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FAQ on Texas Mineral Resources' Alhambra Geophysics Drilling Confirmation

FaqStaq News - Just the FAQs July 24, 2025
By FAQstaq Staff
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FAQ on Texas Mineral Resources' Alhambra Geophysics Drilling Confirmation

Summary

Texas Mineral Resources Corp. announces positive preliminary exploratory drilling results in the Black Hawk Mining District, confirming the effectiveness of the Electro-Magnetic survey method in locating veins, marking a significant step in the exploration and development of silver properties.

What is the main announcement by Texas Mineral Resources Corp.?

The company announced positive preliminary exploratory drilling results in the Black Hawk Mining District, confirming the effectiveness of the Electro-Magnetic survey method in locating veins.

Why is this drilling confirmation significant?

It validates the use of the Electro-Magnetic survey method for locating veins in the district, which is crucial for the ongoing exploration and development of silver properties.

How was the drilling conducted?

Drilling was conducted during March, April, and May 2025, with 20 diamond drill holes aggregating 2751.5 feet at the historic Alhambra mine, guided by geophysical results.

Who is involved in this project?

Texas Mineral Resources Corp. is working under a mineral exploration and option agreement with Santa Fe Gold Corporation, with geophysical surveying conducted by Zonge International.

Where is the drilling taking place?

The drilling is taking place in the Black Hawk Mining District in Grant County, New Mexico.

What are the next steps after the drilling?

Drill core is being logged and analyzed, with a complete report to be released once analysis is complete.

What does the success of the NANOTEM method mean for the project?

The success of the NANOTEM method in identifying veins is encouraging for the ongoing exploration and development of the project, as stated by CEO Daniel Gorski.

What type of ore deposit is found in the Black Hawk Mining District?

The district contains ‘Five Element Veins,’ which are lenticular, carbonate-filled structures with a central high-grade core.

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