Earth and Life Science Quarter 1 Module 9: Igneous Rocks: How Are They Formed?

SHS Earth and Life Science Q1 Module 9 explains how igneous rocks form, intrusive vs extrusive rocks, silica groups, and textures, with activities.

This is the Earth and Life Science Quarter 1 Module 9 self-learning module, “Igneous Rocks: How Are They Formed?”, for Senior High School learners. It was developed by DepEd Region 4A CALABARZON (First Edition, 2021) as an Alternative Delivery Mode module. After working through it, learners can explain how igneous rocks form and classify them by origin, silica content, and texture.

On this page 7 sections

What learners will learn

After going through this module, learners are expected to:

  1. compare the formation of different types of igneous rocks;
  2. distinguish intrusive from extrusive igneous rocks;
  3. differentiate igneous rocks based on silica content; and
  4. describe the different textures of igneous rocks.

The module has one lesson, Lesson 1: Igneous Rocks: How Are They Formed? It builds on the previous lesson on metamorphism of rocks.

How igneous rocks form

Igneous rocks are one of the three major categories of rocks, together with sedimentary and metamorphic rocks. The word “igneous” comes from the Latin word for fire, ignis or ignus.

They form through the solidification and crystallization of molten rock (magma and lava). When molten rock reaches the Earth’s surface, changes in temperature and pressure make it cool, solidify, and crystallize. Magma can also solidify and crystallize beneath the surface. The module notes that igneous rocks are commonly found at divergent and convergent boundaries, subduction zones, and hotspots.

Intrusive and extrusive rocks

Based on formation, the module sorts igneous rocks into two types:

Point of comparisonIntrusive rocksExtrusive rocks
Other nameplutonic rocksvolcanic rocks
Where they formbeneath the Earthsurface of the Earth
Formed frommagmalava
Rate of coolingslowlyquickly
Grain sizelarge or coarsefine, small, or none (glassy)
Crystal sizelargesmall or none
Examplesgabbro, diorite, granitebasalt, obsidian, rhyolite, scoria

The module’s table also describes intrusive rocks as usually dark and dense, and extrusive rocks as usually light colored and low in density.

Classifying igneous rocks by silica and texture

Igneous rocks are made of silica (SiO2), but not in the same amounts. Silica content also affects how viscous (thick) the magma is. The module gives four groups:

GroupSilica (SiO2)ColorDensityMain mineralsExamples
Ultramaficless than 45%black to olive greenvery highpyroxene, olivineperidotite, dunite
Mafic45 to 52%blackhighpyroxene, calcium-rich plagioclase feldspargabbro, basalt
Intermediate53 to 65%grayintermediatebiotite, alkali feldspar, quartzdiorite, andesite
Felsicmore than 65%lightvery lowquartz, alkali feldspargranite, rhyolite

The key rule: the higher the silica content, the lighter the color; the lower the silica, the darker the color. Felsic magma is the most viscous and ultramafic the least. The module also links melting temperature to the groups, about 700°C for felsic and 1200°C for ultramafic.

Textures

Texture is the size and arrangement of the minerals in a rock:

  • Phaneritic: large minerals you can see (granite)
  • Aphanitic: grains too small to see with the unaided eye (basalt)
  • Vesicular: many pits left by escaping gas (basalt)
  • Porphyritic: two distinct grain sizes, large and small (andesite porphyry)
  • Glassy: no obvious minerals (obsidian)

Activities in the module

  • What I Know: a 15-item multiple-choice pretest
  • Activity 1: crossword puzzle reviewing metamorphism
  • Activity 2: comic strip of a grandmother and granddaughter at Taal Volcano talking about granite
  • Activity 3: table on rhyolite, gabbro, granite, scoria, and obsidian (type, origin, cooling rate, crystal size)
  • Activity 4: concept map using a word bank
  • Activity 5: Venn diagram comparing the four silica groups
  • Activity 6: collect three rocks and record their characteristics
  • Activity 7: 20-item fill-in-the-blanks summary
  • Activity 8: a written stand on quarrying, based on the DENR investigation of quarry operations in Rizal after the Typhoon Ulysses floods
  • Assessment: a 15-item multiple-choice post-test
  • Additional Activities: a photo collage of igneous rocks in your barangay, scored with a rubric on creativity, design, and theme

How to use this module

  • Learners: Start with the pretest, then work through the parts in order. Write your answers on a separate sheet of paper and do not mark the module. Check your work with the answer key honestly, and finish with the post-test.
  • Parents and facilitators: Read the Notes to the Teacher for tips. Help your child find safe outdoor rocks for Activity 6 and take photos for the collage.
  • Teachers: Activities 5, 6, and 8 have open answers, so check them yourself. Use the rubric to grade the collage. Check the answer key before using it, because a few printed answers do not match the lesson (see the FAQ).

