Explanations:The South West monsoon winds are a significant climatic feature of the Indian subcontinent, bringing substantial rainfall during the summer months. These winds originate from the Arabian Sea and move towards the Indian landmass, primarily in a north-east direction. The orientation of mountain ranges in relation to these winds can have a significant impact on the distribution of rainfall and the overall climate of the region.
Among the mountain ranges mentioned in the options, the Aravali Range is the one that lies parallel to the direction of the South West monsoon winds. The Aravali Range is a long chain of mountains that runs in a north-south direction, extending from the northwestern part of Rajasthan to the western part of Madhya Pradesh. This orientation makes it parallel to the path of the South West monsoon winds, which move from the Arabian Sea towards the Indian subcontinent in a north-east direction.
The other mountain ranges mentioned in the options do not align parallel to the South West monsoon winds. The Maikala Range, located in central India, is not aligned in a way that it would be parallel to the monsoon winds. The Satpura Range, also located in central India, runs in a north-south direction but is not parallel to the monsoon winds. Similarly, the Vindhya Range, which is also oriented in a north-south direction, does not align parallel to the monsoon winds.
Understanding the orientation of mountain ranges in relation to the monsoon winds is crucial for comprehending the climatic patterns and the distribution of rainfall in the Indian subcontinent. The Aravali Range, being parallel to the South West monsoon winds, plays a significant role in influencing the climate of the region it passes through.