BAB 6 STRUKTUR BUMI DAN PERKEMBANGANNYA BAGIAN 2 - IPA Kelas 8 Kurikulum Merdeka

gurukelas
10 Dec 202309:27

Summary

TLDRIn this educational video for 8th grade science, the focus is on Chapter 6, 'The Structure of Earth and Its Development' under the Merdeka curriculum. It explores various types of earthquakes including tectonic, volcanic, collapse, impact, and human-induced, detailing their causes and effects. The script delves into key geological terms like hypocenter and epicenter, and explains seismic waves. The video also discusses the categorization of earthquakes by strength and the phenomena of aftershocks. Additionally, it covers the significant role of volcanic activity in Indonesia, describing the benefits of volcanoes to the environment, economy, and geology.

Takeaways

  • 🌍 Chapter 6 covers Earth's structure and development, specifically focusing on plate tectonics and their effects, as part of the Merdeka curriculum for eighth grade science.
  • 🌐 Plate movements can cause major natural events such as earthquakes and tsunamis, highlighting the dynamic and interconnected nature of Earth's crust.
  • 🏔️ There are various types of earthquakes: tectonic (due to plate movement), volcanic (caused by magma movement in volcanoes), collapse (triggered by other natural events like landslides), impact (from celestial objects like meteorites), and artificial (human-made through large explosions).
  • 📉 Earthquakes are measured on the Richter scale (or SR scale), proposed by American physicist Charles Richter in 1935, which quantifies the energy and magnitude of seismic events.
  • 🌊 Tsunamis are large ocean waves caused by underwater disturbances such as plate shifts, landslides, volcanic eruptions, or meteor impacts, posing significant risks to coastal areas.
  • 🔍 Key seismic terms include 'hypocenter' (the underground focal point of an earthquake), 'epicenter' (the ground directly above the hypocenter), and seismic waves (energy waves that travel through Earth).
  • 📈 Seismographs are tools used to measure earthquake vibrations, with their recordings called seismograms, which help in understanding and predicting seismic activities.
  • 🔗 Indonesia's geological makeup includes a major volcanic belt extending from Sumatra through Java to the Nusa Tenggara and Sulawesi regions, making it prone to volcanic and seismic activities.
  • 🌋 Volcanoes are prevalent along tectonic plate boundaries, where convergent movements push magma to the surface, causing eruptions of lava, ash, and gases.
  • 🌾 Volcanic activity contributes positively by producing fertile soils, mineral resources, geothermal energy, and stunning landscapes that boost tourism.

Q & A

  • What causes earthquakes according to the video?

    -Earthquakes are caused by the movement of tectonic plates, which can be convergent, divergent, or transform movements.

  • What are the different types of earthquakes mentioned in the script?

    -The script mentions five types of earthquakes: tectonic, volcanic, collapse, impact, and artificial earthquakes.

  • How is the strength of an earthquake measured?

    -The strength of an earthquake is measured using the Richter scale, originally proposed by Charles F. Richter in 1935.

  • What is the difference between the epicenter and the hypocenter of an earthquake?

    -The hypocenter is the point inside the Earth where the earthquake originates, while the epicenter is the point directly above it on the surface of the Earth.

  • What can trigger a tsunami as described in the video?

    -A tsunami can be triggered by underwater disturbances such as tectonic plate shifts, landslides, volcanic eruptions, or the impact of large celestial bodies like meteorites.

  • What are seismic waves and what types are mentioned?

    -Seismic waves are vibrations that travel through the Earth's crust during an earthquake. The script mentions two types: longitudinal (compression) waves and transverse waves.

  • What are the benefits of having volcanoes, according to the video?

    -Volcanoes provide benefits such as rich mineral resources, fossil fuels like oil, geothermal energy, and fertile volcanic soil that supports agriculture.

  • What is the significance of the seismograph and seismogram in understanding earthquakes?

    -A seismograph is an instrument used to record the vibrations of earthquakes, and a seismogram is the actual record or diagram of the seismic waves produced by an earthquake.

  • What is the role of volcanic activity in the formation of islands like Indonesia?

    -Volcanic activity, particularly along tectonic plate boundaries, leads to the formation of volcanic islands such as those found in Indonesia.

