This document provides information about common rock-forming minerals. It discusses the composition, properties and occurrence of silicate minerals like quartz, feldspar, mica, amphibole and pyroxene. It also covers the carbonate mineral calcite and the silicate mineral olivine. These minerals are important components of igneous, metamorphic and sedimentary rocks.
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 summarizes several major clay minerals including kaolinite, illite, and smectites. It then discusses the structures of phyllosilicates including their tetrahedral and octahedral layers. Specific examples of kaolinite, serpentine, and 2:1 clays are provided. The document also briefly discusses carbonate minerals of the calcite, dolomite, and aragonite groups. Finally, it summarizes common sulfate minerals like gypsum, halide minerals such as halite, and oxide minerals including iron oxides.
This document provides an overview of minerals and mining. It discusses the purpose of the lesson, defines what minerals are, and describes the various types of mineral deposits that can form through igneous, hydrothermal, metamorphic, sedimentary, weathering, and placer processes. The document also outlines different mineral classification systems and properties used to identify minerals such as streak, luster, crystal form, hardness, cleavage, and fracture. Mineral extraction methods and the economic and environmental impacts of mining are also summarized.
Minerals and rocks can be identified by their physical and chemical properties. A mineral has definite properties including being naturally occurring, inorganic, solid, having a definite chemical composition and crystal structure. There are several types of rocks including sedimentary, igneous, and metamorphic rocks which are classified based on their formation. Sedimentary rocks form from the accumulation and cementation of sediments and can be clastic, chemical, or organic. Igneous rocks form from the cooling of magma and include extrusive volcanic and intrusive plutonic rocks. Metamorphic rocks form from the alteration of existing rocks through heat, pressure, and chemical changes in the Earth's crust.
Minerals and rocks can be identified based on their physical and chemical properties. A mineral is defined as a naturally occurring, inorganic solid with a definite chemical composition and crystal structure. Minerals may form from the cooling of lava or magma, or from chemical or physical changes to existing rocks. Rocks are composed of one or more minerals and can be classified as sedimentary, igneous, or metamorphic based on their formation process. The identification of a material as a mineral or rock involves testing its properties, such as hardness, crystal structure, or chemical reactivity.
This document provides information about minerals, including their characteristics, formation, and classification. It discusses that all minerals are naturally formed solids with a crystal structure, have a unique chemical makeup, and are made up of particles arranged in repeating patterns. Minerals are grouped based on their elemental composition, with the main groups being silicates, carbonates, sulfates, and oxides. Minerals form through the cooling of magma underground or from elements dissolving in water. They have many uses in everyday life.
Cation and Anion s and Onions hehehe the morning 🌄🌄🌅 I have to your house and you can do it you can do it you can do it you can do it you can do it you can do it to do in a Day the same time as the other day I was reflected in this is the key to the voice of the martyrs to get real talk 🦜 I have no idea what do you want to go to bed now I love you y
This document provides information about common rock-forming minerals. It discusses the composition, properties and occurrence of silicate minerals like quartz, feldspar, mica, amphibole and pyroxene. It also covers the carbonate mineral calcite and the silicate mineral olivine. These minerals are important components of igneous, metamorphic and sedimentary rocks.
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 summarizes several major clay minerals including kaolinite, illite, and smectites. It then discusses the structures of phyllosilicates including their tetrahedral and octahedral layers. Specific examples of kaolinite, serpentine, and 2:1 clays are provided. The document also briefly discusses carbonate minerals of the calcite, dolomite, and aragonite groups. Finally, it summarizes common sulfate minerals like gypsum, halide minerals such as halite, and oxide minerals including iron oxides.
This document provides an overview of minerals and mining. It discusses the purpose of the lesson, defines what minerals are, and describes the various types of mineral deposits that can form through igneous, hydrothermal, metamorphic, sedimentary, weathering, and placer processes. The document also outlines different mineral classification systems and properties used to identify minerals such as streak, luster, crystal form, hardness, cleavage, and fracture. Mineral extraction methods and the economic and environmental impacts of mining are also summarized.
