Freegold Expands and Upgrades Resource at Golden Summit

Base case resource ounces and grades have increased materially from our February 2023 estimates
Indicated Primary Mineral Resource: 12.1 million ounces at 1.08 g/t Au, up 8% and 9% respectively
Inferred Primary Mineral Resource: 10.3 million ounces at 1.04 g/t Au, up 45% and 13%, respectively
Primary Resource reported above a 0.50 g/t Au cut-off grade
In addition, a significant oxide resource exists – 0.9Moz at 0.49 g/t Au (indicated), up 43% and 23%
Soil geochem and historical hard rock mines strongly suggest that Dolphin-Cleary mineralization remains open to the west and southwest another 1.5 km. The current resource footprint is 1.5 km east-west.
Dolphin/Cleary is just one of the target areas within the 13km long, road-accessible project.
The 2024 drill program at Golden Summit is ongoing with two drills operating – additional assay results pending

Freegold Ventures Limited (TSX: FVL) (OTCQX: FGOVF) ("Freegold" or the "Company") is pleased to announce an updated mineral resource estimate for the Golden Summit Project. The revised estimate incorporates data from the 2023 drilling program and the initial two holes of the 2024 program, representing a significant milestone in our exploration and development activities.

CutOff Au g/t	Classification	Au g/t	Tonnes	Ounces
OXIDE
0.15	Indicated	0.49	59,414,000	937,000
0.15	Inferred	0.45	3,252,000	47,000
PRIMARY
0.5	Indicated	1.08	346,304,000	12,050,000
0.5	Inferred	1.04	308,311,000	10,306,000
UNDER PIT
0.75	Indicated	1.29	2,867,000	119,000
0.75	Inferred	1.34	22,900,000	986,000

Mineral Resources for the primary resources are reported at a cut-off grade of 0. 5 0 g/t gold and constrained within an open pit shell using a gold price of US$1, 973 /ounce, US$2.50/t mining cost, US$ 14 /t processing cost, US$2.00/t G+A, 72 % gold recover y , and a 45° pit slope. Tonnes and ounces rounded to the nearest thousand.

Comparison Sept 2024 and Feb 2023 Resource Estimates

	Indicated Primary Resource - Open Pit			Inferred Primary Resource - Open Pit			Oxide Indicated
	Moz	gpT	Cutoff Grd	Moz	gpT	Cutoff Grd	Moz	gpT	Cutoff Grd
Feb-23	11.1	0.99	0.5	7.1	0.92	0.5	0.7	0.39	0.15
Sep-24	12.1	1.08	0.5	10.3	1.04	0.5	0.9	0.49	0.15
Change	8 %	9 %		45 %	13 %		43 %	26 %

The updated resource is the result of primarily infill drilling, upgrading areas considered waste in the February 2023 drill program due to lack of drill density. Ounces and grades increased materially in all categories considered within an open pit context. It is expected that further infill drilling may also positively impact stripping ratios when a mine plan is optimized. Freegold's 2024 drill program is focusing on the west and southwest of the existing resource where soil geochemistry, found to be a strong indicator, and historic gold mines have outlined two logical corridors that extend approximately 1.5 km; in context, Golden Summit's current resource occupies a 1.5 km east-west footprint.

The current estimate is based on a gold price of $1,973 , which reflects the three-year trailing average. Even though the 2024 resource estimate uses a higher gold price than the $1,792 in 2023, this is balanced by a lower recovery rate (72% vs. 90%). Previously, the 2023 resource plan considered using CIL (carbon-in-leach) and oxidation to process the sulphide flotation concentrate for higher recoveries. However, positive test results released earlier this year indicate that a significant portion of the mineralization is non-refractory and can be processed using much less costly gravity and CIL. Although the recovery is projected to be lower, the overall operating and capital cost savings would more than compensate and simplify the project substantially. The 72% recovery used for the resource is believed to be conservative. The reported test work showed recovery rates of up to 87.5%, with an average recovery of 77% using gravity and CIL, based on 5,100 kg of material and eight composites. Furthermore, initial indications are that mineralization to the west, where our 2024 drill program is concentrated, achieves higher recoveries. Additional optimization work and metallurgical samples from four large-diameter drill holes completed will be used for further metallurgical testwork.

The latest resource estimate shows an increase in the resource size and a notable improvement in grade. The discovery cost remains exceptionally low at under $4.00 per ounce. Golden Summit has a substantial resource and presents an excellent development opportunity due to its proximity to robust infrastructure - road accessibility, proximity to a supply centre, and available labour force, all of which are expected to contribute to lower operating costs.

Additional drilling will focus on improving the ore quality and outlining a smaller, higher-grade starter pit within the deposit as the project moves towards pre-feasibility to reduce operating and initial capital costs. The updated resource's results demonstrated this approach's success with its increase in overall resource grades at the various cut-offs. Trade-off studies will be conducted to optimize the overall economics and balance improved recovery rates with capital and operating costs as the project progresses. Additional metallurgical work is also in progress, and four large diameter (PQ) boreholes have been drilled this year. These will undergo a comprehensive suite of metallurgical tests to assess various processing methods to improve recoveries and further reduce the project's risks.

Since 2020, Freegold has completed over 123,000 meters of drilling and established Golden Summit as one of North America's largest undeveloped gold resources.

The 2023 drill program at Golden Summit discovered higher-grade mineralization on the western side of the existing resource. In 2024, the plan is to continue drilling on the portion west of the Dolphin/Cleary deposit and extend exploration drilling further to the west. The 2024 drilling program at the Golden Summit project is progressing well; additional assay results are expected to be reported shortly.

The table below displays the specific cut-off grades within and below the current $1,973 pit.

CutOff Au g/t	Classification	Au g/t	Tonnes	Ounces
OXIDE
1.00	Indicated	1.73	4,745,000	265,000
1.00	Inferred	1.77	127,000	7,000
0.75	Indicated	1.35	8,430,000	366,000
0.75	Inferred	1.17	359,000	14,000
0.50	Indicated	0.97	17,324,000	541,000
0.50	Inferred	0.84	919,000	25,000
0.40	Indicated	0.81	24,758,000	647,000
0.40	Inferred	0.72	1,322,000	31,000
0.15	Indicated	0.49	59,414,000	937,000
0.15	Inferred	0.45	3,252,000	47,000
PRIMARY
1.00	Indicated	2.07	99,704,000	6,628,000
1.00	Inferred	2.01	82,640,000	5,352,000
0.75	Indicated	1.55	174,604,000	8,694,000
0.75	Inferred	1.49	151,918,000	7,271,000
0.50	Indicated	1.08	346,304,000	12,050,000
0.50	Inferred	1.04	308,311,000	10,306,000
0.40	Indicated	0.92	461,582,000	13,711,000
0.40	Inferred	0.88	426,343,000	12,003,000
0.15	Indicated	0.66	778,574,000	16,609,000
0.15	Inferred	0.62	752,540,000	14,960,000
UNDER PIT
1.00	Indicated	1.89	1,193,000	73,000
1.00	Inferred	1.82	11,605,000	677,000
0.75	Indicated	1.29	2,867,000	119,000
0.75	Inferred	1.34	22,900,000	986,000
0.50	Indicated	0.84	7,958,000	216,000
0.50	Inferred	0.87	61,179,000	1,720,000
0.40	Indicated	0.66	14,765,000	313,000
0.40	Inferred	0.71	100,288,000	2,282,000
0.15	Indicated	0.35	64,264,000	720,000
0.15	Inferred	0.41	290,423,000	3,826,000

The mineral resource estimate (MRE) was carried out using ordinary kriging of three-meter composites. The MRE was constrained by two lithological domains, Intrusive and Schist, that were further constrained by a 0.2 g/t gold gradeshell. Hard boundaries were used for the Intrusive and Schist domains so that only composites from each domain were used for the estimation of block grades within that domain. An Oxide domain was flagged within the upper portion of the Schist domain after the estimation process. Composite grades in the Intrusive domain were capped at 20 g/t gold and those within the Schist domain were capped at 90 g/t. Cumulative frequency curves were used to determine capping levels. The estimate was carried out in a single pass with a minimum of four and a maximum of 12 composites, with a maximum of two per drill hole, required for a grade to be interpolated into a block. Blocks were classified as Indicated or Inferred. Indicated blocks are based on a minimum of eight and a maximum of 12 composites within 100 meters of a block. Inferred blocks are based on a minimum of four and a maximum of 12 composites within 300 meters of a block. A maximum of two composites per drill hole was permitted in both categories.

In addition to the ongoing drill program, metallurgical, baseline environmental, cultural resource, and wetland studies are underway.

