2019 TEST PITTING 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: 5747079
Prepared for: CANLAVA Mining Corp. B140 5525 272nd Street Langley, B.C. V4W 1P1
Prepared by: R. A. (Bob) Lane, P.Geo. Plateau Minerals Corp.
Date: September 5, 2019
NAZKO PROPERTY – 2019 ASSESSMENT REPORT
TABLE OF CONTENTS
1 EXECUTIVE SUMMARY ...... 1 INTRODUCTION ...... 2 1.1 LOCATION AND ACCESS ...... 2 1.2 PHYSIOGRAPHY AND CLIMATE ...... 2 1.3 PROPERTY STATUS AND OWNERSHIP ...... 2 1.4 DEVELOPMENT AND EXPLORATION HISTORY ...... 4 2 REGIONAL GEOLOGY ...... 6 3 PROPERTY GEOLOGY ...... 7 4 MINERALIZATION ...... 9 5 2019 EXPLORATION PROGRAM ...... 12 6 INTERPRETATION AND CONCLUSIONS ...... 19 7 RECOMMENDATIONS ...... 19 8 ITEMIZED COST STATEMENT – NAZKO PROPERTY ...... 20 9 REFERENCES ...... 21 10 STATEMENTS OF QUALIFICATIONS ...... 23
LIST OF TABLES TABLE 1: NAZKO PROPERTY – LIST OF MINERAL TENURES ...... 4 TABLE 2: TEST PIT LOCATIONS AND THICKNESSES OF TEPHRA ...... 13
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 ...... 11 FIGURE 5: TEST PIT LOCATIONS ...... 14 FIGURE 6: TEST PIT P19-3 ...... 15 FIGURE 7: TEST P19-9 ...... 16 FIGURE 8: TEST PIT (ROAD CUT) P19-13 ...... 17 FIGURE 9: TEST PIT P19-19 ...... 18
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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 seven mineral claims that cover 1,481.43 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 are currently being mined and processed on the mining leases into finished product by owner-operator CANLAVA. Underling rocks include prospective Eocence Ootsa Lake Group rhyolitic volcanics and Cretaceous Skeena Group fine to coarse-grained siliciclastics.
The intent of the 2019 test pitting program was to identify new sources of black tephra principally on tenures 552589 and 552591 north of the mine leases. A total of 23 sites were investigated using either a John Deere loader and/or hand tools to excavate new test pits, clean previously dug pits, and/or clean off existing road cuts to expose fresh surficial material. Of the 23 sites evaluated, only two had thickness of black tephra that were greater than 1m. Both sites were on or near the northern margin of the mine lease and suggest that a blanket of the desirable black tephra may occupy the northern edge of the lease/southern edge of claims 552589 and 552591.
It is recommended that CANLAVA continue with its test pitting program to explore for additional sources of black tephra to enhance its existing resource. A budget for a 1-week program of mechanical test pitting is an estimated $15,000.00.
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INTRODUCTION
This assessment report has been prepared at the request of CANLAVA Mining Corp. (CANLAVA) to summarize results of a test pitting program completed in May - July 2019 on its Nazko property. This assessment report was prepared by independent Qualified Person R.A. (Bob) Lane, P.Geo.
1.1 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 clearcut 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.
1.2 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.
1.3 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 seven mineral claims that cover an additional 1,481.43 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
Good To Title Number Claim Name Title Type Issue Date Area (ha) Date 316265 Mineral Lease 1993/AUG/20 2020/AUG/20 200.00
329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00
552589 LAVA 7 Mineral Claim 2007/FEB/23 2020/MAY/03 155.86
552591 Mineral Claim 2007/FEB/23 2020/MAY/03 116.90
552592 LAVA 8 Mineral Claim 2007/FEB/23 2020/MAY/03 194.89
552593 LAVA 9 Mineral Claim 2007/FEB/23 2020/MAY/03 155.90
552594 LAVA 10 Mineral Claim 2007/FEB/23 2020/MAY/03 331.43
1041719 CANLAVA SOUTHWEST Mineral Claim 2016/FEB/01 2020/MAY/03 97.51
1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2020/MAY/03 272.95
Mineral Claim Total 1,481.43
All leases and claims are owned 100% by Canlava Mining Corp.
1.4 DEVELOPMENT AND EXPLORATION HISTORY
The Nazko property covers the Recent Nazko cinder cone where scoria and tephra are 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.
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CanLava Mining Legend I Corporation Existing Road NAZKO PROJECT Prince Rupert !( Mineral Tenure Stream Prince George !( Figure 2 Nazko Mineral Tenure ^_ Property Date: 2019-09-05 Projection: NAD 1983 UTM Zone 10N Vancouver Scale:1:50,000 Lake !( Author: tkwitkoski Last Modified By: tkwitkoski Source: US National Park Service Checked By: BL Revision #: Wetland
0 250 500 1,000 1,500
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2 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 (Figure 3). 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).
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
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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).
