Lefroy Exploration Limited announced that a 6000m combined reverse circulation (RC) and diamond drilling program is underway at the Burns Prospect. Burns is within the Eastern Lefroy tenement package, which is part of the wholly owned greater Lefroy Gold Project (LGP) located 50km south east of Kalgoorlie. The Non-JV Eastern Lefroy tenement package covers 249km2. It now spans 40 strike kilometres from the Hang Glider Hill prospect in the north west as one contiguous wholly owned land package to Lake Randall in the south east. The Lefroy Gold Project in its entirety covers 621km2. The Burns Prospect lies within the Lake Randall Exploration Hub that is immediately south east of the Lucky Strike-Havelock-Erinmore BIF trends. The hub contains tenement E15/1715 that covers an area of approximately 20km2 containing the Burns gold-copper prospect that was discovered by Octagonal Resources Limited ("Octagonal") in 2011. The Burns gold copper prospect is situated on the eastern margin of a large interpreted felsic intrusion, termed the Burns Intrusion. The intrusion does not outcrop and has is represented by a distinctive annular aeromagnetic and gravity geophysical signature. The area was then identified as a priority exploration target area for greenstone hosted orogenic gold mineralisation based on targeting parameters developed by Western Mining Corporation (WMC) in the 1990's. Aircore drilling by WMC targeted the northwest and southeast margins of the Burns Intrusion with wide spaced aircore drilling, including drilling in Lake Randall. This drilling returned anomalous gold results that included 2m @2.67g/t Au in hole SAL746 at the Neon prospect on the north west margin of the intrusion. During 2007 to 2010 Newmont Australia (Newmont) recognised the geophysical character and gold prospectivity of the area from regional targeting and completed wide spaced aircore drilling. In May 2011 Octagonal Resources Limited (Octagonal) discovered significant gold and copper anomalism in the regolith (weathered rock) from aircore (AC) drilling. This defined a one square kilometre area of gold anomalism and a two-kilometre-long copper anomaly on the north eastern margin of the Burns Intrusion. This initiated subsequent multiple programs of reverse circulation (RC), diamond drilling (3 Holes) and geophysical surveys during the period 2012-2016. The drilling intersected broad zones of gold (Au) and copper (Cu) associated with magnetite-biotite alteration and hosted in high-magnesian basalt and intermediate intrusive rocks. Significant results from that program include: 9 metres @ 1.5 g/t Au & 1.0 % Cu from 58 metres in OBURC002. 12 metres @ 0.8 g/t Au & 1.7 % Cu from 48 metres in OBURC004. 4 metres @ 0.7 g/t Au & 2.0 % Cu from 40 metres in OBURC005. 1 metre @ 8.5 g/t Au & 6.7 % Cu from 123 metres in OBURC007. 32 metres @ 1.7 g/t Au & 0.6 % Cu from 76 metres in OBURC011. 6 metres @ 4.9 g/t Au & 0.9 % Cu from 24 metres in OBURC012. 50 metre @ 0.9 g/t Au & 0.5 % Cu from 24 metres in OBURC016. 12 metres @ 1.5 g/t Au & 0.5 % Cu from 27 metres in OBURC021. 19 metres @ 0.5 g/t Au & 1.0 % Cu from 44 metres in OBURC022. 9 metres @ 1.0 g/t Au & 0.7 % Cu from 28 metres in OBURC025. 3 metres @ 16.1 g/t Au & 0.5 % Cu from 35 metres in OBURC028. 9 metres @ 1.0 g/t Au & 1.5 % Cu from 115 metres in OBURC031 and 12 metres @ 1.3 g/t Au & 0.8 % Cu from 163 metres in OBURC032. In June 2014 Octagonal completed one diamond hole (OBUDD001), for 401.5m at Burns to test for the source of a strong magnetic anomaly defined by 3D inversion modelling of ground magnetic data. The drill hole was orientated away from the intrusion and intersected strongly fractured high- magnesian basalt intruded by multiple feldspar porphyritic rocks.