This is the Earth and Life Science Quarter 1, Module 8 self-learning module for Senior High School. Its title is Changes in Mineral Components and Texture of Rocks (Metamorphism). It was prepared by DepEd Region 4A CALABARZON as an Alternative Delivery Mode material (First Edition, 2021). It has one lesson. After it, learners can explain how heat and pressure change rocks and identify common metamorphic rocks.
What learners will learn
After going through this module, learners are expected to:
- describe the changes in mineral components and texture of rocks due to changes in pressure and temperature (metamorphism);
- identify rock samples based on the effects of changes in temperature and pressure; and
- analyze, through a diagram, how temperature and pressure affect the mineral components and texture of rocks.
Lessons in this module
- Lesson 1: Changes in Mineral Components and Texture of Rocks (Metamorphism). Defines metamorphism and compares contact and regional metamorphism. It explains the agents that cause it and uses a rock identification table to classify metamorphic rocks by texture and grain size.
Key ideas: what metamorphism is
Metamorphism is the change that takes place within a body of rock when it is exposed to conditions different from those in which it formed. The word comes from the Greek “meta” (change) and “morphe” (form).
Metamorphic rock is the third family of rocks. It forms from igneous or sedimentary rock that has been changed by tremendous heat and pressure. Metamorphism does not melt the rock. Instead, it turns it into a denser, more compact rock, and minerals recrystallize or rearrange. Mineral combinations are stable only within certain ranges of pressure and temperature. Outside those ranges, minerals form new combinations called mineral assemblages.
The three agents of metamorphism
- Heat. Perhaps the most important agent. It provides the energy that drives the chemical changes behind the recrystallization of minerals. Heat increases with depth.
- Pressure. Also increases with depth, so buried rocks are placed under force or stress. Heat and pressure together cause physical changes in buried rocks.
- Chemically active fluids. Usually water containing dissolved ions. As rocks are buried deeply, this water is forced out and helps chemical reactions happen.
Contact and regional metamorphism
- Contact metamorphism. Happens when magma brings a great amount of heat into an existing rock and “bakes” it. Heat is its main factor, and it produces non-foliated rocks such as hornfels.
- Regional metamorphism. Caused by high temperature and high pressure acting over a large volume of crust. Pressure is its main factor. Pressure and recrystallization of minerals give deformed rocks their foliation (layering or lineation), the typical texture of regional metamorphic rocks.
How to identify metamorphic rocks
The module’s Scheme of Metamorphic Rock Identification sorts rocks by texture, grain size, and type of metamorphism.
| Rock | Texture | Grain size | Notes from the module |
|---|---|---|---|
| Slate | Foliated (mineral alignment) | Fine | Low-grade metamorphism of shale |
| Phyllite | Foliated (mineral alignment) | Fine to medium | Foliation surfaces shiny from microscopic mica crystals |
| Schist | Foliated (mineral alignment) | Fine to medium | Platy mica crystals visible, from metamorphism of clay or feldspars |
| Gneiss | Foliated (banding) | Medium to coarse | High-grade metamorphism; minerals separated into bands |
| Hornfels | Non-foliated | Fine | Rocks changed by heat from nearby magma or lava (contact) |
| Quartzite | Non-foliated | Fine to coarse | Metamorphism of sandstone; made of quartz |
| Marble | Non-foliated | Fine to coarse | Metamorphism of limestone or dolostone; calcite and/or dolomite |
| Metaconglomerate | Non-foliated | Coarse | Pebbles may be distorted or stretched |
The foliated rocks (slate, phyllite, schist, gneiss) come from regional metamorphism, where heat and pressure increase with depth. The module also mentions anthracite, which forms from the metamorphism of bituminous coal.
Everyday uses
- Slate: classroom blackboards, pool and snooker table bases, roofing, and garden stones
- Marble: building floors, bathroom walls, counters, and sculpture
- Schist: building, sculpture, and paving decoration
How to use this module
The module follows the usual self-learning module parts. Work through them in order:
- What I Know: a 15-item pretest
- What’s New: pick words linked to metamorphism
- What Is It: the flowchart, rock table, and a checkbox question
- What’s More: four activities: a concept map, a hidden-word puzzle, the Rock You diagram, and a crossword
- What I Have Learned: a matching test
- What I Can Do: list rock uses and make a rock display at home
- Assessment: a 15-item post-test
- Additional Activities
- Learners: Use a separate sheet for your answers. Keep track of your score in each activity for the “Major Task.” Each score number matches a letter, and you think of a metamorphism word that starts with that letter. You record these in the Additional Activities table. Check your work honestly with the answer key at the end.
