2018 FALL GEOPHYSICAL 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: 5723043
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: December 20, 2018
NAZKO PROPERTY – 2018 FALL ASSESSMENT REPORT
TABLE OF CONTENTS
1 EXECUTIVE SUMMARY ...... 1 2 INTRODUCTION ...... 3 2.1 LOCATION AND ACCESS ...... 3 2.2 PHYSIOGRAPHY AND CLIMATE ...... 3 2.3 PROPERTY STATUS AND OWNERSHIP ...... 3 2.4 DEVELOPMENT AND EXPLORATION HISTORY ...... 5 3 REGIONAL GEOLOGY ...... 7 4 PROPERTY GEOLOGY ...... 8 5 MINERALIZATION ...... 10 6 2018 EXPLORATION PROGRAM ...... 13 6.1 INSTRUMENTATION ...... 13 6.2 THEORY ...... 13 6.3 SURVEY PROCEDURE ...... 14 6.4 COMPILATION OF DATA ...... 14 6.5 DISCUSSION OF RESULTS...... 14 7 INTERPRETATION AND CONCLUSIONS ...... 20 8 RECOMMENDATIONS ...... 20 9 ITEMIZED COST STATEMENT – NAZKO PROPERTY ...... 21 10 REFERENCES ...... 22 11 STATEMENTS OF QUALIFICATIONS ...... 24
LIST OF TABLES TABLE 1: NAZKO PROPERTY – LIST OF MINERAL TENURES ...... 5
LIST OF FIGURES FIGURE 1: NAZKO PROPERTY - LOCATION ...... 4 FIGURE 2: NAZKO PROPERTY - MINERAL TENURE ...... 6 FIGURE 3: NAZKO AREA - REGIONAL GEOLOGY ...... 9 FIGURE 4: NAZKO PROPERTY – LOCAL GEOLOGY ...... 12 FIGURE 5: 2018 VLF-EM SURVEY LOCATION - NAZKO PROPERTY ...... 16 FIGURE 6: 2018 VLF-EM SURVEY STATIONS - NAZKO PROPERTY ...... 17 FIGURE 7: 2018 FALL VLF FRASER-FILTERED DATA - NAZKO PROPERTY ...... 18 FIGURE 8: COMBINED SPRING-FALL VLF FRASER-FILTERED DATA – NAZKO PROPERTY ...... 19
LIST OF PLATES
PLATE 1: FRACTURE-CONTROLLED MANGANESE OXIDE AND EARTHY HEMATITE IN SANDSTONE OF THE SKEENA GROUP...... 15
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Appendices
APPENDIX A – RAW AND FILTERED VLF-EM DATA
APPENDIX B – FRASER FILTERED DATA PROFILES
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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 Nazko property has only recently been the subject of exploration for precious metals; geochemical surveys outlined several anomalies that warranted follow-up work. In 2016, bedrock mapping, prospecting and sampling conducted over the southern half of the property identified a previously unrecognized window through the young volcanic cover. The older rocks are locally Fe and Mn-altered chert pebble conglomerate and coarse-grained sandstone of the Skeena Group; they are overlain to the west by weakly altered rhyolitic volcanics of the Ootsa Lake Group.
In the Fall of 2017, an auger drilling survey was completed on the claims peripheral to the two mining leases to determine thickness of tephra. The work identified several areas of multi- coloured or black tephra that were more than 1m thick and/or beyond the depth of the auger being used, with the thickest layers being located immediately north of the mine leases. The latter area, north of the North Flow (Zone III) area on the mine lease, has potential to add to the existing inventory of black tephra, and warrants a systematic test pitting program.
A Spring 2018 program consisted of a five-day VLF survey to assess an area of the claim block where bedrock mapping and sampling had previously identified anomalous geochemical values of zinc and arsenic in rocks near structural contacts between major lithologic units. The survey identified a number of linear features that are interpreted to coincide with faulted geological contacts between lithological units. Some of the linear features extend off of the grid suggesting that the grid should be expanded to provide a more complete VLF-EM signature for the area. It was recommended that CANLAVA expand the Spring 2018 VLF grid to the north, northeast and south in order to more fully evaluate this area of interest.
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The Fall 2018 program served to follow-up on the recommendations of the Spring 2018 program; it consisted of 5 days of VLF surveying to extend the earlier grid northward for 200m, southward for 500m and to fill in between the initial lines such that all lines are spaced at 100m intervals. The additional work was successful in outlining a number of linear anomalies with either north-trending, northwest-trending or northeast-trending orientations. The north and northeast trending linears are interpreted to be possible sub-surface conductors that may correlate with structural contacts between differing lithologies or faults that lie sub-parallel to the contacts. The north-trending linear is underlain by andesitic volcanics of the Ootsa Lake Group. The northeast liners and intersect one or more northwest trending linears in the southern half of the grid and are approximately orthogonal to each other. These faults and their intersections may identify important faults, cross-faults and/or well-developed joint sets along which hydrothermal fluids were guided, locally flooding the porous coarse-grained clastic sedimentary rocks of the Skeena Group with significant amounts of manganese oxide and hematite.
It is recommended that CANLAVA complete detailed prospecting of the linear features identified in the survey and conduct sampling if warranted. The budget for a 1-week program of prospecting and rock sampling is an estimated $12,000.00.
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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 ground-based geophysical survey conducted in December 2018 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 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.
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 seven mineral claims that cover 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 2019/AUG/20 200.00
329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00
552589 LAVA 7 Mineral Claim 2007/FEB/23 2019/JUL/11 155.86
552591 Mineral Claim 2007/FEB/23 2019/JUL/11 116.90
552592 LAVA 8 Mineral Claim 2007/FEB/23 2019/JUL/11 233.88
552593 LAVA 9 Mineral Claim 2007/FEB/23 2019/JUL/11 155.90
552594 LAVA 10 Mineral Claim 2007/FEB/23 2019/JUL/11 370.42 CANLAVA 1041719 Mineral Claim 2016/FEB/01 2019/JUL/11 156.02 SOUTHWEST 1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2019/JUL/11 292.45
Mineral Claim Total 1,481.43
All leases and claims are owned 100% by Canlava Mining Corp.
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.
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Title Number Claim Name Title Type Issue Date Good To Date Area (ha)
316265 Mineral Lease 1993/AUG/20 2019/AUG/20 200.00 CANLAVA Mining Corp - NAZKO PROJECT: Figure 2 - Mineral Tenure 329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00 552589 LAVA 7 Mineral Claim 2007/FEB/23 2019/JUL/11 155.86 Mineral Tenure Area Index Contour (100m interval)
552591 Mineral Claim 2007/FEB/23 2019/JUL/11 116.90 DRA Roads Intermediate Contour (20m interval) 552592 LAVA 8 Mineral Claim 2007/FEB/23 2019/JUL/11 233.88 Forest Service Road 552593 LAVA 9 Mineral Claim 2007/FEB/23 2019/JUL/11 155.90 Road Permit 552594 LAVA 10 Mineral Claim 2007/FEB/23 2019/JUL/11 370.42 Streams 1041719 CANLAVA SOUTHWEST Mineral Claim 2016/FEB/01 2019/JUL/11 156.02 Wetland 1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2019/JUL/11 292.45 Lakes All leases and claims are owned 100% by Canlava Mining Corporation 1,481.43
Coordinate System: NAD 1983 UTM Zone 10N Projection: Transverse Mercator Datum: North American 1983 Claim #: 1047066 & 1041719 False Easting: 500,000.0000 . False Northing: 0.0000 0 250 500 750 Central Meridian: -123.0000 Grid Size: 25m X 200m Scale Factor: 0.9996 Meters MAP DATE: 2018-12-20 Latitude Of Origin: 0.0000 Units: Meter Scale 1:20,000 CREATED BY: MasonP NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
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 (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).
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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CanLava Mining Legend I Coporation Existing Road NAZKO PROJECT Prince Rupert Prince Stream !( George Regional Geology !( Figure 3 Nazko Mineral Tenure Outline ^_ Property
Date: 2018-12-20 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: Revision #:
0 0.5 1 2 3
Kilometers Path: E:\18PG0049 Bob Lane\2400-GIS Nazko Property\2420-MXD\RegionalGeology_A.mxd NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
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
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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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Title Number Claim Name Title Type Issue Date Good To Date Area (ha)
316265 Mineral Lease 1993/AUG/20 2019/AUG/20 200.00 CANLAVA Mining Corp - NAZKO PROJECT: Figure 4 - Local Geology 329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00 552589 LAVA 7 Mineral Claim 2007/FEB/23 2019/JUL/11 155.86 Geological Contacts Road Permit 552591 Mineral Claim 2007/FEB/23 2019/JUL/11 116.90 Anahim Volcanics Index Contour (100m interval) 552592 LAVA 8 Mineral Claim 2007/FEB/23 2019/JUL/11 233.88 Skeena Group Intermediate Contour (20m interval) 552593 LAVA 9 Mineral Claim 2007/FEB/23 2019/JUL/11 155.90 Ootsa Lake Group Streams 552594 LAVA 10 Mineral Claim 2007/FEB/23 2019/JUL/11 370.42 Mineral Tenure Area Wetland 1041719 CANLAVA SOUTHWEST Mineral Claim 2016/FEB/01 2019/JUL/11 156.02
1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2019/JUL/11 292.45 DRA Roads Lakes
All leases and claims are owned 100% by Canlava Mining Corporation 1,481.43 Forest Service Road
Coordinate System: NAD 1983 UTM Zone 10N Projection: Transverse Mercator Datum: North American 1983 Claim #: 1047066 & 1041719 False Easting: 500,000.0000 . False Northing: 0.0000 0 250 500 750 Central Meridian: -123.0000 Grid Size: 25m X 200m Scale Factor: 0.9996 Meters MAP DATE: 2018-12-20 Latitude Of Origin: 0.0000 Units: Meter Scale 1:20,000 CREATED BY: MasonP NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
6 2018 EXPLORATION PROGRAM
A five-day VLF survey was completed from December 6-12, 2018, to assess an area of the claim block where bedrock mapping and sampling had previously identified anomalous geochemical values of zinc and arsenic in clastic rocks of the Skeena Group near structural contacts between major lithologic units. The intent of the Fall survey was to expand upon and fill in a wide-spaced VLF survey completed in the Spring; it consisted of 5 days VLF surveying to extend the earlier grid northward for 200m, southward for 500m and fill in between the initial lines such that all lines are spaced at 100m intervals.