  • What precautions should be taken after a major earthquake, as advised in the video?

    -After a major earthquake, it is recommended to avoid entering buildings and stay in open areas to reduce the risk from aftershocks and potential building collapses.

Outlines

00:00

🌍 Earthquake Types and Terms Explained

This section provides a detailed explanation of various types of earthquakes and related terminologies. Earthquakes can be caused by convergent, divergent, or transform plate movements, leading to different types such as tectonic, volcanic, collapse, impact, and artificial earthquakes. Key terms explained include the hypocenter, the point inside the Earth where the earthquake originates, and the epicenter, directly above it on the surface. Seismic waves, both longitudinal and transverse, are discussed, along with their mechanisms of propagation through the Earth's crust. The earthquake magnitude is measured on a scale developed by Charles F. Richter in 1935.

05:01

🌊 Tsunami Hazards and Volcanic Activities

This section covers the hazards associated with tsunamis and the characteristics of volcanic activities in Indonesia. Tsunamis are large sea waves triggered by underwater disturbances such as tectonic shifts or volcanic eruptions. The discussion includes a geographical overview of volcanic belts in Indonesia and their classification into three types based on historical activity. The benefits of volcanic regions are highlighted, emphasizing rich mineral resources, geothermal energy, and fertile volcanic soils. Additionally, the aesthetic and touristic value of these landscapes is acknowledged.

Mindmap

Keywords

💡Tectonic Plates

Tectonic plates refer to the large and small segments of the Earth's lithosphere which move over the asthenosphere. In the video, the movement of these plates is highlighted as the primary cause of earthquakes. This concept is central as it explains the mechanics behind seismic activity, including divergent, convergent, and transform plate boundaries which lead to various geological phenomena.

💡Earthquake

An earthquake is a sudden, rapid shaking of the Earth caused by the release of energy stored in rocks. It is a key focus in the video, described as resulting from movements at tectonic plate boundaries. Examples include tectonic, volcanic, collapse, and human-induced earthquakes, each defined by their specific causes and effects on the environment and human structures.

💡Seismic Waves

Seismic waves are waves of energy that travel through the Earth's layers, and they are generated by earthquakes, volcanic eruptions, magma movement, large landslides, or large human-made explosions. The video discusses their propagation, distinguishing between longitudinal (compressional) and transverse (shear) waves, and how they affect the Earth's surface.

💡Hypocenter

The hypocenter, or focus, is the point within the Earth where an earthquake rupture starts. The video mentions this term while explaining that the hypocenter is the site of energy release during an earthquake, lying directly beneath the epicenter, which is the point on the Earth's surface located directly above the hypocenter.

💡Epicenter

The epicenter is the point on the Earth's surface directly above the hypocenter of an earthquake. In the video, it is highlighted to help viewers visualize the location of the most intense shaking during an earthquake, which is critical for emergency response and understanding the impacts of seismic events.

💡Seismograph

A seismograph is an instrument used to record the vibrations of the Earth, especially during an earthquake. The video details how seismographs capture the seismic waves and produce a seismogram, which is crucial for analyzing the magnitude and location of the earthquake.

💡Seismogram

A seismogram is the visual record produced by a seismograph. According to the video, it shows the amplitude and frequency of seismic waves as they travel through the Earth, allowing scientists to interpret the details of the earthquake such as its strength and depth.

💡Magnitude Scale

The magnitude scale quantifies the energy released by an earthquake. The video mentions different scales like the Richter Scale, explaining how they classify earthquakes by size and energy release, helping in understanding the potential damage and necessary precautions.

💡Aftershocks

Aftershocks are smaller earthquakes that follow the main shock of a larger earthquake. The video explains that aftershocks occur as the displaced earth adjusts to the effects of the main earthquake, and although they are usually less severe, they can still cause significant damage, especially to structures weakened by the main quake.

💡Tsunami

A tsunami is a series of large ocean waves generated by large undersea disturbances, such as earthquakes, volcanic eruptions, or landslides. The video highlights tsunamis as secondary effects of seismic activity, emphasizing their potential to cause extensive flooding and damage along coastlines.

Highlights

Introduction to the structure of Earth and its development, ideal for Grade 8 science curriculum under the new Merdeka system.