- Parents: For the What I Can Do task, help your child gather rocks with different textures. They can arrange them in a jar or garden and take a photo, or draw the project if printing is not possible.
- Teachers: The Notes to the Teacher suggest a five-step flow: Extend, Explore, Explain, Enable, and Evaluate. Remind learners about the Major Task. Before checking papers, compare the printed answer key with the lesson. Some keys do not match the module’s own content, for example pretest items 2, 9, 14, and 15 and assessment items 3 and 5.
Frequently asked questions
What grade and quarter is this Earth and Life Science module for?
It is Quarter 1, Module 8 of Earth and Life Science, a Senior High School subject. The module does not name a specific grade.
What is metamorphism?
Metamorphism is the change that takes place within a rock when it is exposed to conditions different from those in which it formed. The word comes from the Greek meta (change) and morphe (form).
What is the difference between contact and regional metamorphism?
Contact metamorphism happens when heat from nearby magma bakes surrounding rock, and it forms non-foliated rocks such as hornfels. Regional metamorphism is driven mainly by pressure over a large area of crust and produces foliated rocks such as slate, schist, and gneiss.
What are examples of foliated and non-foliated metamorphic rocks?
Foliated rocks in the module are slate, phyllite, schist, and gneiss. Non-foliated rocks are hornfels, quartzite, marble, and metaconglomerate.
Does the module have an answer key?
Yes. The answer key at the end covers the pretest, activities, and assessment. A few printed answers do not match the lesson, so teachers should check them.
Full text of the module
The text below is a transcription of the PDF above, as printed.
Earth and Life Science Quarter 1 – Module 8: Changes in Mineral Components and Texture of Rocks (Metamorphism)
Senior High School
Earth and Life Science Quarter 1 – Module 8: Changes in Mineral Components and Texture of Rocks (Metamorphism)
[illustration: students studying outdoors under a tree and at a table with a teacher, a globe, and a boy reading by a lamp]
GOVERNMENT PROPERTY NOT FOR SALE
CO_Q1_ELS SHS Module 8
Earth and Life Science Alternative Delivery Mode Quarter 1 – Module 8: Changes in Mineral Components and Texture of Rocks (Metamorphism) 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: Chris B. De Jesus
Editors: Erwin R. Abrencillo, Jocelyn M. Manset
Reviewers: Dominic P. Almirez, Franz Kevin Manalo, 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, 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
Senior High School
Earth and Life Science Quarter 1 – Module 8: Changes in Mineral Components and Texture of Rocks (Metamorphism)
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: hand pressing a finger on a circular button]
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 – Changes in Mineral Components and Texture of Rocks (Metamorphism)
After going through this module, you are expected to:
- describe the changes in mineral components and texture of rocks due to changes in pressure and temperature (metamorphism);
- identify rock samples based on the effects of changes on temperature and pressure; and
- analyze through a diagram on how temperature and pressure affect the mineral components and texture of rocks.
What I Know
[illustration: hand holding a pencil]
Read and analyze each statement and choose the letter which corresponds to the correct answer by writing it on your answer sheet/notebook.
Which of the following statements best describe metamorphosis?
- A. change in rock formation
- B. process of rock formation
- C. process which involves changes
- D. change that takes place within body of rock once expose to different conditions
Which of the following metamorphism is affected by heat and reactive fluid?
- A. contact only
- B. regional only
- C. both contact and regional
- D. neither contact nor regional
Which of the following is an example of rock produced by a contact metamorphism?
- A. gneiss
- B. hornfels
- C. marble
- D. slate
Which of the following led to the formation of deformed rocks with foliation?
- A. volume of air entering the rocks
- B. temperature and rising of magma
- C. temperature and volume of minerals
- D. pressure and recrystallization of minerals
What is the effect of heat and pressure in rocks as there is an increase in depth?
