Amethyst is the purple variety of the quartz mineral species. It's the gem that's most commonly associated with the color purple, even though there are other purple gems such as sapphire and tanzanite<a href="https://www.chordiajewels.com/categories/amethyst"amethyst</a>
Amethyst is a variety of quartz that is purple in color. It is commonly used in jewelry such as rings, bracelets, necklaces and earrings. The document provides background on amethyst, including that it can be found in many parts of the world like Brazil, Sri Lanka and the United States. Additional facts mentioned are that the name amethyst comes from Greek and it was once believed to protect people.
Andesite is an extrusive igneous rock of intermediate composition typically dominated by plagioclase feldspar with pyroxene and/or hornblende. It forms from the mixing of basaltic and crustal magmas in continental margins above subduction zones. Andesites are the most abundant volcanic rocks in island arcs, occurring in belts above Benioff zones. They have been used historically as ornamental stone for buildings.
This document introduces gemmology, the science of natural and artificial gemstones. It discusses what qualifies something as a gemstone, noting that gemstones must be beautiful, durable, and rare enough for personal adornment. The document then explains several methods used to identify unknown gemstones, including measuring the refractive index, specific gravity, and using spectroscopy to analyze light absorption. In conclusion, it encourages learning more about identifying gemstones.
Glacial drift is material deposited by glaciers and can be categorized as either direct deposition till or indirect deposition. Direct deposition till includes lodgement and ablation tills deposited at the base of the glacier. Indirect deposition includes fluvialglacial deposits transported by water and ice-contact stratified drift deposited near melting ice. Drumlins are elongated hills of glacial debris streamlined into mounds, often found in clusters, and formed through various processes including lodgement of debris and reworking by moving ice. Moraines mark the extent and retreat of glaciers and include lateral, medial, terminal, and recessional moraines. Erratics are rocks transported from their place of origin by glacial
Gemology is the scientific study of gemstones, including their identification and evaluation. Key physical properties used to identify gems include cleavage, fracture, hardness according to Mohs scale, toughness, stability, effects of dehydration, sensitivity to light, and specific gravity. Gemstones can be natural minerals, organic materials produced by living things, or certain types of natural glass. Physical properties provide important clues to determining a gem's identity and suitability for various applications.
Kyanite, andalusite, and sillimanite are polymorphs that have the chemical formula Al2SiO5 but different crystal structures. Kyanite forms at high pressures, andalusite at low pressures, and sillimanite at high temperatures. They are commonly found in metamorphic rocks and have various industrial uses, especially as refractory materials. The document provides details on the crystal structures, physical properties, typical locations, and applications of these aluminosilicate minerals.
amphibole asbestos, application of asbestos, applications of asbestos fibres, asbestos grades, mining of asbestos, most common types of asbestos asbestos fibrous min, osha’s asbestos standard, properties of asbestos cement products, properties of asbestos fibres asbestos deposits in, quality control, resources type of asbestos, separating of asbestos, serpentine asbestos (or chrysotile asbestos), the manufacturing process of asbestos, types of egyptian asbestos deposits, typical asbestos types in structures, uses of asbestos, where asbestos is found type of asbestos, world asbestos production, world asbestos production by type
There are two main forms of igneous rocks:
1) Extrusive rocks form from lava erupted at the Earth's surface and cool rapidly. They include lava flows, pyroclastic deposits like volcanic ash and tuff.
2) Intrusive rocks form from magma that cools below the surface. They can be concordant, forming sheets and domes parallel to layers, like sills and laccoliths, or discordant and cutting across layers, like dikes, batholiths, and volcanic necks.
Amethyst is a variety of quartz that is purple in color. It is commonly used in jewelry such as rings, bracelets, necklaces and earrings. The document provides background on amethyst, including that it can be found in many parts of the world like Brazil, Sri Lanka and the United States. Additional facts mentioned are that the name amethyst comes from Greek and it was once believed to protect people.
Andesite is an extrusive igneous rock of intermediate composition typically dominated by plagioclase feldspar with pyroxene and/or hornblende. It forms from the mixing of basaltic and crustal magmas in continental margins above subduction zones. Andesites are the most abundant volcanic rocks in island arcs, occurring in belts above Benioff zones. They have been used historically as ornamental stone for buildings.
This document introduces gemmology, the science of natural and artificial gemstones. It discusses what qualifies something as a gemstone, noting that gemstones must be beautiful, durable, and rare enough for personal adornment. The document then explains several methods used to identify unknown gemstones, including measuring the refractive index, specific gravity, and using spectroscopy to analyze light absorption. In conclusion, it encourages learning more about identifying gemstones.
Glacial drift is material deposited by glaciers and can be categorized as either direct deposition till or indirect deposition. Direct deposition till includes lodgement and ablation tills deposited at the base of the glacier. Indirect deposition includes fluvialglacial deposits transported by water and ice-contact stratified drift deposited near melting ice. Drumlins are elongated hills of glacial debris streamlined into mounds, often found in clusters, and formed through various processes including lodgement of debris and reworking by moving ice. Moraines mark the extent and retreat of glaciers and include lateral, medial, terminal, and recessional moraines. Erratics are rocks transported from their place of origin by glacial
Gemology is the scientific study of gemstones, including their identification and evaluation. Key physical properties used to identify gems include cleavage, fracture, hardness according to Mohs scale, toughness, stability, effects of dehydration, sensitivity to light, and specific gravity. Gemstones can be natural minerals, organic materials produced by living things, or certain types of natural glass. Physical properties provide important clues to determining a gem's identity and suitability for various applications.
