geology
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5 MINERALIZATION The Nazko property encompasses one MINFILE occurrence: Nazko – 093B 060. A summary of the occurrence, abstracted from the British Columbia mineral occurrence data files (MINFILE) is provided below. The Bob MINFILE occurrence lies to the east of the property and is also briefly described; it is an example of exposed gold-silver mineralization that in other nearby areas may be hidden under a relatively thin skin of Eocene to Recent subaerial volcanic rocks.
Nazko (093B 060) The Nazko MINFILE occurrence is between Fishpot and Marmot lakes, 80 km west of Quesnel, British Columbia, and 10 km west of the village of Nazko, in the Cariboo Mining Division. The mineral occurrence consists of a Recent cinder cone consisting of red to black scoria and tephra that are quarried, crushed and/or directly screened, washed and stockpiled. End products are used for landscaping, light-weight construction aggregate, anti-slip material and soil enhancement. Between 1999 and 2005, annual production ranged between 15,000 – 30,000 cubic metres. In 1998, reserves of tephra, tuff breccia and basalt were estimated to total 44,974,000 tonnes including 4,899,000 tonnes of tephra (GCNL #91, May 12, 1998; GCNL #98, May 22, 1998). The estimate was completed prior to the institution of National Instrument (NI) 43-101 Standards of Disclosure for Mineral Projects and are now regarded to be ‘historic’. No NI 43-101 compliant resource or reserve estimates have since been completed for the project.
Bob (093B 054) The Bob MINFILE occurrence is located 75 km west of Quesnel and approximately five km east of the Nazko property. Work by Lac Minerals Ltd. from 1983-1987 identified a previously unrecognized epithermal gold system within the east-central property area. The system is outlined by anomalous concentrations of gold, arsenic, mercury and antimony in soils, surface rocks and drill holes. Mineralization exhibits characteristics of a low sulphidation deposit type, and mineralization defined to date appears to occur at a relatively high structural level (Pawliuk, 2006). Host rocks are conglomerate, sandstone and minor interbedded argillite of the Cretaceous Skeena Group that dip 15° to the southwest and are cut by north-northeast and west-northwest striking fracture systems with steep dips. Quartz eye-feldspar porphyry dykes and/or sills of probable Tertiary age crosscut the Skeena Group sedimentary rocks. These dykes appear to strike generally north-south. Anomalous concentrations of gold and pathfinder elements are associated primarily with silicic and argillic alteration of the host sedimentary rocks. Hematite and limonite (after pyrite?) appear to be associated with anomalous concentrations of gold. Mineralization consists of widespread pyrite (hematite and limonite if oxidized) with very minor arsenopyrite, stibnite and galena (Brown, 1986). Pyrite also occurs proximally to quartz eye-feldspar porphyry dykes.
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6 2016 EXPLORATION PROGRAM A total of 5 days of field work, excluding travel, were completed to evaluate the southern half of the Nazko property. The fieldwork took place on May 16 - 20, 2016. Access to the property was via a 4x4 pickup truck and quad. The crew consisted of Bob Lane and Bruce Johnson.
The intent of the 2016 exploration program was to evaluate the southern half of the property in an effort to explain previously identified anomalous till and stream sediment geochemistry. The work extended off the claim block in order to assess areas of potentially older bedrock that may project beneath the young volcanic cover that dominates the property, but that post-date any gold mineralization.
The focus of the work was to provide 1:10,000 scale or better coverage of the southern half of the claim block and to complete more detailed assessment of areas in the vicinity of geochemical anomalies.
6.1 BEDROCK MAPPING AND PROSPECTING Bedrock mapping and prospecting covered approximately 1,350 hectares on and adjacent to the southern half of the Nazko claim block south of the Nazko cinder cone. Naturally exposed bedrock (sub-outcrop and outcrop) and that exposed by logging road development was assigned to three distinct geological units: Miocene to Holocene Anahim Volcanics, Eocene Ootsa Lake Group, and Cretaceous Skeena Group.
The area mapped is underlain primarily by basalts of the Anahim Volcanics which form an elongate lobe that extends south from Nazko Cone for about 2.5 km. Older rocks consisting of the Eocene Ootsa Lake Group and Cretaceous Skeena Group are exposed west, south and east of the young volcanics and offer some potential for the discovery of mineralization.
Anahim Volcanics consist primarily of grey weathering, medium to dark grey vesicular olivine basalt. Volumetrically less significant are accumulations of red and black scoria such as the Nazko cone.
The Ootsa Lake Group is made up of a bimodal volcanic assemblage of grey weathering, grey- green, commonly plagioclase porphyritic andesitic basalt and tan to cream to pink rhyolite flows and breccias.
The Skeena Group consists of an interbedded sequence of chert pebble conglomerate, coarse- grained sandstone, siltstone and shale.
Mapping identified a previously unknown window through the young cover rocks to older, locally iron and manganese-altered chert pebble conglomerate and coarse-grained sandstone
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that straddles the western edge of the property. No pyrite or other sulphide minerals were identified but nature of the fracture-controlled earthy hematite, goetite and/or pyrolusite is indicative of alteration peripheral to a heat source. Samples of this style of alteration were collected. The altered sedimentary rocks are in contact with rhyolite breccias of the Ootsa Lake Group that are also variably hematite-altered. In one locality, the rhyolite is cut by several mm- scale vitreous or opalesque silica stringers.
Representative samples were collected from selected stations and retained as references and/or sent for analysis. A map showing the distribution of these units is shown in Figure 5 and a list of weigh points is provided in Appendix A.