Frequently asked questions

What grade and quarter is this Earth and Life Science module for?

It is Quarter 1, Module 9 of Earth and Life Science, a Senior High School subject. The module does not name a specific grade.

What is the difference between intrusive and extrusive igneous rocks?

Intrusive (plutonic) rocks form from magma that cools slowly beneath the Earth, so they have large crystals, like granite. Extrusive (volcanic) rocks form from lava that cools quickly on the surface, so they have small or no crystals, like basalt and obsidian.

Which igneous rock group has the highest silica content?

Felsic rocks, with more than 65% silica, have the highest silica content and the lightest color. Ultramafic rocks have the lowest, less than 45%.

Does the module have an answer key?

Yes, it has answers for the pretest, the post-test, and the activities. A few entries do not match the lesson: the post-test key gives C (mafic) for the item on highest silica content, but the lesson says felsic (A), and the pretest key gives B for the item asking which rock is not intrusive, but the lesson points to obsidian (D).

What does the word igneous mean?

It comes from the Latin word for fire, ignis or ignus, because igneous rocks form from molten rock.

Full text of the module

The text below is a transcription of the PDF above, as printed.

Earth and Life Science Quarter 1 – Module 9: Igneous Rocks: How Are They Formed?

Senior High School

[illustration: students reading and studying outdoors and at a table, with a teacher, a globe, and a lamp]

CO_Q1_ELS SHS Module 9

Earth and Life Science Alternative Delivery Mode Quarter 1 – Module 9: Igneous Rocks: How Are They Formed? First Edition, 2021

Republic Act 8293, section 176 states that: No copyright shall subsist in any work of the Government of the Philippines. However, prior approval of the government agency or office wherein the work is created shall be necessary for exploitation of such work for profit. Such agency or office may, among other things, impose as a condition the payment of royalties.

Borrowed materials (i.e., songs, stories, poems, pictures, photos, brand names, trademarks, etc.) included in this module are owned by their respective copyright holders. Every effort has been exerted to locate and seek permission to use these materials from their respective copyright owners. The publisher and authors do not represent nor claim ownership over them.

Published by the Department of Education Secretary: Leonor Magtolis Briones Undersecretary: Diosdado M. San Antonio

Development Team of the Module

Writers: Jessa M. Ariola

Editors: Melanie I. Samudio, Jocelyn M. Manset

Reviewers: Jason Ricaforte, Angelica Beriña, Princess Paolah L. De Guzman, Marissa C. Betchaida, Louie L. Alvarez, Gregorio M. De Chavez, Jr., Jocelyn M. Manset, Mario B. Maramot, Elaine T. Balaogan, Job S. Zape Jr., Crisjee B. Silvestre, Colita I. Patricio, Jhimson V. Cabral

Illustrator: Ednelinda Robles, Lovely Joy La Rosa, Charles Erick A. Jusay, Sandro Carlo B. Tablizo

Layout Artist: Elizalde L. Piol, Anselma M. Ebero, Jocelyn M. Manset

Management Team: Francis Cesar B. Bringas, Job S. Zape, Jr., Ramonito Elumbaring, Reicon C. Condes, Elaine T. Balaogan, Fe M. Ong-ongowan, Merthel M. Evardome, Nadine C. Celindro, Nicolas M. Burgos, Mario B. Maramot, Fe M. Ong-ongowan, Rosalinda A. Mendoza

Printed in the Philippines by ______________________

Department of Education – Region 4A CALABARZON

Office Address: Gate 2 Karangalan Village, Brgy. San Isidro, Cainta, Rizal Telefax: 02-8682-5773/8684-4914/8647-7487 E-mail Address: lrmd.calabarzon@deped.gov.ph

[transcriber’s note: this page repeats the cover title in a plain layout, with the label “Senior High School”, the title “Earth and Life Science, Quarter 1 – Module 9: Igneous Rocks: How Are They Formed?”, and the DepEd logo below it]

Introductory Message

This Self-Learning Module (SLM) is prepared so that you, our dear learners, can continue your studies and learn while at home. Activities, questions, directions, exercises, and discussions are carefully stated for you to understand each lesson.

