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Rough diamond

A rough diamond is the natural, uncut form of , a composed almost entirely of carbon atoms arranged in a rigid , making it the hardest naturally occurring substance known. These crystals form deep within , at depths of approximately 100 to 250 miles (160 to 400 kilometers), where extreme temperatures exceeding 2,000°F (1,100°C) and pressures around 45,000 times atmospheric levels transform carbon into . Billions of years old, rough diamonds are transported to the surface by rare, explosive volcanic eruptions that create pipes—vertical conduits of that carry the crystals upward, often embedding them in ancient . Rough diamonds exhibit diverse morphologies, with the most common shape being the , resembling two pyramids joined at their bases, though they can also appear as cubes, dodecahedrons, or irregular fragments due to resorption or growth variations during formation. Their external surfaces often feature a dull, greasy luster covered by a thin film called the "nyf," but internally, they display exceptional brilliance, (fire), and transparency once the outer layer is removed, properties stemming from their high of 2.42 and adamantine luster. Inclusions, such as minerals from the mantle (e.g., or ), and trace impurities like or , influence color—ranging from colorless to yellow, brown, or rare vivid hues like and —affecting both gem and industrial value. Sourced primarily from alluvial deposits or primary kimberlite sources across Russia, Africa (notably Botswana and South Africa), Canada, and Australia, rough diamonds are mined through open-pit, underground, or artisanal methods, with global production valued at $11.48 billion in 2024, though volumes fluctuate due to economic, regulatory, and competition from laboratory-grown diamonds factors. Approximately 80% serve industrial applications, leveraging diamond's unparalleled hardness for cutting tools, drilling, and abrasives, while the remainder are cut and polished into gemstones for jewelry, symbolizing durability and rarity. The growing market for laboratory-grown diamonds, which reached 18% of the global jewelry market by value in 2023, has increased pressure on natural rough diamond demand. To combat conflict funding, the , established in 2003, mandates traceability for rough diamonds, ensuring they are conflict-free before export.

Definition and Characteristics

Definition

A rough diamond is a natural diamond crystal extracted from the Earth in its uncut and unpolished state, consisting essentially of pure carbon crystallized in the cubic system with tetrahedral coordination of atoms. In , the term "rough" denotes the unprocessed condition of the diamond prior to any human intervention, such as cleaving, sawing, or , preserving its original external form and internal features as formed in . Rough diamonds are fundamentally distinguished from synthetic or treated diamonds by their exclusively natural origin, having formed deep within the over billions of years under extreme pressure and temperature, in contrast to laboratory-grown diamonds produced via high-pressure high-temperature or processes. This geological authenticity excludes lab-created, enhanced, or imitation materials from the definition of rough diamonds.

Physical Appearance

Rough diamonds typically exhibit a translucent to opaque appearance, often displaying a greasy or vitreous luster that contrasts with the brilliant sheen of their cut counterparts. This subdued luster arises from the natural, unpolished surfaces, which can make rough diamonds resemble ordinary rocks such as due to their irregular, crystalline forms and lack of facets. Their high contributes to a resilient, durable exterior that withstands geological transport without significant alteration. The surface of a features a distinctly uneven , marked by natural etchings, trigons—triangular pits or depressions formed during in mantle fluids. These features, resulting from growth and resorption processes, impart a rough, pitted quality that obscures the stone's internal potential until processing. In their natural state, rough diamonds display color variations ranging from colorless and transparent to tinted shades of , , or black, and rarely vivid hues such as , , or , primarily influenced by inclusions and trace impurities captured during formation. These hues remain unenhanced by cutting, often appearing muted or speckled due to internal irregularities.