- A. foliation surfaces shine
- B. low-grade metamorphism
- C. grain size becomes coarse
- D. increase in mineral alignment
Which of the following is the main factor in the process of regional metamorphism?
- A. air
- B. pressure
- C. temperature
- D. water
Which of the following rock samples is less influenced by the heat?
- A. gneiss
- B. phyllite
- C. schist
- D. slate
How do you describe the grain size texture of hornfels?
- A. fine texture
- B. coarse texture
- C. coarse to fine texture
- D. medium coarse texture
Which of the following is not a non-foliated metamorphic rock?
- A. hornfels
- B. marble
- C. phyllite
- D. metaconglomerate
What happened to the temperature and pressure if the rocks are buried down deep?
- A. It increases
- B. It decreases
- C. It remains constant
- D. It is intermittently degrading
Which of the following is NOT true about metamorphism?
- A. Slate and Gneiss are examples of foliated rock.
- B. Contact Metamorphism creates non-foliated rocks.
- C. Pressure is the main factor of contact metamorphism.
- D. Magma will bake the surrounding rocks due to different in temperature.
Which of the following is an example of non-foliated rock?
- A. gneiss
- B. marble
- C. phyllite
- D. schist
Which of the following is the main factor of regional metamorphism?
- A. air
- B. fire
- C. pressure
- D. temperature
Which type of metamorphism is caused by high temperature and high pressure enacted over a large volume of crust?
- A. burial
- B. contact
- C. regional
- D. pyroclastic
Which of the following is a distinct projecting textural feature of regional metamorphic rocks?
- A. ripples
- B. bedding
- C. foliation
- D. non-foliation
Lesson 1 Changes in Mineral Components and Texture of Rocks (Metamorphism)
This part of the module contains topics about metamorphism. Students must describe changes in mineral component and texture of rocks due to changes in pressure and temperature by doing the different activities included in this part of the module. Likewise, concept about the metamorphism is available for the students’ reference in doing each activity incorporated in the procedure.
What’s In
[illustration: hand holding a puzzle piece]
Metamorphism is the change that takes place within a body of rock as a result of it being subjected to conditions that are different from those in which it is formed. It is from the Greek word “meta” means change and “morphe” means form.
Notes to the Teacher
[illustration: hand holding a stack of papers]
General Notes:
- Extend. Provide the materials to the students.
- Explore. Allow the students to explore and check the given materials.
- Explain. Describe each part of the instructional material or the module.
- Enable. Let the students perform or accomplish the module.
- Evaluate. Assess learners’ output and get back to them.
Specific Note:
Remind the students with the major task.
Major Task. Take note of the number of correct responses you will be making in every activity (What I know, What’s new, What is it, What’s More A and B, What I have learned, and What I can do). Then, look for the corresponding letter of each number of responses and think of the words which are associated in metamorphism. Accomplish it in the “Additional Activity” part.
Example:
A. What I Know : 6 – F = fluid B. What’s New : 4 – D = deep rock C. What is It : 7 – G = gneiss D. What’s More A and B : 9 – I = intrusive E. What I Have Learned : 8 – H = heat F. What I Can Do : 5 – E = energy
What’s New
The box on the left side contains important words which may or may not be associated to metamorphic process. Identify words which are related to the said process by choosing and writing the words on the opposite box.
Example: HEAT (It causes changes in rocks. Hence, it is related to metamorphic process.)
[transcriber’s note: the printed exercise is a two-box layout. The left box lists the words below, and an arrow points to the right box, which has the example word HEAT written at its top. The right box is otherwise blank. The Score field is printed at the lower right.]
Left box:
- HEAT
- VOLCANIC ROCK
- PRESSURE
- FLUID
- MANTLE
- TEMPERATURE
- WEATHERING
- CEMENTATION
Right box: HEAT
Score:
What is It
Activity: Heat, Pressure, and Metamorphism
[chart: flowchart; “METAMORPHIC ROCK is formed at the surface of the Earth through the process of metamorphism with recrystallization of minerals in rocks due to changes in pressure and temperature conditions.” branches to “A. Contact Metamorphism” and “B. Regional Metamorphism”, both pointing to “Main Factors”, which branches to “Heat and Reactive Fluids” and “Pressure”]
The table below shows the scheme of metamorphic rock identification. It includes key points on how to classify rocks depending on its type, texture, and grain size. Specific rock samples are also presented with their map symbol. Likewise, compositions of metamorphic rock are also situated parallel to the type of metamorphism.