Kyanite, andalusite, and sillimanite are polymorphs that have the chemical formula Al2SiO5 but different crystal structures. Kyanite forms at high pressures, andalusite at low pressures, and sillimanite at high temperatures. They are commonly found in metamorphic rocks and have various industrial uses, especially as refractory materials. The document provides details on the crystal structures, physical properties, typical locations, and applications of these aluminosilicate minerals.
amphibole asbestos, application of asbestos, applications of asbestos fibres, asbestos grades, mining of asbestos, most common types of asbestos asbestos fibrous min, osha’s asbestos standard, properties of asbestos cement products, properties of asbestos fibres asbestos deposits in, quality control, resources type of asbestos, separating of asbestos, serpentine asbestos (or chrysotile asbestos), the manufacturing process of asbestos, types of egyptian asbestos deposits, typical asbestos types in structures, uses of asbestos, where asbestos is found type of asbestos, world asbestos production, world asbestos production by type
There are two main forms of igneous rocks:
1) Extrusive rocks form from lava erupted at the Earth's surface and cool rapidly. They include lava flows, pyroclastic deposits like volcanic ash and tuff.
2) Intrusive rocks form from magma that cools below the surface. They can be concordant, forming sheets and domes parallel to layers, like sills and laccoliths, or discordant and cutting across layers, like dikes, batholiths, and volcanic necks.
Gems are expensive mineral stones that provide links between various scientific fields. There are about 150 natural gem compounds. Diamonds, emeralds, rubies, and sapphires sell at the highest prices due to their beauty, rarity, traditions, and perceptions of permanence. Gems have characteristics like color, refractive index, dispersion, absorption, and facets that make them attractive. Their properties like hardness, chemical stability, and double refraction also provide practical applications beyond decoration. Many gems like quartz, topaz, and tourmaline are studied scientifically or believed to have healing properties according to traditions.
This document discusses processing sand and silica sand into other materials. It begins by outlining examples of mineral processing including sand, silica sand, and heavy mineral sand. For processing sand and silica sand, it describes extracting, washing, classifying, and removing impurities from the sand through steps like screening, attrition scrubbing, hydrocyclones, and magnetic separation. The sand can then be further processed into silicon, silicon carbide, and silicone through reducing silica to ferrosilicon, purifying it through distillation of trichlorosilane, and using the Siemens process to deposit high purity silicon. Heavy mineral sands can also be separated into minerals like zircon, rut
This document discusses sedimentary structures, which are macroscopic features formed during sediment deposition. It classifies sedimentary structures based on their morphology and formation processes. The key types discussed are physical structures like bedding, cross-bedding, and ripple marks formed directly by sedimentation. Chemical structures like nodules and concretions are formed by precipitation. Biogenic structures such as stromatolites and trace fossils provide evidence of ancient life. Studying sedimentary structures can provide insight into depositional environments, paleocurrents, and stratigraphic relationships.
This document provides an overview of calcareous microfossils, specifically focusing on foraminifera. It defines foraminifera as single-celled organisms with shells composed of calcite or aragonite. Their shells are made of one or multiple chambers. Foraminifera morphology and mineralogy form the basis for identification and classification. They first appeared in the Cambrian period and have been important for paleoclimate reconstruction, paleoceanography studies, archaeology, biostratigraphy, and oil exploration.
This document provides an overview of gemstones, including their physical and optical properties, shapes and cuts, and synthetics and simulants. It discusses the key properties used to identify gemstones such as crystal habit, specific gravity, hardness, refractive index, and luminescence. Different cutting styles including cabochon and faceted cuts are described. The document also covers synthetic gemstones which mimic natural stones, and simulants which have similar appearances but different properties. It aims to equip gemologists with the knowledge to distinguish natural gems from synthetics or enhanced stones.
The document discusses the chlorite group of minerals. Chlorites are phyllosilicate minerals with a 2:1 sandwich structure composed of a tetrahedral-octahedral-tetrahedral layer and an interlayer of (Mg2+, Fe3+)(OH)6. Common chlorite minerals include clinochlore and chamosite. Chlorites form in low-temperature metamorphic rocks, igneous rocks, and sediments. They are also associated with hydrothermal ore deposits. Chlorites have a range of uses including extracting chlorine and as gemstones.
Gemmology is a vast subject to learn about all the Gemstones, their properties, occurrences, geographical location, geometrical structure or formations, various colour shades, transparency to opaque, sheen & luster, cuts & shapes, carat & cost, testing through various instruments & devices for their Real, synthetics or simulants.
This document discusses radiolaria, which are single-celled eukaryotes commonly found in marine environments. Radiolaria have intricate silica skeletons that can be spherical, cone-shaped, or other forms, sometimes with spines or fins. They live throughout the world's oceans and can be found from the surface to depths of 3000 meters. Their long fossil record and diversity over time make radiolaria useful for determining the age and environment of deposits lacking other fossils. Their classification is based on both skeletal and soft tissue features.
1. Wall rock alteration occurs when hot hydrothermal fluids interact with surrounding country rocks, changing their mineralogy. There are two main types: hypogene alteration from ascending fluids and supergene alteration from descending waters.
2. Alteration products depend on the rock character, fluid properties like pH and temperature/pressure conditions. Important reactions include hydrolysis, hydration, dechlorination, silication, and decarbonation.
3. Different alteration types are associated with certain deposit types, like potassic alteration with porphyry copper deposits and greisenization indicating tin or tungsten. Original rock type influences prevalent alteration, such as sericitization and silicification in acidic rocks.
