Apakah Gempa Megathrust Bisa Membelah Pulau Jawa?

Fajrul Fx
17 Aug 202412:29

Summary

TLDRThe video script discusses the potential impact of a 'megatrust' earthquake originating from the Sunda and Mentawai mega-faults, clarifying misconceptions about its magnitude and effects. It emphasizes that while the earthquake could reach magnitudes of up to 9.1, it would not split Java Island as sensationalized. The script provides a detailed simulation of the earthquake's effects, including damage scales and potential tsunami heights, highlighting the importance of understanding and preparing for such natural disasters without succumbing to misinformation.

Takeaways

  • 😀 The video script discusses the potential impact of a 'megatrust' earthquake, particularly focusing on the Sunda Megathrust and its possible effects in Indonesia.
  • 🏞️ The script clarifies that the term 'megatrust' refers to the large contact area between tectonic plates and the upward faulting that can cause significant earthquakes, not just the magnitude of the quake itself.
  • 📊 The potential magnitude of the Sunda Megathrust earthquake is said to reach up to 8.7, with the possibility of a 9.1 magnitude quake if other nearby faults are triggered simultaneously.
  • 🌊 The script mentions that despite the significant magnitude, the depth of the Sunda Megathrust is deeper, which could still result in a high tsunami potential.
  • 📚 It emphasizes the difference between magnitude scales, explaining that each increase of one unit on a logarithmic scale represents a tenfold increase in the quake's power.
  • 🔎 The script compares the Sunda Megathrust's potential with the 2004 Aceh earthquake, which had a magnitude of 9.1, to illustrate the relative strength of the potential quake.
  • 🏠 The video includes a simulation that shows the initial waves of the earthquake and its impact on various regions, using the Modified Mercalli Intensity (MMI) scale to indicate the level of damage.
  • 🚨 The script warns of the high damage potential, with areas like Ujung Kulon experiencing severe destruction up to MMI scale 9, and advises early tsunami warnings and evacuations.
  • 📈 The potential tsunami height from the Sunda Megathrust is highlighted, with maximum heights reaching up to 20 meters in Ujung Kulon and around 3 to 5 meters in southern Java.
  • 🗺️ The script dispels the myth that the earthquake could split Java Island, explaining that while surface cracks may occur, the island would not be split apart by the quake.
  • 👨‍🏫 It calls for caution and preparedness, reminding viewers that the discussion is about potential risks rather than a prediction of when the event will occur, and encourages consulting official information from BMKG.

Q & A

  • What is the main topic discussed in the video script?

    -The main topic is the potential impact and analysis of a mega-quake, specifically the Sunda Megathrust earthquake, including its possible effects on Java Island and the likelihood of it causing significant land division.

  • What is the meaning of 'megatrust' in the context of the video script?

    -In the context of the video script, 'megatrust' refers to a massive area of contact between tectonic plates that can potentially cause a large-scale upward faulting, leading to a powerful earthquake.

  • What is the potential magnitude of the Sunda Megathrust earthquake as discussed in the script?

    -The script mentions that the potential magnitude of the Sunda Megathrust earthquake could reach up to 8.7.

  • How does the script compare the potential impact of the Sunda Megathrust earthquake to the 2004 Aceh earthquake?

    -The script compares the Sunda Megathrust earthquake to the 2004 Aceh earthquake by noting that while the Aceh earthquake had a magnitude of 9.1, the Sunda Megathrust could potentially have a magnitude of 8.7, which is still extremely powerful but less than the Aceh earthquake.

  • null

    -null

  • What is the significance of the logarithmic scale in earthquake magnitudes?

    -The script explains that the magnitude scale is logarithmic, meaning that for each whole number increase in magnitude, the energy released by the earthquake increases by a factor of about 31.6 (10^1.5), not just by a factor of 10.

  • What is the Meralli scale (MMI) mentioned in the script, and how does it relate to earthquake impacts?

    -The Meralli scale (MMI) is a measure of the shaking intensity of an earthquake as perceived by people and the effects on man-made structures. It ranges from I (not felt by people) to XII (total destruction), and the script uses it to illustrate the potential damage an earthquake could cause.

