공시 • Apr 11
Manning Ventures Inc. announced that it has received CAD 0.30002 million in funding On April 9, 2026, Manning Ventures Inc. closed the transaction. The company issued 5,000,331 common shares at an issue price of CAD 0.06 per Share, for gross proceeds of CAD 300,019.86. The securities issued pursuant to the Offering are subject to a statutory hold period of four months plus a day from the date of issuance in accordance with applicable securities legislation. 공시 • Mar 21
Manning Ventures Inc. announced that it expects to receive CAD 0.3 million in funding Manning Ventures Inc. announced a non-brokered private placement of up to 5,000,000 common shares at an issue price of CAD 0.06 per Share for gross proceeds of CAD 300,000 on March 20, 2026. In its discretion, the Company may increase or decrease the size of the Offering in accordance with the policies of the Canadian Securities Exchange. In connection with the Offering, the Company may pay finders’ fees in cash or securities, or a combination thereof, to certain finders, as permitted by the policies of the Exchange. There is no minimum number of Shares or minimum aggregate proceeds required to close the Offering and the Company may, at its discretion, elect to close the Offering in one or more tranches. The securities issued pursuant to the Offering are subject to a statutory hold period of four months plus a day from the date of issuance in accordance with applicable securities legislation. Closing of the Offering and the issuance of the Shares are subject to a number of conditions, including receipt of all necessary regulatory and corporate approvals, including approval from the Exchange. 공시 • Oct 23
Manning Ventures Inc., Annual General Meeting, Dec 18, 2025 Manning Ventures Inc., Annual General Meeting, Dec 18, 2025. Location: british columbia, vancouver Canada 공시 • Jan 17
Manning Ventures Inc. Receives Initial Results and Resumes Drill Program At the Copper Hill Project, Nevada, USA Manning Ventures Inc. provided an update regarding the phase one drill program at the Copper Hill Project, located along the prolific Walker Lane Trend, western Nevada, USA. Drilling has resumed at the Copper Hill Project, initial results have been received for the first four holes. Early assay results and preliminary geology from the on-site logging of these holes is encouraging. The phase one holes were laid out to test for skarn mineralization on the contact between the limestone and the intrusive for the Northern and the Southern Zones. The two zones outline target areas that returned significant copper values (0.5 to > 1.0% copper) in intense skarn alteration. Prior to the holiday break drilling was underway at drill site PDH-7 where hole CH-8, the eighth hole of the program, had reached 200 meters. This hole is targeting down-dip from historic workings with magnetite-skarn. Holes CH-1, CH-3, CH-4, CH-5, CH-6, and CH-7 focused on northwest trending faults and northwest trending diorite dikes in the northern target zone area. All the holes intersected multiple diorite dikes and distinct structural zones. The dike margins and structural zones have skarn mineralization and strong magnetite alteration. CH-4 also intersected numerous clay zones that align with the distinct northwest-southeast finger of intrusive identified from the magnetic survey. CH-1 had an interval of visible oxide copper which returned: 1.52 meters (56.39-57.91 meters) with 2010 ppm Cu (0.21% Cu) and 0.237 g/t Au. Copper in CH-1 ranged from 24 to 2010 ppm Cu with the entire hole averaging 105 ppm Cu. Hole CH-3 intersected multiple northwest tending diorite dikes as well as cutting several northwest fault zones in the top 75 meters of the hole. CH-3 returned: 3.05 meters (50.29-53.34 meters) with 1613 ppm (0.16% Cu). Copper in CH-3 ranged from 37 to 1955 ppm Cu with the entire hole averaging 126 ppm Cu. Hole CH-4 intersected numerous 1.52 to 6.1 meter thick, clay-bearing fault zones that returned from 529 ppm to 928 ppm Cu. Assay results for CH-5 to CH-7 are in progress. These holes have intersected the intrusive- limestone contact where it is cut by the northwest trending dike and structural zones. Encouraging alteration and mineralization in these holes includes: CH-5: 13.72 meters of strong magnetite skarn from 236.22 to 249.94 meters. CH-6: 45.72 meters (67.06 to 112.78 meters) of visible copper oxide and 3.04 meters (175.26 to 178.31 meters) of copper oxide (including chrysocolla). CH-7: 16.76 meters (118.87 to 135.64 meters) of limestone skarn with 3 to 5% pyrite and possible chalcopyrite and 7.62 meters (242.32 to 249.94 meters) of limestone skarn with 5 to 10% pyrite and possible chalcopyrite. Drilling continues and assays are pending. The Company will release results once they are received and verified. Drill chip samples remained under the supervision of company representatives on site until picked up, on site by ALS Global and transported to there Elko Facilities. The company employs a systems of inserting Certified Reference Material (‘CRM’) into the sample stream as a supplement to the quality controls employed by ALS global. 공시 • Sep 13
Manning Ventures Inc., Annual General Meeting, Oct 29, 2024 Manning Ventures Inc., Annual General Meeting, Oct 29, 2024. Location: british columbia, vancouver Canada 공시 • Aug 22
