Fathom Announces Extension of the Historic Gochager Lake Deposit Host Rock over a 3.5+ km Strike Length 
  newsfilecorp.com
  October 23, 2025 8:02 AM EDT | Source:  Fathom Nickel Inc. 
  Calgary, Alberta--(Newsfile Corp. - October 23, 2025) - Fathom Nickel Inc. (CSE: FNI) (FSE: 6Q5) (OTCQB: FNICF) ("Fathom", or the "Company")  is pleased to announce an updated geology map reflecting the most  recent prospecting and pXRF (Portable X-ray Florescence) rock  geochemistry results at the Gochager Lake project. The historic Gochager  Lake deposit host rock (the "container rock"), has now been  mapped consistently along strike northeast of the historic Gochager Lake  deposit for a minimum distance of 3.5 kilometers.   The Company is in  receipt of all assays from the July 2025 program and awaits rock assay  and whole rock geochemistry results from the September-October  prospecting. These results are expected mid-November.   
  Ian Fraser, Fathom CEO and VP Exploration stated, "We  are very pleased and excited about the results of our summer-fall  geochemistry program. We have applied the knowledge gained from drilling  the historic deposit to surface exploration and have now expanded the  Gochager Lake deposit container rock significantly along strike.  We are  currently interpreting and compiling the summer soil geochemistry  program results with the new geology map and will release those results  when complete. The expanded container rock defined to date now is  developing into a very linear feature that is consistent with the  geological settings of many of the world's premier magmatic nickel  districts. We remain adamant that there is much more to this project  than just the historic Gochager Lake deposit. The 3.5 kilometers of  Gochager container rock gives us an expanded playing field for  additional discoveries of significant bodies of semi-massive to massive  Ni-Cu-Co sulphide mineralization. We are very excited to continue our  exploration work as we continue to develop and add high-quality drill  targets at the project."
  Summer-Fall Program Highlights
  The  wildfire that impacted the Gochager Lake property at the end of July  resulted in significant new outcrop exposure. As a result, a second  prospecting campaign was carried out September 25 to October 1, 2025.  Highlights of the combined summer-fall prospecting program include:
 
 - Consistently  occurring surface outcrops, characterized by disseminated sulphide  mineralization, including pyrrhotite +/- pentlandite in  variable-textured gabbro and ultramafic rock (pyroxenite), have been  mapped and form a northeast linear trend measuring 3.5 kilometers. Refer  to map insert. 
 - The mineralized variable-textured gabbro  continues immediately to the northeast of the historic Gochager Lake  deposit towards and under Scurry Lake, south of Rainbow Lake, and  further northeast to the north shore of Weaver Lake.  The  variable-textured gabbro is now mapped for a minimum strike of 3.5  kilometers.  Refer to map insert.    
 - Clotted gabbro has been  consistently mapped in direct contact with variable-textured gabbro  along much of the 3.5 km strike length. Clotted gabbro defines the  footwall lithology at the historic Gochager Lake deposit. Refer to  insert map.
 - During the summer-fall p program:
-  684 outcrop chip samples were collected and analysed on-site by pXRF.
 - Ni-Cu-Co + Mg-Cr pXRF scan values were used to develop the updated geology map.
 - 79  rock grab samples, inclusive of standards and blanks, have been  submitted for multi-element assay and whole rock geochemistry analysis. 
 - Final  rock assay and whole rock geochemistry results will be integrated into  our final compilation / interpretation and will aid in further  refinement of the geology map and future drill targets.
 