Crystal Habits

Rough diamonds exhibit a variety of crystal habits, with the octahedron being the most prevalent form observed in natural specimens. This eight-faced polyhedron, characterized by equilateral triangular faces meeting at sharp points, arises due to the diamond's cubic crystal system and is the dominant growth habit under typical mantle conditions. Other common habits include the cube, featuring six square faces, and the dodecahedron, a twelve-sided form with rhombic faces, both of which can appear alongside or modified from the octahedral shape through processes like resorption. Additionally, macles represent twinned crystals, often flattened into triangular plates due to a 180-degree rotation along the twin plane, resulting in a spinel-law twinning that distinguishes them from single crystals. At the atomic level, the internal structure of rough diamonds consists of a face-centered cubic arrangement of carbon atoms, where each atom is tetrahedrally coordinated to four others through strong covalent bonds. This configuration stems from the sp³ hybridization of the carbon atoms, forming a three-dimensional network of sigma bonds that extends throughout the crystal. The resulting , with a basis of two carbon atoms per , underpins the material's exceptional properties, including its unparalleled , which derives from the directional strength and density of these sp³ bonds. Inclusions and flaws within rough diamonds significantly influence their internal structure and light transmission. Common internal features include feathers, which are small fractures or cleavages often intersecting the crystal planes; needles, elongated inclusions such as silicates or oxides that align along growth directions; and carbon spots, typically aggregates appearing as dark, irregular patches. These imperfections, trapped during , can scatter or block light paths in the rough state, altering the crystal's optical homogeneity without necessarily compromising the overall integrity.

Formation and Occurrence

Geological Formation

Rough diamonds form deep within the under extreme conditions that stabilize the structure of carbon. These conditions typically occur at depths of 140 to 200 kilometers, where pressures range from 45 to 60 kilobars (4.5 to 6 GPa) and temperatures between 900 and 1,300°C allow carbon to crystallize directly from fluids or melts derived from mantle materials. The process involves metasomatic reactions in or eclogite, where carbon atoms arrange into a tetrahedral , forming the hardest known natural material. Diamond formation has occurred over much of Earth's history, with the oldest examples dating back 3.5 to 3.3 billion years to the , when primordial carbon in began crystallizing under these conditions. Subsequent episodes, particularly from 3 billion years ago onward, involved carbon recycled through zones, where carrying organic and inorganic carbon was subducted into , contributing to fluid-rich environments that promoted diamond growth. These events align with major tectonic cycles, such as the stabilization of cratons and the onset of , which facilitated the delivery of carbon to diamond-stable depths. Once formed, rough diamonds remain stable in the mantle until transported to the surface by rare volcanic activity. Kimberlite magmas, originating from depths exceeding 150 kilometers, entrain diamonds and mantle xenoliths during rapid ascent at speeds of 4 to 20 meters per second, preventing significant resorption. These volatile-rich melts solidify en route as they cool, forming kimberlite pipes that serve as the primary conduits for diamonds to reach the crust, with most such eruptions occurring less than 550 million years ago.

Natural Deposits

Rough diamonds are primarily sourced from primary deposits known as and pipes, which are carrot-shaped volcanic conduits formed deep in the and erupted explosively to the surface, transporting from depths of 150-200 kilometers. These pipes are the dominant host rocks for economically viable diamond concentrations, with being the most common type, named after the region in where they were first identified in the 1870s. Notable examples include the kimberlite pipes around , , which have yielded some of the world's earliest commercial discoveries. In , the Yakutian kimberlite province in hosts major deposits such as the and Aikhal pipes, contributing significantly to global supply. pipes, a rarer host rock, are exemplified by the deposit in Western Australia's region, which was a key source of fancy-colored until its closure in 2020. Secondary deposits form when primary sources erode, redistributing into alluvial and placer environments such as riverbeds, terraces, and coastal sediments through fluvial and processes. In , extensive alluvial deposits along northeastern rivers like the Cuango have been a major source, with concentrated in gravel beds from ancient erosion. Brazil's secondary deposits are similarly alluvial, primarily in river systems across and states, where recovers from placer gravels derived from distant primary sources. Globally, Africa accounts for a significant share of rough diamond production, approximately 55% by value as of 2024, from its kimberlite-rich regions, with key contributions from southern and central parts of the continent. Botswana's Jwaneng mine, operating in a large kimberlite pipe, is the world's richest by value and exemplifies high-grade African deposits, producing over 10 million carats annually in recent years. Other significant African locations include South Africa's Premier and Venetia pipes, while non-African deposits like those in Russia and Canada provide additional volume, often from colder cratonic regions conducive to kimberlite formation.

