Mammoth Resources Corp. (the "company", or "Mammoth") provided results from an additional four drill holes from its diamond drilling program at its 100% owned Tenoriba gold-silver property located in the prolific Sierra Madre precious metal belt, Mexico. The drill program is designed to test up to five target zones which measure from hundreds of metres (m) to over one kilometre (km) in strike length along a 4 km, east-west trend of gold-silver mineralization identified in 3-dimensional (3D) modelling incorporating data from over 3,000 soil, chip and channel samples, 26 prior diamond drill holes, geological and structural mapping and the potential continuity at depth of surface mineralization as indicated by an Induced Polarization/Magnetometer (IP/Mag) geophysical survey.

An additional four diamond drill holes have been completed for a total of 320.7 m bringing the total reported to date to 2,234.6 m in 17 holes. Drill Hole Description: Mammoth has initially drilled 2 to 4 holes at significant, up to 250 m drill spacings, within each target area then moved to another target area to drill a similar number of holes. Company geologists were waiting the results from the initial 2 to 4 drill holes in a target area prior to returning to the area to follow up drilling of these areas based on the results from the initial holes.

Where mineralized intervals are intersected in the initial sequence of drilling, or where holes fail to encounter mineralization as suggested by the data, any follow up drilling will be based on field assessments combined with surface geology, sampling and geophysics data to assist in defining additional drill collar locations with the aim of assisting in more clearly understanding and testing the controls and continuity to gold-silver mineralization. Hole TEN 21-14 was collared in the Moreno target area with the objective of testing a similar Carneritos-like epithermal High Sulphidation (HS) precious metal mineralized system and a high resistivity feature identified in the 3D geophysical modelling which coincides on surface to the mapped altered volcanic breccia. Holes TEN 21-15 through TEN 21-17 were collared in the Carneritos target area where abundant surface gold-silver mineralization occurs within a large 1,400 metre long by at least 400 metre wide area typified by advanced argillic altered outcrops of dacite porphyry and associated breccias with alteration assemblages of kaolinite, abundant dickite, silica and vuggy silica.

These altered volcanic rocks coincide with a geophysical magnetic low. The magnetic low is believed to be the result of the destruction of magnetic minerals by intense mineralizing hydrothermal fluids, the same fluids responsible for the alteration assemblages. These combined features are common within High Sulphidation (HS) altered volcanic rocks, typical of a collapsed volcanic dome.