MINERALS AND ROCKS
Earth Science (Modules 3 and 4)
Christopher Allan F. Reballos, MSc
With your permission, we will be
recording this session form
documentation purposes.
We request that you put your audio
on mute to avoid disruptions during
presentation.
You may turn off your camera during
the presentation
Synchronous Google Meet Class
Questions may be typed in the chat
box and will be answered by the
speaker after the presentation.
MELCs
At the end of the lesson, the student should
be able to:
• Identify common rock-forming minerals,
using their physical and chemical
properties (Module 3)
• Classify rocks into igneous, sedimentary
and metamorphic (Module 4)
Rocks vs Minerals
• Minerals are building blocks of rocks
(Module 3)
• Rocks are any naturally occurring solid
mass of mineral aggregates
(Module 4)
MELCs
At the end of the lesson, the student should
be able to:
• Identify common rock-forming minerals,
using their physical and chemical
properties (Module 3)
• Classify rocks into igneous, sedimentary
and metamorphic (Module 4)
Minerals as Building Blocks
• Minerals may be defined as:
SAN JUAN DE DIOS EDUCATIONAL FOUNDATION, INC.
2772-2774 Roxas Boulevard, Pasay City 1300 Philippines
Hospital - Tel. Nos.: 8-831-9731/36; 8-831-5641/49 Website: www.sanjuandedios.org
College - Tel. Nos.: 8-551-2756; 8-551-2763 Website: www.sjdefi.edu.ph
Senior High School Department
EARTH SCIENCE
Semester: 1st
S.Y. 2021-2022
• Take note of the five criteria and you will be able to identify substances whether they are minerals or
#3
The substance must exist as a
SOLID under normal conditions
on Earth
#2
The substance must be
INORGANIC, not living
or made from living things
#4
The atoms that make up
the substance must be
arranged in an ORDERLY
STRUCTURE
#1
The substance must be
NATURALLY
OCCURING on Earth,
not man-made
#5
The substance must have a
FIXED CHEMICAL
FORMULA, made of
specific elements
Adapted from: https://www.iconscout.
Com/icon/mineral-3
Minerals: Physical Characteristics
• Luster
• Hardness
• Color/Streak
• Crystal Forms/Habits
• Cleavage
• Specific Gravity
• Other
• Magnetic
• Taste and Smell (Odor)
• Reaction to Acid
Minerals: Chemical Characteristics
• Silicate Minerals
• Non-Silicate Minerals
• Carbonates
• Oxides
• Halides
• Sulfides
• Sulfates
• Phosphates
• Native Element Minerals
LESSON SUMMARY
MINERALS (Module 3)
• Mineral are naturally occurring, inorganic,
solid, with definite chemical composition
and ordered structure
• Mineralogist mostly used the physical
properties of minerals for them to easily
determine the identify of a mineral.
• Minerals have a specific chemical
composition and each mineral has its
chemical formula.
MELCs
At the end of the lesson, the student should
be able to:
• Identify common rock-forming minerals,
using their physical and chemical
properties (Module 3)
• Classify rocks into igneous, sedimentary
and metamorphic (Module 4)
Rocks
• Are any naturally occurring solid mass of
mineral aggregates
• Classified into:
• Igneous Rocks (Lesson 6)
• Sedimentary Rocks
• Metamorphic Rocks (Lesson 7)
• [Pre-Ass] Rock Flowchart
LESSON SUMMARY
LESSON SUMMARY
ROCKS (Module 4)
• Igneous rocks are recognized by interlocking
texture of the grains; presence of vesicles in
extrusive igneous rocks; maybe dark-colored and
heavy; and may display two grain sizes, one much
larger than the other.
• Sedimentary rocks are recognized by grains
cemented together; the presence of fossils; light
colored and light weight; and may display
interlocking grains but is very light weight.
LESSON SUMMARY
ROCKS (Module 4)
• Metamorphic rocks are recognized by interlocking
texture of large grains; foliation (layering); banded
light and dark colors; and ‘ching’ sound instead of
a ‘chunk’ sound when tapped.
• The rock cycle defined as a process in which rocks
are continuously transformed between the three
rock types.
LESSON SUMMARY
2. Sedimentary rocks are recognized by grains cemented together; the presence of fossils;
light colored and light weight; and may display interlocking grains but is very light
weight.
3. Metamorphic rocks are recognized by interlocking texture of large grains; foliation
(layering); banded light and dark colors; and ‘ching’ sound instead of a ‘chunk’ sound
when tapped.
4. The rock cycle defined as a process in which rocks are continuously transformed
between the three rock types.
Figure 1: Rock Cycle
SOURCE: https://www.flickr.com/photos/121935927@N06/13581730833
LEARNING ACTIVITIES
Module 3
• [PT] MINERAL BROCHURE
• Pair Activity
• Summative Assessment
Module 4
• [Pre-Ass] ROCK FLOWCHART
• Individual Activity
• Formative Assessment

Modules 3 and 4.pptx

  • 1.