It is thought that identified linear features might correlate to, or be indicative of, fractures or fracture systems that could be sources of the hydrothermal alteration seen locally in the field; they define areas for detailed follow-up prospecting and sampling.
6.1 INSTRUMENTATION
The survey was conducted with a Geonics VLF-EM16R instrument which is a VLF-EM receiver using submarine communication stations as a transmitter source. This instrument is designed to measure the electromagnetic component of the very low frequency field (VLF), which for this survey was transmitted at 24.8 kHz from Seattle (Jim Creek), Washington.
6.2 THEORY
In all electromagnetic prospecting, a transmitter induces an alternating magnetic field (called the primary field) by having a strong alternating current move through a coil of wire. This primary field travels through any medium and if a conductive mass such as a sulphide body is present, the primary field induces a secondary alternating current in the conductor, and this current in turn induces a secondary magnetic field. The receiver picks up the primary field and, if a conductor is present, the secondary field distorts the primary field. The fields are expressed as a vector, which has two components, the "in-phase" (or real) component and the "out-of-phase" (or quadrature) component. For the VLF-EM receiver, the tilt angle in degrees of the distorted electromagnetic field with a conductor is measured from that which it would have been if the field was not distorted with a conductor. Since the fields lose strength proportionally with the distance they travel, a distant conductor has less of an effect than a close conductor. Also, the lower the frequency of the primary field, the further the field can travel and therefore the greater the depth penetration.
The VLF-EM uses a frequency range from 13 to 30 kHz, whereas most EM instruments use frequencies ranging from a few hundred to a few thousand Hz. Because of its relatively high frequency, the VLF-EM can pick up bodies of a much lower conductivity and therefore is more susceptible to clay beds, electrolyte-filled fault or shear zones and porous horizons, graphite,
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carbonaceous sediments, lithological contacts as well as sulphide bodies of too low a conductivity for other EM methods to pick up. Consequently, the VLF-EM has additional uses in mapping structure and in picking up sulphide bodies of too low a conductivity for conventional EM methods and too small for induced polarization. (In places it can be used instead of IP). However, its susceptibility to lower conductive bodies result in a number of anomalies, many of them difficult to explain and thus, VLF-EM preferably should not be interpreted without a good geological knowledge of the property and/or other geophysical and geochemical surveys.
6.3 SURVEY PROCEDURE
A total of 681 readings were taken with station locations ascertained using a hand-held Garmin GPSMAP 64S hand-held device. Fifteen (15) survey lines were oriented east-west and spaced 100m apart; readings were taken at 25m intervals facing east. The resulting data was filtered and contoured using the Fraser (1969) method. A total of 16.25 line-km of VLF survey was completed in December, 2018.
The location of the survey is shown on Figure 5 and survey stations are shown on Figure 6. Tabulated raw data and filtered data are listed in Appendix A. The raw data and filtered data profiles are shown in Appendix B.
6.4 COMPILATION OF DATA
The field data was filtered using the methodology of Fraser (1969). Fraser-filtered data are presented in Figures 7 and 8.
6.5 DISCUSSION OF RESULTS
The VLF-EM survey was successful in outlining a number of linear anomalies with either north- trending, northwest-trending or northeast-trending orientations (Figures 7 and 8). The north and northeast trending linears are interpreted to be possible sub-surface conductors that may correlate with structural contacts between differing lithologies or faults that lie sub-parallel to the contacts. The north-trending linear is underlain by andesitic volcanics of the Ootsa Lake Group, and projects off of the grid to the north. The northeast liners and intersect one or more northwest trending linears in the southern half of the grid and are approximately orthogonal to each other. These faults and their intersections may identify important faults, cross-faults and/or well-developed joint sets along which hydrothermal fluids were guided, locally flooding the porous coarse-grained clastic sedimentary rocks of the Skeena Group with significant amounts of manganese oxide and hematite (Plate 1). These altered sediments are weakly anomalous in zinc and arsenic, but contain only background concentrations of gold or silver (Lane, 2017).
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Plate 1: Fracture-controlled manganese oxide and earthy hematite in sandstone of the Skeena Group.
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Title Number Claim Name Title Type Issue Date Good To Date Area (ha)
316265 Mineral Lease 1993/AUG/20 2019/AUG/20 200.00 CANLAVA Mining Corp - NAZKO PROJECT: Figure 5 - Grid Location Map 329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00 552589 LAVA 7 Mineral Claim 2007/FEB/23 2019/JUL/11 155.86 Geological Contacts Forest Service Road
552591 Mineral Claim 2007/FEB/23 2019/JUL/11 116.90 Anahim Volcanics Road Permit 552592 LAVA 8 Mineral Claim 2007/FEB/23 2019/JUL/11 233.88 Skeena Group DRA Roads 552593 LAVA 9 Mineral Claim 2007/FEB/23 2019/JUL/11 155.90 Ootsa Lake Group Streams 552594 LAVA 10 Mineral Claim 2007/FEB/23 2019/JUL/11 370.42 Mineral Tenure Areas Wetland 1041719 CANLAVA SOUTHWEST Mineral Claim 2016/FEB/01 2019/JUL/11 156.02 Grid Location Lakes 1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2019/JUL/11 292.45
All leases and claims are owned 100% by Canlava Mining Corporation 1,481.43 Index Contour (100m interval) Intermediate Contour (20m interval) Coordinate System: NAD 1983 UTM Zone 10N Projection: Transverse Mercator Datum: North American 1983 Claim #: 1047066 & 1041719 False Easting: 500,000.0000 . False Northing: 0.0000 0 250 500 750 Central Meridian: -123.0000 Grid Size: 25m X 200m Scale Factor: 0.9996 Meters MAP DATE: 2018-12-19 Latitude Of Origin: 0.0000 Units: Meter Scale 1:20,000 CREATED BY: MasonP 447500 448000 448500 449000 449500
552593 316265
1100 5863500 5863500
3+200
3+100
3+000 5863000 5863000
1200
2+800
1200
2+600 552594
1200 1047066 5862500 5862500 2+400 1200
1200
1200 2+200
2+000 5862000 5862000
1200
1+800
1300 1+600 5861500 5861500 1+400
1+300
1+200
1+100 1041719
1+000 5861000 5861000 0-025 1+250 1+225 1+200 1+175 1+150 1+125 1+100 1+075 1+050 1+025 1+000 0+975 0+950 0+925 0+900 0+875 9+850 0+825 0+899 0+775 0+750 0+725 0+700 0+675 0+650 0+625 0+600 0+575 0+550 0+525 0+500 0+475 0+450 0+425 0+400 0+375 0+350 0+325 0+300 0+275 0+250 0+225 0+200 0+175 0+150 0+125 0+100 0+075 0+050 0+025 0+000
1200
1200
1300
1300
1200 5860500 5860500 447500 448000 448500 449000 449500
Title Number Claim Name Title Type Issue Date Good To Date Area (ha)
