Assessment Report

on the

Mike Property Lillooet Mining Division Southern British Columbia, Canada

Mineral Claims: 1063762, 1063763, 1063764, 1063765, 1063766, 1063767, 1063768, 1063769, 1063770, 1063771, 1063772, 1063773, 1063774

NTS Map Sheet 92J/13E, 14W Latitude 55°55’N / Longitude 123°25’W

Prepared for

Cresval Capital Corp.

By

Christopher Basil

Coast Mountain Geological Ltd

June, 2019

Contents Page Summary / Introduction….…………………………………………………………………………………………………………1 Property Description, Location and Access……….…………………………………….…………………………………1 Climate, Local Resources, Infrastructure and Physiography……………………..………………………………..3 History……………………………………………………………………………………………………………………………………….5 Regional Geology……………………………………………………………………………………………………………………….5 Property Geology……………………………………………………………………………………………………………………….6 Mineralization …………………………………………………………………………………………………………………………..7 2019 Ground Magnetics Survey……………………………………………………………………………………………….12 Conclusions…………………………………..…………………………………………………………………………………………15 References……………………………………………………………………………………………………………………………….16

Figure 1 – Location Plan…………………………………………………………………………………………………………….2 Figure 2 – Tenure Map………………………….…………………………………………………………………………………..4 Figure 3 – Regional Geology………………….…………………………………………………………………………………..9 Figure 4 – Local Geology……………………………………………………………………………………………………….…11 Figure 5 – Ground Magnetics Survey Location……………………………………………………..…….……………13 Figure 6 – Ground Magnetic Survey Plan ……………………………………………………………………..…………14

Table 1 – Tenure Details………………………………………………………………………………………………………….…3 Table 2 – Regional Geology Legend………………………………………………………………………………………….10

Appendix 1 – Ground Magnetic Survey Maps Appendix 2 – Statement of Qualifications Appendix 3 – Statement of Costs and Mineral Claim Exploration Work Confirmation Event Pages

Summary / Introduction:

This assessment report presents the findings of the geophysical exploration work carried out on behalf of Cresval Capital Corp’s on their Mike Property, west of Goldbridge BC, in the Lillooet Mining Division. This exploration work consisted of 92.1 line kilometers of ground magnetic surveys, with the field data acquisition work conducted from May 1 through May 5, 2019.

The area of interest targeted for this work was over the western portion of the Mike Property, in the vicinity of the BR, NBR and Copper Plateau Minfile occurrences, on the Copper 11 and Copper 12 claims, (1063772, 1063773). The objective of the ground magnetic survey was to map magnetic features to assist with the mapping of geologic units and structures on the property.

Survey conditions were good to excellent on the plateau, with about 2 meters of compact snow, with well frozen crust in the mornings, enabling excellent production over 48 lines and two perpendicular tie lines. The ground magnetic data was of very good quality and daily calibration readings were consistent.

As hoped and expected the results showed a number of lithologic and structural features, the most pronounced being a large, ovoid shaped zone of intense magnetic gradient, as high as 9000 nT, which coincides with a partially mapped basalt. In the area of the Copper Plateau Minfile occurrence and geochem anomaly converging structures, (NNW and NNE) have been identified.

Numerous other structures, ranging from northerly, northwesterly, northeasterly, and circular, (basalt neck?) were delineated from this survey and will provide focus and direction for follow up programs of mapping, sampling and geochemistry.

Property Description, Location and Access:

The Mike Property is composed of 13 mineral titles, 100% owned by Cresval Capital Corp, located in the Lillooet Mining Division in southwestern British Columbia. (see Figure 1)

Mine Number: 1620591 Mine Coordinates: Latitude: 50.9150000 Longitude: -123.4247200

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2 Table 1 – Tenure Details

Title Claim Number Name Owner Map Expiry 1063762 COPPER 1 205969 (100%) 092J 2020/MAR/25 1063763 COPPER 2 205969 (100%) 092J 2020/MAR/25 1063764 COPPER 3 205969 (100%) 092J 2020/MAR/25 1063765 COPPER 4 205969 (100%) 092J 2020/MAR/25 1063766 COPPER 5 205969 (100%) 092J 2020/MAR/25 1063767 COPPER 6 205969 (100%) 092J 2020/MAR/25 1063768 COPPER 7 205969 (100%) 092J 2020/MAR/25 1063769 COPPER 8 205969 (100%) 092J 2020/MAR/25 1063770 COPPER 9 205969 (100%) 092J 2020/MAR/25 1063771 COPPER 10 205969 (100%) 092J 2020/MAR/25 1063772 COPPER 11 205969 (100%) 092J 2020/MAR/25 1063773 COPPER 12 205969 (100%) 092J 2020/MAR/25 1063774 COPPER 13 205969 (100%) 092J 2020/MAR/25

