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The mining industry of
Madagascar Madagascar (; mg, Madagasikara, ), officially the Republic of Madagascar ( mg, Repoblikan'i Madagasikara, links=no, ; french: République de Madagascar), is an island country in the Indian Ocean, approximately off the coast of East Afric ...
is on a small scale, centred mainly around remote locations with large mineral deposits. Mining potential is noted in industrial and metallic minerals, energy, precious and semi-precious stones, as well as ornamental stone. The mining sector was neglected by the government for decades prior to the mid-2000s. In 2013, the mining industry, a main source of foreign investment, was struggling due to "low metals prices and distrustful companies", attributed to a 2009 coup.


History

Mining was a prevalent part of Madagascar’s cultural history dating back to the 15th century before it became a reality in the beginning of the 19th century. Speculations of valuable metal and mineral deposits in Madagascar came with the arrival of the Imerina people, also known as the Antimerina, Merina, or Hova people, in the 15th century when they established their small kingdom in central Madagascar.   These speculations of valuable metal and mineral deposits are rooted in a traditional Malagasy story titled ''Tantaran’ny Andriana'' (which translate as ''The History of the Nobles''). ''Tantaran’ny Andriana'' is a story told in the oral tradition that shares the history of the kings of Imerina. In addition to sharing the history of the Imerina kings, ''Tantaran’ny Andriana'' suggests that there are prevalent silver deposits across the island. As people around the world, especially Europeans, began to hear ''Tantaran’ny Andriana'' and therefore, the assosciated speculations of valuable mineral and metal deposits, explorers began to search for “Malagasy Eldorado,” which roughly translates to “Madagascar, the country of fabulous riches.” The main group of explorers searching for “Malagasy Eldorado” and the precious deposits were Europeans. The first known explorer to search for Madagascar’s deposits was Tristan da Cunha, a Portugese explorer, yet he was followed by many other European explorers. Upon arrival, explorers did not find the extent of valuable deposits that they were expecting – they found that the gold, silver, and other metals and minerals were typically imported to Madagascar and then turned into jewelry. Although European explorers did not find the deposits they were expecting, it is believed that the Malagasy people during this period did have knowledge of and worked alluvial deposits, which is “the mining of stream bed deposits,” for “''volamena''” (gold). These alluvial deposits were a secret guarded by the Sakalava and then Merina monarchs – with hopes to avoid international exploitation – until the 1820s when word got out about the deposits. Once the evidence of the deposits in Madagascar was known internationally, the Merina queen, who by this point was Queen Ranavolana I of Madagascar, sponsored explorations for silver and gold deposits across the island in the name of the crown. These initial push for exploration remained a pattern throughout her reign until major gold deposits were found in the 1840s and 1850s. Although this discovery was significant, Ranavalona I did not push to further develop them because she could feel the European colonial pressures encroaching on Madagascar. In 1883, under the reign of Queen Ranavalona III, the granddaughter of Ranavalona I, this changed, gold deposits were explored and exploited, which ultimately was one of the factors that led to the French colonization of Madagascar in 1896. Madagascar contains deposits of
copper Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pink ...
,
iron Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in ...
and
manganese Manganese is a chemical element with the Symbol (chemistry), symbol Mn and atomic number 25. It is a hard, brittle, silvery metal, often found in minerals in combination with iron. Manganese is a transition metal with a multifaceted array of ...
ores,
graphite Graphite () is a crystalline form of the element carbon. It consists of stacked layers of graphene. Graphite occurs naturally and is the most stable form of carbon under standard conditions. Synthetic and natural graphite are consumed on la ...
, rock salt,
niter Niter or nitre is the mineral form of potassium nitrate, KNO3. It is a soft, white, highly soluble mineral found primarily in arid climates or cave deposits. Historically, the term ''niter'' was not well differentiated from natron, both of w ...
, pyrites, and some minor minerals. By the early 20th century,
gold Gold is a chemical element with the symbol Au (from la, aurum) and atomic number 79. This makes it one of the higher atomic number elements that occur naturally. It is a bright, slightly orange-yellow, dense, soft, malleable, and ductile ...
was mined in alluvial deposits spread over the island. At the same time,
antimony Antimony is a chemical element with the symbol Sb (from la, stibium) and atomic number 51. A lustrous gray metalloid, it is found in nature mainly as the sulfide mineral stibnite (Sb2S3). Antimony compounds have been known since ancient ti ...
, copper, iron and tin were thought to be abundant, in addition to asphalt, coal, and petroleum. Deposits of alluvial gold were found in the valley of the Ampoasary River, a tributary of the
Mananjary River The Mananjary River is located in southern Madagascar, in the region of Vatovavy Vatovavy is a region of Madagascar. Its capital is Mananjary. It was created by dividing the former region of Vatovavy-Fitovinany on 16 June 2021. Cyclone Bat ...
, about east of
Ambositra Ambositra is a city (commune urbaine) in central Madagascar. Ambositra is the capital of the Amoron'i Mania region, and of Ambositra District. It is the centre of Madagascar's' wood-carving industry due to the presence of the Zafimaniry tr ...
. While the auriferous gravel was being washed in pans by approximately 3,000 local workers in the early 20th century, there were expectations that reef mining would supersede the primitive methods of gold extraction. In 1905, several syndicates were formed in the Transvaal to acquire properties in Madagascar, with some Rand mining experts visiting the island that year. In comparison to Madagascar’s mining industry throughout the 19th and 20th centuries, its mining industry today does not have as much of a significant impact on Madagascar’s livelihood. Despite this, it is necessary to note that according to data from 2014, the mining industry provides jobs for over 800,000 people, approximately half of which are filled by women.