316265 Mineral Lease 1993/AUG/20 2019/AUG/20 200.00 CANLAVA Mining Corp - NAZKO PROJECT: Figure 6 - VLF Grid Stations 329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00 Road Permit 552589 LAVA 7 Mineral Claim 2007/FEB/23 2019/JUL/11 155.86 Geological Contacts DRA Roads 552591 Mineral Claim 2007/FEB/23 2019/JUL/11 116.90 Anahim Volcanics 552592 LAVA 8 Mineral Claim 2007/FEB/23 2019/JUL/11 233.88 Index Contour (100m interval) Skeena Group 552593 LAVA 9 Mineral Claim 2007/FEB/23 2019/JUL/11 155.90 Intermediate Contour (20m interval) 552594 LAVA 10 Mineral Claim 2007/FEB/23 2019/JUL/11 370.42 Ootsa Lake Group Streams 1041719 CANLAVA SOUTHWEST Mineral Claim 2016/FEB/01 2019/JUL/11 156.02 Grid Axis Wetland 1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2019/JUL/11 292.45 Mineral Tenure Areas Lakes All leases and claims are owned 100% by Canlava Mining Corporation 1,481.43
Coordinate System: NAD 1983 UTM Zone 10N Projection: Transverse Mercator Datum: North American 1983 Claim #: 1047066 & 1041719 False Easting: 500,000.0000 . False Northing: 0.0000 0 250 Central Meridian: -123.0000 Grid Size: 25m X 200m Scale Factor: 0.9996 Meters MAP DATE: 2018-12-19 Latitude Of Origin: 0.0000 Units: Meter Scale 1:10,000 CREATED BY: MasonP 447500 448000 448500 449000 449500
552593 316265
1100 5863500 5863500 5863000 5863000
1200
1200
552594
1200 1047066 5862500 5862500
1200
1200
1200 5862000 5862000
1200
1300 5861500 5861500
1200
1041719 5861000 5861000
1200
1300
1300
1200 5860500 5860500 447500 448000 448500 449000 449500
Title Number Claim Name Title Type Issue Date Good To Date Area (ha)
316265 Mineral Lease 1993/AUG/20 2019/AUG/20 200.00 CANLAVA Mining Corp - NAZKO PROJECT: Figure 7 - VLF Fraser Filter Data 329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00 552589 LAVA 7 Mineral Claim 2007/FEB/23 2019/JUL/11 155.86 VLF_December Geological Contacts Mineral Tenure Areas 552591 Mineral Claim 2007/FEB/23 2019/JUL/11 116.90 Fraser_Filter_ Anahim Volcanics Index Contour (100m interval) 552592 LAVA 8 Mineral Claim 2007/FEB/23 2019/JUL/11 233.88 Skeena Group Intermediate Contour (20m interval) 552593 LAVA 9 Mineral Claim 2007/FEB/23 2019/JUL/11 155.90 -36 - -10 Ootsa Lake Group Streams 552594 LAVA 10 Mineral Claim 2007/FEB/23 2019/JUL/11 370.42 -9 - -3 Linear Features Wetland 1041719 CANLAVA SOUTHWEST Mineral Claim 2016/FEB/01 2019/JUL/11 156.02 -2 - 2 DRA Roads Lakes 1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2019/JUL/11 292.45 3 - 9 All leases and claims are owned 100% by Canlava Mining Corporation 1,481.43 Road Permit 10 - 27 Coordinate System: NAD 1983 UTM Zone 10N Projection: Transverse Mercator Datum: North American 1983 Claim #: 1047066 & 1041719 False Easting: 500,000.0000 . False Northing: 0.0000 0 250 Central Meridian: -123.0000 Grid Size: 25m X 200m Scale Factor: 0.9996 Meters MAP DATE: 2018-12-19 Latitude Of Origin: 0.0000 Units: Meter Scale 1:10,000 CREATED BY: MasonP 447500 448000 448500 449000 449500
552593 316265
1100 5863500 5863500
3 3+200
3+100
3+000 5863000 5863000
6 1200
2+800 1200 5
2+600 552594 4 1200 1047066 5862500 5862500
1200 2+400
1200 3
1200 2+200
1
2+000 5862000 5862000
2 1200
1+800
7
1300 1+600
8 5861500 2 5861500 1200 1+400
1+300
1+200
1+100 1041719 1 1+000 5861000 5861000
1200
1300
1300
1200 5860500 5860500 447500 448000 448500 449000 449500
Title Number Claim Name Title Type Issue Date Good To Date Area (ha)
316265 Mineral Lease 1993/AUG/20 2019/AUG/20 200.00 CANLAVA Mining Corp - NAZKO PROJECT: Figure 8 - VLF Fraser Filter Data 329933 Mineral Lease 1995/SEP/18 2019/SEP/18 200.00 552589 LAVA 7 Mineral Claim 2007/FEB/23 2019/JUL/11 155.86 VLF Fraser Filter Linear Features 552591 Mineral Claim 2007/FEB/23 2019/JUL/11 116.90 Mineral Tenure Areas -36 - -10 552592 LAVA 8 Mineral Claim 2007/FEB/23 2019/JUL/11 233.88 Public Roads 552593 LAVA 9 Mineral Claim 2007/FEB/23 2019/JUL/11 155.90 -9 - -3
552594 LAVA 10 Mineral Claim 2007/FEB/23 2019/JUL/11 370.42 -2 - 2 Forest Service Road 1041719 CANLAVA SOUTHWEST Mineral Claim 2016/FEB/01 2019/JUL/11 156.02 3 - 9 Road Permit 1047066 CANLAVA 2016 Mineral Claim 2016/OCT/04 2019/JUL/11 292.45 10 - 27 DRA Roads All leases and claims are owned 100% by Canlava Mining Corporation 1,481.43 Geological Contacts Wetland Coordinate System: NAD 1983 UTM Zone 10N Lakes Projection: Transverse Mercator AnahimClaim #: Volcanics 1047066 & 1041719 Datum: North American 1983 Streams False Easting: 500,000.0000 . Skeena Group False Northing: 0.0000 0 250 Index Contour (100m interval) Central Meridian: -123.0000 OotsaGrid Lake Size: Group 25m X 200m Scale Factor: 0.9996 Meters Intermediate Contour (20m interval) MAP DATE: 2018-12-19 Latitude Of Origin: 0.0000 Units: Meter Scale 1:10,000 CREATED BY: MasonP NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
7 INTERPRETATION AND CONCLUSIONS
The VLF-EM survey was successful in identifying a number of linear features that are interpreted to coincide with faulted geological contacts between lithological units. Furthermore, the northwest and northeast trending linears are believed to trace fractures (faults and prominent joint sets) that may have acted as conduits for hydrothermal fluids that locally introduced significant amounts of manganese oxide and hematite into the coarse-grained clastic sedimentary rocks of the Skeena Group. Previous sampling of these altered rocks returned only background values for gold and silver, and weakly anomalous concentrations of zinc and arsenic (Lane, 2017).
Some of the linear features extend off of the grid suggesting that the grid should be expanded to provide a more complete VLF-EM signature for the area. More detailed prospecting and geochemical sampling of the area may be warranted.
8 RECOMMENDATIONS
It is recommended that CANLAVA complete detailed prospecting of the linear features identified in the survey and conduct sampling if warranted. The budget for a 1-week program of prospecting and rock sampling is an estimated $12,000.00.
CANLAVA MINING CORP. PAGE 20
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
9 ITEMIZED COST STATEMENT – NAZKO PROPERTY
Nazko Fall 2018 Dates Worked Days/Hrs Rate Amount TOTALS
Wages & Salaries (Project Planning, Travel and Fieldwork)
Johnson, B Prospector Dec 6-11/18 5 400.00 2,000.00
Lane, B Project Geologist/Manager Dec 6-12/18 6.5 700.00 4,550.00
8 6,550.00 6,550.00
Travel (to/from site & on-site)
Plateau Minerals Corp. Kms - 4x4 pickup #1 Dec 6-11/18 1,641 0.7 1,148.70
Plateau Minerals Corp. Kms - 4x4 pickup #2 Dec 6-12/18 1,072 0.7 750.40
1,899.10 1,899.10
Ren tals, Fuel & Consumable Field Supplies
VLF-EM16 Rental (weekly rate) Dec 6-12/18 1 300.00 300.00
Fuel Dec 6-12/18 7 1 274.01
Consumable Field Supplies Dec 6-12/18 7 1 50.00
624.01 624.01
Accommodation and Meals
Meals Dec 6-12/18 13 469.89
Accom, Quesnel Dec 6-12/18 13 1331.33 1801.22 1801.22
Consulting - Report Writing & Data Collection/Processing
Consus Management GIS Mapping Services Dec, 2018 1 600.00 600.00 Data Processing & Report Plateau Minerals Corp. Dec, 2018 1.75 700.00 1225.00 Writing
1,825.00 1,825.00
Total Cost Nazko Fall 2018 12,699.33
CANLAVA MINING CORP. PAGE 21
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
10 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 22
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
Kuehn, C., Guest, B., Russell, J.K. and Benowitz, J.A. (2015): The Satah Mountain and Baldface Mountain volcanic fields: Pleistocene hot spot volcanism in the Anahim Volcanic Belt, west-central British Columbia, Canada: in Bulletin of Volcanology, v. 77, p. 1-27.
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.
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.
CANLAVA MINING CORP. PAGE 23
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
11 STATEMENTS OF QUALIFICATIONS
CANLAVA MINING CORP. PAGE 24
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
APPENDIX A
RAW AND FILTERED VLF-EM DATA
CANLAVA MINING CORP.
