TRANSCRIPCIÓNEnglish

It’s Getting Crazy… M7.8 Hits Same Region — Third Major Quake hits with TSUNAMI WARNING !

14m 12s1,899 palabras295 segmentsEnglish

TRANSCRIPCIÓN COMPLETA

0:01

LORD,

0:17

WHOA, this is intense. Magnitude 7.8

0:20

along the Pacific Ring of Fire. And that

0:23

comes just

0:25

shortly after we had some other two

0:28

magnitude 7 plus magnitude 7.6 and

0:31

magnitude 7.3

0:33

and now magnitude 7.8 has just struck

0:38

Indonesia right in the Maluku region one

0:42

of the most complex tectonic zones on

0:44

earth. What is going on with the Pacific

0:47

Ring of Fire or the Pacific plate? Is

0:51

this a ripple effect from the other

0:54

quakes? Because the plate is being

0:55

moved. So, here is what should catch

0:59

your attention, guys. One of the most

1:02

complex tectonic zones on Earth and

1:05

magnitude 7.8 that comes just days after

1:08

two other major earthquakes. Tonga,

1:12

Vanuatu. Three powerful earthquakes,

1:15

different locations, but same systems.

1:19

So what's happening beneath the Pacific

1:21

Ocean right now? Let's break this down

1:24

in a way so that it makes actually

1:26

sense. So this Indonesia quake, let's

1:30

talk about this first. It's not a normal

1:33

plate boundary. You see it on the map.

1:35

It's like a little bit of like a

1:36

enclosed valley. This is one of the only

1:40

places on Earth where a tectonic plate

1:43

is being destroyed. destroyed from both

1:47

sides at the same time. You have

1:50

something that is called double

1:52

subduction. [gasps]

1:53

So as if one subduction zone is not

1:57

dangerous enough, double subduction.

2:00

From both sides, you get the pressure.

2:02

The subduction zones are the most

2:04

dangerous earthquake and volcanic zones

2:07

in the world. and the Pacific ring of

2:09

fire that horseshoe formed ring of fire

2:12

that encloses the Pacific we see the

2:15

mega thrust earthquakes the mega

2:16

tsunamis so magnitude 7.8 for sure can

2:20

create a tsunami but it's dependent on

2:23

different factors so let's have a look

2:26

the Muca sea plate that's where we have

2:30

this magnitude 7.8 gate is being

2:33

crushed, squeezed, and forced downwards

2:37

from both directions. That's how it's

2:40

bent. So that creates stress from

2:44

multiple angles. As you can imagine,

2:47

it's not just one clean fault. So when

2:50

that one finally releases, it releases

2:53

big. That's how you get a magnitude 7.8.

2:57

USGS has now downgraded it to 7.4.

3:00

before. So, but now compare this to

3:04

Tonga and Vanuatu. Those are different,

3:08

but they're still connected. And I'll

3:10

tell you why. Out there with the other

3:13

two, you're dealing with like a more

3:15

classic setup, so to speak. A classic

3:18

subduction zone, dangerous setup. The

3:20

Pacific plate is diving beneath the

3:23

Indo-Australian plate along deep ocean

3:26

trenches. This is pure subduction. And

3:29

when I released my last video about

3:31

these two earthquakes, some of you said,

3:32

"Well, I'm in New Zealand. I haven't

3:34

heard about this." Press says nothing.

3:37

Very surprising if you look at the

3:39

location, right? So

3:42

again, I said this is the fastest

3:44

subduction on Earth. It subducts faster

3:47

than in other spots. So in Tonga,

3:50

especially, the Pacific plate is

3:52

plunging down extremely steep. not at an

3:56

at an an angle. It's extremely deep and

3:59

extremely fast. So that's why this

4:02

region produces very deep earthquakes,

4:05

very powerful earthquakes and serious

4:08

tsunami potential. Vanuatu sits along

4:11

the same system just further along this

4:14

arc. So here's the key difference

4:16

between the three. We have Tonga and

4:19

Vanuatu. Clean, fast, powerful

4:22

subduction. Maluku in Indonesia.

4:25

Chaotic, chaotic collision, double

4:29

subduction, multi-directional

4:31

stress, different mechanics, but part of

4:35

the same larger system. Now, let's zoom

4:39

out a little bit. All of this sits along

4:42

the Pacific Ring of Fire. And at the

4:44

center of it all is one thing, the

4:48

Pacific plate. And that plate is

4:50

massive. It's moving. And right now it's

4:53

diving under Tonga. It's interacting

4:56

with Vanuatu and it is transferring

5:00

stress in fragmented zones of Indonesia.

5:04

So think of it like pressure moving

5:06

through a system. So when one section

5:09

shifts, it can redistribute stress along

5:12

the edges. It's not like dominoes in a

5:15

straight line, but basically what we're

5:19

seeing here, tension is moving through a

5:22

cracked surface. So, and that's what

5:26

makes this moment different because we

5:29

are seeing Tonga move, Vanua move, and

5:32

now Indonesia

5:34

releases a magnitude magnitude 7.8.

