DRILLING INTERSECTS TWO SIGNIFICANT SULPHIDE ZONES AT UBEONG PROJECT IN SOUTH KOREA AMENDED

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1 24 November 2017 DRILLING INTERSECTS TWO SIGNIFICANT SULPHIDE ZONES AT UBEONG PROJECT IN SOUTH KOREA AMENDED Diamond drillhole UBD0002 D1, in progress, has intersected two significant zones of sulphide mineralisation correlating with the Taipan and Cobra target zones at the Ubeong Project: i) a 90m zone from 25.9m of skarn mineralisation with variably disseminated sulphides including sphalerite (Zn), arsenopyrite and trace galena (Pb) in the Taipan target zone, ii) a 5.5m quartz-sulphide lode from 334.5m including coarse arsenopyrite and spot XRF readings up to 931 g/t silver, 0.46% Cu and 0.28% Zn in the Cobra target zone The next drillhole (UBD0003) will test south through a coincident electromagnetic (EM) and Induced Polarisation (IP) chargeability sulphide target then continue to test under workings with a previous massive sphalerite channel sample result of 27.9% Zn, 958 g/t silver (Ag) D2 Peninsula Mines Limited ( Peninsula or the Company ) is pleased to provide an update on the diamond drilling that is testing the Taipan and Cobra targets in the Chilbo historical workings area of the Ubeong Project in South Korea (see Figure 1 for location). Shallow angle drillhole, UBD0002, drilled north on section 513,500mE (see Figures 2 and 3), has intersected a 90m zone from 25.9m of skarnified limestone with variably disseminated sulphides including blebs of sphalerite (Zn), patches of arsenopyrite (silver association) and trace galena (Pb) (see Photo 1) through the Taipan target zone (see summary Table 1). The drillhole, UBD0002, then intersected a zone of difficult drilling in pelitic sedimentary rocks before intersecting a down hole width of 5.5m quartzsulphide lode (with coarse arsenopyrite) from 334.5m (see Photo 2) in the Cobra target zone (see summary Table 1). Spot hand-held XRF readings were taken from the quartz-sulphide lode at Cobra have produced results of up to 931 g/t Ag (associated with coarse Figure 1: Project location arsenopyrite), and on the northern side of the lode, up to 0.28% Zn and 0.46% Copper (Cu). Hand-held XRF readings are an indication of mineralisation only and full elemental analyses at ALS in Perth will now be required. UBD0002 was terminated at 394.8m down hole. Drilling of the next drillhole (UBD0003) will commence shortly. The next hole, UBD0003, will be drilled at a moderate angle (-40 ) south on section 513,600mE and test a coincident electromagnetic (EM) and Induced Polarisation (IP) chargeability anomaly obscured by colluvial scree at the base of the valley (see Figures 2 and 3). This EM/IP anomaly represents a massive sulphide target that may link to the outcropping Viper, copper-bearing, massive sulphide zone D3 to the northeast. The hole will then continue to test across the mineralised limestone skarn under previously sampled workings that produced a channel sample result of 27.9% Zn, 958 g/t Silver (Ag) D2 from a steeply dipping sulphide lode close to the southern margin of the skarn-limestone unit. Drillhole details are tabled in Appendix 1.

2 Page 2 of 35 Taipan Cobra UBD0002 Figures 2 & 3: Plan of EM, IP ChargeabilityD10, soil-rockchip geochem (Zn) & Cross Section through 513,500mE Hand held XRF measurements on drillcore from UBD0002 are in progress, prior to completion of logging, selected core cutting and full elemental sample analyses for elements including for Zn, Pb, Cu, Ag and gold (Au) for selected zones. Results will be reported in due course. patchy arsenopyrite disseminated sphalerite Photo 1: UBD0002, 111.8m to 112m, disseminated arsenopyrite & sphalerite in skarn-limestone, Taipan coarse arsenopyrite Photo 2: UBD0002, 337.6m to 337.8m, coarse sulphide (arsenopyrite) in quartz-carbonate lode, Cobra