Explanation of tectonic plate movements causing natural disasters such as earthquakes and tsunamis.

Description of different types of earthquakes: tectonic, volcanic, collapse, impact, and human-made.

Details on the epicenter and hypocenter of earthquakes, illustrating the focal points of seismic activity.

Introduction to seismic waves, including longitudinal and transverse waves, and their movements during earthquakes.

Explanation of how earthquakes are measured using seismographs and represented in seismograms.

Discussion on the Richter Scale, developed in 1935 by Charles Richter, for measuring earthquake magnitude.

Insight into aftershocks following major earthquakes due to the stabilization of tectonic plates.

Overview of tsunamis as large ocean waves triggered by underwater disturbances such as landslides or earthquakes.

Mapping of volcanic regions in Indonesia, highlighting areas from Sumatra to Sulawesi vulnerable to volcanic activities.

Classification of volcanic types based on eruption history and current activity levels.

Description of how volcanoes erupt, detailing the movement of magma and the release of lava, ash, and gases.

Listing several significant volcanic eruptions in Indonesia during 2020, including Mount Sinabung and Mount Merapi.

Discussion of the benefits of volcanoes, including mineral resources, oil, geothermal energy, and fertile soil.

Highlighting the role of volcanoes in tourism, showcasing their natural beauty as a tourist attraction.

Transcripts

play00:00

[Musik]

