Caeneus Minerals Limited confirmed the successful completion of its maiden drilling program at its Roberts Hill project in the highly prospective Mallina Basin, Pilbara WA. A total of 197 air-core drill holes were completed for 15,999 metres of drilling. In this first air-core program, six (6) prospective areas were drilled, essentially on 300 metre spacings to understand the nature and structure of the underlying lithologies. The Company has been highly encouraged with 84 of the 197 drill holes ending in an accumulation of sulphides, remarks on each of these drill holes are included in table 1 of this announcement. A summary of observations from each designated zone is also included below. Zone A: Zone A appears to be an anticlinal structure some 2 square kilometres in area, with a gentle plunge to the south-south-east. The eastern flank of the anticlinal structure exhibits an irregular shaped apophysis clearly identifiable from the Company's recent low level airborne geophysical survey. Zones B, C and D. Drilling in this location focussed on two features; a compelling potential NNW trending structural corridor over 5 kilometres wide (Zones B and C) and a N-S trending potentially intrusive feature (Zone D) to the west. Detailed geological logging and petrology on some air-core samples in this location is still in progress and interpretation is expected to take additional time due to the nature and complexity of the lithologies intersected. A highlight from the drilling in this location was a 28m intersection of abundant coarse sized mixed sulphides from hole RHAC-0104 at Zone C. From 85m to the end of hole (113m) abundant pyrite, pyrrhotite and traces of a silvery sulphide, most likely arsenopyrite were observed initially within pelitic sediments and then terminating in a granitic rock. Zone E: This locality contains a magnetically discrete, arcuate intrusive feature approximately 7 kilometres in length and variable thicknesses. Whilst the western portion of the Roberts Hill tenement is generally overlain by 20 metre-plus thicknesses of overburden, Zone E surprisingly contains sporadic outcrop. Lithologies identified were pelitic and amphibolitic schists and a strongly brecciated, calcified and silica- rich intrusive rock with abundant pseudomorphs most probably after sulphides. Drilling over this locality confirmed the presence at depth of all the above lithologies with extensive quartz veination noted and the presence of fresh sulphides in granodiorite-type rocks. Many drill holes bottomed in pyrite/sulphide accumulations. As with Zones B, C and D, logging and petrological investigations at Zone E are ongoing. Zone F: Air-core drilling at Zone F focussed on a west-north-westerly trending structural feature identified from the Company's earlier aeromagnetic survey. Logging is still in progress.