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The Indian subcontinent has a history of devastating earthquakes. [1] The major reason for the high frequency and intensity of the earthquakes is that the Indian plate is driving into Asia at a rate of approximately 47 mm/year. [2] Geographical statistics of India show that almost 58% of the land is vulnerable to earthquakes.
In general, PTAs do not cover substantially all trade. The India Mercosur Preferential Trade Agreement is an example of a PTA. [2] A free trade agreement (FTA) also involves reducing or eliminating tariffs on items traded between the partner countries; however each maintains individual tariff structure for non-members.
Vietnam free trade agreement [3] China trade and economic agreement; Iran free trade agreement [4] Serbia free trade agreement [5] Singapore free trade agreement [6] European Union Armenia qualifies to export its products under the EU's Generalized System of Preferences (GSP) Georgia [7] Ukraine [8]
The reason for the intensity and high frequency of earthquakes is the Indian plate driving into Asia at a rate of approximately 47 mm/year. [1] The following is a list of major earthquakes which have occurred in India, including those with epicentres outside India that caused significant damage or casualties in the country.
In western India, the Kutch region in Gujarat and Koyna in Maharashtra are classified as a Zone IV region (high risk) for earthquakes. The Kutch city of Bhuj was the epicentre of the 2001 Gujarat earthquake , which claimed the lives of more than 1,337 people and injured 166,836 while destroying or damaging near a million homes. [ 51 ]
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Surface motion map for a hypothetical earthquake on the northern portion of the Hayward Fault Zone and its presumed northern extension, the Rodgers Creek Fault Zone. A seismic hazard is the probability that an earthquake will occur in a given geographic area, within a given window of time, and with ground motion intensity exceeding a given threshold.
The Indian plate (or India plate) is a minor tectonic plate straddling the equator in the Eastern Hemisphere. Originally a part of the ancient continent of Gondwana , the Indian plate broke away from the other fragments of Gondwana 100 million years ago and began moving north, carrying Insular India with it. [ 2 ]