Minerals and rocks can be identified by their physical and chemical properties. A mineral has definite properties including being naturally occurring, inorganic, solid, having a definite chemical composition and crystal structure. There are several types of rocks including sedimentary, igneous, and metamorphic rocks which are classified based on their formation. Sedimentary rocks form from the accumulation and cementation of sediments and can be clastic, chemical, or organic. Igneous rocks form from the cooling of magma and include extrusive volcanic and intrusive plutonic rocks. Metamorphic rocks form from the alteration of existing rocks through heat, pressure, and chemical changes in the Earth's crust.
Minerals and rocks can be identified based on their physical and chemical properties. A mineral is defined as a naturally occurring, inorganic solid with a definite chemical composition and crystal structure. Minerals may form from the cooling of lava or magma, or from chemical or physical changes to existing rocks. Rocks are composed of one or more minerals and can be classified as sedimentary, igneous, or metamorphic based on their formation process. The identification of a material as a mineral or rock involves testing its properties, such as hardness, crystal structure, or chemical reactivity.
This document provides information about minerals, including their characteristics, formation, and classification. It discusses that all minerals are naturally formed solids with a crystal structure, have a unique chemical makeup, and are made up of particles arranged in repeating patterns. Minerals are grouped based on their elemental composition, with the main groups being silicates, carbonates, sulfates, and oxides. Minerals form through the cooling of magma underground or from elements dissolving in water. They have many uses in everyday life.
Cation and Anion s and Onions hehehe the morning 🌄🌄🌅 I have to your house and you can do it you can do it you can do it you can do it you can do it you can do it to do in a Day the same time as the other day I was reflected in this is the key to the voice of the martyrs to get real talk 🦜 I have no idea what do you want to go to bed now I love you y
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.
This document provides an overview of minerals, their composition and structure. It discusses that minerals are naturally occurring inorganic solids with definite chemical compositions and ordered internal structures. It describes the basic building blocks of minerals including elements, atoms, and different types of chemical bonding. It also summarizes the different physical properties used to identify minerals such as crystal form, luster, color, cleavage, fracture and hardness. Finally, it outlines some of the major mineral groups found in Earth's crust including silicates, carbonates, oxides, sulfides and others.
This document provides a summary of the contents of a lecture on minerals. It discusses the definition of a mineral, classification of minerals into rock-forming and ore-forming groups. It also describes various mineral properties that can be used for identification such as color, streak, hardness, cleavage, luster, and explains systems for classifying minerals based on these properties. Common rock-forming minerals and their characteristics are also outlined.
This document discusses key concepts in sedimentary petrology including the study of sedimentary rock characteristics, origins, and the processes involved in their formation. It describes how sedimentary rocks record information about sediment source, transport mechanisms, depositional environment, and post-depositional changes. Identification is based on composition and texture. Major rock types include siliclastic, volcaniclastic, and various carbonate rocks. Weathering of rocks produces sediment which is transported and deposited, becoming lithified over time into sedimentary rocks.
The document discusses minerals and their characteristics. It defines a mineral as a naturally occurring, inorganic solid with a definite chemical composition and crystalline structure. Minerals are the building blocks of rocks and are studied by mineralogists. The document outlines the key characteristics minerals must have and describes different types of minerals including silicate and non-silicate minerals. It also discusses how minerals form and can be identified based on their physical properties such as color, streak, luster, hardness, cleavage/fracture, and density.
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.
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
Igneous rock forms when hot liquid rock called magma cools. When the magma cools below the Earth's surface it cools slowly forming large crystals and is known as an intrusive igneous rock e.g. granite (pictured to the right). When magma reaches the Earth's surface, usually through a volcano, it is called lava and it cools quickly, rocks formed by this process are known as extrusive igneous rock e.g. basalt.
Igneous rocks may have been metamorphic or sedimentary rocks before melted and reforming magma.
We have many granite bodies exposed at the surface in Ireland including the Leinster and Galway Granites. They formed below the surface of the earth but where brought to the surface either through erosion of the overlying material or due to the movement of faults.
This document provides information about minerals and rocks. It defines a mineral as a naturally occurring, inorganic solid with a definite chemical composition and crystal structure. It describes the different types of rocks, including sedimentary rocks which form from the accumulation of sediments, igneous rocks which form from the cooling of magma, and metamorphic rocks which form from the alteration of existing rocks due to heat and pressure. The document also discusses the physical and chemical properties used to identify minerals, as well as how minerals are used and the relationship between minerals and rocks.