3 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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CanLava Mining Legend I Coporation Existing Road NAZKO PROJECT Prince Rupert Prince Stream !( George Regional Geology !( Figure 3 Nazko Mineral Tenure Outline ^_ Property
Date: 2019-09-05 Projection: NAD 1983 UTM Zone 10N Vancouver Scale:1:100,000 Lake !( Author: tkwitkoski Last Modified By: tkwitkoski Source: US National Park Service Checked By: BL Revision #:
0 0.5 1 2 3
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4 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
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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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CANLAVA Legend I Mining Corp. Existing Road Local Geology NAZKO PROJECT EO, Ootsa Lake Group Prince Rupert Stream !( Local Geology Prince George !( Nazko Figure 4 EOlEv, Endako Group Mineral Tenure Outline ^_ Property Date: 2019-09-05 Projection: NAD 1983 UTM Zone 10N Hovb, Unnamed Vancouver Scale:1:40,000 Lake !( Author: tkwitkoski Last Modified By: tkwitkoski Source: US National Park Service Checked By: MiPlCvb, Chilcotin Group Revision #:
0 0.5 1 lKS, Skeena Group Kilometers Path: E:\19PG0003 Bob Lane\2400-GIS Nazko Property\2420-MXD\LocalGeology_A.mxd NAZKO PROPERTY – 2019 ASSESSMENT REPORT
5 2019 EXPLORATION PROGRAM
In late May and early June a test pitting program was completed on the Nazko property. The intent of the work, which took place on claims north of the mining leases, was to identify additional meaningful thicknesses of glassy black tephra that could contribute to the mine’s overall resource base.
A total of 23 sites (Table 4 and Figure 5) were investigated using either a John Deere 844J rubber-tired loader and/or hand tools to excavate new test pits, clean previously dug pits, and/or clean off existing road cuts to expose fresh surficial material. Of the 23 sites, 12 were new test pits, 6 were previously excavated/unreclaimed sites (that required minor cleaning of walls to remove sloughed material), and 5 were existing road cuts (that required minor scraping to expose fresh material). At each site, near vertical cuts exposed fresh surficial material that was then measured (Figures 6 – 8) from surface downwards to either a compact glacial till or purple volcanic rock ‘basement’. A representative sample from all but four sites was collected, bagged and tagged, and retained for future reference. No analytical work was performed on the samples. At the completion of the program all sites were reclaimed.
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Table 2: Test Pit Locations and Thicknesses of Tephra
Test Pit Location Thickness (cm) Depth to Depth to Station ID Date Easting Northing Overburden Tephra rusty Tephra black Tephra grey Glacial Till Bedrock Comments P19-1 1-Jun-19 450884 5866137 na 20 46 - 66 na cleaning of existing road cut P19-2 1-Jun-19 450956 5866081 na 36 61 - 97 na P19-3 1-Jun-19 451030 5866036 na 30 66 - - 96 P19-4 1-Jun-19 451051 5865982 8 30 76 - - 114 cleaning of existing road cut P19-5 1-Jun-19 451044 5865911 5 25 69 - - 99 cleaning of historic pit (1 of P19-6 1-Jun-19 450990 5865861 10 10 76 - 96 na 5); later reclaimed cleaning of historic pit (5 of P19-7 1-Jun-19 450938 5865822 na 18 48 30 - 96 5); later reclaimed P19-8 1-Jun-19 450867 5865784 10 15 50 - - 75 cleaning of existing road cut cleaning of historic pit; later P19-9 1-Jun-19 451038 5865771 10 23 97 - - 130 reclaimed cleaning of historic pit; later P19-10 1-Jun-19 451001 5865737 5 15 86 - - 106 reclaimed cleaning of historic pit; later P19-11 1-Jun-19 450959 5865744 na 25 64 - - 89 reclaimed cleaning of historic pit; later P19-12 1-Jun-19 450932 5865774 na 20 38 - - 58 reclaimed P19-13 2-Jun-19 451182 5866044 13 51 61 - 125 na P19-14 2-Jun-19 451431 5865919 13 25 28 - 66 na P19-15 2-Jun-19 451392 5865746 8 10 18 - 36 na no sample collected P19-16 2-Jun-19 451339 5865597 5 15 0 - 20 na no sample collected P19-17 2-Jun-19 450700 5865597 10 18 117 145 na
P19-18 2-Jun-19 450574 5865729 5 23 41 38 102 na P19-19 2-Jun-19 450442 5865711 8 36 84 - 128 na P19-20 2-Jun-19 450224 5865787 5 13 20 - 38 na no sample collected P19-21 2-Jun-19 450090 5865798 5 10 0 20 35 na no sample collected P19-22 2-Jun-19 450875 5865489 8 25 127 - 160 na cleaning of existing road cut shovel-cleaning of old road P19-23 2-Jun-19 451185 5865484 8 23 64 - 75 na cut
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450000 451000 I
