Rumble Resources Limited announced it has completed RC drilling on the Earaheedy Project (E69/3464) with results highlighting two large-scale (large tonnage), flat lying, shallow sandstone hosted Zn­Pb discoveries. Earaheedy Project ­ Sandstone Hosted Zn-Pb Mineralisation: The Earaheedy Project is located approximately 110km north of Wiluna, Western Australia. Rumble owns 75% of E69/3464 and Zenith Minerals Ltd. owns 25%. Rumble has three (100% RTR) contiguous exploration licence applications ELA69/3743, ELA69/3745 and ELA69/3746. The project area covers the inferred unconformity contact between the overlying Frere Iron Formation and underlying Yelma Formation of the Palaeoproterozoic Earaheedy Basin. The new style of Zn-Pb mineralisation has been delineated on the unconformity contact between the overlying Frere Iron Formation and underlying Navajoh Dolomite and shale of the Yelma Formation. Both formations are part of the lower units of the Palaeoproterozoic Earaheedy Basin. Drilling (current and historic) has intercepted flat lying porous sandstone to grit unit that has been interpreted to be the basal unit of the Frere Iron formation that lies unconformably over the Yelma Formation. The unconformity in general dips between 5 - 10° to the northeast. Sphalerite, galena and pyrite have replaced the matrix (pore) space within the porous sandstone grit host forming laterally extensive sulphide layers. RC Drilling Programme Completed by Rumble: The RC drilling programme comprised of 19 drill holes (1518m total) targeting the interpreted up-dip position of the prospective unconformity related basal sandstone sub-basin. No previous drilling has tested this position. The two areas tested are some 10km apart. The drilling tested along strike on 500m hole spacing. To aid with targeting (shallow cover ­ to 5m), recent passive seismic survey traverses, completed by Rumble, were used to target the inferred surface expression of the prospective sandstone unit. Drill holes were vertical, ranging from 60 to 108m depth. Assaying (wet analysis) was based on systematic on-site pXRF assaying of the RC drill hole cuttings. If the pXRF response was >1000ppm Zn, the sample(s) was submitted for four acid digest multi-element analysis. Results: The current RC drilling has defined two areas of significant Zn Pb mineralisation, Chinook and Magazine, associated with flat to slightly northeast dipping sandstone units. The sandstone units are the basal unconformity to the overlying Frere Iron Formation. Note that all mineralisation defined at Earaheedy is blind. Chinook Prospect: Three RC drill holes drilled 500m apart returned significant flat lying Zn ­ Pb with Ag mineralisation. EHRC019 ­ 11m @ 3.35% Zn, 0.78% Pb, 12.78 g/t Ag (4.13% Zn + Pb) from 61m a broader zone of 22m @ 2.04% Zn, 0.48% Pb (2.52% Zn + Pb) from 53m. EHRC018 ­ 5m @ 1.68% Zn, 0.15% Pb (1.83% Zn + Pb) from 72m. EHRC020 ­ 12m @ 0.48% Zn, 0.72% Pb, 1.4 g/t Ag (1.2% Zn + Pb) from 43m. Drilling has defined strong continuity of flat lying mineralisation over 1000m of strike and in association with historic drilling has demonstrated strong continuity normal to strike. Historic RC drill holes TRC65 and TRC70 returned very significant mineralisation. TRC65 ­ 7m @ 3.57% Zn + Pb from 60m. TRC70 ­ 5m @ 3.55% Zn + Pb from 126m to EOH (note EOH assay of 6.18% Zn + Pb).