Production and impact

Today, Madagascar’s mining industry is separated into two main types of mining: Artisinal and Small-Scale Mining (ASM) and large-scale public-private mining. Artisinal and small-scale operations are typically not associated with companies – it more of an individual operation and large-scale mining involves large, often international companies. ASM operations tend to focus on mining for precious metals and percious and semi-precious stones than large-scale public-private mining. For example, most artisinal and small-scale miners tend to mine for precious metals and stones like gold and sapphires, when large-scale public-private miners tend to mine for large amounts of minerals. For context, the gold output in 1904 was 2,641 kg (84,910 ozs.), valued at £316,995. In the following year, 1905, the quantity produced was 2,370 kg (76,197 ozs.), valued at £286,804. 113 years later, in 2018, according to data from the United States Geological Survey (USGS) the quantity of gold produced in Madagascar in 2018 reached the highest reported record of gold produced on Malagasy land – 3,000.00 kg (105, 821 ozs). The most recent data from the USGS states that the quantity of gold produced in 2020 was 2,100.00 kg (74,075.32 ozs). Production growth rate recorded in this sector was 121% during 2010, which has been sustained by rise in substantial production increase of agate, quartz, zircon, ilmenite, rutile, labradorite, limestone and marble, cement, graphite, gemstones, nickel and cobalt. According to the Plan d’action Madagascar 2007-2012, from both large and small scale mining operations, mining makes up 4% of Madagascar’s GDP. More recently, as of 2018, the mining industry accounts for 4.6% of the GDP, 4.4% of the government revenue, and 28% of exports annually. According to the Extractive Industries Transcparency Initiative (EITI), these statistics highlight the growth of the mining industry to Madagascar’s economy, but the total government revenue should be higher than it currently is. The EITI believes this because of the significant portion of illegal exports of gold. Looking into the future, the Plan d’action Madagascar 2007-2012 predicts that the mining proportion of the GDP will increase to 30% as Madagascar shifts from a mainly artisanal and small-scale based mining industry to a large-scale public-private industry.


Impact of Madagascar's mining industry

Although Madagascar’s economy depends on the mining industry, in terms of ASM, as well as in terms of large-scale public-private mining initiatives, these mining efforts heavily impact Madagascar’s natural environment and therefore, the Malagasy people and culture. These impacts can be recognized as environmental injustices.