The Mike Property is accessible via Highway 99 from Vancouver, through Squamish, Whistler, Pemberton into Lillooet. From Lillooet access continues 110 kms westward along the Carpenter Lake Road, (Highway 40), to Goldbridge. From Goldbridge access continues south along the Hurley River Road for 4 kilometers to the junction with the Bridge River Forest Service Road. The access continues westwards on the Bridge River FSR along the southern shore of the Downton Lake reservoir. At approximately km 38 the Bridge River FSR crosses the Bridge River, then at 41 kms crosses Nichols Creek. Near km 46 the Bridge River FSR enters the Mike Property. The road continues another 10 kms into the Mike Property, turning northward up the Thunder Creek valley. The end of the Bridge River FSR is approximately 1.6 kilometers south of the Griswold (Russnor) Minfile showing. A 2 kilometer four wheel drive trail, (Russnor Trail), continues northward up the valley to a point across Thunder Creek from the Russnor showing.

Climate, Local Resources, Infrastructure and Physiography:

The property lies within and adjacent to the Dickson Range of the Pacific ranges along the eastern margin of the Coast Mountains. and is characterized by rugged mountainous terrain broken by minor isolated plateaus. Valley glaciation is widespread as evident in the "U" shaped valley of Nichols Creek. Three main water courses traverse the property: The north and south forks of the Bridge River, and its tributaries, Thunder Creek and Nichols Creek.

Elevations on the property range from 1150m to over 2400m above sea level with slopes timber covered below 1700 to 1800m and generally glacier covered above 2200m. The forest cover of pine and spruce, with local dense alder chutes, is predominantly along the southern portion of

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the property, within the Bridge River valley, as well as in the lower reaches of Thunder and Nichols Creek. At higher elevations vegetation includes alpine meadows, ranging to scrub spruce and balsam. Along the margins of the glaciers in the far north of the property alpine vegetation diminishes to mosses and lichen.

The area has hot, dry summers and cold winters with high snowfall. The exploration season extends from May through October, although the higher elevations can be snow covered into July.

The current means of access by land is from Goldbridge along the Bridge River Forest Service Road. An ATV trail extends 2 kilometers from the terminus of the Bridge River FSR, giving land access to the Russnor showing area. All remaining areas of the Mike property are accessed by helicopter.

The nearest communities that provide logistical support are Goldbridge and Lillooet. The nearest source of power is just west of Goldbridge.

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History:

The exploration history on the property has been conducted separately on three main copper showings covering a 12 km extent of mineralization; the Nichol (Minfile 092JW 009) to the northeast, with the Russnor (Griswold Minfile 092JW 011) in the centre and the BR (Minfile 092JW 010) to the west.

Exploration on the Mike property undertaken between 1929 and 1987, prior to initial acquisition by Cresval Capital Corp, involved approximately 95m of underground development in two adits, the Nichol (32.9m) and Russnor (62.5m), 1790.4m of diamond drilling in 25 holes, hand trenching and chip sampling, all focused on the three known showings. Limited mapping and preliminary rock and soil geochemistry were completed on the Nichol and Russnor showings with more complete mapping and a grid soil survey at the BR. A reconnaissance magnetic survey was completed in the Nichol area with grid magnetic and induced polarization surveys over the BR showing area.

The Mike project was acquired by Cresval Captial Corp. (Cresval) in 2005, with additional claims added in 2007, 2009, 2010 and 2011. Exploration by Cresval, conducted between 2005 and 2018 has included: prospecting, mapping and sampling; a 7.8 line km induced polarization geophysics/MMI soil survey over the Canyon zone; a 4 line km soil survey and 47.35m of hand trenching on the Copper Plateau (above the BR showing); construction of a 2km access trail into, and a 13.5 line km soil survey on the Russnor showing; a 3.5 line km soil survey over the Windy Copper showing; 2031.5m of diamond drilling in 9 holes testing the Copper Plateau with 5 holes and the Russnor Breccia with 4 holes; and a 1149 line km airborne magnetic and radiometric survey.