3 Page 3 of 35 Table 1: UBD002, significant intervals of sulphides with nature, minerals & abundance (see details Appendices 1 & 2) HoleID From To Interval Lithology Comment UBD Skarn Limestone UBD Skarn limestone Minor blebby arsenopyrite and sphalerite, tr galena UBD Fault zone/pelite UBD Skarn limestone Minor blebby arsenopyrite and sphalerite UBD Limestone/Skarn UBD Limestone/Marble UBD Limestone/Marble Blebby pyrite and pyrrhotite UBD Marble UBD Psammopelite/Faults UBD Fault zone Skarn limestone/calc- UBD Silicate Wollastonite alteration and diopside UBD Fault zone Skarnified limestone/brecciated quartz vein in fault UBD Pelite Pelite flooded by quartz UBD Quartz sulphide lode Quartz vein with medium to coarse arsenopyrite, tr Cu, Zn UBD Pelite Pelite flooded by quartz UBD Quartzite Micaceous sericitic quartzite Background to the Ubeong Zinc-Silver and Copper-Gold Project Peninsula has secured six granted tenements and multiple tenement applications over the eastern 10- kilometre strike length of a highly prospective, limestone-skarn unit that includes the historical Chilbo mine workings and adjoins the operating Keumho Zinc-Lead-Silver Mine (see Figure 4 below). Tenements and applications have also been secured over a southern trend of workings at Ilweol. High-grade zinc-lead-silver and copper-gold D2,D3,D4,D8,D9 rockchip and channel sampling results have been produced from the Chilbo workings area that occurs towards the eastern end of the limestone skarn unit, associated with an extensively faulted zone that has offset the unit and is interpreted to have acted as a conduit for mineralisation. The Company has also carried out detailed mapping, ground-based geophysical programmes (magnetics, electromagnetics and induced polarisation (IP) D10 surveys) and detailed soil sampling programmes, that have defined multiple drilling targets for a drilling programme that is in progress, testing targets for disseminated to massive sulphide zinc-lead-silver +/- copper-gold mineralisation.

4 Page 4 of 35 Keumho Operating Mine H78 Chilbo Historical Mining Area D72 Figure 4: Ubeong Project, rockchip sample results (Zn) on TMI airborne D11, D12 and ground magnetics with granted tenements and tenement applications For further information please contact: Jon Dugdale Managing Director Phone: jdugdale@peninsulamines.com.au About Peninsula Mines Peninsula Mines Ltd is an Australian listed, exploration/development company focused on developing the outstanding opportunities for mineral discovery within South Korea. Peninsula s strategy is to focus on mineral commodities that have a positive price outlook and offer potential for off-take and/or strategic partnerships in-country. The Company is advancing a highly prospective zinc-lead-silver and copper-gold project at Ubeong in eastern South Korea, and also has a dual focus on advancing a series of flake-graphite projects, that offer potential to be advanced and developed to supply high technology, lithium-ion battery and/or expandable graphite applications for which South Korea is the major global end-user.

5 Page 5 of 35 The material and/or releases referenced in this release are listed below: D1 Drilling commenced to test Cu-Au and Zn-Ag targets at Ubeong, 26/09/17 D2 Exceptional zinc-silver grades with copper & gold from surface sampling at Ubeong, 23/05/17 D3 Massive sulphide copper-gold zone discovered in outcrop at Ubeong Project, 06/07/17 D4 High-grade silver-gold-zinc rockchip results, Ubeong Project, South Korea, 26/04/17 D5 Three key tenements granted, Ubeong Zinc Project, 28/03/17 D6 Zinc project fast-tracked for drill targeting after exceptional soil sampling results, 9/03/17 D7 Major zinc-skarn district identified at Ubeong Project in South Korea, 13/12/16 D8 Further exceptionally high-grade zinc-silver results from Ubeong Project, South Korea, 31/10/16 D9 Exceptional zinc-silver-lead grades from newly acquired Ubeong Project, South Korea, 13/9/16 D10 IP survey identifies very strong sulphide targets at Ubeong, 12/07/17 D11 Koo, S,B., Park, Y.S., Lim, M.T., Rim, H.R., Lee, H.I., Sung, N.H., Choi, J,H. and Koo., J.H., 2008, KIGAM 1:100,000 Socheon Aeromagnetic Contour Image. D12 Kim, O.J., Hong, M.S., Park, H.I. and Kim, K.T., 1963, KIGAM 1:50,000 Samgeunri Geology Sheet and Dogyedong Geology Sheet. For full versions of the Company s releases see Peninsula s website Forward looking Statements: This release contains certain forward-looking statements. These forward-looking statements are not historical facts but rather are based on Peninsula Mines Ltd s current expectations, estimates and projections about the industry in which Peninsula Mines Ltd operates, and beliefs and assumptions regarding Peninsula Mines Ltd s future performance. Words such as anticipates, expects, intends, plans, believes, seeks, estimates potential and similar expressions are intended to identify forward-looking statements. These statements are not guarantees of future performance and are subject to known and unknown risks, uncertainties and other factors, some of which are beyond the control of Peninsula Mines Ltd, are difficult to predict and could cause actual results to differ materially from those expressed or forecasted in the forward-looking statements. Peninsula Mines Ltd cautions shareholders and prospective shareholders not to place undue reliance on these forwardlooking statements, which reflect the view of Peninsula Mines Ltd only as of the date of this release. The forward-looking statements made in this release relate only to events as of the date on which the statements are made. Peninsula Mines Ltd does not undertake any obligation to release publicly any revisions or updates to these forward-looking statements to reflect events, circumstances or unanticipated events occurring after the date of this presentation except as required by law or by any appropriate regulatory authority. Competent Persons Statement: The information in this release that relates to Exploration Results, Mineral Resources or Ore Reserves is based on information compiled by Mr Daniel Noonan, a Member of the Australian Institute of Mining and Metallurgy. Mr Noonan is an Executive Director of the Company. Mr Noonan has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Noonan consents to the inclusion in the release of the matters based on this information in the form and context in which it appears. The information in this release that relates to Geophysical Results and Interpretations is based on information compiled by Mr William Peters, a Consulting Geophysicist (Crosmin Pty Ltd) at Southern Geoscience Consultants. Mr Peters is a Fellow of the Australasian Institute of Mining and Metallurgy and Chartered Professional (Geology) and has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Peters consents to the inclusion in the release of the matters based on this information in the form and context in which it appears.

