Strategic Intervention Materials (SIM) (Plate Boundary Convergence) for Grade 10 Earth Science Students of Don Marcelo C. Marty High School, Brgy. Poblacion North, Sta. Cruz, Zambales. S.Y. 2018-2019
I make this activity sheet for students who were absent during the lesson so they can make it at home.Please seach LP and PPT for these topic which I also uploaded
This is an almost complete instructional material based from MELC in Grade 7 Science.
This is only applicable to the teachers in the Philippines. If you have any questions and wanted to avail the powerpoint you may contact me in my Facebook account: Jady Claire Jackson Lullegao
I make this activity sheet for students who were absent during the lesson so they can make it at home.Please seach LP and PPT for these topic which I also uploaded
This is an almost complete instructional material based from MELC in Grade 7 Science.
This is only applicable to the teachers in the Philippines. If you have any questions and wanted to avail the powerpoint you may contact me in my Facebook account: Jady Claire Jackson Lullegao
LAB MODULE 13 PLATE TECTONICSNote Please refer to the GETTIN.docxVinaOconner450
LAB MODULE 13: PLATE TECTONICS
Note:
Please refer to the GETTING STARTEDmodule to learn how to maneuver through, and how to answer the lab questions, in the Google Earth (
) component.
KEY TERMS
You should know and understand the following terms
:
Continental Drift
Pacific Ring of Fire
Reverse Fault
Earthquakes
Pangaea
Subduction
Hotspots
Plate Convergence
Transform Fault
Normal Fault
Plate Divergence
Overthrust fault
Plate tectonics
LAB MODULE LEARNING OBJECTIVES
After successfully completing this module, you should be able to do the following tasks:
·
Explain the theory of plate tectonics
·
Explain the theory of continental drift
·
Identify and describe types of plate movement
·
Identify and describe the three types of volcanoes
·
Explain the concept of hotspots
·
Compute the rates of plate movement
·
Identify and describe the different types of faults
INTRODUCTION
This module examines plate tectonics. Topics include continental drift, tectonic landforms, plate boundaries, faults and hotspots. While these topics may appear to be disparate, you will learn how they are inherently related. The module starts with four opening topics, or vignettes, which are found in the accompanying Google Earth file. These vignettes introduce basic concepts of the internal structure of the Earth. Some of the vignettes have animations, videos, or short articles that will provide another perspective or visual explanation for the topic at hand. After reading the vignette and associated links, answer the following questions. Please note that some links might take a while to download based on your Internet speed.
Expandthe
INTRODUCTION
folder and then check
Topic 1: Introduction
.
Read
Topic 1: Introduction
Question 1:
Based on this map, what is one continent in which the there are two (or more) plates?
A.
North America
B.
Europe
C.
Asia
D.
Africa
Read
Topic 2: Continental Drift
Question 2:
What was discovered in Antarctica that solidified Wegener’s theory of continental drift?
A.
Snow and ice
B.
Mineral deposits
C.
Tropical plant fossils
D.
Extinct volcanoes
Read
Topic 3:
Tectonic Landforms
Question 3:
Where do scientists think the next major ocean will be formed?
A.
Gulf of Mexico
B.
Iceland
C.
Australia
D.
East Africa
Read
Topic 4:
Human Interaction
Question 4:
Based on the article, w
hich is not a reason why humans are drawn to plate boundaries.
A.
Nice scenery
B.
Geothermal energy
C.
Fertile soil
D.
Ore deposits
Collapse and uncheck the
Introduction
folder.
GLOBAL PERSPECTIVE
Expand
GLOBAL PERSPECTIVE
. Double-click and select
Tectonic Plate Boundaries and Names
to display the names on the globe of the major tectonic plates.
Millions of humans live near the major tectonic plate boundaries. The potential dangers of living on or near a plate boundary include earthquakes, volcanoes, and tsunamis. However, these natural hazards do little to discourage people f.