Mining and Recovery

Mining Methods

Diamond mining methods are selected based on the depth and type of diamond-bearing deposits, primarily or for primary sources and alluvial gravels for secondary ones. The three principal techniques—open-pit, , and alluvial mining—enable the extraction of containing rough diamonds, with each method optimized for specific geological conditions to maximize while managing operational costs. Open-pit mining is employed for shallow primary deposits, involving large-scale surface excavation to access or similar pipes near the surface. This method uses heavy machinery to remove and blast the body, creating expansive pits that can reach depths of several hundred meters. A prominent example was the Argyle mine in , which began with alluvial operations in 1983 and open-pit mining in 1985 from a pipe, transitioning to underground in 2013 before closing in 2020; it was the world's largest producer by volume during its peak. The technique is efficient for high-volume extraction but is limited to deposits where the pipe's upper portions are economically viable at surface levels. For deeper primary deposits exceeding 300-500 meters, underground mining is utilized, employing methods such as block caving or shrinkage stoping to access ore bodies below the surface. Block caving induces controlled collapse of the ore mass from undercut levels, allowing gravity to facilitate extraction, while shrinkage stoping involves backfilling mined areas with waste to support the ceiling. The Venetia mine in exemplifies this approach; originally an open-pit operation, it ceased in 2022 and transitioned to underground mining, delivering first in 2023 using sublevel caving to target its K01 and K02 pipes at depths up to 1,000 meters. As of 2025, underground operations continue, with ramp-up to full delayed to 2032 and mine life extended to 2049. These methods enable sustained from vertical pipes but require advanced ventilation, support systems, and safety measures due to the challenging subsurface environment. Alluvial mining targets secondary deposits where diamonds have been eroded and transported to river systems or floodplains, using techniques like and panning to recover gems from and . involves mechanical or suction equipment to excavate and process riverbed materials, often on a semi-industrial scale, while panning is a manual artisanal method where miners sift through gravels in to separate heavy diamonds. In , alluvial operations along rivers such as the Jequitinhonha have historically relied on these low-tech approaches, with independent miners recovering loose crystals from sediments dating back to the . Similar practices occur in African countries like and , where secondary deposits contribute significantly to small-scale production. This method is cost-effective for dispersed, low-grade deposits but yields variable results dependent on seasonal flows and distribution.

Extraction Processes

Once the ore, typically from diamond mines, has been extracted, it undergoes a series of steps to liberate and recover the embedded rough diamonds. These extraction processes aim to separate the valuable diamonds from the surrounding minerals while preserving the integrity of the crystals. The initial stage involves crushing and screening to break down the ore into manageable sizes and concentrate the heavy minerals containing diamonds. Ore is first crushed using gyratory or jaw crushers to reduce it to particles below 250 mm, followed by secondary and tertiary crushing to sizes around 75 mm or smaller, ensuring diamonds are liberated without excessive fragmentation that could damage them. Screening then employs vibrating sieves to classify the material by size, separating finer sands and gravels while directing oversize pieces for further crushing; this step often includes scrubbing in rotary drums with water to remove clay and mud adhering to the particles. Subsequent separation techniques exploit the physical properties of diamonds, such as their high density (3.52 g/cm³), hydrophobicity, and fluorescence under X-rays, to isolate them from lighter gangue. Dense media separation (DMS) is a primary method, where crushed ore is mixed with a slurry of water and ferrosilicon powder to create a medium with a specific gravity between 2.8 and 3.5; in hydrocyclones or baths, denser diamond-bearing material sinks and is collected as the "sink" fraction, while lighter waste floats as "floats" for disposal. X-ray fluorescence (XRF) or luminescence sorting detects diamonds by their unique response to X-ray excitation—diamonds fluoresce brightly due to nitrogen impurities—allowing automated sorters to eject them from conveyor belts via air jets, achieving recovery rates over 90% for sizes above 1 mm. For finer material, grease tables provide hydrophobic recovery: a vibrating table coated with viscous grease captures small diamonds as ore slurry flows over it with water, since diamonds adhere to the grease while hydrophilic gangue washes away; the grease is then scraped off, heated to release diamonds, and recycled. Recovery yields from these processes typically range from 0.1 to 1 of rough per metric ton of ore, depending on the deposit's grade, with higher-value mines like those in pipes averaging around 1 per . To minimize damage, which can reduce value by fracturing gems, operations emphasize controlled crushing with monitoring for indicators and gentle handling in separations, often recovering over 98% of larger than 1 mm while directing fines to specialized recovery units.

