Somaliland’s Prospects of Opportunities and Challenges

Somaliland has 72 records of mines listed by the United States Geological Survey (USGS): According to geology survey, Republic of Somaliland capacity mining is first-grade at 72 mines operational and majority still in development. Somaliland commodity, disposition, development status, and record type in Somaliland:

Mining Commodities in Somaliland

  1. Lead: Lead, while a valuable metal, is primarily used in lead-acid batteries for vehicles, backup emergency systems, and the telecoms sector. Historically, it has been used in a wider range of applications, including paints, plumbing, ammunition, and radiation shielding, but concerns about its toxicity have led to a reduction in these uses. 
  2. Barium-Barite: Barytes, also known as barite (BaSO4), is a barium sulfate mineral with a wide range of applications. Its primary use is as a weighting agent in drilling mud for oil and gas exploration. Other important applications include radiation shielding, filler in paints and plastics, and as a constituent in various chemical and industrial processes. 
  3. Iron: Iron, in the form of iron ore, is primarily used in the production of steel. Steel is the key ingredient in most metal products, including structures, ships, automobiles, and machinery. Steel represents almost 95% of all metal used per year, making it crucial for various industries. Steel is used in construction, transportation, energy infrastructure, and even household appliances.
  4. Beryllium: Beryllium and its compounds are used in a wide range of industries and applications, including aerospace, automotive, electronics, defense, and medical fields. Beryllium’s unique properties, such as high flexural rigidity, thermal stability, and low density, make it a valuable material for various applications.
  5. Manganese: Manganese, a crucial mineral, is widely used in various applications, primarily in the production of steel and as an alloying agent in non-ferrous metals. It’s also used in dry cell batteries, pigments, glass making, and as a micronutrient in fertilizers and animal feed.
  6. Copper: Copper minerals are primarily used for their valuable metallic properties, particularly their excellent electrical and thermal conductivity. This makes them crucial in electrical wiring, power transmission, and a wide range of electrical and electronic devices. Additionally, copper’s durability and resistance to corrosion make it a useful material in building construction, plumbing, and industrial machinery. Furthermore, copper is a key ingredient in many alloys, such as brass and bronze, which are used in various applications including piping, coinage, and musical instruments.
  7. Niobium (Columbium): Niobium, also known as columbium, is primarily used as an alloying element in steels and superalloys, enhancing their strength, corrosion resistance, and temperature resistance. It also plays a role in aerospace, electronics, and energy storage applications. Steel Alloying: Niobium significantly enhances the strength and toughness of low-alloy steels used in various applications like automobiles, aircraft, and pipelines. Superalloys: Niobium is crucial in high-temperature superalloys for jet engines, rocket subassemblies, and other high-performance applications. Welding: Niobium is used in arc-welding rods for stabilized stainless steels. Superconducting Materials: Niobium is a key component in superconducting materials used in MRI scanners and other applications. Energy Storage: Niobium-containing materials are being explored for their impact on battery performance, enhancing storage capacity and power. Other Applications: welding, nuclear industries, electronics, optics, numismatics, and jewelry.
  8. Molybdenum: Structural Steel: A significant portion of molybdenum usage is in structural steel, where it enhances strength and durability. Stainless Steel:Molybdenum is essential for the corrosion resistance of stainless steel, particularly in high-performance grades. Tool Steels: Molybdenum is added to tool steels to increase their hardness, toughness, and resistance to wear, making them suitable for tools and cutting edges. Other Applications: Molybdenum’s ability to withstand high temperatures also makes it useful in applications like furnace parts, electrical contacts, and supports for filaments in light bulbs. Molybdenum, a silver-white metal, is primarily used in metallurgy, particularly for making alloys, and in chemical applications. It’s added to steel to enhance strength, hardness, electrical conductivity, corrosion resistance, and wear resistance, making it a key component in various industrial applications, including engine parts and high-temperature superalloys.
  9. Asbestos: Asbestos is no longer widely used because it poses serious health risks, especially when inhaled, leading to diseases like asbestosis and lung cancer. Due to these dangers, mining and use of asbestos have been phased out in many countries, with bans and restrictions in place to protect public health.
  10. Fluorine-Fluorite: Metallurgy:Fluorite acts as a flux in the smelting and refining of metals like steel, aluminum, lead, and antimony. It helps to lower the melting point of ores, remove impurities, and facilitate the desired chemical reactions. Glass and Ceramics:Fluorite is used in the production of various types of glass, including opalescent glass and enamels. Optics:Due to its low dispersion and refractive properties, fluorite is used in the manufacture of lenses and prisms for cameras, telescopes, and fluorescence microscopes.
  11. Titanium Metal: Aerospace:Titanium’s strength and light weight make it ideal for aircraft engines, frames, and other parts. Medical:Its biocompatibility makes it suitable for implants, prosthetics, and dental implants. Automotive:Titanium’s lightweight and durability contribute to fuel efficiency and long-lasting components. Consumer goods:Titanium is used in jewelry, sporting equipment (golf clubs, bicycles), and other applications where strength, light weight, and corrosion resistance are desired. Extraction and Processing:1.Titanium is primarily extracted from its ores, including ilmenite, rutile, and leucoxene. 2.These ores are processed to obtain titanium dioxide (TiO2) or to produce titanium metal. 3.The Kroll and Hunter processes are used to extract titanium metal from its ores.
  12. Tin: Tin, a versatile metal, is widely used for various applications, including protective coatings, solder, and alloys like bronze. It’s a crucial component in food packaging, electronics, and even has applications in glass-making and ceramics. Solder: Electronics: Tin-lead solder is a major component in electronic circuits, joining components and wires.Plumbing and Machinery: Tin-lead solder is also used in plumbing and machinery applications. Other Applications:Glass Making: Tin oxide is used in glass production. Ceramics: Tin compounds are used in ceramics and glazes. Chemical Applications: Tin compounds are used in plastics, wood preservatives, pesticides, and fire retardants. Batteries: Tin is used in both lead-acid and lithium-ion batteries. Optoelectronics: Tin is a component in transparent, electrically conducting films used in optoelectronic devices. Solar Panels: Tin is used in solder ribbons to connect solar panels.
  13. Garnet: Water Jet Cutting:Its excellent cutting properties make it suitable for cutting various materials like metal, ceramic, and stone. Filtration:Garnet is used as a filtration media in water treatment. Other Abrasive Applications:Garnet is also used in polishing, grinding, and as an antiskid surface for roads and runways. Jewelry and Ornaments:Garnets have been used as gemstones for centuries, with red garnets being particularly popular.
  14. Graphite: Graphite, a form of carbon, has numerous applications due to its unique properties. It’s used as a lubricant, in pencil leads, in steelmaking, and in the production of batteries. Lubricant:Graphite’s soft, flaky nature allows it to slide easily, making it a good solid lubricant. Pencil Lead:While the term “lead” is a misnomer, graphite is the primary material in the “lead” of pencils. Refractory Materials:Graphite is used in bricks that line blast furnaces and in other high-temperature applications. Batteries:Graphite is a key component in the anode of lithium-ion batteries, including those used in electric vehicles. Steelmaking:Graphite is used as electrodes in electric arc furnaces and in other steel production processes. Other Uses:Graphite also finds applications in lubricants, carbon brushes, brake linings, nuclear reactors, and various industrial processes.
  15. Quartz: Quartz sand (silica sand) is the primary ingredient in the production of various types of glass, including containers, flat glass, and fiberglass. Quartz crystals, due to their piezoelectric properties, are used in oscillators for clocks, watches, radios, and other electronic devices. Quartz is used in the production of silicon wafers, which are essential for computer chips and other semiconductors. Cosmetics: Quartz can be used in toothpaste and other cosmetic products. Quartz sand is used in hydraulic fracturing to hold open fractures in oil and gas wells. Construction: Quartz sand, a major component of concrete, is used in building materials, as well as in the production of glass and ceramics. Electronics: Quartz crystals are used in oscillators for clocks, watches, and electronic devices like radios and computers, taking advantage of their piezoelectric properties. Gemstones and Jewelry: Many varieties of quartz, like amethyst and citrine, are used as gemstones in jewelry and decorative carvings. Industrial Applications: Quartz is used in abrasive materials like sandpaper, as well as in sandblasting and for making whetstones and grindstones. Laboratory and Scientific Equipment: Fused quartz, a high-purity form of glass made from quartz, is used in laboratory glassware, tubing, and other equipment due to its heat resistance and chemical inertness. Other Uses: Quartz is also used in the production of silicon for semiconductors and in the petroleum industry for hydraulic fracturing, where it helps to keep fractures open in oil and gas wells.
  16. Silica: 1. Glass and Ceramics: Silica, in the form of sand or quartz, is the primary ingredient in most glass types, including bottles, flat glass, and optical glass. It’s also a key component in ceramics, used in tableware, tiles, and other products. 2. Construction and Building Materials: Silica sand is a vital component of concrete and mortar, and its hardness and resistance to fracture make it suitable for building stones, road construction, and other applications. 3. Foundry Casting: Silica sand’s high melting point and ability to withstand high temperatures make it ideal for forming molds in foundries, particularly for aerospace, military, and automotive components. 4. Filtration: Silica sand, with its carefully controlled particle size, is a common filtration medium in the food and water industries, used to remove solids from potable and wastewater. 5. Food and Pharmaceuticals: Silica is used as a food additive (e.g., anti-caking agent), in beverage clarification, and as a component in some drug and vitamin formulations. 6. Other Industrial Uses: Silica is used in paints, plastics, rubber, and as a filler in various materials. It also plays a role in semiconductor manufacturing, electronics, and other specialized applications.
  17. Uranium: Nuclear Power: Uranium is the main fuel for nuclear reactors, where it undergoes fission to release energy, which is then used to generate electricity. Medical Isotopes: While a small amount of uranium is used, it’s crucial for producing medical isotopes used in diagnostics and treatments. Naval Propulsion: Nuclear reactors powered by uranium fuel are used in naval vessels, including submarines and aircraft carriers. Nuclear weapons: Uranium, particularly highly enriched uranium (HEU), is a key ingredient in nuclear weapons.
  18. Kyanite: Kyanite’s unique combination of hardness, high-temperature resistance, and electrical insulating properties makes it a versatile material with applications ranging from high-temperature industrial processes to gemstone jewelry. High-temperature refractories: Kyanite is crucial in refractory bricks, mortars, and kiln furniture used in high-temperature furnaces, such as those used in steel and glass production. High-strength porcelain:Kyanite’s properties make it ideal for producing high-refractory-strength porcelain, particularly for applications requiring resistance to high temperatures, like spark plug insulators. Ceramic products:Kyanite is incorporated into various ceramic products, including plumbing fixtures and dishware. Electronics and electrical insulators: Kyanite’s electrical insulating properties make it useful in electronic applications. Abrasives: Kyanite’s hardness and durability can be utilized in abrasive materials. Automotive and railroad industries: Kyanite’s heat resistance is important in these industries, with applications in brake shoes and clutch facings.
  19. Chromium: Stainless steel:Chromium is a key component in producing stainless steel, making it durable and resistant to rust and corrosion. Alloys:It’s also used in other alloys, including those that are heat-resistant, like nichrome, and those used in jet engines. Plating:Chromium plating provides a hard, corrosion-resistant surface on various objects, including car parts, appliances, and cutlery. Furnaces and other applications:Chromite’s high melting point and resistance to heat and chemicals make it suitable for use in refractory bricks and linings for furnaces and other industrial applications. Medical applications: Chromium is also used in medical applications due to its corrosion resistance and hygiene properties.