Table 1. Scheme of Metamorphic Rock Identification
[transcriber’s note: the Composition block is printed as six shaded vertical columns headed MICA, QUARTZ, FELDSPAR, AMPHIBOLE, GARNET, and PYROXENE, with no cell text. The Type of Metamorphism entry for the three foliated rows (Phyllite, Schist, Gneiss) and the entry for the three nonfoliated rows (Quartzite, Marble, Metaconglomerate) are printed as merged cells spanning those rows; each is shown once in the first row of its group. The Map Symbol column contains pictures only.]
| Texture | Grain Size | Composition | Type of Metamorphism | Comments | Rock Name | Map Symbol |
|---|---|---|---|---|---|---|
| Foliated – Mineral Alignment | FINE | Regional | Low-grade metamorphism of shale | Slate | [illustration: map symbol for slate] | |
| Foliated – Mineral Alignment | FINE TO MEDIUM | (Heat and Pressure increase with depth) | Foliation surfaces shiny from microscopic mica crystals | Phyllite | [illustration: map symbol for phyllite] | |
| Foliated – Mineral Alignment | FINE TO MEDIUM | Platy mica crystals visible from metamorphism of clay or feldspars | Schist | [illustration: map symbol for schist] | ||
| Foliated – Banding | MEDIUM TO COARSE | High-grade metamorphism; some mica changed to feldspar, segregated by mineral type into bands | Gneiss | [illustration: map symbol for gneiss] | ||
| Nonfoliated | FINE | Variable | Contac Heat | Various rocks changed by heat from nearby magma/lava | Hornfels | [illustration: map symbol for hornfels] |
| Nonfoliated | FINE TO COARSE | Quartz | Regional or Contact | Metamorphism of rocks sandstone | Quartzite | [illustration: map symbol for quartzite] |
| Nonfoliated | FINE TO COARSE | Calcite and/or dolomite | Metamorphism of limestone or dolostone | Marble | [illustration: map symbol for marble] | |
| Nonfoliated | COARE | Various Minerals in particles and matrix | Pebbles may be distorted or stretched | Metaconglomerate | [illustration: map symbol for metaconglomerate] |
The three main factors/agents of metamorphism include heat, pressure, and chemically active fluids. The heat perhaps is the most important factors because it provides the energy to drive the chemical changes which results in the recrystallization of minerals. The heat increases as the depth increases. Pressure just like heat, also increases with depth, and the buried rocks are subjected to the force or stress. Heat and pressure cause physical changes to buried rocks. Chemically active fluids enhanced the metamorphic process. Usually, the common fluid which helps the chemical activity is water containing ions in solution. As the rocks buried deeply, the water is forced out of the rock and becomes available to aid in chemical reactions.
Let’s do it!
Answer the question below by putting a check in the box .
Question: How do temperature and pressure affect the metamorphic rock formation? (5 points)
☐ If the rocks are buried deep, temperature, and pressure will get increased. ☐ Contact metamorphism creates no-foliated metamorphic rocks. ☐ Magma will bake the surrounding rocks due to difference in temperature. ☐ Deformed rocks with foliation/lineation are brought by pressure and recrystallization of minerals. ☐ Pressure is the main factor of contact metamorphism ☐ Slate and gneiss are examples of foliated rocks.
Score:
What’s More
Activity A. Metamorphism Map
Complete the concept map about metamorphism by supplying the missing words and phrases which can be chosen from the box below.
Key Terms:
- form volcano
- lineation/foliation
- schist
- gneiss
- non-Foliated
- fine grain
- hornfels
- marble
- slate
- magma
- pressure
- heat
- quartzite
Activity A. Metamorphism Map (concept map, continued)
[chart: concept map; “Tell something about metamorphism ” at the top. Three branches: ““Meta” means ____ / “Morphe” means“; “Two Classifications of Metamorphic”; “Where are metamorphic rocks formed?”. Under “Two Classifications of Metamorphic”, two branches: a blank box, and “Non-foliates”. Under each of these, a box reading “It projects ________”. Below these, “Ex.:” followed by five blank boxes: two under the left branch and three under the right branch. Score field at the lower right.]