6 Page 6 of 35 JORC Code, 2012 Edition: Table 1 Section 1: Sampling Techniques and Data (Criteria in this section apply to all succeeding sections.) Sampling techniques Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. An Olympus Innovx Delta Premium hand-held XRF unit was used to take spot XRF readings of a selected suite of elements at 10cm intervals along the drill core. The reading points were marked up with a crayon and then read for 60 seconds. The reading number and matching interval were noted in a notebook and later transcribed into an excel spreadsheet and matched with the downloaded data from the XRF unit. The XRF data was collected to aid in the selection of intervals for detailed laboratory analysis. The XRF data is not intended for use in any future resource estimation. A selection of some of the best XRF readings were reported in this release. Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. Aspects of the determination of mineralisation that are material to the Public Report. In cases where industry standard work has been done this would be relatively simple (e.g. reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay ). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information. To avoid bias the XRF readings were taken at an even spacing down the drill run at the highest point on the cores curvature facing the sampler to ensure consistency between readings. The drilling undertaken at the Chilbo Prospect has all been diamond drilling. As stated previously XRF readings were taken at regular 10cm intervals along the drill run and the depth of the readings recorded in a notebook. These were taken purely to assess the nature of the mineralisation and follow-up diamond saw core cutting is planned with aim of completing half core sampling of targeted intervals. The sulphides in the broad 90m skarn altered zone from 25.9m occur as disseminated blebby sulphides 1 to 5mm in diameter. Commonly the sulphide blebs occur along bedding planes. In places small sulphide veinlets are developed generally subparallel with the bedding foliation but on occasions crosscutting the foliation at a high angle, 60 to 70 degrees. The dominant sulphide species are pyrite and pyrrhotite with lesser arsenopyrite and sphalerite and vert occasional bleb of galena. Through the 90m skarnified zone arsenopyrite might average 0.02%, sphalerite 0.01%, pyrite 0.04% and pyrrhotite 0.03%. The mineralised quartz vein zone from 334.5m is characterised by coarse 3 to 25mm crystals of arsenopyrite commonly in large masses up to 5 to 10cm long. Outside the main quartz vein beyond 340m less commonly isolated disseminated sulphide crystals occur aligned with the bedding foliation or as narrow cross cutting veinlets. Within the 5.5m down hole width quartz vein from 334.5m the sulphide abundances are estimated as arsenopyrite 5%, Pyrite 0.01% and chalcopyrite 0.001%.