Soil Forming Rocks and Minerals ClassificationDINESH KUMAR
This document discusses the classification of rocks and minerals. It describes three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma, sedimentary rocks form through the accumulation and cementation of sediments, and metamorphic rocks form from alterations to existing rocks by heat, pressure, and chemically active fluids. Within each rock type are various sub-classifications. The document also examines the classification of important rock-forming minerals and describes their structures, weathering properties, and physical characteristics.
Minerals are naturally occurring inorganic substances with a crystalline structure. They make up many aspects of our lives and humans need at least 16 minerals to survive, though they comprise just 0.03% of our diet. Minerals form in various ways including cooling of magma, evaporation, and hydrothermal processes. The most abundant minerals on Earth are silicates and oxides of silicon and oxygen, which compose 70% of the Earth's crust and are the building blocks of most rocks. Minerals can be identified by their physical properties such as crystal structure, cleavage, fracture, color, hardness, luster, and streak.
Extraction of metals involves several key steps: (1) crushing and grinding ore into a powder, (2) concentrating the ore to remove unwanted materials like sand and clay, (3) preliminary treatments like calcination and roasting, (4) reducing the concentrated ore using methods like smelting or electrolysis to extract the pure metal, and (5) refining the crude metal through processes like distillation, liquation, or electrolytic refining to achieve high purity. The overall process of extracting pure metal from its ore is known as metallurgy.
The document discusses minerals found in the Earth's crust. It describes that minerals exist as either natural elements or compounds, with examples like gold and limestone provided. Key properties of minerals that are described include their hardness, solubility in water, and how they are affected by heat. In particular, it notes that most minerals are insoluble in water, and that metal oxides are stable under heat while sulphides and carbonates will break down into other substances when heated.
This lesson discusses what minerals and rocks are. It tackles various types of minerals and rocks. It discusses the rock cycle and how it produces the different kinds of rocks on our planet.
India has a variety of economically important mineral resources. The major minerals produced in India are iron-ore, bauxite, mica, coal, and petroleum. Iron-ore accounts for nearly two-thirds of the total value of metallic minerals produced in India and is one of the country's most important exports. Other important minerals include bauxite, mica, coal deposits which are majorly found in states like Bihar and West Bengal, and petroleum from regions like Assam. Mineral resources play a vital role in India's industrial development and economic progress.
This document discusses minerals, their properties, and types. It defines a mineral as a naturally occurring inorganic substance with a definite chemical composition and atomic structure. Minerals are divided into rock-forming and ore-forming types. Rock-forming minerals are common in Earth's crust while ore-forming minerals have economic value. Common rock-forming mineral groups include oxides, carbonates, sulphides, sulphates, chlorides, and silicates. The document outlines several physical properties used to identify minerals, such as color, streak, luster, hardness, cleavage, and fracture. It also explains Mohs hardness scale and provides examples of different luster and fracture types.
This is a powerpoint presentation that is about one of the Senior High School Core Subject: Earth and Life Science. It is composed of the definition and the properties of the different classification of minerals.
This document provides an overview of minerals, rocks, and energy resources related to the lithosphere and hydrosphere. It defines minerals as naturally occurring inorganic substances with distinct compositions and structures. It describes how minerals are classified based on properties like color, transparency, hardness, and streak. It also discusses the formation and classification of different rock types. Finally, it examines various energy resources derived from the lithosphere and hydrosphere, including fossil fuels, uranium, geothermal, hydropower, and renewable sources.
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.
This document provides an overview of minerals, their composition and structure. It discusses that minerals are naturally occurring inorganic solids with definite chemical compositions and ordered internal structures. It describes the basic building blocks of minerals including elements, atoms, and different types of chemical bonding. It also summarizes the different physical properties used to identify minerals such as crystal form, luster, color, cleavage, fracture and hardness. Finally, it outlines some of the major mineral groups found in Earth's crust including silicates, carbonates, oxides, sulfides and others.
This document provides a summary of the contents of a lecture on minerals. It discusses the definition of a mineral, classification of minerals into rock-forming and ore-forming groups. It also describes various mineral properties that can be used for identification such as color, streak, hardness, cleavage, luster, and explains systems for classifying minerals based on these properties. Common rock-forming minerals and their characteristics are also outlined.
