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Sabarmati River
The Sabarmati River (Gujarati: [sabəɾmət̪iː]) is one of the major west-flowing rivers in India. It originates in the Aravalli Range of the Udaipur District of Rajasthan and meets the Gulf of Khambhat of the Arabian Sea after travelling 371 km (231 mi) in a south-westerly direction across Rajasthan and Gujarat. 48 km (30 mi) of the river length is in Rajasthan, while 323 km (201 mi) is in Gujarat.
The Sabarmati River originates in the Aravalli Range in the Indian state of Rajasthan. The total length of the river is 371 km (231 mi). After travelling 48 km (30 mi) in Rajasthan it flows into the Indian state of Gujarat where it is joined by a left bank tributary, Wakal, near the village Ghonpankhari. From there, the river continues southwest to Mhauri and meets a right bank tributary, the Sei River. Continuing its journey, it is joined by a left bank tributary, the Harnav River, before entering the Dharoi reservoir. After the Sabarmati passes the Dharoi dam it meets another left bank tributary, the Hathmati River. From there, the river flows past the city of Ahmedabad and is joined by a left bank tributary, the Vatrak River. The Sabarmati River continues to flow and drains into the Gulf of Khambhat, in the Arabian Sea.
The catchment area of the Sabarmati basin is 21,674 km2 (8,368 sq mi) out of which 4,124 km2 (1,592 sq mi) lies in Rajasthan State and the remaining 18,550 km2 (7,160 sq mi) in Gujarat. The basin is located in a semi-arid zone with rainfall ranging from 450 to 800 mm (18 to 31 in) in different parts of the basin. The river traverses three geomorphic zones: rocky uplands, middle alluvial plains, and lower estuarine zone.
The major tributaries are the Watrak, Wakal, Hathmati, Harnav, and Sei rivers. Average annual water availability in the Sabarmati basin is 308 m3 (10,900 cu ft) per capita, which is significantly lower than the national average of 1,545 m3 (54,600 cu ft) per capita.
The Sabarmati is a seasonal river whose flows are dominated by the monsoon, with little or no flows post-monsoon. An average flow of 33 m3 (1,170 cu ft) per second was measured at Ahmedabad during the period 1968–1979. Over the past century, the flood of August 1973 is considered to be the largest flood, when a flow of 14,150 m3 (499,700 cu ft) per second was measured at Dharoi.
In Rajasthan, it is believed that the Sabarmati River originated due to the penance of ascetic Kashyapa on Mount Abu. His penance had pleased Shiva and in return, Shiva gave ascetic Kashyapa the Ganges River. The Ganges River flowed from Shiva's hair onto Mount Abu and became the Sabarmati River. In another legend surrounding the origin of the river, Shiva brought the goddess Ganga to Gujarat and that caused the Sabarmati to come into being.
Rajashekhara's Kavya-mimamsa (10th century) calls the river Shvabhravati (IAST: Śvabhravatī). The 11th century text Shringara-manjari-katha calls it "Sambhramavati" (literally, "full of fickleness").
Jain acharya Buddhisagarsuri has written many poems about the Sabarmati River.
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Sabarmati River
The Sabarmati River (Gujarati: [sabəɾmət̪iː]) is one of the major west-flowing rivers in India. It originates in the Aravalli Range of the Udaipur District of Rajasthan and meets the Gulf of Khambhat of the Arabian Sea after travelling 371 km (231 mi) in a south-westerly direction across Rajasthan and Gujarat. 48 km (30 mi) of the river length is in Rajasthan, while 323 km (201 mi) is in Gujarat.
The Sabarmati River originates in the Aravalli Range in the Indian state of Rajasthan. The total length of the river is 371 km (231 mi). After travelling 48 km (30 mi) in Rajasthan it flows into the Indian state of Gujarat where it is joined by a left bank tributary, Wakal, near the village Ghonpankhari. From there, the river continues southwest to Mhauri and meets a right bank tributary, the Sei River. Continuing its journey, it is joined by a left bank tributary, the Harnav River, before entering the Dharoi reservoir. After the Sabarmati passes the Dharoi dam it meets another left bank tributary, the Hathmati River. From there, the river flows past the city of Ahmedabad and is joined by a left bank tributary, the Vatrak River. The Sabarmati River continues to flow and drains into the Gulf of Khambhat, in the Arabian Sea.
The catchment area of the Sabarmati basin is 21,674 km2 (8,368 sq mi) out of which 4,124 km2 (1,592 sq mi) lies in Rajasthan State and the remaining 18,550 km2 (7,160 sq mi) in Gujarat. The basin is located in a semi-arid zone with rainfall ranging from 450 to 800 mm (18 to 31 in) in different parts of the basin. The river traverses three geomorphic zones: rocky uplands, middle alluvial plains, and lower estuarine zone.
The major tributaries are the Watrak, Wakal, Hathmati, Harnav, and Sei rivers. Average annual water availability in the Sabarmati basin is 308 m3 (10,900 cu ft) per capita, which is significantly lower than the national average of 1,545 m3 (54,600 cu ft) per capita.
The Sabarmati is a seasonal river whose flows are dominated by the monsoon, with little or no flows post-monsoon. An average flow of 33 m3 (1,170 cu ft) per second was measured at Ahmedabad during the period 1968–1979. Over the past century, the flood of August 1973 is considered to be the largest flood, when a flow of 14,150 m3 (499,700 cu ft) per second was measured at Dharoi.
In Rajasthan, it is believed that the Sabarmati River originated due to the penance of ascetic Kashyapa on Mount Abu. His penance had pleased Shiva and in return, Shiva gave ascetic Kashyapa the Ganges River. The Ganges River flowed from Shiva's hair onto Mount Abu and became the Sabarmati River. In another legend surrounding the origin of the river, Shiva brought the goddess Ganga to Gujarat and that caused the Sabarmati to come into being.
Rajashekhara's Kavya-mimamsa (10th century) calls the river Shvabhravati (IAST: Śvabhravatī). The 11th century text Shringara-manjari-katha calls it "Sambhramavati" (literally, "full of fickleness").
Jain acharya Buddhisagarsuri has written many poems about the Sabarmati River.