Mi che lle C ree k B a e za eko FSR P19-1, 46cm !( P19-2, 61cm !( P19-13, 61cm !( 552589 P19-3, 66cm !(
P19-4. 76cm !( 552591 5866000 5866000
!( P19-5, 69cm !( P19-14, 28cm !( P19-6, 76cm P19-7, 48cm P19-21, 0cm !( P19-20, 20cm !( !( P19-8, 50cm!( !( !( P19-9, 97cm P19-18, 41cm P19-12, 38cm !( !( !( !( P19-10, 86cm P19-15, 18cm !( P19-11 64cm P19-19, 84cm
!( P19-17, 117cm !( P19-16, 0cm
!( !( P19-23, 64cm P19-22, 127cm
329933 552592 5865000 5865000
450000 451000 Legend I CanLava Mining !( Test Pits (Stn ID, Tephra Black cm) Corporation Existing Road NAZKO PROJECT Prince Rupert !( Test Pits Stream Prince George !( Figure 5 Nazko Mineral Tenure ^_ Property Date: 2019-09-05 Projection: NAD 1983 UTM Zone 10N Vancouver Scale:1:10,000 Lake !( Author: tkwitkoski Last Modified By: tkwitkoski Source: US National Park Service Checked By: BL Revision #: Wetland
Path: E:\19PG0003 Bob Lane\2400-GIS Nazko Property\2420-MXD\TestPitLocaiton_A.mxd NAZKO PROPERTY – 2019 ASSESSMENT REPORT
Figure 6: Test Pit P19-3
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Figure 7: Test P19-9
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Figure 8: Test Pit (road cut) P19-13
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Figure 9: Test Pit P19-19
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6 INTERPRETATION AND CONCLUSIONS
The 2019 test pitting program successfully identified areas of black tephra. Of the 23 sites evaluated, only two had thickness of black tephra that were greater than 1m. Both sites were on or near the northern margin of the mine lease and suggest that a blanket of the desirable black tephra may occupy the northern edge of the lease/southern edge of claims 552589 and 552591. The paleotopography of the area is very irregular, creating the possibility that much thicker accumulations of tephra may exist in the immediate area and/or in other nearby areas, and therefore the claims merit further investigation.
7 RECOMMENDATIONS
It is recommended that CANLAVA continue with its test pitting program to explore for additional sources of black tephra to enhance its existing resource. A budget for a 1-week program of mechanical test pitting is an estimated $15,000.00.
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8 ITEMIZED COST STATEMENT – NAZKO PROPERTY
Nazko Project 2019 Dates Worked Da ys/Hrs Ra te Amount TOTALS
Wages & Salaries (Project Planning, Travel and Fieldwork) May 30 - Jun 3 & Jul 3, Johnson, B Prospector 5 400.00 2,000.00 2019 May 30 - Jun 4 & Jul 2- Lane, B Project Geologist/Manager 7 700.00 4,900.00 4, 2019 10.5 6,900.00 6,900.00
Travel (to/from site & on- site)
Plateau Minerals Corp. Kms - 4x4 pickup #1 May 30 - Jun 4, 2019 1,061 0.75 795.75
Plateau Minerals Corp. Kms - 4x4 pickup #2 May 30 - Jun 3, 2019 1,501 0.75 1,125.75
Plateau Minerals Corp. Kms - 4x4 pickup #1 Jul 2-4, 2019 779 0.75 584.25 2,505.75 2,505.75 2019 Test Pitting - Loader+Operator Canlava 16.5 hours June 1 -2, 2019 16.5 220.00 3,630.00 Per diem 2 days June 1 -2, 2019 2 180 360.00 3,990.00 3,990.00 Rentals, Fuel & Consumable Field Supplies
Quad Rental (daily rate) Jun 1 & 3; Jul 3, 2019 3 85.00 255.00
Chainsaws (daily rate) 03-Jul-19 2 35.00 70.00
Fuel May 30 - Jun 4, 2019 3 1 301.94
Fuel Jul 2-4, 2019 1 1 156.11
Grass Seed May 30 - Jun 4, 2019 1 75 301.94 Consumable Field Supplies May 30 - Jun 4, 2019 6 1 50.00
1,134.99 1,134.99
Accommodation and Meals
Meals May 30 - Jun 4, 2019 11 287.46
Meals Jul 2-4, 2019 3 150.83
Accom, Williams Lake Jul 2-3, 2019 2 60 120.00
Accom, Quesnel May 30 - Jun 4, 2019 9 996.68 1554.97 1554.97
Consulting - Report Writing & Data Collection/Processing
Consus Mngmt GIS Mapping Services May, 2019 1 866.25 866.25
Allnorth Consultants Maps for Report Sep, 2019 1 450.00 450.00 Data Processing & Report Plateau Minerals Corp. Sep, 2019 2 700.00 1400.00 Writing 2,716.25 2,716.25
TOTAL 18,801.96
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9 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
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Lane, R.A. (2016): 2016 Geological Report on the Nazko Property; BC Ministry of Energy and Mines, Assessment Report 36171, 38 pages.
Lane, R.A. (2017): 2017 Geological Report on the Nazko Property; BC Ministry of Energy and Mines, Assessment Report 36974, 41 pages.
Machibroda, R. (2007): Volcanic Deposits at the Nazko Lava Quarry, Evaluation of Reserves; 78 pages.
Pawliuk, D.J. (2006): Diamond Drill Report on the Nechako Gold Project; BC Ministry of Energy and Mines, Assessment Report 28123, 64 pages.
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