A plan map showing the locations of the 2024 drill holes - exploration and metallurgical holes can be found here:

https://freegoldventures.com/site/assets/files/6287/goldensummit_dolphin-cleary_resource_drilling_western_a.pdf

A sample quality control/quality assurance program has been in place throughout the program. Drill cores were cut in half using a diamond saw, with one-half placed in sealed bags for preparation and subsequent geochemical analysis by ALS Laboratories. Core samples were prepared in ALS's facility using the PREP-31BY package. Each core sample is crushed to better than 70 %, passing a 2 mm (Tyler 9 mesh, US Std. No.10) screen. A split of 1kg is taken and pulverized to better than 85 % passing a 75-micron (Tyler 200 mesh, US Std. No. 200) screen; a portion of this pulverized split is digested by Four Acid and analyzed via ICP-AES (method code ME-ICP61). Fire Assay analyzes all samples with an AAS finish, method code Au-AA23 (30g sample size) and over 10 g/t are automatically assayed using a FA Grav method, Au-GRAV21. Additional Au screening is performed using ALS's Au- SCR24 method; select samples are dry-screened to 100 microns. A duplicate 50g fire assay is conducted on the fine fraction, and an assay is conducted on the entire oversize fraction. Total Au content, individual assays, and weight fractions are reported. Analytical and assay procedures are conducted in ALS's North Vancouver and Reno facilities.

A QA/QC program included laboratory and field standards inserted every ten samples. Blanks are inserted at the start of the submittal, and at least one blank every 25 standards.

Qualified Person and Technical Information

The MRE, with an effective date of September 9, 2024 , was prepared by Tetra Tech Canada. Greg Mosher, P. Geo and Maurie Marks , P.Eng of Tetra Tech Canada are "Qualified Persons" for the Updated Mineral Resource Estimate as defined in NI 43-101 and are considered to be "independent" of Freegold for the purposes of NI 43-101. Greg Mosher and Maurie Marks have reviewed and approved the scientific and technical information herein regarding the Golden Summit project. Greg Mosher visited Golden Summit on November 11 – 12, 2022. Greg Mosher and Maurie Marks visited the project on September 12, 2023 .

The full technical report, which is being prepared in accordance with NI 43-101 by Tetra Tech Canada, will be available on SEDAR ( www.sedarplus.com ) under the Company's issuer profile within 45 days from this news release.

Alvin Jackson, P.Geo, Vice President of Exploration and Development of the Company and a "Qualified Person" as defined in NI 43-101, has supervised the preparation of this news release and has reviewed and approved the scientific and technical information contained herein.

About Freegold Ventures Limited

Freegold is a TSX-listed company focused on exploration in Alaska. Through leases, it holds the Golden Summit Gold Project near Fairbanks and the Shorty Creek Copper-Gold Project near Livengood.

Some statements in this news release contain forward-looking information, including, without limitation, statements as to planned expenditures and exploration programs, potential mineralization and resources, exploration results, the completion of an updated NI 43-101 technical report, and any other future plans. These statements address future events and conditions and, as such, involve known and unknown risks, uncertainties, and other factors which may cause the actual results, performance, or achievements to be materially different from any future results, performance, or achievements expressed or implied by the statements. Such factors include, without limitation, the completion of planned expenditures, the ability to complete exploration programs on schedule, and the success of exploration programs. See Freegold's Annual Information Form for the year ended December 31st, 2023 , filed under Freegold's profile at www.sedar.com , for a detailed discussion of the risk factors associated with Freegold's operations. On January 30, 2020 , the World Health Organization declared the COVID-19 outbreak a global health emergency. Reactions to the spread of COVID-19 continue to lead to, among other things, significant restrictions on travel, business closures, quarantines, and a general reduction in economic activity. While these effects have been reduced in recent months, the continuation and re-introduction of significant restrictions, business disruptions, and related financial impact, and the duration of any such disruptions cannot be reasonably estimated. The risks to Freegold of such public health crises also include employee health and safety risks and a slowdown or temporary suspension of operations in geographic locations impacted by an outbreak. Such public health crises, as well as global geopolitical crises, can result in volatility and disruptions in the supply and demand for various products and services, global supply chains, and financial markets, as well as declining trade and market sentiment and reduced mobility of people, all of which could affect interest rates, credit ratings, credit risk, and inflation. As a result of the COVID-19 outbreak, Freegold has implemented a COVID management program and established a full-service Camp at Golden Summit to attempt to mitigate risks to its employees, contractors, and community. While the extent to which COVID-19 may impact Freegold is uncertain, it is possible that COVID-19 may have a material adverse effect on Freegold's business, results of operations, and financial condition.

SOURCE Freegold Ventures Limited

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Freegold Intersects 4.63 g/t Au over 65.9 Metres at Golden Summit

Freegold Ventures Limited (TSX: FVL) (OCTQX: FGOVF) ("Freegold" or the "Company") is pleased to report initial results from the 2024 drill program. Thirteen holes have been completed, with two more in progress. The 2024 drill program is targeting the western extension as an area that holds significant promise for higher grades closer to surface and at depth. The presence of this higher-grade material, along with promising ongoing metallurgical testwork, can potentially further enhance the overall project economics. The focus for 2024 will be on optimization, which will involve additional drilling, including drilling large-diameter holes (PQ) to facilitate additional metallurgical testwork.

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Eric Sprott Announces Changes to His Holdings in Freegold Ventures Limited

Eric Sprott announces that today, 2176423 Ontario Ltd., a corporation which is beneficially owned by him, purchased 770,000 common shares (Shares) of Freegold Ventures Limited., over the Toronto Stock Exchange (representing approximately 0.2% of the outstanding shares on non-diluted basis) at an average price of approximately $0.53 per share for aggregate consideration of approximately $408,100.

The acquired Shares were purchased in reliance on the normal course purchase exemption from the formal take-over bid requirements set out in Section 4.1 of National Instrument 62-104 - Take-Over Bids and Issuer Bids (NI 62-104). Such Shares do not represent more than 5% of the outstanding Shares, and the aggregate number of Shares acquired in reliance on this exemption with any joint actors within the last 12 months does not exceed 5% of the Shares outstanding at the beginning of the 12-month period. The Shares trade on the Toronto Stock Exchange and the value of the consideration paid for

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Results of the Annual General and Special Meeting

Freegold Ventures Limited (TSX: FVL) (Frankfurt: FR4N) ("Freegold", the Company) today announced that all matters set out in the Management Information Circular dated May 14, 2024 for the 2024 Annual General and Special Meeting of Shareholders held on June 28, 2024 (the "Meeting") were approved by the shareholders holding 101,433,810 shares were voted representing approximately ~ 22.71% of the outstanding shares of the Company.

The following nine nominees were elected as directors of Freegold. The detailed results of the vote for the election of directors are set out below:

Nominee	# of Votes For	% of Votes For	# of Votes Withheld	% of Votes Withheld
Ron Ewing	100,880,186	99.45	553,625	0.55
Kristina Walcott	98,974,508	97.58	2,459,303	2.42
Alvin Jackson	99,068,535	97.67	2,365,276	2.33
David Knight	84,204,358	83.01	17,229,453	16.99
Garnet Dawson	99,597,686	98.19	1,836,125	1.81
Glen Dickson	84,989,006	83.79	16,444,805	16.21
Reagan Glazier	76,043,127	74.97	25,390,684	25.03
Maurice Tagami	99,862,881	98.45	1,570,930	1.55
Vivienne Artz	100,633,536	99.21	800,275	0.79

The Company's shareholders approved the appointment of Davidson & Company LLP, Chartered Professional Accountants, as the company's auditors, as set forth in the management information circular.

The Company's shareholders approved all unallocated stock options, rights or entitlements under the Company's stock option plan.

Each of the matters voted upon at the Meeting is discussed in detail in the Company's Information Circular dated May 14, 2024 , which is filed under the Company's profile at www.sedarplus.com .

Drilling remains ongoing at Golden Summit. Ten holes have been completed to date, and two are currently in progress. Assays will be reported once they are received. The updated resource calculation incorporating the results of the 2023 drilling is expected to be reported in the coming weeks.

Some statements in this news release contain forward-looking information, including without limitation statements as to planned expenditures and exploration programs. These statements address future events and conditions and, as such, involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements to be materially different from any future results, performance or achievements expressed or implied by the statements. Such factors include without limitation the completion of planned expenditures, the ability to complete exploration programs on schedule and the success of exploration programs. See Freegold's Annual Information Form for the year ended December 31st, 2023 filed under Freegold's profile at www.sedar.com for a detailed discussion of the risk factors associated with Freegold's operations.

SOURCE Freegold Ventures Limited

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Freegold Announces Positive Metallurgical Results from Golden Summit

An average gold recovery of 77% from eight composites using conventional processing techniques – gravity and CIL (carbon-in-leach)
97% using gravity + flotation.
A flowsheet of gravity-flotation-CIL on reground concentrate yields 72% gold recovery along with a high mass desulfurized tailings stream
Further optimization studies are underway.

Freegold Ventures Limited (TSX: FVL) (OCTQX: FGOVF) ("Freegold" or the "Company") is pleased to announce positive results based on the initial metallurgical test work completed from the 2020 2022 drill program. The program's objectives were:

Determination of gold recovery and gold deportment to products using standard and commercially employed mineral processing unit operations
Initial environmental assessment of process tailing stream(s)
Characterization of gold losses to focus ongoing metallurgical programs to optimize the flowsheet design.

