Kalo Gold Confirms Vertically Continuous Gold System at Qiriyaga Complex and Identifies Untested Epithermal Feeder Target at Depth - 16.90 m at 3.25 g/t Au

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[{"type":"text","content":"Kalo Gold Confirms Vertically Continuous Gold System at Qiriyaga Complex and Identifies Untested Epithermal Feeder Target at Depth - 16.90 m at 3.25 g/t AuVANCOUVER, BC / ACCESS Newswire / April 8, 2026 / Kalo Gold Corp. (TSXV:KALO)(OTCID:KLGDF)(FSE:9M51) (\"Kalo\" or the \"Company\") reports drill results from VA26-DH17 at the QC1 target within the Qiriyaga Complex, confirming a vertically continuous gold system from surface through to the diatreme. The hole intersected 16.90 m at 3.25 g/t Au within a continuous mineralized profile spanning surge deposits, diatreme-margin breccias, and internal veining. Importantly, the interpreted primary epithermal feeder zone at approximately 395 metres depth - defined by the convergence of the Namalau, Loma, and Buca Faults - remains untested and represents a high-priority drill target.KEY HIGHLIGHTSVertically continuous gold system confirmed - mineralization spans from near-surface surge deposits through diatreme wall breccia into internal veining (VA26-DH17)Untested feeder target at depth - interpreted convergence of Namalau, Loma, and Buca Faults at ~395 m remains a high-priority epithermal drill target16.90 m at 3.25 g/t Au (including 9.00 m at 4.66 g/t Au) - VA26-DH17, QC1Three independent diatreme structures mineralised - QC1, QC3, and QC4 all confirmed gold-bearingBlind geophysical target confirmed on first drill hole - VA25-DH14 at QC416 of 18 identified epithermal upflow centres remain untested at depthVA26-DH17 - QC1, Qiriyaga ComplexVA26-DH17 was designed to test the QC1 system from near-surface surge deposits through to the diatreme. The hole intersected a continuous vertical profile of gold mineralization across pyroclastic surge deposits, basal surge units, wall-rock breccias, and a vein and stockwork zone within the diatreme itself. Drill hole VA26-DH17 was collared 115 metres northeast of VA25-DH11, with approximately 110 metres between the mineralized zones of each hole (figure 1). The strongest gold mineralization occurs at the transition between basal surge deposits and underlying breccias, consistent with interpreted fluid upflow and boiling zones. This confirms that mineralization is not isolated but forms a vertically coherent hydrothermal system across multiple lithological and structural domains.From (m)To (m)Interval (m)Au (g/t)True WidthNotes3.611.17.500.59~7.1 mSu...

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