Copper is an important metal that has been used for over 10,000 years. It has many important uses such as in construction, electronics, transportation and machinery. Copper is highly conductive and does not corrode easily. The global demand for copper is increasing due to growth in emerging economies but new copper mines are difficult to develop due to challenges such as high costs, environmental opposition and political instability. Copper recycling helps offset this demand and supply imbalance but not completely.
This document discusses stable carbon isotopes and their applications. It begins by introducing stable isotopes and focusing on the two stable isotopes of carbon: 12C and 13C. It then discusses how the ratio of these isotopes varies in different materials and can be used to determine organic vs inorganic origins of carbon and distinguish marine vs nonmarine deposits. Applications include determining the source and maturity of fossil fuels, identifying evidence of early life in Precambrian sediments, and studying the deep earth carbon cycle via analyses of carbonatites and diamonds.
This document contains information from 4 experiments on applied geology:
1. Testing the hardness of various minerals using Mohs scale, ranging from talc at 1 to diamond at 10.
2. Studying models of folds and faults in rock formations, including symmetrical, asymmetrical, overturned, and recumbent folds, as well as normal and reverse faults.
3. Identifying international geological symbols used for rocks and minerals.
4. Identifying 11 rock-forming minerals - talc, mica, calcite, malachite, gypsum, hematite, magnetite, bauxite, fluorite, dolomite, and aragonite - based on their physical properties and common uses.
This document provides an introduction to ore microscopy. It defines ores and discusses sample preparation techniques and properties that can be observed through microscopic analysis, including:
- Classification of ore deposits as primary, secondary, syngenetic, or epigenetic
- Properties of ore minerals like color, reflectance, hardness, cleavage, and twinning
- Techniques like polishing, etching, and use of an ore microscope
- Advanced techniques like electron microprobe analysis, Raman spectroscopy, and stable isotope studies
The document aims to outline the key aspects of microscopic ore analysis.
The document provides guidance on starting a rock collection for microfossil study. It recommends properly labeling collected samples with location data and replacing poor samples. Basic collecting equipment includes a geologist's hammer and hand lens. Surface samples can be collected from natural exposures while subsurface samples come from wells and boreholes, with cores providing the most accurate records. The best collecting sites are quarries, road cuts, and outcrops displaying unweathered rock. Careful permanent labeling and record keeping is important for housing and maintaining the collection.
Twinning occurs when two or more crystals share lattice points, adding apparent symmetry. There are three types of twinning: growth twins from accidents during crystal formation, transformation twins from changes in pressure/temperature, and deformation twins from stress. Common twinning includes albite twins in plagioclase feldspar and Carlsbad twins in orthoclase. Twinning can be identified by planes or axes of added symmetry like reflection or rotation.
The document summarizes the key steps in the ore dressing (mineral processing) process. It describes four main steps: 1) Comminution which involves crushing and grinding ore to reduce particle size. 2) Sizing by screening to separate particles by size. 3) Concentration using methods like hydraulic washing, magnetic separation, froth flotation, and leaching to separate minerals from waste rock. 4) Dewatering to remove water from concentrated mineral particles.
This document discusses heavy minerals found in placer deposits. Placer deposits form from weathering and erosion of heavy minerals that are then transported and concentrated by gravity and deposited in areas like beaches. Common heavy minerals include ilmenite, magnetite, rutile, zircon and monazite. These minerals can be separated and extracted using physical processes that exploit differences in their magnetic, electrostatic and density properties, such as magnetic separation, electrostatic separation and gravity separation using spiral concentrators. Heavy minerals are economically important and indicators of sediment sources.
Quartz is found in almost every geological environment. It is a common constituent in most of the rock types and soil groups. Granite, sandstone, limestone, and most of the igneous, sedimentary, and metamorphic rocks contain quartz. Quartz contains mainly oxygen and silicon. These two constituents make upto 75 % of the earth’s crust. An alternate name for the Quartz Group is the Silica Group.
This document discusses types of classifiers used in mineral processing. There are two main types - wet classification and dry classification. Wet classifiers separate minerals based on differences in settling velocities in water, and include spiral classifiers, hydraulic classifiers, and hydrocyclones. Dry classifiers separate minerals using air flow and centrifugal forces, and include gravitational, centrifugal, and gravitational inertial classifiers. The document provides details on how different classifier types operate and the size ranges they can be used to separate.
The Origins of Amethyst’s Purple Hue: Things You Need To KnowBnher.com
Amethyst, a member of the quartz family, is celebrated for its enchanting purple color that ranges from delicate lilac to deep violet. This gemstone has fascinated civilizations throughout history, earning a place of prominence in jewelry and metaphysical practices. The origin of amethyst’s purple color is a captivating journey into the depths of geology and crystallography. In this comprehensive exploration, we delve into the various factors that contribute to the alluring purple hues of amethyst, from its geological formation to the role of trace elements.
The document discusses the history and properties of various birthstones assigned to each month. It provides details on the origins, legends, and sources of gems corresponding to January (garnet), February (amethyst), March (aquamarine or bloodstone), April (diamond), May (emerald), June (pearl or alexandrite), and July (ruby). It describes the appearance, meanings, and care recommendations for each stone.
Gems are expensive mineral stones that provide links between various scientific fields. There are about 150 natural gem compounds. Diamonds, emeralds, rubies, and sapphires sell at the highest prices due to their beauty, rarity, traditions, and perceptions of permanence. Gems have characteristics like color, refractive index, dispersion, absorption, and facets that make them attractive. Their properties like hardness, chemical stability, and double refraction also provide practical applications beyond decoration. Many gems like quartz, topaz, and tourmaline are studied scientifically or believed to have healing properties according to traditions.