Eight drill core composites representing various locations and grades within the Dolphin/Cleary areas were generated using continuous drill intervals selected to represent potential mill feed. ( See map below for hole locations. ) The drill hole and interval selections encompassed the three primary gold-hosting lithologies. Results demonstrate that a significant portion of the mineralization is non-refractory and amenable to conventional processing techniques. The composites were prepared using laboratory assay rejects of fresh rock intervals well below the existing oxide cap at Golden Summit. The eight drill hole composites used 1,192m of drill intercepts representing 587 continuous mineralized intervals with over 5,100kg of material. Results from individual holes demonstrate recoveries up to 87.5%. The average recovery from the eight composites was 77% using gravity and CIL. Recoveries increased to an average of 97.5% where gravity + flotation were utilized. Environmental characterization using standard ABA protocols gave a NP:AP ratio of 85:1 on the flotation tailings stream, which would classify them as non-acid generating.

Metallurgical Composite Hole Results

DDH no.	from m	to m	geochem	test calc grade	gold recovery %
					grav/flot/regr CIL	grav/CIL	gravity	grav+flot
			Au g/t	Au g/t

GS2201	441.1	648.3	1.44	1.06	88.2	87.1	45.0	99.2

GS2203	287.8	478	2.13	2.24	75.1	77.2	48.2	97.6

GS2206	383.1	586.1	1.17	1.02	80.2	87.5	42.7	97.3

GS2207	261.9	468.7	1.35	1.78	60.1	70.2	37.8	98.1

GS2208	266.3	367.2	1.33	1.48	48.1	53.3	25.3	97.5

GS2209	419	544.5	1.26	1.54	73.6	81.2	50.7	97.0

GS2168	352.7	479.5	0.75	0.83	63.7	73.2	31.1	94.3

GS2167	396.3	428	2.15	1.01	71.7	69.2	49.5	96.3

overall predicted grade			1.43

overall calc grade/recovery from test work				1.43	72	77	42	97

The drilling success at Golden Summit since 2020 has been truly remarkable. It has significantly increased the resource and enhanced the project's potential. These positive metallurgical results further solidify Golden Summit's potential. The current pit-constrained resource at Golden Summit hosts both an oxide and a primary resource. The oxide resource is contained within the top 70% metres. Previous column testwork on the oxide material demonstrated that heap leach gold recoveries of 85% can be achieved within two weeks.

Pit Constrained OXIDE Resource using $1,792 Gold

Cutoff Au g/t	Category	Tonnes	Au g/t	Au Ounces
0.15	Indicated	52,030,000	0.39	657,000
0.15	Inferred	18,187,000	0.47	272,000

(approximately top 70 metres)

Pit Constrained PRIMARY Resource using $1,792 Gold: ( February 2023 )

Cutoff Au g/t	Category	Tonnes	Au g/t	Au Ounces
0.45	Indicated	407,544,000	0.92	12,011,000
0.45	Inferred	282,303,000	0.85	7,736,000

Following the February 2023 resource update, Freegold conducted an additional 22,000 meters of drilling in 37 holes within the resource area. A significant increase in visible gold was observed in the drill core compared to previous programs, particularly in the western part of the resource. An updated mineral resource report based on the 2023 drilling is expected later this month. The success of the 2023 drilling program has set the stage for an even more exciting 2024 program. The upcoming phase will focus on optimization, testing the 2km gold-in-soil geochemical anomaly to the west, drilling large diameter (PQ) holes to guide further and optimize metallurgical recoveries, and modelling before economic studies commence. Freegold has postponed the economic studies to investigate the potential for higher grades in the western extension and to conduct additional metallurgical test work, as both could significantly impact the project's economics. The primary areas of focus in the next phase of metallurgical test work are:

Comminution studies using half PQ core
Flotation concentrate oxidation pre-treatment prior to CIL

Map Showing Location of Metallurgical Composite Holes and 2024 Drilling

https://freegoldventures.com/site/assets/files/6287/goldensummit_dolphin-cleary_resource_drilling_western_a.jpg

The Qualified Person for this release is Alvin Jackson , P.Geo., Vice President of Exploration and Development for Freegold, who has approved the scientific and technical disclosure in this news release.

About Freegold Ventures Limited

Freegold is a TSX-listed company focused on exploration in Alaska . It holds the Golden Summit Gold Project near Fairbanks and the Shorty Creek Copper-Gold Project near Livengood through leases.

SOURCE Freegold Ventures Limited

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Lode Gold Identifies New High Priority RIRGS Target ''Steelhead'' at WIN, Tombstone Belt - Yukon

Lode Gold Resources Inc. (TSXV: LOD) (OTCQB: SBMIF) ("Lode Gold " or the "Company") is pleased to announce that it has received and interpreted the data from the previously announced QMAGT survey conducted in summer, 2024. This news release focuses on presenting initial findings, including reporting the identification of a new high-priority target named "Steelhead" extending the emerging Reduced Intrusion Related Gold System (RIRGS) targets already identified on its WIN property. A future news release will expand on these new findings northwards to include Lode's flagship Golden Culvert property as our geological team evaluates a potential genetic relationship, highlighted by the new QMAGT data between the RIRGS mineralization at WIN and the orogenic styles of mineralization present at Golden Culvert.

Highlights include:

Recent QMAG^T system geophysical results integrated with geology and historic geochemical information has identified a new priority prospect, "Steelhead", a previously unrecognized 4km² area of hornfels on the eastern part of the property.
''Steelhead's" prospectivity is enhanced by the presence of anomalous gold and bismuth results in stream sediment samples collected from the catchment draining the new identified 4km² area of hornfels.
The QMAG^T system has successfully enhanced the detailed geology of the property and importantly mapped the targeted Tombstone-Tungsten Cretaceous aged monzonite intrusions as magnetic lows and related hornfels known to be prospective for RIRGS as magnetic highs or areas with "noisy magnetic gradients".
The above adds to the initial 2023 discovery of a RIRGS style sheeted vein system with gold values up to 8.3 g/t coincident with elevated bismuth and tellurium (see news release dated December 13, 2023) hosted in hornfels on the western side of the property and named the "Border Gold Zone".
The Border Gold Zone appears to be controlled by the Border Monzonite and manifests as a "roof zone" above this intrusive and the host Cordierite-Biotite bearing hornfels. The magnetic data clearly defines a 3.5km strike extension to this known mineralized hornfels zone for targeted follow up.
Furthermore, the magnetic data defines deep structures both parallel and coincident with the known mineralization and are thought to be important controlling structures for gold emplacement.

Buddy Doyle, VP Exploration commented that, "Lode Gold has leveraged the quality QMAG^T data to integrate the pre-existing geochemical and geological-structural data on hand to design a targeted ground follow-up program to rapidly generate drill targets on the emerging high-potential RIRGS Targets at WIN, adding materially to its established flagship Orogenic Golden Culvert targets within the large, strategic property package controlled by Lode in the Yukon."

Regional Setting, The RIRGS Model and How Well the WIN Project Fits

The WIN property occurs in the southern portion of the prolific Tombstone gold belt, see Figure 1. The Tombstone Gold Belt is the type locality for RIRGS, with Figure 2 depicting the accepted model for this type of gold mineralization.

Figure 1: The Tombstone Gold Belt, yellow shaded zone, gold stars show RIRGS deposits and prospects, orange stars tungsten deposits, The black star depicts the location of our WIN project. All are related to mid-cretaceous Intrusive suites and their associated contact hornfels aureoles. Figure modified from the Yukon geological survey broacher 2006-6.

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/4064/226527_f5046f6914111af4_004full.jpg

Figure 2:The RIRGS geological model, General plan model of RIRGS (left), note the wide range of mineralization styles and geochemical variations that vary predictably outward from a central pluton. Scale is dependent on the size of the exposed pluton, which is likely to range from 100 m to 5 km in diameter. Hypothetical cross-section (right) of a small (100 m-5 km across) pluton. Of note are the asymmetric hornfels aureole and the early-chilled and more brittle marginal carapace. Preferred sites of intrusion-hosted Au mineralization are above the cupola, where exsolved fluids will accumulate, and mineralized fractures developed in the pluton's apex and shoulders. Modified from Hart, C.J.R., 2007.

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/4064/226527_figure2.jpg

The RIRGS geological model in summary makes the following empirical observations:

Mineralization is associated with a reduced intrusion with the mineralization extending beyond the limits of the intrusion, and locally beyond the thermal aureole (caused by the intrusion), yielding a broad mineralizing system (Fig. 2). The size of the system is generally dictated by the limits of the thermal aureole, commonly several kilometres across, but can be dependent on the depth of erosion with the broadest and best-developed mineralization at the top of or above the pluton. The WIN project contains the known mapped intrusives, the northern part of the Hyland intrusive and the eastern part of the Border Intrusive (see Figure 4) both have extensive hornfels aureoles developed. The known sheeted quartz vein mineralization is hosted in hornfels.

A common characteristic is that the RIRGS exhibits multiple styles of mineralization. Particularly in the thermal aureole. Chemically reactive and/or physically brittle sedimentary strata result in a diversity of mineralization styles, whereas the causative pluton is typically dominated by solely sheeted vein sets containing gold. The WIN project Hyland Intrusive has been subject to exploration for Tungsten and Molybdenum in the past with part of the Tuna Tungsten Mineral occurrence within and next to the property's southern border. The sheeted quartz veins with gold have been found in the roof hornfels.