7 Page 7 of 35 Drilling techniques Drill sample recovery Logging Subsampling techniques and sample preparation Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of diamond tails, facesampling bit or other type, whether core is oriented and if so, by what method, etc). Method of recording and assessing core and chip sample recoveries and results assessed. Measures taken to maximise sample recovery and ensure representative nature of the samples. Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. The total length and percentage of the relevant intersections logged. If core, whether cut or sawn and whether quarter, half or all core taken. If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. The drilling at the Chilbo Prospect, Ubeong Project is all diamond drilling. A short HQ pre-collar was drilled to 11.5m with no core recovered from this weathered zone of soil and historic mine dump material. The hole was then drilled with Q3 (50mmm diameter) size core to m before the hole was cased off due to issues with extreme water loss in a zone of highly fractured pelitic and psammopelitic metasediments. The hole has then been drilled with BQ core to end of hole. The Q3 drilling was all triple tube drilling with areas of core loss mainly the result of excessive core grinding in places and washing away of fine clays around faults. The core loss was 18.8m in total over the first 257m of the hole or 88% recovery. Recovery has improved since the step down to BQ sized core with less core grinding occurring and core losses reduced especially after the hole passed through a fault zone from to 332.3m. Post the fault the coring has been in a more robust mineralised quartz vein and weakly mineralised micaceous quartzite until end of hole. There does not appear to be any grade relationship to zones of core loss with the bulk of the loss being random and most likely attributable to poor drilling technique. The Ubeong drill hole is still being drilled and core logging is ongoing. The hole has been logged to generate extensive structural data from core orientated using a Devicore core orientation device. In addition, all the intervals have been geotechnically logged to allow full Q system geotechnical appraisal to be performed at some future date. Each interval is geologically logged for lithology and mineral abundances and alteration type. The aim being to generate data suitable for the use in any future Mineral Resource Estimation. The data collected is both quantitative and qualitative in nature. The full hole has been logged with selected intervals being marked up for diamond core cutting and subsequent sampling that is anticipated to commence early next month post the completion of the detailed geological logging of the current hole. No core has been sampled at this stage though spot hand-held XRF measurements are being taken at 10cm intervals to assist with the selection of intervals for assay. It is intended that the core will be cut in half at the Company s sample preparation facility using the company s diamond saw. To this end all the core is being marked up with a dedicated cut line in place to preserve the bottom of hole core orientation line for possible future reference. The drill core will be cut in half with a diamond saw except in the case of repeat sampling when quarter core samples will e analysed.

8 Page 8 of 35 For all sample types, the nature, quality and appropriateness of the sample preparation technique. No drill core has been sampled or analysed at this point in time. The selected spot hand held XRF analyses at 10cm intervals has been undertaken to help guide in the selection of intervals for core cutting and full assay in Perth. Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. No QA/QC procedures have been adopted for the spot XRF analyses. The XRF instrument undergoes a calibration check each morning prior to its use for any core spot analyses. Quality of assay data and laboratory tests Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling. Whether sample sizes are appropriate to the grain size of the material being sampled. The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. By taking measurements at the same point on the core and at 10cm intervals regardless of where the best mineralisation may be visible in the core helps to minimise any sampling bias during the XRF analysis process. It is intended that all zones with elevated base metal XRF results will be sawn in half with the non-base of hole core piece kept as a permanent record and the other half sent to ALS Perth for assay. The XRF sampling is non-destructive point sampling at regular intervals down the drill core. The XRF unit only analyses a small window <1cm in diameter. No drill core has been cut or sampled nor analysed at this point in time. The XRF analyses are purely point readings to help in the selection of intervals for assay. The XRF data should only be considered as providing an indication of the potential grade of the drill interval sampled. At best it is a partial analysis. For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivations, etc. The release includes a portion of the Socheon 1:100,000 Total Magnetic Airborne Magnetic Imagery (Figure 4) D10. The Company purchased this image along with other images produced by the Korea Institute of Geoscience and Mineral Resources (KIGAM) as part of the country wide aeromagnetic atlas (Published Dec 2008). The Company has received permission from KIGAM management permitting the use of the KIGAM magnetic images in its ASX announcements, shareholder communications and corporate presentations. The magnetic survey was undertaken by KIGAM using a Geometrics G-813 Proton Magnetometer. The flight lines were flown East-West at a 1 km line spacing with North-South tie lines flown at a 5 km spacing. The flight altitude for the survey was m above ground level. The data processing involved setting the data level at 300m above mean sea level by

9 Page 9 of 35 upward/downward continuation. The International Geomagnetic Reference Field (IGRF) was used to assist with the removal of total magnetic anomaly. The KIGAM colour total magnetic contour maps are printed at 1:100,000 scale and referenced using the Bessel ellipsoid and the Tokyo datum with latitude and longitude coordinate marked. Figure 2 shows a portion of the trial Fixed Loop EM survey conducted by Southern Geosciences at the Chilbo Prospect in November The sulphides at the Chilbo Prospect were found to generally be unresponsive to EM and so the decision was made to do follow-up IP geophysical survey in July The EM survey did return a low level EM response along the main access valley and as part of the planned drilling of UBD0003 this EM response will be tested. Verification of sampling and assaying Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. The verification of significant intersections by either independent or alternative company personnel. No blanks or CRM samples were analysed during the spot XRF readings undertaken on hole UBD0002. The company intends to include standards, blanks and undertake regular repeat sampling during the formal assaying of the drill core. No intercepts have been reported just commentary on spot XRF readings. None of the results reported or commented upon in this release have been independently checked by non-company personnel. This is not considered material at this early reconnaissance stage of the project s evaluation. The use of twinned holes. Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. This is the company s first phase of drilling at the Ubeong Project and at this stage no holes have been twinned. Assay results are stored in an Excel database. All results are checked by the responsible geologist on entry to the database. The Company s data is stored in an excel database and routinely transferred to the Perth Head Office. Location of data points Discuss any adjustment to assay data. Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. The data presented in the Appendices is drill hole location data and a tabulation of the spot XRF readings. Drill holes will all be down hole surveyed. The collar locations and starting azimuth confirmed using a DGPS unit provided by an independent contract surveyor. The collar details for hole UBD0002 are provisional and -held Garmin GPS data points. The location of hole UBD0001 has been surveyed by a contract surveyor using a DGPS unit.