In all, a total of eight rock samples were collected and submitted for analysis. Results for an abbreviated list of pathfinder elements are shown in Table 2. Full analytical results are provided in Appendix B. Rock sample locations are shown in Figure 5.
Plate 1: View of the Nazko cinder cone and CANLAVA’s lava rock quarry operation.
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Plate 2: Grey weathering ‘spotted’ andesite of the Ootsa Lake Group
Plate 3: Fracture-controlled Iron and manganese staining of coarse-grained sandstone that underlies the volcanic stratigraphy.
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Plate 4: Iron and manganese-stained rhyolite breccia, Ootsa Lake Group.
7 SAMPLING METHOD AND APPROACH Samples collected in the field were described by the author. All rock samples were placed in heavy poly bags and labeled with a unique sample number. Samples were collected to assess areas of the property for precious and base metal mineralization. A total of eight (8) rock samples were collected and submitted for analysis.
8 SAMPLE PREPARATION, ANALYSES AND SECURITY All samples were packed into large rice bags and driven from the site and placed in a locked private garage prior to shipping. The bagged samples were then sent via commercial carrier to the MS Analytical (MS) laboratory in Langley, BC, for preparation and analysis.
Rock samples were analyzed for a suite of 48 elements by method IMS-230 and for gold by method FAS-111. Two blind certified reference standards were inserted into the sample stream to provide a level of QA/QC. The lab also conducted its own internal quality control assessment of the sample analytical results.
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Table 2: 2016 Rock Sample Locations, Descriptions and Results
Sample Station Au Ag Cu Pb Zn As Sb Easting Northing Lab ID Description ID ID (ppb) (ppm) (ppm) (ppm) (ppm) (ppm) (ppm) grab from outcrop: NA16- WP616 449707 5860446 1440 rhyolite tuff breccia; <0.005 0.42 5.2 73.5 72.6 17.5 <0.5 06 unaltered grab from outcrop: chert pebble NA16- WP485 448957 5862956 1441 conglomerate; <0.005 0.27 14.8 10.8 34.7 19.1 0.7 09 weakly hematite- altered grab from outcrop: chert pebble conglomerate; locally NA16- brittley fractured & WP485 448957 5862956 1442 <0.005 0.23 13.5 7.4 22.9 169 11.4 09B pervasively hematite- altered to red with specularite and/or goethite grab from outcrop: c- gr sandstone; locally brittley fractured NA16- with earthy hematite WP496 448877 5862370 1443 <0.005 0.21 14.8 7.4 55.4 67.4 0.9 11 +/- specularite and/or goethite alteration envelopes on fractures grab from outcrop: NA16- WP518 451982 5862633 1444 rhyolite flow; <0.005 0.23 1.4 6.6 51.4 4.1 <0.5 19 unaltered grab from outcrop: NA16- pink rhyolite breccia WP533 448268 5862934 1445 <0.005 0.4 2.9 9.0 198.8 2.6 <0.5 23 with manganese oxide grab from outcrop: NA16- rhyolite pebble WP542 448208 5861184 1446 <0.005 0.38 7 15.1 86.3 1.1 <0.5 26 breccia; poorly lithified grab from outcrop: rhyolite breccia with transulscent opalesque veinlets; NA16- WP481 449849 5860247 1447 angular shard like <0.005 0.37 11 10.3 197.5 2.4 <0.5 07 clasts in dense rhyolite matrix, larger blocks of banded, devitrified(?) rhyolite
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Figure 4: Nazko Property – Local Geology
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447500 447750 448000 448250 448500 448750 449000 449250 449500 449750 450000 450250 450500 450750 451000 451250 451500 451750 452000 452250 452500 452750 453000
5867500 I 5867500 5867250 5867250
Fishpot Lake 5867000 5867000 5866750 5866750 5866500 5866500
552589 552591 5866250 5866250
M i
5866000 c 5866000 h e l le C re ek Baezaeko FSR 5865750 5865750 5865500 5865500
5865250 329933 5865250
5865000 WP510, 5865000 NA16-14 (!
5864750 552593 5864750
K lu sk us Ro Nazko
5864500 ad 5864500 WP512 (! FSR Cinder 44 Cone 0 0 R o a d WP513,
5864250 NA16-15 5864250 (! WP511 316265 (! 552592
Ootsa Lake 5864000 Group 5864000 WP514, NA16-16 (! WP516(! WP515, (! NA16-17 5863750 5863750 5863500 5863500
5863250 WP536 5863250 (! WP492, NA16-10 (! WP491 (! WP490 WP531, WP535 WP530 (! NA16-22 WP488 WP553 WP534,(! (! (! WP619 WP487 (!(! (! WP521,
5863000 NA16-24 5863000 (! WP532 (! (! (!(! WP485 NA16-20 (! (! WP618 WP533, WP484, (! NA16-23 NA16-09 WP493 (! WP505 WP499 WP509 WP506, (! (! Skeena (! WP620 WP520 WP517, 5862750 NA16-13 Anahim (! NA16-18 5862750 (! (! Group (! (! WP518, WP622 WP494 Volcanics NA16-19 (! (! (! WP495 WP508 552594 (!WP500 (! (! WP503 WP501 5862500 (!(! WP502 5862500 WP507 WP483, WP497 WP496, (! (! NA16-11 NA16-08 WP504 WP498(! (! (! (!(! WP621 5862250 5862250
5862000 WP464, Skeena 5862000 WP473 NA16-01 (! WP463 Ootsa Lake (! WP472 (! (! (! WP474 Group WP466, WP465, Group NA16-03 E(! NA16-02 (! WP467, WP468 5861750 (! NA16-04 5861750
WP471 WP469 (! 5861500 (! 5861500
WP545 (! WP542, WP546 WP543 (!NA16-26 5861250 (! (! 5861250 WP547 (! 1041719
WP548 (! WP551 5861000 WP482 WP549 5861000 (! (!WP550 (! (!