This document discusses processing sand and silica sand into other materials. It begins by outlining examples of mineral processing including sand, silica sand, and heavy mineral sand. For processing sand and silica sand, it describes extracting, washing, classifying, and removing impurities from the sand through steps like screening, attrition scrubbing, hydrocyclones, and magnetic separation. The sand can then be further processed into silicon, silicon carbide, and silicone through reducing silica to ferrosilicon, purifying it through distillation of trichlorosilane, and using the Siemens process to deposit high purity silicon. Heavy mineral sands can also be separated into minerals like zircon, rut
This document discusses sedimentary structures, which are macroscopic features formed during sediment deposition. It classifies sedimentary structures based on their morphology and formation processes. The key types discussed are physical structures like bedding, cross-bedding, and ripple marks formed directly by sedimentation. Chemical structures like nodules and concretions are formed by precipitation. Biogenic structures such as stromatolites and trace fossils provide evidence of ancient life. Studying sedimentary structures can provide insight into depositional environments, paleocurrents, and stratigraphic relationships.
This document provides an overview of calcareous microfossils, specifically focusing on foraminifera. It defines foraminifera as single-celled organisms with shells composed of calcite or aragonite. Their shells are made of one or multiple chambers. Foraminifera morphology and mineralogy form the basis for identification and classification. They first appeared in the Cambrian period and have been important for paleoclimate reconstruction, paleoceanography studies, archaeology, biostratigraphy, and oil exploration.
This document provides an overview of gemstones, including their physical and optical properties, shapes and cuts, and synthetics and simulants. It discusses the key properties used to identify gemstones such as crystal habit, specific gravity, hardness, refractive index, and luminescence. Different cutting styles including cabochon and faceted cuts are described. The document also covers synthetic gemstones which mimic natural stones, and simulants which have similar appearances but different properties. It aims to equip gemologists with the knowledge to distinguish natural gems from synthetics or enhanced stones.
The document discusses the chlorite group of minerals. Chlorites are phyllosilicate minerals with a 2:1 sandwich structure composed of a tetrahedral-octahedral-tetrahedral layer and an interlayer of (Mg2+, Fe3+)(OH)6. Common chlorite minerals include clinochlore and chamosite. Chlorites form in low-temperature metamorphic rocks, igneous rocks, and sediments. They are also associated with hydrothermal ore deposits. Chlorites have a range of uses including extracting chlorine and as gemstones.
Gemmology is a vast subject to learn about all the Gemstones, their properties, occurrences, geographical location, geometrical structure or formations, various colour shades, transparency to opaque, sheen & luster, cuts & shapes, carat & cost, testing through various instruments & devices for their Real, synthetics or simulants.
This document discusses radiolaria, which are single-celled eukaryotes commonly found in marine environments. Radiolaria have intricate silica skeletons that can be spherical, cone-shaped, or other forms, sometimes with spines or fins. They live throughout the world's oceans and can be found from the surface to depths of 3000 meters. Their long fossil record and diversity over time make radiolaria useful for determining the age and environment of deposits lacking other fossils. Their classification is based on both skeletal and soft tissue features.
1. Wall rock alteration occurs when hot hydrothermal fluids interact with surrounding country rocks, changing their mineralogy. There are two main types: hypogene alteration from ascending fluids and supergene alteration from descending waters.
2. Alteration products depend on the rock character, fluid properties like pH and temperature/pressure conditions. Important reactions include hydrolysis, hydration, dechlorination, silication, and decarbonation.
3. Different alteration types are associated with certain deposit types, like potassic alteration with porphyry copper deposits and greisenization indicating tin or tungsten. Original rock type influences prevalent alteration, such as sericitization and silicification in acidic rocks.
Copper is an important metal that has been used for over 10,000 years. It has many important uses such as in construction, electronics, transportation and machinery. Copper is highly conductive and does not corrode easily. The global demand for copper is increasing due to growth in emerging economies but new copper mines are difficult to develop due to challenges such as high costs, environmental opposition and political instability. Copper recycling helps offset this demand and supply imbalance but not completely.
This document discusses stable carbon isotopes and their applications. It begins by introducing stable isotopes and focusing on the two stable isotopes of carbon: 12C and 13C. It then discusses how the ratio of these isotopes varies in different materials and can be used to determine organic vs inorganic origins of carbon and distinguish marine vs nonmarine deposits. Applications include determining the source and maturity of fossil fuels, identifying evidence of early life in Precambrian sediments, and studying the deep earth carbon cycle via analyses of carbonatites and diamonds.
This document contains information from 4 experiments on applied geology:
1. Testing the hardness of various minerals using Mohs scale, ranging from talc at 1 to diamond at 10.
2. Studying models of folds and faults in rock formations, including symmetrical, asymmetrical, overturned, and recumbent folds, as well as normal and reverse faults.
3. Identifying international geological symbols used for rocks and minerals.
4. Identifying 11 rock-forming minerals - talc, mica, calcite, malachite, gypsum, hematite, magnetite, bauxite, fluorite, dolomite, and aragonite - based on their physical properties and common uses.
This document provides an introduction to ore microscopy. It defines ores and discusses sample preparation techniques and properties that can be observed through microscopic analysis, including:
- Classification of ore deposits as primary, secondary, syngenetic, or epigenetic
- Properties of ore minerals like color, reflectance, hardness, cleavage, and twinning
- Techniques like polishing, etching, and use of an ore microscope
- Advanced techniques like electron microprobe analysis, Raman spectroscopy, and stable isotope studies
The document aims to outline the key aspects of microscopic ore analysis.