    MINERALS AND ROCKS EarthScience (Modules 3 and 4) Christopher Allan F. Reballos, MSc
  • 2.
    With your permission,we will be recording this session form documentation purposes. We request that you put your audio on mute to avoid disruptions during presentation. You may turn off your camera during the presentation Synchronous Google Meet Class Questions may be typed in the chat box and will be answered by the speaker after the presentation.
  • 3.
    MELCs At the endof the lesson, the student should be able to: • Identify common rock-forming minerals, using their physical and chemical properties (Module 3) • Classify rocks into igneous, sedimentary and metamorphic (Module 4)
  • 4.
    Rocks vs Minerals •Minerals are building blocks of rocks (Module 3) • Rocks are any naturally occurring solid mass of mineral aggregates (Module 4)
  • 5.
    MELCs At the endof the lesson, the student should be able to: • Identify common rock-forming minerals, using their physical and chemical properties (Module 3) • Classify rocks into igneous, sedimentary and metamorphic (Module 4)
  • 6.
    Minerals as BuildingBlocks • Minerals may be defined as: SAN JUAN DE DIOS EDUCATIONAL FOUNDATION, INC. 2772-2774 Roxas Boulevard, Pasay City 1300 Philippines Hospital - Tel. Nos.: 8-831-9731/36; 8-831-5641/49 Website: www.sanjuandedios.org College - Tel. Nos.: 8-551-2756; 8-551-2763 Website: www.sjdefi.edu.ph Senior High School Department EARTH SCIENCE Semester: 1st S.Y. 2021-2022 • Take note of the five criteria and you will be able to identify substances whether they are minerals or #3 The substance must exist as a SOLID under normal conditions on Earth #2 The substance must be INORGANIC, not living or made from living things #4 The atoms that make up the substance must be arranged in an ORDERLY STRUCTURE #1 The substance must be NATURALLY OCCURING on Earth, not man-made #5 The substance must have a FIXED CHEMICAL FORMULA, made of specific elements Adapted from: https://www.iconscout. Com/icon/mineral-3
  • 9.
    Minerals: Physical Characteristics •Luster • Hardness • Color/Streak • Crystal Forms/Habits • Cleavage • Specific Gravity • Other • Magnetic • Taste and Smell (Odor) • Reaction to Acid
  • 11.
    Minerals: Chemical Characteristics •Silicate Minerals • Non-Silicate Minerals • Carbonates • Oxides • Halides • Sulfides • Sulfates • Phosphates • Native Element Minerals
  • 13.
    LESSON SUMMARY MINERALS (Module3) • Mineral are naturally occurring, inorganic, solid, with definite chemical composition and ordered structure • Mineralogist mostly used the physical properties of minerals for them to easily determine the identify of a mineral. • Minerals have a specific chemical composition and each mineral has its chemical formula.
  • 14.
    MELCs At the endof the lesson, the student should be able to: • Identify common rock-forming minerals, using their physical and chemical properties (Module 3) • Classify rocks into igneous, sedimentary and metamorphic (Module 4)
  • 15.
    Rocks • Are anynaturally occurring solid mass of mineral aggregates • Classified into: • Igneous Rocks (Lesson 6) • Sedimentary Rocks • Metamorphic Rocks (Lesson 7) • [Pre-Ass] Rock Flowchart
  • 19.
  • 20.
    LESSON SUMMARY ROCKS (Module4) • Igneous rocks are recognized by interlocking texture of the grains; presence of vesicles in extrusive igneous rocks; maybe dark-colored and heavy; and may display two grain sizes, one much larger than the other. • Sedimentary rocks are recognized by grains cemented together; the presence of fossils; light colored and light weight; and may display interlocking grains but is very light weight.
  • 21.
    LESSON SUMMARY ROCKS (Module4) • Metamorphic rocks are recognized by interlocking texture of large grains; foliation (layering); banded light and dark colors; and ‘ching’ sound instead of a ‘chunk’ sound when tapped. • The rock cycle defined as a process in which rocks are continuously transformed between the three rock types.
  • 22.
    LESSON SUMMARY 2. Sedimentaryrocks are recognized by grains cemented together; the presence of fossils; light colored and light weight; and may display interlocking grains but is very light weight. 3. Metamorphic rocks are recognized by interlocking texture of large grains; foliation (layering); banded light and dark colors; and ‘ching’ sound instead of a ‘chunk’ sound when tapped. 4. The rock cycle defined as a process in which rocks are continuously transformed between the three rock types. Figure 1: Rock Cycle SOURCE: https://www.flickr.com/photos/121935927@N06/13581730833
  • 23.
    LEARNING ACTIVITIES Module 3 •[PT] MINERAL BROCHURE • Pair Activity • Summative Assessment Module 4 • [Pre-Ass] ROCK FLOWCHART • Individual Activity • Formative Assessment