TIDMALBA

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Alba Mineral Resources PLC

30 November 2015

30 November 2015

Alba Mineral Resources plc

("Alba" or the "Company")

Amitsoq Project Update

High grade, large flake size confirmed in initial petrographic and geochemical results from Amitsoq Graphite Project in southern Greenland

Further to the company announcement on 6 October 2015, Alba Mineral Resources plc (AIM:ALBA) is pleased to report that a field visit has been completed at the Amitsoq graphite project (the "Project") near Nanortalik in southern Greenland in which Alba has an option to earn up to a 70 per cent. interest. Samples taken from historic workings at the Amitsoq mine have been subjected to graphitic carbon analysis and a petrographic determination of flake size by the British Geological Survey ("BGS") at their laboratory in Keyworth, near Nottingham.

HIGHLIGHTS

-- Graphitic carbon contents vary from 20.5% to 35.4%, with an overall mean graphitic carbon content of 28.7%, significantly higher than the previously reported historic average grade of 20% and higher than most reported advanced graphite projects globally.

-- The graphite exists in various morphologies, ranging from fine-grained specular forms to large discrete crystals, to agglomerations which span areas of up to 15 mm in size.

-- Measurements of the discrete graphite flakes suggests that the mean flake-size varies from 300-500 um ('Jumbo') to 180-300 um ('Large'), however the single most common flake size is in fact 'Super-Jumbo' (>500 um). The larger flake sizes attract a premium in the market.

Historic Exploration and Production

Greenland has a long history of graphite mining. The Amitsoq graphite mine was an open-cut operation between 1914 and 1924 and produced circa 5,500 tonnes at an average grade of 20 per cent graphite. The graphite was sent to Copenhagen for processing. Other than a local government funded mineral inventory and potential study in 1986, conducted by Danish company A/S Nielson, no other graphite exploration or development has taken place in the licence area since production ceased. Metallurgical testwork on behalf of A/S Nielson reported some flakes reaching a maximum of 15 mm ("Super-Jumbo" flake size), with the average flake size being 0.2-0.3 mm (200-300 um,

or "Jumbo" flake size).   Adits into the hillside are also present. 

Present Results

A field visit was undertaken to the historic Amitsoq mine site. The objectives were: to determine the access to the historic mine site via marine and aerial means; to ascertain the suitability of siting drill rigs in the area; to safely access any open workings; and to collect representative samples of one of the worked graphite horizons to determine carbon content and flake size.

The Company is pleased to report that access to the site was straightforward and was achieved by chartering a helicopter from the Narsaq heliport, located 85 km to the northwest. Several landing sites were identified, but access by sea from the port of Nanortalik, 16 km to the southwest, will be the preferred method of access in future. During the helicopter flypast, a 500 m long flat-lying area above the dipping graphite horizons was observed that is considered ideal for the location of drilling pads if resource definition drilling takes place at the site in future.

Access to the underground workings was by structurally-robust unsupported adits that had been driven "horizontally" into the hillside along the graphite lens. The lens varied between 1 to 2 m in thickness, striking northeast, and dipping to the northwest at 35deg. Historical records of the workings state the lens attained a maximum width of 15.2 m, but this was not confirmed during the field visit. A total of ten (10) grab samples (G15101-G15110) were collected during the underground examination: 4 samples across the vein near the entrance; 3 samples across the vein 20 m down the adit; and 3 samples further down the adit to the deepest accessible part of the mine (approximately 40 m from entrance). One grab sample (G15111) from the surface dump was also collected to determine the effects of over 100 years of surficial weathering on the graphite.

Graphitic Carbon Assay

All eleven samples were independently analysed by the BGS at their laboratory in Keyworth, near Nottingham. A 50 g subsample was crushed to <500 <MU>m, and a 1 g aliquot was used to determine carbon content by using a deferential weight loss method (heating the sample to 105degC to drive off water, and a subsequent heating to 1000degC to oxidise the graphite).

The samples present a range of graphitic carbon contents from 20.5% (G15105) to 35.4% (G15101) with an overall mean graphitic carbon content of 28.7% for the eleven samples. Additional metallurgical test work will need to be performed to determine the total recoverable graphitic carbon. These results should be considered to be accurate to +/- 2% as a result of possible loss from ignition of other volatile compounds, such as sulphur and water.