5:38

That tells us one thing. The Pacific

5:41

plate system is highly highly active

5:45

right now. Now, does that mean this is a

5:47

foresshock? Now, does that mean a bigger

5:50

quake is coming? No one can say that. We

5:53

just can't say that, guys. But what we

5:56

can say is this.

5:59

This is not quiet behavior. I'm sitting

6:02

along the Pacific Ring of Fire. I'm

6:04

sitting along the dangerous Cascadia

6:07

subduction zone that can produce a

6:09

magnitude 9 plus. We're all doomed on

6:11

the West Coast if that happened. We're

6:14

dealing here with a stressed moving

6:17

system that is releasing energy across

6:20

multiple major boundaries right now. And

6:24

when you see activity like this spread

6:27

across tectonic styles like this, you

6:31

have to pay attention. And we are. So

6:35

there's one more thing. This Indonesia

6:38

quake didn't just happen on land. It

6:41

happened in a region that is surrounded

6:43

by deep ocean, steep underwater slopes,

6:47

and active volcanic arcs. So that means

6:50

that tsunami risk is real. Aftershocks

6:53

could be strong and nearby volcanic

6:56

systems are sitting on top of the same

6:59

unstable ground.

7:02

So we could see some volcanic eruption.

7:05

Indonesia has so many active volcanoes.

7:08

We've seen this with the Kamchatka mega

7:10

thrust earthquake 8.8 that happened last

7:13

year. We saw volcanoes erupt. So three

7:17

major earthquakes in such a short period

7:19

of time. Three different tectonic

7:22

settings. One connected system. The

7:25

Pacific plate is not quiet right now.

7:28

It's moving. And when it moves like

7:30

this, the effects unfortunately do not

7:34

stay in one place. So I know the

7:37

questions arise now. Can this trigger

7:39

earthquakes on the west coast on the

7:41

opposite side of the Pacific plate? Can

7:43

it trigger something in Japan, Kamchatka

7:45

again, Alaska? Well, uh, yeah, we could

7:49

see some shaking, but not in the same

7:51

way Indonesia moved right now. Not in

7:54

the same way that we say, "Oh,

7:55

California is next." Right? The honest

7:58

answer is a quake like this can

8:01

sometimes dynamically trigger

8:03

earthquakes very far away because

8:05

seismic waves are traveling through the

8:07

planet and of course then they can

8:09

disturb falls that are especially close

8:12

to failure if they're already very very

8:14

close to failure. Right? The USGS says

8:16

that this kind of distant triggering

8:18

does happen especially in places that

8:21

are already very active. So, but that

8:25

does not mean guys that this Indonesia

8:27

quake is now directly loading the falls

8:30

off of the coast of the US or Canada or

8:34

Alaska or Japan in some like clean

8:37

domino pattern, right? The farther away

8:39

you get, the weaker the the the direct

8:42

stress on the other fault systems

8:44

becomes. And most large distant quakes

8:47

still do not lead to a major followon

8:51

event somewhere else. what it really

8:54

means that already stressed regions can

8:57

sometimes get a nudge. So, Japan, this

9:01

is the one I would watch most closely

9:04

right now in a in a broad

9:09

ring of fire sense because Japan is

9:12

already one of the most seismically

9:14

active plate boundary systems on Earth

9:17

with major subduction zones and also

9:20

frequent large earthquakes. We see it

9:22

all the time, right? That does not mean

9:24

that a quake is heading towards Japan.

9:27

If we look at the whole Pacific Ring of

9:29

Fire and the earthquakes that happen

9:30

there every day, every day this thing

9:34

shakes every day. So you cannot say

9:36

because it was shaking here, this is why

9:38

it's shaking here. It's constant, right?

9:41

But Japan is exactly the place where

9:46

distant dynamic triggering is at least

9:48

physically plausible because the system

DESBLOQUEAR MÁS

Regístrate gratis para acceder a funciones premium

VISOR INTERACTIVO

Mira el video con subtítulos sincronizados, superposición ajustable y control total de la reproducción.

REGÍSTRATE GRATIS PARA DESBLOQUEAR

RESUMEN DE IA

Obtén un resumen instantáneo generado por IA del contenido del video, los puntos clave y las conclusiones.

REGÍSTRATE GRATIS PARA DESBLOQUEAR

TRADUCIR

Traduce la transcripción a más de 100 idiomas con un solo clic. Descarga en cualquier formato.

REGÍSTRATE GRATIS PARA DESBLOQUEAR

MAPA MENTAL

Visualiza la transcripción como un mapa mental interactivo. Comprende la estructura de un vistazo.

REGÍSTRATE GRATIS PARA DESBLOQUEAR

CHATEA CON LA TRANSCRIPCIÓN

Haz preguntas sobre el contenido del video. Obtén respuestas impulsadas por IA directamente desde la transcripción.

REGÍSTRATE GRATIS PARA DESBLOQUEAR

SACA MÁS PARTIDO A TUS TRANSCRIPCIONES

Regístrate gratis y desbloquea el visor interactivo, los resúmenes de IA, las traducciones, los mapas mentales y mucho más. No se requiere tarjeta de crédito.

    It’s Getting Cr… - Transcripción Completa | YouTubeTranscript.dev