WP478, NA16-05 (! 5860750 Sample ID Station ID Easting Northing Lab ID Description Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Sb (ppm) 5860750 WP480 (! Ootsa Lake NA16-06 WP616 449707 5860446 1440 grab from outcrop: rhyolite tuff breccia; unaltered <0.005 0.42 5.2 73.5 72.6 17.5 <0.5 grab from outcrop: chert pebble conglomerate; NA16-09 WP485 448957 5862956 1441 <0.005 0.27 14.8 10.8 34.7 19.1 0.7 Group weakly hematite-altered WP527, WP479 WP528 NA16-21 WP616, (! grab from outcrop: chert pebble conglomerate; 5860500 (! (! NA16-06 5860500 (! NA16-09B WP485 448957 5862956 1442 locally brittley fractured & pervasively hematite- <0.005 0.23 13.5 7.4 22.9 169 11.4 WP617 (! altered to red with specularite and/or goethite grab from outcrop: c-gr sandstone; locally brittley WP481, NA16-11 WP496 448877 5862370 1443 fractured with earthy hematite +/- specularite <0.005 0.21 14.8 7.4 55.4 67.4 0.9 NA16-07 (! and/or goethite alteration envelopes on fractures
5860250 NA16-19 WP518 451982 5862633 1444 grab from outcrop: rhyolite flow; unaltered <0.005 0.23 1.4 6.6 51.4 4.1 <0.5 5860250 grab from outcrop: pink rhyolite breccia with NA16-23 WP533 448268 5862934 1445 <0.005 0.4 2.9 9.0 198.8 2.6 <0.5 manganese oxide grab from outcrop: rhyolite pebble breccia; poorly NA16-26 WP542 448208 5861184 1446 <0.005 0.38 7 15.1 86.3 1.1 <0.5 lithified k Cree helle grab from outcrop: rhyolite breccia with Mic 5860000 transulscent opalesque veinlets; angular shard like 5860000 NA16-07 WP481 449849 5860247 1447 <0.005 0.37 11 10.3 197.5 2.4 <0.5 clasts in dense rhyolite matrix, larger blocks of banded, devitrified(?) rhyolite
447500 447750 448000 448250 448500 448750 449000 449250 449500 449750 450000 450250 450500 450750 451000 451250 451500 451750 452000 452250 452500 452750 453000
CANLAVA Mining Corp. Legend I Geologic Contacts E Naglico - Float Lake Southern Half of Nazko Property (! Anahim - Outcrop Wetland Bedrock Geology and Sub Outcrop Existing Road Prince Rupert !( Prince George Figure 5 !( Ootsa - Outcrop Mineral Tenure Nazko (! Stream ^_ Property and Sub Outcrop
Date: 06-30-2016 Skeena - Outcrop Vancouver Projection: NAD 1983 UTM Zone 10N (! !( Scale:1:10,000 and Sub Outcrop Author: tkwitkoski
Last Modified By: tkwitkoski Source: US National Park Service Checked By: Revision #:
0 125 250 500
Meters
Path: C:\16PG0107 Bob Lane\2400-GIS Nazko Property\2420-MXD\BedrockGeology_D.mxd NAZKO PROPERTY - 2016 ASSESSMENT REPORT
9 INTERPRETATION AND CONCLUSIONS The limited 2016 bedrock mapping and prospecting program completed on the southern half of the Nazko property identified a previously unrecognized window through the young volcanic cover. The window exposes locally iron and manganese-altered chert pebble conglomerate and coarse-grained sandstone of the Skeena Group that occurs mainly on the western edge of the claim group. It is in contact to the west with hematite-altered rhyolite breccia of the Ootsa Lake Group. Select grab samples from the altered sandstone and conglomerate returned background levels of pathfinder elements, while two samples of rhyolite breccia returned weakly anomalous values for Zn, but background values for the other pathfinder elements.
Despite weak analytical results, further examination of the area west of the claim boundary to more fully evaluate the rhyolite breccia is warranted.
10 RECOMMENDATIONS It is recommended that CANLAVA consider staking the open ground located immediately west of the existing claim block to cover areas underlain by the altered Ootsa Lake Group rhyolitic rocks. Additionally, it is recommended that detailed examination of the new ground be conducted along with an expanded area to more fully cover the potential of the southwest part of the claims in an effort to determine vectors for identifying mineralization in the immediate area.
Should new claims be added, a suggested budget for a 1-week follow-up program of detailed mapping and prospecting is an estimated $13,000.00.
