TinOne Resources Inc. provided further results from its Great Pyramid Tin (Sn) Project ("Great Pyramid" or the "Project") located in the tier one mining jurisdiction of Tasmania, Australia. Drilling has now concluded, and data compilation and modelling are underway. The program has been highly successful in continuing to define significant tin mineralization near surface and at depth below and adjacent to historical drilling.

Results reported here represent data from both the upper reverse circulation component and the lower diamond drill component of holes 22GPRC014 and 22GPRC021. The reverse circulation components have been previously reported and in this release, the combined intersections are reported where the diamond drill data are contiguous with the previously reported RC data (ie 22GPRC014 from 87 metres and 22GPRC021 from 128). Results have been received for 3,816 metres of the Company's completed 4,687 metre drilling program at Great Pyramid.

These results represent complete results for 18 RC reverse circulation drill holes, results from two diamond cored holes and partial results from one diamond cored hole, in addition to results from six diamond tails and partial results from one other diamond tail. The Great Pyramid deposit is located around a topographical feature known as Pyramid Hill and is hosted by Silurian to Devonian Mathinna Supergroup sandstones. The mineralization is formed by closely spaced sheeted northeast trending cassiterite (SnO2) bearing veins associated with silicification and sericite-pyrite alteration.

The deposit style and regional comparisons suggest that a tin-fertile granite exists at depth below the deposit, however this has not been encountered in drilling and the deposit is open at depth. Geological interpretation indicates that certain sedimentary units within the folded Mathinna Supergroup sediments are more favorable hosts and diamond drilling being undertaken by the Company during the current campaign, combined with numerical modelling, will assist in developing a deeper understanding of controls on grade for follow up drilling. The deposit is currently known over a strike length of more than 500 metres with an average width of approximately 150 metres.

The depth extent of the deposit is unknown with only nine historical drill holes greater than 150 metres deep. These rare deeper holes encountered encouraging tin mineralization to depths of approximately 300 metres below surface. Drill core and RC samples were shipped to ALS Limited in Brisbane, Australia for sample preparation and for analysis.

The ALS, Brisbanefacilities are ISO 9001 and ISO/IEC 17025 certified. Tin and tungsten are analysed by ICP-MS following lithium borate fusion (ALS method ME-MS85), overlimit results are reanalysed by XRF (ALS method XRF15b). Forty-eight element multi-element analyses are conducted by ICP-MS with a four-acid digestion (ALS method ME-MS61).

Control samples comprising certified reference samples, duplicates and blank samples were systematically inserted into the sample stream and analyzed as part of the Company's quality assurance /quality control protocol. The Company's disclosure of technical or scientific information in this press release has been reviewed and approved by Dr. Stuart Smith., Technical Advisor for TinOne. Dr. Smith is a Qualified Person as defined under the terms of National Instrument 43-101.