The document provides guidance on starting a rock collection for microfossil study. It recommends properly labeling collected samples with location data and replacing poor samples. Basic collecting equipment includes a geologist's hammer and hand lens. Surface samples can be collected from natural exposures while subsurface samples come from wells and boreholes, with cores providing the most accurate records. The best collecting sites are quarries, road cuts, and outcrops displaying unweathered rock. Careful permanent labeling and record keeping is important for housing and maintaining the collection.
Twinning occurs when two or more crystals share lattice points, adding apparent symmetry. There are three types of twinning: growth twins from accidents during crystal formation, transformation twins from changes in pressure/temperature, and deformation twins from stress. Common twinning includes albite twins in plagioclase feldspar and Carlsbad twins in orthoclase. Twinning can be identified by planes or axes of added symmetry like reflection or rotation.
The document summarizes the key steps in the ore dressing (mineral processing) process. It describes four main steps: 1) Comminution which involves crushing and grinding ore to reduce particle size. 2) Sizing by screening to separate particles by size. 3) Concentration using methods like hydraulic washing, magnetic separation, froth flotation, and leaching to separate minerals from waste rock. 4) Dewatering to remove water from concentrated mineral particles.
This document discusses heavy minerals found in placer deposits. Placer deposits form from weathering and erosion of heavy minerals that are then transported and concentrated by gravity and deposited in areas like beaches. Common heavy minerals include ilmenite, magnetite, rutile, zircon and monazite. These minerals can be separated and extracted using physical processes that exploit differences in their magnetic, electrostatic and density properties, such as magnetic separation, electrostatic separation and gravity separation using spiral concentrators. Heavy minerals are economically important and indicators of sediment sources.
Quartz is found in almost every geological environment. It is a common constituent in most of the rock types and soil groups. Granite, sandstone, limestone, and most of the igneous, sedimentary, and metamorphic rocks contain quartz. Quartz contains mainly oxygen and silicon. These two constituents make upto 75 % of the earth’s crust. An alternate name for the Quartz Group is the Silica Group.
This document discusses types of classifiers used in mineral processing. There are two main types - wet classification and dry classification. Wet classifiers separate minerals based on differences in settling velocities in water, and include spiral classifiers, hydraulic classifiers, and hydrocyclones. Dry classifiers separate minerals using air flow and centrifugal forces, and include gravitational, centrifugal, and gravitational inertial classifiers. The document provides details on how different classifier types operate and the size ranges they can be used to separate.
The Origins of Amethyst’s Purple Hue: Things You Need To KnowBnher.com
Amethyst, a member of the quartz family, is celebrated for its enchanting purple color that ranges from delicate lilac to deep violet. This gemstone has fascinated civilizations throughout history, earning a place of prominence in jewelry and metaphysical practices. The origin of amethyst’s purple color is a captivating journey into the depths of geology and crystallography. In this comprehensive exploration, we delve into the various factors that contribute to the alluring purple hues of amethyst, from its geological formation to the role of trace elements.
The document discusses the history and properties of various birthstones assigned to each month. It provides details on the origins, legends, and sources of gems corresponding to January (garnet), February (amethyst), March (aquamarine or bloodstone), April (diamond), May (emerald), June (pearl or alexandrite), and July (ruby). It describes the appearance, meanings, and care recommendations for each stone.
The document provides descriptions of various gemstones, including their histories, symbolism, and associations. It discusses stones such as amethyst, aquamarine, black onyx, blue sapphire, blue topaz, citrine, diamond, emerald, garnet, peridot, pink tourmaline, rose quartz, ruby, smoky quartz, tsavorite, and white sapphire. For each stone, it provides 1-2 sentences on their ancient meanings and uses.
Carnelian is a variety of chalcedony, a microcrystalline form of quartz that forms in sedimentary environments. Its color ranges from orange to red due to iron oxide impurities like hematite. Carnelian was highly valued in ancient Egypt and Greece/Rome, used in jewelry, amulets, and seals. Agate is a banded variety of chalcedony that comes in many colors and was commonly used in ancient Greece for ornamental purposes. Corundum is a crystalline form of aluminum oxide that occurs as the gemstones ruby and sapphire, taking their color from transition metal impurities. Olivine is a common magnesium iron silicate in Earth's mantle that we
The birthstone for February is amethyst, a purple quartz gemstone that has been treasured for centuries by royalty and religious figures. According to Greek mythology, amethyst derived its purple color when Dionysus stained white quartz with wine tears after inadvertently harming a young maiden named Amethyst. Historically, amethyst was believed to have various healing properties and protect against evil thoughts or anger. Today, it remains a durable and beautiful choice for jewelry.
The birthstone for February is amethyst, a purple quartz gemstone that has been treasured for centuries by royalty and religious figures. According to Greek mythology, amethyst derived its purple color when Dionysus stained white quartz with wine tears after inadvertently harming a young maiden named Amethyst. Historically, amethyst was believed to have various healing properties and protect against evil thoughts or anger. Today, it remains a durable and beautiful choice for jewelry.
Thomas Disselkamp is a senior product development engineer at 3M who collects agates in his free time. Agate is a crystalline form of silica that forms in volcanic and metamorphic rocks, and is considered a semiprecious gemstone due to its colorful patterns and unique shapes. While agates can be found worldwide, some prized locations include Germany, Botswana, Brazil, and the Upper Midwest of the United States near Lake Superior. Tom Disselkamp has a large collection of agates that vary in size and color, about a third of which he has polished to enhance their beauty.