RIRGS often exhibit a predictable zonation of differing deposit styles outward from the central, mineralizing pluton (Fig. 2). Skarns and replacements are generally pluton proximal, with an increase in structural control on more distal mineralization. There is also crustal scale vertical zonation, with epizonal occurrences forming at shallower levels. Predictable metal signatures develop broad-scale zoning surrounding and above a central causative pluton. The stream, soil and rock samples taken by Lode Gold show metal zonation.
Gold, as well as Tungsten (W), may form ore, but Au does not directly correlate with W. Bismuth (Bi) and Tellurium (Te) are enriched in intrusion-hosted Au ores and correlate with Au. Arsenic enrichments characterize hornfels-hosted mineralization and form regional-scale geochemical anomalies. On the WIN project, the sheeted veins have gold correlating strongly with Bi and Te. The WIN and Golden Culvert projects occur in a regional zone of anomalous Arsenic in stream sediments (see Figure 5).

Each plutonic suite has a characteristic metallogenic association. Plutons of the Tombstone plutonic suite have alkalic compositions (syenites) and associated gold, bismuth and copper. Plutons of the Mayo suite have metalluminous compositions (hornblende monzonites) and the strongest gold association. Plutons of the Tungsten suite are slightly peraluminous (biotite granite) and are associated with tungsten ± copper, zinc and molybdenum mineralization. Mineralized plutons typically have associated pegmatites, aplites, miarolitic cavities and tourmaline veins, which are all indicative of volatile saturation and development of hydrothermal phases. The WIN project covers part of the Hyland and Border intrusive, both are mapped as Hornblende monzonites, the type of intrusion that has the strongest gold association. Tourmaline veins and breccias have been noted in the Tuna mineral occurrences, within and south of the property.

Traditional exploration methods such as mapping, prospecting, and aeromagnetic, regional stream sediment and soil geochemical surveys are all effective. Since mineralization is typically focused in regions at the top of plutons, target areas should include locations where plutons are not exposed. These may be detected by aeromagnetic surveys that may respond to either pyrrhotite-rich hornfels, or low levels of magnetite in the case of the Tombstone suite alkalic intrusions. Summarized and modified from Hart, C.J.R., 2007.

District Geology

Figure 3: District Geology: Lode Gold's Golden Culvert and WIN projects depicted on the regional geology provided by the Yukon Geological Survey. Note the WIN Project is dominated by the Proterozoic Vampire formation intruded by Cretaceous monzonites. Mineral occurrences from the Yukon database are also shown. The WIN property contains the Hyland and Border Intrusive bodies, these bodies are depicted in the following figures for visual reference. They are the likely source of the mineralization.

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Figure 4:Regional Arsenic in stream sediment anomaly encompasses Lode Gold's Golden Culvert and WIN properties. A characteristic signature of RIRGS. After Hart, C.J.R. and Lewis, L.L., 2006

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Figure 1 shows the regional geological setting with a belt of intrusions (the Selwyn Magmatic province) intruding the Proterozoic-aged Selwyn sedimentary basin. Figure 3 illustrates the district geology with both the Golden Culvert property and the WIN property being hosted in the Vampire Formation, the WIN property covers portions of the Hyland and Border monzonite intrusives. Figure 4 demonstrates the projects that occur in a regional arsenic anomaly a common feature of sub-districts with RIRGS within the Tombstone gold belt. Known mineral occurrences are also shown in Figure 4, with the most advanced being the 3 Aces orogenic gold deposit, 15km to the SSW of the WIN project being explored by Seabridge Gold. Aben Minerals have also identified RIRGS style mineralization 18km to the SSW. The nearest historic mineral occurrence to the WIN project is the Tuna prospect, which consists of several zones of veins and breccias with Quartz, Bi, Tungsten, Molybdenum with tourmaline on the south boundary.

Rock Samples Confirmed RIRGS

On December 13, 2023, Lode Gold announced that it had confirmed a RIRGS style mineralization on its WIN property. Rocks samples returned gold values up to 8.53 g/t. with associated bismuth and tellurium at the border gold zone, shown in Figure 5. The mineralization is hosted in sheeted quartz veins, up to 10 veins per metre. The mineralization is hosted in hornfels. Figure 6 shows a photograph of the sheeted quartz veins and a view of the general topography at the border zone sampling area.

Figure 5:Rock sampling sites on the WIN Property. Each dot is a separate sample site, dots are coloured and sized based on gold results, Legends are given in the inset. Colour intervals based on natural breaks. Base image is the 2m Digital Elevation Model (DEM). Blue zone are permanent ice sheets. Monzonite intrusions shown as transparent red stipple. The local geology map shown in figure 7 cover the area surrounded by yellow line.

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Figure 6: Photograph of the sheeted vein system left, photograph of the topography in the border area, sheeted veins near photo origin looking SW towards the Hyland Intrusion. Photo on the right from Moynihan, D.P., 2013

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Geology of the Border Gold-Bearing Sheeted Vein Area

Figure 7: Map of parts of the Hyland and Boundary plutons and their contact aureoles, showing mineral assemblages and isograds. Structural measurements are compiled on the equal area, lower hemisphere stereonet (inset). Grid lines spaced at 1 km intervals; UTM coordinates are NAD 83. Lode Gold rock sample results shown. Map is shown in Figure 5 and coincides with the inset box on that figure.

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The Yukon Geological Survey conducted mapping on the eastern side of the WIN project, see covering the Border Gold Zone, Moynihan, D.P., 2013. Their mapping has been reproduced in Figure 7 with our rock sample gold results overlain. The Hyland and Boundary plutons are hosted by the Latest Proterozoic-Early Cambrian Vampire Formation. The Vampire Formation is dominated by uniform, steel grey to dark grey phyllite that weathers to a rusty brown. The Vampire formation has been altered to hornfels along the contacts with the Hyland and Border monzonite intrusions.

The dominant foliation in the area (S_n) strikes NW/SE, parallel to the orogenic trend, it generally dips NE at 40-70° in the southwest part of the area and dips steeply towards the SW or NE in the northeast part of the area. The sheeted veins located by our field crew appear to be controlled by this S_nstructural direction with a similar strike and dip.

S_n is locally overprinted by kink bands that have steeply dipping axial planes. These kink bands post-date development of the contact aureoles and are best developed in low-grade phyllites, which retain a well-defined cleavage. The Hyland pluton-Vampire Fm contact is offset by a number of steeply-dipping, SW-trending normal faults with downthrow to the NW. These faults are sub-parallel to axial planes of the kink bands, and have the same orientation as 1) a number of fine-grained, biotite and amphibole-bearing mafic dikes, and 2) an array of quartz- tourmaline veins that transect the Boundary aureole. Tourmaline is a common accessory mineral to RIRGS sheeted quartz veins and to our knowledge, the NE/SW trending quartz vein array is yet to be sampled.

The Hyland pluton, which was emplaced at 97.1±2.0 Ma (U-Pb monazite age), is elongated in a NW direction and underlies an area of approximately 9×2.5 km. The roof of the pluton is preserved around the topographically highest point near the centre of the intrusion. The southwest boundary of the pluton dips steeply, whereas its northeast and southeast boundaries have gentle to moderately steep outward dips. It is along this moderately dipping NE part of the pluton that our border gold zone is located. The pluton is a multi-phase, biotite quartz monzonite with a megacrystic internal phase and an equigranular outer phase. The contact aureole includes a phyllite outer part and a yellow-weathering, hornfelsic inner part. With increasing proximity to the Hyland pluton, the proportion of chlorite decreases to zero and cordierite, andalusite, and biotite crystals become larger and more abundant. This zonation is approximately 500m wide and parallels the outcropping boundary of the Hyland intrusion. The presence of andalusite suggest a deep emplacement level (circa 9-11 km) for the Hyland intrusion based on geobarometer calculations. Moynihan, D.P., 2013.

An extensive region of Crd+Bt hornfels is also developed in the area to the west of the Boundary pluton. It is notable that here Cordierite (Crd) is dominant and Andalusite is absent. This indicates a shallower emplacement level for the Border pluton which in turn suggests a younger age. The pattern of Crd+Bt hornfels suggests that the Boundary pluton extends underneath this region to the NW paralleling the border. It is here that our Border Zone gold bearing sheeted quartz veins occur. The suggestion is that the Boundary pluton was intruded at a slightly higher level than the Hyland pluton. The absence of andalusite from metapelite in the aureole of the Boundary pluton suggests it was intruded at

It is likely that the Border zone sheeted veins are genetically linked to the Border Pluton in the Cordierite-Biotite-Chlorite-Muscovite-Quartz hornfels that trend paralleling the border, with the higher-grade samples occurring on the edge of the higher temperature Cordierite-Biotite-Muscovite-Quartz hornfels where the Chlorite drops out.

Stream Sediment Sampling

Figure 8:Stream Sediment sampling sites on the WIN Property. Each dot is a separate sample site, dots are coloured and sized based on gold results, left image 8 (a), and by bismuth right image 8 (b). Legends given in insets. Colour intervals based on natural breaks. Base image is the 2m Digital Elevation Model (DEM). Blue zone are permanent ice sheets. Monzonite intrusions shown as transparent red stipple.

