Penjelasan Lengkap Gempa Dahsyat yang Akan Terjadi di Indonesia

Fajrul Fx
15 Aug 202409:53

Summary

TLDRThe video script discusses the potential for a 'megatrust' earthquake in Indonesia, particularly in the Sunda and Mentawai regions, following Japan's recent 7.1 magnitude quake. It explains the geological concept of 'megatrust' as large contact zones between tectonic plates, which can generate powerful earthquakes but not necessarily. The script emphasizes the uncertainty of predicting exact earthquake timing, highlighting the importance of disaster mitigation, public awareness, and early detection systems to increase survival chances.

Takeaways

  • 🌏 The BMKG (Indonesian Agency for Meteorology, Climatology, and Geophysics) has identified a potential for a mega-quake in Indonesia, with a magnitude of up to 8.9, and it's a matter of time before it occurs.
  • πŸ” Mega-quakes, or 'megatrust' in the script, are not necessarily extremely powerful, but rather they occur over a large contact area between tectonic plates, which can result in a very strong earthquake.
  • πŸŒ€ Earthquakes are caused by the movement of tectonic plates over the Earth's magma, which can lead to significant tremors when these plates interact.
  • πŸŒ‹ Mega-quakes are particularly concerning in Indonesia due to the country's location on the 'Ring of Fire,' where many tectonic plates converge, creating numerous potential seismic gaps.
  • ⏳ The last major earthquake in the Sunda Strait occurred in 1757, and in Mentawai in 1797, indicating that a significant amount of energy may have been accumulating in these areas for centuries.
  • 🚨 Scientists cannot predict exactly when an earthquake will happen, but they can map potential areas of risk, which in the case of mega-quakes, could span hundreds of years.
  • 🏞 Indonesia has 16 identified mega-trust points, with the most active and studied being in the Sunda Strait and Mentawai.
  • πŸ— The potential for mega-quakes is a long-term concern, similar to astronomical events where the likelihood is over a very extended period, not an immediate threat.
  • πŸ“ The recent earthquake in Japan has raised concerns about the possibility of triggering a mega-quake in the Nankai Trough, which could also affect Indonesia.
  • πŸ›‘ Disaster mitigation is crucial, especially in a country as prone to natural disasters as Indonesia. It includes public education on response to earthquakes and tsunamis, and the development of early warning systems.
  • 🏒 The Indonesian government is encouraged to increase early detection systems for earthquakes and tsunamis to provide critical time for people to react and potentially save lives.

Q & A

  • What is a 'megatrust' earthquake according to the script?

    -A 'megatrust' earthquake, as mentioned in the script, is not about the magnitude of the earthquake but refers to the large contact area between tectonic plates. It is an earthquake that occurs over a large contact area where one tectonic plate is beneath another, also known as a subduction zone.

  • What does the term 'mega' in 'megatrust' signify?

    -In the context of 'megatrust', 'mega' indicates the large size of the contact area between tectonic plates, not the magnitude of the earthquake itself.

  • Why are scientists concerned about the 'megatrust' in Indonesia?

    -Scientists are concerned about the 'megatrust' in Indonesia because it has the potential to generate very powerful earthquakes due to the large contact area between tectonic plates and the accumulation of energy over time.

  • What is the potential magnitude of the 'megatrust' earthquakes in Indonesia?

    -The potential magnitude of the 'megatrust' earthquakes in Indonesia could reach up to 8.9, as stated by the head of the BMKG (Indonesian Agency for Meteorology, Climatology, and Geophysics).

  • How does the script explain the occurrence of an earthquake?

    -The script explains that earthquakes occur due to the movement of large tectonic plates above the Earth's liquid magma layer. Contacts between these plates can cause vibrations, which are experienced as earthquakes.

  • What is the difference between potential and prediction regarding earthquakes?

    -Potential refers to the possibility of an earthquake occurring due to certain conditions being met, such as the large contact area in a 'megatrust'. Prediction, on the other hand, involves specifying when an earthquake will happen, which, even with advanced technology, is not yet possible for scientists to do accurately.

