National Instrument 43-101 Standards of Disclosure for Mineral Projects

Mr. Jacques Houle, P.Eng., serves as the qualified person responsible for the technical information contained in this document dated November 14, 2023, and titled "Santana Technical Assessment Report".

Information in the document is not necessarily indicative of the continuity and grades of mineralization on the property.
This is not a technical report, but the document contains all technical information required to be disclosed to make the document not misleading.
Mr. Houle has not visited the project and has no prior involvement with the property.
Mr. Houle is a professional engineer in BC with relevant experience as a mineral exploration consultant on Vancouver Island and he is a "qualified person" for purposes of the instrument.
Mr. Houle is independent of the issuer Kermode Resources Ltd. (TSXV:KLM).

Ministry of Energy and Mines Assessment Report BC Geological Survey TYPE OF REPORT [type of survey(s)]: Technical, Prospecting, Geochemical TOTAL COST: 7757.88 _______ AUTHOR(S): Justin Deveault NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): ______ STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S): 5994120 PROPERTY NAME: Santana Property CLAIM NAME(S) (on which the work was done): Santana Mine COMMODITIES SOUGHT: Gold, Silver, Copper MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN: 092BK013 NTS/BCGS: 092K015 MINING DIVISION: Naniamo $^{\circ}$ 09 $^{\circ}$ 11 $^{\prime}$ 26 '43 50 LONGITUDE: 125 LATITUDE: (at centre of work) OWNER(S): 1) Justin Deveault the control of the control of the control $\overline{2}$ ) MAILING ADDRESS: 6114 Snowdrop Place Duncan, BC V9L5J7 OPERATOR(S) [who paid for the work]: 1) 911 Exploration Corp. $\begin{array}{ c c c c c c c c c c c c c c c c c c c$ MAILING ADDRESS: 6114 Snowdrop Place Duncan, BC V9L5J7 PROPERTY GEOLOGY KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude): Skarn, Limestone, Diorite, Quartz Diorite, Quartz, Chalcopyrite, Pyrite, Pyyhrotite, Triassic Parsons Bay Formation, Granite, Gnei Gold, Copper, Silver, Calcareous Shale, Magnetite REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: N/A	The Best Place on Earth
			Title Page and Summary















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TYPE OF WORK IN THIS REPORT	EXTENT OF WORK (IN METRIC UNITS)	ON WHICH CLAIMS	PROJECT COSTS APPORTIONED (incl. support)
GEOLOGICAL (scale, area)
Ground, mapping ______
Photo interpretation Example 2018
GEOPHYSICAL (line-kilometres)
Ground
Magnetic ______
	Electromagnetic ______
Induced Polarization ______
Radiometric Executive Constitution
	Seismic ______
	Other ______
Airborne ______
GEOCHEMICAL (number of samples analysed for)
Soil ______
Silt ______
Rock 11 Portable XRF Samples		1097236	550.40
Other ______
DRILLING (total metres; number of holes, size)
Core ______
Non-core ______
RELATED TECHNICAL
Sampling/assaying 11 XRFs
Petrographic ___ ________
Mineralographic ______
Metallurgic ______

PROSPECTING (scale, area) Prospecting		1097236	7207.48
PREPARATORY / PHYSICAL
Line/grid (kilometres)
Topographic/Photogrammetric (scale, area)
Legal surveys (scale, area) ______
Road, local access (kilometres)/trail ______
Trench (metres) ______
Underground dev. (metres) ______

Other ______			7757.88
		TOTAL COST:

TECHNICAL ASSESSMENT REPORT ON PROSPECTING

Owners - Operators

Justin Deveault FMC#277308 911 Exploration Corp. 6114 Snowdrop Place V9L 5J7

SANTANA PROPERTY

Tenure Numbers: 1097236

Property Size: 517.19 Quadra Island, B.C. Nanaimo Mining Division Latitude 50 11 26 N - Longitude 125 09 43 W 10N 55622055N, 346255E BCGS: 092K015

Information for this report compiled and written by: Justin Deveault of 911 Exploration Corp. FMC#277308 Date Written: November 13th, 2023

Cover Pages	1-3
Table of Contents	4
Property Summary/Introduction	5
Tenure Access & Location	6
Physiographic Setting & Climate	7
History	7
Property Geology	7
Mineralization & Occurrences	8-9
XRF Testing	10-11
Conclusions & Recommended Exploration	12-13
References	13
Statement of Costs	14
Statement of Qualifications	14
Expiry Date Change	15
Mapping	16-26