  • According to the script, what is the maximum potential height of the tsunami generated by the Sunda Megathrust earthquake?

    -The script states that the maximum potential height of the tsunami generated by the Sunda Megathrust earthquake could reach up to 20 meters, particularly in the Ujung Kulon area.

  • Does the script suggest that the Sunda Megathrust earthquake could split Java Island?

    -The script clarifies that despite the significant power of the Sunda Megathrust earthquake, it is not possible for it to split Java Island. The term 'split' in the context of earthquakes refers to surface ruptures, which are unlikely to occur to the extent of dividing an entire island.

  • What is the difference between the type of earthquake that could cause land division and the type discussed in the script?

    -The script differentiates between the type of earthquake that could cause land division, which is typically a strike-slip fault where one side moves up or down relative to the other, and the type of earthquake discussed, which is a thrust fault where the movement is predominantly horizontal, pushing the landmasses against each other.

  • What is the advice given in the script regarding the potential of the Sunda Megathrust earthquake?

    -The script advises that while the potential of the Sunda Megathrust earthquake is significant, it is important to remember that this is a potential scenario and not a prediction. It emphasizes the need for preparedness and awareness, and encourages viewers to refer to official information from the BMKG (Indonesian Meteorology, Climatology, and Geophysical Agency) for more accurate and detailed information.

Outlines

00:00

🌏 Understanding Megathrust Earthquakes and Their Impacts

The first paragraph introduces the concept of a 'megathrust' earthquake, explaining that it is not just about the sheer power of the quake but also the large area of tectonic plate interaction. It clarifies that 'mega' refers to the extensive contact area between plates, while 'thrust' indicates the upward movement along faults. The paragraph discusses the potential magnitude of such earthquakes, particularly focusing on the Sunda Megathrust in Indonesia, which could reach up to 8.7 in magnitude. It compares this to the devastating 2004 Aceh earthquake, which was magnitude 9.1, to emphasize the scale of potential destruction. The paragraph also dispels myths about the earthquake's ability to split the island of Java, stating that while it could cause significant damage, a split is unlikely.

05:00

📏 Measuring Earthquake Impact with the Modified Mercalli Intensity Scale

The second paragraph delves into the effects of an earthquake, using the Modified Mercalli Intensity (MMI) scale to quantify the level of damage and shaking felt in different areas. It outlines the scale's various levels, from I, where the quake is not felt by most, to IX, where even well-constructed buildings may suffer severe damage. The paragraph provides a hypothetical scenario of the Sunda Megathrust's impact, with detailed descriptions of the damage at different MMI levels. It also touches on the potential for a tsunami, highlighting the high risk in areas like Ujung Kulon and the southern part of Java Island, with maximum tsunami heights estimated up to 20 meters based on simulations by researchers from ITB and the Indonesian Meteorological, Climatological, and Geophysical Agency (BMKG).

10:02

🏞️ The Reality of Earthquake-Induced Land Divisions and Public Awareness

The final paragraph addresses the misconception that earthquakes can split landmasses, such as the island of Java, into separate parts. It explains that while earthquakes can cause surface ruptures, they do not typically cleave land apart as depicted in movies. The paragraph uses the example of the 2018 Palu earthquake, which was a strike-slip fault and resulted in significant surface ruptures but not a land split. It also references the geological phenomenon in Iceland, where the land is slowly splitting due to the movement of tectonic plates, but this process takes an extremely long time. The paragraph concludes by emphasizing the importance of public awareness and preparedness, encouraging viewers to seek accurate information from official sources like BMKG and to remain vigilant.

Mindmap

Keywords

💡Megatrust

Megatrust refers to a large-scale tectonic plate interaction where the contact area between plates is extensive, and the fault type is predominantly thrust, meaning one plate moves upward relative to the other. In the context of the video, Megatrust is used to describe the potential for a powerful earthquake along the Sunda Megathrust, which could have significant impacts, including the generation of a large tsunami. The term is central to understanding the video's theme of the potential disaster from a massive earthquake.