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A series of closed space stream sediment samples were taken on the WIN project with the results depicted in Figure 8a for gold and for bismuth in Figure 8b. There are two strong gold anomalies (>45ppb) in separate streams, one stream eventually drains the Border gold zone, and the other highlights an area mainly hosted in the Hyland Intrusive and its contact aureole near its NE edge. This drainage also has high Bismuth and has never been investigated by soil or rock sampling. The area has been given the name of the Steelhead Prospect (using the naming theme started by the Tuna mineral occurrence.).

The entire Hyland Intrusive is elevated in Bi, As, Sb, W, Pb, Zn. Only Bi is shown. The stronger Bi stream sediment anomalies (>8.4ppm red, purple) need further follow-up due to their strong correlation with gold in the RIRGS model.

Soil Sampling

Figure 9: Soil Sampling sites on the WIN Property. Each dot is a separate sample site, dots are coloured and sized based on gold results. Legends given in inset. Colour intervals are natural breaks based on entire dataset which includes Golden Culvert, the number of samples in class in brackets. Base image is the 2m Digital Elevation Model (DEM). Blue zones are permanent ice sheets. Monzonite intrusions shown as transparent red stipple.

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Soil sampling on the WIN property have in the past been restricted due to the mountainous topography and the glaciated surfaces that are either rock or transported moraine. A small grid over the border zone contains anomalous samples with a zone of >20ppb gold stretching 300m over 3 lines paralleling the border. The project would be amenable for further sampling.

QMAG^T Survey

The RIRGS model makes the observation that aeromagnetic surveys are an effective exploration tool. The QMAG^Tsurvey conducted over the WIN property is a relatively new system which utilizes a Super-conducting Quantum interference device (SQUID) magnetometer which measures the full tensor response of the earth's magnetic field. The system is flown beneath the Helicopter in a Dewar filled within a liquid helium super cold bath. The WIN property was flown at a one-hundred-meter line spacing with lines trending NE-SW perpendicular to the geological trend. DIAS, the company that operates the QMAG^T system, have provided the following products derived from this survey:

Bxx delineates E-W boundaries preferentially (symmetric for vertical magnetisation, antisymmetric for horizontal magnetisation)
Byy delineates N-S boundaries preferentially (symmetric for vertical magnetisation, antisymmetric for horizontal magnetisation)
Bxy delineates body corners preferentially (anomaly signs depend on magnetisation direction)
Bzz delineates steep boundaries preferentially (symmetric for vertical magnetisation, antisymmetric for horizontal magnetisation)
Bxz delineates E-W boundaries preferentially (antisymmetric for vertical magnetisation; symmetric for N-S horizontal magnetisation)
Byz delineates N-S boundaries preferentially (antisymmetric for vertical magnetisation; symmetric for E-W horizontal magnetisation)
I1 highlights deeper and/or large, smoother magnetic sources
I2 highlights shallow and/or small, complex magnetic sources
THC - Total Horizontal Curvature highlights areas of high curvature in the magnetic field that may be associated as being close to a strong source or a curving geometric feature
THG - Total Horizontal Gradient highlights areas of high gradient independent of direction and can be useful in edge detection.
Total field ( a cesium magnetometer was also flown along with the SQUID device to give this product)

This product suite was interrogated with the geochemical results discussed above and the known geology to form an interpretation map and future exploration guide.

QMAG^T Interpretation

Interpretation of the QMAG^T dataset has confirmed its utility in mapping geology and highlighting structure. Figure 10 shows the total magnetic field. The Hyland and Border intrusions stand out as magnetic lows (blue colours) with low gradients (smooth surfaces) as expected for reduced intrusions containing no magnetite. The hornfels zone between the two intrusives is highlighted in the magnetic response and textures. The chlorite out higher temperature hornfels that host the Border Gold zone, can be seen as a magnetic high parallel to the territorial border. The contact hornfels around the Hyland intrusion shows a more subdued magnetic response but have a distinct magnetic texture, some of which appears structurally controlled, with the same NE-SW trend of structures and quartz-tourmaline veins noted in the mapping. Also highlighted is a distinct zone of magnetic highs on the western boundary of the Hyland Monzonite, these require field investigations and a thought to be hornfels similar to those hosting the Border gold zone on the eastern boundary of the Border intrusive.

Figure 10:Total Field magnetic response colour grid. Mapped extent of the Hyland and Border Monzonite shown in red stipple. The intrusions are expressed as magnetitic lows reflecting their reduced nature, and lack of magnetite. Strong, red magnetic responses interpreted to highlight hornfels (mapped as Cordierite-Biotite Hornfels), grey shaded area less magnetic zone of hornfels, but they exhibit a similar magnetic texture some with clear structural control.

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Figure 11: Bzz vertical tensor component. Left image Figure 11a is gridded colour image of the Bzz, right image Figure 11b same image with structural interpretation overlain with black lines

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Figure 11 depicts the vertical tensor of the magnetic field Bzz, this product and the other direction tensors were used to make a structural interpretation shown in Figure 11b. The generally SW-NW structure picked up in the Border Gold zone mapping appears to be property-wide. The geophysical product that picked up the NW-SE regional S₀ structural fabric and the strike direction of the sheeted veins measured in the Border gold Zone was the LI map, said to be best for picking up deeper magnetic sources, shown below in Figure 12. It is probable that these are the structures controlling the sheeted veins and thus can be used to guide further exploration.

Figure 12: The LI product Greyscale coloured grid left Figure 12a and interpreted structures on the right Figure 12b. This geophysical product picks up the NW structural fabric that controls the known sheeted gold-bearing quartz veins.

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Future Plans

By combining our historic geochemical data, with geological mapping and the QMAG^T products a clear exploration plan for the 2025 field season emerges. The highest priority is the Border Gold zone where we have already identified gold-bearing sheet quartz veins striking NW-SE. This mineralization is hosted in Cordierite-biotite hornfels that parallel the western boundary of the Border monzonite. The mapped outline of these hornfels coincides with a distinct magnetic high that the QMAG^T survey demonstrates these rocks continue to the NW and SW past the area of government mapping and Lode Gold sampling. Further rock and soil samples along this trend are a high priority.

Gold mineralization also appears to be associated with the eastern boundary of the Hyland Monzonite, here stream sediment sampling shows anomalous gold and bismuth in streams draining the area. This zone has been named the Steelhead Prospect. Government mapping records SW-NE trending quartz-tourmaline veins in this area and relocating and sampling these and determining the source of the stream geochemical anomaly is a priority.

The QMAG^T system mapped a previously unknown zone of hornfels on the western side of the Hyland Pluton, given the geochemical anomalous nature of the intrusion, high in Bi, W, As, Zn, Pb and Mo this western hornfels zone might host RIRGS, the area has not seen any historic exploration focus. Putting field teams out to map and sample this zone is also planned for 2025.

Director and Technical Committee Chair, Jonathan Hill comments, "We are pleased to see a strong confirmation of Reduced Intrusion Related Gold System (RIRGS) at WIN property. With the mapping and geophysical survey data from this work, we can delineate and generate high-potential drilling targets for 2025."

ABOUT LODE GOLD

Lode Gold (TSXV: LOD) is an exploration and development company with projects in highly prospective and safe mining jurisdictions in Canada and the United States.

Our Golden Culvert and WIN Projects in the Yukon, cover 99.5 km2, are situated in the southern portion of the Tombstone Gold Belt. This 1500km long belt is dominated by RRIGS and sediment hosted Gold deposits, including Fort Knox, Brewery Creek, Keno Hill (Silver), Dublin Gulch, Hecla and Snowline's Gold's recent world class, Valley discovery. The company has intersected gold mineralization on the Golden Culvert property, with a best result of 33.1m @ 12.53 g/t from one of our drill holes and has identified a gold bearing sheeted vein system (RRIGS) on the WIN property.

In New Brunswick, within the emerging Appalachian/ Iapetus gold belt, Lode Gold has formed a strategic Joint Venture with Fancamp called Acadian Gold together we form one of the largest land packages in New Brunswick with 420km2 of exploration rights between McIntyre Brook and Riley Brook projects. Jointly focused on the Wapske Formation a geological unit identified to have the best gold potential in particular where there are structures bounding felsic units. With 36km strike of the Wapske formation under control Acadian is a key and leading member of this play.

Our 111 km2, McIntyre Brook Project, is surrounded by Puma Exploration's Williams Brook Project (where their Lynx project has reported 5.55 g/t Au over 50m)¹ The first 2 drill holes completed by Lode Gold intersected (one hole intersected 5.73 g/t gold over 2.0 m within a broader low-grade interval averaging 1.20 g/t gold over 20 m), further drilling is warranted. Fancamp's 309 km2 Riley Brook project covers 25 km strike of Wapske formation containing numerous mapped felsic units. Previous exploration efforts were directed at VMS-style mineralization focused on the base metals often not assaying for gold. :– Acadian is the first to focus on gold.