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11 ITEMIZED COST STATEMENT – NAZKO PROPERTY
Dates Nazko Project 2016 Days/Hrs Rate Amount TOTALS Worked
Wages & Salaries (Project Planning, Travel and Fieldwork) May 16- Johnson, B Prospector 5 350 1,750.00 20/16 Project May 15- Lane, B 7 650 4,550.00 Geologist/Manager 21/16 12 6,300.00 6,300.00
Travel (to/from site & on-site) May 15- Plateau Minerals Corp Kms - 4x4 pickup #1 1280 0.6 768.00 21/16 May 16- Plateau Minerals Corp Kms - 4x4 pickup #2 924.00 0.6 554.40 20/16 May 16- Plateau Minerals Corp Quad Rental 5 75 375.00 20/16 1,697.40 1,697.40 Fuel and Consumable Field Supplies Fuel 7 1 200.00
Consumable Field Supplies 7 1 50.00
250.00 250.00 Accommodation and Meals May 16- Crew, Fishpot Lake Shared 4 474.78 19/16 May 15 & Crew, Quesnel Shared 2 578.59 20/16 1053.37 1053.37 Geochemical Analysis & Assaying standards CDN Labs - 2 standards 2 10.00 20.00 shipping Greyhound 1 55.35 55.35 MS Analytical - 8 rock Job # MA0029-JUN16 10 34.62 346.13 samples 421.48 421.48 Consulting - Report Writing & Data Collection/Processing Noble Exploration Maps for Report June, 2016 1 599.50 599.50 Services Allnorth Consultants GIS Mapping Services June, 2016 1 663.83 663.83 Plateau Minerals Corp. PGEO Report Writing June, 2016 2.25 650 1,462.50
2,725.83 2,725.83
Total Cost Nazko Project 2016 12,448.08
CANLAVA MINING CORP. PAGE 18
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
12 REFERENCES Anderson, R.G., Resnick, J., Russell, J.K., Woodsworth, G.J., Villeneuve, M.E., and Grainger, N.C. (2001): The Cheslatta Lake suite: Miocene mafic, alkaline magmatism in central British Columbia; in Canadian Journal of Earth Sciences, v. 38, p. 697-697, Angen, J.J., Westberg, E., Hart, C.J.R., Kim, R. and Rahimi, M. (2015): Preliminary bedrock geology of the TREK area, central British Columbia; Geoscience BC map 2015-10-01, scale 1:250 000. B.C. Geological Survey (2015): MINFILE BC mineral deposits database; B.C. Ministry of Energy and Mines, URL
CANLAVA MINING CORP. PAGE 19
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
Pawliuk, D.J. (2006): Diamond Drill Report on the Nechako Gold Project; BC Ministry of Energy and Mines, Assessment Report 28123, 64 pages. Riddell, J.M. (2011): Lithostratigraphic and tectonic framework of Jurassic and Cretaceous Intermontane sedimentary basins of south-central British Columbia; Canadian Journal of Earth Sciences, v. 48, p. 870–896. Souther, J.G., Clague, J.J. and Mathews, R.W. (1987): Nazko Cone: a Quaternary volcano in the eastern Anahim Belt; Canadian Journal of Earth Sciences, 24, pages 2477-2485.
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NAZKO PROPERTY - 2016 ASSESSMENT REPORT
APPENDIX A – TABULATED WEIGH POINT DATA
CANLAVA MINING CORP.
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
Sample ID Station ID Type Rock Group Northing Easting Description WP460 5861917 450140 end of built road
WP461 5861865 450209 Stream sample03/water02 - previous yr.
WP462 5861830 450250 Bark 06 - previous yr.
sub-angular basalt under tree root WP463 suboutcrop Anahim 5861871 450224 @edge of creek NA16-01 WP464 outcrop Anahim 5861889 449960 grey olivine basalt grey olivine basalt with circular patches NA16-02 WP465 outcrop Anahim 5861798 449957 of chlorite augite phyric angular basalt - Jr/Tr flat, NA16-03 WP466 float Naglico 5861796 449938 sub-angular to sub rounded grey, finely vesicular basalt with white NA16-04 WP467 outcrop Anahim 5861737 449881 spots on weathered surface; fine-grained olivine WP468 outcrop Anahim 5861683 449873 same as WP467
WP469 suboutcrop Anahim 5861443 447718 same as WP467
WP470 5861440 449501 road - North/south
WP471 suboutcrop Anahim 5861481 449727 grey olivine basalt
WP472 suboutcrop Anahim 5861863 449959 same as WP471
grey, finely vesicular basalt with white WP473 outcrop Anahim 5861881 449345 spots on weathered surface; fine-grained
olivine WP474 outcrop Anahim 5861842 449382 grey vesicular olivine
WP475 5861296 449805 end of clear cut - no outcrop
WP476 5860902 449598 edge of clearcut
WP477 5860898 449800 esker
NA16-05 WP478 outcrop Ootsa 5860727 449874 plag phyric olivine basalt plag phyric olivine basalt near ctc with WP479 suboutcrop Ootsa 5860476 449710 biotite-phyric flow banded rhyolite and
rhyolite tuff breecia NA16-06 WP616 outcrop Ootsa 5860446 449707 Rhyolite tuff breccia in ctc with basalt WP617 outcrop Ootsa 5860376 449661 Rhyolite ash tuff
WP480 outcrop Anahim 5860620 449862 frothy vesicular basalt lava - Anahim
NA16-07 WP481 outcrop Ootsa 5860247 449849 flow-banded rhyolite to rhyolite breccia weakly lithified lapilli basalt; bedded - WP482 outcrop Anahim 5860918 449546 100/37SE NA16-08 WP483 outcrop Anahim 5862334 449362 vesicular olivine basalt WP618 outcrop Skeena 5862952 448830 chert pebble conglomerate
from this station to next station: NA16-09 WP484 outcrop Skeena 5862945 448931 greywacke & chert pebble conglomerate WP485 outcrop Skeena 5862956 448957 from WP485 to WP484
from this station to next station: WP487 outcrop Skeena 5862977 448983 greywacke & chert pebble conglomerate
CANLAVA MINING CORP.