Deadline is on Tuesday ,September 16 th2014I would like to .docxtheodorelove43763
Deadline is on Tuesday ,September 16 th/2014
I would like to have a design of the four broadcast protocols using a written description with the graphic representation showing how the design looks like and how information/communication happen between nodes beside the details explanation using scenarios to estimate the complexity.
Each of the designs should have an evaluation of the efficiency in the context of message complexity and round complexity.
The design should be based on a cube system with 8 nodes using
1. message-passing model
2. shared-memory model
3. mobile agent communication model
So the final work will have a total of 4 graphic designs with use case scenarios for each design to explain and calculate the complexity and efficiently of each design. The efficiency would be calculated for each design in term of message complexity and round complexity. Then decide on the best protocol among the proposed designs based on the efficiency.
geology2.pdf
geology1.pdf
1
Plate Tectonics Name: ________________
INTRODUCTION
Plate tectonics is a well established theory that unifies and provides a framework for
all geologic observations. Most geologic phenomenon observed near the Earth’s
surface are linked in some way to plate tectonic processes. The theory states that the
outer 60-100 km of the Earth is divided into slabs of rigid rock (the lithosphere). These
slabs (the plates) rest upon a semi-viscous layer of easily deformable rock (the
asthenosphere). Thermal convection within the asthenosphere pushes the plates in
horizontal directions at rates ranging from 1 cm to 12 cm/year. This causes the plates
to move in relation to one another. Boundaries between the 8 principle plates and
several smaller plates are zones of rock deformation, earthquakes and volcanism.
This lab utilizes real data that demonstrates and/or validates the theory of Plate
Tectonics. Four exercises, modified from Jones and Jones (2003), follow.
o Part A examines global maps of tectonic plate boundaries and earthquake data
to identify plate boundary locations and assess relative motion between the
plates.
o Part B uses maps of the ocean floor to calculate spreading rates across a mid-
oceanic ridge in the South Pacific.
o Part C interprets maps and utilizes geologic ages for Hawaiian Islands to better
understand movement of the underlying Pacific plate over a “hot spot”.
o Part D examines a geologic map along a portion of the San Andreas Fault to
evaluate the direction and rate of plate movement.
OBJECTIVES
Upon completion of this exercise, you will be able to understand:
1. basic differences between major types of plate boundaries.
2. magnetic stripping and use it to calculate spreading rates
3. the concept of “hot spots” and use this understanding to determine the speed
and direction of movement of plates
4. how to interpret a geological map of the San Andreas Fault and calculate the
rate of movement al.
Download the paper to access it as a word document
This is an exam style question paper (if any doubts, just comment and within days I will reply). I hope you like this. Please like and also download the pdf so you can have it as reference. Moreover, I have combined all past papers into one which is in your hands now. Please, do not hesitate if you have any doubts regarding plate boundaries/tectonic plates or even any comments to improve my work.
This tacklesabout locating epicenter,3 typesof plate boundaries hotspot.
A ppt presentation for module 1 in 1st quarter in grade 10sciencein the Philippines.
Feel free tomessage mefor any corrections/suggestions forimprovement.
The topic of plate tectonics is largely based on Alfred Wegner's theory of continental drift, which became accepted with the discovery of seafloor spreading in the Atlantic Ocean, and after fossil, flora, and geological studies in Africa and South America. In this lesson, students will learn about Earth’s structure, differences between various types of tectonic plate boundaries, their outcomes, and their connection to locations of volcanoes and earthquake activity.
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
Biological screening of herbal drugs: Introduction and Need for
Phyto-Pharmacological Screening, New Strategies for evaluating
Natural Products, In vitro evaluation techniques for Antioxidants, Antimicrobial and Anticancer drugs. In vivo evaluation techniques
for Anti-inflammatory, Antiulcer, Anticancer, Wound healing, Antidiabetic, Hepatoprotective, Cardio protective, Diuretics and
Antifertility, Toxicity studies as per OECD guidelines
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
Instructions for Submissions thorugh G- Classroom.pptxJheel Barad
This presentation provides a briefing on how to upload submissions and documents in Google Classroom. It was prepared as part of an orientation for new Sainik School in-service teacher trainees. As a training officer, my goal is to ensure that you are comfortable and proficient with this essential tool for managing assignments and fostering student engagement.