  20. Nickel: 1. Stainless Steel Production: Nickel is a key component in austenitic stainless steel, which is known for its corrosion resistance and strength. About 65-70% of nickel production is used in stainless steel applications. Stainless steel is used in a wide range of applications, including buildings, bridges, kitchen appliances, and industrial equipment. 2. Rechargeable Batteries: Nickel is essential in high-performance rechargeable batteries, especially those used in electric vehicles. Nickel-based batteries (e.g., nickel-cadmium, nickel-metal hydride, and lithium-ion batteries) contribute to the development of greener technologies. Nickel helps improve the energy density and extend the range of electric vehicles. 3. Alloys and Plating: Nickel is used in various alloys, including copper-nickel alloys used in desalination plants and nickel-steel alloys used for armor plating. Nickel electroplating provides a protective coating on other metals, enhancing their durability.
  21. Bismuth: Bismuth is a mineral used in a variety of applications, including pharmaceuticals, cosmetics, electronics, and alloys. It’s known for its low toxicity and unique properties, which make it a useful replacement for lead in some materials. Pharmaceuticals: Bismuth subsalicylate, found in Pepto-Bismol, is used to treat upset stomachs and diarrhea. Cosmetics: Bismuth oxychloride (BiOCl) is used as a pearly powder in lipsticks, eyeshadow, and nail polish to create a shiny effect. Electronics: Bismuth can be used in electronic components and semiconductors due to its high electrical resistance and low thermal conductivity. Nuclear Medicine: Bismuth isotopes are used in nuclear medicine to treat certain types of cancer and other medical conditions. Alloys: Bismuth is used in low-melting point alloys and as a component in solders. Other Uses: Bismuth can also be found in pigments, paint, and even as a replacement for lead in certain materials like ceramic glazes and fishing sinkers.
  22. Platinum: Catalytic Converters: Platinum, along with other platinum group metals (PGMs), is a key component in catalytic converters, which reduce harmful emissions from vehicles. Jewelry: Platinum’s durability and luster make it a popular choice for jewelry. Dentistry: Platinum is used in dental alloys for crowns, bridges, and other dental appliances. Chemical Industry: Platinum serves as a catalyst in the production of various chemicals, such as nitric acid, silicone, and benzene. Electronics: Platinum is used in electrical contacts, capacitors, and other electronic components. Medical Devices: Platinum is used in pacemakers, heart valves, and certain chemotherapy drugs. Glass Manufacturing: Platinum is used in bushing for making glass fibers used in fiber-reinforced plastics. Other Applications: Platinum is also used in high-temperature electric furnaces, resistance wire, laboratory equipment, and corrosion-resistant devices.
  23. Mica: 1. Electronics and Electrical Components: Insulation:Mica’s excellent insulation properties are crucial for protecting delicate electronic components and preventing electrical breakdowns. Capacitors:Mica is used in the construction of mica capacitors, known for their stability and precision. Flexible Sheets:Flexible mica sheets can be used as insulation in various applications, including heating elements and micro-electronic motors. Electrical Wiring:Grounded mica can be used in electrical cables and for general insulation. 2. Construction and Industrial Applications: Reinforcement in Plastics:Mica enhances the mechanical strength, dimensional stability, and heat resistance of plastics, particularly in automotive and electronic components. Asphalt and Roofing:Mica is used as a protective coating and weather-proofing material in asphalt roofing felts and shingles. Concrete and Gypsum Board:Mica can be used to reinforce concrete structures, improve fire resistance, and enhance sound absorption in gypsum board. Paint and Coatings:Mica improves the physical properties, durability, adhesion, and water-proofing of paints. High-Temperature Applications:Mica’s heat resistance makes it suitable for lining materials in furnaces, kilns, and crucibles. 3. Other Uses:Ornamental and Decorative Applications: Mica’s aesthetic appeal makes it suitable for use in ornaments, decorative panels, and as a decorative stone. Artificial Snow: Mica can be used to create artificial snow effects. Lasers: Mica is used in lasers, as some types of mica are used for lithium extraction, which is a key ingredient in laser technology.
  24. Silver: Silver, both as a metal and in various compounds, is used in a wide array of applications, including photography, electronics, medicine, and industrial processes. Photography: Silver halides (like silver chloride, bromide, and iodide) are light-sensitive and form the basis of photographic film and printing. Electronics: Silver is used in electrical contacts, batteries, printed circuits, and semiconductors due to its excellent conductivity and corrosion resistance. Medicine: Silver, especially in its colloidal form or as compounds like silver nitrate, has antimicrobial properties and is used in wound dressings, disinfectants, and medical devices. Industrial Processes: Silver is used in solder and brazing alloys, mirrors (where its reflectivity is valuable), and as a catalyst in various chemical reactions. Solar Technology: Silver is used in photovoltaic (solar) panels, contributing to their efficiency. Jewelry and Decorative Objects: Silver’s beauty and durability make it a popular choice for jewelry, tableware, and other decorative items. Currency and Investment: Historically, silver was a key component of monetary systems and is still used as an investment asset. Other uses: Silver is also found in water purification systems, some food packaging, and certain types of stained glass.
  25. Gemstone: Gemstones, which are minerals or organic materials prized for their beauty, durability, and rarity, are primarily used for jewelry and decorative purposes. They are cut and polished to enhance their natural beauty and are incorporated into a variety of jewelry pieces, such as necklaces, bracelets, rings, and earrings. Additionally, some gemstones are used in decorative arts, such as artwork, mosaics, and carved items. Jewelry: Gemstones are a cornerstone of the jewelry industry, with various types like diamonds, sapphires, emeralds, and rubies being widely used in jewelry making. Decorative Arts: Beyond jewelry, gemstones have been used throughout history to decorate and embellish various objects, including combs, plates, ceremonial objects, and even weapons. Other Uses: While primarily used for adornment, some gemstones have specialized applications. For example, certain types of diamonds have been used in semiconductors due to their electrical properties. Organic Gemstones: While many gemstones are minerals, some are organic materials, such as amber and pearls, which are still valued for their beauty and are used in jewelry and decorative arts. Gemstone Properties: Gemstones are chosen for their beauty, which can include their color, luster, and other special features like iridescence, opalescence, and chatoyance. They are also chosen for their durability, which means they are resistant to wear and tear and can maintain their polish over time.
  26. Zinc: Zinc, a metallic element, is widely used for corrosion protection (galvanizing), creating alloys (like brass and bronze), and in various industrial applications, including die-casting and the production of compounds like zinc oxide used in paints, rubber, and pharmaceuticals. It also plays a vital role in the human body, supporting immune function, wound healing, and other processes. 1. Corrosion Protection: Galvanizing: Zinc is applied to iron and steel surfaces to form a protective layer that prevents rust. This is a major use of zinc, accounting for a significant portion of global production. 2. Alloys: Brass: Zinc is a key component in brass, an alloy of copper and zinc, which is used in musical instruments, jewelry, and coins. Bronze: Zinc can also be combined with copper and tin to create bronze. Other Alloys: Zinc is also alloyed with other metals for die-casting into shapes like door handles and other components. 3. Industrial Applications: Die-casting: Zinc is used in die-casting to produce precision parts, particularly in the automotive industry. Zinc Oxide: Zinc oxide is a versatile compound used in paints, rubber, textiles, pharmaceuticals, and other products. Batteries: Zinc is used in some types of batteries.
  27. Gold: Nearly half of all mined gold is used to manufacture jewelry – 46%, to be specific. This makes the gold jewelry industry the single biggest demand driver for gold bullion
  28. Diamonds: Diamonds, a mineral made of pure carbon, are known for their hardness and are used in a variety of applications, including jewelry, industrial tools, and medical devices.
  29. Galena: Galena is primarily used as a lead ore, making it a crucial source of lead. It’s also mined for its silver content, which is often present as an impurity. Beyond these core uses, galena has been utilized as a semiconductor and in early wireless communication systems, such as crystal radios.
  30. Fluorite: Metallurgy:Fluorite acts as a flux in the smelting of metals, including steel, aluminum, and lead, helping to melt ores and remove impurities. Chemical Industry:It’s a crucial source of fluorine, used in the production of hydrofluoric acid, which is a key ingredient in various chemical processes. Optical Applications:Fluorite’s unique optical properties, including its low dispersion and high refractive index, make it suitable for making apochromatic lenses and other optical instruments, particularly for applications in the ultraviolet and infrared spectrums. Other Industries:Fluorite is also used in the manufacture of glass, ceramics, and enamels, as well as in the production of some fuels and refrigerants. Dental Applications:Fluoride, derived from fluorite, is added to toothpaste and water to prevent tooth decay by strengthening tooth enamel. Ornamental and Lapidary Uses:Due to its colorful and sometimes fluorescent properties, fluorite is also used for ornamental and lapidary purposes.
  31. Apatite: Gemstone: While not as common as other gemstones, apatite can be faceted and used in jewelry. It comes in various colors, including green, blue, violet, brown, and colorless. Blue apatite, often the result of heat treatment, is a popular choice. Industrial Applications: Other chemical industries: Apatite can be used in various chemical processes, including the production of hydrofluoric acid (by byproduct) and in the sugar refining industry.Ceramics: Apatite can be used in the production of ceramics.Pharmaceuticals: It’s used in the pharmaceutical industry, though the specific uses are not detailed in the provided search results.Textiles: Apatite plays a role in the production of textiles.Insecticides: Apatite is also used in the production of insecticides.Explosives: Apatite is used in the manufacture of explosives.5. Potential Nuclear Waste Storage: Apatites are being investigated as potential host materials for storing nuclear waste.
  32. Magnetite: Iron Ore for Steel Production:Magnetite is a major source of iron for making steel, which is crucial for various industries and applications. Magnetic Applications:Its strong magnetic properties are utilized in creating magnets, magnetic tapes for audio and video recording, and in data storage technologies. Medical Applications:Magnetite can be used in MRI contrast agents and for targeted drug delivery in the body. Heavy Media Separation:Its high density makes it valuable for separating minerals and materials based on density, such as in coal washing. Catalyst:Magnetite can act as a catalyst in chemical reactions, such as in the Haber process for ammonia production. Pigment:Magnetite is used as a pigment in paints and ceramics. Environmental Applications:Magnetite nanoparticles are used for water treatment and pollutant removal. Thermal Energy Storage:Magnetite can be used in thermal energy storage applications. Cementitious Composites:Magnetite nanoparticles can improve the properties of cement, such as strength and resistance to water absorption.
  33. Rhodonite: Rhodonite is primarily used as an ornamental stone, particularly in jewelry and decorative items like carved objects and beads. Its distinctive pink color and pattern, often contrasted with black manganese veins, make it a visually appealing material. While not as hard as some other gemstones, its unique beauty ensures its popularity for various decorative and jewelry applications. Ornamental Stone:Rhodonite’s striking appearance makes it a popular choice for decorative purposes. Jewelry:It’s often used in jewelry, particularly for beads, cabochons, and carved pieces. Decorative Items:Rhodonite is also used to create various decorative items like vases, tables, and even tombstones, as evidenced by the sarcophagus for Russian Empress Maria Alexandrovna. Carved Objects: Its relatively soft nature allows for carving into various shapes and forms, including sculptures and smaller decorative items.
