SHB337~1.Powerpoint prsentation in ELSSScjoypingaron
?
Minerals are naturally occurring solid substances with a crystalline structure. They are formed through natural geological processes and are not living or once living. All minerals share the properties of having a definite shape and volume, being made up of unique chemical compounds or elements, and having particles arranged in repeating crystalline patterns. Minerals are grouped based on their chemical composition, with the largest group being silicates that contain silicon and oxygen. Other common mineral groups include non-silicates, carbonates, oxides, sulfides, sulfates, and native elements. Minerals form through the cooling of magma or the recrystallization of dissolved elements in water. Their properties like color, luster, hardness, cleavage/fracture
1) Minerals are naturally formed solid substances with a crystal structure that are not alive and have a definite volume and shape.
2) All minerals share characteristics of being formed by natural processes, having a unique chemical makeup, and being made up of particles arranged in a repeating crystal pattern.
3) Minerals are grouped based on their chemical composition, with the most abundant group being silicates containing oxygen and silica like quartz and mica.
The document discusses the properties of rocks and minerals. It defines a mineral as having a definite chemical composition and naturally occurring inorganic formation. It notes that the two most abundant elements in the Earth's crust are silicon and oxygen, which combine to form silicate compounds. Minerals can be identified based on properties like crystal structure, color, streak, luster, hardness, cleavage, and fracture.
This document discusses how minerals are identified. It begins by defining minerals as naturally occurring inorganic solids with a crystal structure and specific chemical composition. It then explains that minerals are identified based on their physical properties, including hardness, luster, streak, color, cleavage, and fracture. The document focuses on Mohs hardness scale as an important identification tool and provides examples of different luster, streak, color, cleavage and fracture properties.
The document discusses minerals, their properties, and how they are classified. It defines minerals as naturally occurring solid substances with a crystal structure. All minerals share common characteristics - they form through natural processes, are not living, have a definite shape and volume, and are made of elements or compounds arranged in repeating crystal patterns. Minerals are grouped based on their chemical composition, with the most abundant group being silicates like quartz and mica. Physical properties like color, luster, hardness, cleavage/fracture, and specific gravity can be used to identify different minerals.
Minerals are naturally occurring inorganic solids with definite chemical compositions and orderly atomic structures. There are about 4,000 known minerals on Earth. Minerals form through natural geological processes without human involvement and are distinguished from other substances based on properties like hardness, crystal structure, luster, specific gravity, streak, and cleavage/fracture. Common minerals are important materials for construction, technology, and gems that are valued for their beauty and rarity.
Minerals are naturally occurring inorganic solids that have a definite chemical composition and crystal structure. They form through geological processes such as cooling of magma or crystallization of dissolved materials. Minerals are identified based on properties like color, crystal structure, hardness, and density. They have many important economic uses in construction, technology, and everyday products.
Minerals are naturally occurring inorganic solids that have a definite chemical composition and crystal structure. They form through geological processes such as cooling of magma or crystallization of dissolved materials. Minerals are identified based on properties like color, crystal structure, hardness, and chemical makeup. The main minerals in Earth's crust include oxygen, silicon, aluminum, and iron.
There are five key characteristics of minerals:
1. They are naturally formed and not man-made.
2. They are inorganic, composed of non-living materials like iron and lead.
3. They are solids with a definite volume and shape under normal conditions.
4. They have a definite and consistent chemical composition throughout, like galena (PbS).
5. They have a crystalline atomic structure with atoms arranged in repeating patterns, like NaCl.
Minerals are naturally occurring inorganic solids that have a crystalline structure and definite chemical composition. All minerals must form naturally, be inorganic, solid, and crystalline in structure. Minerals can be identified based on their physical properties, including color, luster, streak, hardness, and whether they exhibit cleavage or fracture.
This document provides information about minerals, including their formation, composition, properties, and crystal structures. It discusses how minerals are the building blocks of rocks and are made up of arrangements of atoms. There are over 2,500 known mineral types that are classified based on their chemical composition and crystalline structure. Common properties described for identifying minerals include color, streak, luster, hardness, cleavage, and crystal shape.
Minerals are naturally occurring inorganic solids with definite chemical compositions and ordered atomic structures. They form through natural geological processes on or inside Earth. Key properties used to identify minerals include hardness, luster, specific gravity, streak, and cleavage/fracture. Minerals have many important uses beyond gems, including as sources of useful elements like iron, aluminum, and titanium that are integral to infrastructure, transportation, and technology.
