MELC BASED GRADE 10 SCIENCE QUARTER 1, MODULE 1: PLATE TECTONICS ( TAGALOG ) EINSTEINATICS TV

Einsteinatics tv
26 Sept 202016:53

Summary

TLDRThis educational video script explores the concept of plate tectonics, focusing on its significance in understanding Earth's geological activities. It reviews key concepts from grades 7 to 10, highlighting the lithospheric plates, their movements, and the three types of plate boundaries: divergent, convergent, and transform. The script clarifies misconceptions about the Earth's crust and asthenosphere, and uses examples like the San Andreas Fault to illustrate the impact of tectonic plate interactions on natural phenomena such as earthquakes and volcanic eruptions.

Takeaways

  • 🌏 The script covers a range of geological concepts from tectonics, subgrade, earthquakes, volcanic eruptions, weather patterns, and motions of the Earth, to solar systems and celestial phenomena.
  • 📚 It reviews learning materials for different grade levels, specifically focusing on plate tectonics for grade 10, which is a central topic for understanding Earth's geological activity.
  • 🔍 The script introduces the concept of plate tectonics, explaining the movement and interaction of Earth's lithospheric plates, and how they are instrumental in various geological phenomena.
  • 📏 It discusses the six activities in the learner's module for the first quarter, which seem to be designed to engage students in understanding the dynamics of plate tectonics.
  • 🌌 The script touches on the concept of the asthenosphere, clarifying that it is a viscoelastic solid beneath the lithospheric plates, not a liquid.
  • đŸ”ïž It explains the three types of plate boundaries: divergent, convergent, and transform, each with distinct geological implications such as the formation of mountains and volcanic island arcs.
  • 🌋 The script highlights the relationship between plate boundaries and seismic and volcanic activities, noting that these natural phenomena often occur at these boundaries.
  • 🌍 It mentions the eight primary plates, including the Eurasian, Philippine, Australian, Pacific, South American, Cocos, and Antarctic plates, and how they are identified through seismic activity, volcano locations, and mountain belts.
  • 📉 The movement of tectonic plates is described as slow, typically 1 to 10 centimeters per year, but significant over millions of years.
  • 🌐 The script dispels a common misconception about the asthenosphere, emphasizing that it is not liquid but behaves like a solid that can flow and deform over geological time.
  • 🔗 It concludes with an invitation for viewers to like, subscribe, and share the content to spread knowledge about plate tectonics.

Q & A

  • What is the main focus of the first quarter's module for Grade 10 in the context of this script?

    -The main focus of the first quarter's module for Grade 10 is plate tectonics, specifically covering the Earth's interior and the dynamics of tectonic plates.

  • What are the six activities included in the learner's module for understanding plate tectonics?

    -The six activities are: Activity 1 - Find the Center, Activity 2 - Let's Mark Your Boundaries, Activity 3 - Hidden Collision, Activity 4 - Going Separate Ways, Activity 5 - Slide and Shake, and Activity 6 - Drop It Like a Setback.

  • How do scientists determine the different types of lithospheric plates?

    -Scientists determine the different types of lithospheric plates based on seismicity, the distribution of earthquakes, the location of volcanoes, and the location of major mountain belts.

  • What is the average speed at which tectonic plates move?

    -Tectonic plates move very slowly, at an average speed of 1 to 10 centimeters per year.

  • What is the difference between the Earth's crust and lithospheric plates?

    -The Earth's crust is the outermost layer of the Earth, chemically distinct from the underlying mantle layer. Lithospheric plates, on the other hand, include not only the crust but also the uppermost part of the mantle, making them thicker and more rigid.

  • What is the asthenosphere, and how is it different from the Earth's mantle?

    -The asthenosphere is a part of the upper mantle that lies below the lithospheric plates. Unlike the solid mantle, the asthenosphere is viscoelastic, meaning it can flow and deform under stress over geological timescales.

  • What are the three types of plate boundaries?

    -The three types of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move towards each other; and transform boundaries, where plates slide past each other.

  • What happens at an oceanic-continental convergent boundary?

    -At an oceanic-continental convergent boundary, the denser oceanic plate is subducted beneath the lighter continental plate, often leading to the formation of volcanic arcs and strong earthquakes.

  • How do two continental plates interact at a convergent boundary?

    -When two continental plates interact at a convergent boundary, they collide and push up against each other, resulting in the formation of large mountain ranges, such as the Himalayas.

  • What is a transform boundary, and what is an example of this type of boundary?

