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भारतीय प्लेट और यूरेशियन प्लेट में होने वाली भूगर्भीय गतिविधियों के कारण यह पूरा क्षेत्र भूकंपीय रूप से संवेदनशील है. रिपोर्ट- नरेंद्र निषाद.

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00:00There is no reason why it is going to fall, whether it is an earthquake, or it is going to
00:05fall, or another trigger factor.
00:08It is a trigger factor, but because of the lake, it is going to fall,
00:13it is going to fall, where there is a fire, where there is a fire.
00:20In the past 20-30 years, there were many new fires in Himalaya,
00:27and there are many small fires in Himalaya.
00:31Therefore, the fires in Himalaya and the fires in Himalaya,
00:35the fires in Himalaya are always going to fall.
00:39So, the fires in Himalaya are going to fall.
00:44When the fires in Himalaya are going to fall,
00:50the fires in Himalaya are going to fall,
00:51the fires in Himalaya are going to fall.
00:57So, this seismology is a different way.
01:01This is an active zone,
01:03and the new fires are going to fall,
01:05the fires in Himalaya are going to fall.
01:19Summer are going to fall in Himalaya,
01:23and then, the clouds are going to fall.
01:24So, this is the one that is going to fall.
01:27Or if the impacts of the thunderstorm,
01:28this events are going to fall,
01:29the waves are going to fall.
01:30But we handle the waves from the waves,
01:32the waves of the waves of the waves of the waves.
01:34And we have to fall in the waves of the waves,
01:36which is a very severe storm.
01:39And the waves of the waves of the waves have been circled.
01:42glacier collapse and debris flow.
01:46Can glacier collapse collapse?
01:50Yes, some people have related to earthquake and seismic events
01:56to the earth.
01:59After this, it became a disaster.
02:03Now, some people say that the earthquake is a different thing
02:07and the glacier is a different thing.
02:10But if you can see both of them,
02:14these are two different ones.
02:16and the glacier is a different choice.
02:20The glacier is different from shock.
02:23It is different from the glacier.
02:27And it can be different from seismic events.
02:30The earthquake and the shock, aftershock.
02:34which is safe, which will come out of the seismic event or the glaciers of the seismic event,
02:45will come out of the study, but it will be possible to change both of them.
02:51How do we know about seismic data, how do we know about the seismic data,
02:56or the landslide or glacier collapse?
03:27In the mountains of the heavens, the main
03:28can be used in both signals.
03:32Can you see some of the glacier
03:34or the big landslides,
03:36such small seismic signals
03:38can be found in which
03:39the danger of the danger?
03:42Now, in our Himalaya region,
03:45there are not many seismometers
03:46that you can monitor
03:48individual glaciers.
03:50Therefore,
03:53the
03:53the
03:57seismic monitoring,
03:58there is no seismic monitoring.
04:01In the whole,
04:03there is no seismic monitoring.
04:05and there is no seismic monitoring.
04:06There is no seismic monitoring in some centers,
04:08but
04:09individual glaciers
04:11are not going to be able to relate
04:13to that.
04:14So, what should we do?
04:16I think we have less monitoring
04:19so what should we do?
04:23This is the
04:24for instance,
04:25at this time,
04:27you can monitor
04:33which gravity is formed,
04:36which gravity is showing up.
04:41You can see
04:43and see the gravity
04:43which gravity
04:46can be destroyed.
04:48which can be destroyed by you, and how big it is, it can be done by the modeling of all
04:57glaciers.
04:57So that's why the government can map all glaciers and see all the buildings
05:04that are destroyed or not.
05:07You can work on the future.
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