This document discusses key concepts in sedimentary petrology including the study of sedimentary rock characteristics, origins, and the processes involved in their formation. It describes how sedimentary rocks record information about sediment source, transport mechanisms, depositional environment, and post-depositional changes. Identification is based on composition and texture. Major rock types include siliclastic, volcaniclastic, and various carbonate rocks. Weathering of rocks produces sediment which is transported and deposited, becoming lithified over time into sedimentary rocks.
The document discusses minerals and their characteristics. It defines a mineral as a naturally occurring, inorganic solid with a definite chemical composition and crystalline structure. Minerals are the building blocks of rocks and are studied by mineralogists. The document outlines the key characteristics minerals must have and describes different types of minerals including silicate and non-silicate minerals. It also discusses how minerals form and can be identified based on their physical properties such as color, streak, luster, hardness, cleavage/fracture, and density.
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.
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
Igneous rock forms when hot liquid rock called magma cools. When the magma cools below the Earth's surface it cools slowly forming large crystals and is known as an intrusive igneous rock e.g. granite (pictured to the right). When magma reaches the Earth's surface, usually through a volcano, it is called lava and it cools quickly, rocks formed by this process are known as extrusive igneous rock e.g. basalt.
Igneous rocks may have been metamorphic or sedimentary rocks before melted and reforming magma.
We have many granite bodies exposed at the surface in Ireland including the Leinster and Galway Granites. They formed below the surface of the earth but where brought to the surface either through erosion of the overlying material or due to the movement of faults.
This document provides information about minerals and rocks. It defines a mineral as a naturally occurring, inorganic solid with a definite chemical composition and crystal structure. It describes the different types of rocks, including sedimentary rocks which form from the accumulation of sediments, igneous rocks which form from the cooling of magma, and metamorphic rocks which form from the alteration of existing rocks due to heat and pressure. The document also discusses the physical and chemical properties used to identify minerals, as well as how minerals are used and the relationship between minerals and rocks.
Soil Forming Rocks and Minerals ClassificationDINESH KUMAR
This document discusses the classification of rocks and minerals. It describes three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma, sedimentary rocks form through the accumulation and cementation of sediments, and metamorphic rocks form from alterations to existing rocks by heat, pressure, and chemically active fluids. Within each rock type are various sub-classifications. The document also examines the classification of important rock-forming minerals and describes their structures, weathering properties, and physical characteristics.
Minerals are naturally occurring inorganic substances with a crystalline structure. They make up many aspects of our lives and humans need at least 16 minerals to survive, though they comprise just 0.03% of our diet. Minerals form in various ways including cooling of magma, evaporation, and hydrothermal processes. The most abundant minerals on Earth are silicates and oxides of silicon and oxygen, which compose 70% of the Earth's crust and are the building blocks of most rocks. Minerals can be identified by their physical properties such as crystal structure, cleavage, fracture, color, hardness, luster, and streak.
Extraction of metals involves several key steps: (1) crushing and grinding ore into a powder, (2) concentrating the ore to remove unwanted materials like sand and clay, (3) preliminary treatments like calcination and roasting, (4) reducing the concentrated ore using methods like smelting or electrolysis to extract the pure metal, and (5) refining the crude metal through processes like distillation, liquation, or electrolytic refining to achieve high purity. The overall process of extracting pure metal from its ore is known as metallurgy.
The document discusses minerals found in the Earth's crust. It describes that minerals exist as either natural elements or compounds, with examples like gold and limestone provided. Key properties of minerals that are described include their hardness, solubility in water, and how they are affected by heat. In particular, it notes that most minerals are insoluble in water, and that metal oxides are stable under heat while sulphides and carbonates will break down into other substances when heated.
This lesson discusses what minerals and rocks are. It tackles various types of minerals and rocks. It discusses the rock cycle and how it produces the different kinds of rocks on our planet.
India has a variety of economically important mineral resources. The major minerals produced in India are iron-ore, bauxite, mica, coal, and petroleum. Iron-ore accounts for nearly two-thirds of the total value of metallic minerals produced in India and is one of the country's most important exports. Other important minerals include bauxite, mica, coal deposits which are majorly found in states like Bihar and West Bengal, and petroleum from regions like Assam. Mineral resources play a vital role in India's industrial development and economic progress.