  34. Chalcopyrite: Copper Production:Chalcopyrite is a key ore for copper extraction, which is a vital metal used in various applications. Electrical Equipment:Copper’s excellent conductivity makes it essential for wiring, motors, and other electrical components. Construction:Copper is used in plumbing, roofing, and other building materials. Technology:Copper is increasingly important in renewable energy, electronics, and other advanced technologies. Jewelry and Design:While not its primary use, chalcopyrite’s aesthetic qualities can be utilized in jewelry or decorative pieces. Chalcopyrite is primarily used as the world’s most abundant source of copper. It’s the main copper mineral in various ore deposits, especially porphyry deposits. The extracted copper is used in a wide range of applications, including electrical equipment, construction, and emerging technologies like solar energy production.
  35. Bismuthinite: Alloys:Bismuth is used in various alloys, especially those with low melting points for applications like fire detection, fire extinguishers, and solders. Lead Replacement:Due to its non-toxic nature, bismuth is used as a replacement for lead in applications like ceramic glazes, fishing sinkers, and plumbing. Pharmaceuticals and Cosmetics:Bismuth compounds are used in medications, such as stomach medicines like Pepto-Bismol, and in cosmetics, including pigments and pearly effects. Other Applications:Bismuth is also used as a catalyst in the production of acrylic fibers, in nuclear reactors, and in certain fire detection devices. Pathfinder for other deposits:Bismuthinite’s presence can indicate the potential for other valuable deposits, such as those containing copper, lead, or tungsten.
  36. Olivine: Foundries:Olivine sand is used for cores and molds in metal casting, especially in ferrous and non-ferrous metal casting. Its non-wetting properties make it ideal for manganese steel casting. Refractory Materials:Olivine’s high melting point and resistance to chemical reagents make it suitable for furnace linings and kilns, where materials are subjected to heat and chemical processes. Fertilizer:Olivine can be a source of magnesium, an essential nutrient for plant growth. Gemstone:Peridot, a green variety of olivine, is a prized gemstone used in jewelry. Other Applications:Mineral Wool: Olivine delivers a stable MgO, which is a key component in mineral wool for insulation, soundproofing, and fire-resistant applications. Slag Conditioner: Olivine helps regulate the chemistry of molten steel in steel mills. Animal Feeds: Olivine can be incorporated into animal feed to provide a source of magnesium. Horticultural Applications: Olivine can be used as a soil amendment to provide magnesium and other trace elements.Acid Waste Neutralizer: Olivine can neutralize industrial acid waste. Cement Clinker: Olivine can be used as a component of cement clinker. Lithium-Iron Phosphate Batteries: Olivine’s crystal structure can be used to create high-power-density batteries.
  37. Pyroxene: Construction and Decorative Applications:Crushed stone:Pyroxene is a primary or secondary component of rocks used for crushed stone applications, like road and railroad bed construction. Paving stones:Pyroxene, especially amphiboles like hornblende, are used as paving stones and as veneer or facing on buildings. Decorative stone:Pyroxenes, particularly those with dark green to black colors, are important components of decorative building stones and tile. Architectural stone:They are found in trap rock and “black granites” used for making decorative tile and facing stone. Blast Media:Industrial applications:Pyroxene’s unique properties make it a suitable ingredient for abrasive blasting media in various applications.Precast concrete:It is used in medium to light abrasive blasting applications, such as finishing precast concrete.Restoration work:Pyroxene is ideal for light restoration work on brick & stone, automotive bodies, and wood, removing paint, varnish, and other pollutants. Other Uses:Clinopyroxene thermobarometry:Clinopyroxene, a type of pyroxene, is used in scientific methods to determine the temperature and pressure of magma when the mineral crystallized. Source of lithium:Spodumene, a type of pyroxene, is mined as a source of lithium, used in ceramics and sometimes as a gemstone. Geothermometry:Pyroxene can be used as a geothermometer to estimate the temperature of equilibration in rocks.
  38. Amphibole: Amphibole minerals have various uses, including as decorative materials, building stones, and in construction applications like road and railroad construction. Some amphiboles, particularly those classified as asbestos, were historically used for insulation and fireproofing but are now largely prohibited due to health hazards.
  39. Pyrochlore: Pyrochlore minerals are used in a variety of technological applications, including luminescence, ionic conductivity, nuclear waste immobilization, and thermal barrier coatings. They can also be used as indicators for specialty metal deposits and in the production of various materials like insulators and superconducting materials. Technological Applications:Luminescence:Pyrochlore materials can be used to produce light. Ionic Conductivity:Some pyrochlores exhibit good ionic conductivity, making them useful in applications like solid oxide fuel cells. Nuclear Waste Immobilization:Pyrochlore’s ability to encapsulate radionuclides makes it a potential material for safely disposing of nuclear waste. Thermal Barrier Coatings:High-temperature thermal barrier coatings can be made using pyrochlore materials. Other Applications:Pyrochlores are also used in automobile exhaust gas control, catalysts, and as ionic/electrical conductors. Synthesis and Material Properties:Synthetic Analogues:Synthetic versions of pyrochlore minerals can be created to mimic various properties, including being insulators, ionic conductors, or superconducting.Specific Applications:Different pyrochlore compositions can be tailored for specific applications, such as insulating, conductive, or superconducting materials.
  40. Hematite: Hematite, a common iron oxide mineral, has numerous uses, ranging from being a primary iron ore for steel production to being used as a pigment and in jewelry. It is also employed in medical equipment and even used on Mars. “Blueberries” on Mars: Hematite has been identified as a major component of the “blueberries” found on Mars, contributing to the planet’s red appearance.
  41. Columbite: Electronics:Tantalum, extracted from columbite, is crucial for manufacturing tantalum capacitors, essential components in devices like phones, computers, and cameras. Aerospace:Niobium, also derived from columbite, is used to create superalloys for low-mass, high-strength applications in spacecrafts and jet engines. Construction:Niobium can also be incorporated into high-strength low-alloy (HSLA) steel for construction. Medical:Niobite, extracted from columbite, can be used to create electronic components for medical equipment like MRI and NMR machines. Other uses:Niobium and tantalum are also used in other industries, including defense, chemical processing, and the production of medical implants.
  42. Niobium:1. Steel Alloys:High-Strength, Low-Alloy (HSLA) Steels:Niobium is a key component in HSLA steels, which are used in construction, automotive, and energy pipeline industries. Stainless Steels:Niobium enhances the strength and resistance of stainless steels, particularly at low temperatures. Microalloyed Steels:Niobium’s use in microalloyed steels is increasing due to their application in various industries like car manufacturing, building, and ship construction. 2. Aerospace Applications:Jet Engines and Gas Turbines:Niobium alloys are used in high-temperature applications like turbine blades in jet engines and gas turbines.Rocket Components:Niobium’s high-temperature resistance and strength make it suitable for rocket components. 3. Nuclear Industry:Reactor Components:Niobium’s structural integrity at high radiation levels makes it vital for nuclear reactors. Superconducting Magnets:Niobium-titanium and niobium-tin alloys are used in superconducting magnets for MRI machines, fusion reactors, and other research facilities. 4. Electronics:Lithium-Ion Batteries: Niobium-containing materials enhance battery performance and storage capacity. Capacitors: Niobium oxides are used in capacitors for energy storage. Electronics Components: Niobium wire is used in various electronic components. 5. Medical and Other Applications:Implants: Niobium’s biocompatibility makes it suitable for medical implants like bone plates, screws, and dental prosthetics. Optical Lenses: Niobium is added to glass to create lenses with a higher refractive index, improving optical quality. Catalysts: Niobium oxides are used as catalysts in chemical processes. Nanomaterials: Niobium plays a role in the development of nanomaterials.
  43. Spinel: Spinel is a mineral that is primarily used as a gemstone due to its durability, various colors, and affordability. It is also used in industrial applications, such as in the production of ceramics, due to its hardness and high melting point.
  44. Allanite: Allanite is primarily used as a source for rare earth elements (REEs) and for radiometric dating of rocks. It is also used as a collector’s item due to its interesting appearance. Allanite is a mineral in the epidote group and is known for its high content of REEs, which make it a valuable ore.
  45. Muscovite: Electrical and Thermal Insulation:Electronics: Used in capacitors, electronic components, and as insulation in electric motors and generators. Industrial Furnaces: Thin, transparent sheets of muscovite can be used as high-temperature windowpanes in furnaces and ovens. Insulation: Used to insulate in electrical and thermal equipment, including stove and kerosene heater windows, and in various types of electrical insulation. Paper Industry: Muscovite is used in the manufacture of paper. Roof Coverings: It’s also used in the production of roof coverings. Plasters: Muscovite is used in the manufacture of plasters. Other Applications:Fillers and Extenders: Ground and flaked muscovite is used as a filler in paints, plastic, and wallboard. Paints and Glazes: Muscovite adds a pearly luster and sparkle to paints and ceramic glazes. Cosmetics: Its pearly luster and sparkle make it a valuable ingredient in cosmetics. Wallpaper: Muscovite lends a silky luster to wallpaper. Rubber and Plastic Manufacturing: It’s used as a mold release agent in tire manufacture and as a filler in the production of plastic and rubber products. Drilling Mud: Muscovite is used in drilling mud. Thermal Insulation: Due to its heat resistance, it’s used in applications requiring thermal insulation.
  46. Ilmenite: Ilmenite, a titanium-iron oxide mineral, is primarily used as the main source for titanium dioxide (TiO2), a key ingredient in various products like paints, paper, plastics, and cosmetics. It’s also used to produce titanium metal, which is valued for its strength, lightness, and corrosion resistance, making it ideal for aerospace, medical implants, and other high-performance applications. Additionally, ilmenite is used in steelmaking as a flux and in some ceramics and glass manufacturing.
  47. Malachite: Malachite, a copper carbonate hydroxide mineral, is used for various purposes, including as a gemstone, a decorative stone, a pigment in paints, and as a copper ore indicator. It has also been used in jewelry, decorative objects, and even as a medicinal remedy.
  48. Nickel: Nickel, a silvery-white metal, is primarily used in the production of stainless steel, making up about 65-70% of its global demand. Beyond stainless steel, nickel finds application in batteries, alloys, plating, alloy steels, and various other industrial processes. Major Uses:Stainless Steel:A significant portion of nickel production is used to create stainless steel, which is valued for its corrosion resistance and antimicrobial properties. Batteries:Nickel is a key component in rechargeable batteries, including nickel-cadmium (NiCd) batteries, nickel-metal hydride (NiMH) batteries (used in hybrid vehicles), and lithium-ion batteries (like NCA and NMC used in electric vehicles). Alloys:Nickel is alloyed with other metals to create various alloys with enhanced properties, such as those used in desalination plants, armor plating, and boat propeller blades. Plating:Nickel is used to electroplate steel or brass articles, providing a hard, shiny, and tarnish-resistant surface, often followed by a chromium topcoat. Foundry Products and Metal Powders:Nickel is used in foundries and in the production of metal powders for various industrial applications.Other Uses:Coinage: The US nickel is 25% nickel and 75% copper. Catalysts and Chemicals: Nickel is used as a catalyst in various chemical processes. Medical Devices: Nickel is used in artificial hips and knees, and kidney dialysis equipment. Consumer Products: Nickel can be found in items like zippers, eyeglass frames, cosmetics, detergents, and electronics. Power Plants: Nickel-containing alloys are used in boilers and heat exchangers in power plants. Space Technology: Nickel-containing stainless steel is used in test chambers designed to simulate outer space conditions. Why is Nickel Important? Corrosion Resistance:Nickel’s ability to form alloys that resist corrosion makes it vital in various industrial applications, including shipbuilding, water pipes, and power plants. Essential Nutrient:Nickel is an essential micronutrient for plants. Clean Energy:Nickel is a critical mineral for the development of clean energy technologies, particularly in batteries for electric vehicles and wind and solar power. High Demand:Nickel demand is expected to increase significantly in the coming years, driven by the growth of the EV market and other clean energy applications. 
  49. Kyanite: Kyanite is primarily used as a raw material in the manufacture of refractory products, such as bricks, mortars, and kiln furniture for high-temperature furnaces. It’s also used in ceramics, porcelain, and electrical insulators, and can be a gemstone, though its brittleness limits its use in jewelry.