Regional Geology:

The Mike property lies within the southeastern Coast Belt dominated by Cretaceous to Tertiary aged intrusive rocks of the Coast Plutonic Complex. To the east, the Coast Plutonic Complex intrudes Triassic to Jurassic island arc related volcano-sedimentary rocks of the Bridge River terrane, upper Cretaceous Powell Creek volcaniclastic rocks and Jura-Cretaceous sedimentary rocks of the Tyaughton Basin.

The most recent regional mapping in the Mike property area was by Roddick and Woodsworth (1977). The surrounding area was mapped by Schiarizza et al. (1997) and a digital compilation was completed by Cui et al. (2017), updating the ages of the lithological units. The Bridge River Pluton was discovered and delineated as a separate, younger pluton by the Geological Survey of Canada in 1928 (Dolmage, 1929).

5 Within the regional area, the Coast Plutonic Complex primarily consists of Late Cretaceous quartz diorite (LKqd) and granodiorite (LKgd) intrusions; the latter includes the Dickson – McClure Batholith along the eastern margin of the Complex. Locally younger Late Cretaceous to Paleogene granodiorite (LKPeBgd) to quartz monzonite (LKPqm) intrusions intrude the above; the former (LKPeBgd) includes the Lord River pluton, one of the Bendor plutonic suite, primarily exposed to the north, west and southwest of the property. The “LKPqm” pluton which underlies the Mike property will be informally referred to as the Bridge River pluton in this report. The Miocene aged Salal Creek pluton of quartz monzonite composition, which hosts the Salal porphyry molybdenum prospect just south of the Mike Property, represents one of the youngest intrusions within the Coast Plutonic Complex.

The intrusive rocks are locally overlain by flat lying Pleistocene aged plateau basaltic lavas of the Garibaldi Group (Plev, Miv ).

Property Geology:

Less than 20% of the Mike property has been mapped in detail. Historical mapping has included reconnaissance mapping by Phelps Dodge Corp. on the Nichol area in 1963 (Meyer, 1963), limited mapping be Cerro Mining Company on the Russnor in 1970 to 1971 and preliminary mapping on the Russnor and Nichol areas in 2005; and the BR, Russnor and Windy Copper showings in 2010, with discovery of the Snowfield zone.

The Mike property is primarily underlain by the probable Paleogene aged Bridge River pluton (LKPqm) which intrudes Late Cretaceous granodiorite to the south, and adjoins the Lord River pluton (LKPeBgd), a larger, similarly aged granodiorite body, to the north, west and southwest. The intrusive rocks are locally overlain by flat lying Pleistocene aged plateau basaltic flows (Plev, Miv) and intruded by related basalt to diorite feeder dykes and felsite, quartz porphyry and feldspar porphyry dykes.

The Bridge River pluton was first discovered by the Geological Survey of Canada in 1928 and described as a younger white granite with a soda granite composition, consisting of 40% quartz, 40% albite-oligoclase, 5% orthoclase and 15% biotite (Dolmage, 1929).

Those parts of the Bridge River pluton examined during the 2005 and 2007 to 2011 programs in the Canyon, Nichol, Russnor and Windy Copper showing areas are consistent with a granite composition, but quartz monzonite predominates in the BR showing area and southeast of Russnor, with local alkali granite compositions at BR. The contact between the Bridge River pluton and the older quartz diorite was observed above (east of) the Nichol showing exposed as a fault.

6 A mineralized intrusive breccia (Russnor Breccia) occurs within the Bridge River pluton at the Russnor showing area and is exposed for 80m in the canyon walls of Thunder Creek, in the adit and in the core from the 1961 drill program by Phelps Dodge Corp. The breccia consists of clast supported subangular fragments of granite with varying amounts of sulphide cement. Six small quartz monzonite breccia pipes have been identified in the vicinity of the BR showing but largerly appear to be post mineral with exception of the breccia bodies north of DDH 71-4, which appear weakly hydrothermal at surface (Enns and Lebel, 1980).