Identification and Sorting

Identifying Rough Diamonds

Identifying rough diamonds requires a combination of physical tests, visual examinations, and advanced analytical techniques to verify authenticity and distinguish them from common simulants such as and . These methods are essential in both field and laboratory settings, where rough diamonds often appear as irregular, translucent crystals that can resemble other minerals. Initial assessments focus on inherent properties unique to , a form of pure carbon with exceptional physical characteristics. Physical tests provide straightforward ways to confirm diamond's distinctive traits. The hardness test involves attempting to scratch a known corundum (Mohs hardness 9) with the suspected stone; genuine diamonds, rated at Mohs 10, will scratch corundum, while most simulants like zircon (Mohs 7.5) will not. Specific gravity measurement, typically 3.52 g/cm³ for diamond, can be assessed using a balance and water displacement, though accuracy is limited for small samples and requires calibration. Thermal conductivity is evaluated with a diamond tester, which detects the rapid heat dissipation unique to diamond. However, basic thermal conductivity testers may not reliably differentiate diamond from moissanite due to the latter's high thermal conductivity; testers that also measure electrical conductivity are needed, as moissanite conducts electricity while diamond does not. Visual cues offer non-destructive indicators during preliminary inspection. Rough diamonds often exhibit angular, cubic habits such as octahedrons, with triangular features called trigons on their faces, and they may lack cleavage planes in certain directions due to irregular fracturing. Under (UV) light, many rough diamonds display blue , though this varies and is not universal; simulants like may show different colors or none at all. These traits, combined with a greasy or luster, help rule out look-alikes in the field. For definitive confirmation, advanced tools like are employed in laboratory settings. infrared (FTIR) spectroscopy analyzes the stone's absorption spectrum to confirm its carbon-based lattice structure, producing characteristic peaks that distinguish diamond from (silicon carbide) and (zirconium silicate). This method is particularly useful for rough specimens with opaque inclusions or irregular surfaces, ensuring accurate identification without invasive procedures.

Sorting Criteria

Rough diamonds, once identified as authentic through preliminary tests such as thermal conductivity assessment, are sorted into categories to facilitate efficient and distribution. This sorting primarily occurs at major trading centers like those operated by ' Diamond (), where stones are manually examined and classified into thousands of distinct categories based on key attributes. Size is a foundational step, typically beginning with mechanical methods for smaller stones and precise measurements for larger ones. For diamonds, which weigh less than 0.2 s, sorters use mesh screens or sieves with varying aperture sizes to separate them by approximate weight and dimension. Larger rough diamonds, such as those in the small category (0.2 to 1 ) or commercial sizes (above 1 ), are weighed on scales and often scanned using laser-based systems for accurate dimensional . These categories help determine handling requirements, with often destined for stones and larger pieces evaluated for potential yield. Shape classification focuses on the natural of the , which influences its suitability for specific polished forms. Common habits include octahedrons, dodecahedrons, and cubes, with well-formed octahedrons often deemed "makeable" for brilliant cuts due to their symmetrical structure that allows maximal retention of weight. In contrast, irregular or macle shapes—such as twinned crystals or distorted forms—are typically allocated to cuts like pears or marquises, where their unique contours can be preserved for aesthetic appeal. employs standardized shape charts to codify these forms, ensuring consistency across sorting operations. Quality tiers provide an initial grouping based on observable color and visibility, serving as a rough for clarity before detailed grading. Color is assessed via the stone's natural under controlled lighting, categorizing from colorless (high tiers) to those with faint or hues (lower tiers), with rare colors separated entirely. visibility is gauged by eye or , grouping stones into tiers where minimal surface-reaching flaws indicate higher potential quality, while heavily included pieces are flagged for use. ' integrated shape/size charts incorporate these quality indicators, combining them with size and form data to create over 16,000 provisional classifications for trading sight boxes.