This document provides information on minerals, rocks, and their properties. It defines minerals as naturally occurring solid materials with a defined chemical composition and internal structure. The most common elements in Earth's crust are oxygen, silicon, aluminum, iron, calcium, sodium, and potassium. Minerals are divided into silicate and non-silicate groups. Key silicate minerals include quartz, feldspar, mica, amphibole, pyroxene, olivine, and garnet. Non-silicates include carbonates, oxides, sulfides, phosphates, and native elements. Physical properties used to identify minerals include color, streak, luster, hardness, crystal shape, cleavage, fracture, and specific
The document discusses minerals and their properties. It defines minerals as inorganic, solid, naturally occurring substances with defined chemical compositions. It then lists 13 common mineral properties including crystal form, luster, color, streak, hardness, cleavage, specific gravity, taste, touch, magnetism, magnification, smell, and chemical reactions. It also outlines the 7 main mineral groups and provides examples of minerals within each group, which include silicates, carbonates, halides, native elements, sulfates, sulfides, and oxides.
Properties of minerals can be used to identify them, including color, luster, streak, cleavage, fracture, hardness, specific gravity, acid test, crystals, and special properties. Color is not always reliable since many minerals can be the same color or a mineral can come in different colors. A mineral's luster refers to how it shines and can be metallic, non-metallic, vitreous, or pearly. Hardness is measured on Mohs scale from 1 to 10 based on which materials can scratch the mineral. Special properties include traits like magnetism, radioactivity, or fluorescence under UV light that are unique to certain minerals.
Properties of Minerals - Earth and Life ScienceJennGarcia21
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This presentation explores the key properties that define minerals, crucial components of Earth's crust. It covers the fundamental characteristics used to identify and classify minerals, such as hardness, luster, color, streak, cleavage, fracture, and specific gravity. The presentation also discusses how these properties relate to the mineral's internal structure and composition.
The document defines minerals as natural, inorganic, crystalline solids with a definite chemical composition. It describes the key physical properties of minerals - color, streak, hardness, cleavage, fracture, and luster - which are used to identify different minerals. Special properties like magnetism, fluorescence, and piezoelectricity are also discussed. Identification tests involving hardness, streak, and acid reactions are presented as ways to determine the type of mineral.
1) The document is a report on mineralogy presented to an Earth Science professor at Technological University of the Philippines by Hannah Joy N. Lontayao.
2) It defines minerals and rocks, and explains that minerals have definite chemical compositions and atomic structures while rocks are combinations of minerals.
3) The report describes several properties of minerals including crystal form, luster, color, streak, hardness, cleavage, fracture, and specific gravity. It also discusses the seven main mineral groups.
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Gems aren't just pretty faces; they've got science behind them. From the geological birth of gems in igneous, metamorphic, and sedimentary rocks to their chemical makeup, we've uncovered the secrets that make each stone unique. Ever wondered how a diamond gets its sparkle? It's all in the dispersion, folks!
But it's not just about looks; we're talking physical properties too. From thermal conductivity that makes diamonds feel cool to the touch to the electrostatic magic that makes amber cling to your sweater, these stones have tricks up their sleeves.
When it comes to telling gems apart, we've got the tools. Whether it's a trusty magnifying glass for a 10x closer look or a high-tech infrared spectrometer for serious analysis, we've got the lowdown on the gadgets that reveal a gem's true colors.
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The document provides information on rocks and minerals. It begins by defining a mineral as a naturally occurring, inorganic solid with a definite chemical composition and crystalline structure. Minerals can be identified based on their physical properties like color, streak, luster, hardness, cleavage, and crystal shape. Rocks are composed of two or more minerals and are classified based on their formation process as igneous, sedimentary, or metamorphic. Igneous rocks form from cooling magma, sedimentary rocks form through compaction and cementation of sediments, and metamorphic rocks form from changes to existing rocks through heat, pressure, and chemical activity.
The document discusses minerals and how they are used to identify rocks. Minerals are naturally occurring inorganic solids that make up Earth's rocks. There are over 2000 minerals but a dozen are most common. Scientists identify minerals through their physical and chemical properties such as color, hardness, streak, luster, cleavage, and special properties. Hardness is a mineral's ability to resist scratching and is measured using Mohs scale. Streak is the colored powder that remains when a mineral is rubbed on porcelain. Cleavage and fracture refer to how a mineral breaks into pieces. Luster describes a mineral's shininess. These properties are used to identify unknown minerals.
The document provides an overview of minerals, including their definition, classification, properties, and importance. It discusses that minerals are the building blocks of rocks and there are over 4,000 known types. Minerals have specific physical properties like crystal structure, hardness, and cleavage that allow them to be identified. The most abundant minerals in the Earth's crust are silicates, which make up the majority of rocks.
