Minerals / Common Rock-forming Minerals and their Physical and Chemical Prope...Simple ABbieC
Department of Education | Senior High School
Topic: Minerals / Common Rock-forming Minerals and their Physical and Chemical Properties
Learning Competency:
Earth and Life Science: Identify common rock-forming minerals using their physical and chemical properties.
Earth Science (for STEM): Identify common rock-forming minerals using their physical and chemical properties.
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Minerals / Common Rock-forming Minerals and their Physical and Chemical Prope...Simple ABbieC
Department of Education | Senior High School
Topic: Minerals / Common Rock-forming Minerals and their Physical and Chemical Properties
Learning Competency:
Earth and Life Science: Identify common rock-forming minerals using their physical and chemical properties.
Earth Science (for STEM): Identify common rock-forming minerals using their physical and chemical properties.
Please LIKE / FOLLOW and SHARE my other social media accounts.
Facebook: https://www.facebook.com/Simple-ABbieC-131584525051378/
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Youtube:
http://tiny.cc/SimpleABbieC
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Slideshare:
https://www.slideshare.net/AbbieMahinay
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Blogger:
https://simpleabbiec.blogspot.com/?m=1
The six minerals amphibole, feldspar, mica, olivine, pyroxene, and quartz are the most common rock-forming minerals and are used as important tools in classifying rocks, particularly igneous rocks. This document provides an overview of the six commonest rock-forming minerals.
Rocks and Minerals
A mineral is a naturally occurring inorganic compound with a unique chemical structure and physical properties.
A rock is a solid, stony mass composed of a combination of minerals or other organic compounds.
For example, quartz and feldspars are minerals, but when formed together, they make a rock, granite”
To determine if an Earth rock is a mineral, it should exhibit the following characteristics
Naturally occurring
Inorganic
Can be represented by a chemical formula
Crystalline structure
Solid
Most minerals form by inorganic processes but some, identical in all respects to inorganically formed minerals, are produced by organic processes
Transparency describes how well light passes through a mineral sample
There are three degrees of transparency: transparent, translucent, and opaque.
Habit of a mineral may be define as the size and shape of the crystal, and the structure of form shown by the crystal.
1. Accicular minerals showing needle like crystal. E.g. natrolite
2. Fibrous minerals showing an aggregate of long thin fibers. E.g. Asbestos
3. Tabular minerals showing bladed habit occur as small knife blades. E.g. Kyanite
4. Granular minerals which occur as aggregate of equidimensional grains. E.g. chromites
5. Pisolitic minerals which occur as aggregate of rounded grains of a pea size. E.g. oolite
6. Columnar minerals showing columnar crystal. E.g. tourmaline
Minerals strength determines how easy the mineral breaks or deforms when exposed to stress.
Reaction with Acid. Some minerals, especially carbonate minerals, react visibly with acid. (Usually, a dilute hydrochloric acid [HCl] is used.)
When a drop of dilute hydrochloric acid is placed on calcite, it readily bubbles or effervesces, releasing carbon dioxide
The six minerals amphibole, feldspar, mica, olivine, pyroxene, and quartz are the most common rock-forming minerals and are used as important tools in classifying rocks, particularly igneous rocks. This document provides an overview of the six commonest rock-forming minerals.
Rocks and Minerals
A mineral is a naturally occurring inorganic compound with a unique chemical structure and physical properties.
A rock is a solid, stony mass composed of a combination of minerals or other organic compounds.
For example, quartz and feldspars are minerals, but when formed together, they make a rock, granite”
To determine if an Earth rock is a mineral, it should exhibit the following characteristics
Naturally occurring
Inorganic
Can be represented by a chemical formula
Crystalline structure
Solid
Most minerals form by inorganic processes but some, identical in all respects to inorganically formed minerals, are produced by organic processes
Transparency describes how well light passes through a mineral sample
There are three degrees of transparency: transparent, translucent, and opaque.
Habit of a mineral may be define as the size and shape of the crystal, and the structure of form shown by the crystal.
1. Accicular minerals showing needle like crystal. E.g. natrolite
2. Fibrous minerals showing an aggregate of long thin fibers. E.g. Asbestos
3. Tabular minerals showing bladed habit occur as small knife blades. E.g. Kyanite
4. Granular minerals which occur as aggregate of equidimensional grains. E.g. chromites
5. Pisolitic minerals which occur as aggregate of rounded grains of a pea size. E.g. oolite
6. Columnar minerals showing columnar crystal. E.g. tourmaline
Minerals strength determines how easy the mineral breaks or deforms when exposed to stress.
Reaction with Acid. Some minerals, especially carbonate minerals, react visibly with acid. (Usually, a dilute hydrochloric acid [HCl] is used.)
When a drop of dilute hydrochloric acid is placed on calcite, it readily bubbles or effervesces, releasing carbon dioxide
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Artificial Intelligence (AI) technologies such as Generative AI, Image Generators and Large Language Models have had a dramatic impact on teaching, learning and assessment over the past 18 months. The most immediate threat AI posed was to Academic Integrity with Higher Education Institutes (HEIs) focusing their efforts on combating the use of GenAI in assessment. Guidelines were developed for staff and students, policies put in place too. Innovative educators have forged paths in the use of Generative AI for teaching, learning and assessments leading to pockets of transformation springing up across HEIs, often with little or no top-down guidance, support or direction.
This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
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Safalta Digital marketing institute in Noida, provide complete applications that encompass a huge range of virtual advertising and marketing additives, which includes search engine optimization, virtual communication advertising, pay-per-click on marketing, content material advertising, internet analytics, and greater. These university courses are designed for students who possess a comprehensive understanding of virtual marketing strategies and attributes.Safalta Digital Marketing Institute in Noida is a first choice for young individuals or students who are looking to start their careers in the field of digital advertising. The institute gives specialized courses designed and certification.
for beginners, providing thorough training in areas such as SEO, digital communication marketing, and PPC training in Noida. After finishing the program, students receive the certifications recognised by top different universitie, setting a strong foundation for a successful career in digital marketing.
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
2. What is a Mineral?
The building block of rocks
Naturally occurring (versus synthetic)
Inorganic (no C-H bonds)
Solid (ice is a mineral then, but water is not)
3. What is a Mineral?
Chemical composition & crystalline structure
are the two most important properties of a
mineral
Elements
fundamental component of matter
Cannot be broken down by ordinary means
88 naturally occurring elements in Earth’s
crust
4. Elements of the Earth
8 elements make up
98% of Earth’s crust
Oxygen
Silicon
Aluminum
Iron
Calcium
Magnesium
Potassium
Sodium
5. Elements of the Earth
Some few elements ARE minerals (eg: gold)
Most are comprised of 2 to 5 elements
Held together by + / - electrical charges
Many can vary a little is components
88 elements form over 3,500 minerals
9 rock-forming mineral groups
6. Crystals: the crystalline
nature of minerals
Crystal – any substance whose atoms are
arranged in a periodic, repeating pattern
This pattern is crystalline structure
Unit cell – the smallest group of atoms making up
the unique pattern
Crystal face – flat surface occurring when a
crystal grows freely
Reflects light
Bonding creates crystal structure
9. Physical properties of minerals
Crystal habit
the way crystals aggregate
Cleavage
Some minerals tend to break along flat surfaces
Fracture
The way a mineral breaks other than cleavage
10. Physical properties of minerals
Hardness – Moh’s scale
1 to 10, based on
minerals
Specific gravity
Density relative to water
Color
Obvious, but limited use
Streak
Color of fine powder
Luster
The manner it reflects
light
“Other” properties
11. Mineral classes and
rock-forming minerals
Silicates
Carbonates
Sulfides
Sulfates
Native elements
Halides
Oxides
Hydroxides
Phosphates
12. Mineral classes and
rock-forming minerals
Silicates
Most abundant rock-
forming minerals
Carbonates
Form many sedimentary
rocks
Phosphates
Turquoise
Hydroxides
Bauxite
Halides
Table Salt
Sulfates
Gypsum
Sulfides
Pyrite
Oxides
Hematite
Native Elements
Gold, Silver
14. Igneous
Intrusive (inside)
Cool slowly
Forms from molten
magma
Has visible (large)
crystals
Ex: granite/quartz
Extrusive (outside)
Cool quickly
Forms from lava
Has invisible (small)
crystals
Ex:
basalt/pumice/Rhyolite
Formed from cooling magma
15. Metamorphic
(large – change)
Formed by heat and pressure (physical) OR
By chemical changes which occur through
reaction between rock and outside chemical
Two types of metamorphism:
Contact and regional
Contact happens under the surface when magma
intrudes into the rock
Regional happens on the surface from intense heat and
pressure usually during mountain building
17. Metamorphic
Two types form different characteristics
Foliated have visible bands
Ex: gneiss and slate
Non-Foliated have no visible bands
marble
18. Sedimentary
Formed from Sediment
created by weathering and
erosion of existing rocks
which is then compacted
and cemented
Weathering and erosion
Particles, altered, or dissolved
materials
Transported and deposited
Compaction
Lithification (“glueing”
together)
Four Types
Clastic
Chemical
Organic
Bioclastic
20. Chemical
Formed by Chemical
Processes
Evaporation
Solid forms when
water is evaporated
Halite (salt)/Gypsum
Precipitate
Forms when two
liquids are mixed
limestone
21. Bioclastic
Are formed from
living organisms
shell fragments
Hard-shelled
organisms
Clams, corals, oysters,
etc.
Carbonate skeletons
22. Organic
Formed from living
organisms -
plants/animals
Coal made from
plants
Limestone made
from shells