NI 43-101 reports on our New Brunswick and Yukon projects are available on Sedar+ and on our website

The Company is also advancing its Fremont Gold development project in the historic Mother Lode Gold Belt of California where 50,000,000 oz of gold has been produced. Fremont, located 500km north of Equinox Gold's Castle Mountain and Mesquite mines, has a Preliminary Economic Assessment(" PEA") with an after-tax NPV (5%) of USD $217M, a 21% IRR, 11-year LOM, averaging 118,000 Oz per annum at USD $1,750 gold. A sensitivity to the March 31, 2023 PEA at USD $2,000/oz gold gives an after-tax NPV (5%) of USD $370M and a 31% IRR over an 11-year LOM. The project hosts an NI 43-101 resource of 1.16 MOz at 1.90 g/t Au within 19.0 MT Indicated and 2.02 MOz at 2.22 g/t Au within 28.3 MT Inferred. The MRE evaluates only 1.4 km of the 4 km strike length of the Fremont property which features five gold-mineralized zones. Significantly, three step-out holes at depth hit the mineralized structure, typical of orogenic deposits that often occur at depth. Fremont is located on 3,351 acres of 100% owned private land in Mariposa, the original gold rush county, and is 1.5 hours from Fresno, California.

The property has year-round road access and is close to airports and rail. A planned V-TEM airborne geophysical survey to be flown over both properties.

Please refer to the Fremont Gold project NI 43-101 PEA technical report dated March 31, 2023, which is available on the Company's profile on SEDAR+ (www.sedarplus.ca) and on the Company's website (www.lode-gold.com). The PEA technical report has been reviewed and approved by independent "Qualified Persons" Eugene Puritch, P.Eng., FEC, CET, and Andrew Bradfield, P.Eng. both of P&E, and Travis Manning, P.E. of KCA.

QUALIFIED PERSON STATEMENT

The scientific and technical information contained in this press release has been reviewed and approved by Jonathan Victor Hill, Director, BSc (Hons) (Economic Geology - UCT), FAusIMM, and who is a "qualified person" as defined by NI-43-101.

ON BEHALF OF THE COMPANY

Wendy T. Chan, CEO & Director

Information Contact

Winfield Ding
CFO
info@lode-gold.com
+1-416-320-4388

Kevin Shum
Investor Relations
kevin@lode-gold.com
+1 (647) 725-3888 ext. 702

REFERENCES CITED

Hart, C.J.R., 2007, Reduced intrusion-related gold systems, in Goodfellow, W.D., ed., Mineral deposits of Canada: A Synthesis of Major Deposit Types, Dis- trict Metallogeny, the Evolution of Geological Provinces, and Exploration Methods: Geological Association of Canada, Mineral Deposits Division, Special Publication No. 5, p. 95-112.

Moynihan, D.P., 2013. A preliminary assessment of low pressure, amphibolite-facies metamorphism in the upper Hyland River area (NTS 105H), southeast Yukon. In: Yukon Exploration and Geology 2012, K.E. MacFarlane, M.G. Nordling, and P.J. Sack (eds.), Yukon Geological Survey, p. 99-114.

Hart, C.J.R. and Lewis, L.L., 2006. Gold mineralization in the upper Hyland River area: A non- magmatic origin. In: Yukon Exploration and Geology 2005, D.S. Emond, G.D. Bradshaw, L.L. Lewis and L.H. Weston (eds.), Yukon Geological Survey, p. 109-125.

Cautionary Note Related to this News Release and Figures

This news release contains information about adjacent properties on which the Company has no right to explore or mine. Readers are cautioned that mineral deposits on adjacent properties are not indicative of mineral deposits on the Company's properties.

Cautionary Statement Regarding Forward-Looking Information

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

This news release includes "forward-looking statements" and "forward-looking information" within the meaning of Canadian securities legislation. All statements included in this news release, other than statements of historical fact, are forward-looking statements including, without limitation, statements with respect to the use of proceeds, advancement and completion of resource calculation, feasibility studies, and exploration plans and targets. Forward-looking statements include predictions, projections and forecasts and are often, but not always, identified by the use of words such as "anticipate", "believe", "plan", "estimate", "expect", "potential", "target", "budget" and "intend" and statements that an event or result "may", "will", "should", "could" or "might" occur or be achieved and other similar expressions and includes the negatives thereof.

Forward-looking statements are based on a number of assumptions and estimates that, while considered reasonable by management based on the business and markets in which the Company operates, are inherently subject to significant operational, economic, and competitive uncertainties, risks and contingencies. These include assumptions regarding, among other things: the status of community relations and the security situation on site; general business and economic conditions; the availability of additional exploration and mineral project financing; the supply and demand for, inventories of, and the level and volatility of the prices of metals; relationships with strategic partners; the timing and receipt of governmental permits and approvals; the timing and receipt of community and landowner approvals; changes in regulations; political factors; the accuracy of the Company's interpretation of drill results; the geology, grade and continuity of the Company's mineral deposits; the availability of equipment, skilled labour and services needed for the exploration and development of mineral properties; currency fluctuations; and impact of the COVID-19 pandemic.

There can be no assurance that forward-looking statements will prove to be accurate and actual results, and future events could differ materially from those anticipated in such statements. Important factors that could cause actual results to differ materially from the Company's expectations include a deterioration of security on site or actions by the local community that inhibits access and/or the ability to productively work on site, actual exploration results, interpretation of metallurgical characteristics of the mineralization, changes in project parameters as plans continue to be refined, future metal prices, availability of capital and financing on acceptable terms, general economic, market or business conditions, uninsured risks, regulatory changes, delays or inability to receive required approvals, unknown impact related to potential business disruptions stemming from the COVID-19 outbreak, or another infectious illness, and other exploration or other risks detailed herein and from time to time in the filings made by the Company with securities regulators, including those described under the heading "Risks and Uncertainties" in the Company's most recently filed MD&A. The Company does not undertake to update or revise any forward-looking statements, except in accordance with applicable law.

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RUA GOLD's Drill Program Intersects near Surface Gold at the Reefton Project

Rua Gold Inc. (TSXV: RUA) (OTCQB: NZAUF) (WKN: A4010V) ("Rua Gold" or the "Company") is pleased to provide an update from the drilling campaign underway at the Reefton Project on the South Island of New Zealand.

The Company commenced its near mine drill program on the Murray Creek targets in July. A second drill rig was introduced in September to test the Capleston vein system. These historic mines collectively produced ~700koz of gold at 25.2g/t within a radius of ~20 kilometers.

Robert Eckford, CEO of Rua Gold commented: "Our five years of meticulous surface exploration work over the Reefton project is paying dividends from the outset of this drill program. Both of the initial drill holes have confirmed we are in right area and are locating these lodes. The near surface intercepts on Capleston are encouraging and makes for compelling economic ounces, it supports our thesis that the surface veins are continuous past the old workings. Despite the initial drill hole at Murray Creek hitting old workings, it is extremely encouraging that we have identified the dip angle of the Victoria lode and we have even more confidence with the subsequent hole that is underway now, and results from this will be ready in the next few weeks."

Capleston

On the second drill rig, which was introduced to test the Capleston vein system, the Company targeted an undeveloped and near-surface vein at the southern end of the two kilometer long historic Capleston project, the highest-grade producer of the Reefton Goldfield historically. Near surface targets lend themselves to early development and are the closest to transportation and infrastructure, providing low-cost operational advantages.

The first diamond drill hole, DD_REF_043, intersected a 12m zone of quartz-pyrite-arsenopyrite in the hanging wall, with a 1m quartz vein from 31m to 32m @ 3.86 g.t Au.

A legacy drill hole intercepted the southern lode at 33m downhole, with 1m @ 24g/t Au followed by 1m @ 2.5g/t Au¹. Mapping has recorded historical waste samples up to 32.0g/t Au in the vicinity¹, and a strong soil anomaly enveloping the vein (up to 410ppb Au).

Figure 1: Capleston Section DD_REF_043, drill intersection and core highlighted

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Murray Creek

Rua Gold reports the completion of the first hole testing the down-dip extension of the Victoria lode, DD_VIC_041, which is being evaluated by the team. This intersected the targeted reef at 344m down hole and encountered historical underground workings over a 4m length. It then exited out to the footwall before drilling on for an additional 20m.

This confirms that the lode extension is accurate and, with the precise location confirmed, a second hole is underway that is 50m deeper down dip from the initial drill hole. The Company anticipates an intersection into an un-mined portion of the reef at around 350m. Results from this testing will be available in the coming weeks.

Figure 2: Cross section through the first Murray Creek drill target, Victoria

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Background

Capleston Group historical production 134,927 oz @ 49.1 g/t Au (Barry, 1993). The Capleston Group represents a 2km long vein system with a series of north-plunging shoots dipping steeply to the east. Welcome-Hopeful was the major producer (88,620 oz @ 61.4 g/t Au recovered; Barry, 1993; Figure 3). Fiery Cross was singular for its exceptionally high antimony (Figure 4).

A table of historic production in this district is included in Table 2.

Figure 3: Historical schematic of Capleston Lodes (section 90.313) c.1920, annotated to accentuate the lodes and Reform drill site.

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Figure 4: Fiery Cross Battery, Capleston 1930. Image from Reefton Isite.

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Figure 5: Location of Reefton Projects

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About Rua Gold

Rua Gold is an exploration company, strategically focused on New Zealand. With decades of expertise, our team has successfully taken major discoveries into producing world-class mines across multiple continents. The team is now focused on maximizing the asset potential of RUA's two highly prospective high-grade gold projects.