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
Sample ID Station ID Type Rock Group Northing Easting Description WP488 outcrop Skeena 5862985 448991 from WP488 to WP487
WP489 5863328 449040 end of built road
WP490 suboutcrop Skeena 5863036 448988 chert pebble conglomerate
WP491 suboutcrop Skeena 5863077 448825 chert pebble conglomerate
chert pebble conglomerate; rusty WP619 outcrop Skeena 5862942 448786 weathering; 6x8m in size grey-brown andesite w late calcite+/- NA16-10 WP492 outcrop Skeena 5863094 448796 zeolite; pseudo breccia texture chert pebble conglomerate; small 2 x 4 WP493 outcrop Skeena 5862817 448741 area chert pebble conglomerate; 50m N-S x WP494 outcrop Skeena 5862595 448755 20m E-W chert pebble conglomerate; 20m N-S x WP495 outcrop Skeena 5862541 448781 4m E-W chert pebble conglomerate edge of road WP620 outcrop Skeena 5862685 448809 (possible float - large, but near larger
exposure on road) greywacke & chert pebble conglomerate NA16-11 WP496 outcrop Skeena 5862370 448877 with fracture-controlled Fe & Mn alteration chert pebble conglomerate; 15m N-S x WP497 outcrop Skeena 5862346 448831 3m E-W WP498 outcrop Skeena 5862306 448733 chert pebble conglomerate
WP621 outcrop Skeena 5862304 448709 chert pebble conglomerate
poorly lithified volcanic conglomerate WP499 outcrop Ootsa 5862740 448598 with rounded clasts up to 30cm across;
12m x 3m chert pebble conglomerate - north end WP622 outcrop Skeena 5862590 448618 of large knob interbedded silstone/shale & sandstone; WP500 outcrop Skeena 5862573 448664 locally cut by hem-mang healed
fractures; bedding: 166/48W WP501 outcrop Skeena 5862523 448677 continuous from last station
chert pebble conglomerate outcrop WP502 outcrop Skeena 5862452 448665 continuous to next station WP503 outcrop Skeena 5862445 448639 continuous from last station
WP504 outcrop Ootsa 5862307 448594 chert pebble conglomerate
plagioclase phyric grey basalt, locally WP505 outcrop Ootsa 5862741 448428 flow-banded NA16-13 WP506 outcrop Ootsa 5862677 448350 pink rhyolite breccia grey, pebbly weathering vesicular basalt; WP507 outcrop Anahim 5862388 449485 blotchy chlorite alteration grey, finely vesicular basalt with white WP508 outcrop Anahim 5862533 449581 spots on weathered surface; fine-grained
olivine
CANLAVA MINING CORP.
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
Sample ID Station ID Type Rock Group Northing Easting Description large ovoid o/c extends from last station WP509 outcrop Anahim 5862750 449578 to WP509 grey vesicular basalt o/c on south side of NA16-14 WP510 outcrop Anahim 5864873 449860 4400 Rd; 40m x 20m blocky weathering pale maroon basalt WP511 outcrop Anahim 5864144 450008 lava and tephra WP512 outcrop Anahim 5864444 449516 o/c continuous from last station NA16-15 WP513 outcrop Anahim 5864172 449188 dk grey olivine basalt breccia buff wthg, poorly lithified tuffaceous NA16-16 WP514 outcrop Ootsa 5863782 449174 sandstone with subrounded rhyolite clasts; 15m x 3m same as last station; o/c extends to NA16-17 WP515 outcrop Ootsa 5863747 449180 WP516 WP516 outcrop Ootsa 5863728 449173 o/c extends from last station
pale grey f-gr sandstone-siltstone-shale; NA16-18 WP517 outcrop Skeena 5862665 451919 bedding uncertain; jointing: 070/75S; 50m x 4m road cut exposure NA16-19 WP518 outcrop Ootsa 5862633 451982 rhyolite flow; unaltered; 15m x 2m WP519 meadow 5862059 451949
dark grey shale in road bed and road cut; WP520 outcrop Skeena 5862698 451868 12m x 3m area of vesicular and amygdaloidal grey andesite; upslope are several NA16-20 WP521 suboutcrop Ootsa 5862910 451862 suboutcrops of white weathering, cream-coloured rhyolite w liesegang rings WP523 outcrop Skeena 5857619 450365 grey shale; bedding: 104/20N
WP524 outcrop Skeena 5857907 449728 grey shale; bedding: 104/20N
WP525 - 5860291 449646 quad - start of trav
WP526 - 5860460 449386 S edge of small alke
greenish-grey olivine basalt with white NA16-21 WP527 outcrop Anahim 5860456 449356 spots on weathered surface WP528 outcrop Anahim 5860457 449315 o/c semi continuous to WP528
WP529 5860599 448750 turn around point - end of trav
polylithic volcanic WP530 outcrop Ootsa 5862989 448367 brecccia/conglomerate; clasts include bt-
phyric rhyolite NA16-22 WP531 outcrop Ootsa 5862974 448324 as above as above; pink colouration due to WP532 outcrop Ootsa 5862946 448286 pervasie hematite; local manganese
oxide grab from outcrop: pink rhyolite breccia NA16-23 WP533 outcrop Ootsa 5862934 448268 with manganese oxide NA16-24 WP534 outcrop Ootsa 5862927 448190 volcanic breccia; ash matrix; hematitic
CANLAVA MINING CORP.