The average grade of 28.7% from these samples at Amitsoq compares favourably with the average grades of

advanced graphite projects globally. Of 36 projects analysed, only two have grades of 20% or more(1) .

While these results at Amitsoq are taken from grab samples, the grade, coupled with the confirmation of the prevalence of Jumbo and Super-Jumbo flake size, provides great encouragement for future work.

Graphitic Flake-Size Analysis

The flake size and petrography of four thin section samples was performed at the BGS utilising polarizing microscope equipment. Petrographic analysis indicated the samples were all recrystallized graphitic gneiss/mica-schist. The graphite exists in various morphologies ranging from fine-grained specular forms to dust and are intergrown with silicate minerals to coarser-grained, discrete, elongate laths that often lie parallel to the rock's fabric to dense mesh- or web-like agglomerations which span areas of up to 15 mm in size.

 
  Sample     Flake               Graphite flake-size (%)               Mean 
  number     counts                                                     size 
                                                                        (um) 
---------  --------                                                  -------- 
                       >500    300-500   180-300   150-180   75-150 
                        um        um        um        um       um 
---------  --------  -------  --------  --------  --------  -------  -------- 
                      Super     Jumbo     Large    Medium    Small 
                       Jumbo 
---------  --------  -------  --------  --------  --------  -------  -------- 
  G15101      940       39       21        17         7        15     300-500 
---------  --------  -------  --------  --------  --------  -------  -------- 
  G15104      504       26       23        25        11        15     300-500 
---------  --------  -------  --------  --------  --------  -------  -------- 
  G15106      432       31       20        18        15        17     300-500 
---------  --------  -------  --------  --------  --------  -------  -------- 
  G15110      68        16       17        28        17        22     180-300 
---------  --------  -------  --------  --------  --------  -------  -------- 
 

N.B. These grain sizes only correspond to discrete graphite flakes, and do not consider specular/aggregated forms.

The mean flake-size of the discrete graphite varies from 300-500 <MU>m ('Jumbo') (G15101, G15104 and G15106) to 180-300 <MU>m ('Large') (G15110). This is in reasonable agreement with a historic study by A/S Nelson, which reported a slightly smaller average flake size of 0.2-0.3 mm (200 - 300 <MU>m). However the most common flake size in three of the four samples tested is in fact 'Super-Jumbo' (>500 um), comprising 16 to 39 per cent of the total graphite flake size across the four thin sections sampled. The market places a premium on larger graphite flake sizes.

Proposed Future Work

Several of the samples will now be dispatched to an independent assay laboratory to determine the presence of deleterious elements and to quantify the presence of sulphides.

A remote sensing study on the Project is expected to begin shortly, funded by Alba, with the main aim of identifying surficial occurrences of graphite on the 146 km(2) land mass of the licence area. A second aim of this study is to identify ultramafic intrusions which were investigated on Amitsoq in the early 1970s and found to contain up to 2.4 g/t combined gold, platinum, and palladium.

Quotations are currently being reviewed for a high-resolution modern airborne electromagnetic (EM) and magnetic surveys to identify graphitic horizons and sulphide bodies associated with ultramafic intrusions. It is anticipated that this work will commence in the summer of 2016. Follow-up work, if warranted, will consist of diamond drilling to provide a resource estimation.

Additional maps and photographs of the Project area are available on the Alba website at www.albamineralresources.com.

Mike Nott, Alba's CEO, commented:

"The results from this preliminary study are highly encouraging. We have demonstrated that Amitsoq contains large flake size graphite and appears to be of a high grade. Both of these factors provide great encouragement for future work and development at Amitsoq.

"The priority for Alba is to now determine the graphite prospectivity on other parts of the licence by using modern remote sensing and airborne geophysical techniques. The results of these surveys can then be used to prove continuity and to plan an exploration drilling programme to estimate the thickness and to confirm continuity of the graphite horizons known to exist in the Project area.

"The additional prospect of receiving Platinum Group Element (PGE) credits within the Licence will be an exciting area for Alba to investigate."

Competent Person's Declaration

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