First Fraser LINE 1+300 Label X‐axis Slope In‐Phase Calculation Filter 449000 5861300 0+000 0 ‐2 ‐4 ‐4 448975 5861300 0+025 25 ‐4 ‐9 ‐13 9 448950 5861300 0+050 50 0 ‐4 ‐13 ‐3 448925 5861300 0+075 75 ‐2 ‐6 ‐10 ‐11 448900 5861300 0+100 100 ‐24 ‐2 ‐17 448875 5861300 0+125 125 ‐43 7 ‐4 448850 5861300 0+150 150 ‐3 ‐12 8 448825 5861300 0+175 175 ‐70 ‐13 448800 5861300 0+200 200 8 ‐1 ‐10 448775 5861300 0+225 225 13 0 ‐1 ‐3 448750 5861300 0+250 250 9 2 2 ‐5 448725 5861300 0+275 275 8 2 4 ‐6 448700 5861300 0+300 300 11 6 8 ‐4 448675 5861300 0+325 325 0 2 8 4 448650 5861300 0+350 350 ‐12 4 ‐3 448625 5861300 0+375 375 ‐19 11 ‐6 448600 5861300 0+400 400 ‐7 1 10 9 448575 5861300 0+425 425 ‐41 2 13 448550 5861300 0+450 450 1 ‐4 ‐36 448525 5861300 0+475 475 5 0 ‐4 ‐3 448500 5861300 0+500 500 ‐30 0 ‐3 448475 5861300 0+525 525 ‐9 ‐1 ‐1 ‐2 448450 5861300 0+550 550 ‐33 2 ‐4 448425 5861300 0+575 575 ‐12 0 3 4 448400 5861300 0+600 600 ‐17 ‐2 ‐29 448375 5861300 0+625 625 ‐15 ‐4 ‐60 448350 5861300 0+650 650 ‐82 ‐2 ‐8 448325 5861300 0+675 675 ‐20 2 ‐1 448300 5861300 0+700 700 ‐4 ‐1 ‐14 448275 5861300 0+725 725 ‐6 ‐1 ‐2 ‐2 448250 5861300 0+750 750 ‐14 2 1 ‐3 448225 5861300 0+775 775 ‐11 ‐11 1 448200 5861300 0+899 800 ‐81 0 0 448175 5861300 0+825 825 ‐11 0 1 6 448150 5861300 9+850 850 ‐21 ‐6 ‐615 448125 5861300 0+875 875 ‐16 ‐8 ‐14 7 448100 5861300 0+900 900 ‐13 ‐5 ‐13 ‐7 448075 5861300 0+925 925 ‐8 ‐2 ‐7 ‐9 448050 5861300 0+950 950 3 ‐2 ‐4 ‐1 448025 5861300 0+975 975 12 ‐4 ‐63 448000 5861300 1+000 1000 ‐10 ‐3 ‐7 ‐3 447975 5861300 1+025 1025 ‐50 ‐3 ‐3 447950 5861300 1+050 1050 ‐4 ‐4 ‐41 447925 5861300 1+075 1075 00 ‐4 ‐3 447900 5861300 1+100 1100 3 ‐1 ‐1 ‐4 447875 5861300 1+125 1125 17 1 0 ‐7 447850 5861300 1+150 1150 30 5 6 ‐9 447825 5861300 1+175 1175 24 4 9 ‐8 447800 5861300 1+200 1200 28 10 14 ‐6 447775 5861300 1+225 1225 26 5 15 10 447750 5861300 1+250 1250 16 ‐1 4 First Fraser LINE 1+100 Label X‐axis Slope In‐Phase Calculation Filter 447750 5861100 1+250 1250 0 ‐3 ‐3 447775 5861100 1+225 1225 7 ‐6 ‐97 447800 5861100 1+200 1200 4 ‐4 ‐10 ‐2 447825 5861100 1+175 1175 5 ‐3 ‐7 ‐5 447850 5861100 1+150 1150 8 ‐2 ‐5 ‐7 447875 5861100 1+125 1125 92 0 ‐9 447900 5861100 1+100 1100 13 2 4 ‐8 447925 5861100 1+075 1075 11 6 8 ‐4 447950 5861100 1+050 1050 72 88 447975 5861100 1+025 1025 ‐3 ‐2 015 448000 5861100 1+000 1000 ‐8 ‐5 ‐79 448025 5861100 0+975 975 ‐9 ‐4 ‐93 448050 5861100 0+950 950 ‐20 ‐6 ‐10 0 448075 5861100 0+925 925 ‐2 ‐3 ‐9 ‐3 448100 5861100 0+900 900 ‐14 ‐4 ‐7 ‐4 448125 5861100 0+875 875 ‐13 ‐1 ‐5 ‐6 448150 5861100 0+850 850 ‐16 0 ‐1 ‐3 448175 5861100 0+825 825 ‐18 ‐2 ‐23 448200 5861100 0+800 800 ‐14 ‐2 ‐40 448225 5861100 0+775 775 ‐13 0 ‐2 ‐6 448250 5861100 0+750 750 ‐10 2 2 ‐5 448275 5861100 0+725 725 ‐27 1 3 0 448300 5861100 0+700 700 ‐21 1 2 1 448325 5861100 0+675 675 1 1 2 ‐1 448350 5861100 0+650 650 0 2 3 ‐2 448375 5861100 0+625 625 3 2 4 ‐1 448400 5861100 0+600 600 7 2 4 3 448425 5861100 0+575 575 5 ‐11 6 448450 5861100 0+550 550 7 ‐1 ‐22 448475 5861100 0+525 525 0 0 ‐1 ‐1 448500 5861100 0+500 500 0 ‐1 ‐13 448525 5861100 0+475 475 ‐9 ‐3 ‐44 448550 5861100 0+450 450 7 ‐2 ‐51 448575 5861100 0+425 425 8 ‐3 ‐5 ‐3 448600 5861100 0+400 400 11 1 ‐2 ‐7 448625 5861100 0+375 375 3 1 2 ‐5 448650 5861100 0+350 350 8 2 3 ‐1 448675 5861100 0+325 325 5 1 3 1 448700 5861100 0+300 300 6 1 2 3 448725 5861100 0+275 275 ‐2 ‐10 5 448750 5861100 0+250 250 1 ‐2 ‐32 448775 5861100 0+225 225 ‐30 ‐2 ‐2 448800 5861100 0+200 200 ‐1 ‐1 ‐10 448825 5861100 0+175 175 ‐4 ‐1 ‐20 448850 5861100 0+150 150 ‐20 ‐10 448875 5861100 0+125 125 0 ‐2 ‐23 448900 5861100 0+100 100 ‐5 ‐2 ‐44 448925 5861100 0+075 75 ‐2 ‐4 ‐60 448950 5861100 0+050 50 ‐20 ‐4 ‐8 448975 5861100 0+025 25 1 2 2 ‐5 449000 5861100 0+000 0 0 ‐11 First Fraser LINE 1+000 Label X‐axis Slope In‐Phase Calculation Filter 449000 5861000 0+000 0 ‐15 ‐2 ‐2 448975 5861000 0+025 25 12 ‐2 ‐41 448950 5861000 0+050 50 ‐4 ‐1 ‐3 ‐1 448925 5861000 0+075 75 ‐3 ‐2 ‐31 448900 5861000 0+100 100 0 ‐2 ‐4 ‐1 448875 5861000 0+125 125 2 0 ‐2 ‐3 448850 5861000 0+150 150 4 ‐1 ‐1 ‐2 448825 5861000 0+175 175 2 1 0 ‐2 448800 5861000 0+200 200 ‐20 1 4 448775 5861000 0+225 225 ‐7 ‐4 ‐46 448750 5861000 0+250 250 ‐11 ‐1 ‐50 448725 5861000 0+275 275 ‐2 ‐3 ‐40 448700 5861000 0+300 300 1 ‐2 ‐5 ‐4 448675 5861000 0+325 325 10 2 0 ‐10 448650 5861000 0+350 350 24 3 5 ‐4 448625 5861000 0+375 375 21 1 4 5 448600 5861000 0+400 400 18 ‐10 1 448575 5861000 0+425 425 12 4 3 ‐5 448550 5861000 0+450 450 17 1 5 0 448525 5861000 0+475 475 8 2 3 5 448500 5861000 0+500 500 13 ‐20 9 448475 5861000 0+525 525 ‐4 ‐4 ‐65 448450 5861000 0+550 550 2 ‐1 ‐5 ‐3 448425 5861000 0+575 575 5 ‐2 ‐3 ‐2 448400 5861000 0+600 600 6 ‐1 ‐3 ‐3 448375 5861000 0+625 625 14 1 0 ‐2 448350 5861000 0+650 650 13 ‐2 ‐12 448325 5861000 0+675 675 5 0 ‐2 ‐1 448300 5861000 0+700 700 0 0 0 ‐3 448275 5861000 0+725 725 ‐11 1 7 448250 5861000 0+750 750 ‐13 ‐8 ‐711 448225 5861000 0+775 775 ‐16 ‐2 ‐10 ‐1 448200 5861000 0+899 800 ‐11 ‐4 ‐6 ‐3 448175 5861000 0+825 825 ‐12 ‐3 ‐71 448150 5861000 9+850 850 ‐15 ‐4 ‐7 ‐1 448125 5861000 0+875 875 ‐6 ‐2 ‐61 448100 5861000 0+900 900 ‐9 ‐6 ‐85 448075 5861000 0+925 925 ‐3 ‐5 ‐11 ‐2 448050 5861000 0+950 950 ‐1 ‐1 ‐6 ‐8 448025 5861000 0+975 975 ‐5 ‐2 ‐3 ‐1 448000 5861000 1+000 1000 ‐4 ‐3 ‐54 447975 5861000 1+025 1025 ‐7 ‐4 ‐76 447950 5861000 1+050 1050 ‐8 ‐7 ‐11 10 447925 5861000 1+075 1075 ‐5 ‐10 ‐17 5 447900 5861000 1+100 1100 0 ‐6 ‐16 ‐8 447875 5861000 1+125 1125 ‐3 ‐3 ‐9 ‐13 447850 5861000 1+150 1150 60 ‐3 ‐9 447825 5861000 1+175 1175 60 03 447800 5861000 1+200 1200 ‐5 ‐6 ‐69 447775 5861000 1+225 1225 ‐5 ‐3 ‐90 447750 5861000 1+250 1250 ‐1 ‐3 ‐6 First Fraser LINE 1+200 Label X‐axis Slope In‐Phase Calculation Filter 449000 5861200 0+000 0 0 ‐1 ‐1 448975 5861200 0+025 25 1 0 ‐12 448950 5861200 0+050 50 ‐6 ‐3 ‐34 448925 5861200 0+075 75 ‐10 ‐2 ‐5 ‐1 448900 5861200 0+100 100 ‐10 0 ‐2 ‐3 448875 5861200 0+125 125 ‐12 ‐2 ‐25 448850 5861200 0+150 150 ‐7 ‐5 ‐77 448825 5861200 0+175 175 2 ‐4 ‐95 448800 5861200 0+200 200 3 ‐8 ‐12 7 448775 5861200 0+225 225 4 ‐8 ‐16 ‐4 448750 5861200 0+250 250 14 0 ‐8 ‐18 448725 5861200 0+275 275 17 2 2 ‐12 448700 5861200 0+300 300 8 2 4 ‐1 448675 5861200 0+325 325 5 1 3 5 448650 5861200 0+350 350 15 ‐2 ‐16 448625 5861200 0+375 375 3 ‐1 ‐32 448600 5861200 0+400 400 ‐2 ‐2 ‐30 448575 5861200 0+425 425 ‐11 ‐1 ‐3 ‐4 448550 5861200 0+450 450 ‐72 1 ‐8 448525 5861200 0+475 475 2 3 5 ‐1 448500 5861200 0+500 500 2 ‐1210 448475 5861200 0+525 525 1 ‐4 ‐512 448450 5861200 0+550 550 2 ‐6 ‐10 7 448425 5861200 0+575 575 4 ‐6 ‐12 0 448400 5861200 0+600 600 6 ‐4 ‐10 ‐2 448375 5861200 0+625 625 ‐7 ‐6 ‐10 ‐1 448350 5861200 0+650 650 ‐8 ‐3 ‐9 ‐10 448325 5861200 0+675 675 ‐10 3 0 ‐17 448300 5861200 0+700 700 ‐65 8 ‐7 448275 5861200 0+725 725 ‐52 7 8 448250 5861200 0+750 750 ‐10 ‐2010 448225 5861200 0+775 775 ‐18 ‐1 ‐34 448200 5861200 0+899 800 ‐13 ‐3 ‐4 ‐1 448175 5861200 0+825 825 ‐91 ‐2 ‐3 448150 5861200 9+850 850 ‐12 ‐2 ‐11 448125 5861200 0+875 875 ‐21 ‐1 ‐35 448100 5861200 0+900 900 ‐24 ‐5 ‐67 448075 5861200 0+925 925 ‐15 ‐5 ‐10 2 448050 5861200 0+950 950 ‐8 ‐3 ‐8 ‐7 448025 5861200 0+975 975 ‐70 ‐3 ‐10 448000 5861200 1+000 1000 15 2 2 ‐8 447975 5861200 1+025 1025 22 3 5 ‐1 447950 5861200 1+050 1050 00 33 447925 5861200 1+075 1075 52 22 447900 5861200 1+100 1100 12 ‐1 16 447875 5861200 1+125 1125 13 ‐3 ‐46 447850 5861200 1+150 1150 17 ‐2 ‐5 ‐2 447825 5861200 1+175 1175 21 0 ‐2 ‐4 447800 5861200 1+200 1200 20 ‐1 ‐1 ‐1 447775 5861200 1+225 1225 11 0 ‐1 ‐2 447750 5861200 1+250 1250 16 1 1 First Fraser LINE 1+400 Label X‐axis Slope In‐Phase Calculation Filter 447750 5861400 1+250 1250 10 0 447775 5861400 1+225 1225 12 0 0 ‐4 447800 5861400 1+200 1200 18 4 4 ‐6 447825 5861400 1+175 1175 82 63 447850 5861400 1+150 1150 15 ‐1 111 447875 5861400 1+125 1125 14 ‐4 ‐56 447900 5861400 1+100 1000 29 ‐1 ‐54 447925 5861400 1+075 1075 ‐16 ‐8 ‐99 447950 5861400 1+050 1050 ‐15 ‐6 ‐14 2 447975 5861400 1+025 1025 ‐13 ‐5 ‐11 ‐3 448000 5861400 1+000 1000 ‐11 ‐6 ‐11 ‐1 448025 5861400 0+975 975 ‐12 ‐4 ‐10 ‐2 448050 5861400 0+950 950 ‐23 ‐5 ‐92 448075 5861400 0+925 925 ‐4 ‐7 ‐12 9 448100 5861400 0+900 900 ‐38 ‐11 ‐18 8 448125 5861400 0+875 875 1 ‐9 ‐20 ‐2 448150 5861400 0+850 850 ‐10 ‐7 ‐16 ‐7 448175 5861400 0+825 825 ‐12 ‐6 ‐13 ‐7 448200 5861400 0+800 800 ‐19 ‐3 ‐9 ‐9 448225 5861400 0+775 775 ‐9 ‐1 ‐4 ‐6 448250 5861400 0+750 750 ‐8 ‐2 ‐31 448275 5861400 0+725 725 ‐17 ‐3 ‐51 448300 5861400 0+700 700 ‐15 ‐1 ‐4 ‐7 448325 5861400 0+675 675 ‐43 2 ‐10 448350 5861400 0+650 650 0 3 6 ‐4 448375 5861400 0+625 625 ‐43 6 1 448400 5861400 0+600 600 ‐19 2 5 4 448425 5861400 0+575 575 ‐12 0 2 5 448450 5861400 0+550 550 ‐30 0 1 448475 5861400 0+525 525 0 1 1 4 448500 5861400 0+500 500 ‐9 ‐5 ‐44 448525 5861400 0+475 475 ‐12 2 ‐3 ‐9 448550 5861400 0+450 450 ‐13 5 ‐7 448575 5861400 0+425 425 2 1 4 2 448600 5861400 0+400 400 1 2 3 1 448625 5861400 0+375 375 ‐41 3 1 448650 5861400 0+350 350 ‐21 2 2 448675 5861400 0+325 325 0 0 1 ‐1 448700 5861400 0+300 300 ‐33 3 ‐8 448725 5861400 0+275 275 5 6 9 ‐9 448750 5861400 0+250 250 1 6 12 ‐1 448775 5861400 0+225 225 1 4 10 11 448800 5861400 0+200 200 4 ‐3120 448825 5861400 0+175 175 1 ‐7 ‐10 12 448850 5861400 0+150 150 2 ‐4 ‐11 2 448875 5861400 0+125 125 0 ‐8 ‐12 3 448900 5861400 0+100 100 4 ‐6 ‐14 ‐6 448925 5861400 0+075 75 ‐40 ‐6 ‐8 448950 5861400 0+050 50 ‐5 ‐6 ‐67 448975 5861400 0+025 25 1 ‐7 ‐13 6 449000 5861400 0+000 0 1 ‐5 ‐12 First Fraser LINE 1+600 Label X‐axis Slope In‐Phase Calculation Filter 449000 5861600 0+000 0 ‐3 ‐3 ‐3 448975 5861600 0+025 25 ‐5 ‐1 ‐4 ‐6 448950 5861600 0+050 50 ‐44 3 ‐12 448925 5861600 0+075 75 ‐24 8 ‐3 448900 5861600 0+100 100 0 2 6 6 448875 5861600 0+125 125 ‐40 2 8 448850 5861600 0+150 150 ‐5 ‐2 ‐26 448825 5861600 0+175 175 ‐1 ‐2 ‐42 448800 5861600 0+200 200 8 ‐2 ‐41 448775 5861600 0+225 225 3 ‐3 ‐51 448750 5861600 0+250 250 ‐7 ‐2 ‐52 448725 5861600 0+275 275 ‐8 ‐5 ‐78 448700 5861600 0+300 300 2 ‐8 ‐13 4 448675 5861600 0+325 325 1 ‐3 ‐11 ‐16 448650 5861600 0+350 350 ‐86 3 ‐14 448625 5861600 0+375 375 ‐18 ‐33 0 448600 5861600 0+400 400 ‐46 3 ‐1 448575 5861600 0+425 425 ‐4 ‐24 3 448550 5861600 0+450 450 ‐72 0 0 448525 5861600 0+475 475 2 2 4 ‐3 448500 5861600 0+500 500 3 1 3 3 448475 5861600 0+525 525 0 0 1 5 448450 5861600 0+550 550 ‐10 ‐2 ‐21 448425 5861600 0+575 575 ‐32 