Legend Mining Limited reported geology, DHTEM and assay results from the latest diamond drillholes at its Mawson nickel-copper-cobalt prospect within the Rockford Project, Fraser Range, Western Australia. Comprehensive details are contained in the body of this report. Systematic step-out diamond drilling continues to grow the Mawson intrusion to the north-east, intersecting fertile intrusion as well as defining the architecture of the Mawson intrusion in relation to the country rock. The evolving understanding of the Mawson structural architecture has resulted in the potential identification of trap sites for massive Ni-Cu sulphide accumulations in this north-east zone. The 3D model driving predictive exploration at Mawson continues to evolve with new data and continues to be very accurate as a predictive tool for targeting interpreted fertile intrusion. The updated 3D constrained gravity model at this stage appears to have a high correlation for mineralised intrusion. To date, the mineralised intrusive footprint at Mawson extends over 1.4km in strike length, with the gravity model suggesting the intrusion extends over 3km in strike length. Ongoing drilling across Mawson will focus on continued definition of these mineralised intrusive bodies and targeting of structural trap sites for massive Ni-Cu sulphide accumulation. Section 6,599,000mN: Diamond drillhole RKDD065 was completed 200m east of RKDD042, designed to extend the mineralised chonolith to the interpreted eastern margin of the Mawson intrusion. The drillhole also provided a point location test of a series of complex DHTEM and MLTEM conductors interpreted to be the D3 stratigraphic conductor. RKDD065 encountered a dominantly mafic sequence with minor interleaved ultramafic zones of the chonolith below a metasedimentary hanging wall sequence of meta-pelite before entering a variably mineralised intrusive, dominantly ultramafic, from 280.36m to 391.56m downhole. The hole then entered the footwall sequence of recrystallised mafic intrusives before finishing in a faulted metasedimentary package including graphitic and sulphidic zones to end of hole at 554.2m. The graphitic and sulphidic zones are interpreted to represent a complex set of EM conductors associated with stratigraphic conductor D3. The mineralised intrusion in close proximity to these complex conductors confirms the current working model at Mawson that Ni-Cu sulphide mineralisation can be masked in the EM shadow of these highly conductive stratigraphic features. Section 6,599,200mN: Diamond drillhole RKDD064 has been completed 400m east of RKDD044. Drilling continues to target the interpreted northern extension of the Mawson chonolith with RKDD064 designed to extend the mineralised chonolith to the interpreted eastern margin of the Mawson intrusion on this section. The drillhole also provided a point location test of a series of complex DHTEM and MLTEM conductors interpreted to be the D3 stratigraphic conductor. RKDD064 intersected a series of thick ultramafic units bounded by thin units of mafic interpreted to be a significant thickening of the ultramafic chonolith core. The chonolith is over 400m in vertical thickness in RKDD064, with the dominantly ultramafic component being the thickest intersection to date at Mawson. The chonolith finished at 406.84m downhole, where the drilllhole entered a complex zone of interleaved graphitic metasediments, amphibolites, and small mafic intrusions to 624.5m. The retrogressive amphibolites encountered are indicative of the margin of the Mawson intrusion. The graphitic zones intersected are interpreted to represent a complex set of EM conductors associated with stratigraphic conductor D3. Section 6,599,400mN: Four diamond drillholes have been completed on this section, continuing to follow the interpreted mineralised chonolith to the north-east corner of the Mawson intrusion. RKDD056 intersected thin zones of mafic chonolith at the top and bottom of the hole either side of a thickened zone of metasedimentary units. The chonolith remains open to the west. RKDD062 intersected a variably mineralised mafic zone of the chonolith before finishing in a metasedimentary package to 381.3m downhole. Subsequent DHTEM on RKDD062 resulted in a series of discrete offhole conductors, interpreted to be within the chonolith. RKDD069 was designed to target these offhole conductors. RKDD069 was drilled to 345.1m and intersected mafic chonolith up to the DMTEM conductors before intersecting highly sulphidic meta-BIF, interpreted to be the conductors. These internal meta-BIF units are interpreted to be rafts of country rock caught up during the chonolith emplacement RKDD063 drilled 200m east of RKDD062 encountered an increased thickness of mafic chonolith with minor disseminated mineralisation. RKDD066 drilled 200m east of RKDD063 intersected a thickened ultramafic unit bound by thinner mafic, interpreted to be the extension of the thickened ultramafic core of the chonolith seen on section 6,599,200mN. Minor dissemination was logged in the ultramafic. The chonolith remains open to the west, east, and north. DHTEM is pending on RKDD066. Section 6,599,600mN: Four diamond drillholes have been completed on this section, continuing to follow the interpreted mineralised chonolith to the north-east corner of the Mawson intrusion. RKDD068 intersected a thickened package of metasediments of dominantly pelite, meta-BIF and meta-conglomerate. Structural logging will determine the significance of this thickened package once additional drillholes are completed on this section. RKDD070 intersected dominantly gneissic, meta-BIF, meta conglomerate, and metasedimentary lithologies with interleaved norite intrusion between 290m and 396m downhole. The hole is currently undergoing detailed structural logging and is interpreted to be near the intrusion margin. DHTEM is now scheduled. RKDD071 intersected multiple intervals of Ni-Cu mineralised mafic and ultramafic chonolith from 99.26m through to 207.18m downhole before finishing in a metasedimentary package of dominantly pelite, meta conglomerate, and meta-BIF at 363.2m. Mineralisation ranged from disseminated to net textured sulphide throughout the intrusive sequence. Structural interpretation suggests the Ni-Cu mineralisation encountered in RKDD071 is the continuation of the mineralisation intersected in RKDD044 located 400m south-west. This is based on structural vectoring, which continues to prove a positive targeting tool. DHTEM is now scheduled to search for offhole conductors related to the mineralisation encountered in-hole. RKDD072 intersected a meta-BIF and metasedimentary package down to 477.7m bottom of hole. The current interpretation is that RKDD072 represents an internal raft of thickened country rock or is the northern margin of the Mawson intrusion in this location. DHTEM is now scheduled.