Somaliland location mining:

  • The Wiget Lead Prospect is located in close proximity to Berbera, a city in the region of Somaliland. The primary minerals extracted from this mining site are chalcopyrite (Copper) and galena (Lead). The ore deposit can be characterized as tabular in shape, measuring approximately 50 meters (164 feet) in length and 6 meters (19 feet) in thickness. The dominant rock type in the vicinity is hornfels, which formed during the Neoproterozoic era, specifically between 1.00 and 0.54 billion years ago. (Lead, Copper)
  • The Hudiso Garnet Prospect is located in Somaliland. The mineralized ores extracted from this prospect primarily consist of kyanite, garnet, and rhodonite. The ore deposit itself exhibits a particular shape, resembling a lens or lenticular structure, with dimensions measuring approximately 3.00 meters (9.84 feet) in length and 3.00 meters (9.84 feet) in thickness. The surrounding host rock in this region is schist, which formed during the Neoproterozoic period, around 1.00 to 0.54 billion years ago. (Garnet)
  • The Fulanful Copper Prospect is located in close proximity to Berbera, which is situated in the region of Somaliland. The ore extracted from this prospect primarily comprises pyrite, galena, and chalcopyrite. The ore body itself is characterized as having a tabular shape, although the exact dimensions remain unknown. The mineralization present in this area dates back to the Pliocene epoch, spanning a period from approximately 5.33 to 2.58 million years ago. (Copper, Iron)
  • The Darreh Hos Prospect is located in Somaliland, specifically Somaliland. It was initially discovered in 1924 by Colonel Ashby. Currently, the Darreh Hos Prospect is not operational and there are no known intentions to reopen it. During its active period, it was classified as a small-scale production site. The mined ore at this location primarily consists of muscovite, beryl, and columbite. The ore body is described as having a tabular shape with its exact dimensions remaining unknown. The surrounding rock in the area is pegmatite, which was formed during the Neoproterozoic era around 1.00 to 0.54 billion years ago. (Beryllium)
  • The Dananjieh Lead Prospect is located near the city of Berbera in the province of Somaliland. It operates as an underground mine, with a single known shaft. The depth of the subsurface workings reaches a maximum of 18 meters (59 feet), spanning a length of 15 meters (49 feet). The ore extracted from this mine primarily consists of fluorite, barite, and galena. The ore body at the Dananjieh Lead Prospect is described as a tabular formation, stretching over 550 meters (1,804 feet) in length and possessing a thickness of 6 meters (19 feet). The host rock in this area is schist, which was formed during the Neoproterozoic era, approximately 1.00 to 0.54 billion years ago. (Barium-Barite)
  • The Dala Ad Occurrence, located in Somaliland, Somaliland, is known for its mineralization of ore. Although, the exact grade, tonnage, and extent of the mineralization have not been determined. As a result, there has been no production at this site, and only minimal activity is observed, mainly limited to routine claim maintenance. The ore composition primarily consists of chrysotile. (Asbestos)
  • The Infero Iron Occurrence is located in Somaliland. This occurrence has been identified as having ore mineralization. However, the exact grade, tonnage, and extent of the mineralization have not been determined. So far, there has been no production and minimal activity, with only routine claim maintenance being conducted since the discovery of mineralization. The ore found in this occurrence is primarily composed of magnetite and hematite, which are both significant sources of iron. The surrounding rock formation in this area is predominantly marble, a type of metamorphic rock. The geology and geography of the Infero Iron Occurrence contribute to its potential as a target for further exploration and potential development in the mining industry. (Iron)
  • The Theb Bismuth Occurrence is located in Somaliland, Somaliland. Ore mineralization has been identified in this area, the exact grade, tonnage, and extent of the mineralization remain uncertain. No mining operations have taken place thus far, with minimal activity primarily limited to the maintenance of mining claims following the discovery of the minerals. The mined ore consists of bismutite, beryl, and bismuthinite. The ore body is described as having a tabular shape, but its exact dimensions are unknown. The host rock in this region is schist, which dates back to the Neoproterozoic era around 1.00 to 0.54 billion years ago. (Beryllium)
  • The Wai Wai Occurrence, located in Somaliland, is known for the presence of ore mineralization. Although the exact grade, tonnage, and extent of the mineralization remain unknown. As of now, there has been no production and minimal activity except for regular claim maintenance following the discovery of these minerals. The ore extracted from this site consists of beryl and rhodonite. The ore body is described as tabular in shape; however, its dimensions are yet to be determined. The host rock in this region is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Beryllium)
  • The Dobo Niobium-Columbium Occurrence is located in Somaliland, Somaliland. Ore mineralization has been identified at this site, and the exact grade, tonnage, and extent of the mineralization remain uncertain. There has been no production to date, and aside from routine claim maintenance, there has been limited activity since the discovery of the minerals. The main minerals extracted from the ore are columbite and molybdenite. The ore body is described as having a tabular shape, but its dimensions are unknown. The host rock in this region is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Niobium-Columbium)
  • The Gedad Lead Occurrence is situated in Somaliland. At this location, ore mineralization has been identified. However, detailed information regarding the specific grade, tonnage, and extent of the mineralization is currently unknown. As of now, there has been no production from the site, and little to no activity has taken place apart from routine claim maintenance since the discovery of the mineral deposit. The ore found at the Gedad Lead Occurrence consists of galena and barite. The ore body is described as having a tabular shape, although the exact dimensions of the deposit remain uncertain. Due to the limited information available, further geological, geographic, and historical details about the Gedad Lead Occurrence within Somaliland are not provided. (Barium-Barite)
  • The Idiq Barium-Barite Occurrence is situated in Somaliland, Somaliland. Ore mineralization has been identified in this location. However, the precise grade, tonnage, and extent of the mineralization remain unknown. To date, there has been no production, and aside from routine claim maintenance, little to no activity has occurred since the discovery of the minerals. The mined ore primarily consists of galena and barite, with the waste material predominantly composed of quartz. The ore body is described as having a tabular shape, although its dimensions are yet to be determined. The host rock in the vicinity is Neoproterozoic sandstone, which formed approximately 1.00 to 0.54 billion years ago. (Barium-Barite)
  • The Magar Lead Occurrence is located in Somaliland, specifically in the Neoproterozoic era sedimentary rocks known as siltstone. This occurrence has shown evidence of ore mineralization, with the main minerals being barite and galena. Although the precise grade, tonnage, and extent of the mineralization are not yet known. Despite the discovery of mineralization, there has been no production at the Magar Lead Occurrence, and little to no activity has been observed apart from routine claim maintenance. The ore body is described as tabular-shaped, although its exact dimensions remain unknown. Geologically, the siltstone formation in this area was formed between 1.00 and 0.54 billion years ago during the Neoproterozoic era. These sedimentary rocks provide the geological setting for the occurrence of the mineralization. (Barium-Barite)
  • The Asaha Gotin Occurrence is located in Somaliland, Somaliland. The presence of ore mineralization has been confirmed at this site. However, important details regarding the precise grade, tonnage, and extent of the mineralization are currently unknown. Consequently, no mining production has taken place thus far, and there has been minimal activity at the site apart from routine claim maintenance since the discovery of the minerals. The rhodonite mineral is the primary constituent of the ore that would be extracted from this deposit, while the ore body itself has a lenticular or lens-shaped form of undetermined dimensions. The surrounding host rock in the area is composed of schist, which dates back to the Neoproterozoic era, specifically between 1.00 and 0.54 billion years ago. (Manganese)
  • The Hirmadleh Manganese Occurrence is located in Somaliland, Somaliland. It is an area where the presence of ore minerals has been identified, indicating the potential for manganese deposits. However, accurate information regarding its grade, tonnage, and extent is currently unknown. The mining activity in this location has been limited, with no production reported to date. Apart from routine claim maintenance, there has been little to no active exploration or development following the discovery of the mineralization. The primary ore mined at the Hirmadleh Manganese Occurrence is rhodonite, a manganese mineral. The ore body is characterized by a lenticular or lens-shaped form, although the exact dimensions of the deposit remain uncertain. Geologically, the host rock in this area is schist, which is dated back to the Neoproterozoic era that occurred between 1.00 to 0.54 billion years ago. This schist formation provides the necessary geological context for the occurrence of manganese deposits in this region. Overall, while the Hirmadleh Manganese Occurrence shows potential for manganese mineralization, further exploration and analysis are required to determine the exact size, grade, and economic viability of the deposit. (Manganese)
  • The Garba Rared Occurrence is located in Somaliland. Extensive exploration has identified ore mineralization at this site. The exact grade, tonnage, and extent of the mineralization have not been determined yet. As a result, no mining production has occurred, and there has been minimal activity at the site other than routine claim maintenance. The main ores present in this deposit are pyrite and magnetite. The geological formation in the area is predominantly gabbro, which serves as the host rock for mineralization. (Iron)
  • The Dibrawein Nickel Occurrence is located in Somaliland, specifically in the region of Somaliland. Exploration activities in this area have identified the presence of ore mineralization. However, the exact quality, quantity, and distribution of the mineralization remain uncertain. No mining operations have commenced, and there has been minimal activity apart from regular maintenance of claims following the initial discovery. The prevalent rock type in this region is gabbro, which is the host rock for the nickel mineralization. Additional geological, geographical, and historical information about this occurrence is currently unavailable. (Chromium)
  • The Barkasan Molybdenum Occurrence is situated in the region of Somaliland, which is located in Somaliland. Geological investigations have identified the presence of ore minerals at this site. Unfortunately, accurate information regarding the grade, tonnage, and extent of the mineralization is currently unavailable. As a result, no mining operations have commenced, and minimal activity has been observed, limited to routine maintenance of mining claims. The primary ore extracted from this occurrence is molybdenite, a mineral predominantly comprised of molybdenum sulfide. The ore deposit is described as having a tabular shape, although the specific dimensions are unknown at this time. (Molybdenum)
  • The Daarbuduq Asbestos Occurrence is located in Somaliland, Somaliland. Geological investigations have confirmed the presence of ore mineralization at this site, indicating a medium-sized deposit. However, detailed information regarding the grade, tonnage, and extent of the mineralization remains unknown. Despite the discovery of minerals, there has been no significant production or activity at this location apart from routine claim maintenance. The ore mined from this occurrence primarily consists of anthophyllite, a type of asbestos mineral. (Asbestos)
  • The Asilihe Tin Prospect is located in Somaliland, specifically in Somaliland. The valuable mineral extracted from this site is called cassiterite, which is the main ore of tin. The shape of the ore deposit at this location is described as tabular, stretching for approximately 120 meters (393 feet) in length and 6 meters (19 feet) in width. The surrounding geological formation in this region is predominantly composed of sandstone, and it belongs to the Neoproterozoic era, which occurred from 1.00 to 0.54 billion years ago. (Tin)
  • The Hamar Beryllium Occurrence is situated in Somaliland, Somaliland. The site has shown signs of ore mineralization. Unfortunately, the exact grade, tonnage, and extent of the mineralization have yet to be determined. As a result, no production has taken place, and there has been limited activity apart from standard claim upkeep since the discovery of the minerals. The ore extracted from this location is primarily composed of beryl, with waste material consisting mainly of graphite, spinel, and magnetite. The ore body itself is in the form of a tabular shape, but its dimensions are currently unknown. The host rock in this region is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Beryllium)
  • The Dobo Niobium-Columbium Occurrence is located in Somaliland, Somaliland. Ore mineralization has been identified in this area. However, the exact grade, tonnage, and extent of the mineralization have not been determined. As of now, there has been no production and only minimal activity, limited to routine claim maintenance, since the discovery of the minerals. The mined ore primarily consists of molybdenite and columbite. The ore body is described as having a tabular shape, with its dimensions remaining unknown. The host rock in this region is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Niobium-Columbium)
  • The Dalan Tin Prospect is located in Somaliland, Somaliland. It was initially discovered by J. E. G. W. Greenwood in the year 1955. As of the data entry period, the Dalan Tin Prospect had been closed and there were no known plans to reopen it. During its active period, the production size was relatively small. The primary mineral extracted from this site is cassiterite, which is a major source of tin. The ore body at this prospect is described as being tabular shaped, measuring approximately 100 meters (328 feet) in length and 2 meters (6 feet) in width. In terms of the geological context, the associated rock in the vicinity of the Dalan Tin Prospect is gabbro. Gabbro is a coarse-grained igneous rock that is formed from the cooling and solidification of magma deep within the Earth’s crust. The gabbro in this area is believed to have originated during the Neoproterozoic era, specifically between 1.00 to 0.54 billion years ago. (Tin)
  • The Elan Gubado Prospect is located in Somaliland, a country in northeastern Africa. The primary mineralization in this prospect consists of malachite and chalcopyrite. The ore deposit is characterized as tabular in shape, although its specific dimensions are currently unknown. In the vicinity of the prospect, the predominant rock type is granite, which formed during the Neoproterozoic era around 1.00 to 0.54 billion years ago. (Copper)