💡Magnitude

In seismology, magnitude is a measure of the size of an earthquake, expressed as a number on a logarithmic scale. The video discusses the potential magnitudes of a Megatrust earthquake, such as 8.7 or 9.1, to convey the severity of the expected impact. The script uses the term to compare the potential strength of the Sunda Megatrust to the 2004 Aceh earthquake, which had a magnitude of 9.1.

💡Sunda Megathrust

The Sunda Megathrust is the specific area of the Earth's crust where the Indian Plate is being pushed under the Eurasian Plate, creating a significant seismic hazard. The video emphasizes the potential for a large earthquake from this area, with a magnitude that could reach 8.7, and the subsequent tsunami risks. It is a key concept in the video's exploration of the potential for a devastating earthquake and tsunami in Indonesia.

💡Tsunami

A tsunami is a series of ocean waves caused by a large, sudden displacement of water, often resulting from an underwater earthquake. The video script discusses the potential for a tsunami resulting from a Megatrust earthquake, with estimated maximum wave heights reaching up to 20 meters in certain areas. The term is integral to the video's message about the combined threats of an earthquake and the ensuing tsunami.

💡MMI (Modified Mercalli Intensity)

The Modified Mercalli Intensity scale is a measure of the shaking intensity of an earthquake as perceived by people. The video uses the MMI scale to illustrate the varying degrees of damage that could be caused by the Megatrust earthquake, from imperceptible at the lowest levels to severe damage at higher levels, such as the 9 intensity experienced near the epicenter.

💡Epicenter

The epicenter is the point on the Earth's surface directly above the hypocenter, or the point within the Earth where an earthquake originates. The video script describes the epicenter of the simulated Megatrust earthquake as being south of Java, which helps viewers understand the geographical focus of the potential disaster.

💡Hoax

A hoax is a false or misleading claim, often spread for malicious purposes. The video script mentions that the idea of an earthquake splitting Java Island is a hoax, emphasizing the importance of distinguishing between real threats and unfounded rumors in discussions about natural disasters.

💡Strike-slip fault

A strike-slip fault is a type of fault where the movement of the plates is horizontal and parallel to the fault line. The video contrasts this with the thrust fault of the Megatrust, explaining that while a strike-slip fault can cause significant surface breaks, it is less likely to result in the splitting of landmasses like Java Island.

💡Offset

In the context of earthquakes, offset refers to the amount of displacement along a fault line. The video script uses the example of the 2018 Palu earthquake to illustrate the concept of offset, explaining that the maximum offset observed was 5 meters, which is significant but does not equate to the land splitting apart.

💡Simulation

A simulation in this context refers to a computer-generated model that imitates the behavior of the physical phenomenon, such as an earthquake and its effects. The video script mentions a simulation by Indo Quake, which visualizes the potential impacts of the Megatrust earthquake, including the shaking intensity and tsunami wave heights.

💡BMKG

BMKG stands for Badan Meteorologi, Klimatologi, dan Geofisika, which is the Indonesian Agency for Meteorology, Climatology, and Geophysics. The video script advises viewers to refer to official information from BMKG for accurate and reliable data on seismic activities and potential disasters, emphasizing the importance of authoritative sources in disaster preparedness.

Highlights

The video discusses the potential impact of a megatrust earthquake in Indonesia, particularly from the Sunda Megathrust and Mentawai, Siberut regions.

Megatrust earthquakes are characterized by large contact areas between tectonic plates and upward fault movements.

The Sunda Megatrust has the potential to reach a magnitude of 8.7, while the Mentawai Megatrust could reach up to 8.9.

A simultaneous occurrence of megatrust earthquakes could generate a combined magnitude of up to 9.1.

The term 'megatrust' is often misunderstood, with 'mega' indicating a large contact area and 'trust' referring to upward fault movements.

The Richter magnitude scale is logarithmic, meaning each whole number increase represents a tenfold increase in measured amplitude.