The Environmental Injustices of Madagascar’s Mining Industry

In general, mining is a naturally destructive profession and the mining industry in Madagascar is not excluded from this generalization. The sheer definition of mining – “the industry and activities connected with getting valuable or useful minerals from the ground” – inherently results in the destruction of a physical environment to obtain these minerals from the earth. When conducting explorations or excavations of an area for the purposes of mining, entire ecosystems are destroyed which in turn results in a loss of overall biodiversity. In Madagascar, the two types of mining used affect the natural environment in different ways. In terms of ASM operations, there are fewer miners that work individually or in small groups in remote areas to find precious metals and stones. These mining initiatives take place away from permanent settlements like villages. The land that artisinal and small-scale miners often explore are areas known as “tany malalaky” meaning land that is “open and available” – highlighting the Malagasy belief that no one person or group “owns” the land. Because of this customary land selection process, there is no displacement of people involved – even other miners. Miners can not select pieces of land that could potentially harm the structure of another miner’s “pit” or “basin.” “Tany malalaky” is an unspoken Malagasy custom that reflects their belief that the land does not “belong” to one person –  “it ‘belongs’ to its guardian spirits.” When looking at large-scale public-private mining initiatives, “tany malalaky” doesn’t play a significant role in the land selection process. When selecting an area for a large-scale intiative, the factors taken into consideration are mainly economic – the amount of mineral or metal available for extraction and the potential profits. The social and cultural impacts of this large-scale mining initiative are not often taken into account. Many of these social and cultural factors are rooted in the loss of individual livelihood and communities by way of physical displacement of (typically rural) populations or restricted access to protected natural zones. Additionally, for those working on site, they often suffer from poor working conditions and mistreatment due to unjust policies, as well as concerns about the pollutants inherently associated with the industry and the potential health impacts of them. Over the past 40 years, these social and cultural injustices have gained nationwide attention due to two large-scale mining initiatives: the QIT Madagascar Minerals (QMM) SA Project in Anosy, Madagascar (previously known as Fort-Dauphin, Madagascar) >and the World Titanium Resources’ (WTR) Toliara Sands project located just outside of Toliara, Madagascar in the Ranobe protected area. The QMM SA project is an initiative that began with a 1986 agreement between QIT-Fer et Titane Inc. – a subsidiary of the Rio Tinto Corporation, one of the largest mineral and metal mining corporations globally, and Office des Mines Nationales et des Industries Stratégiques (the Office of National Mines and Stragtegic Industries of Madagascar) – a Malagasy public agency – saying that the profits of the QMM project will be split 80% to the Rio Tinto Corporation and 20% to the Malagasy government. This project consists of sand mining for zircon and open pit mining for ilmenite (the primary ore of titanium). The Toilara Sands project is a sand mining initiative for mineral that is projected to last for up to 100 years. As discussed earlier, both projects deeply impact their surrounding natural environment, yet they also impact the social and cultural environments of Madagascar. For example, both projects led to the displacement of people, yet the displacement had different effects depending on the implicated population. In terms of the QMM SA project, people were displaced from their homes without any say in the project – the only ones discussing the potential implications were the corporate and governmental parties involved. This lack of communication resulted in those who were displaced, who are typically the rural populations, having two options: to move to a dedicated piece of land or to be bought out by the government or corporation involved. The compensation provided was insufficient to purchase land that was suitable for agriculture, nor was the provided land suitable for agriculture. This becomes a problem when approximately 64% of Madagascar’s population depends on agriculture as their livelihood. Additionally, even when communities are not forcefully displaced, in certain scenarios it is necessary for them to leave. For example, this is what happened with the Toilara Sands project. Surrounding communities were forced to leave because of the restrictions placed on natural resources. In the case of the Toilara Sands project, water access was cut-off. This is not only a problem because water is a necessity of life, but was also necessary to maintain their agricultural livelihood. For those who are not displaced forcefully or out of necessity, and continue to live near or work at the mines, they often suffer from poor working conditions due to a lack of enforced policies, as well as face the health impacts due to the pollution caused by the mining projects. These injustices associated with the mining industry in Madagascar tend to be the most visible and therefore are often the most contested. For example, when World Titanium Resources was pushing for the Toilara Sands project there was immediately pushback against the project because of the proposed area for the mine (a protected, natural environment) and due to the destruction and pollution that this mining project would bring. Although there is pushback against the projects and the mining industry in general due to the injustices involved, it is necessary to recognize that both projects mentioned above are on-going. The Toilara Sands project has been under construction since 2013 and the QMM SA project has been active since 1981.


Legal framework

The Mining Law of 20 February 1902, was amended in November 1905; amongst other provisions the charge for a prospecting permit was reduced from £4 to £1. The present-day laws of the land related to the mining sector are: Act No. 2005-022 of 17 October 2005 which is an amendment to Law No. 2001-031 of 8 October 2002 prescribing specific rules for large investments; Act No. 2005-021 of 17 October 2005 which is an amendment to Law No. 99-022 of 19 August 1999; and Mining Code; and Decree No. 2006-910 of 19 August 2006 on execution of mining Code.