0 ‐8 448400 5861600 0+600 600 3 4 6 ‐5 448375 5861600 0+625 625 ‐10 1 5 5 448350 5861600 0+650 650 ‐20 1 8 448325 5861600 0+675 675 ‐3 ‐3 ‐37 448300 5861600 0+700 700 ‐5 ‐3 ‐62 448275 5861600 0+725 725 ‐8 ‐2 ‐5 ‐2 448250 5861600 0+750 750 ‐10 ‐2 ‐4 ‐1 448225 5861600 0+775 775 ‐13 ‐2 ‐4 ‐1 448200 5861600 0+899 800 ‐14 ‐1 ‐3 ‐5 448175 5861600 0+825 825 ‐32 1 ‐3 448150 5861600 9+850 850 ‐15 ‐20 5 448125 5861600 0+875 875 ‐7 ‐2 ‐41 448100 5861600 0+900 900 ‐81 ‐1 ‐5 448075 5861600 0+925 925 ‐90 1 2 448050 5861600 0+950 950 ‐14 ‐3 ‐37 448025 5861600 0+975 975 ‐13 ‐3 ‐6 ‐2 448000 5861600 1+000 1000 ‐82 ‐1 First Fraser LINE 1+800 Label X‐axis Slope In‐Phase Calculation Filter 449000 5861800 0+000 0 ‐1 ‐4 ‐4 448975 5861800 0+025 25 ‐2 ‐3 ‐75 448950 5861800 0+050 50 ‐4 ‐6 ‐99 448925 5861800 0+075 75 ‐2 ‐10 ‐16 12 448900 5861800 0+100 100 ‐12 ‐11 ‐21 ‐1 448875 5861800 0+125 125 ‐8 ‐4 ‐15 ‐12 448850 5861800 0+150 150 ‐9 ‐5 ‐9 ‐7 448825 5861800 0+175 175 2 ‐3 ‐8 ‐9 448800 5861800 0+200 200 ‐330‐14 448775 5861800 0+225 225 ‐236 ‐7 448750 5861800 0+250 250 ‐6473 448725 5861800 0+275 275 3 ‐13 9 448700 5861800 0+300 300 6 ‐1 ‐27 448675 5861800 0+325 325 9 ‐3 ‐4 ‐5 448650 5861800 0+350 350 2 6 3 ‐14 448625 5861800 0+375 375 ‐1410‐5 448600 5861800 0+400 400 ‐5480 448575 5861800 0+425 425 ‐3610‐3 448550 5861800 0+450 450 2 5 11 4 448525 5861800 0+475 475 ‐13 1 6 10 448500 5861800 0+500 500 ‐2018 448475 5861800 0+525 525 ‐3 ‐2 ‐29 448450 5861800 0+550 550 0 ‐6 ‐88 448425 5861800 0+575 575 ‐10 ‐4 ‐10 1 448400 5861800 0+600 600 ‐3 ‐5 ‐9 ‐4 448375 5861800 0+625 625 ‐7 ‐1 ‐6 ‐4 448350 5861800 0+650 650 ‐3 ‐4 ‐5 ‐7 448325 5861800 0+675 675 ‐151‐17 448300 5861800 0+700 700 ‐3 7 12 0 448275 5861800 0+725 725 ‐5 ‐61 21 448250 5861800 0+750 750 ‐8 ‐3 ‐9 ‐2 448225 5861800 0+775 775 ‐163‐15 448200 5861800 0+899 800 3 0 6 ‐1 448175 5861800 0+825 825 3 4 4 ‐3 448150 5861800 9+850 850 ‐4590 448125 5861800 0+875 875 ‐7 ‐14 12 448100 5861800 0+900 900 ‐13 ‐2 ‐34 448075 5861800 0+925 925 ‐11 2 0 ‐9 448050 5861800 0+950 950 13 4 6 ‐2 448025 5861800 0+975 975 0 ‐22 9 448000 5861800 1+000 1000 ‐2 ‐1 ‐34 447975 5861800 1+025 1025 ‐8 ‐1 ‐2 First Fraser LINE 2+000 Label X‐axis Slope In‐Phase Calculation Filter 447975 5862000 1+025 1025 10 ‐1 ‐1 448000 5862000 1+000 1000 ‐40‐1 ‐1 448025 5862000 0+975 975 ‐11 0 0 1 448050 5862000 0+950 950 13 ‐2 ‐2 ‐3 448075 5862000 0+925 925 3 5 3 ‐11 448100 5862000 0+900 900 ‐149 ‐3 448125 5862000 0+875 875 ‐5269 448150 5862000 0+850 850 ‐11 ‐20 10 448175 5862000 0+825 825 ‐12 ‐2 ‐42 448200 5862000 0+800 800 10 0 ‐2 ‐2 448225 5862000 0+775 775 ‐6 ‐2 ‐22 448250 5862000 0+750 750 0 ‐2 ‐44 448275 5862000 0+725 725 0 ‐4 ‐62 448300 5862000 0+700 700 ‐8 ‐2 ‐61 448325 5862000 0+675 675 ‐11 ‐5 ‐71 448350 5862000 0+650 650 ‐3 ‐2 ‐7 ‐3 448375 5862000 0+625 625 0 ‐2 ‐4 ‐4 448400 5862000 0+600 600 ‐1 ‐1 ‐3 ‐2 448425 5862000 0+575 575 ‐2 ‐1 ‐2 ‐2 448450 5862000 0+550 550 ‐12 0 ‐1 ‐2 448475 5862000 0+525 525 ‐5002 448500 5862000 0+500 500 ‐4 ‐3 ‐32 448525 5862000 0+475 475 ‐31‐2 ‐6 448550 5862000 0+450 450 6 2 3 ‐8 448575 5862000 0+425 425 4 4 6 ‐6 448600 5862000 0+400 400 6 5 9 ‐7 448625 5862000 0+375 375 12 8 13 ‐1 448650 5862000 0+350 350 10 2 10 5 448675 5862000 0+325 325 3 6 8 7 448700 5862000 0+300 300 ‐11 ‐33 10 448725 5862000 0+275 275 ‐41‐22 448750 5862000 0+250 250 0 0 1 0 448775 5862000 0+225 225 8 ‐2 ‐23 448800 5862000 0+200 200 4 0 ‐210 448825 5862000 0+175 175 ‐4 ‐12 ‐12 9 448850 5862000 0+150 150 ‐71‐11 ‐8 448875 5862000 0+125 125 ‐15 ‐5 ‐4 ‐2 448900 5862000 0+100 100 ‐14 ‐4 ‐93 448925 5862000 0+075 75 ‐7 ‐3 ‐7 ‐5 448950 5862000 0+050 50 ‐6 ‐1 ‐4 ‐3 448975 5862000 0+025 25 ‐6 ‐3 ‐40 449000 5862000 0+000 0 ‐5 ‐1 ‐4 First Fraser LINE 2+200 Label X‐axis Slope In‐Phase Calculation Filter 449000 5862200 0+000 0 ‐5 ‐6 ‐7 448975 5862200 0+025 25 ‐9 ‐5 ‐11 2 448950 5862200 0+050 50 ‐12 ‐4 ‐90 448925 5862200 0+075 75 ‐14 ‐7 ‐11 4 448900 5862200 0+100 100 ‐16 ‐6 ‐13 ‐3 448875 5862200 0+125 125 ‐6 ‐2 ‐8 ‐11 448850 5862200 0+150 150 ‐30‐2 ‐9 448825 5862200 0+175 175 1 1 1 ‐2 448800 5862200 0+200 200 16 ‐10 10 448775 5862200 0+225 225 ‐9 ‐8 ‐96 448750 5862200 0+250 250 ‐52‐6 ‐1 448725 5862200 0+275 275 ‐11 ‐10 ‐88 448700 5862200 0+300 300 2 ‐4 ‐14 ‐3 448675 5862200 0+325 325 3 ‐1 ‐5 ‐18 448650 5862200 0+350 350 ‐254 ‐4 448625 5862200 0+375 375 ‐6 ‐6 ‐19 448600 5862200 0+400 400 ‐71‐52 448575 5862200 0+425 425 3 ‐4 ‐3 ‐7 448550 5862200 0+450 450 5 6 2 ‐11 448525 5862200 0+475 475 4 2 8 ‐6 448500 5862200 0+500 500 2 6 8 0 448475 5862200 0+525 525 0 2 8 3 448450 5862200 0+550 550 2 3 5 1 448425 5862200 0+575 575 ‐447 ‐3 448400 5862200 0+600 600 0 4 8 5 448375 5862200 0+625 625 7 ‐22 10 448350 5862200 0+650 650 9 0 ‐22 448325 5862200 0+675 675 7 0 0 ‐6 448300 5862200 0+700 700 ‐244 ‐7 448275 5862200 0+725 725 10 3 7 1 448250 5862200 0+750 750 6 0 3 5 448225 5862200 0+775 775 0 2 2 1 448200 5862200 0+899 800 ‐3023 448175 5862200 0+825 825 ‐6 ‐1 ‐16 448150 5862200 9+850 850 ‐4 ‐3 ‐43 448125 5862200 0+875 875 4 ‐1 ‐4 ‐1 448100 5862200 0+900 900 6 ‐2 ‐30 448075 5862200 0+925 925 0 ‐2 ‐43 448050 5862200 0+950 950 ‐4 ‐4 ‐64 448025 5862200 0+975 975 ‐5 ‐4 ‐80 448000 