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Point Palmyras
Palmyras Point or Point Palmyras is a low headland in the Bay of Bengal. It is located at the eastern end of the Brahmani River delta in the state of Odisha, India, close to the Bhitarkanika wildlife sanctuary, an area of mangroves. False Point, located further south, derives its name from the circumstance that vessels proceeding up the Bay of Bengal frequently mistook it for Point Palmyras. Hugh Murray et al., ''Historical and descriptive account of British India'' (1843) See also *False Point *Bhitarkanika Mangroves Bhitarkanika Mangroves is a mangrove wetland in Odisha, India, covering an area of in the Brahmani River and Baitarani River deltas. History The Bhitarkanika Mangroves were zamindari forests until 1952, when the government of Odisha abolish ... References {{reflist Headlands of India Mangroves ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay Of Bengal
The Bay of Bengal is the northeastern part of the Indian Ocean, bounded on the west and northwest by India, on the north by Bangladesh, and on the east by Myanmar and the Andaman and Nicobar Islands of India. Its southern limit is a line between Sangaman Kanda, Sri Lanka, and the north westernmost point of Sumatra, Indonesia. It is the largest water region called a bay in the world. There are countries dependent on the Bay of Bengal in South Asia and Southeast Asia. During the existence of British India, it was named as the Bay of Bengal after the historic Bengal region. At the time, the Port of Kolkata served as the gateway to the Crown rule in India. Cox's Bazar, the longest sea beach in the world and Sundarbans, the largest mangrove forest and the natural habitat of the Bengal tiger, are located along the bay. The Bay of Bengal occupies an area of . A number of large rivers flow into the Bay of Bengal: the Ganges– Hooghly, the Padma, the Brahmaputra–Yamuna, the Barak†... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brahmani River
The Brahmani is a major seasonal river in the Odisha state of eastern India. The Brahmani is formed by the confluence of the Sankh and South Koel rivers, and flows through the districts of Sundargarh, Deogarh, Angul, Dhenkanal, Cuttack, Jajapur and Kendrapara. Together with the river Baitarani, it forms a large delta before emptying into the Bay of Bengal at Dhamra. It is the second widest river in Odisha after Mahanadi . Sources The Brahmani is formed by the confluence of the rivers South Koel and Sankh near the major industrial town of Rourkela at 22 15'N and 84 47' E. The Sankh has its origins near the Jharkhand-Chhattisgarh border, not far from the Netarhat Plateau. The South Koel too arises in Jharkhand, near Lohardaga, on the other side of a watershed that also gives rise to the Damodar River. Both of these sources are in the Chota Nagpur Plateau. The site of the Brahmani's origin is mythologically reputed to be the place where Sage Parashara fell in love with the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Odisha, India
Odisha (English: , ), formerly Orissa ( the official name until 2011), is an Indian state located in Eastern India. It is the 8th largest state by area, and the 11th largest by population. The state has the third largest population of Scheduled Tribes in India. It neighbours the states of Jharkhand and West Bengal to the north, Chhattisgarh to the west, and Andhra Pradesh to the south. Odisha has a coastline of along the Bay of Bengal in Indian Ocean. The region is also known as Utkala and is also mentioned in India's national anthem, "Jana Gana Mana". The language of Odisha is Odia, which is one of the Classical Languages of India. The ancient kingdom of Kalinga, which was invaded by the Mauryan Emperor Ashoka (which was again won back from them by King Kharavela) in 261 BCE resulting in the Kalinga War, coincides with the borders of modern-day Odisha. The modern boundaries of Odisha were demarcated by the British Indian government when Orissa Province was established ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bhitarkanika
Bhitarkanika Mangroves is a mangrove wetland in Odisha, India, covering an area of in the Brahmani River and Baitarani River deltas. History The Bhitarkanika Mangroves were zamindari forests until 1952, when the government of Odisha abolished the zamindari system, and put the zamindari forests in the control of the state forest department. In 1975, an area of was declared the Bhitarkanika Wildlife Sanctuary. The core area of the sanctuary, with an area of , was declared Bhitarkanika National Park in September 1998. The Gahirmatha Marine Wildlife Sanctuary, which bounds the Bhitarkanika Wildlife Sanctuary to the east, was created in September 1997, and encompasses Gahirmatha Beach and an adjacent portion of the Bay of Bengal. Bhitarkanika Mangroves were designated a Ramsar Wetland of International Importance in 2002. Flora and fauna About 62 mangrove species occur in the Bhitarkanika Mangroves, including '' Avicenna'', ''Bruguiera'', ''Heritiera'' and ''Rhizophora''. Rep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mangroves