  • The Gal Hamud Occurrence is located near Berbera, Somaliland. Mineralization of ore has been identified at this site. Unfortunately, the precise grade, tonnage, and extent of the mineralization remain uncertain. As of now, there has been no active production at this site, with very limited or no activities apart from regular claim maintenance since the initial discovery of minerals. The primary ore extracted from this occurrence is chalcopyrite, a copper iron sulfide mineral. The ore body is described as tabular in shape, but its dimensions are yet to be determined. The surrounding rock in this area is composed of sandstone from the Upper Triassic epoch, which occurred approximately 237.00 to 201.30 million years ago. (Copper)
  • The Ido Faito Occurrence is located near Berbera, Somaliland. Geological investigations have identified the presence of ore mineralization at this site. Unfortunately, the exact grade, tonnage, and extent of the mineralization have not been determined. As of now, there has been no mining activity or production at the site, with the exception of routine claim maintenance. The primary ore mineral that has been identified is beryl. The shape of the ore body is described as tabular, but its dimensions remain unknown. (Beryllium)
  • The Hulul Lead Prospect is located in close proximity to Berbera, Somaliland. The ore extracted from this prospect consists of fluorite, galena, and barite. The ore deposit is characterized as having a tabular shape, with its exact dimensions yet to be determined. The surrounding rock in this region is primarily composed of granite that was formed during the Neoproterozoic era, approximately 1.00 to 0.54 billion years ago. (Barium-Barite)
  • The Sarar Awr Occurrence is a mineral deposit located in Somaliland, Somaliland. The exact grade, tonnage, and extent of the mineralization are currently unknown, but it is believed to be a large deposit. So far, no production has taken place at this site, and there has been minimal activity apart from routine claim maintenance since the mineral discovery. The ore extracted from this location consists predominantly of sand. The ore body has a blanket shape, but its dimensions are not yet determined. The host rock in the area is sandstone, which was formed during the Upper Cretaceous epoch between 100.50 and 66.00 million years ago. (Silica)
  • The Qodli Asbestos Occurrence is located in Somaliland. This site has shown signs of ore mineralization, indicating the presence of asbestos deposits. Although the estimated size of the deposit is considered to be small, the exact grade, tonnage, and extent of the mineralization remain uncertain. As a result, no production has taken place at this location, and there has been minimal activity apart from routine claim maintenance since the discovery of the minerals. The ore body at Qodli Asbestos Occurrence is described as having a tabular shape, but its dimensions are still unknown. The surrounding rock in this area is predominantly schist, a metamorphic rock typically associated with significant geological activity and mineral formation.(Asbestos)
  • The Teaq Tug Occurrence is located in Somaliland, Somaliland. Ore mineralization has been identified at this site. The exact grade, tonnage, and extent of the mineralization have not been determined yet. As a result, there has been no production and minimal activity, primarily limited to routine claim maintenance, since the discovery of minerals. The main ore mineral found in this area is beryl. The ore body is described as having a tabular shape, but its dimensions are currently unknown. The host rock in the region is gneiss, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago.(Beryllium)
  • The Las Gal Tug Occurrence is located in Somaliland, specifically in Somaliland. In this area, there have been findings of ore mineralization, although the exact grade, tonnage, and extent of the mineralization have not been determined. Currently, there has been no mining activity and only routine claim maintenance has taken place since the discovery of the minerals. The ore that can be extracted from this location consists mainly of beryl, with tourmaline being the primary waste material. The ore body has a tubular shape, but its dimensions are unknown at this time. The associated rock in this region is gabbro, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Beryllium)
  • The Mur Bakayale Mine is located in Somaliland, Somaliland. As of the time of data entry, the mine had ceased operations and there are no known plans for its reopening. The ore extracted from the mine consisted of allanite, muscovite, and ilmenite. The ore body itself is described as having a tabular shape, although its exact dimensions are unknown. The surrounding rock in the area is primarily composed of schist, formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Beryllium)
  • The B1yo Dader Occurrence is situated in the region of Somaliland, specifically within Somaliland. It has been identified as a site where ore mineralization has been observed. The exact grade, tonnage, and extent of the mineralization have not yet been determined. As a result, there has been no mining activity at this location aside from regular claim maintenance activities. The sand, predominantly composed of sandstone, serves as the primary ore mined from this area. The ore body assumes a blanket shape, but its dimensions remain uncertain. The host rock in the vicinity originates from the Upper Jurassic epoch, which occurred approximately 163.50 to 145.00 million years ago. (Silica)
  • The Rakdasafaka Gemstone Occurrence is situated in Somaliland, Somaliland. It is a location where ore mineralization has been identified. Unfortunately, the exact grade, tonnage, and extent of the mineralization are not currently known. As a result, there has been no production of minerals at this site, and apart from routine claim maintenance, there has been little to no activity since the initial discovery of the mineral deposit. The type of ore that can be extracted from the Rakdasafaka Gemstone Occurrence is spinel. This gemstone occurs naturally within the rocks present in this area. The surrounding host rock is composed of mafic metamorphic rock, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. It is worth noting that additional geological, geographic, and historical information regarding the Rakdasafaka Gemstone Occurrence may not be available due to the limited exploration and development activities carried out in this location. (Gemstone)
  • The Biyo Dader Occurrence is located in Somaliland. Mineralization of ore has been identified at this site. The exact grade, tonnage, and extent of the mineralization have not been determined. No production has taken place, and there has been limited activity aside from routine claim maintenance since the discovery of minerals in the area. The primary mineral mined at Biyo Dader is rutile. The ore body is described as having a tabular shape, although its dimensions are unknown. The host rock in this region is schist, dating back to the Neoproterozoic era, which occurred approximately 1.00 to 0.54 billion years ago. (Titanium Metal)
  • The Rakdasafaka Gemstone Occurrence is situated in Somaliland, Somaliland. It is a location where ore mineralization has been identified. Unfortunately, the exact grade, tonnage, and extent of the mineralization are not currently known. As a result, there has been no production of minerals at this site, and apart from routine claim maintenance, there has been little to no activity since the initial discovery of the mineral deposit. The type of ore that can be extracted from the Rakdasafaka Gemstone Occurrence is spinel. This gemstone occurs naturally within the rocks present in this area. The surrounding host rock is composed of mafic metamorphic rock, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. It is worth noting that additional geological, geographic, and historical information regarding the Rakdasafaka Gemstone Occurrence may not be available due to the limited exploration and development activities carried out in this location. (Gemstone)
  • The Waran-Weis Occurrence is located in Somaliland, Somaliland. It is an area where ore mineralization has been identified. Unfortunately, the exact grade, tonnage, and extent of the mineralization have not been determined yet. As a result, there has been no production of minerals from this occurrence, and little to no activity has taken place apart from routine claim maintenance since the initial discovery. The primary ore mineral found in this location is rutile, a titanium dioxide minera The ore body itself is described as tabular shaped, although the exact dimensions are unknown. The geological composition of the area consists of schist, which is a metamorphic rock formed during the Neoproterozoic era, specifically between 1.00 to 0.54 billion years ago. (Titanium Metal)
  • The Darkainle Niobium-Columbium Occurrence is situated in Somaliland. It is an area where ore mineralization has been identified. Unfortunately, specific details regarding the grade, tonnage, and extent of the mineralization remain unknown. To date, there has been no commercial production at this location, and little activity has occurred other than routine claim maintenance following the initial discovery of the minerals. The primary ore being mined is pyrochlore, a mineral rich in niobium and columbium. Geologically, the surrounding rock in this region is predominantly schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. This type of rock often exhibits a layered structure and is commonly associated with metamorphic processes. (Niobium-Columbium) URANIUM
  • The Ubali Manganese Occurrence is located in Somaliland, Somaliland. Ore mineralization has been discovered in this area. The exact grade, tonnage, and extent of the mineralization remain unknown. So far, there has been no production and very little activity, with routine claim maintenance being the only notable action since the initial mineral discovery. The ore that has been mined from this occurrence is primarily composed of rhodonite. Geologically, the host rock in the Ubali Manganese Occurrence area is schist. This schist belongs to the Neoproterozoic era, which spanned from 1.00 to 0.54 billion years ago. The formation of this rock dates back to that particular period in Earth’s history. (Manganese)
  • The Marodile Beryllium Occurrence is situated in Somaliland, a country in the Horn of Africa. Mining operations at this location have identified the presence of ore mineralization. Unfortunately, the exact grade, tonnage, and extent of the mineralization have not been determined yet. As a result, no production has taken place, and there has been minimal activity other than regular upkeep of mining claims since the initial discovery of the minerals. The ore extracted from the Marodile Beryllium Occurrence primarily consists of graphite and beryl. Geologically, the ore body is described as having a tabular shape, although its dimensions are unknown. The host rock in this region is schist, which formed during the Neoproterozoic era, approximately 1.00 to 0.54 billion years ago. This geological context provides insights into the formation and age of the mineral deposit in the area. (Beryllium)
  • The Ubali Beryllium Occurrence is located in Somaliland, Somaliland. Ore mineralization has been identified at this site. However, detailed information on the exact grade, tonnage, and extent of the mineralization is not currently available. As of now, there has been no production and minimal activity, aside from routine claim maintenance, following the discovery of these minerals. The mined ore primarily consists of beryl. The ore body at this occurrence is described as tabular in shape, although its specific dimensions are unknown. The host rock in the surrounding area is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Beryllium)
  • The Waran-Weis Occurrence is located in Somaliland, a country in the eastern part of Africa. The occurrence has revealed the presence of ore mineralization. However, detailed information regarding the precise grade, tonnage, and extent of the mineralization is currently unknown. Since the initial discovery of these minerals, there has been minimal activity in terms of production or exploration at the site. The only notable work carried out has been routine claim maintenance, indicating limited interest in developing the deposit further. The ore extracted from the Waran-Weis Occurrence consists mainly of columbite and beryl. The ore body itself is described as tabular in shape, but its exact dimensions have not been determined. The host rock in this area is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Beryllium)
  • The Hargeisa-Awareh Road Occurrence, located near Hargeysa, Somaliland, is a site where ore mineralization has been identified. While the deposit is estimated to be of medium size, the exact grade, tonnage, and extent of the mineralization remain unknown. To date, there has been no production at this location, and minimal activity beyond routine claim maintenance has occurred since the mineral discovery. The mined ore consists primarily of hematite, and the ore body exhibits a blanket shape, although its dimensions have not been determined. The host rock in this area is sandstone, formed during the Upper Cretaceous epoch approximately 100.50 to 66.00 million years ago. (Iron)
  • The Elk Iron Occurrence is located in Somaliland, Somaliland. It is a site where ore mineralization has been identified. The deposit is believed to have a medium size, although the specific grade, tonnage, and extent of the mineralization remain uncertain. So far, there has been no production at this location, and aside from routine claim maintenance, there has been little to no activity since the discovery of the mineral deposit. The mined ore at the Elk Iron Occurrence mainly consists of hematite, a mineral that is rich in iron. The ore body has a blanket shape and extends to a thickness of 39 meters (127 feet). The host rock in this area is primarily composed of sandstone, which formed during the Upper Cretaceous epoch approximately 100.50 to 66.00 million years ago. (Iron)
  • The Doboweina Iron Occurrence is located in Somaliland. Geological exploration in this area has identified the presence of ore mineralization, primarily hematite. However, the size and extent of the deposit are still uncertain. In terms of grade and tonnage, detailed information is currently lacking. Since the initial discovery of minerals, there has been limited activity at the Doboweina Iron Occurrence. Apart from routine claim maintenance, no production has taken place. The ore body itself has a formation resembling a blanket, measuring approximately 4 meters or 13 feet in thickness. This deposit is hosted within sandstone rocks, which were formed during the Upper Cretaceous epoch, specifically between 100.50 and 66.00 million years ago. (Iron)
  • The Arorigaben Iron Occurrence can be found in Somaliland, which is located in the Horn of Africa. Ore mineralization has been identified in this area, indicating the presence of a medium-sized deposit. However, detailed information regarding the precise grade, tonnage, and extent of the mineralization is currently unknown. As a result, no mining production has taken place at this site, and there has been minimal activity apart from regular claim maintenance following the mineral discovery. The ore extracted from this occurrence primarily consists of hematite, a significant iron ore mineral. The ore body itself has a broad, sheet-like morphology, with a thickness of approximately 30 meters (98 feet). (Iron)