Score:
Activity B. The Hidden Word
Arrange the jumbled letters by putting the correct sequence on the shaded boxes to form a word (names of rocks) based on the given description. Use the numbered boxes to discover the hidden word.
Example: It is formed when limestone is exposed to high temperature and pressure.
| L | E | B | A | R | M |
|---|---|---|---|---|---|
| M | A | R | B | L | E |
- It has low-grade metamorphism of shale.
| T | E | L | A | S |
|---|---|---|---|---|
| 2 |
- Plays mica crystals visible from metamorphism of clay or feldspar.
| T | S | S | I | C | H |
|---|---|---|---|---|---|
| 4 |
- Metamorphism of bituminous coal.
| A | N | I | T | H | R | A | C | T | E |
|---|---|---|---|---|---|---|---|---|---|
| 3 |
- High –grade metamorphism.
| S | S | I | N | E | G |
|---|---|---|---|---|---|
- Foliation surface is shiny from microscopic mica crystals.
| E | T | P | Y | H | L | L | I |
|---|---|---|---|---|---|---|---|
| 1 |
The hidden word is _______________________.
Activity C: Rock You
Read and analyze the diagram below. It will provide you better understanding about the lesson.
[chart: three-circle diagram with double-headed arrows between each pair; circles labeled “Sedimentary Rock” (top), “Igneous Rock” (left), and “Metamorphic Rock” (right). A large curved arrow leads from Metamorphic Rock down to the text box below.]
The third family of rock is the metamorphic rock formed from either igneous rock or sedimentary rocks that have been changed due to tremendous heat and pressure.
Metamorphism does not actually melt the rocks but transforms them into denser, more compact rocks. Mineral may also be rearranged due to chemical reactions involving fluids that enter rocks
Metamorphic Rocks are used for variety of purposes.
Slate is used commercially for your classroom blackboards and for pool tabletops.
Marble is used in the construction of building floors, bathroom walls, and counter parts (Pavico and Faraon, 2007, 224-225).
Extreme heat and pressure change the original state of an existing rock. They also change chemical composition and physical structure of existing rocks. Combinations of minerals in rocks are stable only over specific ranges of pressure and temperature. At pressure and temperature not within the ranges, the minerals form different combinations call mineral assemblages (Kasten 2012, 290-291).
Activity D: My Metamorphic Puzzle
Complete the crossword puzzle by filling in a word which corresponds to the description written in the across and down clues.
[chart: crossword grid with numbered cells 1 to 10; the vertical entry 1 reads N O N F O L I A T E D; the other entries are blank]
ACROSS
- Used commercially classroom blackboards
- Rock formed by heat and pressure changing one type of rock into another
- Different combination of a mineral formation
- Metamorphic rocks which forms a layer
- Changes in a rock that is in contact with magma
DOWN
- Metamorphic rocks which do not have a layered or banded appearance
- Used as a decorative stone such as cover walls and stair treads
- Occurs from the increasing in both heat and pressure
- It transforms rock into denser and more compact rock
- Used in construction of building floors
What I Have Learned
Match the statements in column A with the indicated terms in column B. Write the letter of the correct answer on the blank before each number.
| Column A | Column B |
|---|---|
| ____ 1. It is a Greek word which means “change” | A. quartzite |
| ____ 2. It is one of the factors affecting metamorphic rock which creates lineation | B. metamorphism |
| ____ 3. Hornfels, marble and ________ | C. meta |
| ____ 4. It is the main factor of contact metamorphism | D. regional metamorphism |
| ____ 5. It is a process of changing rock formation | E. heat |
| ____ 6. It has a foliation surface shiny from microscopic mica crystal | F. pressure |
| ____ 7. A rock sample which maybe distorted or stretched | G. phyllite |
| ____ 8. A rock sample with carbon composition | H. metaconglomerate |
| ____ 9. It is formed by great heat and pressure deep within the earth | I. anthracite |
| ____ 10. It takes place when magma introduces great amount of heat into an existing rock resulting in the recrystallization and mineral reaction in the rock | J. metamorphic rock |
| K. contact metamorphism |
Score:
Additional Task
For your own reflection and understanding, answer the posted question below. You may use the available diagram in answering the question.