Introduction to AI for Nonprofits with Tapp NetworkTechSoup
Dive into the world of AI! Experts Jon Hill and Tareq Monaur will guide you through AI's role in enhancing nonprofit websites and basic marketing strategies, making it easy to understand and apply.
Honest Reviews of Tim Han LMA Course Program.pptxtimhan337
Personal development courses are widely available today, with each one promising life-changing outcomes. Tim Han’s Life Mastery Achievers (LMA) Course has drawn a lot of interest. In addition to offering my frank assessment of Success Insider’s LMA Course, this piece examines the course’s effects via a variety of Tim Han LMA course reviews and Success Insider comments.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
For more information, visit-www.vavaclasses.com
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
1. Department of Education
Region III
Division of Zambales
DON MARCELO C. MARTY HIGH SCHOOL
Poblacion North, Sta. Cruz, Zambales
STRATEGIC INTERVENTION MATERIALS (SIM)
SCIENCE 10
John Paul A. Montalla
T-1
TITLE CARD
2. OBJECTIVES
This Strategic Learning Material will focused on “Plate
Boundary Convergence—types, geologic features and events”.
At the end of this intervention, learners are expected to
accomplish the following objectives;
1. Identify the characteristics of a Convergent plate boundary
movement.
2. Recognize the different types of plate convergence
3. Predict the possible geologic formations found on plate convergence.
4. Give the possible geological phenomena occur on plate convergence.
GUIDE CARD 1
3. LEAST LEARNED CONCEPT
• Explain the different processes that occur
along the “convergent” plate boundaries.
(S9ES-Ia-j-36.3)
GUIDE CARD 2
4. OVERVIEW
Plate boundaries are the line between two different plates—and
they are in constant movement!
There are three types of Plate Tectonic Boundaries which are
classified according to plate movements—the Divergent, the
Transform fault and the CONVERGENT PLATE BOUNDARIES.
Plate movements contribute to the formation of geologic
features and occurrence of different geological phenomena.
Types of crust (oceanic or continental) is a factor to be consider
in predicting geologic formations on convergence boundaries.
GUIDE CARD 3
6. LET’S CROSS IT OUT!
Put an “X” on the type of Convergence/s best described by the
following statement. (Note: C-C-C known as continental-continental
convergence, O-O-C means oceanic-oceanic convergence, and C-O-C stands for
continental-oceanic convergence.)
CHARACTERISTICS C-C-C O-O-C C-O-C
Combination of oceanic and Continental crust
Convergence of two less dense type of crust.
Two thin crusts that move towards one another
Presence of subduction zones
Occurrence of Earthquakes
Occurrence of Tsunami
ACTIVITY CARD 2
7. B
PREDICT THE FEATURE
Through the use of the clue pictures, identify the geologic feature
formed in (a) OCEANIC-OCEANIC and OCEANIC-CONTINENTAL
and (b) CONTINENTAL-CONTINENTAL convergence
A
ACTIVITY CARD 3
8. CLUTTERED PHENOMENA!
Arrange the jumbled letters to identify the different geological
phenomena describe by the following statement.
ACTIVITY CARD 4
DESCRIPTIONS GEOLOGIC EVENTS
The source of molten materials from the mantle that causes
volcanic island arc.
TANMEL UMPLE
An event in convergence known as a destructive
underwater earthquakes that can generate series of ocean
waves with very long wavelengths
ITAUNMS
The vibration of Earth due to rapid release of energy,
naturally occur in any plate movement.