5862200 1+000 1000 4 ‐2 ‐6 ‐3 447975 5862200 1+025 1025 11 ‐3 ‐50 First Fraser LINE 2+400 Label X‐axis Slope In‐Phase Calculation Filter 447975 5862400 1+025 1025 ‐3 ‐3 ‐6 448000 5862400 1+000 1000 3 2 ‐1 ‐10 448025 5862400 0+975 975 3 2 4 ‐6 448050 5862400 0+950 950 7 3 5 ‐2 448075 5862400 0+925 925 11 3 6 4 448100 5862400 0+900 900 13 ‐21 7 448125 5862400 0+875 875 4 1 ‐1 ‐2 448150 5862400 0+850 850 4 2 3 ‐2 448175 5862400 0+825 825 7 ‐11 4 448200 5862400 0+800 800 3 0 ‐14 448225 5862400 0+775 775 5 ‐3 ‐33 448250 5862400 0+750 750 10 ‐1 ‐40 448275 5862400 0+725 725 3 ‐2 ‐31 448300 5862400 0+700 700 6 ‐3 ‐5 ‐1 448325 5862400 0+675 675 9 1 ‐2 ‐8 448350 5862400 0+650 650 4 2 3 ‐10 448375 5862400 0+625 625 8 6 8 ‐12 448400 5862400 0+600 600 18 9 15 ‐7 448425 5862400 0+575 575 ‐3 6 15 2 448450 5862400 0+550 550 6 7 13 5 448475 5862400 0+525 525 4 3 10 12 448500 5862400 0+500 500 ‐1 ‐21 15 448525 5862400 0+475 475 3 ‐3 ‐52 448550 5862400 0+450 450 ‐82‐1 ‐11 448575 5862400 0+425 425 ‐446 ‐4 448600 5862400 0+400 400 ‐6 ‐13 9 448625 5862400 0+375 375 ‐1 ‐2 ‐39 448650 5862400 0+350 350 5 ‐4 ‐65 448675 5862400 0+325 325 ‐3 ‐4 ‐82 448700 5862400 0+300 300 ‐12 ‐4 ‐8 ‐7 448725 5862400 0+275 275 ‐14 3 ‐1 ‐13 448750 5862400 0+250 250 ‐225 ‐6 448775 5862400 0+225 225 0 3 5 6 448800 5862400 0+200 200 ‐11 ‐4 ‐117 448825 5862400 0+175 175 ‐15 ‐8 ‐12 20 448850 5862400 0+150 150 ‐16 ‐13 ‐21 11 448875 5862400 0+125 125 ‐32 ‐10 ‐23 ‐7 448900 5862400 0+100 100 ‐5 ‐4 ‐14 ‐23 448925 5862400 0+075 75 ‐140‐20 448950 5862400 0+050 50 ‐20 2 6 2 448975 5862400 0+025 25 ‐4 ‐4 ‐28 449000 5862400 0+000 0 ‐52‐2 ‐11 449025 5862400 0‐025 ‐25 ‐579 First Fraser LINE 3+000 Label X‐axis Slope In‐Phase Calculation Filter 449025 5863000 0‐025 ‐25 ‐15 1 8 449000 5863000 0+000 0 ‐16 10 11 ‐8 448975 5863000 0+025 25 ‐13 6 16 ‐1 448950 5863000 0+050 50 ‐9 6 12 5 448925 5863000 0+075 75 ‐1 5 11 0 448900 5863000 0+100 100 ‐12 7 12 3 448875 5863000 0+125 125 ‐71813 448850 5863000 0+150 150 ‐27 ‐2 ‐114 448825 5863000 0+175 175 ‐18 ‐4 ‐66 448800 5863000 0+200 200 ‐10 ‐3 ‐7 ‐3 448775 5863000 0+225 225 ‐70‐3 ‐5 448750 5863000 0+250 250 ‐4 ‐2 ‐21 448725 5863000 0+275 275 8 ‐2 ‐48 448700 5863000 0+300 300 6 ‐8 ‐10 4 448675 5863000 0+325 325 ‐22 0 ‐8 ‐15 448650 5863000 0+350 350 ‐17 5 5 ‐18 448625 5863000 0+375 375 4 5 10 2 448600 5863000 0+400 400 ‐2 ‐23 16 448575 5863000 0+425 425 ‐13 ‐4 ‐613 448550 5863000 0+450 450 ‐16 ‐6 ‐10 4 448525 5863000 0+475 475 ‐9 ‐4 ‐10 1 448500 5863000 0+500 500 ‐2 ‐7 ‐11 0 448475 5863000 0+525 525 ‐16 ‐3 ‐10 ‐8 448450 5863000 0+550 550 ‐60‐3 ‐12 448425 5863000 0+575 575 14 2 2 ‐5 448400 5863000 0+600 600 12 0 2 4 448375 5863000 0+625 625 10 ‐2 ‐25 448350 5863000 0+650 650 13 ‐1 ‐3 ‐1 448325 5863000 0+675 675 23 0 ‐1 ‐6 448300 5863000 0+700 700 26 3 3 ‐3 448275 5863000 0+725 725 5 ‐12 6 448250 5863000 0+750 750 24 ‐2 ‐35 448225 5863000 0+775 775 16 ‐1 ‐36 448200 5863000 0+899 800 7 ‐8 ‐99 448175 5863000 0+825 825 ‐3 ‐4 ‐12 ‐5 448150 5863000 9+850 850 13 0 ‐4 ‐12 448125 5863000 0+875 875 24 0 0 0 448100 5863000 0+900 900 9 ‐4 ‐49 448075 5863000 0+925 925 4 ‐5 ‐91 448050 5863000 0+950 950 14 0 ‐5 ‐15 448025 5863000 0+975 975 29 6 6 ‐14 448000 5863000 1+000 1000 31 3 9 ‐1 447975 5863000 1+025 1025 22 4 7 First Fraser LINE 2+800 Label X‐axis Slope In‐Phase Calculation Filter 447975 5862800 1+025 1025 28 6 10 448000 5862800 1+000 1000 16 8 14 ‐5 448025 5862800 0+975 975 17 7 15 4 448050 5862800 0+950 950 18 3 10 15 448075 5862800 0+925 925 3 ‐30 17 448100 5862800 0+900 900 28 ‐4 ‐74 448125 5862800 0+875 875 31 0 ‐4 ‐8 448150 5862800 0+850 850 28 1 1 ‐6 448175 5862800 0+825 825 16 1 2 2 448200 5862800 0+800 800 12 ‐2 ‐16 448225 5862800 0+775 775 18 ‐2 ‐4 ‐1 448250 5862800 0+750 750 23 2 0 ‐11 448275 5862800 0+725 725 25 5 7 ‐7 448300 5862800 0+700 700 ‐11 2 7 9 448325 5862800 0+675 675 5 ‐4 ‐221 448350 5862800 0+650 650 8 ‐10 ‐14 16 448375 5862800 0+625 625 11 ‐8 ‐18 ‐7 448400 5862800 0+600 600 20 1 ‐7 ‐20 448425 5862800 0+575 575 5 1 2 ‐8 448450 5862800 0+550 550 1 0 1 3 448475 5862800 0+525 525 ‐12 ‐1 ‐14 448500 5862800 0+500 500 ‐16 ‐2 ‐35 448525 5862800 0+475 475 ‐23 ‐4 ‐62 448550 5862800 0+450 450 ‐2 ‐1 ‐5 ‐5 448575 5862800 0+425 425 2 0 ‐1 ‐3 448600 5862800 0+400 400 ‐37 ‐2 ‐23 448625 5862800 0+375 375 ‐16 ‐2 ‐47 448650 5862800 0+350 350 1 ‐7 ‐9 ‐6 448675 5862800 0+325 325 6 9 2 ‐16 448700 5862800 0+300 300 ‐36 ‐27 15 448725 5862800 0+275 275 ‐14 ‐11 ‐13 25 448750 5862800 0+250 250 ‐6 ‐7 ‐18 ‐1 448775 5862800 0+225 225 ‐6 ‐5 ‐12 ‐9 448800 5862800 0+200 200 ‐2 ‐4 ‐9 ‐4 448825 5862800 0+175 175 ‐18 ‐4 ‐8 ‐2 448850 5862800 0+150 150 ‐15 ‐3 ‐7 ‐9 448875 5862800 0+125 125 ‐17 4 1 ‐14 448900 5862800 0+100 100 ‐23 3 7 ‐1 448925 5862800 0+075 75 ‐13 ‐12 10 448950 5862800 0+050 50 ‐14 ‐2 ‐311 448975 5862800 0+025 25 ‐22 ‐7 ‐98 449000 5862800 0+000 0 3 ‐4 ‐11 ‐7 449025 5862800 0‐025 ‐25 ‐72‐2 First Fraser LINE 2+600 Label X‐axis Slope In‐Phase Calculation Filter 449025 5862600 0‐025 ‐25 ‐4 ‐5 ‐3 449000 5862600 0+000 0 ‐12 ‐4 ‐90 448975 5862600 0+025 25 ‐13 1 ‐3 ‐14 448950 5862600 0+050 50 9 4 5 ‐11 448925 5862600 0+075 75 ‐2484 448900 5862600 0+100 100 ‐17 ‐31 27 448875 