TECHNICAL ASSESSMENT & PROSPECTING REPORT ON THE SANTANA PROPERTY

By Justin Deveault (FMC#277308) 911 Exploration Corp. November 13, 2023

SUMMARY, INTRODUCTION & DESCRIPTION

Justin Deveault of 911 Exploration Corp. holds ownership of the mineral tenure 1097236. The property covers 517.19 hectares and is located above Conville Point on Quadra Island, BC. The claim cell was staked using British Columbia's Mineral Titles Online staking system. The reason for staking the tenure was to evaluate the mineral potential of the property, which according to research appeared promising. Previous exploration attempts were few, very dated and not well documented.

Portions of the property have had previous work; mostly occurring around the vicinity of the old Santana adit. The completion of our initial phase of exploration consisted of general prospecting, sampling, limited XRF analysis, locating old workings, trenches, and open cuts. A total of three days with two prospectors was spent exploring the property.

Eleven grab samples from various mineral showings were taken. All samples were visually examined to confirm sample descriptions, then analyzed by a handheld portable XRF. The XRF was calibrated to analyze copper readings only. All these eleven samples were split in half to preserve a duplicate of each sample, these will be sent in for analysis to a lab later. All samples that were taken were removed from the property and catalogued.

The results of the initial prospecting are extremely encouraging as many of the historical showings were found. Copper skarns were found in many areas over a strike distance of five hundred meters, with some of the showing widths exceeding fifteen meters. Most showings consisted of heavily disseminated up to massive chalcopyrite, with minor pyrite and pyrrhotite.

A total of nine trenches, seven small open cuts and three mine adits were found over three days. This report discusses exploration with primary focus on the eleven sample areas we analyzed via XRF only. The report is intended as an account of our 2023 preliminary exploration program. The information presented here is based upon field work conducted on the property by two individuals, working for 911 Exploration Corp.

TENURE LOCATION, ACCESS, INFRASTRUCTURE

The Santana Property is located on Quada Island in British Columbia. The tenure is located on private forestry land which is accessible year-round. During the initial exploration program, a cottage with amenities located 15km away from the property was used for accommodations. Quadra has many campsites, RV parks, motels and resorts and accommodations can be found year-round. A second option for accommodations is Campbell River which is only a 10-minute full-service ferry ride away, this runs every 20 minutes.

Travel was initially from Duncan to the BC Ferries terminal in Campbell River by truck. Then from the BC ferries terminal to Quadra and from the Quadra terminal to the center of the property. Access to the showings and old adits is a 200-700m hike from the edge of an old, decommissioned logging road. This took less than 30 minutes to the furthest portion visited.

Local infrastructure including a network of logging roads, transmission lines and communication services are well developed nearby. Accommodation, supplies, and equipment are readily available in various areas on Quadra and other nearby larger communities like Campbell River which have adequate supplies for day and overnight trips to the property.

PHYSIOGRAPHIC SETTING & CLIMATE

The property lies between elevations of sea level up to elevations of 250m. The terrain is moderately steep on 50% of the property, however some portions of the claim block are almost flat. Abandoned logging roads, an old mine road and foot trails provide easy access. Forest cover is dominantly, pine, fir, cedar with much of it either recently logged or in second growth ready to be logged.

The climate in the area is mild with an average winter temperature of 2° C and an average summer temperature of 20.0° C. Winter lows can reach -10° C and summer can on occasion reach up to 40° C. During the program, the temperature we had a strong heat wave on much of the Island. This brought temperatures from to 35-39 degrees celsius during the day. Portions of the property are close to the ocean which made for a cooling breeze and allows for slightly cooler temperatures. The average annual precipitation is less than 1,000mm. Exploration and development work is possible throughout 12 months of the year depending on minor snowfall.

SANTANA PROPERTY HISTORY

Mineralization was first discovered at the Santana occurrence in 1915. The owners conducted hand trenching, 250m of hand stripping, blasted various open cuts, and drove three adits. In 1916 a shipment of hand-sorted ore, from adit number one was sent to the Anyox Smelter, at Granby Bay. From 158 metric tonnes 14,370 gram of silver, 93 grams of gold and 4779 kilograms of copper was recovered.