Opal gemstone build a number of the foremost stunning items of jewellery accessible. the majority area unit acquainted with diamonds, rubies, and pearls. but there area unit several others that attract the attention because of their exquisite beauty, however they're less standard. Keep reading for a quick description of a number of the foremost eye-appealing gems within the world.
This document provides an overview of diamonds, including their history, formation, types, mining, and cutting/polishing processes. It discusses how diamonds formed deep within the earth under extreme heat and pressure. It outlines the early history of diamonds in India and their various uses. The document details the major types of diamonds including pink, white, champagne, and yellow varieties. It describes the two main mining methods - pipe mining which extracts diamonds from volcanic pipes and alluvial mining from riverbeds. Finally, it summarizes the multi-step cutting and polishing process to transform rough diamonds into brilliant gemstones.
Fundamentals Of Gemstones | Drishti GemsDrishti Gems
From generation to generation, stones have been and still are there to fascinate us for thousands of years and tell us part of the history of the Earth. Mankind is learning about the world of minerals and gems, objects of art and vast subjects of science. In this article, we will review. We are Drishti Gems, a provider of premium and natural gemstones direct driven through mines worldwide. You want to know more about gemstones and their price, then you can contact us at +91-7814474383
Top 12 emerald engagement rings you're going to want right now Janny Chan
May birthday celebrants are really in luck because it is one of the months when the winter comes to an end and the final school month before summer arrives. Emerald is one of the most iconic of all birthstones. Here, 12 emerald engagement rings you'll envy–until one of them becomes yours.
Birthstones are associated with each month of the year. The document discusses the traditional birthstones from January to December, describing their gemological properties and where they are sourced from around the world. Some of the birthstones mentioned include garnet for January, amethyst for February, aquamarine for March, diamond for April, emerald for May, pearl for June, ruby for July, peridot for August, sapphire for September, opal for October, topaz for November, and turquoise for December. The document provides details on factors like each stone's color, hardness, locations where the finest quality gems are found, and tips for caring for some of the more delicate varieties.
Jade is the gem name for mineral aggregates composed of either or both of two different minerals, Jadeite and Nephrite. Jadeite is a sodium-rich aluminous pyroxene; nephrite is a fine-grained, calcium-rich, magnesium, iron, aluminous amphibole. All jade is composed of fine-grained, highly intergrown, interlocking crystals of one or both of these minerals. Though neither mineral is very hard (6-7), jade is one of the toughest gem minerals known because of the intergrown nature of the individual crystals.
Humankind has been obsessed with gemstones starting from ancient civilisations to this modern era. This beautiful work of art by nature is made naturally from minerals in Earth's crust. Gemstone jewellery has been a part of our culture with its simplicity, elegance and colourful appearance gemstones and is still ruling the minds of jewellery lovers around the world.
Let’s look at some interesting facts about gemstones:
Brazil is a major producer of gemstones, mining more than half of the world's colored gems. Some of the most important gemstones found in Brazil include aquamarines, beryls, chrysoberyls, topazes, amethysts, tourmalines, emeralds and agates. Emeralds were first discovered in Egypt but significant deposits were later found in South America after Columbus' exploration, establishing Brazil as an important source. Gemstones from Brazil like emeralds, aquamarines and topazes are renowned for their beauty and valued worldwide.
Pearl, the birth stone for month of June, is among the foremost dateless, classic and precious of all opal stone. Through out history, these noble gems are related to knowledge, wealth, purity, romance and mystery. the traditional Egyptian were buried with them. In Rome, Pearls were thought-about the final word image of wealth and standing. The Greeks prized them for his or her beauty and association amorously and wedding. Medieval Knights wore them in battle as a amulet against injury. And, throughout the renaissance, some European countries prohibited near nobility from the correct to wear opal bracelet.
This document provides information about minerals and crystals, including their properties and classification. It discusses how minerals are composed of elements or chemicals and can form in crystalline shapes or shapeless masses. It also describes the eight main mineral groups based on their chemical composition, including native elements, silicates, oxides, sulfides, sulfates, halides, carbonates, and phosphates. The rest of the document discusses the properties of different birthstones for each month.
Amber is a fossilized tree resin that was originally extruded from conifer trees 20-60 million years ago. It has been greatly appreciated as a gemstone for thousands of years in Europe. Though not given much importance by mineralogists, amber is scientifically significant as it often preserves ancient life intact. Found in sedimentary rocks worldwide, amber forms in various colors and transparencies. Highly valued since antiquity, amber continues to be used for jewelry, ornamentation, and folk medicine remedies today.
Hematite is a common mineral that is usually colored black, steel, gray, brown, reddish brown, or red. It forms in a variety of shapes but always has a rust-red streak. Large deposits of hematite are found in banded iron formations and near bodies of standing water or mineral hot springs. Hematite was popular in Victorian-era European jewelry and remains common in Native American jewelry and art of the western United States where it is found. The mineral is responsible for the red color of many sedimentary rocks and gets its name from the Greek word for blood due to its blood-like red color.
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CapCut is an easy-to-use video editing app perfect for beginners. To start, download and open CapCut on your phone. Tap "New Project" and select the videos or photos you want to edit. You can trim clips by dragging the edges, add text by tapping "Text," and include music by selecting "Audio." Enhance your video with filters and effects from the "Effects" menu. When you're happy with your video, tap the export button to save and share it. CapCut makes video editing simple and fun for everyone!