Evaluation and Valuation

Factors Affecting Value

The value of a rough diamond is primarily determined by four key criteria analogous to the 4Cs of polished diamonds, adapted for the uncut state: (carat weight), , color, and clarity. Larger s generally command a higher value per due to their rarity and the potential to yield significant polished stones, with stones exceeding 10 s often fetching premiums because of limited supply. The , or "make," of a influences its value based on cutting efficiency; for instance, "makable" shapes that allow for minimal during are more valuable than irregular forms like macles, which may limit output to smaller or specialty cuts. Color plays a pivotal role in valuation, with colorless or near-colorless rough diamonds (graded D-J) forming the baseline, while tinted varieties like (K-M) or (beyond M) see reduced prices unless exhibiting desirable hues. Rare fancy colors, such as pinks or blues, significantly elevate value due to their , often multiplying the price by up to 100 times compared to standard white diamonds of similar size. Clarity assesses the presence of internal imperfections, where fewer inclusions lead to higher grades and greater worth, as high-clarity rough can yield flawless or near-flawless polished results. Inclusions critically impact by affecting both post-cut and ; minor types like pinpoints—tiny, isolated —typically have negligible effects and do not substantially lower price if they remain hidden after . In contrast, fractures or feathers, which are tension-induced cracks, can drastically reduce by complicating cutting, increasing breakage risk, and potentially lowering the final clarity grade. Beyond these attributes, rarity amplifies for exceptional specimens, such as large stones over 10 carats or those with intense colors, where natural occurrence rates are low— colored represent approximately 2% of rough production, though vivid hues are much rarer. For example, a vivid rough of substantial size can achieve multipliers far exceeding standard gems, reflecting its geological uniqueness and market demand.

Market and Trading

The global market for rough diamonds is dominated by a few key producers and trading hubs, with De Beers Group and ALROSA PJSC as the leading players. De Beers, a subsidiary of Anglo American, controls approximately 30% of the global rough diamond supply volume, primarily through its operations in Botswana, Namibia, and South Africa, where it influences pricing and distribution via its Diamond Trading Company (DTC) sightholder system. ALROSA, based in Russia, is the world's largest producer by volume, accounting for about 27% of global output, mainly from Siberian mines, and contributes significantly to the supply chain through state-backed exports. Since 2024, G7 and EU sanctions on Russian diamonds have banned direct imports of Russian rough to participating countries, reducing global trade volumes through traditional hubs and prompting ALROSA to cut production by 4.6% in 2024, with further reductions planned for 2025. Major trading centers include Antwerp, Belgium, which handles over 80% of the world's rough diamonds through its historic district and serves as a primary sorting and valuation hub, and Dubai, United Arab Emirates, which has emerged as a key player since 2021, with annual rough diamond trade values exceeding $20 billion as of 2023 due to favorable regulations and logistics. To ensure ethical trade and curb the flow of conflict diamonds—those funding rebel groups—the was established in 2003 as an international agreement among governments, industry, and . The scheme requires all participating countries, representing over 99% of global production, to certify shipments of rough diamonds as conflict-free before export, involving rigorous verification of origins, secure transport, and chain-of-custody documentation to prevent illicit entry into legitimate markets. Compliance is monitored through annual audits and peer reviews, with non-compliant shipments subject to bans, though critics note limitations in addressing abuses beyond armed conflict. Rough diamond pricing is influenced by supply-demand imbalances in the polished market, with transactions primarily occurring through auctions, tenders, and allocation systems rather than open exchanges. Producers like conduct regular tenders, where buyers bid competitively on parcels, while uses fixed-price sightholders for select clients and occasional auctions for surplus stock, leading to price volatility; for instance, rough prices declined 10-15% in late 2024 to stimulate demand amid oversupply. Indices such as the track these fluctuations by weighting average prices across size, shape, and quality categories, showing ties to polished diamond retail trends and economic factors like consumer spending in major markets such as the and .