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
Sample ID Station ID Type Rock Group Northing Easting Description o/c continues along road bed in curved WP535 outcrop Anahim 5863003 448181 fashion to WP535 where it consists of
bombs in mafic ash - Anahim immature pale grey (volcanic) sandstone WP536 outcrop Skeena 5863179 448059 or greywacke; 25m x 2m WP539 5863939 447384 end of spur road
grab from outcrop: rhyolite pebble NA16-26 WP542 outcrop Ootsa 5861184 448208 breccia; poorly lithified WP543 outcrop Ootsa 5861231 448201 o/c continues from last station to WP543
WP544 5861849 447784 end of upper road
o/c from end of road on road bed to WP548 volcanic breccia: predominaatly WP545 outcrop Ootsa 5861268 448060 sub-angular rhyolite clasts in tuffaceous matrix WP546 outcrop Ootsa 5861203 448028 o/c in road bed continues
WP547 outcrop Ootsa 5861097 447956 o/c in road bed continues
WP548 outcrop Anahim 5860971 447863 end of o/c in mafic volcanic breccia
WP549 suboutcrop Anahim 5860917 450019 andesite-basalt breccia
white-spotted pale grey basalt, angular WP550 suboutcrop Anahim 5860888 449730 blocks white-spotted pale grey basalt, angular WP551 suboutcrop Anahim 5860934 449730 blocks WP552 till 5863326 449039 end of road
chert pebble conglomerate; rusty WP553 outcrop Skeena 5862977 449211 weathering; 2m x 2m in road bed/road
cut end of trav from last station - no o/c WP554 5862477 449040 encountered
CANLAVA MINING CORP.
NAZKO PROPERTY - 2016 ASSESSMENT REPORT
APPENDIX B – LABORATORY CERTIFICATES
CANLAVA MINING CORP.
Met-Solve Analytical Services Inc. To: Plateau Minerals Corp. Unit 1, 20120 102nd Avenue 3000 - 18th St Langley, BC V1M 4B4 Vernon, BC An A2 Global Company Phone: +1-604-888-0875 V1T 4A6 CERTIFICATE OF ANALYSIS: MA0029-JUN16 SAMPLE PREPARATION METHOD CODE DESCRIPTION Project Name: Plateau PRP-910 Dry, Crush to 70% passing 2mm, Split 250g, Pulverize to 85% passing 75µm Job Received Date: 09-Jun-2016 Job Report Date: 28-Jun-2016 Report Version: Final ANALYTICAL METHODS METHOD CODE DESCRIPTION COMMENTS: FAS-111 Au, Fire Assay, 30g fusion, AAS, Trace Level Detection limit for sodium changed to 0.2% due to matrix IMS-230 Multi-Element, 0.2g, 4-Acid, ICP-AES/MS, Ultra Trace Level interferences.
Test results reported relate only to the samples as received by the laboratory.Unless otherwise stated above, sufficient sample was received for the methods requested and all samples were received in acceptable condition. Analytical results in unsigned reports marked "preliminary" are subject to change, pending final QC review. Please refer to Met-Solve Analytical Services' Schedule of Services and Fees for our complete Terms and Conditions
Signature: Jimbo Zheng BSc., PChem, BC Certified Assayer Senior Analytical Chemist Met-Solve Analytical Services Inc.
Page 1 of 6 Met-Solve Analytical Services Inc. To: Plateau Minerals Corp. Unit 1, 20120 102nd Avenue 3000 - 18th St Langley, BC V1M 4B4 Vernon, BC An A2 Global Company Phone: +1-604-888-0875 V1T 4A6 CERTIFICATE OF ANALYSIS: MA0029-JUN16
Project Name: Plateau Job Received Date: 09-Jun-2016 Job Report Date: 28-Jun-2016 Report Version: Final