Manning Ventures Inc. Provides Drilling Update for Its Copper Hill Project, Nevada, USA Manning Ventures Inc. announced to update its shareholders on the initial drill program planning at the Copper Hill Project located within the Walker Lane Trend, southern Nevada, USA. Plans are underway to drill inclined holes testing the skarn on the contact between the limestone and the intrusive for the Northern and the Southern Zones. The two zones outline target areas which host significant copper values (0.5 to >1.0% copper) in intense skarn alteration. Each zone is over 1500 meters (>5000 feet) long and is defined by prominent gravity and magnetic geophysical signatures as reported previously by Manning. Specific drill hole locations will be defined utilizing all the data collected, and the historic data accumulated by the Company. Sites will be chosen to drill-test the targets with the most favorable geochemistry, geophysics, and geology. Specific sites will be permitted with the U.S. Bureau of Land Management. Access and drill sites will utilize the proscribed Notice Level process that allows for up to five (5) acres of disturbance. Once submitted, the Notice Level plan is typically accepted and authorized in less than one month. The Company anticipates confirming the exact drill locations over the next few weeks and will provide details once the permit application has been submitted. Recent geological mapping has identified four primary rock units within Triassic Luning limestone which was intruded by a Jurassic igneous complex which was then overlain by Neogene age Volcanic rocks and Quarternary aged unconsolidated gravels. Comparison of the geophysical interpretations and surface geochemical sampling results announced previously with the current geological mapping indicates a series of west-northwest and northwest trending structural fabrics providing the primary controls to copper mineralization at Copper Hill. The northwest faults and associated magnetic and gravity linears represent structural breaks and pathways for mineralizing fluids as witnessed by the elevated copper values returned within these zones. Skarn-type alteration and mineralization is found throughout the Mesozoic limestone and igneous rocks. It occurs in two prominent geologic settings on the copper hill property. Limestone-granodiorite contact, Along northwest and west-northwest trending faults and fault zones; dominantly in the Jurassic igneous rocks with less intense, more distal-type skarn-type alteration in the Triassic Luning Limestone. The mapping and compilation of all exploration data at Copper Hill outlines an untested, highly prospective, copper/gold bearing skarn target. Potential may exist for a porphyry type copper deposit to be found deep beneath Copper Mountain or beneath the covered southeast intrusive. Additionally, porphyry-related veins and local chloritic and sericitic alteration is found along these northwest trends. Two exploration corridors termed the Northern Zone and the Southern Zone outline areas with over 1500 meters (>5,000 feet) of strike length which host significant, intense skarn alteration and elevated copper values (0.5 to >1.0% copper). The most significant features on the west-northwest trends are: Northern Zone- Correlates with northern copper in soils anomaly, Aligns with garnetite, copper-bearing zones, Aligns with larger dikes of diorite. Southern Zone- Adjacent to deepest historic mineralization and proximal to historic shallow, near surface mines (limestone host in historic mine area is likely very thin and gets wider and thicker moving to southeast). Aligns with gravity trend indicating Limestone/intrusive contact connecting southeast to SE buried intrusive. Northern end of southern zone associated with high-grade surface sampling and historic mining of garnetite and massive magnetite skarn zones. Correlates with southern high copper in soils anomaly. Located within the prolific Walker Lane trend in southern Nevada, Copper Hill is situated one of the premier jurisdictions for precious metals mining in the world. Historic endowment within Walker Lane includes 50Moz Au, 700Moz Ag, and 4Mt Cu. Copper Hill hosts copper-gold- molybdenum mineralization in both porphyry and skarn styled deposits in Mineral County, Nevada. The property consists of 108 mineral claims covering an area of 893-ha, located 22 miles north of Hawthorne, Nevada and is accessible using well-maintained County Roads. The Project is centered on a Jurassic Age quartz monzonite porphyry intruding Triassic age Luning Limestone. The claims cover 2.3 sq miles and are 33 miles east of the Yerington Copper District which hosts the Yerington Copper Mine (Anaconda 1952-1978), Ann Mason Deposit, Bear Deposit, MacArthur Deposit, and the Pumpkin Hollow Mine. Historically at Copper Hill, reported high-grade copper was mined from underground shafts from skarn and porphyry-copper styled mineralization at the Copper Mountain Mine. Between 1914 to 1926 mining from the "Copper Mountain Mine" produced an estimated 1,000,000 pounds of copper from shallow underground workings. Historic reporting from the period of production describes ore zones of contact skarn- type and porphyry-type mineralization with shipping grades ranging from 3.5 to 11.0% copper. 