10 Page 10 of 35 Specification of the grid system used. All sample sites were surveyed in the UTM WGS84 zone 52N coordinate system or WGS 84 Latitudes and Longitudes. Data spacing and distribution Quality and adequacy of topographic control. Data spacing for reporting of Exploration Results. Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. Whether sample compositing has been applied. The National Geographic Information Institute (NGII) has 1:5,000 scale digital contour data for the entire country. The diamond drilling is being undertaken to standards that will allow any assay results and geological and geotechnical information to be used in the generation of a future Mineral Resource but at this stage it is too early in the exploratory phase to say whether this work will ultimately lead to the definition of a Mineral Resource. This first phase of drilling is purely exploration drilling and it is too early to say whether this will lead to the eventual definition of a Mineral Resource. None of the XRF results have been composited. Orientation of data in relation to geological structure Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. The structural orientation data being generated from this first phase of drilling will be used to help design future drill holes at the Chilbo prospect. Sample security If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. The measures taken to ensure sample security. The drilling from hole UBD0002 has been designed to intersect the interpreted structures as close to normal as practically possible given drill rig limitations and the nature of the topography. The data obtained to date suggests that the weakly mineralised zone from 26 to 116m down hole was intersected at an angle for 60 to 70 degrees to the bedding of the host skarn limestone unit. The XRF data is downloaded directly from the instrument to a text file and then matched in an excel spreadsheet with the measured depths via the recorded reading number. This excel data is then transferred electronically to the Perth office. Audits or reviews The results of any audits or reviews of sampling techniques and data. No audits have been undertaken of the XRF procedure at this stage.

11 Page 11 of 35 (Criteria in this section apply to all succeeding sections.) Section 2: Reporting of Exploration Results (Criteria listed in the preceding section also apply to this section.) Tenement and land tenure status Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. On 27 th April 2017, MDS covering the historic Chilbo mine workings blocks Hyeondong 59, 60 and 69 were accepted and the Company was formally granted the exploration rights for up to 7 years over these three titles D4. In addition, in mid-june 2017, the MDS field survey was completed over blocks Hyeondong 70 and 78 and MDS reports have been filed with the Ministry of Trade, Industry and Energy (MOTIE) for the grant of these blocks. On the 25 th August 2017, the company was formally granted title for exploration over these 2 blocks D5. SMCL, was granted tenure over Dogyedong 72 tenement that covers the main Ilweol prospects on the 27 th September A MDS survey has recently been completed over the adjoining block Dogyedong 82 following the discovery of the recently sampled underground workings. An additional 22 applications have been renewed over surrounding blocks considered prospective for identifying blind zinc mineralisation. The formal grant of title gives the Company the exploration rights for up to 7 years over the title. Exploration rights are granted by commodity for tenement blocks defined by the GRS080 grid system over 1x1 minute graticule blocks. The Ministry of Trade, Industry and Energy (MOTIE) reviews the MDS report and if satisfied, will issue an exploration right. The Company has been granted tenure for 6 months and is required to submit an MDS report for each of the 22 applied tenements prior to the end of the 6 month application period. In the case of Hyeondong 68 and Dogyedong 82 the company is awaiting the Ministry s evaluation of the MDS application. If the MDS report is accepted by the Ministry, the Company will be granted Mining rights over the applied tenement for a further 3 years. Following the successful filing of the MDS, the applicant is required to file a Prospecting Application (PA). The PA report details the planned exploration activities to be completed over the tenement during the 3 year prospecting period. This includes the completion of a minimum quantum of geophysical surveys, geochemical surveys or drilling as defined under the Mines Act. Provided that at least 50% of the statutory requirement is completed within the initial 3 year