Each SLM is composed of different parts. Each part shall guide you step-by-step as you discover and understand the lesson prepared for you.

Pre-tests are provided to measure your prior knowledge on lessons in each SLM. This will tell you if you need to proceed on completing this module or if you need to ask your facilitator or your teacher’s assistance for better understanding of the lesson. At the end of each module, you need to answer the post-test to self-check your learning. Answer keys are provided for each activity and test. We trust that you will be honest in using these.

In addition to the material in the main text, Notes to the Teacher are also provided to our facilitators and parents for strategies and reminders on how they can best help you on your home-based learning.

Please use this module with care. Do not put unnecessary marks on any part of this SLM. Use a separate sheet of paper in answering the exercises and tests. And read the instructions carefully before performing each task.

If you have any questions in using this SLM or any difficulty in answering the tasks in this module, do not hesitate to consult your teacher or facilitator.

Thank you.

What I Need to Know

[illustration: a hand with a pointing finger inside a circle]

This module was designed and written with you in mind. It is here to help you master the nature of Earth and Life Science. The scope of this module permits it to be used in many different learning situations. The language used recognizes the diverse vocabulary level of students. The lessons are arranged to follow the standard sequence of the course. But the order in which you read them can be changed to correspond with the textbook you are now using.

The module covers:

  • Lesson 1 – Igneous Rocks: How Are They Formed?

After going through this module, you are expected to:

  1. compare the formation of different types of igneous rocks;
  2. distinguish intrusive from extrusive igneous rocks;
  3. differentiate igneous rocks based on silica content; and
  4. describe the different textures of igneous rocks.

What I Know

[illustration: a hand holding a pencil inside a circle]

Choose the letter of the best answer. Write the chosen letter on a separate sheet of paper.

  1. What classification of rocks is formed from solidification and crystallization of molten rocks?

    • A. igneous rocks
    • B. metamorphic rocks
    • C. sedimentary rocks
    • D. all of the above
  2. What Latin word was the term “igneous” derived from?

    • A. ignus
    • B. lithos
    • C. meta
    • D. sedere
  3. Which of the following is/are the process/es to igneous rocks?

    • A. recrystallization
    • B. sedimentation
    • C. solidification and crystallization
    • D. solidification and recrystallization
  4. Which type of igneous rocks based on composition has the highest amount of silica content?

    • A. felsic
    • B. intermediate
    • C. mafic
    • D. ultramafic
  5. What happens to the molten rocks when they reach the Earth’s surface?

    • A. They flow continuously.
    • B. They cool down and solidify.
    • C. Their temperature remains the same.
    • D. They remain semi-liquid molten rocks.
  6. Which of the following is NOT an extrusive igneous rock?

    • A. basalt
    • B. granite
    • C. obsidian
    • D. rhyolite
  7. Which type of igneous rock forms from lava on Earth’s surface?

    • A. clastic
    • B. extrusive
    • C. intrusive
    • D. non-clastic
  8. Which type of igneous rock forms when magma hardens beneath Earth’s surface?

    • A. clastic
    • B. extrusive
    • C. intrusive
    • D. non-clastic
  9. What is the size of the crystals if the rock cools slowly and forms below the Earth’s surface?

    • A. large
    • B. no crystal
    • C. small
    • D. none of the above
  10. Which of the following is NOT an intrusive igneous rock?

    • A. diorite
    • B. gabbro
    • C. granite
    • D. obsidian
  11. Which of the following is NOT true about extrusive rocks?

    • A. They cool down quickly.
    • B. They have small crystals.
    • C. These are formed beneath the Earth.
    • D. Basalt and scoria are examples of these rocks.
  12. Which of the following is TRUE about intrusive rocks?

    • A. They have fine grains.
    • B. They are usually dark.
    • C. They are formed from lava.
    • D. They have usually low density.
  13. What type of igneous rock texture has large minerals?

    • A. aphanitic
    • B. glassy
    • C. phaneritic
    • D. vesicular
  14. How are igneous rocks classified based on their origin?

    • A. from magma or lava
    • B. coarse or fine grains
    • C. large or small crystals
    • D. plutonic and volcanic
  15. How does the amount silica affect the color of igneous rock?

    • A. It has no effect at all.
    • B. It doesn’t matter what the color is.
    • C. The lesser the silica has, the lighter the color is.
    • D. The more the silica it has, the lighter the color is.

Lesson 1 – Igneous Rocks: How Are They Formed?

