मराठी
महाराष्ट्र राज्य शिक्षण मंडळएस.एस.सी (इंग्रजी माध्यम) इयत्ता ७ वी

Find out the following with the help of your teacher and the internet. Seasonal Rains (monsoon) in India and other countries.

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प्रश्न

Find out the following with the help of your teacher and the internet.

Seasonal Rains (monsoon) in India and other countries.

कृती
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उत्तर

A monsoon is a seasonal change in the direction of the prevailing winds of a region. The summer and winter monsoon determine the climate for most of India and Southeast Asia. The summer monsoon is associated with heavy rainfall between April and September. It brings humid climate and torrential rainfall to India, Sri Lanka, Bangladesh, and Myanmar after blowing from the southwest Indian Ocean. Agriculture in these countries relies on these seasonal rains. Too little of it causing drought and too much of it causing floods and the resultant loss of life and property. Winter monsoon that starts in the air above Mongolia and northwestern China is less powerful than its summer equivalent. As these winds change direction with the change of seasons; the rains they bring along are called seasonal rains.

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पाठ 1.3: In Time of Silver Rain - English workshop [पृष्ठ ९]

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बालभारती English Standard 7 Maharashtra State Board
पाठ 1.3 In Time of Silver Rain
English workshop | Q 7.1 | पृष्ठ ९
बालभारती English Integrated Standard 7 Maharashtra State Board
पाठ 1.3 In Time of Silver Rain
ENGLISH WORKSHOP | Q 7. i | पृष्ठ ९

संबंधित प्रश्‍न

The energy stored in coal and petroleum originally came to the earth from the sun. The bulk of the present-day supplies was laid down some 200 to 600 million years ago, when tropical conditions were widespread. Lush, swampy forests produced huge trees; warm coastal seas swarmed with microscopic forms of life. When these organisms died, much of their tissue was recycled as it is today — through scavenging and decay. But a significant amount of dead plant and animal material was covered with mud, which prevented complete decomposition.

With the passage of time, layer upon layer of the fine sediment was deposited over the once-living material; the sheer weight turned the sediments to rock. Sandwiched between the layers, both coal and petroleum were produced and preserved under pressure. Coal was formed mostly of giant fern-like plants that have only small counterparts today. Coal may still be forming here and there on earth, but conditions are not right for the production of significant quantities.

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