play00:07

jangan lupa like share dan

play00:09

subscribe bab 6 struktur bumi dan

play00:12

perkembangannya pelajaran IPA kelas 8

play00:14

kurikulum

play00:16

Merdeka aktivitas pergerakan lempeng

play00:19

dapat menyebabkan yang pertama gempa

play00:22

bumi Kemudian yang kedua adalah

play00:26

tsunami gempa bumialahcana yang dap bawa

play00:30

kerusakan besar baik pada bangunan Jalan

play00:33

Jembatan alam bahkan hingga merenggut

play00:36

nyawa manusia gemba bumi terjadi akibat

play00:40

pergerakan lempeng baik secara konvergen

play00:43

divergen dan transform Nah inilah contoh

play00:46

gambar di mana ini adalah Gempa bumi

play00:49

yang terjadi di muka

play00:51

bumi macam-macam gempa yang pertama ada

play00:54

gempa tektonik adalah Gempa bumi yang

play00:58

terjadi karena adanya gerakan lempeng

play01:00

bumi yang kedua ada gempa vulkanik

play01:03

terjadi karena pergerakan magma dalam

play01:06

gunung berapi akibat tekanan gas yang

play01:10

ketiga ada gempa runtuhan terjadi akibat

play01:12

peristiwa alam lain yang dapat

play01:14

menyebabkan gempa yaitu tanah longsor

play01:18

yang keempat yaitu gempa tumbukan

play01:20

disebabkan oleh jatuhnya benda langit

play01:23

yang berukuran besar dan berat contohnya

play01:26

meteorit dan Asteroid yang kelima gempa

play01:29

buat dibuat oleh manusia apabila kita

play01:32

menggunakan bahan peledak berskala besar

play01:34

misalnya untuk meruntuhkan gedung-gedung

play01:37

tinggi itulah kelima macam-macam gempa

play01:40

istilah-istilah dalam gempa bumi yang

play01:42

pertama ada hiposentrum yaitu sumber di

play01:46

dalam bumi tempat terjadinya gempa atau

play01:49

titik pusat gempa kemudian ada gelombang

play01:52

seismik adalah energi dalam bentuk

play01:55

Getaran yang merambat baik dalam

play01:58

dilempeng bumi dan juga di kerak atau

play02:01

permukaan bumi kemudian ada seismograf

play02:05

adalah alat untuk mengukur besarnya

play02:08

getaran gempa bumi kemudian ada

play02:11

seismogram adalah diagram hasil

play02:14

pengukuran

play02:15

seismograf kekuatan gempa bumi diukur

play02:17

dalam skala r atau SR skala ini

play02:21

diusulkan oleh seorang ahli fisika dari

play02:24

Amerika yang bernama Charles rer Pada

play02:27

tahun

play02:28

1935

play02:30

itulah istilah-istilah dalam gempa

play02:33

bumi nah ini adalah contoh gambar dari

play02:38

hiposentrum dan episentrum hiposentrum

play02:41

itu merupakan titik ya titik gempa yang

play02:44

berada di dalam bumi yang ini kemudian

play02:47

episentrum itu adalah titik gempa di

play02:49

mana titik gempanya itu lurus ya titik

play02:52

gempa yang ada pada permukaan atau kerak

play02:56

bumi yang paling

play02:58

luar berikut gambar gelombang seismik ya

play03:02

ini contoh gelombang longitudinal atau

play03:06

kompresi ya kompresi ini pergerakannya

play03:09

secara lurus ke atas seperti ini ya

play03:13

permukaan bumi didorong dan ditarik jadi

play03:15

ke atas dan ke bawah Ya ini seperti ini

play03:19

seperti loncat ke bawah ke atas kalau

play03:22

secara gelombang transversal saismiknya

play03:24

itu eh bergetarnya itu ke kiri dan ke

play03:28

kanan seperti ini seperti digeser-geser

play03:31

gitu perbedaan antara gelombang

play03:33

longitudina dan transversar pada ee

play03:36

gempa bumi atau yang menjadikan

play03:38

gelombang

play03:40

seismik kategori gempa berdasarkan

play03:43

Kekuatan gempa yang pertama

play03:45

ini lebih dari Del itu dikategorikan

play03:50

sebagai gempa yang sangat besar kemudian

play03:52

7 sampai 7,9 ini besar kemudian 6 sampai

play03:58

6,9 skala liter ya skala liter untuk

play04:01

ukuran gempa ini ini kuat kemudian 5

play04:05

sampai 5,9 ini sedang 4 sampai 4,9 ini

play04:09

kategori ringan kemudian 3 sampai dengan

play04:13

3,9 itu kategori minor itulah eh tabel

play04:17

kategori gempa berdasarkan kekuatan

play04:21

gempanya bencana yang terjadi segerah

play04:23

gempa itu yang pertama adalah gempa

play04:25

susulan Nah setelah gempa utama yang

play04:28

berm ini tudo besar lempeng bumi yang

play04:31

telah bergerak karena saling bertumbukan

play04:33

atau bergesekan membutuhkan waktu untuk

play04:35

kembali ke posisi stabil pergerakan

play04:38

kembalinya lempeng bumi ke posisi stabil

play04:40

setelah gempa utama ini ya yang

play04:44

menyebabkan gempa susulan jadi ketika

play04:46

gempa gempa utama atau gu ini kita ini

play04:50

maka akan terjadi yang namanya gempa

play04:52

susulan nah gempa susulan ini apa untuk

play04:55

menstabilkan lempeng ya lempeng yang di

play04:58

ada di dalam bumi jadi muncullah gempa

play05:01

susulan kekuatan gempa susulan biasanya

play05:03