Processing

Planning and Cutting

The planning process for cutting a rough diamond begins with careful to determine the optimal strategy for transformation into a polished gem, aiming to maximize the final stone's value based on the four Cs: weight, color, clarity, and cut. s are first sorted by size using sieves and gauges, (such as sawable, makeable, or cleavable), color under daylight conditions, and clarity to assess cutting potential. Markers then use a and to measure dimensions and identify inclusions, marking a precise line on the stone to guide divisions that minimize visibility of flaws while preserving maximum yield. Advanced scanning technologies enhance this planning by creating detailed three-dimensional models of the rough diamond. Systems like the Dia-Expert employ cameras and light sources to scan the stone in multiple orientations, generating a virtual representation that reveals internal structures, including inclusions, and simulates potential cut outcomes with estimated weights and values. As of 2025, integrations of in planning systems, such as those developed by Sarine Technologies and implemented by producers like , further automate decision-making, optimizing cut plans for higher yields and efficiency by analyzing vast datasets of rough diamond morphologies. This computer-aided approach allows planners to evaluate various options, such as the number and size of polished stones that can be extracted, ensuring decisions align with market demands and production costs. Manual marking remains essential for final decisions, often incorporating the scanned data to position cuts strategically around inclusions. Initial cuts follow planning to divide or shape the rough diamond, primarily through cleaving or sawing. Cleaving exploits the diamond's natural octahedral cleavage planes, where a laser first creates a shallow V-shaped groove (kerf) along the marked line to weaken the structure, followed by a precise strike with a knife and hammer to split the stone. This method is ideal for pieces with strong cleavage directions but requires expertise to avoid shattering. Alternatively, sawing uses a high-speed phosphor-bronze blade coated with diamond powder, rotating at up to 10,000 rpm, or a YAG laser that vaporizes material along the marked path, offering greater flexibility for irregular shapes and reducing the risk of uncontrolled breaks. Laser sawing, in particular, processes a 1-carat diamond in about 20 minutes, compared to over two hours mechanically, while maintaining precision. After division, bruting rounds the diamond's edges to form the outline, establishing the basic shape for further processing. In this step, two rough pieces are mounted on opposing lathes rotating in opposite directions at around 3,000 rpm, grinding against each other through mutual to create a symmetrical, typically round or fancy-shaped contour. Automated bruting machines incorporate centering systems and real-time monitoring to ensure uniformity, minimizing material loss and preparing the stone for . This labor-intensive process, whether manual or machine-assisted, directly influences the final diamond's proportions and appeal.

Yield and Waste

The yield in diamond processing refers to the of the rough diamond's that is converted into polished gem-quality , typically ranging from 40% to 50% for well-shaped, inclusion-free stones. For instance, a 5-carat rough diamond might 2 to 2.5 carats of polished diamonds after cutting and . This metric is calculated simply as ( of polished diamond / of rough diamond) × 100, guiding manufacturers in assessing profitability. However, the placement and nature of inclusions often necessitate strategic cuts to exclude flaws, reducing yield to below 30% in challenging cases, as portions of the rough must be sacrificed to achieve clarity in the final stone. Planning decisions, such as selecting facet orientations, directly influence these outcomes by balancing size against quality preservation. Major sources of waste include kerf loss during sawing, where each cut removes 0.1 to 0.2 mm of as a thin sliver, and fine powder generated from grinding and , which can account for up to 50% of the rough's weight. Offcuts—larger remnants unsuitable for gem-quality —are frequently repurposed for applications, such as abrasives in cutting tools or equipment, thereby recovering some value from otherwise lost . To optimize and minimize waste, modern strategies employ computer modeling and scanning technologies, such as high-resolution inclusion mapping systems, which simulate cut plans to maximize recoverable weight while avoiding defects. These advancements, including laser sawing introduced since the 1980s, have improved efficiency over historical manual methods, elevating average yields from around 30% in mid-20th-century practices to 40-50% today through precise material removal and automated planning.