    -A transform boundary is where two plates slide past each other horizontally. An example of a transform boundary is the San Andreas Fault in California, USA.

  • What is the significance of understanding plate tectonics in the context of the Earth's geological activity?

    -Understanding plate tectonics is crucial as it helps explain the movement of the Earth's crust, the formation of various geological features like mountains and volcanoes, and the occurrence of earthquakes and tsunamis.

Outlines

00:00

🌏 Plate Tectonics and Earth's Dynamics

This paragraph introduces the concept of plate tectonics, which is a fundamental topic in geology for students from grades 7 to 10. It emphasizes the importance of understanding the movements of the Earth's crust, including tectonics, volcanic eruptions, earthquakes, and weather patterns. The script mentions various activities designed to engage learners in the study of these geological phenomena, such as finding the center of tectonic plates, marking boundaries, and understanding the dynamics of continental drift. The paragraph also includes a brief musical interlude, suggesting an educational yet entertaining approach to the subject.

05:36

🌍 Earth's Lithospheric Plates and Their Movements

The second paragraph delves into the specifics of the Earth's lithospheric plates, explaining that they include both the crust and the upper mantle. It outlines the eight primary plates, such as the Eurasian, Philippine, Australian, Pacific, South American, Cocos, and Antarctic plates, and discusses how scientists identify and study these plates using seismic activity, the location of volcanoes, and major mountain belts. The paragraph also clarifies misconceptions about the asthenosphere, which is a viscoelastic solid rather than a liquid, and touches on the slow but significant movement of tectonic plates, which can be measured in centimeters per year over long geological timescales.

10:38

đŸ”ïž Types of Plate Boundaries and Their Geological Impacts

This paragraph focuses on the three main types of plate boundaries: divergent, convergent, and transform. It describes how these boundaries affect the Earth's crust, leading to the formation of mountains, earthquakes, and volcanic activity. The script provides examples of each type, such as the formation of volcanic island arcs at oceanic-oceanic convergent boundaries and the creation of mountain ranges like the Himalayas at continental-continental convergent boundaries. It also mentions the San Andreas Fault as a prominent example of a transform boundary. The paragraph aims to differentiate these boundaries and their effects on the Earth's geological features.

15:44

📚 Understanding Plate Tectonics for Educational Growth

The final paragraph serves as a conclusion, summarizing the importance of understanding plate tectonics and encouraging viewers to engage with the content by liking, subscribing, and sharing the video. It highlights the educational value of the video in helping students grasp the concept of plate tectonics, which is crucial for their academic development. The speaker, Cinatix, thanks the viewers for watching and invites them to continue learning about the Earth's dynamic processes in future videos.

Mindmap

Keywords

💡Tectonics

Tectonics refers to the study of the structure, dynamics, and changes within the Earth's crust. In the context of the video, tectonics is the main theme, focusing on the movement and interaction of the Earth's lithospheric plates, which is essential for understanding various geological phenomena such as earthquakes and volcanic eruptions. The script mentions 'plate tectonics' as a key topic for Grade 10, indicating its significance in the curriculum.

💡Subgrade

Although 'subgrade' is not explicitly defined in the script, it generally refers to the layer of soil or material beneath a constructed surface, which is important in civil engineering and construction. In the video's context, it might be used metaphorically to indicate foundational knowledge or the basic layer of understanding required before delving into more complex concepts like plate tectonics.

💡Earth's Interior

The Earth's interior encompasses the layers beneath the surface, including the crust, mantle, and core. The script discusses this concept as part of the first quarter's module, emphasizing the importance of understanding the structure of the Earth for studying tectonics. It helps explain the dynamics that drive plate movements and the generation of geological activities.

💡Volcanic Eruptions

Volcanic eruptions are the release of molten rock, ash, and gases from a vent in the Earth's crust. The script connects volcanic eruptions to tectonics, particularly at convergent boundaries where one tectonic plate is forced under another, leading to the formation of volcanoes. This is a key concept in understanding the script's discussion on the relationship between plate tectonics and volcanic activity.

💡Weather Patterns

Weather patterns refer to the regular atmospheric conditions in a region over time. While not the main focus of the script, weather patterns can be influenced by tectonic activities, such as the formation of mountains that affect wind and precipitation. The script lists weather patterns as part of the broader learning context for students studying tectonics.

