हाई रिस्क जोन 6 में पूरी हिमालयन बेल्ट, बढ़ा भूकंप का खतरा, उत्तराखंड के कई शहरों पर विशेष नजर

ETVBHARAT

3 hours ago

भूकंप के ने नक्शे में जोन 6 को जोड़ा गया है. हिमालयी राज्यों को भी इसी नए जोन में रखा गया है. जानिए आखिर क्यों?

Transcript

00:00The government has been working on a new seismic map, which has been kept in the sixth zone.

00:05We are currently working on the Vardia Institute of Human Engineering Geology Director Dr. Rubinit Gahelo.

00:11Sir, the new map has been kept in the sixth zone.

00:17What is the sixth zone?

00:21The old map was kept in the zone 4 and 5.

00:29If you look at it, Dharadun and Shivalik were kept in the zone 4.

00:36After that, the area of Pitharola was kept in the zone 5.

00:41If you look from the Vardia Institute of Human Engineering Geology,

00:44and the way we understand how it is coming in the Uttarakhand or the whole area,

00:49it was not good for us.

00:52It was important that the whole area of Pitharola,

00:59the whole area of Pitharola should be in the high seismic zone.

01:04If you look at it in any kind of seismic zone,

01:11or if you look at the previous one,

01:13or if you look at the first seismic zone,

01:15or if you look at the history of Pitharola,

01:17it was clear that the whole area of Pitharola needs to be one seismic zone.

01:21And because in this area, the Himalaya area,

01:26the most important area of Pitharola,

01:30and the damage of Pitharola,

01:35the vulnerability is very large.

01:38That's why we keep it in the high seismic zone.

01:41Sir, what do we change from 5 to 6?

01:44How much do we map from 5 to 6?

01:46How much do we differentiate this?

01:48Look, every number here,

01:52is the seismic zone 2 to 5,

01:55and now the 2 to 6,

01:59there is a word called seismic coefficient.

02:02If there is a zone,

02:04when there is a seismic zone,

02:07when there is a seismic zone,

02:09there is an acceleration.

02:11With that,

02:13we follow the design of the building.

02:17So, these eyes can be found

02:20that the old seismic zone map

02:23and the seismic zone are slightly different.

02:25Both numbers are the same,

02:27but the corresponding seismic coefficient is different.

02:31So, that's why we don't have to worry about it

02:36that we are going to the seismic zone 6.

02:38There is no doubt about it,

02:40that if there is a seismically vulnerable area,

02:45then it is in the Himalaya area.

02:48So, there is no doubt about it.

02:50So, according to my opinion,

02:51the previous map,

02:52there is a slight decrease,

02:55or that it has been upgraded.

02:57It is a seismic zone in the same area.

03:00It is a seismic zone 4 or 5.

03:02Now,

03:04at least,

03:05we have to overcome that area

03:07and we have to put the whole area

03:09into the seismic zone 6.

03:10Which is perfectly all right.

03:12But,

03:13as I said,

03:15you don't go into numbers.

03:18Look at this,

03:19the first thing we thought

03:21that the building will be made

03:23and the building will be made

03:24and the building will be made

03:25in the other side.

03:26Then,

03:27the building will be made

03:28and the building will be made.

03:29I mean,

03:30it is a big structure.

03:31It is a dam.

03:32But,

03:33now the thing is

03:34perfect.

03:35So,

03:36if we are talking about the whole

03:37Himalaya Thrust,

03:38we have kept the whole zone 6

03:41so,

03:42we are seeing that

03:43a huge shocker

03:44can come from Himalaya?

03:45Or in Himalaya,

03:46in Himalaya,

03:47anywhere?

03:48Look,

03:49there is no problem

03:50with the shocker

03:51of the shocker.

03:52When the shocker comes,

03:53the damage will come from it.

03:54We talk about the damage.

03:55We talk about the damage.

03:56We talk about its damage

03:58and how many of those

03:59have been hurt

04:00in the structures

04:02and as it is done,

04:03we talk about the damage.

04:05Therefore,

04:07with about which the damage

04:09is the damage

04:10which we have made

04:12and the damage

04:13which we have made

04:15in Himalaya,

04:16is the damage

04:17to the whole Himalaya.

04:19So,

04:20when you build the buildings

04:22which you are in the Mookashmir

04:23or in the Vimachal

04:24or in the Assam

04:25you will not make the same style of building.

04:29In this case, in this map,

04:32there is no matter where to go.

04:37We are talking about MCT.

04:39Where is MCT?

04:42The MCT is a geological feature.

04:51It is called fault.

04:53The main central thrust,

04:55which divides the lesser Himalayas and higher Himalayas.

04:59In this case, MCT is the most important part of the context.

05:04In this case, MCT is the most important part of the Himalayas seismic belt.

05:08Whether it is Chamoliot or Uttrakashiyat or Dharachulat.

05:12All are the most important part of the MCT.

05:15What is the most important part of the map?

05:17Since the map is 5 to 6,

05:19we have to do the infrastructure,

05:21which is the most important part of the map?

05:24As I said,

05:25that every seismic zone,

05:27which is the corresponding

05:29one of the seismic factors,

05:33we take it.

05:35So, basically,

05:37if you are in the seismic zone 6,

05:40then you will use the corresponding seismic factor for the building.

05:47You will use it.

05:48So, this means that if you,

05:50as I will again,

05:52that if you are in Dharadun or Pithoragad,

05:55you will have to use the same seismic factor.

05:57You will not have to use it.

05:58But in the previous map,

06:00it was different.

06:01Thank you very much.

06:03The Wadi Institute of Himalayan Geology Director,

06:05Dr. Binit Gheilov,

06:06who told me that the map is going on.

06:08In this case,

06:09it will be kept in the 6th zone.

06:12In any region,

06:13if there is any infrastructure in any region,

06:15you will also move towards the zone.

06:18You will also move towards the zone.

06:19It will also Нов

हाई रिस्क जोन 6 में पूरी हिमालयन बेल्ट, बढ़ा भूकंप का खतरा, उत्तराखंड के कई शहरों पर विशेष नजर

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