  • What historical 'megatrust' earthquake is mentioned in the script?

    -The script mentions the 2004 'megatrust' earthquake in Aceh, which was very powerful and also caused a tsunami.

  • How many 'megatrust' points are there in Indonesia according to the script?

    -The script states that there are a total of 16 'megatrust' points in Indonesia.

  • What is the longest time since a significant earthquake occurred in the 'megatrust' areas of the Sunda Strait and Mentawai Siberut?

    -The last significant earthquake in the Sunda Strait occurred in 1757, and in Mentawai Siberut, it was in 1797, meaning it has been over 200 years since an earthquake occurred in these areas.

  • What measures are suggested in the script to mitigate the impact of 'megatrust' earthquakes in Indonesia?

    -The script suggests increasing public awareness about disaster response, improving early detection systems for earthquakes and tsunamis, and possibly adopting building designs that can withstand earthquakes, similar to those in Japan.

  • Why is it important to have an early detection system for earthquakes and tsunamis?

    -An early detection system is crucial because it can provide valuable time for warnings to be issued, potentially saving lives by giving people a chance to react and seek safety before the disaster strikes.

Outlines

00:00

🌏 Understanding Earthquake Megathrusts in Indonesia

This paragraph discusses the concept of megathrust earthquakes, particularly in the context of Indonesia. It explains the geological structure of the Earth, which consists of layers and plates moving over the liquid magma. The interaction between these plates at the Earth's surface is what causes earthquakes. The term 'megathrust' is clarified, indicating that it refers to the large size of the contact area between plates, not necessarily the strength of the earthquake. Megathrust earthquakes occur in areas with a broad contact zone, such as subduction zones, where one plate is beneath another. The potential for a powerful earthquake depends on the extent of the contraction of the upper plate. The paragraph also highlights the historical significance of megathrust earthquakes, such as the one in Aceh in 2004, which caused a tsunami. It emphasizes the importance of understanding these phenomena to better prepare for potential disasters.

05:02

πŸ” Assessing the Potential of Megathrust Earthquakes in Indonesia

The second paragraph delves into the potential of megathrust earthquakes in Indonesia, as identified by BMKG (Indonesian Agency for Meteorology, Climatology, and Geophysics). It mentions that these earthquakes could reach a magnitude of 8.9 and are waiting for the right conditions to occur. The paragraph highlights the long period since the last major earthquakes in the Sunda Strait and Mentawai, Siberut, suggesting a significant build-up of energy. It clarifies the difference between potential and prediction, stating that while scientists can map the potential for such earthquakes, they cannot predict the exact timing. The paragraph also discusses the importance of disaster mitigation, including public awareness and early warning systems for earthquakes and tsunamis. It suggests learning from Japan's approach to disaster mitigation, where buildings are designed to withstand earthquakes. The paragraph concludes by emphasizing the need for vigilance and the implementation of early detection systems to increase the chances of survival during such events.

Mindmap

Keywords

πŸ’‘Megaquake

A megaquake, also known as a mega thrust earthquake, is a large-scale seismic event that occurs along subduction zones where one tectonic plate is forced under another. In the video, the term is used to describe the potential for massive earthquakes in Indonesia, particularly in the Sunda and Mentawai subduction zones, which have not experienced a significant quake for over 200 years, indicating a high strain accumulation.

πŸ’‘Seismic Gap

A seismic gap refers to a region along a tectonic plate boundary that has not experienced significant seismic activity for an extended period, suggesting that stress is accumulating and a large earthquake may be overdue. The script mentions the seismic gaps of Sunda and Mentawai, which are of concern to scientists due to the potential for a megaquake.

πŸ’‘Subduction Zone

A subduction zone is an area where one tectonic plate moves under another, creating a deep ocean trench. These zones are prone to large earthquakes and tsunamis. The video script discusses the subduction zones in Indonesia, which are critical in understanding the potential for megaquakes.

πŸ’‘Tectonic Plates

Tectonic plates are large slabs of the Earth's lithosphere that float on the semi-fluid asthenosphere below. The movement of these plates is responsible for most of the world's earthquakes and volcanic activity. The script explains that the interaction of these plates is a key factor in the occurrence of earthquakes.