  • The Qoton Dabo Occurrence is located in Somaliland. This site has shown evidence of ore mineralization, indicating the presence of economically valuable minerals. The size of the deposit is estimated to be of medium scale, but the exact grade, tonnage, and extent of the mineralization have not been determined. Consequently, no mining production has taken place at this location, with only minimal activity being conducted for routine claim maintenance since the initial discovery of the mineral deposit. The ore found at Qoton Dabo is primarily composed of hematite, a mineral with high iron content. The ore body itself has a blanket-like shape, extending approximately 34 meters (111 feet) in thickness. The host rock in this area is sandstone, formed during the Upper Cretaceous epoch, which occurred between 100.50 and 66.00 million years ago. (Iron)
  • The Dagahh Kuled Prospect is located in Somaliland, specifically in the region of Somaliland. The primary mineral extracted from this mining site is rutile. The ore deposit is characterized as having a tabular shape, although its exact dimensions are currently unknown. The prevailing rock type in this region is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Titanium Metal)
  • The Salawel Manganese Prospect is located in Somaliland. This area is characterized by the presence of schist, a metamorphic rock formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. The schist serves as the host rock for the manganese deposits at Salawel, indicating that the manganese mineralization occurred during this ancient geological period. (Manganese)
  • The Darkainle Molybdenum Prospect is located in Somaliland. The ore extracted from this prospect consists of pyrochlore, molybdenite, and chalcopyrite. The ore body is characterized as tabular in shape, measuring approximately 25.00 meters (82.02 feet) in length and 0.02 meters (0.07 feet) in width. The surrounding rock formation in this region is identified as nepheline syenite. (Molybdenum)
  • The Daba Shabeli Occurrence is situated in Somaliland. This region has shown indications of mineralization, particularly of ore minerals. Detailed information regarding the grade, tonnage, and extent of the mineralization is currently unavailable. As a result, no actual mining operations have taken place, and there has been minimal activity apart from regular claim maintenance since the initial discovery of the minerals. The ore present at this occurrence primarily consists of magnetite and chromite. These minerals are commonly found in ultramafic intrusive rocks, which serve as the host rock in this particular area. Ultramafic rocks are rich in iron and magnesium, and commonly contain minerals such as olivine, pyroxene, and amphibole. The presence of magnetite and chromite suggests the potential for iron and chromium resources in the Daba Shabeli Occurrence. However, further exploration and geological studies are required to ascertain the economic feasibility and potential of the deposit. Currently, the knowledge and understanding of this mineral occurrence are limited, and future assessments may provide more insights into the geological, geographical, and historical significance of this site in the mining industry. (Iron)
  • The Bustanka Lead Prospect is located in close proximity to Berbera, Somaliland. The primary minerals extracted from the ore deposits at this prospect include fluorite, barite, and galena. The specific dimensions of the tabular-shaped ore body remain uncertain. The host rock in this region is mainly comprised of migmatite, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Barium-Barite)
  • The Bihen Gaha Prospect is located in Somaliland. The ore body in this area is described as having an irregular shape with unknown dimensions. The host rock surrounding the ore body is limestone, which was formed during the Eocene epoch, approximately 56.00 to 33.90 million years ago. (Manganese)
  • The Maag Barium Prospect is located in Somaliland, a region in the Horn of Africa. The mining operation at this prospect focuses on extracting galena and barite ores. These ores are found within a tabular-shaped ore body, the exact dimensions of which are currently unknown. The surrounding rock formation in this area is schist, which dates back to the Neoproterozoic era, specifically between 1.00 and 0.54 billion years ago. This geological information provides insights into the composition and age of the rocks and minerals present at the Maag Barium Prospect. (Barium- Barite)
  • The Qabri Bahir Beryllium Occurrence is located in Somaliland, Somaliland. It is an area where ore mineralization has been identified. Although the exact grade, tonnage, and extent of the mineralization are yet to be determined. Currently, there has been no production activity in this area, with very limited activity limited only to routine claim maintenance. The ore minerals that have been discovered at this site are columbite and beryl. The ore body is described as having a tabular shape, but the specific dimensions are unknown. The rocks surrounding the deposit are primarily gneiss, which formed during the Neoproterozoic era, approximately 1.00 to 0.54 billion years ago. (Beryllium)
  • The Hammas Tin Prospect is located in Somaliland, a country in East Africa. The main minerals extracted from this prospect are quartz and cassiterite. The deposit has a tabular shape, measuring approximately 40 meters (131 feet) in length and 30 meters (98 feet) in thickness. The surrounding rock formation in this area is gneiss, which was formed during the Neoproterozoic era around 1.00 to 0.54 billion years ago. (Quartz)
  • The Buhl Bismuth Prospect is located in Somaliland, which is a region in Somaliland. The primary minerals being extracted from this prospect are chalcopyrite, bismuthinite, and garnet. The ore deposit itself takes on a lenticular or lens-shaped form, stretching for approximately 150 meters (492 feet) in length and 15 meters (49 feet) in width. The surrounding geological formation in this area is predominantly composed of granite. (Bismuth)
  • The Dobo Well Occurrence is located in Somaliland, specifically in the country of Somaliland. Geological exploration at this site has revealed the presence of ore mineralization. Unfortunately, detailed information regarding the grade, tonnage, and extent of the mineralization is currently unknown. As a result, there has been no production and minimal activity apart from regular claim maintenance since the initial discovery of the minerals. The mined ore primarily consists of molybdenite, a mineral that is a significant source of molybdenum. The ore body is described as tabular-shaped, but its exact dimensions are yet to be determined. The surrounding rock in the Dobo Well area is composed of gneiss, a metamorphic rock formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Molybdenum)
  • The Unkah Silver Prospect is located in Somaliland, Somaliland. The ore body at this prospect is characterized as having a tabular shape and has a thickness of 0.46 meters (1.51 feet). The host rock in the area consists of slate, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Barium-Barite)
  • The Karajiv Lead Occurrence is located in Somaliland. Geologically, this occurrence is notable for its ore mineralization, particularly the presence of galena and barite. Although the precise grade, tonnage, and extent of the mineralization are yet to be determined. To date, no production has taken place at this site, with little to no activity observed apart from routine claim maintenance. The ore body itself is described as tabular in shape, although its exact dimensions remain unknown. The waste material associated with mining operations primarily consists of quartz. (Barium-Barite)
  • The Karin Kul Occurrence is located in Somaliland, Somaliland. This site has shown evidence of ore mineralization. Unfortunately, the specific grade, tonnage, and extent of the mineralization have not been determined yet. As a result, there has been no production at this location, and very minimal activity has taken place beyond regular claim maintenance since the discovery of the minerals. The ores that have been discovered consist of galena and barite. The ore body is described as having a tabular shape, but the exact dimensions are currently unknown. (Barium-Barite)
  • The Mokhor Holeh Occurrence, located in Somaliland, Somaliland, is known for the presence of ore mineralization. There is currently limited knowledge about the precise grade, tonnage, and extent of the mineralization. As of now, no production has taken place and minimal activity, apart from routine claim maintenance, has been observed since the discovery of the minerals. The dominant ore minerals present at this occurrence are barite and galena, while quartz constitutes the majority of the waste material. The ore body is described as having a tabular shape, but its dimensions remain unknown. The host rock in this area is mudstone, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Barium-Barite)
  • The Veliya Tug Occurrence is located in Somaliland, specifically in the region of Somaliland. Mineralization of ore has been identified in this area. Unfortunately, the exact grade, tonnage, and extent of the mineralization have yet to be determined. Since the initial discovery of minerals, there has been no mining production and minimal activity, mainly limited to routine claim maintenance. The mined ore at Veliya Tug consists mainly of galena and barite. It is noteworthy that the shape of the ore body is described as tabular, although its dimensions are currently unknown. The host rock in this region is composed of limestone, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Barium-Barite)
  • The Luqunlo Ad Occurrence is located in Somaliland, specifically in the region of Somaliland. It is known to contain ore mineralization. Detailed information regarding the grade, tonnage, and extent of the mineralization is not available at this time. Since the discovery of the mineral deposit, there has been no production and very little activity apart from routine claim maintenance at the site. The ore body is described as having a tabular shape, but its exact dimensions are unknown. In terms of geology, the host rock in the area is granite, which was formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. This provides some insights into the geological context of the Luqunlo Ad Occurrence. (Manganese)
  • The Manja Asseh Occurrence is situated near the city of Berbera in Somaliland. Geological investigations at this site have identified the presence of ore minerals. Unfortunately, the precise grade, tonnage, and extent of the mineralization remain uncertain. Consequently, no mining operations have been conducted, and there has been minimal activity at the site, limited only to routine claim maintenance. The ore extracted from the Manja Asseh Occurrence primarily consists of a mineral called rhodonite. The ore body itself takes the form of a lens or lenticular shape, with its dimensions yet to be determined. The predominant rock type in this area is schist, which formed during the Neoproterozoic era approximately 1.00 to 0.54 billion years ago. (Manganese)
  • The Lalis Manganese Occurrence, located in Somaliland, Somaliland, is a deposit where ore mineralization has been identified, although the precise grade, tonnage, and extent of the mineralization remain uncertain. As of now, no mining activities have taken place at this site, and only routine claim maintenance has been conducted since the discovery of the minerals. The primary ore mined at the occurrence is rhodonite. The ore body has a lenticular or lens-shaped form, but its exact dimensions are unknown. The area is predominantly composed of schist, a type of metamorphic rock formed during the Neoproterozoic era, which occurred approximately 1.00 to 0.54 billion years ago. (Manganese)
  • The Marso Manganese Occurrence, located in Somaliland, Somaliland, is a site where ore mineralization has been discovered. Although the exact grade, tonnage, and extent of the mineralization have not been determined. Thus far, there has been no production and little to no activity, aside from routine claim maintenance, following the mineral discovery. The primary ore mined at this occurrence is rhodonite, a manganese silicate mineral. The ore body itself has a lenticular or lens-shaped form, but the dimensions of the deposit are currently unknown. The surrounding host rock is schist, which originated during the Neoproterozoic era, specifically around 1.00 to 0.54 billion years ago. (Manganese)
  • The Daimoleh Wein Occurrence is situated in close proximity to Berbera, Somaliland. Geological investigations have identified the presence of ore mineralization at this site. Unfortunately, the exact grade, tonnage, and extent of the mineralization have not been determined yet. As a result, no production has taken place in this area and there has been minimal activity, limited to routine claim maintenance, following the initial mineral discovery. The ore extracted from this occurrence primarily consists of rhodonite, a manganese inosilicate mineral. The mineralization at Daimoleh Wein dates back to the Neoproterozoic era, which occurred roughly between 1.00 and 0.54 billion years ago. (Iron)
  • The Didin Iron Occurrence is situated near Berbera, in the region of Somaliland. Geologists have discovered ore mineralization in this location. Unfortunately, the exact grade, tonnage, and extent of the mineralization are not currently known. As a result, there has been no mining activity or production taking place at this site, aside from routine claim maintenance. The ore that could potentially be mined from this occurrence consists primarily of magnetite, which is a valuable iron ore mineral. The waste material associated with this deposit is mainly composed of apatite, a phosphate mineral. In terms of geological history, the rocks in the Didin Iron Occurrence area are classified as gabbro. These rocks were formed during the Neoproterozoic era, which occurred approximately 1.00 to 0.54 billion years ago. Gabbro is a type of igneous rock that forms from the slow cooling of magma beneath the Earth’s surface. Overall, while the Didin Iron Occurrence shows potential for iron ore mining, further exploration and assessment are required to determine the precise characteristics and economic viability of the deposit. (Iron)
  • The Hul Qabobe Occurrence is situated in Somaliland, a region in the Horn of Africa. Mineralization of ore has been identified at this specific location. Unfortunately, the accurate information regarding the precise grade, tonnage, and extent of the mineralization is currently unknown. As a result, no production has taken place, and there has been limited to no activity in the area apart from routine claim maintenance since the discovery of the minerals. The ore extracted from the Hul Qabobe Occurrence primarily consists of magnetite, with the waste material consisting predominantly of apatite. The ore body itself is disseminated in nature, but the precise dimensions are yet to be determined. The host rock in this particular region is composed of amphibole schist, a metamorphic rock formed under high pressure and temperature conditions. (Iron)
  • The Ardahh Barium Prospect is located in close proximity to Berbera, Somaliland. Mining operations at this site primarily focus on the extraction of barite, galena, and fluorite ores. The ore body at the prospect is considered to have a tabular shape, with its dimensions being currently unknown. In terms of geological context, the prevailing rock formation in the area is sandstone, which formed during the Upper Triassic epoch (roughly 237.00 to 201.30 million years ago) until the Upper Jurassic epoch (approximately 163.50 to 145.00 million years ago). (Barium-Barite)