An earthquake with a magnitude of 8.7 is twice as strong as one with a magnitude of 8.3, illustrating the scale's exponential nature.

The 2004 Aceh earthquake, with a magnitude of 9.1, was twice as strong as the potential Sunda Megatrust earthquake.

The video includes a visualization of the Sunda Megatrust earthquake's impact, showing the initial wave movements and damage scales.

The Mercalli Intensity Scale (MMI) is used to measure the severity of an earthquake's effects on human populations and structures.

The simulation shows that a magnitude 8.7 earthquake could cause significant damage, with some areas experiencing MMI levels up to 9.

The potential for a tsunami following a Sunda Megatrust earthquake is discussed, with maximum wave heights reaching up to 20 meters in certain areas.

The video clarifies that while the earthquake could be powerful, it is unlikely to split the island of Java.

The difference between the potential for an earthquake and a prediction is highlighted, emphasizing the uncertainty of when such an event might occur.

The video calls for vigilance and preparedness, regardless of the uncertainty, and encourages viewers to refer to official information from the BMKG for the most accurate data.

The video concludes by inviting corrections from experts in geophysics and thanking viewers for their attention.

Transcripts

play00:00

tidak jawabannya enggak teman-teman

play00:02

Kalau waktu kalian terbatas informasi

play00:04

itu saja sudah cukup silakan melanjutkan

play00:07

aktivitas lagi intinya gempa megatrust

play00:10

tidak akan bisa membelah pulau Jawa itu

play00:12

hanyalah sekedar hoax yang

play00:14

dilebih-lebihkan dan kalau kalian pengin

play00:16

tahu analisis lengkapnya Bagaimana gempa

play00:19

megatrust ini termasuk simulasi

play00:21

kerusakannya Bagaimana tsunaminya

play00:24

silakan tonton Sampai Akhir

play00:31

baik video ini adalah video lanjutan

play00:33

dari video sebelumnya yang membahas

play00:35

tentang potensi gempa megatrust di

play00:38

Indonesia khususnya yang berasal dari

play00:40

megatras Selat Sunda dan Mentawai

play00:43

Siberut jika belum Nonton videonya

play00:46

silakan nanti bisa ditonton setelah

play00:48

menyelesaikan video

play00:50

ini di video ini kita akan membahas

play00:52

dampak sebenarnya dari gempa megatrust

play00:55

ini nah di pemberitaan banyak

play00:57

disampaikan bahwa megatrust ini dapat

play01:00

hasilkan gempa dengan magnitude hingga

play01:02

8,9 bahkan

play01:05

9,1 tapi banyak yang belum tahu dan

play01:08

belum jelas juga magnitude 8,9 itu

play01:11

Sebesar apa dampaknya akan seburuk apa

play01:15

jika terjadi tsunami akan Sebesar apa

play01:18

tsunaminya dan Apakah benar gempa ini

play01:20

dapat sampai membelah pulau

play01:24

Jawa pertama kita recap dulu terkait

play01:26

dengan istilah megatrust yang masih

play01:29

sering salah dipahami ketika kita

play01:31

mendengar kata gempa megateras maka

play01:34

kesannya adalah ini sebuah gempa dengan

play01:36

kekuatan yang sangat besar tapi ini

play01:39

tidak sepenuhnya Tepat kata Mega dalam

play01:42

megatrust menunjukkan bahwa area kontak

play01:45

antar lempeng yang bertumpukan sangatlah

play01:47

besar dan kata trust sendiri berarti

play01:50

bahwa jenis patahannya yang menyebabkan

play01:53

gempa adalah naik ke atas nah area

play01:56

kontak yang besar dan patahan yang naik

play01:58

ke atas ini memiliki potensi untuk

play02:01

menghasilkan gempa dengan kekuatan yang

play02:03

besar Meskipun tidak selalu demikian

play02:07

dalam hal Sunda megatrust potensinya

play02:09

mencapai magnitude 8,7 megatrust

play02:13

mentawisi berut potensi gempanya

play02:15

mencapai

play02:16

8,9 dan juga ada banyak megatrust lain

play02:19

yang jika kondisinya terburuk ketika

play02:21

megatrust di sekitarnya ikut terpicu

play02:24

secara bersamaan gempa yang dihasilkan

play02:26

bisa mencapai kekuatan 9,1 magnitudo

play02:31

biar lebih jelas di sini kita fokus ke

play02:33

satu hal dulu aja Sunda megatrust yang

play02:35

memiliki magnitudo