   Significance of the Gochager Lake Deposit Container Rock
 
 - The historic Gochager Lake deposit2 is contained within a steeply oriented mineralized variable-textured gabbro (the "container rock"), with a thickness of up to 100-meters. 
 - Mineralization,  including pyrrhotite +/- pentlandite and +/- chalcopyrite within the  variable-textured gabbro, is characterized by a broad halo of  disseminated sulphide mineralization, containing stringer to massive  sulphide veins, local net-texture mineralization, and semi-massive to  locally massive sulphide breccias that form steeply oriented chutes and  zones.  
 - Fathom drilling within the Gochager Lake deposit container rock yielded:
- 3.25%  Ni, 0.26% Cu, 0.11% Co / 0.64m intersected in a massive sulphide vein  in drillhole GL23008: (Fathom Press Release November 21,2003).
 - 1.43%  Ni, 0.38% Cu, 0.11% Co / 7.39m, including 2.43% Ni, 0.55% Cu, 0.19% Co /  2.94m intersected in semi-massive to massive sulphide breccias in  drillhole GL24016: (Fathom Press Release May 28, 2024).
 
  - Disseminated  sulphide in variable-textured gabbro - the Gochager Lake deposit  container rock, is now recognized along a 3.5km strike length northeast  of the deposit and remains open for expansion.
 - Furthermore, the  container rock at the deposit contains multiple borehole electromagnetic  (BHEM) off-hole anomalies / conductors that remain untested by  drilling.
 - It is very significant to see the continuation of the  variable-textured gabbro and clotted gabbro footwall contact along  strike of the Gochager Lake deposit (clotted references an increase in  biotite clots). Fathom drilling at the deposit indicates a relationship  of sulphide concentration / accumulation along, at and near the footwall  contact.
  Fathom drillhole GL23011 drilled in the vicinity  of the well mineralized variable-textured gabbro on the west shore of  Scurry Lake, intersected mineralized variable-texture gabbro and the  BHEM survey resulted in 3 prominent off-hole conductivity anomalies that  remain untested by drilling. The Company is confident that the  container rock, containing disseminated sulphide mineralization within  the expanded 3.5 kilometers of strike has the potential to yield  additional off-hole BHEM conductivity anomalies. More importantly, and  like at the Gochager Lake deposit, the expanded container rock has the  potential to yield chutes of high-grade sulphide breccia mineralization,  massive sulphide veins, and massive sulphide bodies that typically  occur in this type of magmatic setting. 
  The Company will make  announcements once we have completed our thorough evaluation of all  results from the summer-fall surface exploration programs.
    
  Gochager Lake Deposit Area Geology Map
  To view an enhanced version of this graphic, please visit: images.newsfilecorp.com
  Quality Assurance / Quality Control (QA/QC) Disclosure Statement
  As  part of its ongoing exploration activities, Fathom is utilizing a  portable Vanta™ XRF Analyzer ("pXRF") to provide real-time  lithogeochemical, multi-element data on surface rock chip samples and  rock grab samples collected in the field. The Vanta™ XRF Analyzer is a  hand-held device, held in position for a total 120 seconds - beam 1 (30  seconds), beam 2 (60 seconds) and beam 3 (30 seconds) to allow for an  effective reading of elements occurring at that specific point, and at  that specific surface of a rock sample.  All elements detected at that  specific point; nickel, copper, cobalt plus key pathfinder elements,  chrome and magnesium, are recorded. The reader is cautioned that pXRF  data should be treated only as an indication of elements, as the accuracy of the beam position on a particular element is variable.  
  Qualified Person and Data Verification
  Ian  Fraser, P.Geo., CEO, VP Exploration and a Director of the Company and  the "qualified person" as such term is defined by National Instrument  43-101, has verified the data disclosed in this news release, and has  otherwise reviewed and approved the technical information in this news  release on behalf of the Company. 
  About Fathom Nickel Inc.
  Fathom  is an exploration company that is targeting magmatic nickel sulphide  discoveries to secure the supply of North American Critical Minerals and  to support the global green energy transition. The Company now has a  portfolio of three high-quality exploration projects located in the  prolific Trans Hudson Corridor in Saskatchewan:
  1) The Albert Lake Project, a 90,000+ hectare project that hosts the historic Rottenstone Mine1. Fathom exploration to date at the Albert Lake project confirms: 
 