Commodities

Minerals, both industrial and metallic, are numerous including
ilmenite Ilmenite is a titanium-iron oxide mineral with the idealized formula . It is a weakly magnetic black or steel-gray solid. Ilmenite is the most important ore of titanium and the main source of titanium dioxide, which is used in paints, printing ...
,
graphite Graphite () is a crystalline form of the element carbon. It consists of stacked layers of graphene. Graphite occurs naturally and is the most stable form of carbon under standard conditions. Synthetic and natural graphite are consumed on la ...
,
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms w ...
,
gypsum Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula . It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, blackboard or sidewalk chalk, and drywa ...
,
dolomite Dolomite may refer to: *Dolomite (mineral), a carbonate mineral *Dolomite (rock), also known as dolostone, a sedimentary carbonate rock *Dolomite, Alabama, United States, an unincorporated community *Dolomite, California, United States, an unincor ...
,
silica Silicon dioxide, also known as silica, is an oxide of silicon with the chemical formula , most commonly found in nature as quartz and in various living organisms. In many parts of the world, silica is the major constituent of sand. Silica is ...
,
mica Micas ( ) are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is ...
,
titanium Titanium is a chemical element with the symbol Ti and atomic number 22. Found in nature only as an oxide, it can be reduced to produce a lustrous transition metal with a silver color, low density, and high strength, resistant to corrosion i ...
,
quartz Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical f ...
, gold, platinum group,
silver Silver is a chemical element with the symbol Ag (from the Latin ', derived from the Proto-Indo-European ''h₂erǵ'': "shiny" or "white") and atomic number 47. A soft, white, lustrous transition metal, it exhibits the highest electrical ...
,
iron Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in ...
,
copper Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pink ...
,
zinc Zinc is a chemical element with the symbol Zn and atomic number 30. Zinc is a slightly brittle metal at room temperature and has a shiny-greyish appearance when oxidation is removed. It is the first element in group 12 (IIB) of the periodi ...
,
nickel Nickel is a chemical element with symbol Ni and atomic number 28. It is a silvery-white lustrous metal with a slight golden tinge. Nickel is a hard and ductile transition metal. Pure nickel is chemically reactive but large pieces are slow t ...
,
cobalt Cobalt is a chemical element with the symbol Co and atomic number 27. As with nickel, cobalt is found in the Earth's crust only in a chemically combined form, save for small deposits found in alloys of natural meteoric iron. The free element, p ...
,
chromite Chromite is a crystalline mineral composed primarily of iron(II) oxide and chromium(III) oxide compounds. It can be represented by the chemical formula of FeCr2O4. It is an oxide mineral belonging to the spinel group. The element magnesium can ...
,
coal Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when ...
, and
uranium Uranium is a chemical element with the symbol U and atomic number 92. It is a silvery-grey metal in the actinide series of the periodic table. A uranium atom has 92 protons and 92 electrons, of which 6 are valence electrons. Uranium is weak ...
. Madagascar is also rich in precious and semi-precious stones:
ruby A ruby is a pinkish red to blood-red colored gemstone, a variety of the mineral corundum ( aluminium oxide). Ruby is one of the most popular traditional jewelry gems and is very durable. Other varieties of gem-quality corundum are called ...
,
sapphire Sapphire is a precious gemstone, a variety of the mineral corundum, consisting of aluminium oxide () with trace amounts of elements such as iron, titanium, chromium, vanadium, or magnesium. The name sapphire is derived via the Latin "sa ...
,
emerald Emerald is a gemstone and a variety of the mineral beryl (Be3Al2(SiO3)6) colored green by trace amounts of chromium or sometimes vanadium.Hurlbut, Cornelius S. Jr. and Kammerling, Robert C. (1991) ''Gemology'', John Wiley & Sons, New York, p ...
, aquamarine,
beryl Beryl ( ) is a mineral composed of beryllium aluminium silicate with the chemical formula Be3Al2Si6O18. Well-known varieties of beryl include emerald and aquamarine. Naturally occurring, hexagonal crystals of beryl can be up to several ...
,
tourmaline Tourmaline ( ) is a crystalline Silicate mineral, silicate mineral group in which boron is compounded with elements such as aluminium, iron, magnesium, sodium, lithium, or potassium. Tourmaline is a gemstone and can be found in a wide variety o ...
,
topaz Topaz is a silicate mineral of aluminium and fluorine with the chemical formula Al Si O( F, OH). It is used as a gemstone in jewelry and other adornments. Common topaz in its natural state is colorless, though trace element impurities can mak ...
,
garnet Garnets () are a group of silicate minerals that have been used since the Bronze Age as gemstones and abrasives. All species of garnets possess similar physical properties and crystal forms, but differ in chemical composition. The different ...
,
cordierite Cordierite (mineralogy) or iolite (gemology) is a magnesium iron aluminium cyclosilicate. Iron is almost always present and a solid solution exists between Mg-rich cordierite and Fe-rich sekaninaite with a series formula: to . A high-temperat ...
,
rose quartz Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical form ...
,
amethyst Amethyst is a violet variety of quartz. The name comes from the Koine Greek αμέθυστος ''amethystos'' from α- ''a-'', "not" and μεθύσκω (Ancient Greek) / μεθώ (Modern Greek), "intoxicate", a reference to the belief that ...
, and citrine. Decorative stones found are
marble Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite. Marble is typically not foliated (layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphose ...
, silicified wood, and
jasper Jasper, an aggregate of microgranular quartz and/or cryptocrystalline chalcedony and other mineral phases,Kostov, R. I. 2010. Review on the mineralogical systematics of jasper and related rocks. – Archaeometry Workshop, 7, 3, 209-213PDF/ref ...
.


References


Bibliography

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External links

{{Mining in Africa Mining in Madagascar Economy of Madagascar
Madagascar Madagascar (; mg, Madagasikara, ), officially the Republic of Madagascar ( mg, Repoblikan'i Madagasikara, links=no, ; french: République de Madagascar), is an island country in the Indian Ocean, approximately off the coast of East Afric ...