South American and Nazca tectonic plate boundary;
The boundary between the South American and the Nazca plates is a vibrant one. These two plates have the same density, so they collide and lift the land upwards, which is why the Andean Mountain Range formed. Occasionally there are earthquakes and they can be very strong. This is a convergent boundary.
Indian and Eurasian tectonic plate boundary;
The tectonic between the Indian and the Eurasian tectonic plates is also a convergent one, where we have two tectonic plates with the same density pushing against each other, and thus lifting up the land, which is how the Himalayan Mountain Range was formed. The earthquakes are relatively rare, and are of different velocity.
Pacific and North American tectonic boundary;
The border between these two plates is a a convergent one as well, but the Pacific plate has a smaller density than the North American one, so it is subducting underneath it. This brings in a very big geological activity, so there's multiple volcanoes and volcanic activities, as well as a big amount of earthquakes.
Oh okay, so do you have any more info?
Answer:
Linguistically India is divided into two major linguistic families, and few more smaller linguistic families.
Explanation:
India is a country that has the second highest number of languages spoken in one country, 780 to be more precise. The majority of the languages are part of the Indo-Aryan language family, with the Dravidian languages being the second most spoken languages. Some of the smaller linguistic families are the Austroasiatic, Sino-Tibetan, and Tai-Kadai. This enormous diversity when it comes to the languages in India comes from the enormous ethnic diversity among the people of India.
- The Indo-Aryan languages dominate India, apart from the southern part where they are absent.
- The Dravidian languages dominate the southern part of India.
- The smaller linguistic families are either located on the periphery of the country, or have small dispersed enclaves across the country.
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