Have you tried mountain climbing? Did you notice different rocks in the mountain trail? Are they the same? Do they have different colors? Are there crystals? Do they undergo the same process of formation? Some of you might think that all rocks are just the same, however if we study it thoroughly, you will be surprised that they are different in terms of their formation, physical and chemical characteristics.

In your previous lesson, you already learned that rocks can be classified as igneous, sedimentary, and metamorphic. For this module, we will be focusing on igneous rocks and how they are formed.

What’s In

[illustration: a hand holding a puzzle piece inside a circle]

Activity 1. Crossword Puzzle

In the previous lesson, you have learned about metamorphism of rocks. Let us take a review before we proceed to the next topic.

Fill-in the crossword puzzle with the words being described. Match the number of the sentences with the boxes placed across or down the grid.

[transcriber’s note: the crossword grid is a blank puzzle with numbered boxes at the start of its entries; no answers are filled in. The clues are printed beside it as follows.]

ACROSS

  1. It is the change that takes place within a body of rock as a result of being subjected to conditions.
  2. It is a type of metamorphic rock which is formed due to pressure.

DOWN

  1. It is the main factor of regional metamorphism.
  2. It is a type of metamorphic rock which is formed due to heat.
  3. It is the main factor of contact metamorphism.
What’s New
Activity 2. Comic Strip Analysis

This comic presented below is about a short conversation of a grandmother and her granddaughter. Read the comics and answer the given questions.

[illustration: four-panel comic of a grandmother and granddaughter at a railing overlooking a volcano, then a woman picking up rocks, then the two sitting on a rock outcrop]

Speech bubbles, in reading order:

  • Panel 1: “Grandma, is that Taal Volcano?”
  • Panel 2: “Yes, my dear. That is Taal Volcano. It has rocks formed from solidified lava.”
  • Panel 4: “This is a granite. It is an igneous rock.”
  • Panel 5: “Wow! I want to learn more about rocks Grandma.”

Guide Questions:

  1. Who are the characters in the comic?
  2. Where do you think is the location of the characters?
  3. What is the topic of their conversation?
  4. According to the grandmother, Taal Volcano is composed of what kind of rock?
  5. What specific rock is mentioned in the conversation?

Notes to the Teacher

This module will help you to understand the concepts about the formation of igneous rocks. All parts consist of activities. Be guided with the instruction on how you will answer each. Expectedly, you will meet the target at the end of the module.

What is It
What are igneous rocks?

Igneous rocks are one of the three major categories of rocks. The word igneous is derived from the Latin word for fire, ignis or ignus.

These rocks are commonly found in the surface and beneath the Earth, specifically in divergent boundaries, convergent boundaries, subduction zones and hotspots. Not all igneous rocks have the same physical and chemical characteristics. They differ in the origin, process of formation, color, density, size of grains, crystals and many more.

How are igneous rocks formed?

Igneous rocks are formed through the process of solidification and crystallization of molten rocks; magma and lava. When hot, molten rocks reach the surface of the earth, they undergo changes in temperature and pressure, causing them to cool, solidify and crystallize. Moreover, there are also solidification and crystallization magma beneath the earth.

What are the types of igneous rocks based on their formation?

In terms of formation, igneous rocks can be classified into two: intrusive and extrusive rocks. Below is the comparison of these two types.

Table 1. Differences Between Intrusive and Extrusive Rocks

Point of ComparisonIntrusive RocksExtrusive Rocks
Other terminologyplutonic rocksvolcanic rocks
Locationbeneath the Earthsurface of the Earth
Process of Formationplutonicvolcanic
Originformed from magmaformed from lava
Colorusually darkusually light colored
Densityusually denseusually low density (light)
Compositionmafic: magnesium and ironfelsic: feldspar (aluminum)
Rate of Coolingcools slowlycools quickly (with voids/holes)
Size of Grainslarge/coarse grainsfine/small or no grains (fine/glassy)
Size of Crystalslarge crystalssmall or no crystals

[photo: gabbro rock sample] [photo: diorite rock sample] [photo: granite rock sample]

Gabbro Diorite Granite

Figure 1. Examples of Intrusive Rocks

[photo: basalt rock sample] [photo: obsidian rock sample]

Basalt Obsidian

[photo: rhyolite rock sample] [photo: scoria rock sample]

Rhyolite Scoria

Figure 2. Examples of Extrusive Rocks

Igneous rocks can also be classified according to their composition. They are composed of SiO2 or silica. Not all igneous rocks have the same silica content. If there is oversaturation of silica in the magma, its minerals will precipitate. On the other hand, if there is undersaturation of silica in the magma, its minerals will not precipitate and will not be present in the igneous rocks. The viscosity of magma is also affected because of silica content.