Uses and Significance

Jewelry and Industrial Applications

Rough diamonds, valued for their natural, unpolished form, find niche applications in contemporary jewelry designs that celebrate their raw aesthetic over traditional faceted gems. Artisans often select high-quality rough stones with minimal shaping to create pieces like necklaces, rings, and earrings, where the irregular surfaces and internal inclusions highlight an organic, earthy appeal. For instance, raw diamond necklaces typically feature hand-set rough crystals on or chains, allowing the stones' translucent yet rugged beauty to stand out in everyday or statement jewelry. This trend appeals to consumers seeking authenticity and uniqueness, diverging from the conventional sparkle of cut diamonds. In traditional contexts, uncut diamonds appear in styles like Polki jewelry, a technique originating in that embeds rough or lightly crushed diamonds into intricate settings to preserve their inherent luster and form. These pieces emphasize while showcasing the diamonds' natural shine without polishing, making them prized in bridal and ceremonial wear. Such applications are relatively rare, as most rough diamonds do not meet the clarity or size standards for direct jewelry use, but they underscore a growing appreciation for the stone's unaltered state. Emerging trends in ethical jewelry further promote rough diamonds through varieties like salt-and-pepper stones, which contain distinctive inclusions that create a mottled, appearance reminiscent of . These diamonds, often sourced from conflict-free mines, require little to no cutting, minimizing environmental impact and appealing to eco-conscious buyers who value imperfection and over flawless clarity. Their popularity has surged in modern engagement rings and minimalist designs, positioning them as an affordable, unique alternative in the ethical gemstone market. In industrial applications, approximately 80% of mined rough diamonds are classified as industrial grade due to imperfections that render them unsuitable for gems, and they are primarily processed by crushing into or for use as abrasives. This , derived from fragmenting low-quality rough stones, serves as a key component in grinding wheels, compounds, and cutting tools, leveraging diamond's unmatched hardness (10 on the ) to shape hard materials like , ceramics, and stone. For example, diamond is electroplated onto saw blades and files for precision cutting in and . Rough diamonds also play a vital role in and , where crushed forms are embedded in bits for , gas, and operations to penetrate tough geological formations efficiently. These polycrystalline diamond compact (PDC) cutters, made from aggregated rough particles, withstand extreme pressures and temperatures, extending tool life in downhole by up to several times compared to alternatives. After minimal crushing and sizing, such rough diamonds enable these durable products, though synthetic diamonds now dominate over 99% of the overall market for and reasons.

Notable Examples

One of the most notable rough diamonds in recent history is the Lesedi La Rona, a 1,109-carat gem-quality discovered in April 2015 at the Karowe Mine in . Recovered by Lucara Diamond Corp., it represented the largest found in over a century, symbolizing 's prominence in global diamond production and sparking international interest in ethical practices. In 2017, the rough stone was sold privately to Graff Diamonds for $53 million, a record price that underscored its exceptional size, clarity, and potential yield of high-value polished gems. Graff subsequently cut the Lesedi La Rona into 10 principal diamonds, including several flawless D-color stones exceeding 100 carats, enhancing its legacy as a modern icon of luxury and craftsmanship. The Cullinan Diamond stands as the largest gem-quality rough diamond ever discovered, weighing 3,106 carats and found on January 25, 1905, at the near , . Unearthed during a routine inspection by mine superintendent Frederick Wells, the massive, colorless captured global attention and was named after Sir Thomas Cullinan, the mine's owner. Presented as a to VII in 1907 to symbolize loyalty from the , it was cut in into nine major facets—the largest being the 530-carat Great Star of Africa—and 96 smaller brilliants, many of which now adorn the British . This diamond's discovery and royal association elevated it to a symbol of imperial prestige, influencing perceptions of diamonds as emblems of power and enduring legacy. Another landmark rough diamond is , a 995.2-carat stone discovered on June 30, 1893, at the in South Africa's . Found by a mine worker sifting gravel, the irregular, slightly bluish-white crystal was the largest known at the time, holding that distinction until the Cullinan's unearthing over a decade later. Its exceptional size and subtle blue tint contributed to its fame, representing the era's and the geological richness of South African kimberlites. The was later cut into 21 pieces by Joseph Asscher in , yielding gems that circulated in high-society jewelry, thereby cementing its place in the annals of diamond exploration and trade history. The Motswedi diamond, discovered in August 2024 at the Karowe Mine in by Lucara Diamond Corp., weighs 2,488 carats after cleaning and ranks as the second-largest gem-quality ever found. This Type IIa , named "Motswedi" (meaning "the river" in Setswana), measures approximately 106 × 72 × 54 mm and exhibits no detectable impurities, confirming its high gem potential. Recovered using advanced technology, it underscores ongoing innovations in mining and 's continued role in major diamond discoveries as of 2025.

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