This document provides information about minerals, including their typical uses, definitions, groups, properties, and identification tests. It discusses the main mineral groups like silicates and non-silicates. It also describes several properties used to identify minerals, such as crystal form, luster, hardness, cleavage, specific gravity, and reactions to acid. Identification of minerals involves analyzing their physical and chemical properties.
Minerals are naturally occurring inorganic solids that have a definite chemical composition and crystal structure. The key properties used to identify minerals are streak, luster, cleavage or fracture, density, and hardness. Streak is the color of the powdered mineral, luster describes the surface reflection or shine, cleavage and fracture refer to how the mineral breaks, density is a mineral's weight compared to water, and hardness tests how easily a mineral can be scratched. These physical properties allow minerals to be distinguished from one another.
rocks and minerals-131013154238-phpapp01.pptAyele Akuma
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This document provides information about minerals and rocks. It defines minerals as solid, naturally occurring substances that have a definite chemical composition and internal structure. Minerals can be identified based on their physical properties like color, luster, hardness, cleavage, and crystal shape. Rocks are composed of two or more minerals and form through igneous, sedimentary, and metamorphic processes. Igneous rocks form from the cooling of magma, sedimentary rocks form through the compaction and cementation of sediments, and metamorphic rocks form under heat and pressure.
Earth and Life Science lesson minerals.pptHazelJoanTan1
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This lesson explores minerals, the naturally occurring, inorganic substances that form the building blocks of Earth's crust. Students learn about their physical and chemical properties, including color, luster, hardness, and crystal structure.
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There are five key characteristics of minerals:
1. They are naturally formed and not man-made.
2. They are inorganic, composed of non-living materials like iron and lead.
3. They are solids with a definite volume and shape under normal conditions.
4. They have a definite and consistent chemical composition throughout, like galena (PbS).
5. They have a crystalline atomic structure with atoms arranged in repeating patterns, like NaCl.
Minerals are naturally occurring inorganic solids that have a crystalline structure and definite chemical composition. All minerals must form naturally, be inorganic, solid, and crystalline in structure. Minerals can be identified based on their physical properties, including color, luster, streak, hardness, and whether they exhibit cleavage or fracture.
This document provides information about minerals, including their formation, composition, properties, and crystal structures. It discusses how minerals are the building blocks of rocks and are made up of arrangements of atoms. There are over 2,500 known mineral types that are classified based on their chemical composition and crystalline structure. Common properties described for identifying minerals include color, streak, luster, hardness, cleavage, and crystal shape.
Minerals are naturally occurring inorganic solids with definite chemical compositions and ordered atomic structures. They form through natural geological processes on or inside Earth. Key properties used to identify minerals include hardness, luster, specific gravity, streak, and cleavage/fracture. Minerals have many important uses beyond gems, including as sources of useful elements like iron, aluminum, and titanium that are integral to infrastructure, transportation, and technology.
This document provides information on minerals, rocks, and their properties. It defines minerals as naturally occurring solid materials with a defined chemical composition and internal structure. The most common elements in Earth's crust are oxygen, silicon, aluminum, iron, calcium, sodium, and potassium. Minerals are divided into silicate and non-silicate groups. Key silicate minerals include quartz, feldspar, mica, amphibole, pyroxene, olivine, and garnet. Non-silicates include carbonates, oxides, sulfides, phosphates, and native elements. Physical properties used to identify minerals include color, streak, luster, hardness, crystal shape, cleavage, fracture, and specific
The document discusses minerals and their properties. It defines minerals as inorganic, solid, naturally occurring substances with defined chemical compositions. It then lists 13 common mineral properties including crystal form, luster, color, streak, hardness, cleavage, specific gravity, taste, touch, magnetism, magnification, smell, and chemical reactions. It also outlines the 7 main mineral groups and provides examples of minerals within each group, which include silicates, carbonates, halides, native elements, sulfates, sulfides, and oxides.
Properties of minerals can be used to identify them, including color, luster, streak, cleavage, fracture, hardness, specific gravity, acid test, crystals, and special properties. Color is not always reliable since many minerals can be the same color or a mineral can come in different colors. A mineral's luster refers to how it shines and can be metallic, non-metallic, vitreous, or pearly. Hardness is measured on Mohs scale from 1 to 10 based on which materials can scratch the mineral. Special properties include traits like magnetism, radioactivity, or fluorescence under UV light that are unique to certain minerals.
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This presentation explores the key properties that define minerals, crucial components of Earth's crust. It covers the fundamental characteristics used to identify and classify minerals, such as hardness, luster, color, streak, cleavage, fracture, and specific gravity. The presentation also discusses how these properties relate to the mineral's internal structure and composition.