There are four classifications of igneous rocks based on silica content: ultramafic, mafic, intermediate, and felsic.

1. Ultramafic Igneous Rocks

  • They have a very low silica content; less than 45% of SiO2.
  • Before forming into igneous rocks, its magma has very low viscosity.
  • Its color is ranged too black (peridotite) to olive green (dunite).
  • Their density is very high.
  • They are rich in pyroxene and olivine minerals.
  • Examples of these rocks are peridotite and dunite.

2. Mafic Igneous Rocks

  • They have a low silica content; 45-52% of SiO2.
  • Before forming into igneous rocks, its magma has low viscosity; more viscous than ultramafic magma.
  • They have black color.
  • Their density is high.
  • They are composed of pyroxene, calcium-rich plagioclase feldspar
  • Examples of these rocks are gabbro and basalt.

3. Intermediate Igneous Rocks

  • They have a high silica content; 53-65% of SiO2.
  • Before forming into igneous rocks, its magma has intermediate viscosity; more viscous than the mafic magma.
  • Their color is gray.
  • Their density is intermediate.
  • They are composed of biotite, alkali feldspar and quartz.
  • Examples of these rocks are diorite and andesite.

4. Felsic Igneous Rocks

  • They have a very high silica content; more than 65% of SiO2
  • Before forming into igneous rocks, its magma has high viscosity; more viscous than the intermediate magma.
  • They have light color.
  • Their density is very low.
  • They are composed of quartz and alkali feldspar.
  • Examples of these rocks are granite and rhyolite.
GraniteDioriteGabbroPeridotite
Rock Types[photo: granite rock sample][photo: diorite rock sample][photo: gabbro rock sample][photo: peridotite rock sample]
CompositionFELSICINTERMEDIATEMAFICULTRAMAFIC
ColorLight ⟶ Dark [illustration: ten gray circles shading from light on the left to black on the right, with an arrow labeled Light and Dark]
SiO270%60%50%40%
MgO0.95%2.5%15%48%
Major mineral contentQuartz
Alkali Feldspar
Biotite
Alkali Feldspar
Quartz
Pyroxene
Plagioclase Feldspar
Pyroxene
Olivine

Figure 3. Differences of Igneous Rocks based on Composition

Based on the illustration, you will notice the differences of these four classifications of igneous rocks in terms of their color. Ultramafic has the darkest color and felsic has the lightest color. To sum, the higher the silica content is, the lighter its color while the lower the silica content is, the darker its color. Thus, the amount of silica affects the color of the rocks.

CompositionFELSICINTERMEDIATEMAFICULTRAMAFIC
Rock TypesGranite
Rhyolite
Diorite
Andesite
Gabbro
Basalt
Peridotite

[chart: line graph of mineral percentage by volume (y-axis 0 to 100, labeled “Percentage of Mineral by Volume”) against silica content and temperature; curves and labels printed: Orthoclase feldspar, Quartz, Na-rich, Plagioclase feldspar, Ca-rich, Pyroxene, Muscovite, Biotite mica, Amphibole, Olivine. Values are not labeled on the chart.]

Bands printed below the graph:

  • 70% ← Silica content → 40%
  • Sodium and potassium content (arrow pointing left)
  • Iron, magnesium, and calcium content (arrow pointing right)
  • 700°C Temperature at which melting starts 1200°C

Figure 4. Differences of Igneous Rocks based on Composition in Relation to Silica Content and Temperature

This is another illustration showing the differences of ultramafic, mafic, intermediate, and felsic igneous rocks; rock types, kind, and percentage of minerals; percentage of silica content; and ranges of temperature.

Felsic has the highest silica content while ultramafic has the lowest silica content. On the other hand, felsic is exposed to 700 degree Celsius and ultramafic is exposed to 1200 degree Celsius. It means when igneous rock is exposed to extreme high temperature, its color is darker, while if it is exposed to lower temperature, its color is light.

What are the types of igneous rocks based on texture?

Igneous rocks have different textures. The texture of a rock is the size and arrangement of the minerals it contains.

  • Phaneritic texture. Rocks have large minerals (example: granite)
  • Aphanitic texture. The mineral grains are too small to see with the unaided eye (example: basalt)
  • Vesicular texture. Rocks have many pits from gas escape (example: basalt)
  • Porphyritic texture. Rocks have two (2) distinct grain sizes, large and small (example: andesite porphyry)
  • Glassy texture. Rocks do have obvious minerals (example: obsidian)
What’s More
Activity 3. Types of Igneous Rocks, Described!