 - The high-grade Ni-Cu-Co+3E Rottenstone deposit mineralization extends to the south a minimum 40m and remains open.
 - The Rottenstone deposit is potentially offset and continues within the footwall of a prominent fault defined by drilling. 
 - A  new Rottenstone-like discovery (similar host rock, and similar  mineralization) by drilling 500-550m W-NW of the historic mine; the  300+m Bay Island Trend, remains open along strike.
 - Similar  Rottenstone-like host rock and mineralization intersected by drilling  approximately 1.5km S-SW of the historic mine (the Nic5-Tremblay-Olson  area). 
   2) The 33,000+ hectare Gochager Lake Project that hosts the historic Gochager Lake deposit2. Fathom exploration to date at the Gochager Lake project confirms: 
 
 - Vertical  extension of Ni-Cu-Co mineralization a minimum of 150m below the  historic Gochager Lake deposit interpreted boundary, and very good  potential for expansion of mineralization in all directions.
 - Multiple  high-grade vertically oriented Ni-Cu-Co sulphide breccia mineralization  zones and chutes occur within the historic deposit, and the zones,  chutes remain open for further expansion and delineation in all  directions.
 - Surface mapping and soil / rock geochemistry has  confirmed the Gochager Lake deposit host rock; the container rock and  mineralization style extends a minimum 3.5km to the east-northeast and  remains open for expansion along strike. 
  3) The 10,000+  hectare Friesen Lake Project located 40km southwest of the historic  Rottenstone Mine and 30km northwest of the historic Gochager Lake  deposit. 
  The Friesen Lake property hosts the Olsen Cu-Ni-Pt  Showing also referred to as the Friesen Lake Cu-Ni-Pt showing and is  described as an ultramafic dyke that historic trenching and drilling  demonstrates Cu-Ni-Pt-Pd and Au mineralization within the ultramafic  dyke (Saskatchewan Mineral Deposit Index (SMID) #0928a). To date Fathom  has not performed any exploration at the Friesen Lake Project.  
  1  - The Rottenstone Mine; a small open-pit mining / milling operation was  in production 1965-1969. Milling commenced September 5, 1965, operated  through November 7, 1965, and 5,500 short tons were mined and milled  during this period. The average production grade; 3.23% Ni, 1.83% Cu,  0.14 oz/ton Pt, 0.10 oz/ton Pd, 0.03 oz/ton Au (9.26 g/t* 3E, 3E =  Pd-Pt+Au) and 0.20 oz/ton Ag.  Initial milling operations 1965 produced  1,070 dry short tons of concentrates, the average concentrate grade was  10.835% Ni, 5.74% Cu, 0.33 oz/ton Pt, 0.53oz/ton Pd, 0.10 oz/ ton Au  (32.91 g/t* 3E) and 1.25 oz/ton Ag.  Richards, B.R. and Robinson, B.G.W.  (1966), Mining and milling a small ore deposit …. Rottenstone Mining  Limited: The Canadian Mining and Metallurgical Bulleting for December  1966.  The Saskatchewan Mineral Deposit Index (SMDI) #0958 reports final  mine production in 1969 of 28,724 tons with an average grade of 3.28%  Ni, 1.83% Cu and 9.63 g/t 3E and that approximately 9,000 tons of  concentrate were sold to the International Nickel Company of Canada  Limited.
   * A factor of 34.286 g/tonne was used to convert 1 oz/ton to g/tonne (g/t).
    2 - The Gochager Lake property is host to the historic Gochager Lake  Ni-Cu deposit. There is no source or available Technical Reports to  verify the historic resource estimate for the Gochager Lake deposit;  hence, Fathom will treat the historic estimate as an Exploration Target.  Available records in the SMDI and Saskatchewan Mineral Assessment  Database (SMAD) suggest an Exploration Target of 4-5 million tons  grading 0.3% Ni - 0.4% Ni and 0.08% Cu - 0.09% Cu, containing a  higher-grade core of 1.5-2 million tons grading 0.6% NiEq - 0.7% NiEq  (note NiEq is based on Ni-Cu only). The ranges of tons and grade are  conceptual as there is insufficient historic data to verify the  historical resource estimate(s) for the Gochager Lake deposit, and the  higher-grade core. At present, Fathom has drilled 16 drillholes (5,549m)  into the historic Gochager Lake deposit and has confirmed Ni-Cu grades  comparable to and higher than the historical grades reported, thus  confirming that a deposit of Ni-Cu+Co metal accumulation does exist at  the historic Gochager Lake deposit / property. Furthermore, insufficient  drilling has been done by the Company to define a current mineral  resource, and again at