In 1929 and 1930 the property was controlled by Santana Copper Syndicate; little work was reported. The property lay inactive until 1964 when surface work exposed a mineralized zone over 1500m, with widths of up to twenty-five meters. In 1964 R. Renshaw conducted diamond drilling. Four holes were drilled in the hanging wall totalling 762 metres, all holes missed the skarn zone and intersected granite and quartz diorite. The entirety of all four holes is reported to contain 0.3% copper. In 1970 Hebert L. Coons P. Geo recommended mining the 0.3% low-grade copper by open pit but funding could not be raised.

Prospecting work was carried out by two prospectors in 1987 and 1988, twenty-five samples were taken and assayed. Samples assayed as low as 113ppm copper up to 12% copper. In 1989, Lonsdale Capital Corporation had an option to earn 100% interest in the Santana property. A geologist visited the property initially and three samples were taken, however no work is recorded after July 19th, 1989.

GENERAL PROPERTY GEOLOGY

The Santana occurrence lies approximately 7-kilometres east of the Insular tectonic belt and Coast Plutonic Complex boundary. Diorite and quartz diorite are the predominant intrusive compositions along the western edge of the Coast Plutonic Complex. Other intrusive phases include granodiorite, quartz monzonite and granite. The oldest rocks of the Insular tectonic belt are altered basaltic flows, breccia and tuffs with minor greywacke, argillite and chert of the Permian Sicker Group. These are overlain by basalt flows, porphyritic andesite agglomerate and tuffs of the Triassic Karmutsen Formation. The overlying Late Triassic to Early Jurassic Quatsino and Kunga formations are composed of limestone.

The Santana occurrence is underlain by two lithologies. To the west is quartz diorite which, in the east, is in contact with thinly interbedded grey limestone and calcareous shale of the Triassic Parson Bay Formation. The limestone and shale strike 180 degrees and dip 75 to 85 degrees to the west.

MINERALIZATION, MINERAL OCCURENCES & SAMPLING

During our exploration program, time spent examining the rock and bedrock exposures was in the search of skarn and copper mineralization. The main purpose of noting rock types was to see the number of sulphides in each rock type and to look for areas of skarn with copper mineralization.

The most common mineralization on the property is chalcopyrite, followed by pyrrhotite and pyrite. These three sulphides can be found in skarnified rock, gneissic rock and occasionally in limestone. The mineralization at most showings appears to be mostly in gneissic rock which at times has the appearance of skarn, however no magnetite is present with the chalcopyrite. I noted in many places quartz veining which is interwoven and contacting the limestone. Mineralization in the quartz varies from finely disseminated in some areas to containing large patches of chalcopyrite in the Santana adit number one. Here the quartz is well over two meters wide and is contacting limestone.

Below are several areas exposed by historic work with significant mineralization, which we located during our 2023 exploration program. These showings were substantial in the fact they have significant mineralization in grade and width.

Santana Adit #1 (10N 345727E, 5561990N)

The Santana adit combined with the opencut at the portal is approximately 30m long and cuts through the hanging and footwall. This is the area where mineralization is best exposed, and the width is best seen. Mineralization is exposed over 15m in the portal entrance and opencut. The mineralization is heavily disseminated up to massive chalcopyrite with minor pyrite and pyrrhotite. Samples taken from the heavily malachite stained, hanging wall are gneissic and at times skarnified. Mineralization is also in the footwall and the true width is incompletely exposed.

Inside the adit there is mineralized gneiss, a large quartz vein which narrows at the entrance and widening to almost three meters close to the limestone contact. This vein has patches of massive chalcopyrite up to 10cm wide. The limestone contact past this is well defined at the base/start of the raise. This is located fifteen meters inside the adit portal. The remainder of the adit and a short crosscut are in limestone. Areas with lesser mineralization were noticed along with quartz diorite throughout the adit.

The raise surfaces fifteen meters in elevation above the adit and is opened by a 3m x 4m rectangular hole. The prospect hole cuts a blue/grey limestone. Semi-massive to massive chalcopyrite, pyrrhotite and pyrite can be sampled along the entire width exposed in the prospect hole.

Below the adit there is a dump approximately fifteen meters tall, twenty meters wide and at minimum three to four meters deep which contains considerable mineralization. Most samples observed contain mineralization from disseminated to massive sulphides. Below the dump a second pile roughly 6m x 5m x 4m was found containing stockpiled samples, which have been historically mined and likely stockpiled for the "smelter." All samples hammered open were semi-massive to massive chalcopyrite.