This document discusses minerals, their properties, and types. It defines a mineral as a naturally occurring inorganic substance with a definite chemical composition and atomic structure. Minerals are divided into rock-forming and ore-forming types. Rock-forming minerals are common in Earth's crust while ore-forming minerals have economic value. Common rock-forming mineral groups include oxides, carbonates, sulphides, sulphates, chlorides, and silicates. The document outlines several physical properties used to identify minerals, such as color, streak, luster, hardness, cleavage, and fracture. It also explains Mohs hardness scale and provides examples of different luster and fracture types.
This is a powerpoint presentation that is about one of the Senior High School Core Subject: Earth and Life Science. It is composed of the definition and the properties of the different classification of minerals.
This document provides an overview of minerals, rocks, and energy resources related to the lithosphere and hydrosphere. It defines minerals as naturally occurring inorganic substances with distinct compositions and structures. It describes how minerals are classified based on properties like color, transparency, hardness, and streak. It also discusses the formation and classification of different rock types. Finally, it examines various energy resources derived from the lithosphere and hydrosphere, including fossil fuels, uranium, geothermal, hydropower, and renewable sources.
This document provides an overview of wound healing, its functions, stages, mechanisms, factors affecting it, and complications.
A wound is a break in the integrity of the skin or tissues, which may be associated with disruption of the structure and function.
Healing is the body’s response to injury in an attempt to restore normal structure and functions.
Healing can occur in two ways: Regeneration and Repair
There are 4 phases of wound healing: hemostasis, inflammation, proliferation, and remodeling. This document also describes the mechanism of wound healing. Factors that affect healing include infection, uncontrolled diabetes, poor nutrition, age, anemia, the presence of foreign bodies, etc.
Complications of wound healing like infection, hyperpigmentation of scar, contractures, and keloid formation.
Walmart Business+ and Spark Good for Nonprofits.pdfTechSoup
"Learn about all the ways Walmart supports nonprofit organizations.
You will hear from Liz Willett, the Head of Nonprofits, and hear about what Walmart is doing to help nonprofits, including Walmart Business and Spark Good. Walmart Business+ is a new offer for nonprofits that offers discounts and also streamlines nonprofits order and expense tracking, saving time and money.
The webinar may also give some examples on how nonprofits can best leverage Walmart Business+.
The event will cover the following::
Walmart Business + (https://business.walmart.com/plus) is a new shopping experience for nonprofits, schools, and local business customers that connects an exclusive online shopping experience to stores. Benefits include free delivery and shipping, a 'Spend Analytics” feature, special discounts, deals and tax-exempt shopping.
Special TechSoup offer for a free 180 days membership, and up to $150 in discounts on eligible orders.
Spark Good (walmart.com/sparkgood) is a charitable platform that enables nonprofits to receive donations directly from customers and associates.
Answers about how you can do more with Walmart!"
Level 3 NCEA - NZ: A Nation In the Making 1872 - 1900 SML.pptHenry Hollis
The History of NZ 1870-1900.
Making of a Nation.
From the NZ Wars to Liberals,
Richard Seddon, George Grey,
Social Laboratory, New Zealand,
Confiscations, Kotahitanga, Kingitanga, Parliament, Suffrage, Repudiation, Economic Change, Agriculture, Gold Mining, Timber, Flax, Sheep, Dairying,
Leveraging Generative AI to Drive Nonprofit InnovationTechSoup
In this webinar, participants learned how to utilize Generative AI to streamline operations and elevate member engagement. Amazon Web Service experts provided a customer specific use cases and dived into low/no-code tools that are quick and easy to deploy through Amazon Web Service (AWS.)
A Visual Guide to 1 Samuel | A Tale of Two HeartsSteve Thomason
These slides walk through the story of 1 Samuel. Samuel is the last judge of Israel. The people reject God and want a king. Saul is anointed as the first king, but he is not a good king. David, the shepherd boy is anointed and Saul is envious of him. David shows honor while Saul continues to self destruct.