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2. Amethyst Story
Amethyst is a violet variety of quartz. The name comes from the Koine
Greek αμέθυστος amethystos from α- a-, "not" and μεθύσκω (Ancient
Greek) methysko / μεθώ metho (Modern Greek), "intoxicate", a reference
to the belief that the stone protected its owner from drunkenness. The
ancient Greeks wore amethyst and carved drinking vessels from it in the
belief that it would prevent intoxication
3. Structure
Amethyst is a purple variety of quartz (SiO2) and owes its violet
color to irradiation, impurities of iron and in some cases other
transition metals, and the presence of other trace elements, which
result in complex crystal lattice substitutions. The hardness of the
mineral is the same as quartz, thus making it suitable for use in
jewelry.
4. Hue and Tone
Amethyst occurs in primary hues from a light lavender or pale violet, to a deep purple.
Amethyst may exhibit one or both secondary hues, red and blue. High quality amethyst
can be found in Siberia, Sri Lanka, Brazil, Uruguay, and the Far East. The ideal grade is
called "Deep Siberian" and has a primary purple hue of around 75–80%, with 15–20% blue
and (depending on the light source) red secondary hues. Rose de France’ is defined by its
markedly light shade of the purple, reminiscent of a lavender/lilac shade. These pale colors
were once considered undesirable but have recently become popular due to intensive
marketing.
Green quartz is sometimes incorrectly called green amethyst, which is a misnomer and not
an appropriate name for the material, the proper terminology being prasiolite. Other names
for green quartz are vermarine or lime citrine.
5. Amethyst frequently shows color zoning, with the most intense color typically found at
the crystal terminations. One aspect in the art of lapidary involves correctly cutting the
stone to place the color in a way that makes the tone of the finished gem
homogeneous. Often, the fact that sometimes only a thin surface layer of violet color
is present in the stone or that the color is not homogeneous means that only a small
portion of the material is suitable for faceting.
The color of amethyst has been demonstrated to result from substitution by irradiation
of trivalent iron (Fe3+) for silicon in the structure, in the presence of trace elements of
large ionic radius, and, to a certain extent, the amethyst color can naturally result from
displacement of transition elements even if the iron concentration is low. Natural
amethyst is dichroic in reddish violet and bluish violet, but when heated, turns yellow-
orange, yellow-brown, or dark brownish and may resemble citrine, but loses its
dichroism, unlike genuine citrine. When partially heated, amethyst can result in
ametrine.
6. History
Amethyst was used as a gemstone by the ancient Egyptians and was largely
employed in antiquity for intaglio engraved gems.
The Greeks believed amethyst gems could prevent intoxication, while medieval
European soldiers wore amethyst amulets as protection in battle in the belief
that amethysts heal people and keep them cool-headed. Beads of amethyst
were found in Anglo-Saxon graves in England. Anglican bishops wear an
episcopal ring often set with an amethyst, an allusion to the description of the
Apostles as "not drunk" at Pentecost in Acts 2:15.
A large geode, or "amethyst-grotto", from near Santa Cruz in southern Brazil
was presented at a 1902 exhibition in Düsseldorf, Germany.
7. Geographic Distribution
Amethyst is found in many locations around the world. Between 2000 and 2010,
the greatest production was from Marabá and Pau d'Arco, Pará, and the Paraná
Basin, Rio Grande do Sul, Brazil; Sandoval, Santa Cruz, Bolivia; Artigas,
Uruguay; Kalomo, Zambia; and Thunder Bay, Ontario. Lesser amounts are found
in many other locations in Africa, Brazil, Spain, Argentina, Russia, Afghanistan,
South Korea, Mexico, and the United States.
Amethyst is produced in abundance from the state of Rio Grande do Sul in Brazil
where it occurs in large geodes within volcanic rocks. Many of the hollow agates
of southwestern Brazil and Uruguay contain a crop of amethyst crystals in the
interior. Artigas, Uruguay and neighboring Brazilian state Rio Grande do Sul are
large world producers, with lesser quantities mined in Minas Gerais and Bahia
states.
8. Amethyst is also found and mined in South Korea. The large opencast amethyst vein at
Maissau, Lower Austria, was historically important, but is no longer included among
significant producers. Much fine amethyst comes from Russia, especially from near
Mursinka in the Ekaterinburg district, where it occurs in drusy cavities in granitic rocks.
Amethyst was historically mined in many localities in south India, though these are no
longer significant producers. One of the largest global amethyst producers is Zambia in
southern Africa with an annual production of about 1000 tons.
Amethyst occurs at many localities in the United States. The most important production is
at Four Peaks, Gila and Maricopa Counties, Arizona, and Jackson's Crossroads, Wilkes
County, Georgia. Smaller occurrences have been reported in the Red Feather Lakes, near
Fort Collins, Colorado; Amethyst Mountain, Texas; Yellowstone National Park; Delaware
County, Pennsylvania; Haywood County, North Carolina; Deer Hill and Stow, Maine and in
the Lake Superior region of Minnesota, Wisconsin and Michigan. Amethyst is relatively
common in the Canadian provinces of Ontario and Nova Scotia. The largest amethyst mine
in North America is located in Thunder Bay, Ontario
11. Ancient Greece
The Greek word "amethystos" may be translated as "not drunken", from Greek a-, "not" + methustos,
"intoxicated". Amethyst was considered to be a strong antidote against drunkenness, which is why
wine goblets were often carved from it. In his poem "L'Amethyste, ou les Amours de Bacchus et
d'Amethyste" (Amethyst or the loves of Bacchus and Amethyste), the French poet Remy Belleau
(1528–1577) invented a myth in which Bacchus, the god of intoxication, of wine, and grapes was
pursuing a maiden named Amethyste, who refused his affections. Amethyste prayed to the gods to
remain chaste, a prayer which the chaste goddess Diana answered, transforming her into a white
stone. Humbled by Amethyste's desire to remain chaste, Bacchus poured wine over the stone as an
offering, dyeing the crystals purple.