Santana Adit #2 (10N 345715E, 5562074N)

The second adit is only 50-60m distance from adit #1. The adit appears to run for 40m or more and contains fifteen to eighteen meters of heavily mineralized, skarnified gneissic rock. Due to slight flooding, we did not go in this adit fully, but merely sampled the first mineralized area out of safety concerns.

Santana Adit #3 (10N 345728E, 5562147N)

The third adit is partially collapsed, and it was not safe to enter more than a couple meters. The limestone contact can be seen from the entrance and a heavily weathered area assumed to be mineralized. Several other trenches are near this adit; however, most are sloughed and would require hand excavation to expose bedrock.

Opencut #1 (10N 345756E, 5562064N)

Opencut number one is struck on a thirty by fifteen-meter-tall outcrop. Significant stripping appears to have been previously done and several areas blasted into disseminated up to massive sulphides over the open cuts. Several other areas of heavily mineralized outcrop were in this area.

Opencut #2 (10N 345773E, 5562098N)

This area has a small three by three-meter open cut struck into outcrop. The gneissic outcrop was moss covered so hand stripping was needed to expose a ten-meter-wide area. At least five meters of the area contained semi massive chalcopyrite and pyrite. This contacts a grey-white quartz vein which was weakly mineralized only in a few areas. The quartz vein cuts through vertically and was chased for fifteen meters. Twenty meters above quartz and quartz diorite was found with some areas containing heavily disseminated magnetite blebs.

Trench #2 (10N 345736E, 5562251N)

Disseminated chalcopyrite, pyrite and pyrrhotite exposed in an open cut attached to a small trench five by three meters wide. The trench is sloughed in however, massive chalcopyrite can be seen in both skarn, gneiss and quartz in a small pile left outside the trench. Bedrock is exposed over three meters and disseminated to semi-massive chalcopyrite was sampled at the back wall after hand exposing the bedrock.

Trench #1 (10N 345744E, 5562171N)

A ten meter long, by two-meter-wide trench exposes bedrock over a three-meter-wide area. The bedrock consists of heavily disseminated chalcopyrite in a weathered skarn like rock. Beside the mineralized area there is a barren quartz vein over one meter wide.

Steep Showing (10N 345755E, 5561961N)

The showing is exposed above the Santana adit. The showing follows the strike of the adit and cut across the mountain peak away from the main limestone contact. The sulphides are disseminated up to semimassive chalcopyrite. The width exposed is under a meter but has a strike of over a strike of a hundred fifty meters. This new showing is not following the historically documented line of contact with limestone and may be an offshoot. Quartz veining was seen crosscutting the mineralization is several areas. Malachite and azurite can also be seen.

PORTABLE XRF ANALYSIS

During our exploration program an Olympus Delta portable XRF (Model DS 6500CC) was used to determine a general idea of copper content only for each sample. All samples analyzed with a portable XRF were duplicated. The duplicates may be sent out for lab analysis at a future date so we can test for multi-elements. For this purpose of this report and field program we were only interested in obtaining immediate copper values.

The XRF was used for reference only and are not substituted for commercial lab analysis. Several previous XRFs were completed by the lab and were used in the calibration of the portable XRF to gain more accurate results. Following is the process used at every calibration. At each startup, a calibration coin was analyzed, and subsequent analysis was only performed when a pass was obtained, which was calculated internally by the XRF instrument.

The XRF unit was set to geochemical mode and a full 200 second test was run to determine copper content. While the instrument detects many elements, only copper was tested. The XRF analyzes only a small portion of the sample, so half the sample was crushed to pass an 80-mesh screen before testing. During analysis of the samples by handheld XRF, non-blind control samples were analysed to monitor the XRF instrument calibration and performance. A correction factor for all base metals was applied to the raw data.

The correction factor was determined by analyzing samples that had previously been analyzed at a commercial laboratory. These rock samples were of varying concentrations and analyzed by the handheld XRF using the method described above. The portable XRF is accurate to within a 5% error for copper content. We did not use the portable XRF to determine accurate readings for other elements.