“Humans are different from each other, also men, and women are far way different from each other. On the other hand, they possess characteristics and functions which are both important and needed for the world progression and development. Like rocks, which display different texture and colors but despite of these differences they both possess beauty and brilliance.”
Based on the quotation above, how do you see the similarities and differences of human and rocks?
[chart: Venn diagram of two overlapping circles; the left circle is labeled “Human” and the right circle is labeled “Rock”. Values are not labeled on the chart.]
What I Can Do
A. Give the uses of the following metamorphic rock samples. Write your answer in the box provided under each rock samples.
| Slate | Marble | Schist |
|---|---|---|
B. Read the following tips on how you can make rock useful at home. Look for rocks with different textures as the highlight of your task. Choose one from the three suggestions and once you do it, take a picture of it and attach it in the space below. In case, you do not have ways to print it, just illustrate your project on the space provided.
- Rock can be displayed in crystal or transparent vase/jar.
- Make a good arrangement of rocks in a jar. You can make it with same color, same textures, or sizes.
- Aside from the rock in jar. You can also use them in a garden by putting it together with plants. Arrange it according to your taste.
[transcriber’s note: blank box provided for the learner’s photo or illustration]
Assessment
Multiple Choice. Read and analyze each statement and choose the letter which corresponds to the correct answer by writing it on your answer sheet/notebook.
Which of the following words is NOT associated with metamorphism?
- A. heat
- B. mantle
- C. pressure
- D. weathering
What is the effect of heat and pressure in rocks as there is an increase in depth?
- A. foliation surfaces shine
- B. low-grade metamorphism
- C. grain size becomes coarse
- D. increase in mineral alignment
What is the main factor that affects regional metamorphism?
- A. heat
- B. fluid
- C. water
- D. pressure
Which of the following rock sample contains fine texture?
- A. gneiss
- B. hornfels
- C. quartzite
- D. metaconglomerate
What rock is the result of the metamorphism of sandstones?
- A. slate
- B. schist
- C. marble
- D. phyllite
What are the main factors for contact metamorphism to occur?
- A. air and water
- B. heat and reactive fluid
- C. temperature and water
- D. pressure and temperature
How do you describe the grain size texture of Hornfels?
- A. It has fine texture
- B. It has coarse texture
- C. It has coarse to fine texture
- D. It has medium coarse texture
Which of the following rock samples is less influenced by the heat?
- A. phyllite
- B. gneiss
- C. schist
- D. slate
Which of the following is NOT true about metamorphism?
- A. Slate and gneiss are examples of foliated rock.
- B. Contact metamorphism creates non-foliated rocks.
- C. Pressure is the main factor of contact metamorphism.
- D. Magma will bake the surrounding rocks due to different in temperature.
What happens to the grain size of the minerals in rocks when the heat is increased?
- A. It increases
- B. It decreases
- C. It remains constant
- D. It degrades intermittently
Which of the following DOESN’T belong to the group?
- A. dolomite
- B. feldspar
- C. mica
- D. quartz
Foliation or lineation happens among deformed rocks due to
- A. pressure and recrystallization of rocks
- B. eruption of magma from the mantle to the crust
- C. increase in temperature in the surrounding area
- D. increase in volume of water as the rocks’ depth increases
Which of the following relationships is INCORRECT?
- A. fine grain: slate
- B. banding: gneiss
- C. non-foliated: phyllite
- D. contact heat: hornfels
How do temperature and pressure affect metamorphism?
- A. Pressure and temperature increase as you go up to the crust.
- B. The deeper the rock depth, the higher the pressure and temperature.
- C. Foliation happens as there is an increase in the pressure and temperature.
- D. Magma cannot bake the surrounding rocks due to the difference in temperature.
Samer is walking down the river when she sees an unknown metamorphic rock. Which of the following characteristic can BEST help her to immediately identify the type of metamorphism that the rock underwent using a magnifying glass?