play02:37

8,7 seberapa Kuatkah gempa magnitude

play02:42

8,7 sebagai perbandingan gempa besar di

play02:45

Aceh tahun 2004 memiliki kekuatan

play02:48

magnitude 9,1 dan sama-sama bertipe

play02:52

megatras secara sekilas angka 9,1 dan

play02:56

8,7 ini kesannya hanya beda dikit saja

play02:59

selisihnya hanya 0,4 Tapi perlu kita

play03:02

ingat bahwa Skala magnitudo adalah skala

play03:06

logaritmik artinya gini untuk setiap

play03:09

kenaikan skala satu aja maka di sini

play03:12

Sebenarnya kekuatannya naik 10 kali

play03:15

lipat gempa skala magnitude 7

play03:18

kekuatannya 10 kali lebih kuat daripada

play03:21

gempa skala 6 gempa skala 8 kekuatannya

play03:25

bukan dua kali lipat lebih besar

play03:27

daripada skala 6 tapi 100 kali lipat itu

play03:31

adalah perbandingan kekuatannya sehingga

play03:35

jika kita memiliki nilai perbedaannya

play03:37

adalah 0,4 maka nilai sebenarnya adalah

play03:40

10^

play03:41

0,4 nilainya adalah 2 artinya gempa Aceh

play03:46

tahun 2004 dua kali lipat lebih kuat

play03:49

daripada potensi gempa dari Sunda

play03:51

megatrust jadi gempa Sunda megatrust

play03:54

kekuatannya setengah kali dari gempa

play03:57

Aceh tahun 2004 yang pada waktu itu

play03:59

mengakibatkan lebih dari 200.000 orang

play04:03

meninggal dunia gempa Sunda megatras

play04:06

dengan kekuatan 8,7 ini adalah gempa

play04:09

yang sangat besar juga teman-teman

play04:11

karena ini lebih besar daripada gempa

play04:13

yang ada di Palu gempa yang ada di Jogja

play04:16

tapi meskipun demikian gempa Aceh bahkan

play04:19

dua kali lipat lebih kuat lagi baru

play04:22

ketika Sunda megatrust ini terjadi

play04:24

secara bersamaan dengan megatras lainnya

play04:27

gempa yang dihasilkan akan menghasilkan

play04:29

Al magnitude 9,1 yang artinya setara

play04:32

dengan gempa Aceh tahun

play04:35

2004 agar lebih jelas seberapa kuat

play04:39

gempa 8,7 dan bagaimana dampaknya kita

play04:42

akan melihat visualisasi dari simulasi

play04:45

gempa ini simulasi ini dibuat oleh

play04:48

channel Indo quake ini bagus banget

play04:50

visualisasinya dan kita akan melihatnya

play04:54

Oke pusat gempanya berada di arah

play04:56

selatan dari Pulau Jawa di bagian bawah

play05:00

dari Ujung Kulon dan kita lihat di sini

play05:02

untuk gelombangnya gelombang awalnya

play05:05

sudah mulai

play05:07

mengenai pemukiman

play05:10

Oke dan di sini diberikan angka-angka

play05:12

ini teman-teman ini adalah skala yang

play05:14

disebut dengan skala

play05:16

MMI atau Skala merkali yang mana ini

play05:20

menunjukkan seberapa besar dampak

play05:22

kerusakan yang terjadi pada suatu daerah

play05:25

akibat gempa dan ini ada banyak skalanya

play05:29

mulai dari skala satu ini adalah

play05:31

getarannya tidak dirasakan kecuali dalam

play05:34

keadaan luar biasa oleh beberapa orang

play05:36

jadi enggak begitu kerasa skala dua

play05:39

menunjukkan getarannya mulai dirasakan

play05:42

skala tiga getarannya dirasakan

play05:44

seakan-akan seperti ketika ada truk yang

play05:48

berlalu skala empat ini mulai kerasa

play05:51

getarannya dan skala lima getarannya

play05:53

bahkan lebih kerasa lagi sampai mungkin

play05:55

jendelanya ada yang pecah skala enam

play05:58

lebih besar lagi

play06:00

sebagian bangunan mungkin akan mengalami

play06:03

kerusakan skala

play06:05

tu semakin banyak kerusakannya skala Del

play06:08

ini bahkan sampai bangunan dengan

play06:10

struktur yang kuat juga mengalami

play06:12

kerusakan dan

play06:14

seterusnya di sini gelombang awalnya

play06:17

sudah mulai bergerak dan bagian

play06:19

sebenarnya dari gempa yang kuat itu

play06:22

adalah gelombang yang datang kedua ini

play06:25

teman-teman dan

play06:27

evaku oke yang dapat enam skala

play06:31

kerusakannya

play06:33

[Musik]

play06:37

oke

play06:39

tujuh Ini daerah mana ini Sukabumi

play06:46

Oke gempanya bahkan sudahud sampai di

play06:49

daerah Cirebon hampir sampai daerah Jawa

play06:54

Tengah mulai muncul peringatan gempa

play07:00

[Musik]