ID	ANALYSIS	RESULT	ELEVATION	GPS	SAMPLE	SAMPLE DESCRIPTION
		HIGHLIGHTS		LOCATION	TYPE
XRF	Portable XRF	23.32% Cu,	142m	10 N 345722E	Grab	Sample taken from the gneissic
1				5561993N		rock which has the appearance
						of being skarnified. Malachite
						stained sample with massive
						chalcopyrite.
XRF	Portable XRF	16.97% Cu	159m	10 N 345740E	Grab	Sample from the prospect hole
2				5561961N		at the top of the raise. Sample
						from massive chalcopyrite, pyrrhotite with minor pyrite.
XRF	Portable XRF	4.72% Cu,	163m	10 N 345744E	Grab	Heavily weathered sample with
3				5562171N		20% chalcopyrite taken from a
						gneissic rock beside a quartz
						vein, inside a trench.
XRF	Portable XRF	18.43% Cu	137m	10 N 345716E	Grab	Sample taken from the lower
4				5561982N		portion of the dump. Sample
						was massive chalcopyrite with
						some skarn attached.
						Malachite-stained chalcopyrite.
XRF	Portable XRF	12.69% Cu	130m	10 N 345701E	Grab	Random grab sample from the
5				5561971N		stockpile. Sample of semi
						massive chalcopyrite in a
						gneissic rock.
XRF	Portable XRF	16.76% Cu	140m	10 N 345715E	Grab	Grab from in the adit. Gneiss
6				5562074N		with chalcopyrite and pyrrhotite. Sample contained
						50% chalcopyrite.
XRF	Portable XRF	4.56% Cu,	154m	10 N 345728E	Grab	Sample found inside the
7				5562147N		entrance of adit #3. Sample
						had limestone and gneissic
						rock with 15% chalcopyrite.
XRF	Portable XRF	8.60% Cu	163m	10 N 345756E	Grab	Large outcrop with several
8				5562064N		small open cuts and areas of
						stripping. Sample has 30%
						chalcopyrite and 10% pyrite.
XRF	Portable XRF	14.14% Cu	175m	10 N 345773E	Grab	Grab from the center of a 5m
9				5562098N		wide mineralized area. Sample
						had 40% chalcopyrite in
						gneiss.
XRF 10	Portable XRF	8.51% Cu,	166m	10 N 345737E 5562250N	Grab	Outcrop at the back of a small opencut with sulphides. 30%
						chalcopyrite, 5% pyrite and
						10% pyrrhotite.
XRF	Portable XRF	3.33% Cu	184m	10 N 345755E	Grab	Grab from a quartz vein/skarn
11				5561961N		area with 10% chalcopyrite.
						Sample is from an offshoot
						above main adit.

CONCLUSIONS & RECOMMENDED EXPLORATION

Based on the results of exploration it is determined that significant mineralization can be found over multiple areas along a 500m strike. Values in copper exceeded 3.33% in all samples and most samples exceeded 8.50% copper. Further exploration is advised in advancing this property. More detailed work should be completed to determine the potential of the property. Several phases of exploration are outlined below.

Phase One Details & Budget:

Detailed prospecting of the entire property as this program was focused mainly on the historic mine sites.
Digging out all historic open cuts and trenches by hand so they can be sampled properly.
Geochemical lab analysis including grabs and larger chip sampling.

Two prospectors for 30 days.	\$30,000
Lab analysis for samples.	\$4,000
Equipment, tools, supplies, travel and or accommodation.	\$5000
Technical reporting, mapping and documentation.	\$3000
Subtotal For Entire Phase One	\$42,000

Phase Two Details & Budget:

Waste rock, stockpile sampling and geochemical analysis.
Geological mapping of the entire property by a geologist.
Plotting areas for shallow backpack drilling.

Two prospectors for five days.	\$5000
Geologist, mapping, office documentation and sampling.	\$4000
Geochemical analysis.	\$1000
Equipment, tools, supplies, travel and or accommodation.	\$2000
Technical reporting and documentation.	\$3000
Subtotal For Entire Phase Two	\$15,000

Phase Three Details & Budget:

Backpack drilling in areas of mineralization.
Core analysis.
Mapping of drill holes.

Twenty-five days of backpack drilling.	\$37500
Additional supplies, tools, travel, accommodation.	\$7000
Core Logging and core logging supplies.	\$4000
Lab assaying drill core.	\$10000
Geologist site visit, samples, travel	\$2000
Subtotal For Entire Phase Three	\$60,500

Phase Four Details & Budget:

Ground based magnetometer survey.
Data analysis.
43-101 Technical Report.