πŸ’‘Magnitude

In the context of earthquakes, magnitude refers to a measure of the earthquake's size based on the amount of energy released. The script mentions a potential megaquake with a magnitude of up to 8.9, indicating an extremely powerful seismic event.

πŸ’‘BMKG

BMKG stands for Badan Meteorologi, Klimatologi, dan Geofisika, which is the Indonesian Agency for Meteorology, Climatology, and Geophysics. The script cites BMKG as the source of information regarding the potential for a megaquake in Indonesia.

πŸ’‘Potential

In the script, potential refers to the likelihood or possibility of an event occurring, specifically the occurrence of a megaquake. It is distinguished from prediction, which would imply a more precise timing. The potential for megaquakes in Indonesia is a central theme of the video.

πŸ’‘Mitigation

Mitigation in the context of the video refers to the measures taken to reduce the impact of a disaster, such as an earthquake or tsunami. The script suggests that while the potential for megaquakes exists, the focus should be on disaster mitigation strategies, including early warning systems and public education.

πŸ’‘Tsunami

A tsunami is a series of ocean waves caused by a large underwater disturbance, such as an earthquake. The video script connects the potential for megaquakes with the risk of tsunamis, emphasizing the need for early detection systems to provide critical warning time.

πŸ’‘Strain Accumulation

Strain accumulation is the build-up of stress along a fault line due to the movement of tectonic plates. The script uses this term to explain why the seismic gaps in Indonesia are of concern, as the lack of recent earthquakes indicates a large amount of strain may have accumulated, increasing the potential for a future megaquake.

πŸ’‘Disaster Preparedness

Disaster preparedness involves planning and activities taken in advance to ensure effective response to emergencies. The video script highlights the importance of preparedness, including public education on response actions and the development of early warning systems for earthquakes and tsunamis.

Highlights

BMKG highlights that Indonesia is at risk of a megathrust earthquake, potentially reaching a magnitude of 8.9.

The seismic gap in the Sunda Strait and Mentawai-Siberut region is a major concern for Indonesian scientists, similar to the megathrust threat in Japan.

Megathrust earthquakes occur in subduction zones, where one tectonic plate slides beneath another, leading to large-scale seismic activity.

Contrary to popular belief, 'megathrust' refers to the large size of the contact area between plates, not necessarily the strength of the earthquake.

The strength of a megathrust earthquake depends on how much the upper plate contracts before releasing its energy.

The 2004 Aceh earthquake was caused by a megathrust, resulting in a powerful tsunami that affected the region.

Indonesia has 16 megathrust zones, with the Sunda Strait and Mentawai-Siberut being among the most studied and active.

The last major earthquake in the Sunda Strait occurred in 1757, indicating a long buildup of seismic energy.

The Mentawai-Siberut region's last major earthquake occurred in 1797, further emphasizing the risk of a future megathrust event.

Scientists emphasize that megathrust earthquakes are potential events, not predictions, meaning they could happen anytime within a broad timeframe.

Modern technology still cannot predict the exact timing of earthquakes, only the potential risk areas.

Mitigation efforts, including public education and disaster preparedness, are crucial for minimizing the impact of future earthquakes.

Indonesia's government is encouraged to implement early warning systems to provide crucial seconds for evacuation during earthquakes and tsunamis.

Japan's disaster preparedness, including earthquake-resistant buildings, serves as a model for Indonesia to improve its infrastructure.

The importance of staying vigilant and ready for potential disasters is emphasized, along with the need for increased public awareness and government action.

