Block D, Merelani: The Artisanal Quarter of the Tanzanite Fields
Block D, Merelani: The Artisanal Quarter of the Tanzanite Fields
The southernmost concession of the Merelani Hills, worked predominantly by small-scale miners
Block D is the southernmost of the four administrative mining concessions that together constitute the Merelani tanzanite deposit in the Lelatema Mountains of northern Tanzania, situated roughly 70 kilometres south-east of Arusha near the town of Simanjiro. Like the other three blocks — A, B, and C — it occupies a portion of the narrow, steeply dipping graphitic gneiss horizon within which gem-quality zoisite, the mineral species that gives tanzanite its identity, formed during the Mozambique Belt metamorphic event approximately 585 million years ago. Block D is distinguished not by any geological or gemmological peculiarity but by its administrative and socio-economic character: it is the concession allocated to small-scale and artisanal miners, making it the most populous and, in human terms, the most complex sector of the entire deposit.
The Four-Block System
The concession framework at Merelani was established by the Tanzanian government to organise mining rights, royalty collection, and taxation across a deposit that had, since its commercial discovery in 1967, attracted a chaotic mixture of large corporate interests and informal diggers. The four blocks — designated A, B, C, and D — were demarcated as administrative units and do not correspond to any recognised geological subdivision of the orebody. Block A was historically associated with larger-scale operations; Block C became the concession of TanzaniteOne (later Richland Resources, subsequently rebranded), which at its peak operated one of the most mechanised tanzanite mining programmes on the continent. Block D, by contrast, was set aside for small-scale miners operating under licences issued by the Tanzanian government's Ministry of Minerals.
The boundaries between blocks are administrative lines on a survey map rather than lithological boundaries. The gem-bearing graphitic gneiss that hosts tanzanite runs continuously beneath all four concessions, and the mineralising conditions — the precise combination of vanadium-rich fluids, tectonic fracturing, and high-grade metamorphism — were uniform across the deposit. A tanzanite crystal extracted from Block D is, in every measurable physical and optical property, identical to one extracted from Block C or Block A.
Geology and Mineralisation
Tanzanite — the blue-to-violet gem variety of the calcium aluminium silicate mineral zoisite — occurs at Merelani within a series of steeply inclined graphitic gneiss lenses intercalated with calc-silicate rocks and marbles. The gem-bearing zones, locally termed mirerani pockets or simply "pockets," are irregular and unpredictable in their distribution. Mineralisation is controlled by structural features: shear zones, fold hinges, and boudinage necks where fluid infiltration was concentrated during the Pan-African metamorphic episode.
The deposit is notably shallow in its upper reaches but extends to considerable depth — underground workings in the mechanised blocks have followed the orebody to depths exceeding 800 metres. In Block D, artisanal operations have historically been confined to shallower levels, though hand-dug shafts and adits have in some areas reached significant depths, often under precarious conditions. The rough produced spans the full quality spectrum: from deeply saturated, clean crystals of the finest commercial grade to heavily included, pale, or poorly formed material suitable only for lower-grade cutting or carving.
Small-Scale Mining in Block D
The artisanal character of Block D has made it the most visible face of tanzanite mining for journalists, researchers, and development organisations. Thousands of individual licence-holders and their workers have operated within its boundaries, digging by hand or with minimal mechanisation, often in conditions that carry significant occupational hazard. Cave-ins, flooding during the rainy season, and inadequate ventilation have been documented hazards across the artisanal sector.
The economic structure of Block D differs substantially from the corporate model of Block C. Individual miners sell rough to a network of dealers and brokers concentrated in the nearby trading centre of Arusha, which functions as the primary rough tanzanite market. Pricing is negotiated stone by stone or parcel by parcel, and the supply chain from pit to polished gem is correspondingly fragmented. This structure has made Block D rough more difficult to trace through formal chain-of-custody programmes, a consideration that has grown in importance as the jewellery industry has placed greater emphasis on responsible sourcing documentation.
Tanzanian government policy has periodically sought to formalise and consolidate the artisanal sector, including through the establishment of the Tanzanite Foundation and, later, through revised mining legislation. The 2017 amendments to Tanzania's Mining Act, which imposed restrictions on the export of unprocessed rough and required a greater proportion of value addition to occur within Tanzania, affected Block D operators alongside all other concession holders, though implementation and enforcement have varied.
Gemmological Identity of Block D Tanzanite
From a gemmological standpoint, tanzanite from Block D carries no distinguishing characteristics. The mineral's defining properties — orthorhombic crystal system, refractive indices of approximately 1.691 to 1.700, biaxial positive optic sign, strong trichroism displaying blue, violet, and burgundy-red axes, and the characteristic vanadium-driven colour centre responsible for its blue-violet hue — are uniform across the entire Merelani deposit regardless of concession of origin. No reputable gemmological laboratory, including the GIA or Gübelin Gem Lab, has identified spectroscopic, chemical, or inclusion-scene markers that would allow reliable attribution of a tanzanite to a specific block within Merelani.
The colour of tanzanite as it emerges from the ground is typically a brownish or reddish-brown hue caused by natural pleochroism and the presence of iron. The vivid blue-violet colour for which tanzanite is prized is almost universally achieved through heat treatment — gentle heating to approximately 500–600 degrees Celsius drives off the brown component and stabilises the blue-violet axis. This treatment is applied to rough or cut stones from all four blocks without distinction and is universally accepted within the trade as a standard finishing process. It is permanent and requires no disclosure beyond the general understanding that virtually all commercial tanzanite has been heated.
Market and Trade Significance
Block D's significance in the market is primarily one of volume and accessibility rather than quality differentiation. Because artisanal operations produce a wide and unpredictable range of material, Block D has historically contributed substantially to the lower and mid-range segments of the tanzanite market — smaller stones, more included goods, and calibrated commercial-grade material — while also occasionally yielding exceptional large crystals when a significant pocket is encountered. The unpredictability of artisanal mining means that notable finds are not uncommon, even if they are irregular.
For buyers and dealers sourcing tanzanite, the block designation carries administrative and ethical connotations more than gemmological ones. Material described as "Block D tanzanite" signals artisanal origin and, for buyers engaged in responsible sourcing, prompts questions about traceability and fair-trade certification. Organisations such as the Tanzanite Foundation have worked to extend certification schemes into the artisanal sector, though coverage remains incomplete.
The broader Merelani deposit is the world's only known commercial source of tanzanite, a geological rarity that underpins the gem's enduring market value. Within that singular locality, Block D represents the human dimension of the deposit — the thousands of individual livelihoods dependent on a narrow seam of metamorphic rock in the East African Rift zone.