💡Plate Boundaries

Plate boundaries are the edges where tectonic plates meet and interact. The script explains that there are eight primary plates and discusses how scientists identify these boundaries based on seismic activity and the location of volcanoes and mountain belts. Understanding plate boundaries is crucial for the script's exploration of tectonic activities and their effects on Earth's surface.

💡Seismicity

Seismicity is the distribution of earthquakes in a given region. The script uses seismicity as a basis for identifying plate boundaries, as areas with high seismic activity often coincide with these boundaries. This term is central to the video's discussion on how scientists determine the locations and movements of tectonic plates.

💡Convergent Boundaries

Convergent boundaries occur where two tectonic plates move towards each other. The script describes different types of convergent boundaries, such as oceanic-to-oceanic and oceanic-to-continental plate convergences, which can lead to the formation of volcanic island arcs and mountain ranges, respectively. This concept is key to understanding the video's explanation of how certain geological features are formed.

💡Transform Boundaries

Transform boundaries are where two plates slide past each other horizontally. The script uses the San Andreas Fault in California as an example of a transform boundary, which is characterized by frequent earthquakes due to the friction and movement between plates. This term is important for the video's discussion on the different types of plate interactions and their geological implications.

💡Asthenosphere

The asthenosphere is a part of the upper mantle that lies below the lithospheric plates. The script clarifies a misconception about the asthenosphere, stating that it is viscoelastic, meaning it can flow and deform under stress, which is important for understanding plate movement. This term is relevant to the video's explanation of the dynamics beneath the Earth's crust.

💡Lithospheric Plates

Lithospheric plates, also known as tectonic plates, include the rigid upper part of the mantle along with the crust. The script explains that these plates are rigid and brittle, which is why they can break and cause earthquakes. The concept of lithospheric plates is fundamental to the video's theme, as it discusses their movement and interaction as the driving force behind various geological phenomena.

Highlights

Introduction to the concept of plate tectonics and its importance in understanding Earth's geological activities.

Review of past concepts on tectonics, subgrade, earthquakes, volcanic eruptions, weather patterns, and motions of the Earth.

Discussion on the solar system, constellations, and the Philippine environment's interactions with Earth's movements.

Explanation of the learning supply for grades 7 to 10, focusing on plate tectonics, earthquakes, and volcanoes.

Description of the learner's module comprising six activities to understand plate tectonics.

Activity 1: Finding the centers of tectonic plates and their significance.

Activity 2: Marking boundaries and the role of plate boundaries in geological events.

Activity 3: Hidden collision and the process of plates moving apart.

Activity 4: Going separate ways and the formation of new crust.

Activity 5: Slide and shake, illustrating the effects of earthquakes.

Activity 6: Dynamic Earth, exploring the movement of continents and the speed of plate tectonics.

Clarification of the misconception about the asthenosphere and its properties.

Differentiation between the three types of plate boundaries: divergent, convergent, and transform.

Explanation of how earthquakes and volcanoes are associated with plate boundaries.

The role of seismicity in identifying the boundaries of tectonic plates.

The significance of the lithosphere in the context of plate tectonics and its composition.

The movement of tectonic plates and its impact over geological time scales.

The formation of volcanic island arcs and mountain ranges due to plate interactions.

The San Andreas Fault as an example of a transform boundary and its seismic activity.

Encouragement to like, subscribe, and share the channel for further understanding of plate tectonics.

Transcripts

play00:28

learnings

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so let's get right to it let us review

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human

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past concepts that you could use for

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your learning supply tectonics

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subgrade six nanjing tatlong module

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engineering earthquake volcanic

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eruptions weather patterns motions of

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the earth

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achakayon solar systems a great seven

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amman and genuine philippine environment

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interactions champion seasons and

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eclipses so grade 8

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and genuine earthquakes faults

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understanding typhoons and other members

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of the solar system

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grade nine volcanoes climate

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constellations a grade 10 delaware focus

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plate tectonics at chakayong earth's

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interior

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specific concepts and autotune from

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grades 7 to 10

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which would be instrumental to fully

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understand jung topic natanza grade 10

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which is

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plate tectonics

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[Music]

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do

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[Music]

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if we are going to look at it closely

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delavalang you main focus

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on first quarter your module one you can

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play tectonics

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module 2 earth's interior

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modules revolve

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for the first quarter

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so here's a closer look

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learner's module it comprises of six

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activities

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i saw so you might want to try this out

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so binobu channel 6 activities activity

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1

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find the center activity 2 let's mark

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your boundaries activity 3

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hidden collision four going separate