- A. foliation
- B. grain size
- C. name of the rock
- D. kind of mineral present in the rock
Additional Activities
A. Indicate the scores you obtained from the previous activities. Please refer to the major task in case you forget the directions. Write your answer on the space provided in the box below.
| Activity | Score | Formed Words |
|---|---|---|
| What I Know | ||
| What’s New | ||
| What is it | ||
| What’s More (A+B) | ||
| What I have Learned | ||
| What I can Do | ||
| Assessment |
B. For additional information, take time to read and observe the concept map.
[chart: concept map; no title printed above it]
Nodes and links as printed:
- Pressure (up arrow) → melting: “influenced by”
- Pressure (down arrow) → melting: “influenced by”
- Water → melting: “influenced by”
- melting → Existing Rock: “can occur to”
- underground → melting: “of rock, occurs in”
- melting → magma: “of rock, forms”
- magma → density: “moves upwards because of low”
- magma → lava: “rises to Earth’s surface, where it is called”
- magma → intrusive rocks: “rises but cool below surface, becoming”
- lava → extrusive rocks: “cools to make”
- lava → volcano: “erupts from a”
[transcriber’s note: arrows are shown as the direction of the link; the up and down arrows are printed inside the Pressure boxes]
The concept map above presents the processes between igneous and metamorphic rocks. It shows how metamorphism takes place from any existing rocks such as igneous rock.
Answer Key
Assessment
- D
- C
- C
- B
- C
- B
- A
- D
- C
- A
- A
- A
- C
- B
- B
What I Have Learned?
- C
- F
- A
- E
- B
- G
- H
- I
- J
- K
Additional Task (Answer may Vary)
Example
- Human shows characteristics and attitudes which are unique to humans as a rational being.
- Rocks display characteristic, beauty, appearance which are different from other types of rocks
- In spite of differences, both are the same when it comes to the ability of showing how unique and wonderful they are.
What I Can Do
Slate:
- Good roofing material
- Decorative gardening stones
- Base for snooker tables
- And it was used as a writing board (or writing slate)
Marble:
- Use for building or sculpture material
- Can be ground down and use as cleaning and soap material
Schist:
- Use for building, sculpture. Paving grade decoration
What is It
- If the rocks buried deep, temperature and pressure in get increase
- Contact metamorphism creates non-foliated metamorphic rocks
- Magma will bake the surrounding rocks due to difference in temperature
- Deformed rocks with foliation/lineation are brought by pressure and recrystallization of minerals
- Slate and gneiss are examples of foliated rocks
What’s More
A.
[chart: concept map of melting, magma, lava, and rock types; the labels are too small to read reliably in this rotated image]
B.
- Slate
- Schist
- Anthracite
- Gneiss
- Phyllite
D.
- Nonfoliated
- Quartzite
- Metamorphosis
- Slate
- Metamorphic
- Assessmages [?]
- Regional
- Foliated
- Marble
- Contact
What I Know
- D
- B
- B
- D
- C
- B
- D
- A
- D
- A
- C
- B
- C
- D
- D
What’s New
- Heat
- Pressure
- Fluid
- Mantle
- Temperature
- Volcanic Rock
References
A. Books
Acosta Herma D. et al. Science Learners Material Grade 10, 2015.
Commission on Higher Education. Earth and Life Science for Senior High School. C.P. Garcia Ave., Diliman, Quezon City Philippines. Commission on Higher Education, 2016
Kasten Lileth P. Integrated Science: Secondary Education Curriculum, 2012.
Pavico-Ferriols Josefina and Faraon-Darvin Genevieve, Exploring Life Through Science: Integrated Science, 2007.
Vengco Lilia G. and Religioso Teresita F. You and the Natural World: Integrated Science, 3rd Edition 2008.
B. Electronic References
Steven Earle, Gabriola Island, 2015 retrieved from
For inquiries or feedback, please write or call:
Department of Education – Bureau of Learning Resources (DepEd-BLR)
Ground Floor, Bonifacio Bldg., DepEd Complex Meralco Avenue, Pasig City, Philippines 1600
Telefax: (632) 8634-1072; 8634-1054; 8631-4985
Email Address: blr.lrqad@deped.gov.ph * blr.lrpd@deped.gov.ph
Leave a Reply