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...PECB
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
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Training: ISO/IEC 27001 Information Security Management System - EN | PECB
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How to Make a Field Mandatory in Odoo 17Celine George
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
How to Setup Warehouse & Location in Odoo 17 InventoryCeline George
In this slide, we'll explore how to set up warehouses and locations in Odoo 17 Inventory. This will help us manage our stock effectively, track inventory levels, and streamline warehouse operations.
3. RECOMMENDED BOOKS
• No book is recommended as prescription.
• Any relevant book of mineralogy can be used as
reference book.
• Selected chapters compilation is available at junaid
Photoshop, Department of Physics
4. Mineralogy
Scientific discipline that is concerned with all aspects
of minerals:
1. Physical Properties
2. Chemical Composition
3. Crystal Structure
4. Occurrence and Distribution in Nature
5. Origins (physicochemical conditions of formation).
7. THE HISTORY OF MINERALOGY
• The term minera (ore) was introduced by the Italian scientist Bernard Cesi (1581-
1630 AD).
• Mineral world began with the use of stones.
• Stones were used for the most primitive tools of labor and arms.
• Stones were selected based on form, mass and strength.
• Articles made up of silicon, obsidian, chalcedony were of high quality.
• Clay was being used to manufacture pottery.
8. • Bright color stones were used for ornaments and amulets.
• Mineral paints were used for rocks and cave drawings, and
for cosmetic manufacture.
• Some stones were used in food and as medicines.
• In metal age, mining of the ores of gold, silver, copper, tin,
lead, mercury, iron and precious stones developed
9. • Bronze (alloy of Cu and Pb) and Fe were used later for
arms, labor and domestic tools.
• Limestone and sand stones were used as building
material while marble, granite, basalt and quartzite
were used for interior and exterior decoration.
• Baked clay and lead were used for manufacture of
water pipes
10. VARIETIES OF MINERALS
CHEMICAL VARIETY
• Characterized by the presence of additional elements
within certain natural boundaries.
• Sometimes they have their own names.
• E.g. Ferrous Sphalerite or Marmatite
ZnS (Zn,Fe)S
12. STRUCTURAL VARIETY
• Distinguished by some specific features of the crystal
structure, usually with the chemical composition
remaining constant.
• E.g. Right handed and left handed structural forms of
Quartz, Orthoclase/ Sanidine.
14. MORPHOLOGICAL VARIETY
• Posses innately their own shape of individuals or mineral
aggregate. e.g.
• Chalcedony, Cryptocrystalline Quartz.
• Selenite, fibrous variety of Gypsum.
• Serpentine and asbestoses.
17. PHYSICAL VARIETY
• Characterized by specific physical properties mainly
optical, such as transparency and color.
• E.g. Colored: Beryl, Green Emerald, Blue Aquamarine,
Yellow Heliodor.
• Transparent: Quartz, brown-Citrine, colorless-Rock
Crystal, purple- Amethyst, white-Milky.
32. Monoxides (MO)
Rock salt oxides MgO, FeO, MnO, CaO, NiO
Periclase MgO - Wuestite FeO
Manganosite MnO
Lime CaO
Bunsenite NiO
Zincite oxides: zincite ZnO, bromellite BeO
Other monoxides:
TenoriteCuO, MontroyditeHgO
33. Sesquioxides (M2O3)
A sesquioxide is an oxide containing three atoms of oxygen with two
atoms of another element.
Corundum Group
Corundum Al2O3
Hematite Fe2O3
Karelianite V2O3 and Eskolaite Cr2O3
Other Sesquioxides
• – Bixbyite Mn2O3
35. Complex Oxides
Two or more different cations
Spinel Group: M2TO4
Ilmenite Group : FeTiO3
Pseudobrookite Group : A2BO5
Perovskite Group : CaTiO3
High Pressure silicate analogues
49. Phosphates, Tungstates, Vanadates
Phosphates are based on P5+O4 tetrahedron.
By far the most important one is apatite.
Ca5(PO4)3(OH,F,Cl)
Tungstate and Vanadate are based on W6+O4 and V5+O4
tetrahedra.
Some are isostructural with apatite and so included in the
same group, but they are usually considered oxides.
50. Apatite Ca5(PO4)3(OH,F,Cl)
Hydroxy- Fluor-, and Chlor- apatites
Major component of teeth and bone
Common accessory mineral in igneous and metamorphic
rock.
Some sedimentary phosphates (phosphate sands).