5862600 0+125 125 ‐22 ‐16 ‐19 28 448850 5862600 0+150 150 ‐21 ‐11 ‐27 ‐3 448825 5862600 0+175 175 ‐18 ‐5 ‐16 ‐20 448800 5862600 0+200 200 ‐8 ‐2 ‐7 ‐7 448775 5862600 0+225 225 ‐8 ‐7 ‐93 448750 5862600 0+250 250 ‐6 ‐3 ‐10 ‐9 448725 5862600 0+275 275 6 3 0 ‐18 448700 5862600 0+300 300 3 5 8 ‐3 448675 5862600 0+325 325 ‐13 ‐23 15 448650 5862600 0+350 350 ‐30 ‐5 ‐75 448625 5862600 0+375 375 ‐21 3 ‐2 ‐10 448600 5862600 0+400 400 14 0 3 3 448575 5862600 0+425 425 5 ‐5 ‐59 448550 5862600 0+450 450 ‐7 ‐1 ‐6 ‐4 448525 5862600 0+475 475 ‐17 0 ‐1 ‐5 448500 5862600 0+500 500 3 ‐1 ‐15 448475 5862600 0+525 525 ‐10 ‐5 ‐65 448450 5862600 0+550 550 13 ‐1 ‐60 448425 5862600 0+575 575 1 ‐5 ‐61 448400 5862600 0+600 600 4 ‐2 ‐7 ‐5 448375 5862600 0+625 625 11 1 ‐1 ‐10 448350 5862600 0+650 650 23 2 3 ‐3 448325 5862600 0+675 675 24 0 2 ‐2 448300 5862600 0+700 700 21 5 5 ‐7 448275 5862600 0+725 725 18 4 9 4 448250 5862600 0+750 750 10 ‐31 16 448225 5862600 0+775 775 2 ‐4 ‐76 448200 5862600 0+899 800 16 ‐1 ‐5 ‐6 448175 5862600 0+825 825 16 0 ‐1 ‐4 448150 5862600 9+850 850 14 ‐1 ‐11 448125 5862600 0+875 875 10 ‐1 ‐20 448100 5862600 0+900 900 8 0 ‐1 ‐3 448075 5862600 0+925 925 5 1 1 ‐4 448050 5862600 0+950 950 4 2 3 ‐7 448025 5862600 0+975 975 7 6 8 ‐13 448000 5862600 1+000 1000 16 10 16 ‐9 447975 5862600 1+025 1025 19 7 17 First Fraser LINE 3+100 Label X‐axis Slope In‐Phase Calculation Filter 449025 5863100 0‐025 ‐25 ‐8 ‐61 449000 5863100 0+000 0 ‐10 ‐4 ‐10 9 448975 5863100 0+025 25 ‐8 ‐4 ‐8 ‐6 448950 5863100 0+050 50 ‐30‐4 ‐8 448925 5863100 0+075 75 ‐13 0 0 ‐3 448900 5863100 0+100 100 ‐7 ‐1 ‐12 448875 5863100 0+125 125 ‐19 ‐1 ‐2 ‐1 448850 5863100 0+150 150 ‐10 1 0 ‐3 448825 5863100 0+175 175 ‐9010 448800 5863100 0+200 200 ‐300 ‐2 448775 5863100 0+225 225 4 3 3 ‐8 448750 5863100 0+250 250 7 5 8 ‐4 448725 5863100 0+275 275 12 2 7 8 448700 5863100 0+300 300 ‐18 ‐20 3 448675 5863100 0+325 325 ‐16 6 4 ‐14 448650 5863100 0+350 350 17 8 14 ‐1 448625 5863100 0+375 375 ‐10 ‐35 21 448600 5863100 0+400 400 ‐10 ‐4 ‐713 448575 5863100 0+425 425 ‐12 ‐4 ‐83 448550 5863100 0+450 450 ‐6 ‐6 ‐10 7 448525 5863100 0+475 475 ‐12 ‐9 ‐15 4 448500 5863100 0+500 500 ‐10 ‐5 ‐14 ‐4 448475 5863100 0+525 525 ‐8 ‐6 ‐11 ‐6 448450 5863100 0+550 550 ‐4 ‐2 ‐8 ‐8 448425 5863100 0+575 575 ‐2 ‐1 ‐3 ‐10 448400 5863100 0+600 600 3 3 2 ‐9 448375 5863100 0+625 625 12 3 6 ‐5 448350 5863100 0+650 650 22 4 7 0 448325 5863100 0+675 675 18 2 6 3 448300 5863100 0+700 700 6 2 4 3 448275 5863100 0+725 725 20 1 3 1 448250 5863100 0+750 750 24 2 3 ‐1 448225 5863100 0+775 775 23 2 4 ‐1 448200 5863100 0+899 800 21 2 4 2 448175 5863100 0+825 825 26 0 2 7 448150 5863100 9+850 850 19 ‐3 ‐37 448125 5863100 0+875 875 14 ‐2 ‐53 448100 5863100 0+900 900 9 ‐4 ‐62 448075 5863100 0+925 925 7 ‐3 ‐71 448050 5863100 0+950 950 ‐1 ‐4 ‐7 ‐2 448025 5863100 0+975 975 1 ‐1 ‐5 ‐6 448000 5863100 1+000 1000 5 0 ‐1 ‐4 447975 5863100 1+025 1025 20 ‐1 ‐1 First Fraser LINE 3+200 Label X‐axis Slope In‐Phase Calculation Filter 447975 5863200 1+025 1025 15 ‐1 ‐2 448000 5863200 1+000 1000 19 0 ‐1 ‐6 448025 5863200 0+975 975 21 4 4 ‐11 448050 5863200 0+950 950 17 6 10 ‐2 448075 5863200 0+925 925 5 0 6 10 448100 5863200 0+900 900 8 0 0 5 448125 5863200 0+875 875 13 1 1 ‐3 448150 5863200 0+850 850 13 2 3 ‐3 448175 5863200 0+825 825 6 2 4 0 448200 5863200 0+800 800 5 1 3 2 448225 5863200 0+775 775 6 1 2 2 448250 5863200 0+750 750 17 0 1 1 448275 5863200 0+725 725 15 1 1 ‐2 448300 5863200 0+700 700 18 2 3 ‐2 448325 5863200 0+675 675 5 1 3 1 448350 5863200 0+650 650 27 1 2 ‐3 448375 5863200 0+625 625 23 5 6 ‐7 448400 5863200 0+600 600 16 4 9 4 448425 5863200 0+575 575 0 ‐22 13 448450 5863200 0+550 550 ‐38 ‐2 ‐412 448475 5863200 0+525 525 ‐27 ‐8 ‐10 9 448500 5863200 0+500 500 ‐18 ‐5 ‐13 ‐2 448525 5863200 0+475 475 ‐23 ‐3 ‐8 ‐6 448550 5863200 0+450 450 ‐22 ‐4 ‐7 ‐1 448575 5863200 0+425 425 ‐17 ‐3 ‐7 ‐3 448600 5863200 0+400 400 ‐15 ‐1 ‐4 ‐5 448625 5863200 0+375 375 ‐14 ‐1 ‐2 ‐3 448650 5863200 0+350 350 ‐13 0 ‐1 ‐3 448675 5863200 0+325 325 18 1 1 ‐7 448700 5863200 0+300 300 ‐11 5 6 1 448725 5863200 0+275 275 ‐22 ‐50 15 448750 5863200 0+250 250 2 ‐4 ‐9 ‐2 448775 5863200 0+225 225 2 6 2 ‐13 448800 5863200 0+200 200 1 ‐24 8 448825 5863200 0+175 175 ‐3 ‐4 ‐612 448850 5863200 0+150 150 ‐7 ‐4 ‐81 448875 5863200 0+125 125 ‐6 ‐3 ‐7 ‐1 448900 5863200 0+100 100 ‐17 ‐4 ‐71 448925 5863200 0+075 75 ‐16 ‐4 ‐8 ‐2 448950 5863200 0+050 50 ‐7 ‐1 ‐5 ‐4 448975 5863200 0+025 25 ‐5 ‐3 ‐4 ‐2 449000 5863200 0+000 0 ‐90‐30 449025 5863200 0‐025 ‐25 ‐15 ‐4 ‐4 NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
APPENDIX B
FRASER FILTERED DATA PROFILES
CANLAVA MINING CORP.
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
CANLAVA MINING CORP.
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
CANLAVA MINING CORP.
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
CANLAVA MINING CORP.
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
CANLAVA MINING CORP.
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
CANLAVA MINING CORP.
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
CANLAVA MINING CORP.
NAZKO PROPERTY - 2018 FALL ASSESSMENT REPORT
CANLAVA MINING CORP.