lebih kecil dibandingkan gempa utama

play05:05

walaupun kekuatan yang lebih kecil namun

play05:08

dapat merusak bangunan-bangunan yang

play05:10

rangkanya telah rusak akibat gempa utama

play05:13

Oleh karena itu setelah terjadi gempa

play05:15

selama beberapa waktu kita tidak

play05:16

disarankan untuk masuk ke dalam bangunan

play05:18

dan menunggu di ruang terbuka karena e

play05:21

dikhawatirkan masih terjadi gempa

play05:24

susulan Ya kita harus menunggu di ruang

play05:26

terbuka seperti itu kemud lanjutnya ya

play05:30

ini

play05:32

bencana tsunami ya tsunami itu merupakan

play05:35

gelombang air laut besar yang dipicu

play05:37

oleh pusaran air bawah laut karena

play05:40

pergeseran lempeng tanah longsor erupsi

play05:43

gunung api dan jatuhnya meteor maka

play05:46

terjadilah tsunami nah ini ya contoh

play05:49

dari gelombang yang sangat besar karena

play05:51

adanya pergeseran lempeng tadi bisa

play05:54

tanah longsor ataupun erupsi gunung

play05:57

berapi dan jatuhnya meteor

play06:00

ini peta gunung berapi ya yang ada di

play06:03

Indonesia

play06:04

jalur-jalurnya lihat dari

play06:07

ujung pulau Sumatera ya hingga ke Jawa

play06:12

kemudian hingga ke sini ke Pulau Nusa

play06:15

Tenggara ke ke Sulawesi ya di sini

play06:19

merupakan jalur-jalur gunung api ya

play06:22

Sumatra Jawa Bali Nusa Tenggara Banda

play06:25

hahera dan sulut jadi eh di Indonesia

play06:29

ini ada 4,5 juta masyarakat yang tinggal

play06:33

di daerah yang rawan bencana ya jadi di

play06:37

sini ada tipe a gunung tipe a ini di

play06:40

mana 77 dengan catatan sejarah letusan

play06:44

sejak tahun 1600 tipe B ini 29 dengan

play06:48

catatan sejarah letusan sebelum tahun

play06:50

1600 sedangkan Tipe C ini yaitu 21

play06:53

dengan tidak ada sejarah letusan tetapi

play06:55

masih memperlihatkan jejak aktivitas

play06:58

volkanik seperti at atau

play07:03

fumarolo bagaimana gunung berapi

play07:05

mengeluarkan Lapa gunung berapi terletak

play07:07

pada batas lempeng tektonik karena

play07:09

terbentuk dari pergerakan lempeng secara

play07:12

konvergen kemudian tekanan akibat

play07:14

tumbungan lempeng mendorong lelehan

play07:16

batuan magma ke atas magma terdapat

play07:19

dalam gunung berapi karena berbentuk

play07:21

cairan magma akan menyebar dan menembus

play07:24

batuan celah-celah atau tanah di

play07:26

sekitarnya untuk naik ke permukaan bumi

play07:29

Magma yang naik ke permukaan bumi

play07:31

disebut dengan lava atau sebagai lava

play07:33

nah pada saat letusan terjadi keluarlah

play07:36

lava debu dan awan yang sangat panas

play07:39

serta gas hidrogen sufida peristiwa ini

play07:42

disebut sebagai erupsi gunung berapi Nah

play07:45

itulah proses ya bagaimana gunung berapi

play07:48

itu mengeluarkan

play07:49

lava ini adalah contoh erupsi Beberapa

play07:53

gunung berapi yang ada di Indonesia ini

play07:55

Gunung Sinabung ini pada Agustus tahun

play07:59

20 Gunung Merapi Februari ya tahun 2020

play08:03

kemudian Gunung Agung ini Mei 201 gunung

play08:08

ile lewet toowok ini November 2020 ini

play08:12

contoh erupsi gunung di

play08:14

Indonesia nah Apa saja manfaat memiliki

play08:17

banyak gunung berapi nah di Indonesia

play08:19

ini karena banyak memiliki gunung berapi

play08:22

pasti memiliki manfaat yang pertama

play08:24

banyak sumber mineral dalam bentuk

play08:26

batuan bijih logam yang terletak pada

play08:29

batas lempeng yang kedua sumber energi

play08:32

berupa minyak bumi yang berasal dari

play08:33

fosil yang mengalami dekomposisi dalam

play08:36

jangka waktu berjuta-juta tahun sehingga

play08:39

membentuk hidrokarbon dan membentuk

play08:41

minyak bumi yang ketiga sumber energi

play08:44

lain yang dapat dimanfaatkan adalah gas

play08:47

bumi atau yang disebut sebagai energi

play08:50

geothermal yang keempat materi yang

play08:52

dikeluarkan oleh gunung berapi termasuk

play08:54

debu vulkanik akan terdekomposisi dan

play08:58

mengalami perubahan sehingga

play08:59

lama-kelamaan membentuk tanah yang

play09:01

paling subur di bumi ini gunung berapi

play09:04

juga menyuguhkan keindahan alam sebagai

play09:07

salah satu daya tarik pariwisata suatu

play09:10

daerah Nah itulah manfaat dari memiliki

play09:14

banyak gunung berapi untuk materi bab 6

play09:18

tentang struktur bumi dan

play09:21

perkembangannya Cukup sekian semoga

play09:23

bermanfaat sampai jumpa di video yang

play09:26

lainnya

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الوسوم ذات الصلة
Earth ScienceEducational VideoNatural DisastersEarthquakesTsunamisVolcanic ActivityGrade 8SeismologyIndonesian GeographyScience Curriculum
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