Different examples of igneous rocks are given below. Supply the missing information to complete the table below.

RockType of Igneous Rock (intrusive or extrusive)Formed from (magma or lava)Cooling rate (fast or slow)Crystal size (small, large or no crystal)
[photo: rhyolite rock sample] Rhyoliteextrusive1.2.small
[photo: gabbro rock sample] Gabbro3.4.slowlarge

transcriber’s note: table continued from the previous page

RockType of Igneous Rock (intrusive or extrusive)Formed from (magma or lava)Cooling rate (fast or slow)Crystal size (small, large or no crystal)
[photo: granite rock sample] Graniteintrusive5.slow6.
[photo: scoria rock sample] Scoria7.lava8.No crystals
[photo: obsidian rock sample] Obsidian9.lavafast10.
Activity 4. Concept Map

Complete the blank concept map by supplying the needed information using the given terms and phrases related to igneous rocks.

[chart: concept map; Activity 4. Concept Map. Boxes and links as printed:]

  • Igneous Rock
    • [blank box: transcriber’s note: the box beneath Igneous Rock is empty on the printed page]












transcriber’s note: the word bank table has no printed header row

Extrusivecomposed of magnesium and ironmagma cools slowly
Intrusivelava cools quicklysmall or no crystal form
large crystal formcomposed of aluminumform from cooling and solidification of lava and magma
Activity 5. Venn Diagram

Compare the four classifications of igneous rocks based on composition.

[chart: Venn diagram of four overlapping circles; Activity 5. Venn Diagram. Labels: Ultramafic, Felsic, Mafic, Intermediate]

Activity 6. Apply It!

Go outside and collect 3 pieces of rock. Observe their color, shape, texture, and other physical characteristics. You may crack or scratch the rock to observe them clearly. Then, record your data in the table on the next page.

Rocks (Drawing)Type of Igneous Rock and its Characteristics
1.
2.
3.

What I Have Learned

Activity 7. Complete Me!

Read the following statements and fill-in the blanks with the correct term or phrase.

  1. The word igneous is derived from the Latin word for _____, ignis or ignus.


  2. Igneous rocks are commonly found in the _____ and _____ the Earth, specifically in divergent boundaries, convergent boundaries, subduction zones and hotspots.


  3. Igneous rocks are formed through the process of _____ and _____ of molten rocks; magma and lava.


  4. When hot, molten rocks reach the surface of the earth, they undergo changes in _____ and _____ causing them to _____, _____ and _____.


  5. In terms of formation, igneous rocks can be classified into two; _____ and _____ rocks.


  6. Intrusive rocks are formed solidified _____ while extrusive rocks are formed from solidified _____.


  7. Intrusive rocks cool _____ while extrusive rocks cool _____.


  8. Intrusive rocks have _____ grains and crystals while extrusive rocks have _____ grains and crystals.


  9. Examples of intrusive rocks are _____, _____, and _____.


  10. Examples of extrusive rocks are _____, _____, _____, and _____.


  11. Igneous rocks can also be classified according to their composition. They are composed of _____.


  12. If there is _____ of silica in the magma, its minerals will precipitate.


  13. If there is _____ of silica in the magma, its minerals will not precipitate and will not be present in the igneous rocks.


  14. There are four classifications of igneous rocks based on silica content; _____, _____, _____ and _____.


  15. _____ has the highest amount of silica while _____ has the lowest.


  16. _____ is the most viscous while _____ is the least.


  17. _____ has the darkest color while _____ has the lightest.


  18. _____ is the densest while _____ is the lightest.


  19. _____ is exposed to the highest temperature while _____ is exposed to the lowest temperature.


  20. The higher the silica content is, the _____ the color is and the _____ the silica content is, the darker the color is.


What I Can Do

Activity 8. Apply It!

Read the given statement and justify your answer.

Quarrying is the process of removal of rocks, sand, gravel, or other minerals from the ground to produce materials for construction and others. Last December 2020, the Department of Environment and Natural Resources (DENR) launched an investigation into quarry operations in Rizal after heavy flooding hit the province and Marikina City. Torrential rains due to Ulysses pushed the water level in the Marikina River to swell over 22 meters –higher than what it reached in 2009 because of Typhoon Ondoy, inundating Marikina City.