The document defines minerals as natural, inorganic, crystalline solids with a definite chemical composition. It describes the key physical properties of minerals - color, streak, hardness, cleavage, fracture, and luster - which are used to identify different minerals. Special properties like magnetism, fluorescence, and piezoelectricity are also discussed. Identification tests involving hardness, streak, and acid reactions are presented as ways to determine the type of mineral.
1) The document is a report on mineralogy presented to an Earth Science professor at Technological University of the Philippines by Hannah Joy N. Lontayao.
2) It defines minerals and rocks, and explains that minerals have definite chemical compositions and atomic structures while rocks are combinations of minerals.
3) The report describes several properties of minerals including crystal form, luster, color, streak, hardness, cleavage, fracture, and specific gravity. It also discusses the seven main mineral groups.
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Gems aren't just pretty faces; they've got science behind them. From the geological birth of gems in igneous, metamorphic, and sedimentary rocks to their chemical makeup, we've uncovered the secrets that make each stone unique. Ever wondered how a diamond gets its sparkle? It's all in the dispersion, folks!
But it's not just about looks; we're talking physical properties too. From thermal conductivity that makes diamonds feel cool to the touch to the electrostatic magic that makes amber cling to your sweater, these stones have tricks up their sleeves.
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CHARACTERISTICS OF MINERALS AND THEIR PROPERTIES.ppt
2. WHAT IS A MINERAL?
? A MINERAL IS A:
?SOLID
?NATURALLY OCCURING (made up
of elements)
?INORGANIC
?CRYSTAL SHAPE (unique to the
mineral)
?CHEMICAL COMPOSITION
(elements bond together to make a
compound)
3. WHAT DOES THAT MEAN?
? Naturally Occurring = NOT man-made
? Inorganic = NOT made of/from a living thing
? Crystal Shape = Repeating pattern of atoms
? Chemical Composition = chemical formula
? Ex: Quartz has a chemical formula of SiO2
4. NOT A MINERAL?
COAL IS NOT A
MINERAL, WHY?
It is not inorganic
because it formed
from the remains of
living organisms
It does not have a
crystal shape
5. NOT A MINERAL?
? PEARL IS ALSO NOT A MINERAL, WHY?
Pearls are organic
because they are
made from
oysters.
They do not have a
crystal shape
6. NOT A MINERAL?
? GLASS IS ALSO NOT A MINERAL, WHY?
Glass does not
a crystal shape.
7. NOT A MINERAL?
? STEEL IS ALSO NOT A MINERAL, WHY?
1: It is man-made (not naturally occurring)
2: It does not have a chemical composition
because it is a mixture of iron and carbon
3: It does not have a crystal shape
8. ¡°Diamonds are Forever¡± Reading
? Before you Read:
? Review the definition of a mineral (SNICC)
? After you Read:
? Answer these questions:
¡ð Can the LifeGem diamonds be considered true minerals?
Explain your answer.
¡ð How are these diamonds different than diamonds mined
out of the ground?
¡ð Would you want to use this company for yourself or for a
relative?
9. TWO GROUPS OF MINERALS
Silicate Minerals Nonsilicate Minerals
?Have both Silicon (Si) and
Oxygen (O) elements in them
?Make up more than 90% of
Earth¡¯s crust
?Might have other elements in
them as well
?Examples: Quartz (SiO2)
Talc Mg3Si4O10(OH)2
?Do NOT contain Silicon and
Oxygen
? Dividing into different classes
depending on elements in them
?Examples: Copper (Cu)
Calcite (CaCO3)
Galena (PbS)
http://www.mineralogy4kids.org/groups.html
13. 2. HARDNESS
? The ability of a mineral to resist
being scratched.
? Relative to the hardness of other
minerals and objects
? 2 scales
?Field hardness scale
?Moh¡¯s hardness scale
19. 4. STREAK
? Powdered residue left behind when
rubbed across a porcelain tile
? Only works for minerals with a hardness
less than 7 (tile=7)
? Streak may be different than outer color
? More consistent/reliable than color
20. 5. CLEAVAGE
? The breaking of a mineral
along flat surfaces
? Can be 1,2, or 3 directional
? 3 Directions: Similar to
sides of a cube or rhombus
Mica breaks into single sheets- 1 Directional
21. 6. FRACTURE
? Breaking of a mineral
in an uneven or
jagged fashion
? ¡°Splintery¡±-splits like
wood
? ¡°Earthy¡±/Uneven
? ¡°Conchoidal¡±-curved
? ¡°Fibrous¡±- like fibers
22. 7. DENSITY
? = Mass per volume (g/mL)
? Every mineral has its own
unique density, regardless of its
size
¡ð Ex: The density of any piece of gold
will always be 19 g/mL
The density of any piece of silver
will always be 10.5 g/mL