play07:04

oke di sini juga terjadi eh ada pusat

play07:09

gempa lagi yang di daerah sini dan di

play07:11

sini kita bisa melihat bahwa daerah yang

play07:13

ada di Ujung Kulon ini ya tingkat

play07:16

kerusakannya bahkan sampai 9 ini

play07:19

kerusakan yang udah sangat

play07:23

parah nah peringatan dini tsunami di

play07:27

bentenarkan

play07:29

harap evakuasi ke tempat yang lebih

play07:31

tinggi

play07:33

Oke karena memang ini adalah gempa

play07:36

dengan skala yang sangat besar ya

play07:37

teman-teman memang nilai skala

play07:39

kekuatannya lebih kecil daripada yang

play07:42

ada di Aceh tapi perlu diingat bahwa

play07:44

megatra Sunda ini secara kedalaman dia

play07:48

lebih dangkal Jadi potensi tsunaminya

play07:51

juga tetap ada dan tetap tinggi ini

play07:54

adalah hasil simulasi dari peneliti di

play07:56

ITB dan tim BMKG jadi di sini ditemukan

play08:02

bahwa gempa Sunda megatrust ini akan

play08:05

memiliki potensi tsunami dengan

play08:07

ketinggian maksimum hingga di 20 m yaitu

play08:12

adalah di daerah Ujung Kulon sini

play08:16

utamanya kemudian di daerah selatan

play08:19

pulau Jawa ini pun juga memiliki potensi

play08:22

di sekitar mungkin sekitar 3 sampai 5

play08:25

m Adapun untuk di daerah Jakarta karena

play08:28

dia ada di seberang dari sumber

play08:31

tsunaminya potensi tsunaminya akan cukup

play08:34

kecil inilah Dia gambaran dari apa yang

play08:38

akan terjadi dari gempa Sunda megatras

play08:41

ini beserta tsunaminya dan kembali lagi

play08:43

pertanyaannya Apakah gempa Sunda

play08:46

megatrust ini akan bisa sampai membelah

play08:48

pulau Jawa tentu saja Jawabannya adalah

play08:52

tidak kita sudahudah melihat dampaknya

play08:54

di sini dan juga sebenarnya meskipun

play08:58

seringkiali kita melihat di di film-film

play09:00

ketika ada gempa maka tanah itu retak

play09:03

sampai ke belah terus ada orang sampai

play09:05

ke cemplung nah di dunia nyata tidak

play09:08

seperti itu yang mungkin terjadi

play09:11

hanyalah berupa robekan Di lapisan atas

play09:14

di tanah pada Lokasi gempa tersebut tapi

play09:17

bukan sampai ke belah dan sampai

play09:20

pisah apalagi di sini lokasi Sunda

play09:23

megatras adalah di laut sehingga andai

play09:26

kata memang bisa membelah kemungkinan

play09:28

yang terbelah ada di bagian ini dan lagi

play09:31

pula Ketika gempa terjadi di sini

play09:34

gelombangnya Kemudian menyebar bukan

play09:37

yang tiba-tiba lurus dan langsung

play09:39

membelah pulau Jawa dan

play09:41

kepotong jenis gempa yang lebih

play09:43

memungkinkan untuk terjadi belahan

play09:46

adalah jenis gempa di mana sumber

play09:48