The Company controls the Reefton Gold District as the dominant landholder in the Reefton Goldfield on New Zealand's South Island. Rua Gold will have approximately 120,000 hectares of tenements, following the completion of its previously announced acquisition of Reefton Resources Pty Limited², in a district that historically produced over 2 million ounces of gold grading between 9 and 50 grams per tonne.

The Company's Glamorgan Project solidifies Rua Gold's position as a leading high-grade gold explorer on New Zealand's North Island. This highly prospective project is located within the North Islands' Hauraki district, a region that has produced an impressive 15 million ounces of gold and 60 million ounces of silver. Glamorgan is within 3 kms of OceanaGold Corporation's biggest gold mining project, WKP.

For further information, please refer to the Company's disclosure record on SEDAR+ at www.sedarplus.ca.

New Investor Relations agreement - Gold Standard Media, LLC

On October 11, 2024, the Company entered into an advertising agreement with Gold Standard Media LLC ("Gold Standard") for total cash consideration of US$200,000, payable immediately. Gold Standard has agreed to provide the Company with its services to create landing pages and provide digital marketing, email marketing and influencer marketing services. Gold Standard will provide its services for a period of 90 days commencing on October 14, 2024. Gold Standard and its principals are arm's length from the Company. To the best of the Company's knowledge and as of the date hereof, certain affiliates of Gold Standard own 5,037,951 common shares in the capital of the Company. Gold Standard is a Texas-based firm and is owned by Kenneth Ameduri, Juliet Ameduri, and Lior Gantz. The Company will not issue any securities to Gold Standard as compensation for its marketing services.

Technical Information

Simon Henderson CP, AUSIMM, a qualified person under National Instrument 43-101 Standards of Disclosure for Mineral Projects, has reviewed and approved the technical disclosure contained herein.

QAQC Drilling

The majority of drillholes were sampled in full, typically following 1-m sample intervals unless geological contacts (i.e. dolerite intrusions) dictated otherwise. NQ core was analyzed as whole core; therefore, only requiring cutting along sample intervals. PQ and HQ core were sampled as half core.

Drill core samples were sent to SGS Westport for sample preparation. Core was crushed to 75% passing 2 mm, and 1-kg split of material was pulverized (to 85% passing 75 µm). No split duplicates were collected during the crushing steps. Two scoops were taken from the pulverize bowl: one for laboratory analysis (~150 g) and the other for pXRF analysis (~100 g). The pulp reject is stored in Reefton.

Rua Gold Contact

Robert Eckford

Chief Executive Officer

Tel: +1 604 655 7354

Email: reckford@RUAGOLD.com

Website: www.RUAGOLD.com

This news release includes certain statements that may be deemed "forward-looking statements". All statements in this new release, other than statements of historical facts, that address events or developments that the Company expects to occur, are forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words "expects", "plans", "anticipates", "believes", "intends", "estimates", "projects", "potential" and similar expressions, or that events or conditions "will", "would", "may", "could" or "should" occur and specifically include statements regarding: the Company's strategies, expectations, planned operations or future actions, including but not limited to exploration programs at its Reefton project and the results thereof; and the Company's acquisition of Reefton Resources Pty Limited. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results may differ materially from those in the forward-looking statements.

Investors are cautioned that any such forward-looking statements are not guarantees of future performance and actual results or developments may differ materially from those projected in the forward-looking statements. A variety of inherent risks, uncertainties and factors, many of which are beyond the Company's control, affect the operations, performance and results of the Company and its business, and could cause actual events or results to differ materially from estimated or anticipated events or results expressed or implied by forward looking statements. Some of these risks, uncertainties and factors include: general business, economic, competitive, political and social uncertainties; risks related to the effects of the Russia-Ukraine war; risks related to climate change; operational risks in exploration, delays or changes in plans with respect to exploration projects or capital expenditures; the actual results of current exploration activities; conclusions of economic evaluations; changes in project parameters as plans continue to be refined; changes in labour costs and other costs and expenses or equipment or processes to operate as anticipated, accidents, labour disputes and other risks of the mining industry, including but not limited to environmental hazards, flooding or unfavourable operating conditions and losses, insurrection or war, delays in obtaining governmental approvals or financing, and commodity prices. This list is not exhaustive of the factors that may affect any of the Company's forward-looking statements and reference should also be made to the Company's CSE Form 2A - Listing Statement filed under its SEDAR+ profile at www.sedarplus.ca for a description of additional risk factors.

Forward-looking statements are based on the beliefs, estimates and opinions of the Company's management on the date the statements are made. Except as required by applicable securities laws, the Company undertakes no obligation to update these forward-looking statements in the event that management's beliefs, estimates or opinions, or other factors, should change.

Table 2: Historical production from mines within the Capleston Project (Barry, 1993).

Lode	Easting	Northing	Quartz tonnes	Au (kg)	Total Production (Au oz)	Recovered grade (oz)	Recovered grade (g/t)
Welcome-Hopeful	1512383	5342261	44,868.9	2,756.4	88,620.3	2.0	61.4
Fiery Cross	1512133	5341691	24,956.4	869.5	27,955.1	1.1	34.8
Just in Time	1511983	5341202	13,754.9	534.1	17,171.7	1.2	38.8
Reform-Imperial-South Hopeful	1511803	5341543	1,698.9	33.3	1,070.6	0.6	19.6
Lone Star	1511833	5340402	243.8	3.4	109.3	0.4	13.9

Source: Barry, J.M., 1993. The History and Mineral Resources of the Reefton Goldfield. Ministry of Commerce Resource Information Report No. 15.

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Dynasty Gold Announces 2024 Annual General Meeting Results and Provides Thundercloud Drilling Update

Dynasty Gold Corp. (TSXV: DYG) (FSE: D5G1) (OTC Pink: DGDCF) ("Dynasty" or the "Company") is pleased to report the results from its 2024 annual general meeting held on Friday, Oct. 4, 2024. Total vote counts represent more than 42% of total issued and outstanding shares. All resolutions put forward to the shareholders were approved. The following directors were elected to hold office until the next annual general meeting of the Company:

Ivy Chong	99.98%
Roman Shklanka	99.98%
Larry Kornze	98.93%
Richard Redfern	98.92%

Dynasty would like to thank its shareholders for their votes and attendance at the meeting.

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Lode Gold Closes $3.5 Million Financing and Strategic Alliance; Ready to Advance Properties in Yukon and New Brunswick

Lode Gold Resources Inc. (TSXV: LOD) (OTCQB: SBMIF) ("Lode Gold" or the "Company") is pleased to announce it has obtained conditional approval from the TSXV and closed the transaction with Fancamp Exploration Ltd. ("Fancamp") pursuant to the definitive Investment Agreement for $3.5 million investment that the Company announced in its August 27, 2024 news release. $500,000 goes into the Company for subscription of 14,285,714 Special Warrants of the Company, each Special Warrant, at $0.035 per unit, upon completion of the Spin Out, will convert to one common share of Lode Gold and one 5-year Lode Gold share purchase warrant with an exercise price of $0.05 per share. If fully exercised, the warrant subscription proceeds will total an additional $714,286; $3,000,000 goes into the Company's wholly-owned subsidiary Gold Orogen, for 5,423,078 common shares or 19.9% of Gold Orogen. As part of the Investment Agreement, the Company has transferred its interests in the McIntyre Brook Property (111 km2) and Fancamp transferred its interests in the Riley Brook Property (309 km2), both located in New Brunswick, into a 5050 joint venture between Gold Orogen and Fancamp, that is called Acadian Gold Corp. The Company has also transferred its interest in its Golden Culvert and WIN Property to Gold Orogen. Fancamp has become a key shareholder of Lode Gold and a 19.9% shareholder of Gold Orogen.

Details of the transaction were disclosed in the Company's August 27, 2024 news release.

The transaction remains subject to final acceptance of the TSX Venture Exchange. The proceeds from the Special Warrant financing will be used for general and administrative costs, including transaction costs, and on the Company's Fremont property. The Special Warrants and the securities acquired on conversion thereof are subject to a four-month hold period from the closing date under applicable Canadian securities laws.

A copy of the Investment Agreement is available on the Company's profile on SEDAR+ (www.sedarplus.ca).

About Lode Gold

Lode Gold (TSXV: LOD) is an exploration and development company with projects in highly prospective and safe mining jurisdictions in Canada and the United States.

Its Golden Culvert and WIN Projects, Yukon, covering 99.5 km² across a 27-km strike length, are situated in a district-scale, high-grade-gold-mineralized trend within the southern portion of the Tombstone Gold Belt. Gold deposits and occurrences within the Belt include Fort Knox, Pogo, Brewery Creek and Dublin Gulch, and Snowline Gold. A NI 43-101 technical report entitled "Technical Report on the WIN-Golden Culvert Property for Lode Gold" with an effective date of May 15, 2024 summarizing the work to date on these properties is available on the Company's profile on SEDAR+ (www.sedarplus.ca) and on the Company's website (www.lode-gold.com).

