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Spark Energy Extends Pegmatite Trend to 28.4km at the Arapaima Lithium Project in Brazil's Lithium Valley

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Vancouver, British Columbia--(Newsfile Corp. - January 17, 2025) - Spark Energy Minerals Inc. (CSE: SPRK) (OTC Pink: SPARF) (FSE: 8PC) ("Spark" or the "Company") an exploration Company focused on the discovery of battery metals in Brazil's prestigious Lithium Valley, is pleased to announce that after the first week back on-site of the Arapaima Lithium project in Brazil's Lithium Valley, the exploration team has identified another pegmatite corridor measuring ~1.2km in length. This brings the new total of the trend to a combined 28.4km in length.

Arapaima Lithium Project Highlights:

  • Spark Energy's 64,359-hectare land package runs parallel to Sigma Lithium, Brazil's largest lithium company with a market cap of ~C$2 billion and sits only 15km away at the closest point.

  • 80% of the extensive tenement package remains to be explored, underscoring the potential as new pegmatite corridors continue to be uncovered. A 1.2km extension was identified 3km northeast of prospective area 1 increasing the combined trend to 28km.

  • Q1 2025 exploration program continues a focused follow-up of the priority target areas identified towards the end of last year.

  • Beau Nicholls of Sahara Mining Services completed a site visit for an independent NI 43-101 Exploration Report over the company's 64,359-hectare Arapaima Lithium Project.

  • Q4 2024 exploration program samples are with SGS Laboratory and assay results are anticipated any day now.

Spark Energy increases pegmatite trend to combined 28.4km:

Figure 1: Figure showing newly identified pegmatite trend of ~1.2km in length located ~3km northeast of priority target area 1 in the northern section of the Arapaima Lithium project tenements

To view an enhanced version of this graphic, please visit:
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Arapaima's 64,359-hectare tenement area comprises a dissected plateau characterized by a thick covering of lateritic regolith. A well-developed network of drainage is carved into the plateau exposing sections through the regolith into oxidized, granitoid intrusive rocks of the basement complex in the valley sides and floors. The granitoids are cut by an anastomosing suite of late-stage pegmatites continually identified in the windows of weathered exposure between the cover.

Within these windows of exposure Spark Energy's prospecting team noted the prospective target area 1 is largely underlain by the two mica G2 granite rock suite which is host to multiple pegmatite bodies, some attaining thickness's over 5m. Back on the ground for 2025's field program they followed this geology to the northeast identifying pegmatite veins hosted in the same two-mica G2 granite suite. These newly recognized pegmatites are composed of quartz, feldspar, white mica, and variable concentrations of tourmaline in a trend that shows NE-SW and NW-SE over ~1.2km in length extending the total combined trend to 28.4km.