this time, it is uncertain if further drilling  will result in the Exploration Target being delineated as a mineral  resource. The disclosed potential quantity and grade has been determined  by historic records notably; the Saskatchewan Mineral Deposit Index  (SMDI #0880) reports delineation drilling outlined a deposit  at the  historic Gochager Lake Deposit;  Steel, J.S. (1990),(SMAD 73P15-0091):  Report on a Diamond Drilling Program on the Gallagher (Gochager) Lake  Property of McNickel Inc., reported that Scurry-Rainbow Oil Ltd.  constructed vertical sections and a longitudinal section from drill data  collected 1966-1968, and an orebody with reasonably well-defined limits  was interpreted. Ore reserves were then calculated for Zone A. As  stated above, the historic estimate is not well documented and there are  no available Technical Reports to support the historic resource  estimate(s). 
  ON BEHALF OF THE BOARD
  "Ian Fraser" CEO, VP Exploration, Director
  For further information, please contact:
  Ian Fraser, CEO, VP Exploration 1-403-650-9760  ifraser@fathomnickel.com
  Or
  Doug Porter, President and CFO 1-403-870-4349  dporter@fathomnickel.com
  Forward-Looking Statements:
  This  news release contains "forward-looking statements" that are based on  expectations, estimates, projections and interpretations as at the date  of this news release. Forward-looking statements are frequently  characterized by words such as "plan", "expect", "project", "seek",  "intend", "believe", "anticipate", "estimate", "suggest", "indicate" and  other similar words or statements that certain events or conditions  "may" or "will" occur, and include, without limitation, statements  regarding payment of terms under the Option Agreement, permitting for  the Property, receipt of an exploration permit,  timing of the  exploration program on the Property and the Company achieving the  earn-in thresholds under the Option Agreement. Forward-looking  statements relate to information that is based on assumptions of  management, forecasts of future results, and estimates of amounts not  yet determinable. Any statements that express predictions, expectations,  beliefs, plans, projections, objectives, assumptions or future events  or performance are not statements of historical fact and may be  "forward-looking statements." Forward-looking statements are subject to a  variety of risks and uncertainties which could cause actual events or  results to differ from those reflected in the forward-looking  statements, including, without limitation: risks related to failure to  obtain adequate financing on a timely basis and on acceptable terms;  risks related to the outcome of legal proceedings; political and  regulatory risks associated with mining and exploration; risks related  to the maintenance of stock exchange listings; risks related to  environmental regulation and liability; the potential for delays in  exploration or development activities or the completion of feasibility  studies; the uncertainty of profitability; risks and uncertainties  relating to the interpretation of drill results, the geology, grade and  continuity of mineral deposits; risks related to the inherent  uncertainty of production and cost estimates and the potential for  unexpected costs and expenses; results of prefeasibility and feasibility  studies, and the possibility that future exploration, development or  mining results will not be consistent with the Company's expectations;  risks related to commodity price fluctuations; and other risks and  uncertainties related to the Company's prospects, properties and  business detailed elsewhere in the Company's disclosure record. Such  forward looking statements involve known and unknown risks,  uncertainties and other factors which may cause the actual results,  performance or achievements of the Company to be materially different  from any future results, performance or achievements expressed or  implied by such forward-looking statements. These forward-looking  statements are made as of the date hereof and the Company does not  assume any obligation to update or revise them to reflect new events or  circumstances except in accordance with applicable securities laws.  Actual events or results could differ materially from the Company's  expectations or projections.
 
    SOURCE:  Fathom Nickel Inc. |