Magnetometer survey of the entire property.	\$35000
Data analysis reporting.	\$6000
43-101 Technical Report and site visit.	\$12500
Travel, supplies, accommodations.	\$5000
Subtotal For Entire Phase Four	\$58,500

Completion of all phases will cost approximately \$176,000. Allowing for an additional 10% contingency of \$17,600 based on additional work as determined throughout all four phases. All proposed work does not require permitting or significant consultations.

REFERENCES

This is a list of historic reports/property file documents used for reference in the making of this report. Additional services such as Map Place, Minfile and MTO Online were used for mapping.

Assessment Report – 17,256 (Santa Copper Mine - Dave Javorsky) Assessment Report – 19,037 (Geological Report - Santana Mineral Claims - Lonsdale Capital Corp.) Property File – PF011840 (Synopsis – Santana Mineral Claims) Property File – PF520345 (Herbert L Coons, P. Geo. – Geological Report Santana Mines) Property File – PF520348 (Santana Copper Syndicate - Prospectus) Thesis For Master of Arts in Anthropology – University of Victoria (By Volgelaar Colton) (Lidar Map)

Additional Assessment Reports

http://www.empr.gov.bc.ca/Mining/Geoscience/ARIS/Pages/default.aspx

Geological Survey Publications

http://www.empr.gov.bc.ca/Mining/Geoscience/PublicationsCatalogue/Pages/default.aspx

Map Place

http://www.empr.gov.bc.ca/Mining/Geoscience/MapPlace/Pages/default.aspx

Mineral Deposit Profiles

http://www.empr.gov.bc.ca/Mining/Geoscience/MineralDepositProfiles/Pages/default.aspx

MINFILE

http://www.empr.gov.bc.ca/Mining/Geoscience/MINFILE/Pages/default.aspx

Mineral Titles Online

https://www.mtonline.gov.bc.ca/mtov/home.do

STATEMENT OF EXPENDITURES

All exploration and testing took place from August 13th, 2023 – August 17th, 2023. Field supervision was done by Justin Deveault.

Justin Deveault (Prospector)

• August 13, 14, 15, 17

Justin McNutt (Field Assistant)

• August 13, 14, 15

Reporting, mapping, and documentation was completed through November 5 th, 11th, 12th, 13th

Personnel, Travel & Supplies	Days	Rate	Total
Justin Deveault (Supervisor)	3.5 days	\$600/day	\$2,100
Justin McNutt (Prospector)	3 days	\$400/day	\$1,200
Truck, Fuel & Maintenance	722km	\$1/km	\$722
Hotel Accommodations	3 days	\$293	\$879
Meals	3 days	\$150	\$450

Analysis Costs
Portable Field XRF Rental	1 Day	\$550.40/day	\$550.40

Additional Costs
Sample Bags/Tags/Flagging Tape, ect.			\$56.48

Office
Report, Documentation, Mapping	3 Days	\$600/Day	\$1,800

		Total Expenses	\$7757.88

STATEMENT OF QUALIFICATIONS

I Justin Deveault (FMC277308) of 911 Exploration Corp. have practiced my profession for 15 years. I have been employed in the mineral exploration industry.

I have experience working with individuals, companies preforming grassroots mineral exploration throughout British Columbia, primarily Vancouver Island.

I have extensive experience working with highly experienced geologists and other professionals in the mineral exploration industry across British Columbia.

I have studied the geology of Vancouver Island extensively. I have taken several geology and exploration courses.

I am the owner, operator, and supervisor for 911 Exploration Corp.

This report is based on the results general prospecting, sampling, handheld XRF analysis under my supervision and in consult with several geologists.

Date Completed: November 12th, 2023.

Author: Justin Deveault (FMC277308)

Signed: Justin Deveault

Mineral Titles Online

Mineral Claim Exploration and Development Work/Expiry Date Change

Confirmation

Recorder:	DEVEAULT, JUSTIN RON (277308)	Submitter:	DEVEAULT, JUSTIN RON (277308)
Recorded:	2023/AUG/18	Effective:	2023/AUG/18
D/E Date:	2023/AUG/18

Confirmation

If you have not yet submitted your report for this work program, your technical work report is due in 90 days. The Exploration and Development Work/Expiry Date Change event number is required with your report submission. Please attach a copy of this confirmation page to your report. Contact Mineral Titles Branch for more information.

Event Number:	5994120
Work Type: Technical Items:	Technical Work Geochemical, Prospecting
Work Start Date:	2023/AUG/13
Work Stop Date:	2023/AUG/17
Total Value of Work:	\$7759.30
Mine Permit No: