I learned many things about natural science that formed the earth, It took time to create beautiful forms of rocks and minerals that we can treasure and take care of .
Minerals
There are Over 100 Elements are the basic building blocks of
minerals.
Atoms
Smallest particles of matter
Have all the characteristics of an element
The nucleus is the central part of an atom and
contains
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protons, which have positive electrical charges
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neutrons, which have neutral electrical charges
Energy levels, or shells
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surround the nucleus
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contain
electrons—negatively charged particles
The atomic number is the number of protons in the nucleus of an atom.
Atoms Bond when an atom’s outermost energy level does not contain the maximum number of
electrons, the atom is likely to form a chemical bond with one or more
atoms.
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A compound consists of two or more
elements that are chemically combined in specific proportions.
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An
ion is an atom that gains or loses electrons.
The Three Types of Chemical Bonds are Ionic bonds form between positive and
negative ions, Covalent bonds form when atoms share
electrons and Metallic bonds form when metal ions
share electrons.
Mineral is:
1. Naturally occurring
2. Solid substance
3. Orderly crystalline structure
4. Definite chemical composition
5. Generally considered inorganic
Minerals Form by
1. Crystallization from magma
2. Precipitation
3. Pressure and temperature
4. Hydrothermal solutions
Mineral Groups
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1. Silicates
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Silicon and oxygen combine to form a structure
called the silicon-oxygen tetrahedron. This silicon-oxygen tetrahedron
provides the framework of every silicate mineral.
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2. Carbonates
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Minerals that contain the elements carbon,
oxygen, and one or more other metallic elements
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3. Oxides
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Minerals that contain oxygen and one or more
other elements, which are usually metals
4. Sulfates and Sulfides
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Minerals that contain the element sulfur
5. Halides
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Minerals that contain a halogen ion plus one or
more other elements
6. Native elements
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Minerals that exist in relatively pure form
There are different Properties of mineral that helps us know their characteristics like:
Color
Small amounts of different elements can give the same mineral different colors.
• Streak
Streak is the color of a mineral in its powdered form.
Luster
Luster is used to describe how light is reflected from the surface of a
mineral.
Crystal Form
Crystal form is the visible expression
of a mineral’s internal arrangement of atoms.
of a mineral’s internal arrangement of atoms.
Hardness
Hardness is a measure of the resistance of a mineral to being scratched.
Mohs scale consists of 10 minerals arranged from 10 (hardest) to 1
(softest).
Cleavage
Cleavage is the tendency of a mineral to cleave, or break, along flat,
even surfaces.
Fracture
Minerals that do not show cleavage when broken are said to fracture.
Fracture—the uneven breakage of
a mineral
a mineral
Density
Density is a property of all matter that
is the ratio of an object’s mass to its volume.
is the ratio of an object’s mass to its volume.
Distinctive Properties of Minerals
Some minerals can be recognized by other distinctive properties.
Rocks
Rocks are any solid mass of mineral or mineral-like matter occurring
naturally as part of our planet.
Types of Rocks
1. Igneous rock is formed by the
crystallization of molten magma.
2. Sedimentary rock is formed from the
weathered products of preexisting rocks that have been transported, deposited,
compacted, and cemented.
3. Metamorphic rock is formed by
the alteration of pre-existing rock deep within Earth (but still in the solid
state) by heat, pressure, and/or chemically active fluids.
The Rock Cycle
Shows the interrelationships among the three rock types (igneous, sedimentary,
and metamorphic)
Magma is molten material that forms deep beneath the Earth’s surface.
Lava is magma that reaches the surface.
Weathering is a process in which rocks are broken down by water, air,
and living things.
Sediment is weathered pieces of Earth elements.
Energy That Drives the Rock Cycle
Processes driven by heat from the Earth’s interior are responsible for forming
both igneous rock and metamorphic rock.
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Weathering and the movement of weathered materials are external processes
powered by energy from the sun.
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External processes produce sedimentary rocks.
Formation of Igneous Rocks
1. Intrusive igneous rocks are formed
when magma hardens beneath Earth’s surface.
2. Extrusive igneous rocks are formed
when lava hardens.
Classification of Igneous Rocks
Igneous rocks can be classified based on their composition and texture.
Coarse-grained texture is caused by slow cooling resulting in larger
crystals.
1. Texture
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Fine-grained texture is caused by rapid cooling resulting in smaller,
interconnected mineral grains.
2. Composition
• Granitic
composition rocks are made mostly
of light-colored quartz and feldspar.
of light-colored quartz and feldspar.
Formation of Metamorphic Rocks
Metamorphism means “to change form.”
Most metamorphic changes occur at elevated temperatures and pressures.
Conditions for formation are found a few kilometers below the Earth’s surface
and extend into the upper mantle.
Classification of Metamorphic
Rocks
Two main categories
1. Foliated Metamorphic Rock
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Has a banded or layered appearance
2. Nonfoliated Metamorphic Rock
Does not have a banded texture
We watched videos about minerals and rocks that shows the different colors of it and there different classifications