12 Page 12 of 35 prospecting period, the tenement holder is entitled to apply for an additional 3 year extension to facilitate the completion of the specified exploration programme. A Prospecting Report must then be submitted to the Ministry at the completion of the exploration programme. The tenement holder must then submit a Mine Planning Application (MPA) to the local Government Authority who will, if the MPA is approved, grant tenure for mining for a period of 20 years subject to statutory requirements as set out under the terms of the MPA approval. The applicant holding a Mining Right can apply for extensions provided all statutory requirements have been met over the life of the mine. Exploration done by other parties Acknowledgement and appraisal of exploration by other parties. The Company is currently translating and reviewing reports on past Korea Mineral Promotion Corporation (KMPC) work on the Chilbo prospect. To date the company has been unable to locate any reports showing the location of historic underground development or reports on past production from the Chilbo prospect. All the exploration work by KIGAM has been undertaken as high level reconnaissance surveys including airborne geophysics, regional scale stream sediment surveys and large scale regional geological mapping D10,D11. The Company has recently located 2 historic KMPC reports regarding drill programmes completed at Ubeong North and at Chilbo in 1982 and The bulk of the KMPC drilling at Chilbo focussed on two 500m and one 600m vertical holes into a granite body located in the southeast corner of the prospect area. All 3 holes failed to intersect any mineralisation and recent work by the Company indicate that the area targeted by KMPC is not geochemically anomalous. The IP survey over this area failed to identify any conductive units in the area drilled by KMPC. Two holes drilled to target the skarn mineralisation were drilled into a pelitic horizon between two horizons of skarn mineralised limestone. The third hole intersected minor skarn mineralisation adjacent to a granite body but much of the prospective core was not assayed. Two of these holes have targeted a soil geochemical low (pelitic sediments) and in an area between the Taipan Zinc (Zn) target and the Cobra copper (Cu) target further to the north D1. Similarly, at the Ubeong North prospect, three of the holes intersected broad widths of limestone but again much of the core was not assayed. Some low grade Pb and Zn intercepts were reported. The Company has presented and commented upon all past exploration work in the area that the Company is currently aware of. The Company is continuing its search for historical mine records and past Korea Resources Corporation (KORES) or historic Korea Mineral Promotion Corporation (KMPC) reports on the Ubeong Project.

13 Page 13 of 35 The Company has no records of the past production from any of the historic mines in the district. Geology Deposit type, geological setting and style of mineralisation. The geological target is skarn associated copper, lead, zinc, gold and silver mineralisation. Following the successful completion of the recent IP survey over the Chilbo Prospect, the Company has been able to broaden its range of targets at the Ubeong Project D12. The original geological target was skarn associated polymetallic zinc, silver +/- copper, lead and gold mineralisation. This style of mineralisation remains the key target for the Taipan (Zn, Pb Ag), Cobra (Cu, Zn, Au), Adder (Cu, Au) and Viper (Cu, Au, Ag) prospects located to the east of the recently identified Copperhead and Krait (Cu, Au) targets D12. The prospectivity of these geophysical targets is further enhanced by the presence of coincident soil anomalies recently identified over these eastern skarn targets. The Prospectivity of the eastern skarn targets is further enhanced by the assay results of rock chip samples collected over the respective target areas D2,D4. The Company s past rock chip sampling indicates that there is potential in the area for zinc, lead, copper, silver, gold, stibnite and tin mineralisation D2,D4. The Proterozoic limestone at the former mine site has undergone intense skarn metasomatic alteration, most likely associated with a blind intrusive body now interpreted to be the Copperhead Porphyry Body. Typical calc-silicate skarn alteration minerals such as hedenbergite, garnet and epidote are observed in rock chip samples. The intense magnetite and pyrrhotite mineralisation is typical of many other Korean skarn deposits and is interpreted to represent the first phase of mineralisation subsequently overprinted by later base metal Cu, Zn and Pb mineralising event. The intense magnetic high sympathetically tracking the mapped limestone unit is interpreted to reflect strong magnetite and pyrrhotite mineralisation associated with skarnification of the limestone D7.

14 Page 14 of 35 The Kumho mine to the west of the Ubeong Project (Figure 4) was also discovered during the Japanese occupation of Korea and initially mined as a manganese bearing skarn deposit. Subsequently, copper, lead, zinc, silver and gold mineralisation was discovered at depth in the 1940s. The Kumho mine has operated intermittently since 1930s with mining activities ceasing at times due to declining metal prices. The mine is currently active and is reportedly operating at around a 6% zinc head grade. Drill hole information A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: easting and northing of the drill hole collar elevation or RL (Reduce Level) elevation above sea level in metres) of the drill hole collar dip and azimuth of the hole down hole length and interception depth hole length If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case. A tabulation of location details for the drill holes completed to date is included as appendix 1. This tabulation also includes location details of the next hole planned in the current drill programme. The Company s drilling at Ubeong is ongoing with no assaying undertaken at this point in time. The XRF data commented upon in this release is spot data generated to aid in the identification of drill intercepts for assay. Data aggregation methods In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material and should be stated. No weightings or averaging has been applied to the data. All the data presented in this release is raw data. The images in this release relate to drill core from UBD0002.