HEERAAQKTU
A concentration of heat in the mantle, during convergence,
capable of creating magma.
OHT OSPT
An event in which a slab of rock thrusts into the mantle. TISDOBUNUC
9. IDENTITY REVELATION
Determine if the following statement describe characteristic of
DIVERGENCE, CONVERGENCE or TRANSFORM-FAULT.
________________1. A boundary in which two plates move toward each other.
________________2. A region where the crustal plates are moving apart.
________________3. A boundary produced when two plates slide past each other.
________________4. The plate boundary that can produce shallow earthquakes.
________________5. The type of plate boundary where trench and volcanic island can be formed
________________6. Plate boundary also known as the “destructive boundary”.
________________7. Plate boundary also known as the “constructive boundary”.
________________8. Plate boundary where subduction process can only occur.
________________9. A boundary that can only form mountains and mountain ranges.
________________10. The Plate boundary movement of the Philippine Plate.
ASSESSMENT CARD 1
10. SHADE TO BE RECOGNIZED
Shade “CC” if the statement describes the characteristic of
continental-continental, “OO” if oceanic-oceanic, and “CO”
for continental-oceanic convergence.
CC OO CO 1. Convergence that give rises to formation of volcanoes
CC OO CO 2. Convergence that forms the Sierra Madre Mountain ranges
CC OO CO 3. Convergence present in the Philippine plate.
CC OO CO 4. Convergence that can generates underwater earthquakes.
CC OO CO 5. Convergence that give rises to formation of trenches and
volcanic island arcs
ASSESSMENT CARD 2
12. PHENOME-(a)NALOGY
Complete the following analogy of the geologic events
associated in Convergent Plate Boundary Movements.
1) C-C Convergence : Earthquakes :: O-O Convergence : _______________
2) Mountains : C-C Convergence :: ______________ : O-C Convergence
3) Upward movement : C-C Convergence :: ___________ : O-C Convergence
4) Mantle Plume : O-C Convergence :: _______________ : O-O Convergence
5) Seafloor: Sedimentation process :: Trenches : ______________________
ASSESSMENT CARD 4
13. QUAKE-IT-OFF!
Convergence of plate boundaries cause movement of crust that can bring harsh and
destructive earthquakes. Being part of a converging plate, the Philippines is prone
to many earthquake attacks.
The government invested lots of effort to instill preparedness on earthquake
emergencies among Filipino students.
What are the things we need to do BEFORE, DURING and AFTER EARTHQUAKES?
ENRICHMENT CARD 1
Before Earthquake During Earthquake After Earthquake
• • •
• • •
• • •
14. MY “EARTHQUAKEMERGENCY” KIT
Illustrate on the box the 15 things that you need to have in your
“Family Emergency Kit” that can be use during or after a
disaster.
ENRICHMENT CARD 2
16. LET’S CROSS IT OUT!
Put an “X” on the type of Convergence/s best described by the
following statement. (Note: C-C-C known as continental-continental
convergence, O-O-C means oceanic-oceanic convergence, and C-O-C stands for
continental-oceanic convergence.)
CHARACTERISTICS C-C-C O-O-C C-O-C
Combination of oceanic and continental crust X
Convergence of two less dense type of crust. X
Two thin crusts that move towards one another X
Presence of subduction zones X X
Occurrence of Earthquakes X X X
Occurrence of Tsunami X X
ANSWER CARD 2
17. B
PREDICT THE FEATURE
Through the use of the clue pictures, identify the geologic feature
formed in (a) OCEANIC-OCEANIC and OCEANIC-CONTINENTAL
and (b) CONTINENTAL-CONTINENTAL convergence
A
ANSWER CARD 3
VOLCANIC ISLAND ARC
VOLCANOES
TRENCHES
MOUNTAINS
MOUNTAIN RANGES
18. CLUTTERED PHENOMENA!
Arrange the jumbled letters to identify the different geological
phenomena describe by the following statement.