Flat lying Pleistocene basalts unconformably overlie the intrusive rocks with a discontinuous regolith, up to 10m wide, exposed at the base. The regolith (cgl), primarily observed northwest of the Nichol showing, consists of rounded pebbles to boulders of granite cemented by basalt. The regolith was intersected in DDH 71-3 at the BR showing and in DDH RS11-08 at the Russnor showing. The basalt is generally brownish to black in colour, locally dark green near the base, porphyritic, highly vesicular and commonly exhibits columnar jointing. Interflow sedimentary rocks are intercalated with the basalts, at the base of the lavas northeast of the Russnor showing and southwest of the Nichol showing.

Basaltic and diorite dykes, probably feeders to the lavas, intrude the plutonic rocks. Andesite dykes also occur and may be related to the Pleistocene volcanic lavas or possible earlier. Northwest to northerly trending felsite and quartz porphyry dykes, an easterly trending latite feldspar porphyry dyke in the BR showing area and latite dykes and volcanic rocks in the Slide Creek area south of the Russnor showing also intrude the granite and are probably associated with Pleistocene plutonism.

Mineralization:

The Mike property covers the historical Nichol (Raelode), Griswold (Russnor, Mel), Red Creek and BR (Bridge River, BR 4) Minfile copper porphyry showings as documented by the British Columbia Survey Branch as Minfile numbers 092JW 011, 092JW 009, 092JW 053 and 092JW 010. Work by Cresval resulted in the discovery of significant additional showings which have been identified and Minfile showings and include the Copper Plateau or NBR (092JW 050) and the Windy and Snowfield Copper showings (092JW 054).

Mineralization at the Nichol showing appears to occur as quartz-sulphide and sulphide veins and fracture fillings exposed over a 600m by 400m area, hosted by the Bridge River pluton. Sulphide minerals consist of chalcopyrite and pyrite. Individual veins trend 015 to 056°, dipping moderate to steeply easterly, with an overall trend to the mineralized zone of approximately 010°. Disseminated chalcopyrite is widespread between the veins within the granite host but is difficult to sample due to lack of exposure, interspersed with cliff outcrops. Alteration includes silica, sericite, potassic alteration and local kaolinization.

7 Mineralization at the Russnor showing consists of disseminated, blebby and poddy chalcopyrite, bornite and pyrite with trace molybdenite hosted by an intrusive breccia that may trend 330°/85W within the Bridge River pluton. Wallrock alteration consists of chlorite, sericite and potassium feldspar. The mineralization is incompletely exposed within an 80m long canyon along Thunder Creek, where malachite and azurite have locally resulted in distinct green and blue staining of the walls.

The Windy Copper showing covers a 1km by 400m copper mineralized area approximately 3 km to the northwest of the Russnor showing. The zone consists of west dipping, primarily northerly to northwesterly trending (025° to 340°) quartz +/- sulphide (chalcopyrite, bornite +/- tetrahedrite) stringer-stockwork veins and fracture fillings mineralized with chalcopyrite hosted by well fractured silica-sericite altered granite with disseminated chalcopyrite and bornite.

Copper mineralization at the BR showing extends over a 1.7 km by 0.5 km area with a central higher-grade zone 1.45 km by 150 to 300m wide, exposed along south facing cliffs north of the North Fork of the Bridge River. The mineralization consists of chalcopyrite, cupriferous limonite, chrysocolla, malachite, azurite, tenorite, bornite, chalcocite, magnetite and trace molybdenite in fractures with sericite and quartz gangue.

In 2008 and 2009, copper mineralization was traced onto the plateau area above the BR. A 450 by 550m copper in soil anomaly was delineated on the Copper Plateau.