Variations of the story include that Dionysus had been insulted by a mortal and swore to slay the next
mortal who crossed his path, creating fierce tigers to carry out his wrath. The mortal turned out to be a
beautiful young woman, Amethystos, who was on her way to pay tribute to Artemis. Her life was
spared by Artemis, who transformed the maiden into a statue of pure crystalline quartz to protect her
from the brutal claws. Dionysus wept tears of wine in remorse for his action at the sight of the beautiful
statue. The god's tears then stained the quartz purple.
12. Other Cultural Associations
Tibetans consider amethyst sacred to the Buddha and make prayer
beads from it. Amethyst is considered the birthstone of February. In the
Middle Ages, it was considered a symbol of royalty and used to
decorate English regalia. In the Old World, amethyst was considered
one of the Cardinal gems, in that it was one of the five gemstones
considered precious above all others, until large deposits were found in
Brazil.
13. Value
Up until the 18th century, amethyst was included in the cardinal, or most valuable,
gemstones (along with diamond, sapphire, ruby, and emerald). However, since the
discovery of extensive deposits in locations such as Brazil, it has lost most of its value.
Collectors look for depth of color, possibly with red flashes if cut conventionally. As
amethyst is readily available in large structures the value of the gem is not primarily
defined by carat weight; this is different from most gemstones where the carat weight
exponentially increases the value of the stone. The biggest factor in the value of
amethyst is the color displayed.
The highest-grade amethyst (called "Deep Russian") is exceptionally rare and
therefore, when one is found, its value is dependent on the demand of collectors. It is,
however, still orders of magnitude cheaper than the highest-grade sapphires or rubies.
14. Color Of Amethyst Gemstone
1. Amethyst Gemstone is very attractive gemstone
because of purple color. Amethyst is the name of the
color as like word Turquoise.
2. Variety of shades of Amethyst Orchid and Lavender
for light color, Reddish Purple or Violetish color.
15. Amethyst Crystal
Amethyst receiving at purple color during crystal growth
when trace amount of iron are in corporate into a
growing quartz crystal.
The intensity of purple color vary from crystal to crystal.
After the crystallization, gamma rays emitted by the
radioactive material, and use iron to purple color.
17. Properties Of Amethyst
Gemstone
1. Amethyst is a powerful and protective gemstone.
2. Amethyst boosts hormone production, tune the
endocrine system and metabolism.
3. Amethyst protects the wearer from all types of harm
psychic attack and other health problem.
18. Care Of Amethyst Gem and
Jewelry
Avoid prolonged to bright light.
Always cleaned amethyst jewelry with warm and
sudsy water or use soft cloth.
19. Amethyst Treatment to
Citrine and Prasiolite
. The color of Amethyst can be modified by
heating.
. Yellow or Golden Quartz sold as “Citrine”.
. Natural heating can also change the color of
Amethyst to pale green the name of the treatment
is called Prasiolite.
20. CUT
Amethyst can be cut into a wide variety of shapes. As this is the case, you
will be almost guaranteed to find a stone to fit your personal style. You will
find these gemstones cut into standard shapes like rounds, pears, ovals,
and cushions.
You will also find purple quartz cut into faceted patterns referred to as
brilliant cuts. And, if you are exceptionally adventurous, it is possible to
find this special stone cut into one-of-a-kind shapes.
21. CARAT
Carat weight is always of importance in the discussion
of gemstones. This stunning gemstone is often chosen
as a center stone in jewelry as the cost of an amethyst
does not increase in cost as dramatically with size as
many other gemstones. Like other semi-precious
gemstones, a large amethyst will be noticeably more
cost-effective than precious stones like diamonds,
rubies, sapphires, and emeralds.
22. CLARITY
Although clarity can have an impact on the value of
your amethyst, so long as inclusions are
indistinguishable to the naked eye, they will not greatly
reduce the value of your stone. Indeed, color is more
important in determining the value of this particular gem
than minor flaws. Even with minor undistinguishable
flaws, an amethyst with good color will retain most of its
value.
23. How is Amethyst Graded?
Whether you are born in the month of February or are
just a fan of this engaging purple gemstone, you will
want to understand how amethysts are graded for
quality.
Amethysts gemstones typically fall under a AAAA
to B grading system.
24. AAAA GRADING
It is extremely rare to find an amethyst with
this rating. Only 1% of all amethysts can be
expected to fall under this category. These
stones will have no inclusions visible to the
naked eye. Considered heirloom quality,
these much sought after gemstones will
have a distinctly dark purple hue.
25. AAA GRADING
You can expect to find only 10% of amethyst to fall
into this category. These exceptional gemstones
will have no visible flaws and a medium to dark
purple color.
26. AA GRADING
Approximately 33% of amethyst on the
market will fall into this category. You can
expect to find slight inclusions in these
medium purple gemstones.
27. A GRADING
Still considered good, these light purple
amethysts can be expected to have
slight to moderate inclusions.
28. B GRADING
There are also amethysts with a B grading, but we do
not recommend B grade amethysts to be set in jewelry.
They have obvious inclusions, and its color would have
hues of grey and/or brown. B grade amethysts are
usually chosen to be cut into cabochons, or beads.
However, there are circumstances where it can be
treated to have a richer purple color.