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WEEK+26

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Rocks & Minerals
Differentiate between rocks and minerals,
1
objectives
including their characteristics, formation
processes, and geological significance.
2
Describe the formation processes and
characteristics and the rock cycle of major rock
types (igneous, sedimentary, metamorphic) and
the role of minerals in their composition.
3
Apply knowledge of rocks and minerals to solve
real-world problems or make informed decisions
regarding land use, resource management, and
sustainable development.
Activity:
Minerals
Rocks
•
Directions: Come up to the board and write a word, a phrase that pops into your head when
you think about minerals or rocks.
Rocks and minerals are fundamental components of the
Earth's crust and play a crucial role in shaping its
landscape and supporting various life forms.
Rocks are solid natural substances composed of one or more
minerals. They are an essential part of the Earth's crust and have been
integral to the planet's geological processes for billions of years.
IGNEOUS ROCKS
Igneous Rocks: These rocks form
from the cooling and solidification of
molten magma or lava.
GRANITE
Granite is a common type of igneous rock
that forms from the slow crystallization of
magma below the Earth's surface.
DIORITE
Diorite typically has a speckled
appearance due to the
interlocking crystals of its
constituent minerals.
Extrusive Igneous Rocks: Formed on
the Earth's surface as lava cools
quickly, resulting in smaller crystals or
glassy textures.
Basalt is one of the most abundant rock types in the
Earth's crust and can be found in oceanic crust, volcanic
regions, and in some continental areas.
PUMICE
Pumice forms when frothy lava with high gas
content erupts explosively from a volcano.
SEDIMENTARY ROCK
These rocks form through the accumulation
and compaction of sediments, which may
include fragments of other rocks, minerals,
and organic materials.
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ORGANIC SEDIMENTARY
Metamorphic rocks are a type of rock that forms
from the alteration of pre-existing rocks due to
heat, pressure, and/or chemically active fluids.
FOLIATED METAMORHPHIC ROCK
SLATE
Slate is a fine-grained metamorphic
rock that forms from the metamorphism
of shale or mudstone.
FOLIATED METAMORHPHIC ROCK
SCHIST
Schist is a type of metamorphic
rock characterized by its
medium to coarse-grained
texture and pronounced foliation
FOLIATED METAMORHPHIC ROCK
GNEISS
Gneiss is a type of metamorphic rock
characterized by distinct bands or
layers of minerals that have undergone
intense heat and pressure over millions
of years.
FOLIATED METAMORHPHIC ROCK
PHYLLITE
Phyllite is a type of foliated
metamorphic rock that forms from
the metamorphism of shale or slate.
MINERALS
PROPERTIES OF MINERALS
Luster: Appearance of a mineral's surface in reflected light, categorized as metallic, vitreous
(glassy), pearly, silky, or dull.
A "dull mineral" refers to a mineral that lacks the characteristic shiny or reflective appearance
typically associated with metallic minerals or the glassy appearance of vitreous minerals.
Instead, dull minerals have a matte or earthy appearance with little to no luster.
The term "pearly" is used to describe a specific type of luster exhibited by certain minerals.
Pearly luster refers to a soft, subdued sheen that resembles the appearance of a pearl.
A vitreous mineral is a type of mineral that exhibits a glassy or vitreous luster, which means it
has a shiny, reflective surface similar to that of glass. This type of luster is characterized by its
smooth and reflective appearance, often giving the mineral a translucent or transparent quality
when viewed under light.
1.Industrial Applications: Minerals are used in
construction (e.g., limestone, granite), manufacturing
(e.g., iron, aluminum), and energy production (e.g.,
coal, uranium).
2.Gemstones: Precious and semi-precious minerals
like diamonds, rubies, and emeralds are used in jewelry
and decorative items.
3. Agriculture: Minerals like phosphates and
potash are essential components of fertilizers.
4. Technology: Minerals such as silicon, used
in the production of semiconductors, are vital
for electronics and communication devices.
6. Health and Nutrition: Minerals like calcium, iron, and
magnesium are essential for human health, forming the
basis of bones, blood, and various bodily functions.
7. Metallurgy: Many metals are extracted from mineral
ores through processes like smelting, refining, and alloying.
Weathering: This is the process where rocks are broken down into smaller pieces by physical (such
as temperature changes, frost action, and abrasion) and chemical (such as acid rain, oxidation,
and hydrolysis) processes.
Erosion and Transport: Weathered rock fragments are transported by agents such as water, wind,
ice, and gravity. They can be carried over long distances before being deposited elsewhere.
Deposition: The transported rock particles settle and accumulate in new locations, forming
sedimentary deposits.
Lithification: Over time, the accumulated sediments are compacted under pressure and
cemented together by minerals, forming sedimentary rocks.
Metamorphism: If these rocks are subjected to high temperatures and pressures, typically
deep within the Earth's crust, they undergo metamorphism. This process can change their
mineral composition and texture, forming metamorphic rocks.
Melting and Solidification: If rocks are subjected to extreme heat, they may melt to form
magma. This molten material can cool and solidify either beneath the Earth's surface,
forming intrusive igneous rocks, or on the surface, forming extrusive igneous rocks.
Uplift and Exposure: Through tectonic processes like mountain building or erosion, rocks
are uplifted to the Earth's surface and exposed to weathering and erosion again, restarting
the cycle.
Understanding rocks and minerals is crucial for addressing various real-world
challenges related to land use, resource management, and sustainable
development.
Water Resource Management:
Certain rocks and minerals affect
groundwater quality and
availability. For instance, porous
rocks like limestone can act as
aquifers.
RENEWABLE SOURCE DEVELOPMENT
Climate Change Mitigation: Some minerals,
such as olivine, have the potential to sequester
carbon dioxide from the atmosphere through a
process called weathering. Knowledge of these
mineral-carbon interactions can inform strategies
for carbon capture and storage to mitigate
climate change.
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