Sample PWE-100 Method FAS-111 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 Type Rec. Wt. Analyte Au Ag Al As Ba Be Bi Ca kg Units ppm ppm % ppm ppm ppm ppm % Sample ID 0.01 LOR 0.005 0.01 0.01 0.2 10 0.05 0.01 0.01 01435 Rock 0.85 <0.005 0.29 0.33 11.2 200 0.36 0.01 17.72 01436 Rock 1.59 <0.005 0.08 0.07 4.0 32 0.15 0.02 3.77 01437 Rock 2.64 0.017 0.63 2.10 49.6 490 0.87 0.14 10.34 01438 Rock 1.90 <0.005 0.19 1.41 5.8 215 0.78 0.13 19.33 01439 Pulp 0.23 2.988 >100 4.59 2776.8 1736 0.91 16.30 3.66 01440 Rock 1.17 <0.005 0.42 6.26 17.5 1118 2.27 0.07 0.68 01441 Rock 1.44 <0.005 0.27 2.51 19.1 321 0.51 0.07 0.09 01442 Rock 2.32 <0.005 0.23 0.82 169.0 395 0.38 0.07 0.02 01443 Rock 1.87 <0.005 0.21 3.81 67.4 188 0.51 0.04 0.04 01444 Rock 0.59 <0.005 0.23 7.39 4.1 1160 2.01 0.02 0.17 01445 Rock 0.75 <0.005 0.40 8.79 2.6 1183 1.40 0.02 3.01 01446 Rock 0.95 <0.005 0.38 7.34 1.1 1176 2.26 0.16 0.91 01447 Rock 1.46 <0.005 0.37 7.49 2.4 1188 1.89 0.05 2.07 01448 Pulp 0.23 0.491 4.12 7.32 27.4 337 0.87 0.99 1.31 01449 Pulp 0.23 8.411 1.47 6.08 20.8 1357 1.07 0.33 1.55 DUP 01435 0.29 0.32 11.0 158 0.33 <0.01 17.75 DUP 01449 8.581 STD BLANK <0.01 <0.01 <0.2 <10 <0.05 <0.01 <0.01 STD BLANK <0.005 STD OREAS 24b 0.16 7.91 8.1 692 2.92 0.74 1.07 STD CDN-GS-2Q 2.319
***Please refer to the cover page for comments regarding this certificate. *** Page 2 of 6 Met-Solve Analytical Services Inc. To: Plateau Minerals Corp. Unit 1, 20120 102nd Avenue 3000 - 18th St Langley, BC V1M 4B4 Vernon, BC An A2 Global Company Phone: +1-604-888-0875 V1T 4A6 CERTIFICATE OF ANALYSIS: MA0029-JUN16
Project Name: Plateau Job Received Date: 09-Jun-2016 Job Report Date: 28-Jun-2016 Report Version: Final
IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 Cd Ce Co Cr Cs Cu Fe Ga Ge Hf In ppm ppm ppm ppm ppm ppm % ppm ppm ppm ppm Sample ID 0.02 0.01 0.1 1 0.05 0.2 0.01 0.05 0.05 0.1 0.005 01435 16.32 4.87 3.2 29 1.57 4.5 5.70 1.09 0.17 <0.1 <0.005 01436 71.76 2.29 1.4 98 0.16 3.2 3.32 0.58 0.12 <0.1 <0.005 01437 85.96 26.34 10.7 103 0.76 20.8 15.66 7.76 0.40 0.1 0.023 01438 0.25 36.81 10.4 14 0.53 4.5 1.98 3.50 0.12 <0.1 0.010 01439 133.04 >500 63.1 43 7.12 7648.8 9.41 26.54 1.13 1.2 37.279 01440 0.27 55.77 1.0 83 2.77 5.2 0.61 13.47 0.34 2.7 0.047 01441 0.23 19.85 6.0 182 0.56 14.8 1.38 5.87 0.20 1.0 0.023 01442 0.09 15.89 1.6 342 0.60 13.5 7.86 4.89 0.24 0.6 0.018 01443 0.13 18.96 5.5 223 0.57 14.8 9.99 8.24 0.34 1.5 0.026 01444 0.03 35.20 0.7 52 1.58 1.4 0.50 14.13 0.21 2.0 <0.005 01445 0.10 55.21 9.0 22 0.77 2.9 3.09 18.73 0.59 4.8 0.050 01446 0.13 57.17 2.9 46 3.44 7.0 1.26 15.50 0.38 3.2 0.034 01447 0.10 50.39 5.6 23 1.30 11.0 2.56 15.69 0.53 4.8 0.041 01448 4.25 26.86 12.3 40 7.76 3805.0 5.46 14.85 0.34 0.3 0.244 01449 1.66 24.53 12.4 41 6.43 56.6 3.78 14.53 0.33 1.7 0.043 DUP 01435 15.61 4.64 2.9 28 1.47 4.7 5.76 1.01 0.15 <0.1 <0.005 DUP 01449 STD BLANK <0.02 <0.01 <0.1 <1 <0.05 <0.2 <0.01 <0.05 <0.05 <0.1 <0.005 STD BLANK STD OREAS 24b 0.06 82.76 16.9 111 10.74 38.0 4.42 20.40 0.76 4.1 0.074 STD CDN-GS-2Q
***Please refer to the cover page for comments regarding this certificate. *** Page 3 of 6 Met-Solve Analytical Services Inc. To: Plateau Minerals Corp. Unit 1, 20120 102nd Avenue 3000 - 18th St Langley, BC V1M 4B4 Vernon, BC An A2 Global Company Phone: +1-604-888-0875 V1T 4A6 CERTIFICATE OF ANALYSIS: MA0029-JUN16
Project Name: Plateau Job Received Date: 09-Jun-2016 Job Report Date: 28-Jun-2016 Report Version: Final
IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 K La Li Mg Mn Mo Na Nb Ni P Pb % ppm ppm % ppm ppm % ppm ppm ppm ppm Sample ID 0.01 0.5 0.2 0.01 5 0.05 0.2 0.1 0.2 10 0.5 01435 0.43 3.7 83.6 10.09 369 1.96 <0.2 0.3 10.2 138 720.7 01436 0.04 2.0 2.6 1.23 96 2.88 <0.2 0.1 9.7 1233 1817.4 01437 1.16 12.7 9.9 4.00 361 3.37 <0.2 1.6 52.5 210 >10000 01438 0.77 17.5 8.3 10.80 483 0.19 <0.2 1.1 23.2 479 115.8 01439 1.51 489.9 13.8 1.55 2181 73.15 0.6 108.7 43.0 3230 7176.8 01440 3.08 28.8 13.7 0.18 237 2.43 2.3 10.5 4.1 159 73.5 01441 0.50 9.8 9.4 0.14 88 2.44 <0.2 2.9 26.1 146 10.8 01442 0.30 8.0 3.7 0.07 71 1.60 <0.2 1.8 9.2 257 7.4 01443 0.38 9.6 11.7 0.07 106 3.51 <0.2 4.4 31.6 144 7.4 01444 3.50 18.8 11.1 0.08 219 0.51 1.8 8.7 8.0 93 6.6 01445 2.33 26.4 8.4 0.30 358 2.55 2.8 10.4 8.4 2801 9.0 01446 3.51 30.2 6.1 0.51 519 2.63 1.8 11.6 15.5 254 15.1 01447 2.36 24.1 4.7 0.10 438 1.56 2.7 11.2 3.7 1651 10.3 01448 2.50 13.3 24.2 0.81 983 19.68 0.6 3.5 25.8 716 110.3 01449 1.84 11.3 29.8 0.90 490 891.77 1.6 3.1 30.7 432 11.4 DUP 01435 0.42 3.5 76.6 10.13 370 1.80 <0.2 0.3 9.6 129 727.8 DUP 01449 STD BLANK <0.01 <0.5 <0.2 <0.01 <5 <0.05 <0.2 <0.1 <0.2 <10 <0.5 STD BLANK STD OREAS 24b 2.78 42.2 52.9 1.62 433 4.01 0.8 14.6 59.7 674 22.8 STD CDN-GS-2Q
