The directors of Thor Mining Plc ("Thor") announced that visible gold in stream sediment sample panning, from the third phase of gold geochemical sampling, carried out earlier this month, at the 100% owned Pilbara Goldfield tenements (E46/1262 and E46/1190) in Western Australia. Further to the announcement of 14 October 2020, a total of 112 stream sediment samples (20PST 35 to 55, 55A, 56 to 89) were collected from 54 creek sites with both fine (< 2mm) and coarse fractions (>2mm) collected for geochemical analysis as well as an additional <2mm sample for in-field panning. Samples are now undergoing laboratory analyses with results anticipated in three to four weeks. The geochemical program was designed to follow up anomalous gold identified in stream sampling programs completed in October 2019 and September 2020, with values up to 256ppb (19PST 19F -AR25) and 130ppb (20PST 24F-BLEG). Stream Sediment Sampling-Gold Anomalism: Fifty-four (54) sample sites with a total of 112 stream sediment samples were selected for reconnaissance and follow up sampling to the 2019 and 2020 geochemical programs. A 10-12 kg pan sample of -2mm material was collected and panned at the end of each day. Gold count and description summaries in Table A. A total of 13 out of the 54 samples returned gold in pan with a maximum of 6 colours in samples 20PST 54 and 20PST 84 (Figure2 and Table A). These 13 visible gold samples consistently lie within the anomalous 13km gold corridor along the thrust faulted mafic/ultramafic contact. The presence of visible gold in sample 20PST 58 is a good interactor that the gold corridor is open along strike extending south into application E46/1355 (100% Thor Mining). The anticipated aeromagnetic data may assist with further delineation of the NE cross cutting structures which may be critical to gold mineralization. ROCK SAMPLING PROGRAM: In conjunction with the stream sediment program a small rock chip sampling program was undertaken in the central gold anomalous catchment zone identified during the past 2019 and 2020 sampling campaigns. A 1.5km traverse trending NE-SW was centred around 780500E/7586000N and up stream of past anomalous stream samples 20PST 14, 24, 29 34, with a total of 14 rock samples (20PST 1 to 14) collected. Geologically, the eastern portion of the traverse is dominated by a range of low hills of fine grained mafics and pillow lavas. The western portion comprises relatively flatter country with well exposed ultramafics. In contrast, a wide expanse in the central portion of the traverse is dominated by colluvial material composed predominately of quartz (quartz breccia, quartz with anhedral boxwork, yellow jarositic stained quartz and banded quartz/ironstone material), ironstone (generally massive with some skeletal /spongy textured ironstone), mafic and ultramafic fragments on soil. The majority of the rock samples collected along the traverse comprised colluvial float/scree material.