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9 Legend

?og Age Unknown metamorphic rocks

PiHoGv Pliocene to Holocene Garibaldi Group volcanic rocks

PiHoGvb Pliocene to Holocene Garibaldi Group basalt

MiPlCvb Miocene to Pleistocene Chilcotin Group volcanic rocks

Miqm Miocene quartz monzonite

Miqd Miocene quartz diorite

Miv Miocene volcanic rocks

Olfp Oligocene intrusive rocks

Egd Eocene granodiorite

PeEfp Paleocene to Eocene intrusive rocks

PeEca Paleocene to Eocene volcanic rocks

LKTg Late Cretaceous to Paleogene intrusive rocks

LKTfp Late Cretaceous to Paleogene feldspar prophyritic intrusive rocks

LKTdr Late Cretaceous to Paleogene diorite

LKTgd Late Cretaceous to Paleogene granodiorite

LKTqm Late Cretaceous to Paleogene quartz monzonite

LKgd Late Cretaceous granodiorite

LKqd Late Cretaceous quartz diorite

uKPovc Upper Cretaceous Powell Creek Formation volcanic rocks

uKPosc Upper Cretaceous Powell Creek Formation sedimentary rocks

uKPo Upper Cretaceous Powell Creek Formation volcanic rocks

uKPocg Upper Cretaceous Powell Creek Formation sedimentary rocks

luKs Cretaceous sedimentary rocks

luKTB Cretaceous Taylor Creek Group Beece Creek Succession sedimentary rocks

ETgd Early Cretaceous granodiorite

lKTca Lower Cretaceous Taylor Creek Group volcanic rocks

lKvc Lower Cretaceous volcanic rocks

lKE Lower Cretaceous Elbow Pass Formation sedimentary rocks

lKR Lower Cretaceous Relay Mountain Group sedimentary rocks

lKs Lower Cretaceous sedimentary rocks

lKGsv Lower Cretaceous Gambier Group sedimentary rocks

lKTs Lower Cretaceous Taylor Creek Group sedimentary rocks

lKTC Lower Cretaceous Tosh Creek Succession sedimentary rocks

lKTD Lower Cretaceous Taylor Creek Group Dash Formation sedimentary rocks

lKTL Lower Cretaceous Taylor Creek Group Lizard Formation sedimentary rocks

LJKqd Late Jurassic to Early Cretaceous intrusive rocks

uJKR Upper Jurassic to Lower Cretaceous Relay Mountain Group sedimentary rocks

muJR Middle to Upper Jurassic Relay Mountain Group sedimentary rocks

uTrTy Upper Triassic Tyaughton Group sedimentary rocks

uTrCsv Upper Triassic Cadwallader Group sedimentary rocks

PzMzog Paleozoic to Mesozoic metamorphic rocks

Table 2 – Regional Geology Legend 10

11 2019 Ground Magnetics Survey:

The area of interest targeted for this ground magnetic survey work was over the western portion of the Mike Property, in the vicinity of the BR, NBR and Copper Plateau Minfile occurrences. The objective of the survey was to map magnetic features to assist with the mapping of geologic units and structures on the property including any magnetic features that may relate to known mineralization.

Survey conditions were good to excellent on the plateau, with about 2 meters of compact snow, with a well frozen crust in the mornings, enabling excellent production over 48 lines and two perpendicular tie lines with a total survey production of 92.1 line kilometers.

For the magnetometer survey two GEM GSM-19W Overhauser magnetometers with integrated GPS units were used as rovers to collect total field measurements along the survey lines. The GMS-19V unit was setup as a base station to record diurnal variations in the magnetic field. A recording interval of 3 seconds was selected for the base station unit.

Thanks to the favorable terrain and clear GPS signal acquisition conditions the magnetic data was collected in “walking mode”, whereby readings are taken every 2 seconds and reading locations recorded with an integrated GPS system. This resulted in magnetic readings taken around every 2 meters along lines separated by 50 meters. The ground magnetic data was of very good quality and daily calibration readings were consistent.

As hoped and expected the results showed a number of lithologic and structural features, the most pronounced being a large, ovoid shaped zone of intense magnetic gradient, as high as 9000 nT, which coincides with a partially mapped basalt. In the area of the Copper Plateau Minfile occurrence and geochemical anomaly converging structures, (NNW and NNE) have been identified.

Numerous other structures, ranging from northerly, northwesterly, northeasterly, and circular, (basalt neck?) were delineated from this survey and will provide focus and direction for follow up programs of mapping, sampling and geochemistry. (See figure 6 – Ground Magnetic Survey Plan)

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Figure 6: Ground Magnetic Survey Plan

14 Conclusions:

The results of the Spring 2019 ground magnetic survey over the Copper Plateau and western region of the Mike claims delineated a number of lithological and structural features. As recent reporting has indicated there has been limited property mapping and the extent of certain units, such as the recent basalts, are not fully defined. The ground magnetic survey results indicate their effectiveness in aiding in this mapping effort as the recent basalts generate an intense high gradient response (~9000 nT).

It appears from the magnetic response that the recent basalt may not be as extensive as has been represented from regional mapping and past airborne magnetic surveys. This is encouraging as its presence poses significant challenges when considering geophysical surveys to search for evidence of porphyry targets at depth.