ANSWER CARD 4
DESCRIPTIONS GEOLOGIC EVENTS
The source of molten materials from the mantle that causes
volcanic island arc.
MANTLE PLUME
An event in convergence known as a destructive
underwater earthquakes that can generate series of ocean
waves with very long wavelengths
TSUNAMI
The vibration of Earth due to rapid release of energy,
naturally occur in any plate movement.
EARTHQUAKE
A concentration of heat in the mantle, during convergence,
capable of creating magma.
HOT SPOT
An event in which a slab of rock thrusts into the mantle. SUBDUCTION
19. IDENTITY REVELATION
Determine if the following statement describe characteristic of
DIVERGENCE, CONVERGENCE or TRANSFORM-FAULT.
CONVERGENCE 1. A boundary in which two plates move toward each other.
DIVERGENCE 2. A region where the crustal plates are moving apart.
TRANSFORM-FAULT 3. A boundary produced when two plates slide past each other.
TRANSFORM-FAULT 4. The plate boundary that can produce shallow earthquakes.
CONVERGENCE 5. The type of plate boundary where trench and volcanic island can be formed
CONVERGENCE 6. Plate boundary also known as the “destructive boundary”.
DIVERGENCE 7. Plate boundary also known as the “constructive boundary”.
CONVERGENCE 8. Plate boundary where subduction process can only occur.
CONVERGENCE 9. A boundary that can only form mountains and mountain ranges.
CONVERGENCE 10. The Plate boundary movement of the Philippine Plate.
ANSWER CARD 5
20. SHADE TO BE RECOGNIZED
Shade “CC” if the statement describes the characteristic of
continental-continental, “OO” if oceanic-oceanic, and “CO”
for continental-oceanic convergence.
CC OO CO 1. Convergence that give rises to formation of volcanoes
CC OO CO 2. Convergence that forms the Sierra Madre Mountain ranges
CC OO CO 3. Convergence present in the Philippine plate.
CC OO CO 4. Convergence that can generates underwater earthquakes.
CC OO CO 5. Convergence that give rises to formation of trenches and
volcanic island arcs
ANSWER CARD 6
21. PREDICTION IS COMPLETE…
Complete the following convergence sentence-
equation of expected geologic formations.
1. [Volcanic Island Arc]= CONVERGNENCE (Oceanic + Oceanic) –Trench.
2. Trench = CONVERGENCE (Oceanic + Continental) –[Volcano]
3. [Mountains] = CONVERGENCE (Continental + Continental)
4. Volcano = CONVERGENCE (Oceanic + [Continental]) – Trench.
5. Volcanic Island Arc = CONVERGENCE (Oceanic-Oceanic) –[Trench].
ANSWER CARD 7
22. PHENOME-(a)NALOGY
Complete the following analogy of the geologic events
associated in Convergent Plate Boundary Movements.
1) C-C Convergence : Earthquakes :: O-O Convergence : TSUNAMIS
2) Mountains : C-C Convergence :: VOLCANOES: O-C Convergence
3) Upward movement : C-C Convergence :: SUBDUCTION : O-C Convergence
4) Mantle Plume : O-C Convergence :: HOT SPOT : O-O Convergence
5) Seafloor: Sedimentation process :: Trenches : SUBDUCTION PROCESS
ANSWER CARD 8
23. THANK YOU VERY MUCH!!!
Department of Education, Bureau of Secondary Education.
Project EASE Integrated Science 1, Module 12 : Inside
Earth.
Department of Education, Bureau of Secondary Education
(2013). Science Grade 8 Learner’s Module. Vibal
Publishing House, Inc.
Tarbuck, E.J. et al. (2009). Earth Science 12th ed. Pearson
Education South Asia Pte Ltd.
http://www.skoool.ie/ accessed March 3, 2014
http://earthds.info/ accessed March 3, 2014
http://www.platetectonics.com accessed March 5, 2014
REFERENCE CARD 8