gempanya langsung di bawah daratan itu

play09:52

seperti misalnya gempa Palu

play09:55

2018 gempa ini terjadi karena ada

play09:58

gerakan pada sesar atau patahan lempeng

play10:01

di mana satu sisi bergerak ke arah atas

play10:04

dan satu sisi bergerak ke arah bawah

play10:06

atau yang disebut Strike slip fault Gema

play10:10

yang seperti ini akan lebih memungkinkan

play10:12

untuk menghasilkan robekan pada tanah

play10:15

tapi lagi-lagi ini bukan belahan yang

play10:18

sampai dalam teman-teman pada gempa Palu

play10:21

misalnya robekan yang dihasilkan pada

play10:23

titik yang paling besar nilainya adalah

play10:26

sejauh 5 m tapi enggak sampai membah

play10:30

kami nyebutnya sebagai Sur rure yaitu

play10:33

robekan pada bidang gempa ya Misalnya

play10:36

gempa

play10:37

Palu jadi saya jalan 40 Kil dari Utara

play10:40

Palu sampai ke selatan Palu ya Dan kami

play10:42

menemuk offset

play10:44

2 jadi maksimum

play10:48

5 itu yang disebut tapi ya tetap di situ

play10:51

gitu rumah Masih kelihatan

play10:58

gituur kalau memang pengin yang bisa

play11:00

sampai terbelah maka kita perlu berada

play11:03

di sebuah daratan yang terletak di dua

play11:06

lempeng bumi yang berbeda contohnya

play11:08

adalah Iceland atau

play11:11

Islandia negara ini daratannya terletak

play11:14

pada dua lempeng bumi yang berbeda dan

play11:16

di sini kedua lempengnya bergerak saling

play11:19

menjauh sehingga lama-lama mereka akan

play11:22

terbelah tapi ini membutuhkan proses

play11:24

dalam waktu yang sangat-sangat

play11:28

lama seperti itu teman-teman Semoga bisa

play11:32

meluruskan potensi gempa ini memang ada

play11:35

dan kekuatannya juga cukup besar tapi

play11:37

gempa ini tidak bisa membelah pulau Jawa

play11:40

dan lagi-lagi yang perlu kita ingat

play11:42

sifatnya adalah potensi bukan prediksi

play11:45

jadi kita belum tahu kapan ini akan

play11:48

terjadi bisa jadi tahun depan 10 tahun

play11:51

lagi atau 100 tahun lagi tapi yang pasti

play11:54

kita harus tetap

play11:56

berhati-hati Jika ada dari teman-teman

play11:59

yang lebih ahli dalam hal geofisika

play12:01

boleh tolong dibantu untuk mengoreksi

play12:03

andai kata ada kekeliruan yang aku

play12:06

sampaikan di video ini sebagian

play12:07

informasinya disederhanakan biar bisa

play12:10

lebih mudah dicerna yang pasti silakan

play12:12

nanti teman-teman merujuk ke informasi

play12:14

yang resmi dari BMKG Oke demikian dan

play12:18

terima kasih

Rate This

5.0 / 5 (0 votes)

関連タグ
Earthquake ImpactSunda MegathrustJava IslandDisaster SimulationTsunami PotentialGeophysicsNatural DisasterEarthquake MagnitudeIndonesia SeismologyDisaster Preparedness
英語で要約が必要ですか?