15 Page 15 of 35 Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail. The data has not been aggregated. The assumptions used for any reporting of metal equivalent values should be clearly stated. No metal equivalent vales have been reported. Relationship between mineralisation widths and intercept lengths These relationships are particularly important in the reporting of Exploration Results. If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g. down hole length, true width not known ). The broad low grade skarn zone from 25.9m to 116m is characterised by disseminated blebs and occasional sulphide veinlets. This zone has not been assayed and no assays or XRF data from this interval has been commented upon in this release. The intersected low grade skarn zone dips at ~60 degrees to the southeast and is estimated to have a true width of 70m. The mineralised quartz vein from 334.5m has a downhole width of 5.5m but as the core from this portion of the hole was not orientated it is difficult to determine the true width of this zone. Indications from the angles of the surrounding foliation are that the vein cuts the core axis at a low angle and as such is likely to have a true width of less than 2m. The orientation data generated and logging completed to date suggests that the skarn unit dips steeply to the southeast in the early part of the hole but that the sequence flattens markedly to the north with parasitic folds developed on the upper limb of an eastward plunging recumbent synformal fold structure. The skarn mineralisation appears to be blebby strata bound sulphides. The sulphides within the pelitic sequence occur as blebs and veinlets developed sub-parallel to bedding and less commonly as veinlets at a high angle to bedding. The true orientation of the quartz vein intersected from 337.7m is not known. No assaying has been completed on the Ubeong core as yet. Limited spot XRF readings have been taken at regular intervals along the core to assist in selecting intervals from full laboratory assay.

16 Page 16 of 35 Diagrams Balanced reporting Other substantive exploration data Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results. Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. Figure 2 shows the location of hole UBD0002 and planned hole UBD0003 on the EM image. Also shown are the results of XRF soil analyses and relevant rock chip assay results D4,D6. Figure 3 is a cartoon schematic cross section drawn along hole UBD0002. Also shown is the proposed trace of UBD0003 to be drilled off section further to the east. Figure 4 shows the location of the granted Ubeong Project tenements and surrounding applications on the KIGAM Total Magnetic Image D11. The figure also shows the KIGAM regional mapping of the skarn limestone along with some of the more significant regional fault structures. The Chilbo Prospect is highlighted by mass of soil data points on the ground magnetics image D4, D5, D6. The photographic images are examples of the disseminated skarn mineralisation and the coarser crystalline arsenopyrite mineralisation from the quartz vein structure. The hole location details are included as Appendix 1. A table of XRF data from the quartz vein readings is included as Appendix 2. This release only includes XRF data from the quartz vein structure intersected from 337.7m To date the company has completed reconnaissance stream sediment survey in the area and follow-up rock chip sampling and limited surface mapping. A ground based magnetic survey was completed over the immediate Chlbo prospect area in late A trial EM project was undertaken in November 2016 the results of which suggested that IP may be more effective at the Ubeong project. A detailed IP survey was then completed on 100m spaced lines locally closed to 50m to undertake dipole-dipole IP over the Krait prospect. The culmination of this work has been the drilling of hole UBD0001 into the Krait IP target. The drilling of UBD0002 to test areas of low conductivity at the Taipan Prospect marked by elevated Zn in the soil geochemistry. This hole has also tested the Cobra Prospect. The final hole is designed to test the EM target beneath the valley floor and a zone of elevated Zn in soils and rock chips further to the south. These last 2 holes will test a full cross section of the skarnified limestone target. The company is still searching for any historic records of past work by KMPC now KORES and other non-government parties.

17 Page 17 of 35 Further work The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large-scale step-out drilling). The completion of the third hole at Ubeong UBD0003 is the immediate goal. Selected intervals from all 3 holes will be assayed and all the data from the drill programme assessed to assist in planning further drill holes into the intensely altered and structurally complex Chilbo Prospect. The soil geochemical data will be further reviewed and additional follow-up soil samples are being collected to more fully define additional target areas. The results of the follow-up stream sediment programme will be assessed to identify additional prospects within the 10km long highly prospective Ubeong skarn trend. Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. The targets identified to date were discussed more fully in earlier ASX releases D1, D10.