Transcripts

play00:00

BMKG sebut gempa megatrust Indonesia

play00:03

tinggal menunggu waktu bisa capai

play00:05

magnitudo

play00:07

8,9 hal tersebut dikatakan kepala pusat

play00:10

gempa bumi dan tsunami BMKG Daryono

play00:13

ketika menyinggung kekhawatiran ilmuwan

play00:15

Indonesia soal Seismic gap megatrust

play00:18

salat Sunda dan megatrust Mentawai

play00:21

sibero Oke kita akan membahas secara

play00:23

lengkap semuanya terkait dengan gempa

play00:25

megatrust di video kali ini agar

play00:28

semuanya menjadi jelas tanpa ada yang

play00:30

dilebih-lebihkan dan kita bisa tahu apa

play00:33

yang sebenarnya terjadi

play00:39

Oke Kabar tentang gempa megatras di

play00:41

Indonesia ini kembali ramai setelah

play00:43

terjadi gempa bumi berkekuatan magnetudo

play00:46

7,1 yang baru saja melanda Jepang Minggu

play00:50

lalu gempa ini telah memicu kekhawatiran

play00:53

di kalangan ilmuwan Jepang bahwa akan

play00:55

ada potensi gempa Dahsyat berikutnya di

play00:58

zona yang disebut dengan megatrust

play01:02

nankai kekhawatiran ini juga adalah

play01:04

kekhawatiran yang sama yang dialami oleh

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ilmuwan di Indonesia khususnya terhadap

play01:10

megatrust salat Sunda dan megatrust

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Mentawai Siberut karena kedua l ini

