Ora Gold Limited (Ora or the Company) advised that it is undertaking a follow up drilling campaign at the Crown Prince Prospect within the Company's broader Garden Gully Project. The program is set to continue for several weeks. Assays and interpretations will be released as they become available.

Further to the Company's recent exploration announcements outlining a new high-grade zone at Crown Prince. Ora is commencing a 5,000m combined RC and diamond drilling program targeting the newly delineated mineralized zone to the south east of the known gold resource. Strongly mineralized intercepts recorded in the recent drilling include 20m @ 14.49g/t Au (from 30m, OGGAC456), and 17m @ 10.73 g/t Au (from 28m, OGGAC457).

The Crown Prince mineral resource currently stands at 479,000t at 3.6g/t Au for a total of 55,000 ounces Au. The Garden Gully Gold Project comprises a 217km2 package of tenements held by Ora which cover the majority of the Abbots Greenstone Belt, to the north west of Meekatharra in Western Australia. The most advanced prospect within the broader project is Crown Prince which is located 16kms north of Meekatharra.

Crown Prince is the site of small-scale historic mining (Kyarra Gold Mine) and is on a granted mining lease (M51/886). Regional Geology The north-north easterly trending Abbotts Greenstone Belt, comprises a succession of metamorphosed komatiitic and tholeitic volcanics with interflow sediments. The volcanic sequence is overlain by felsic volcanic and epiclastic rocks with sulphidic black shale horizons.

Intrusions of differentiated ultramafic to mafic sills intrude the entire sequence. Along its south eastern margin, the belt is attenuated in the south westerly and north easterly directions by a zone of deformation near the contact with external granitoids, interpreted on the basis of magnetic data to be associated with the regionally significant Abernethy Shear Zone that has been shown by drilling to be associated with gold mineralisation. Several strike slip faults are also present within the stratigraphy and may represent the northern extension of a major structure which passes through the Big Bell deposit.

Locally, mineralisation at Crown Prince is hosted within WNW ­ ESE striking (steep southerly dip) quartz rich lodes. These lodes are offset by N-S to NNE trending shears, which are interpreted to have a near vertical dip or to dip steeply to the west. Movement along the shears is dextral, displacing mineralisation with offsets of around 100 metres.

In fresh rock, gold mineralisation occurs in quartz veins hosted by chloritized, carbonated and strongly sheared meta-basalt, dolerite, black shale units and quartz porphyry, showing strong sericite-carbonate alteration in the vicinity of the quartz veins. Some gold mineralisation occurs in the near surface indurated and saprolitic layers in the lateritic profile as supergene mineralisation. Drill Targeting A series of RC holes have been planned to target a newly delineated zone of mineralisation (SEB) which is offset to the south east of the main ore body (MOB).

The MOB and SEB lodes are interpreted to be on either side of a N-S trending shear zone which has dextrally offset the lodes. Planned RC drilling to the south east of the MOB is therefore targeting mineralization in a shallow and high position (i.e. in the hanging wall) refer. A further focus area for resource growth is a high-grade intersection zone between the northern ore body (NOB) and the MOB.

This grade enrichment is evident in resource modelling and is interpreted to occur where the more northerly striking NOB lode intersects the NW striking MOB lode. RC and diamond drilling is planned to target this high grade zone and to test plunge continuity both up and down plunge. The zone of high grade is interpreted to run up to bounding N-S trending offsetting shears.

The location of these boundaries will be better constrained by this round of drilling with extensions to high-grade zones expected.