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Liberia

New Liberty Mine

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Overview

Mine TypeUnderground
StatusActive
Commodities
  • Gold
Mining Method
  • Longitudinal stoping
  • Transverse stoping
  • Transverse open stoping
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SnapshotNew Liberty is the key asset in Avesoro Resources’ portfolio and stands as Liberia’s first and largest commercial gold mine. The New Liberty operation consists of two worked-out open pits, an underground mine with three separate portals, and a large processing plant supported by tailings dams.

The open pit operations, which lasted from October 2014 was completed in June 2022.The underground mining operation, which began in August 2020, features three distinct declines: Larjor, Kinjor, and Marvoe.

Avesoro Holdings Ltd., a private equity firm, acquired the mine in December 2018. Mine operations data has not been publicly available since then.

Owners

SourceSource
CompanyInterestOwnership
Government of Liberia 10 % Indirect
MNG Group 90 % Indirect
Avesoro Resources Inc. holds its interests in the New Liberty Gold Mine through its subsidiary Bea Mountain Mining Corporation (“Bea”). On July 29, 2009 Bea was granted a Class A Mining Licence (“Bea Mining Licence”) within the Bea Mountain Mineral Development Agreement property (the “Bea MDA Property”) by the Government of Liberia (“GoL”). The Bea Mining Licence permits mining within the 478 km2 area which encompasses the New Liberty Gold Mine. The GoL holds a 10% free carry interest in the Bea Mining Licence.

Avesoro Resources was delisted at TSX in January 2020.

Contractors

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Deposit type

  • Orogenic
  • Vein / narrow vein

Summary:

The New Liberty Property hosts a typical Upper Archean to lower Proterozoic style of metallogeny, characteristic of greenstone-hosted lode gold mineralisation, where deposits are often referred to as orogenic, and characterised by the presence of gold-quartz veins and disseminated mineralisation. Gold mineralisation is hosted in moderate to steeply dipping quartz-dominated shear zones with associated extensional vein systems. This model is consistent with Archean orogenic gold deposits described by Hagemann and Cassidy (2000), Richards and Tosdal (2001), Goldfarb et al. (2001) and Roberts et al. (1989).

The New Liberty deposit is hosted in sheared and altered ultramafic rocks. The gold mineralisation is associated with disseminated sulphides. The disseminated sulphide host bodies are more conOnuous than a typical quartz hosted vein. The orebody is in a highly sheared and myloniOsed schist belt which trends east-southeast.

The average dip of the orebody is approximately 60°, with local variations in dip ranging from near vertical to around 40°. The orebody consists of a number of veins, generally parallel to each other. Mineralisation can occur in more than one of the veins, creating the potential for multiple parallel stopes in some parts of the deposit.

The widths of the mineralised zones range from 2 m to 30 m, with an average width of 10 m.

Within the ultramafic unit, silicification is found proximal to the mineralisation, within the immediate hangingwall and rarely in the footwall gneisses. Other alteration styles associated with the mineralisation include the presence of phlogopite as well as chlorite within the mineralised zone, and an associated sulphidic bleaching of the rocks linked with the destruction of magnetite.

These features point to a pathway for the mineralising fluids which was active over a long period of time. The deposit shows the classic signs of sulphidation, with iron sulphides (mainly pyrrhotite) replacing the magnetite and it has a low sulphide content with sulphides forming between 0.1% and 1% of the mineralised zones.

Multi element analyses of cores have highlighted a clear association between gold and arsenic, sulphur, nickel and tungsten in the mineralised zones. Enhanced values of magnesium, sodium, potassium, rubidium and barium occur along the margins of the mineralisation. It is hypothesised that the gold-bearing metamorphic fluid may include a granitic component in its evolution.

Vast majority of the mineralisation at the Project is hosted within the altered parts of the sheared ultramafic rocks. Pyrrhotite, gersdorffite and arsenopyrite are the main sulphides with occasional pyrite and rare chalcopyrite or pentlandite. Metallurgical tests of the mineralised sections carried out by Lakefield Research Limited (Lakefield, 1999b) indicated that the gold is free in form. Gold mineralisation occurs in zones of variable thickness, with average widths of 10 m, and is nearly continuous along 2 km of strike.

Reserves

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Mining Methods

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Comminution

Crushers and Mills

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Processing

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Production

CommodityUnits2023201820172016
Gold koz  ....  Subscribe1107664
All production numbers are expressed as metal in doré.

Operational metrics

Metrics2023201820172016
Plant annual capacity  ....  Subscribe1.1 Mt
Tonnes processed  ....  Subscribe1,411 kt1,144 kt842 kt
Stripping / waste ratio  ....  Subscribe16.1 11.1 9
Ore tonnes mined  ....  Subscribe1,352 kt1,166 kt996 kt
Waste OP  ....  Subscribe21,797 kt12,935 kt8,965 kt
Total tonnes mined  ....  Subscribe23,149 kt14,102 kt9,961 kt

Production Costs

CommodityUnits20182017
Cash costs (sold) Gold USD 862 / oz   918 / oz  
All-in sustaining costs (sold) Gold USD 1,120 / oz   1,427 / oz  

Operating Costs

Currency2017
OP mining costs ($/t mined) USD  ....  Subscribe

Financials

Units20182017
Revenue M USD 140.3   95.2  
After-tax Income M USD -40.3   -20.8  

Required Heavy Mobile Equipment

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AV - Autonomous

Personnel

Mine Management

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....................... Subscription required ....................... Subscription required Subscription required Sep 21, 2024
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Aerial view:

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