play01:16

yaitu potensi megatras yang ada di nanai

play01:18

Jepang dan potensi megatras yang ada di

play01:21

Indonesia keduanya sama-sama berada

play01:23

dalam kondisi kritis tinggal menunggu

play01:26

waktunya saja sebelum gempannya akan

play01:28

terjadi

play01:31

agar lebih jelas di sini kita akan

play01:32

membahas terlebih dahulu terkait dengan

play01:35

bagaimana gempa bumi bisa

play01:37

terjadi pertama-tama perlu kita pahami

play01:40

dulu bahwa bumi kita memiliki struktur

play01:43

yang terdiri dari lapisan-lapisan dan

play01:46

lempeng-lempeng yang bergerak di atas

play01:48

lapisan magma cair di dalam bumi

play01:51

lempeng-lempeng ini ukurannya sangat

play01:53

besar masing-masingnya dan mereka

play01:56

semuanya bergerak secara perlahan kontak

play01:59

antar tempeng bumi inilah yang kemudian

play02:01

mengakibatkan muncul Getaran yang kita

play02:04

sebut sebagai gempa

play02:06

bumi Jenis dari gempa bumi ada

play02:09

bermacam-macam dan salah satunya adalah

play02:11

yang kita sebut sebagai gempa megatras

play02:14

nah ini ada yang perlu diluruskan ketika

play02:17

kita mendengar kata gempa megatras maka

play02:19

kesannya adalah Ini adalah sebuah gempa

play02:21

dengan kekuatan yang sangat besar karena

play02:24

ada kata Mega atau besar di situ nah ini

play02:28

adalah hal yang tidak sepenuhnya nya

play02:30

tepat karena arti dari megatrust

play02:32

Sebenarnya bukan seperti itu kata Mega

play02:35

dalam megatrust menunjukkan bahwa ukuran

play02:37

dari kontak antar lempengnya sangatlah

play02:40

besar jadi yang besar adalah ukurannya

play02:43

bukan

play02:45

kekuatannya kontak yang besar ini memang

play02:47

bisa menghasilkan sebuah gempa dengan

play02:49

kekuatan yang sangat besar tapi tidak

play02:51

selalu demikian hasilnya lebih

play02:54

spesifiknya gempa megatras adalah gempa

play02:57

yang terjadi dengan wilayah kontak yang

play02:59

luas pada area di mana satu lempeng bumi

play03:03

berada di bawah lempeng lainnya area ini

play03:06

disebut juga dengan zona

play03:08

subduksi ketika kedua lempeng ini

play03:11

mengalami kontak dan lempeng yang ada di

play03:13

bawah bergerak ini membuat lempeng yang

play03:16

menempel di atas

play03:18

berkontraksi ada energi besar yang

play03:20

tersimpan pada lempeng

play03:23

ini ketika lempeng atas sudah tidak bisa

play03:25

menahan kontraksinya maka lempeng ini

play03:28

akan lepas dan hasilkan energi yang

play03:31

besar inilah Getaran yang mengakibatkan

play03:34

gempa megatras yang memiliki potensi

play03:36

kekuatan sangat besar simpelnya kekuatan

play03:40

gempa megatras bergantung pada seberapa

play03:42

jauh lempeng di atas ini berkontraksi

play03:45

jika baru sedikit sudah lepas maka

play03:47

gempanya akan cukup pelan gampangnya

play03:50

tapi jika sudah sampai berkontraksi

play03:52

sampai jauh maka potensi gempa yang

play03:54

dihasilkan memiliki kekuatan yang lebih

play03:57

besar gempa megga ini jugalah yang

play04:00

menjadi penyebab dari Kejadian gempa

play04:02

yang terjadi di Aceh tahun 2004 yang

play04:06

juga gempa yang sangat kuat ini sampai

play04:08

mengakibatkan terjadi tsunami dan di

play04:11

sini juga bisa kita lihat ada banyak

play04:14

sekali daftar Kejadian gempa megatras

play04:16

yang sudah pernah terjadi Dan inilah

play04:19

yang dikhawatirkan juga di Indonesia

play04:22

Indonesia adalah sebuah negara yang

play04:25

sangat sangat rawan di sini bisa kita

play04:29

lihat gambaran umumnya untuk petanya di

play04:32

mana terdapat area subduksi atau daerah

play04:35

ketika ada lengeng yang bertumpukan

play04:37

dengan lemeng lainnya di sini bisa kita

play04:39

lihat bahwa hampir semua tempat di

play04:42

Indonesia

play04:43

ternyata memiliki area ini kecuali

play04:47

Kalimantan di sini Jika dipetakan ada

play04:50

total 16 titik megatrust di Indonesia

play04:53

dengan titik yang paling aktif yang

play04:56

paling sering banyak diteliti adalah

play04:58

yang ada di Selat Sunda dan Mentawai si

play05:02

berut Lokasinya ada di daerah

play05:05

ini oleh BMKG disampaikan bahwa

play05:09

megatrust ini memiliki potensi gempa

play05:12

yang kekuatannya dapat mencapai

play05:15

8,9 magnitudenya dan ini tinggal

play05:18

menunggu waktu maksudnya gini ketika

play05:21

kontak antara kedua lempeng sudah

play05:23

terjadi dan juga sudah bergerak lempeng

play05:25

bawahnya maka Hanya tinggal menunggu

play05:27

waktu kapan lempeng di atas tidak bisa

play05:30

menahan kontraksi dan kemudian melepas

play05:34

energinya dan problemnya untuk lempeng

play05:37