A mangrove is a shrub or tree that grows in coastal saline or brackish water. The term is also used for tropical coastal vegetation consisting of such species. Mangroves are taxonomically diverse, as a result of convergent evolution in several plant families. They occur worldwide in the tropics and subtropics and even some temperate coastal areas, mainly between latitudes 30° N and 30° S, with the greatest mangrove area within 5° of the equator. Mangrove plant families first appeared during the Late Cretaceous to Paleocene epochs, and became widely distributed in part due to the movement of tectonic plates. The oldest known fossils of mangrove palm date to 75 million years ago. Mangroves are salt-tolerant trees, also called halophytes, and are adapted to live in harsh coastal conditions. They contain a complex salt filtration system and a complex root system to cope with saltwater immersion and wave action. They are adapted to the low-oxygen conditions of water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
False Point
False Point is a low headland in the Bay of Bengal. It is located in the Kendrapara district of Odisha, India. The point derives its name from the circumstance that vessels proceeding up the Bay of Bengal frequently mistook it for Point Palmyras, less than a degree farther north. A lighthouse is situated 2 km inland from the point, at a place which screens it from the southern monsoon. History False Point is also the name of a harbor in the area. It was reported by the famine commissioners in 1867 to be the best harbour on the coast of India from the Hooghly to Bombay. The anchorage is safe, roomy and completely landlocked, but large vessels are obliged to lie out at some distance from its mouth in an exposed roadstead. The capabilities of False Point as an anchorage remained long unknown, and it was only in 1860 that the port was opened. It was rapidly developed, owing to the construction of the Odisha canals. Two navigable channels lead inland across the Mahanadi delta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hugh Murray (geographer)
Hugh Murray FRSE FRGS (1779–1846) was a Scottish geographer and author. He is often referred to as Hew Murray. Life He was the younger son of Matthew Murray (minister), Rev Matthew Murray FRSE (1735–1791), minister of North Berwick, and his wife, Anne Hill (d.1803) daughter of Ref John Hill, of St. Andrews, and sister of Henry David Hill, professor at St. Andrews, and of George Hill (minister), Rev George Hill. Murray entered the Edinburgh excise office as a clerk. On 22 January 1816 he was elected a Fellow of the Royal Society of Edinburgh. His proposers were Thomas Brown (minister), Rev Thomas Brown, John Leslie (physicist), John Leslie and John Playfair. At this time he was living at 24 Stockbridge, Edinburgh. He was also a Fellow of the Royal Geographical Society of London. Murray was editor of the ''Scots Magazine'' from 1816 to 1817.Hunter, Adrian (ed.) (2020), ''James Hogg: Contributions to English, Irish and American Periodicals'', Edinburgh University Press, pp. 19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bhitarkanika Mangroves
Bhitarkanika Mangroves is a mangrove wetland in Odisha, India, covering an area of in the Brahmani River and Baitarani River deltas. History The Bhitarkanika Mangroves were zamindari forests until 1952, when the government of Odisha abolished the zamindari system, and put the zamindari forests in the control of the state forest department. In 1975, an area of was declared the Bhitarkanika Wildlife Sanctuary. The core area of the sanctuary, with an area of , was declared Bhitarkanika National Park in September 1998. The Gahirmatha Marine Wildlife Sanctuary, which bounds the Bhitarkanika Wildlife Sanctuary to the east, was created in September 1997, and encompasses Gahirmatha Beach and an adjacent portion of the Bay of Bengal. Bhitarkanika Mangroves were designated a Ramsar Wetland of International Importance in 2002. Flora and fauna About 62 mangrove species occur in the Bhitarkanika Mangroves, including '' Avicenna'', ''Bruguiera'', ''Heritiera'' and ''Rhizophora''. Rep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of India
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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