Titanium Occurrence in Somaliland, Republic of Somaliland. Ore mineralization has been found at 2 regions many location and the size of the deposit is estimated to vary, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of rutile. The ore body is described as tabular shaped of unknown dimensions. The host rock in this area is schist from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location Gabiley region 2 mines & 1 mine Sanaag

Silica: Occurrence is in Somaliland, Republic of Somaliland. Ore mineralization has been found at two regions location and the size of the deposit is estimated to be large, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of sand. The ore body takes a blanket shape of unknown dimensions. The host rock in this area is sandstone from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. Location Gabiley & Sarar region. Silica also is used in grinding and polishing glass and stone; in foundry molds; in the manufacture of glass, ceramics, silicon carbide, ferrosilicon, and silicones; as a refractory material; and as gemstones. Silica gel is often used as a desiccant to remove moisture. 4 major uses for silicon in technology Electronics: 1.High-purity silicon is created by thermally decomposing the ultra-pure trichlorosilane. Silicone. 2.Silicon is used to create silicone, which chemically are silicon-oxygen polymers with methyl groups attached. 3.Solar panels. 4.High power lasers.

Gemstone Occurrence is in Somaliland, Republic of Somaliland. Ore mineralization has been found at this location and the size of the deposit is estimated to be small, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of spinel. The host rock in this area is mafic metamorphic rock from the Neoproterozoic era 1.00 to 0.54 billion years ago. Gabiley region

Chromium: The Nickel Occurrence is in Somaliland, Somaliland. Ore mineralization has been found at this location, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The host rock in this area is gabbro. Location Awdal. The 80/20 nickel chromium alloy is often used for wrought and cast parts for high temperature applications, as it has better oxidation and hot corrosion resistance compared to cheaper iron-nickel-chromium alloys. This nickel chromium alloy is highly suited to applications that are subject to oxidation. Nickel–chromium alloys are mainly used in the form of wires for electrical heating and for making heat resistant parts in situations where mechanical considerations are low.