Its McIntyre Brook Project, New Brunswick, covering 111 km² and a 17-km strike length in the emerging Appalachian/Iapetus Gold Belt, is surrounded by Puma Exploration's Williams Brook Project (5.55 g/t Au over 50m)¹ and is hosted by orogenic rocks of similar age and structure as New Found Gold's Queensway Project.

The Company is also advancing its Fremont Gold development project in the historic Mother Lode Gold Belt of California where 50,000,000 oz of gold has been produced. Fremont, located 500km north of Equinox Gold's Castle Mountain and Mesquite mines, has a Preliminary Economic Assessment(" PEA") with an after-tax NPV (5%) of USD $217M, a 21% IRR, 11-year LOM, averaging 118,000 Oz per annum at USD $1,750 gold. A sensitivity to the March 31, 2023 PEA at USD $2,000/oz gold gives an after-tax NPV (5%) of USD $370M and a 31% IRR over an 11-year LOM. The project hosts an NI 43-101 resource of 1.16 MOz at 1.90 g/t Au within 19.0 MT Indicated and 2.02 MOz at 2.22 g/t Au within 28.3 MT Inferred. The MRE evaluates only 1.4 km of the 4 km strike length of the Fremont property which features five gold-mineralized zones. Significantly, three step-out holes at depth hit the mineralized structure, typical of orogenic deposits that often occur at depth. Fremont is located on 3,351 acres of 100% owned private land in Mariposa, the original gold rush county, and is 1.5 hours from Fresno, California. The property has year-round road access and is close to airports and rail.

About Fancamp

Fancamp is a growing Canadian mineral exploration company focused on creating value through medium-term growth and monetization opportunities with its strategic interests in high-potential mineral projects, royalty portfolio and mineral properties. The company is focused on an advanced asset play poised for growth and selective monetization with a portfolio of mineral claims across Ontario, Quebec and New Brunswick, Canada, including copper, gold, zinc, titanium, chromium, strategic rare-earth metals and others. The company continues to identify near-term cash-flow-generating opportunities and in parallel aims to advance its investments in strategic mineral properties. Fancamp has investments in an existing iron ore operation in the Quebec-Labrador Trough, a rare earth elements company, NeoTerrex Minerals Inc., a copper-gold exploration company, Platinex Inc., in addition to an investment in a near term cash flow generating zinc mine, EDM Resources Inc. in Nova Scotia. The Company has future monetization opportunities from its Koper Lake transaction in the highly sought-after Ring of Fire in Northern Ontario. Fancamp is developing an energy reduction and titanium waste recycling technology with its advanced titanium extraction strategy. The company is managed by a focused leadership team with decades of mining, exploration and complementary technology experience.

QUALIFIED PERSON STATEMENT

The scientific and technical information contained in this press release has been reviewed and approved by Jonathan Victor Hill, Director, BSc (Hons) (Economic Geology – UCT), FAusIMM, and who is a "qualified person" as defined by NI-43-101.

ON BEHALF OF THE COMPANY

Wendy T. Chan, CEO & Director

Information Contact

Winfield Ding
CFO
info@lode-gold.com
+1-416-320-4388

Kevin Shum
Investor Relations
kevin@jeminicapital.com
+1 (647) 725-3888 ext. 702

Cautionary Note Related to this News Release and Figures

Cautionary Statement Regarding Forward-Looking Information

All statements, trend analysis and other information contained in this press release about anticipated future events or results constitute forward-looking statements. Forward-looking statements are often, but not always, identified by the use of words such as "seek", "anticipate", "believe", "plan", "estimate", "expect" and "intend" and statements that an event or result "may", "will", "should", "could" or "might" occur or be achieved and other similar expressions. All statements, other than statements of historical fact, included herein, including, without limitation, statements regarding the anticipated use of proceeds from the Special Warrant financing, additional proceeds from the exercise of the warrants underlying the Special Warrants, and the receipt of final acceptance from the TSX Venture Exchange with respect to the transactions, are forward-looking statements. Although Lode Gold believes that the expectations reflected in such forward-looking statements and/or information are reasonable, undue reliance should not be placed on forward-looking statements since Lode Gold can give no assurance that such expectations will prove to be correct. These statements involve known and unknown risks, uncertainties and other factors that may cause actual results or events to differ materially from those anticipated in such forward-looking statements, including the risks, uncertainties and other factors identified in Lode Gold's periodic filings with Canadian securities regulators, and assumptions made with regard to: the ability of Lode Gold to obtain final acceptance from the TSX Venture Exchange with respect to the transactions; that the Company will be able to use the proceeds of the Special Warrant financing as anticipated; and the ability of the Company to continue with its stated business objectives and its ability to obtain required approvals and raise additional capital to proceed. Forward-looking statements are subject to business and economic risks and uncertainties and other factors that could cause actual results of operations to differ materially from those contained in the forward-looking statements. Important factors that could cause actual results to differ materially from expectations include risks associated with the business of Lode Gold and Fancamp; risks related to the Company's ability to obtain final acceptance from the TSX Venture Exchange with respect to the transactions; the risk that the use of proceeds from the Special Warrant financing may differ from management's expectations; and other risk factors as detailed from time to time and additional risks identified in the Companies' filings with Canadian securities regulators on SEDAR+ in Canada (available at www.sedarplus.ca). Forward-looking statements are based on estimates and opinions of management at the date the statements are made. The Company does not undertake any obligation to update forward-looking statements except as required by applicable securities laws. Investors should not place undue reliance on forward-looking statements.

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Fancamp Announces Closing of the Transaction with Lode Gold Resources to Advance New Brunswick and Yukon Mineral Properties

Fancamp Exploration Ltd. (" Fancamp " or the " Company ") (TSX Venture Exchange: FNC ) is pleased to announce that it has closed the transaction with Lode Gold Resources Inc. (" Lode Gold ") (TSX Venture Exchange: LOD ) and 1475039 B.C. Ltd. (" Gold Orogen "), a subsidiary of Lode Gold, as previously announced on August 27, 2024, to advance the exploration and development of certain mineral properties located in the Yukon and New Brunswick (the " Transaction "). The Transaction represents the opportunity for the joint advancement of significantly sized and under-explored land packages, in highly prospective regions for gold and polymetallic mineral discovery, with the potential to create district scale projects on orogenic belts where other major developers are established and host certain world-class deposits.

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Element79 Gold Corp. Reports Significant Progress in Community Relations and Development Efforts in Chachas, Peru

(TheNewswire)

October 9, 2024 TheNewswire - Vancouver, B.C. Element79 Gold Corp. (CSE: ELEM) (FSE: 7YS0) (OTC: ELMGF) ("Element79" or the "Company") is pleased to announce significant progress in its ongoing community engagement efforts with the community of Chachas, Peru, near the Company's Lucero Project. These efforts are part of the Company's broader strategy to align mining operations with sustainable community development and long-term value creation.

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Hole Number	Dip	Azimuth	From (m)	To (m)	Interval (m)	Au g/t	Cut to 90 g/t
GS2403	-50	315	162.7	164	1.3	6.37
GS2404	-50	360	365	394.9	29.9	0.67
GS2405	-50	360	12.2	34.7	22.5	1.26
GS2406	-55	360	45.8	161	115.2	3.36	1.36
including			45.8	46.4	0.6	476
			231.3	280.8	49.5	0.96
			444.3	470	25.7	1.22
			484.7	520.1	35.4	0.7
Hole Number	Dip	Azimuth	From (m)	To (m)	Interval (m)	Au g/t	Cut to 90 g/t
GS2407	-50	360	119.5	148.4	28.9	2.29
including			119.5	120.4	0.9	57
			194.2	229	34.8	0.65
			330.4	371.2	40.8	1.9
including			369.5	371.2	1.7	37.6
			522.4	609.8	87.4	1.59
including			528.5	531.6	3.1	25.1
GS2408	-55	360	51.7	76.6	24.9	0.72
			241.4	247.1	5.7	1.76
			341.8	358.9	17.1	1.17
			455.3	471	15.7	0.75
			528	570	42	3.06
including			550.8	553.5	2.7	30.9
			593.9	610.2	16.3	2.4
			642	672	30	0.63
GS2409	-55	360	332.1	333.3	1.2	15.5
GS2410	-45	360	68.6	96.6	28	0.49

HOLE NUMBER	AZIMUTH	DIP	DEPTH (M)	FROM (M)	TO	INTERVAL (M)	AU
HOLE NUMBER	AZIMUTH	DIP	DEPTH (M)	FROM (M)	(M)	INTERVAL (M)	G/T
GS2401	360	-90	946.1	331.3	355.7	24.4	0.99
				495.9	544.7	48.8	0.90
				692.1	758	65.9	4.63
including				755	758	3	85.9

GS2402	315	-50	751.6	71	83	12	0.96
				431	483.9	52.9	0.68
				545	590	45	5.51
including				581	584	3	67.0
				604.4	620	15.6	3.74
				667.9	713	45.1	1.18
The width refers to drill hole intercepts; true width cannot be determined due to the uncertain geometry of mineralization

Rajesh Sharma, President & CEO +1 (604) 434 8829 info@fancamp.ca	Debra Chapman, CFO +1 (604) 434 8829 info@fancamp.ca

Tara Asfour, Director of Investor Relations +1 (604) 434 8829 tasfour@fancamp.ca

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