Of additional interest are the structural features defined by this survey. In the area of the Copper Plateau minfile showing, where a 450 by 550m copper in soil anomaly was delineated, the magnetic survey indicates NNW/NNE intersecting structures. Numerous other intersecting magnetic features were obtained and will provide good guidance for recommended prospecting, mapping and geochemical surveys.

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References:

Cui, Y., Miller, D., Schiarizza, P., and Diakow, L.J. 2017. British Columbia digital geology. British Columbia Ministry of Energy, Mines and Petroleum Resources, British Columbia Geological Survey Open File 2017-8, 9p.

Dolmage, V. 1929. Gun Creek map area, Lillooet District, BC; Geological Survey of Canada, Summary Report 1928, pp 78A-93A

Enns, S.G. and Lebel, J.L. 1980. Bridge River Property, British Columbia Ministry of Energy, Mines and Petroleum Resources Assessment Report 8804

Meyer, W. 1963. Geological, geophysical and geochemical report Nichols Creek, British Columbia. BCMEMPR Assessment Report #534

Paulter, J.M. 2017. 43-101 Technical Report on the Mike Project for Cresval Capital Corp.

2011. Report on the 2010 geological and geochemical program, Bridge River Project. BCMEMPR Assessment Report #32065

2009. Geological and geochemical assessment report on the Bridge River Project. BCMEMPR Assessment Report #30991

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APPENDIX 1

GROUND MAGNETIC SURVEY MAPS

GROUND MAGNETIC SURVEY GRID MAP

GROUND MAGNETIC SURVEY STACKED TOTAL MAGNETIC INTENSITY PROFILES MAP

GROUND MAGNETIC SURVEY TOTAL MAGNETIC INTENSITY MAP

GROUND MAGNETIC SURVEY TOTAL MAGNETIC INTENSITY MAP: SHADOW ENHANCED

GROUND MAGNETIC SURVEY TOTAL MAGNETIC INTENSITY MAP WITH STACKED PROFILES

APPENDIX 2

STATEMENT OF QUALIFICATIONS

STATEMENT OF QUALIFICATIONS:

I, Christopher Basil, of Gibsons BC, do hereby certify that:

1. I majored in Physics at McGill University, Montreal from 1978 through 1982. 2. I completed the Province of British Columbia, Ministry of Energy Mines and Petroleum Resources / Malaspina College ADVANCED PROSPECTING COURSE in 1989 3. I began my career as a Geophysical Operator with the BC Ministry of Highways, Geotech and Materials Division from 1982 through 1986. 4. I have been Vice President of Coast Mountain Geological Ltd from 1988 through the present. 5. I have been practicing my profession for 35 years as a Geophysical Operator, Project Manager, Safety Manager and Mineral Exploration Consultant. 6. I hold BC Mine Supervisor Certification, No. 835948, issued by the British Columbia Ministry of Energy, Mines and Petroleum Resources, valid until June 27, 2023 7. I personally designed and oversaw the ground magnetic survey that is the subject of this report.

Dated this 2nd day of July, 2018

______Christopher Basil

APPENDIX 3

STATEMENT OF COSTS And MINERAL CLAIM EXPLORATION AND DEVELOPMENT EVENT CONFIRMATION PAGES (EVENTS: 5740238, 5748813)

TYPE OF WORK IN THIS REPORT EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS GEOPHYSICS: GROUND MAGNETICS SURVEY PREPERATORY: Property Scale Review & Program Planning 1063772, 1063773 Personnel Time: C. Basil, Project Manager: 1 Day @ $700 $ 700.00 $ 700.00

GEOPHYSICAL: Accommodation: Mag Survey - 7 Days 1063772, 1063773 $ 1,980.00 Fuel: $ 113.74 Mag Survey Equipment and Operators $ 10,175.00 Meals: $ 810.34 Mobilization/Demobilization: $ 2,036.87 Helicopter: (15 hrs @ $1,635/hr) $ 24,525.00 Helicopter fuel: $ 2,675.97 Personnel: C. Basil, Project Manager: 3 Days @ $700 $ 2,100.00 $ 44,416.92

REPORTING: Property Scale Review Mag Data Processing and Reporting: $ 3,201.00 Personnel Time: C. Basil, Project Manager: 3.5 Days @ $700 $ 2,450.00 J. Lewis, GIS Tech.: 10 Hrs @ $65 $ 650.00 $ 6,301.00

Total of Work Performed: $ 51,417.92

Total Assessment Work Filed: $ 49,470.25