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ways five slide and shake

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drop it like a setback suck cv6 at chaka

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find the centers activity seven

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young activities

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amazing graves dynamic earth let's fit

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it

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engendering young drifting suffering

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continents split and separate

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how fast does it go

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[Music]

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mundo

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it would rise up once it reaches the top

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it would cool off or lala migsha and

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then it would be

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pushed back down so yeah and then when

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it reaches again a certain temperature

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tatas

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primary plates includes eurasia plate

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one de

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philippine australian pacific nazga

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south american you have also cocos plate

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antarctic plate at

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ibapa so yumibang manga plates

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contain satania

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and that is because from what we learned

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earlier because of conviction current

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quick question manaka einstein do you

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have any idea

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as to how they come up with this design

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of the plate boundaries

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how did they identify that there are

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eight primary

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boundaries or there are eight primary

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plates government basilan and several

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instruments

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like explore basilas

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what was the basis for

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the design of the tectonic plates

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the first basis for the boundaries of

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the tectonic plates

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is what you call a seismicity at

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chakayong distribution of earthquakes in

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other words

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linda

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another quick question

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deepist earthquakes based on the diagram

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okay so you still have

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15 seconds left

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remember

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einstein

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[Music]

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you still have ten nine eight

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seven six five four three

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two and ayan so completing the nut in

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sama

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where there are earthquakes there are

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also volcanoes

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and most likely volcanoes

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on the plate boundaries

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favorite place so

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in order for the scientists to determine

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what are the different type of

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lithospheric plates

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so you have this missibility

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another is location of volcanoes

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and the last one are the location of

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major mountain belts

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so you might be wondering

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so actually guma galosha but it moves

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very slow

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so 1 to 10 centimeters long per year so

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about

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it isn't much but if you are going to

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multiply it

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by say a millions of years then

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definitely

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young distance or your movement would be

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very evident or capable

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so young's lowest ay nasa african plate

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young fastest

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microplate let's learn more about

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tectonic plates tectonic plates like

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what we said is also known as the

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lithospheric plates

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now let us put this straight

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hum crust achaka young lettuce fairy

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plates are

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makaiba when we talk about lithospheric

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plates

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kabilangadito young crushed upper

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mountain

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when we talk about the crust it is the

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outer rack layer of the earth

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chemically distinct from the underlying

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mantle layer

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so young crust is only a part of

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the lithospheric plates when we talk

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about the atmospheric plates it is rigid

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and

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brittle contains grass and upper mantle

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100 kilometers thick

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at merengue fractures

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[Music]

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earthquake

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now let's proceed to another

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misconception

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uh that pertains to asthenosphere when

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we talk about asthenosphere

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etou young hatter upper mantel below the

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lithospheric plates

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so young asthenosphere malaysian

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liquid actually it is viscoelastic

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solid okay so meaning

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liquid smoke flow cooperation and

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plastic

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now let's proceed to the different type

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of plate boundaries

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actually there are three types of plate

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boundaries

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convergent boundary and the third type

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is the transform boundary

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now naka depending in between this

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lithospheric plates effect tonito

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earth's crust

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mountains now let us try to

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differentiate between the three

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boundaries

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the first type is the divergent boundary

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places with this type of

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boundaries as earthquakes

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as it pulls apart virgin boundaries

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plates next type of plate boundary is

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convergent

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boundaries

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the next type of boundary is what you

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call

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as convergent boundaries now there are

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three main types

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for this type of boundaries anjan young

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oceanic toshanek plate convergence

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another is oceanic

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continental place there are two main

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concepts

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einstein you must or you did surpass

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with this type of events now oceanic

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oceanic plate convergence

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so it could form volcanic island arcs

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it is because

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because this is where the strong

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earthquakes or

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originate aside from that

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tsunami because of convergent boundaries

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between ocean to continental plate but

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instead volcanic island

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are you

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now let's proceed to another type of

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boundary

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yongsa convergent boundary and that is

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between

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two continental plates now

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and it would form now a mountain

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so this is how mount everest was formed

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junglas type boundary is what you call

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as transform

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in this type of boundary

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class casino pass each other

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but definitely it would surely cause

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earthquakes one clear example of this

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one

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is yung san andreas fault in california

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in the united states of

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america so here are the different

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sources

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napoleon in order for you to fully

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understand

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about plate tectonics channel

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please do not forget to click like and

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subscribe and share it to your

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classmates

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so that others would also learn so till

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next time i'm cinatix

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thank you for watching

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you

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