Selat Sunda misalnya di sini dia

play05:40

terakhir terjadi gempa besar adalah di

play05:42

tahun

play05:44

1757 artinya sudah lebih dari 200 tahun

play05:48

belum terjadi gempa lagi jadi

play05:51

konstruksinya ini sudah sangat besar

play05:54

teman-teman Begitu juga dengan yang

play05:56

terjadi di mentaw si berut yang terakhir

play05:59

terjadi adalah di tahun

play06:02

1797 sudah ratusan tahun dan area kontak

play06:06

ini belum melepaskan energi lagi

play06:08

sehingga ada potensi gempa yang sangat

play06:10

besar yang masih tersimpan nah Dan ini

play06:13

juga yang perlu diluruskan teman-teman

play06:16

di sini sifatnya potensi ya dan potensi

play06:19

itu berbeda dengan prediksi dengan

play06:22

teknologi yang paling maju di dunia yang

play06:24

ada saat ini para ilmuwan masih belum

play06:26

bisa memprediksi Kapan gempa bumi akan

play06:29

terjadi secara eksak mereka hanya bisa

play06:32

memetakan potensinya dan ketika kita

play06:35

berbicara tentang potensi maka rentang

play06:37

waktunya itu sangatlah lama bukan lagi

play06:41

tentang besok Minggu depan atau tahun

play06:44

depan tapi bisa jadi sampai ratusan

play06:46

tahun rentang kemungkinannya memang ada

play06:49

kemungkinan ini akan terjadi dalam waktu

play06:51

dekat tapi kemungkinan ini rentangnya

play06:53

adalah sampai ratusan tahun teman-teman

play06:56

ini mirip juga seperti yang ada di

play06:58

bidang astrofisika bintang betelgest

play07:01

adalah salah satu bintang yang ukurannya

play07:03

sangat besar dan bisa kita bilang cukup

play07:05

dekat dengan tata surya kita dan

play07:08

harusnya dalam waktu dekat dia akan

play07:12

meledak tapi meledaknya Ini kemungkinan

play07:15

rentangnya adalah sampai ratusan ribu

play07:18

tahun Jadi kemungkinannya sangat

play07:22

panjang potensi megatrust ini sebenarnya

play07:25

sudah diteliti sejak lama tiap beberapa

play07:28

tahun informasi ini ramai lagi viral

play07:31

lagi terutama yang terkait dengan Sunda

play07:33

megatrust dan memang bahwa potensi ini

play07:36

memang benar ada dan kita tidak bisa

play07:40

menghentikannya termasuk ketika terjadi

play07:43

gempa di Jepang Minggu lalu yang mana

play07:46

gempa ini ada kemungkinan Untuk memicu

play07:48

megatras rankai Ada kemungkinan juga

play07:51

bahwa megatrust ini nantinya juga akan

play07:53

memicu terjadinya gempa megateras yang

play07:56

ada di Indonesia meskipun kita belum

play07:58

dapat memastikannya satu hal yang pasti

play08:02

yang bisa kita lakukan adalah melakukan

play08:05

mitigasi bencana untuk yang tinggal di

play08:08

daerah rawan bencana yang artinya hampir

play08:11

seluruh wilayah Indonesia maka kita

play08:13

harus mengetahui penanganan pertama

play08:15

ketika terjadi gempa itu seperti apa

play08:19

Jika memungkinkan keluar maka segera

play08:21

keluar ke area terbuka jika terjebak di

play08:24

ruangan segera berlindung dari

play08:27

reruntuhan itu yang bisa kita lakukan

play08:30

kemudian kalau dari sisi pemerintah ini

play08:32

yang pasti perlu sosialisasi aktif ke

play08:35

masyarakat terkait dengan Bagaimana

play08:37

caranya untuk bereaksi ketika bencana

play08:41

tersebut terjadi dan juga harusnya nih

play08:44

ya harusnya perlu banyak sistem

play08:46

pendeteksi Dini untuk gempa dan tsunami

play08:49

sehingga ketika ada tsunami ataupun

play08:51

Gempa yang terjadi langsung ada notifnya

play08:54

dan ada jedanya dari kejadian sampai

play08:56

merambat ke lokasi semenitlah paling ee

play09:00

untuk jedanya tapi 1 menit ini sangat

play09:02

berharga dan menambah kemungkinan untuk

play09:05

bisa menyelamatkan diri akan jauh lebih

play09:08

baik lagi kalau kita bisa meniru seperti

play09:10

Jepang dalam hal mitigasi bencana di

play09:14

Jepang struktur bangunannya didesain

play09:16

agar tetap tahan terhadap gempa jadi

play09:19

meskipun goyang enggak langsung hancur

play09:22

dan ini PR sangat besar untuk di

play09:25

Indonesia dan itulah dia teman-teman

play09:28

informasi terkait dengan potensi gempa

play09:30

megatrust potensi itu ada tapi kita

play09:33

enggak tahu kapan akan terjadinya yang

play09:37

perlu kita lakukan adalah kita harus

play09:38

waspada dan dari sisi pemerintah harus

play09:41

segera nambah sistem pendeteksi Dini

play09:44

biar nanti bisa menambah kemungkinan

play09:46

untuk menyelamatkan diri oke demikian

play09:48

terima kasih

play09:50

[Musik]

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Related Tags
EarthquakeTsunamiMegaquakeSeismic GapIndonesiaDisaster PreparednessGeologyNatural HazardsEmergency ResponseEducational