Based on this event, what is your stand about this? Justify your answers.






Assessment

Multiple Choice. Read the following questions and choose the letter of the best answer. Write the chosen letter on a separate sheet of paper.

  1. Which type of igneous rock forms when magma hardens beneath Earth’s surface?
    A. clastic
    B. extrusive
    C. intrusive
    D. non-clastic


  2. What type of igneous rock texture has large minerals?
    A. aphanitic
    B. glassy
    C. phaneritic
    D. vesicular


  3. What classification of rocks is formed from solidification and crystallization of molten rocks?
    A. igneous rocks
    B. metamorphic rocks
    C. sedimentary rocks
    D. all of the above


  4. Which type of igneous rocks based on composition has the highest amount of silica content?
    A. felsic
    B. intermediate
    C. mafic
    D. ultramafic


  5. Which of the following is/are the process/es of igneous rocks?
    A. recrystallization
    B. sedimentation
    C. solidification and crystallization
    D. solidification and recrystallization


  6. Which of the following is NOT an extrusive igneous rock?
    A. basalt
    B. granite
    C. obsidian
    D. rhyolite


  7. What happens to the molten rocks when they reach the Earth’s surface?
    A. They flow continuously.
    B. They cool down and solidify.
    C. Their temperature remains the same.
    D. They remain semi-liquid molten rocks.


  8. Which type of igneous rock forms from lava on Earth’s surface?
    A. clastic
    B. extrusive
    C. intrusive
    D. non-clastic


  9. What Latin word was the term “igneous” derived from?
    A. ignus
    B. lithos
    C. meta
    D. sedere


  10. Which of the following is NOT an intrusive igneous rock?
    A. diorite
    B. gabbro
    C. granite
    D. obsidian


  11. What is the size of the crystals if the rock cools slowly and forms below the Earth’s surface?
    A. large
    B. no crystal
    C. small
    D. none of the above


  12. Which of the following is TRUE about intrusive rocks?
    A. They have fine grains.
    B. They are usually dark.
    C. They are formed from lava.
    D. They have usually low density.


  13. Which of the following is NOT true about extrusive rocks?
    A. They cool down quickly.
    B. They have small crystals.
    C. These are formed beneath the Earth.
    D. Basalt and scoria are examples of these rocks.


  14. How are igneous rocks classified based on their origin?
    A. from magma or lava
    B. coarse or fine grains
    C. large or small crystals
    D. plutonic and volcanic


  15. How does the amount silica affect the color of igneous rock?
    A. It has no effect at all.
    B. It doesn’t matter what the color is.
    C. The lesser the silica has, the lighter the color is.
    D. The more the silica it has, the lighter the color is.


Additional Activities

Take some pictures of igneous rocks available in your barangay and make a collage. Write a short paragraph or description about your output.

Criteria4321
CreativityAll of the pictures used in the collage reflect a degree of student creativity in their display.Most of the pictures used in the collage reflect student creativity in their display.Only a few pictures reflect student creativity, but the ideas were typical rather than creative.None of the pictures reflects student creativity.
DesignPictures are cut to an appropriate size, shape and are arranged neatly.1-2 Pictures are lacking in design or placement. There may be a few smudges or glue marks.3-4 Pictures are lacking in design or placement. Too much background is showing. There are noticeable smudges or glue marks.Pictures are not an appropriate size shape.
ThemeThe student gives a reasonable explanation of how every item in the collage is related to the assigned theme.The student gives a reasonable explanation of how most items in the collage are related to the assigned theme.The student gives a fairly reasonable explanation of how most items in the collage are related to the assigned theme.The student’s explanations are weak and illustrate difficulty understanding how to relate items to the assigned theme.

Answer Key

[transcriber’s note: this page is printed upside down; sections are given in the module’s order, and entries are transcribed as printed]

What I Know
  1. A
  2. A
  3. C
  4. A
  5. B
  6. B
  7. B
  8. C
  9. A
  10. B
  11. C
  12. B
  13. C
  14. A
  15. D
What’s In

Activity 1

Across

  1. metamorphism
  2. regional

Down 2. pressure 4. contact 5. heat

What’s New

Activity 2

  1. grandmother and her granddaughter
  2. place where Taal volcano can be seen
  3. They are talking about rocks found in Taal volcano.
  4. igneous rocks
  5. granite
What’s More

Activity 3

  1. lava
  2. fast
  3. intrusive
  4. magma
  5. magma
  6. large
  7. extrusive
  8. fast
  9. extrusive
  10. no crystals

