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Durga Puja (worship of Durga) is a major religious festival for Hindus in West Bengal, Bihar, Tripura, Odisha, Assam, Mithila and other parts of India and Bangladesh. In the rest of India, it coincides with Navaratri and Dussehra, and with Dashain in Nepal, all of which signify the victory of good over evil. Durga Puja is celebrated in autumn (Sharad), in the months of September or October. In Kolkata, Durga Puja was first organised in 1610 CE by the Sabarna Roy Chowdhury family at their ancestral home at Barisha. They were zamindars (hereditary landowners with the right to collect tax) during the Mughal period and held zamindari rights of Sutanuti, Gobindapur and Kolkata villages, which were acquired by the British East India Company (BEIC). The BEIC merged the three villages to establish Kolkata. As the capital of the British Empire, Kolkata emerged as a major trading port, and enterprising Bengalis migrated to the city and made their fortune in business, trade, banking, and working for the BEIC as administrators, civil servants and zamindars. These nouveau riche Bengalis settled in Sutanuti, in what is today’s North Kolkata, where they built palatial mansions along Chitpur Road, the only arterial road of the city 300 years ago. Thus, these Bengali families were the symbols of aristocracy and were considered the foundation of Kolkata’s haute society and high culture. In the eighteenth and nineteenth centuries, they came to be known as bonedibari in colloquial Bengali; bonedi, derived from buniyadi, meaning foundation, and bari meaning house/family.  After centuries of Islamic rule, protection under the British guns of Fort William allowed elite Bengali Hindus to express their religiosity more publicly, and they organised grand festivals, spending astronomical sums of money. Durga Puja celebrations became increasingly popular in bonedi baris of Kolkata, and, for this purpose, a thakur dalan is a common feature in all these mansions. Several weeks before the festiva

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Ocean Bottom Topography Modern technology and various expeditions have revealed that the ocean floor is not a monotonous plain as some have imagined, but rather a topographical complex containing many diverse landform features that are as varied as, if not more diverse than, those found on land. On the ocean floor, there are four major divisions that can be easily identified.    A.    The Continental Shelf.   B.    The Slope of the Continental Plate.   C.    The Rise of the Continent.   D.    The Abyssal Plain   •    Oceanic ridges, hills, seamounts, guyots, oceanic trenches, submarine canyons, oceanic plateau, Bank, Shoal, fracture zones, island arcs, coral reefs, submerged volcanoes, and sea-scarps are just a few of the associated and minor landform features.   •    The interaction of tectonic, volcanic, erosional, and depositional processes has resulted in a wide range of relief. The tectonic and volcanic phenomena are more significant processes at greater depths.   Continental Shelf •    The continental shelf is the area along each continent's extended margin that is occupied by relatively shallow seas and gulfs. It is the ocean's shallowest part, with an average gradient of 1° or even less. Typically, the shelf ends at a very steep slope known as the shelf break.   •    The continental shelves vary in width from one ocean to the next. Continental shelves have an average width of 80 kilometers. Along some of the margins, such as the Chilean coasts and the west coast of Sumatra, the shelves are almost non-existent or extremely narrow.    •    On the other hand, the world's largest shelf, the Siberian shelf, stretches 1,500 kilometers across the Arctic Ocean. The depth of the shelves varies as well; on average, they are nearly 200 meters below mean sea level. However, they can be as shallow as

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