18 Page 18 of 35 JORC Code, 2012 Edition: Table 1 Section 1: Sampling Techniques and Data (Criteria in this section apply to all succeeding sections.) Sampling techniques Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. As a follow-up to 2016 regional stream sediment sampling a second phase of stream sediment sampling was undertaken over the Ubeong tenements (125 samples analysed by ALS Global services, Perth). This work identified elevated zinc, lead and copper associated with the historic Ilweol mining district. Followup field mapping has identified historic mine workings from the main Ilweol mine as well as smaller scale workings developed along shear structures and associated mafic dykes. During follow-up investigations of the historic Chilbo workings 7 rock chip samples were collected. The first sample ILW0001 was taken above a historic adit developed on a brecciated mineralised shear structure on block Dogyedong 72. Four rock chip channel samples were collected underground from accessible workings on block Dogyedong 82. A float sample from a conglomerate boulder with mineralised skarn related basemetal mineralisation was analysed (ILW0007) and one sample was taken from the oxidised dump material close to a large open stope at Ilweol that daylights at surface on block Dogyedong 72. The rock chip samples were analysed for a suite of elements by ALS Global Laboratory Services, Perth using ICP analyses and Fire Assay for gold. Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. Aspects of the determination of mineralisation that are material to the Public Report. In cases where industry standard work has been done this would be relatively simple (e.g. reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay ). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information. The rock chip sampling was standard sampling using a geology hammer, mallet. The stream sediment sampling followed standard industry practices. Samples were sieved at the sample site to generate a -0.18mm sample. Rock chip samples were collected in a calico bag and taken using a geology hammer and mallet. These were dispatched by courier to ALS Perth where the samples were jaw crushed and pulverised to produce a 1m sample for ICP analysis for a broad suite of elements and a 50gm charge was prepared for fire assay. The stream samples were collected in a water tight plastic ziplock bag and then dried post collection at the Company s sample preparation facility at its Sotae-myeon office. These samples were couriered to ALS Perth. On arrival 1gm subsamples were digested in a four-acid mix prior to ICP analysis for a broad suite of elements.

19 Page 19 of 35 Drilling techniques Drill sample recovery Logging Subsampling techniques and sample preparation Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of diamond tails, facesampling bit or other type, whether core is oriented and if so, by what method, etc). Method of recording and assessing core and chip sample recoveries and results assessed. Measures taken to maximise sample recovery and ensure representative nature of the samples. Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. The total length and percentage of the relevant intersections logged. If core, whether cut or sawn and whether quarter, half or all core taken. No drilling has been undertaken at Ilweol by the Company and no commentary is being presented here on past drilling results. The drilling at the Chilbo Prospect, Ubeong Project is all diamond drilling. A short HQ pre-collar was drilled to 11.5m with no core recovered from this weathered zone of soil and historic mine dump material. The hole was then drilled with Q3 (50mmm diameter) size core to 257.7m before the hole was cased off due to issues with extreme water loss in a zone of highly fractured pelitic and psammopelitic metasediments. The hole has then been drilled with BQ core to end of hole. No drilling has been undertaken at Ilweol by the Company and no commentary is being presented here on past drilling results. The Q3 drilling was all triple tube drilling with areas of core loss mainly the result of excessive core grinding in places and washing away of fine clays around faults. The core loss was 18.8m in total over the first 257m of the hole or 88% recovery. Recovery has improved since the step down to BQ sized core with minimal core grinding occurring and core losses reduced to <1m over the remainder of the hole. There does not appear to be any grade relationship to zones of core loss with the bulk of the loss being random and most likely attributable to poor drilling technique. No drilling has been undertaken at Ilweol by the Company and no commentary is being presented here on past drilling results. The Ubeong drill hole is still being drilled and core logging is ongoing. The hole has been logged to generate extensive structural data from core orientated using a Devicore core orientation device. In addition, all the intervals have been geotechnically logged to allow full Q system geotechnical appraisal to be performed at some future date. Each interval is geologically logged for lithology and mineral abundances and alteration type. The aim being to generate data suitable for the use in any future Mineral Resource Estimation. The full hole has been logged with selected intervals being marked up for diamond core cutting and subsequent sampling that is anticipated to commence early next month post the completion of the detailed geological logging of the current hole. No drilling has been undertaken at Ilweol by the Company and no commentary is being presented here on past drilling results. No core has been sampled at this stage though spot hand-held XRF measurements are being taken at 10cm intervals to assist with the selection of intervals for assay. It is intended that the core will be cut in half at the Company s sample preparation facility using the company s diamond saw. To this end all the