Activity 4

  1. form from cooling and solidification of lava and magma
  2. intrusive
  3. crystal form large
  4. magma cools slowly
  5. composed of magnesium and iron
  6. extrusive
  7. small or no crystal form
  8. lava cools quickly
  9. composed of aluminum

Activity 5

Answers may vary

Activity 6

Answers may vary. Their color, density, grains, crystals, and location of the rocks

Assessment
  1. C
  2. C
  3. A
  4. C
  5. C
  6. B
  7. B
  8. B
  9. A
  10. D
  11. A
  12. B
  13. C
  14. A
  15. D
What I Can Do

Activity 8

Answers may vary

What I Have Learned

Activity 7

  1. fire
  2. surface, beneath
  3. solidification, crystallization
  4. temperature, pressure, cool, solidify, crystallize
  5. intrusive, extrusive
  6. magma, lava
  7. slowly, quickly
  8. large, small or no
  9. gabbro, diorite, granite
  10. basalt, obsidian, rhyolite, scoria
  11. silica
  12. oversaturation
  13. undersaturation
  14. ultramafic, mafic, intermediate, felsic
  15. felsic, ultramafic
  16. felsic, ultramafic
  17. ultramafic, felsic
  18. ultramafic, felsic
  19. ultramafic, felsic
  20. lighter, lower

References

“An Introduction to Geology”, University of Hawai’i at Manoa, accessed May 31, 2020, http://www.soest.hawaii.edu/lecture/gg101/powerpoints/Minerals_Igneous.pdf

“How to Classify Igneous Rocks Into (Ultramafic, Mafic, Intermediate and Felsic)?”, Geology In, accessed May 31, 2020, http://www.geologyin.com/2014/12/how-to-classify-igneous-rocks-into.html

“Igneous Rocks Worksheet”, Study Resource, accessed May 28, 2020, https://studyres.com/doc/959258/igneous-rocks-worksheet

“Igneous Rocks”, Columbia Education, accessed May 31, 2020, http://www.columbia.edu/~vjd1/igneous.htm

“Introduction to the Rock Cycle”, OHMAA+, accessed May 25, 2020, https://ops.instructure.com/courses/10087/pages/introduction-to-the-rock-cycle

“Intrusive Igneous Rocks”, Minerals4Kids, accessed May 27, 2020, http://www.mineralogy4kids.org/?q=rock-cycle/intrusive-igneous-rocks

“Lesson 3: “The Big Rock” Lesson: Introduction to Rocks”, Lehigh University, accessed May 28, 2020, http://www.ei.lehigh.edu/envirosci/geology/rocks/pdf/lesson3.pdf

“Question: Because Magmas and The Igneous Rocks That Form From”, Chegg Study, accessed May 31, 2020, https://www.chegg.com/homework-help/questions-and-answers/magmas-igneous-rocks-form-large-range-chemical-compositions-geologists-use-classifications-q17090207

C.E. Jones, “Igneous Rocks by Composition”, Department of Geology and Planetary Science, accessed May 31, 2020, https://www.pitt.edu/GeoImages/2IgneousRocks/IgneousCompositions.html

David Michaud, “Igneous Rocks Formations”, 911metallurgist, published October 15, 2015, https://www.911metallurgist.com/blog/igneous-rocks

“DENR probes quarry ops in Rizal after massive flood in province, Marikina City”, Gabriel Pabico Lalu, Department of Environment and Natural Resources, published in December 11, 2020, https://newsinfo.inquirer.net/1370548/denr-probes-quarry-ops-in-rizal-after-massive-flood-in-province-marikina-city

Fran Anderson, “When Earth Speaks”, Pinterest, accessed May 25, 2020, https://www.pinterest.com.au/pin/393713192409577434/

Hobart M. King, Ph.D., RPG. “What are Igneous Rocks?”, Geoscience News and Information Geology.com, accessed May 27, 2020, https://geology.com/rocks/igneous-rocks.shtml

Matt Williams, “Igneous Rocks: How Are They Formed?”, Universe Today, published December 16, 2015, https://www.universetoday.com/82009/how-are-igneous-rocks-formed/

Stephen A. Nelson, “Classification of Igneous Rocks”, Tulane University General, updated January 12, 2011, https://geology.com/dictionary/glossary-u.shtml

“What is Quarrying?”, The Institute of Quarrying, accessed August 13, 2021, https://www.quarrying.org/about-quarrying/quarrying-explained

For inquiries or feedback, please write or call:

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