Molybdenum Occurrence is in Somaliland, Somaliland. Ore mineralization has been found at this location and the size of the deposit is estimated to vary, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of molybdenite. The ore body is described as tabular shaped of unknown dimensions. The host rock in this area is gneiss from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location 2 mines Awdal. Most molybdenum is used to make alloys. It is used in steel alloys to increase strength, hardness, electrical conductivity and resistance to corrosion and wear. These ‘moly steel’ alloys are used in parts of engines. Other alloys are used in heating elements, drills and saw blades.

The Niobium-Columbium Occurrence is in Somaliland, Republic of Somaliland. Ore mineralization has been found at this location and the size of the deposit is estimated to be small, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of pyrochlore. The host rock in this area is schist from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location 2 mines Awdal. Niobium is used in various superconducting materials. These superconducting alloys, also containing titanium and tin, are widely used in the superconducting magnets of MRI scanners. Other applications of niobium include welding, nuclear industries, electronics, optics, numismatics, and jewellery. Niobium is used in arc-welding rods for stabilized grades of stainless steel. It is also used in advanced airframe systems. Superconductive magnets are made with Nb-Zr wire, which retains superconductivity in strong magnetic fields. Niobium is used in lamp filaments.

The Copper Prospect is near Berbera, Somaliland. The ore mined is composed of pyrite, galena and chalcopyrite. The ore body is described as tabular shaped of unknown dimensions. The mineralization at this location is from the Pliocene epoch 5.33 to 2.58 million years ago. Location 4 mines Sahil region. Most copper is used in electrical equipment such as wiring and motors. This is because it conducts both heat and electricity very well, and can be drawn into wires. It also has uses in construction (for example roofing and plumbing), and industrial machinery (such as heat exchangers).

The Barium-Barite Lead Prospect is near Berbera, Somaliland. Mine operations consist of underground workings. There is one known shaft. Subsurface depth reaches a maximum of 18 meters (59 feet) and extends 15 meters (49 feet) in length. The ore mined is composed of fluorite, barite and galena. The ore body is described as tabular shaped 550 meters (1,804 feet) long and 6 meters (19 feet) thick. The host rock in this area is schist from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location 2 mines Sahil region & 4 mines Sanaag & Awdal. Barite is the primary ore of barium, which is used to make a wide variety of barium compounds. Some of these are used for x-ray shielding. Barite has the ability to block x-ray and gamma-ray emissions. Barite is used to make high-density concrete to block x-ray emissions in hospitals, power plants, and laboratories.

The Quartz Tin Prospect is in Somaliland, Somaliland. The ore mined is composed of quartz and cassiterite. The ore body is described as tabular shaped 40 meters (131 feet) long and 30 meters (98 feet) thick. The host rock in this area is gneiss from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location Sahil region. Cassiterite is an economically important mineral, being the primary ore of the metal tin. It is also used as a collectors mineral with the transparent forms being highly desired. Cassiterite is occasionally used as a minor gemstone, being faceted mostly for collectors. Quartz is an important mineral with numerous uses. Sand, which is composed of tiny Quartz pebbles, is the primary ingredient for the manufacture of glass. Transparent Rock Crystal has many electronic uses; it is used as oscillators in radios, watches, and pressure gauges, and in the study of optics.

The Bismuth Prospect is in Somaliland, Somaliland. The ore mined is composed of chalcopyrite, bismuthinite and garnet. The ore body has a lenticular or lens shaped form extending 150 meters (492 feet) long and 15 meters (49 feet) wide. Associated rock in this area is granite. Location of Mine Salel region & Gabiley region. Industrial and military uses of bismuth: Bismuth compounds are used as catalysts in the manufacturing process of synthetic fiber and rubber. When bismuth is combined with other metals such as lead, tin, iron and cadmium, it forms alloys with low melting points that can be used in fire detectors and extinguishers.

Manganese: The Asaha Gotin Occurrence is in Somaliland, Somaliland. Ore mineralization has been found at this location and the size of the deposit is estimated to be small, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of rhodonite. The ore body has a lenticular or lens shaped form of unknown dimensions. The host rock in this area is schist from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location mine Togdheer & 7 mines Sahil region & Gabiley. Manganese is often used by the steel industry in deoxidizing and desulfurizing additives and as an alloying constituent. It can improve the rolling and forging qualities, as well as the strength, toughness, stiffness, hardness, wear resistance, and hardenability of steels.

The Iron Occurrence is in Somaliland, Republic of Somaliland. Ore mineralization has been found at divers regions of Somaliland and the size of the deposit is estimated to be extreme large, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of hematite. The ore body takes a blanket shape extending 39 meters (127 feet) thick. The host rock in this area is sandstone from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. Location mine Togdheer region & 5 mines Sahil region & Sanaag & Hargeisa & 2 mines Odweyne. It is used to manufacture steel and also used in civil engineering like reinforced concrete, girders etc. Iron is used to make alloy steels like carbon steels with additives such as nickel, chromium, vanadium, tungsten, and manganese. Iron ore and steel industry is one of the basic industries of the country and plays an important role in strengthening the economy. 

The Garnet Prospect is in Somaliland, Somaliland. The ore mined is composed of kyanite, garnet and rhodonite. The ore body has a lenticular or lens shaped form 3.00 meters (9.84 feet) long and 3.00 meters (9.84 feet) thick. The host rock in this area is schist from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location North Sheikh (Sahil region). They are used in waterjet cutting, “sand” blasting, sandpaper, water filtration, and a number of other uses. Almandine is the hardest garnet and also the most abundant.

The Beryllium Prospect is in Somaliland, Somaliland. The site was first discovered in 1924 by Colonel Ashby. The Production size when active was considered to vary. The ore mined is composed of muscovite, beryl and columbite. The ore body is described as tabular shaped of unknown dimensions. The host rock in this area is pegmatite from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location 5 mines ( Sahil region) & 3 mines of Awdal region & 4 mines Gabiley. Beryllium is a silvery-white metal. It is relatively soft and has a low density. Beryllium is used in alloys with copper or nickel to make gyroscopes, springs, electrical contacts, spot-welding electrodes and non-sparking tools. Mixing beryllium with these metals increases their electrical and thermal conductivity. Other beryllium alloys are used in high-speed aircrafts and missiles, as well as spacecraft and communication satellites.

The Lead Prospect is near Berbera, Somaliland. The ore mined is composed of fluorite, barite and galena. The ore body is described as tabular shaped of unknown dimensions. The host rock in this area is migmatite from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location Berbera district. Lead is still widely used for car batteries, pigments, ammunition, cable sheathing, weights for lifting, weight belts for diving, lead crystal glass, radiation protection and in some solders.

The Tin Prospect is in Somaliland, Somaliland. The ore mined is composed of cassiterite. The ore body is described as tabular shaped 120 meters (393 feet) long and 6 meters (19 feet) wide. The host rock in this area is sandstone from the Neoproterozoic era 1.00 to 0.54 billion years ago. Location 2 mines (Sanaag). Tin has many uses. It takes a high polish and is used to coat other metals to prevent corrosion, such as in tin cans, which are made of tin-coated steel. Alloys of tin are important, such as soft solder, pewter, bronze and phosphor bronze. A niobium-tin alloy is used for superconducting magnets.

The Molybdenum Occurrence is in Somaliland, Republic of Somaliland. Ore mineralization has been found at this location and the size of the deposit is estimated to be small, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of molybdenite. The ore body is described as tabular shaped of unknown dimensions. Location North Madheera (Sahil region). Most molybdenum is used to make alloys. It is used in steel alloys to increase strength, hardness, electrical conductivity and resistance to corrosion and wear. These ‘moly steel’ alloys are used in parts of engines. Other alloys are used in heating elements, drills and saw blades. Molybdenum compounds are usually used in the chemical industry as catalysts and lubricants. For example, molybdenum sulfide is employed as a catalyst to eliminate sulfur in the refining of petroleum, and it is also a useful lubricant, especially at high temperatures where oils would decompose.

Somaliland’s Exploration Attempt

The Republic of Somaliland is very ambitious and optimistic to extract its natural resources as oil and gas and this is justifiable whilst Somaliland pursues a de facto state, which is peaceful, and democratic that managed its internal frictions of the post- conflict era. However, it is worth mention that Somaliland still is struggling state institutional reforms, holding timely elections and effective implementation rule of law. Since Somaliland regained its independence in 1991 from the Somali Republic which was collapsed in 1991. The state to attain the social and economic needs was indispensable strategy and national priority. From this perspective, the successive governments of Somaliland efforts hampered by combating poverty reduction, poor socio-economic conditions and improving infrastructure as ports, airports, roads and other government sectors such as education, health, agriculture, energy, tourism and water development. Moreover, Somaliland was attempting to undertake the oil and gas explorations since 2006 Many Somalilanders are confident that this is the only way that the poverty and socio-economic vulnerability can be alleviated.

Despite its economic and political ambition Somaliland has little experiences in this sector of the extractive economy and managing such highly sophisticated projects of the hydrocarbon extraction and production. Somaliland is very hopeful to discover oil and gas resources as indications prove because before the seismic activities started, Somaliland had some encouraging signs of preliminary geological data and this is a very vital project to overcome some poor livelihood conditions. Finally, many Somalilanders argue that the political and economic aspirations of the country may not constrain the underlying factors such as lack of comprehensive regulatory framework, lack of transparent and accountability and misuse of land resources. Nevertheless, improving social infrastructure, economic infrastructure and livelihood of the people can lead a better outcome of Somaliland’s hydrocarbon production and sustainable development. From a regional perspective, the geology of Somaliland shows many similarities with Yemen and the exploration has focused on searching for Jurassic rifts where source-rocks have accumulated.

Furthermore, it is apparent that Somaliland’s ambitious goals to accomplish marketable oil and gas deposits should be required legal and regulatory framework that administer the sector. Right now there is strong public and international demand of legal instrument. According to the Minister of Energy and Minerals, Somaliland is “developing a new modern regulatory framework to guide the sector before anything gets out of the ground”. Somaliland had to call on international expertise to draft a hydrocarbon law and to provide support in Production sharing agreement PSA negotiations.

There is a heated debate about how Somaliland can produce its natural resources and how this is domestically agreeable in order to respond the extreme poverty, poor infrastructure and the high rates of unemployment, the exploitation of resources could have significant benefits for local communities in the form of employment opportunities, infra-structure development, and citizen participation in decision-making and better institution-building.

                                                                           Somaliland Blocks map