***Please refer to the cover page for comments regarding this certificate. *** Page 4 of 6 Met-Solve Analytical Services Inc. To: Plateau Minerals Corp. Unit 1, 20120 102nd Avenue 3000 - 18th St Langley, BC V1M 4B4 Vernon, BC An A2 Global Company Phone: +1-604-888-0875 V1T 4A6 CERTIFICATE OF ANALYSIS: MA0029-JUN16
Project Name: Plateau Job Received Date: 09-Jun-2016 Job Report Date: 28-Jun-2016 Report Version: Final
IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 Rb Re S Sb Sc Se Sn Sr Ta Te Th ppm ppm % ppm ppm ppm ppm ppm ppm ppm ppm Sample ID 0.1 0.002 0.01 0.5 0.1 1 0.2 0.2 0.05 0.05 0.2 01435 17.3 0.002 6.81 1.8 1.0 <1 <0.2 127.8 <0.05 <0.05 0.5 01436 1.3 <0.002 4.82 1.0 0.1 <1 <0.2 29.1 <0.05 <0.05 <0.2 01437 34.8 0.006 >10 9.8 4.4 2 0.8 162.9 0.09 <0.05 3.6 01438 22.4 <0.002 1.43 <0.5 4.2 <1 0.3 148.0 0.07 <0.05 3.9 01439 61.2 0.028 6.03 327.2 10.2 7 >500 626.4 0.42 0.05 89.3 01440 108.1 0.002 0.02 <0.5 2.6 <1 1.6 119.7 0.80 <0.05 8.6 01441 19.2 0.003 <0.01 0.7 5.5 <1 0.6 56.0 0.21 <0.05 2.1 01442 12.7 <0.002 0.03 11.4 3.0 <1 0.6 68.6 0.13 <0.05 1.6 01443 13.5 <0.002 0.02 0.9 6.1 <1 0.6 53.0 0.37 <0.05 2.7 01444 125.0 <0.002 <0.01 <0.5 1.5 <1 0.4 183.3 0.78 <0.05 7.2 01445 58.3 0.002 <0.01 <0.5 11.9 <1 1.1 622.1 0.67 <0.05 5.6 01446 112.3 0.002 <0.01 <0.5 4.0 <1 1.1 175.4 0.90 <0.05 9.2 01447 68.6 <0.002 <0.01 <0.5 7.5 <1 1.1 539.6 0.69 <0.05 5.3 01448 82.5 0.159 3.43 1.8 7.6 4 1.6 166.2 0.29 0.07 4.1 01449 46.4 0.052 1.34 33.8 9.3 8 2.3 299.5 0.25 0.10 2.2 DUP 01435 16.0 0.003 6.87 1.7 1.0 <1 <0.2 126.5 <0.05 <0.05 0.6 DUP 01449 STD BLANK <0.1 <0.002 <0.01 <0.5 <0.1 <1 <0.2 <0.2 <0.05 <0.05 <0.2 STD BLANK STD OREAS 24b 165.7 0.003 0.19 0.9 16.0 <1 4.0 123.1 1.28 <0.05 17.1 STD CDN-GS-2Q
***Please refer to the cover page for comments regarding this certificate. *** Page 5 of 6 Met-Solve Analytical Services Inc. To: Plateau Minerals Corp. Unit 1, 20120 102nd Avenue 3000 - 18th St Langley, BC V1M 4B4 Vernon, BC An A2 Global Company Phone: +1-604-888-0875 V1T 4A6 CERTIFICATE OF ANALYSIS: MA0029-JUN16
Project Name: Plateau Job Received Date: 09-Jun-2016 Job Report Date: 28-Jun-2016 Report Version: Final
IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 IMS-230 Ti Tl U V W Y Zn Zr % ppm ppm ppm ppm ppm ppm ppm Sample ID 0.01 0.02 0.1 1 0.1 0.1 2 0.5 01435 <0.01 40.91 1.1 30 0.1 3.0 >10000 1.7 01436 <0.01 31.48 8.8 8 4.1 2.7 >10000 0.8 01437 0.07 10.86 1.2 52 0.5 5.5 >10000 4.0 01438 0.05 4.91 0.7 24 0.5 9.7 85 2.2 01439 0.16 7.49 3.0 69 16.7 13.2 >10000 38.5 01440 0.07 0.96 2.8 8 0.9 16.1 81 72.6 01441 0.14 0.20 0.9 49 4.1 6.1 73 34.7 01442 0.10 0.15 0.7 64 0.5 3.3 34 22.9 01443 0.18 0.16 1.2 68 3.7 6.5 70 55.4 01444 0.05 1.06 2.5 3 0.5 7.9 21 51.4 01445 0.69 0.15 1.9 91 1.4 17.2 83 198.8 01446 0.12 0.81 3.6 32 0.9 16.5 63 86.3 01447 0.48 0.23 1.7 51 1.3 12.5 80 197.5 01448 0.18 1.44 0.8 73 2.6 7.4 941 7.8 01449 0.25 5.67 0.9 255 32.1 8.9 68 62.9 DUP 01435 <0.01 37.76 1.0 29 <0.1 2.9 >10000 1.8 DUP 01449 STD BLANK <0.01 <0.02 <0.1 <1 <0.1 <0.1 <2 <0.5 STD BLANK STD OREAS 24b 0.47 0.89 3.0 106 3.8 20.1 109 139.6 STD CDN-GS-2Q
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