Answer:
Therapy???? That's a tough question
The subcontinent has fewer natural barriers to invasion than East Asia.
There are lot of educated people in India who are fluent in English.
Explanation:
The Indian subcontinent and East Asia are both regions in Asia. They border with each other, with the border being on the northern part of the Indian subcontinent and southwestern part of East Asia. These two regions have lot of differences between them, including culture, languages, religion, lifestyle, politics, geography etc., but they also have several similarities too.
One similarity of these two regions is that both of them have natural barriers, which throughout history have helped a lot in their protection. The Indian subcontinent has only two natural barriers, the Himalayas, which are massive and occupy almost the entirety of the northern part of the region, and the ocean. East Asia has multiple natural barriers, including the Himalayas, Taklamakan Desert, several seas, and the taiga.
One big difference between the regions is that in India there are much higher percentage of educated people that are fluent in English than in East Asia. This is mostly because India is a former British colony, so the English language is a legacy from the colonialism, but it is also seen as advantageous when looking for jobs.
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Explanation:
11 What are TWO environmental advantages of
building a high-density development?
<u>D. Landscaping after the development is built helps</u>
<u>D. Landscaping after the development is built helpsoffset the environmental impact.</u>
Answer:
The approximate population of india is about 1.3 billion people (2018)
Explanation:
Answer:
- Plate movements on Earth’s crust create stress.
- This adds energy to the crust, which then bends and breaks, forming mountains and geological basins.
Explanation:
The tectonic plates literally float over the magma. Thus, what makes the tectonic plates move is precisely the movement of this magma! And this movement does not happen at all, but in a cyclical variation, which we call Earth convection currents or cells.
The movement of tectonic plates moving over the asthenosphere (pasty part) interacting over time in a geodynamic process that results in the origin of mountains and geological basins, causing seismic quakes (earthquakes and tidal wave), volcanism, magmatism and other geological events (formation of mountain ranges and underwater pits) all due to these plate movements.
