Explanation: The Eastern Ghats and Western Ghats are two significant mountain ranges in India, each with distinct characteristics that set them apart. The Western Ghats, located along the western coast of India, are a more continuous and higher range of mountains. They stretch from the state of Gujarat in the north to Tamil Nadu in the south, covering a distance of about 1,600 kilometers. The Western Ghats are known for their high peaks, dense forests, and rich biodiversity. They are also an important source of water for the region, with numerous rivers originating from these mountains.
In contrast, the Eastern Ghats are a discontinuous range of mountains that run along the eastern coast of India. They are less continuous and more broken compared to the Western Ghats. The Eastern Ghats extend from the Mahanadi River in the north to the Pennar River in the south, covering a distance of about 1,000 kilometers. The Eastern Ghats are characterized by their uneven terrain, with several isolated hills and ranges. They have been more affected by erosion over time, leading to a more fragmented landscape.
The geological history of these mountain ranges plays a crucial role in their current physical characteristics. The Western Ghats were formed due to the collision of the Indian and Eurasian tectonic plates, resulting in a more continuous and higher range. The Eastern Ghats, on the other hand, were formed by the uplifting of the Indian landmass and subsequent erosion, leading to a more broken and uneven landscape.
Understanding the physical features of these mountain ranges is essential for comprehending the geographical diversity of India. The Western Ghats and Eastern Ghats not only contribute to the country's rich biodiversity but also play a significant role in the climate and water resources of the regions they span. The Western Ghats, with their continuous range, act as a barrier to the monsoon winds, leading to heavy rainfall on the western side and a rain shadow effect on the eastern side. The Eastern Ghats, being more broken, do not have the same effect on the monsoon winds.
In conclusion, the Eastern Ghats are the correct answer as they are broken and uneven, while the Western Ghats are more continuous and higher. This distinction is crucial for understanding the geographical and geological features of these mountain ranges and their impact on the environment and climate of the regions they occupy.