Nan River at Wat Tha Luang, Phichit Province
|- left||Wa River, Pat River, Khwae Noi River, Wang Thong River|
|- right||Yom River|
|Cities||Nan, Uttaradit, Phitsanulok, Phichit, Nakhon Sawan|
|- location||Luang Prabang Range, Bo Kluea District, Nan Province|
|- elevation||1,240 m (4,068 ft)|
|Mouth||Confluence with Ping River|
|- location||Pak Nam Pho, Nakhon Sawan Province|
|- elevation||25 m (82 ft)|
|Length||740 km (460 mi)|
|Basin||57,947 km2 (22,373 sq mi)|
|Discharge||for Nakhon Sawan|
|- average||472 m3/s (16,669 cu ft/s)|
|- max||1,522 m3/s (53,749 cu ft/s)|
The Nan River originates in the Luang Prabang Range, Nan Province. The provinces along the river after Nan Province are Uttaradit, Phitsanulok and Phichit. The Yom River joins the Nan River at Chum Saeng District, Nakhon Sawan Province. When the Nan river joins together with the Ping River at Pak Nam Pho within the town Nakhon Sawan it becomes the Chao Phraya River. The Nan river runs about 390 miles south.
The chief tributary of the Nan is the Yom River, which joins the Nan within Chum Saeng District in Nakhon Sawan Province. Other direct tributaries include the Butsabong and Wang Pong rivers of the lower Nan Basin, the Wat Ta Yom and Wang Thong Rivers which join the Nan within Phichit Province, the Khwae Noi River which joins the Nan within Phitsanulok Province, the Tron and Pat Rivers, which join the Nan within Uttaradit Province, the Wa, Haet, Pua, Yao and Hao Rivers, which join the Nan within Nan Province.
Greater Nan Basin
The expanse of the Nan River's tributaries, i.e. the Nan River System, together with the land upon which falling rain drains into these bodies of water, form the Greater Nan Basin, which is part of the Chao Phraya Watershed. The total area drained by the Nan and its tributaries is 57,947 km². Much of the lower basin has perfect soil for farming.
Most drainage analyses, however, divide the Greater Nan Basin into the Nan Basin and the Yom Basin. Using this convention, and subtracting the 23,616 km² of land drained by the Yom and its tributaries, the Nan basin drains a total of 34,331 km² of land in the provinces of Phitsanulok, Phichit, Nan and Uttaradit.
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Early Nan River Civilizations · Tai
|Modern Siam / Thailand|
Ancient civilizations lived in the fertile land along the Nan River and its tributaries, as is evidenced by Stone Age tools unearthed near Phitsanulok. However, these early hunter-gatherers are not likely to be ancestors of the Tai who presently inhabit the Nan basin. The human population around the Chao Phraya River and its tributaries, such as the Nan, remained sparse until late in the region’s history. The settlement of the indigenous populations of the region began around the advent of rice agriculture during the Bronze Age, and continued through the Iron Age. Archaeologists suspect that Mon–Khmer speaking tribes spread through the region, bringing rice agriculture, metalworking, domestic animals. The main course of migration during the metal ages probably ran along the coast of Thailand, but migrants also travelled inland along the Chao Phraya to the Nan Basin and other areas, where it was relatively easier to establish settlements. The next major wave of migration into the Nan Basin came not from the coast along the Chao Phraya, but rather from the mountainous areas of northern Thailand. These migrants were the Tai. Their course of immigration probably began south of the Yangzi River. As the Han Chinese spread south of the Yangzi around the sixth century BC, the ancestors of the Thai retreated into the high valleys and, over many centuries, migrated west along an arc from the Guangxi to the Brahmaputra Valley. The Thai brought rice-farming expertise to the mountainous areas of Northern Thailand, and eventually to the Nan Basin and the other lowland regions of Thailand. Some of the Nan River Mon-Khmer retreated into the hills as the Thai expansion continued, while others generally adopted dialects of the Tai language and blended into the culture of the new settlers. The Tai language spoken in the area was heavily influenced by the Khmer culture as well, and evolved into the language we now call Thai, which is considerably different from other Tai dialects. Even after this Thai migration, the population in the Nan Basin, other than along the banks of the Nan River and its major tributaries, was sparse. predator animal species, as well as malaria, tropical temperatures and other hardships, kept the population from expanding far from the river, despite the region's extremely fertile soil. As the population grew during these ancient times, settlements along the Nan eventually became more urban, as populations of larger scale were better able to survive the hardships of the heavily forested region. The earliest urban developments along the Nan were modelled after the Mon-Khmer capital at Angkor in Cambodia, which was already quite advanced by the time the Nan Basin had significant population to support urban settlement. Along with the positive effects of urbanization (e.g., development of art and specialization of labor), however, came slavery, war and other societal problems associated with urban culture in the forecoming city-state period. Even in spite of urbanization along the river banks, most of the Nan Basin (aside from the river-side settlements) consisted of virgin forests until around the turn of the 20th century. One of the early river-side urban areas of the Nan emerging during the era of the Khmer Empire was Song Khwae, which over the years developed into the modern city of Phitsanulok.
Phitsanulok is the only place in Thailand where houseboats are legal, as they have been an important aspect of regional culture since long before the drafting of modern municipal law. People of Phitsanulok still gather on houseboats and raft houses along both sides of the Nan River in the city, and adhere to a traditional way of life. There is even a floating houseboat museum along the Nan in Phitsanulok, which allows tourists to experience the Nan houseboat culture first-hand.
The Naresuan Dam, named after King Naresuan, was constructed throughout the span of 1976 through 1985 on the Nan River in Phitsanulok Province, north of the city of Phitsanulok, as part of the Phitsanulok Irrigation Project.
Water quality in the Nan River is deteriorating from heavy bacterial contamination attributed primarily to the rapid increase of urban development in the provinces of Phitsanulok, Phichit, Nan and Uttaradit.
- Lonely Planet Thailand, Vietnam, Laos & Cambodia Road Atlas
- River and Watershed Facts on the Chao Phraya
- ISBN 978-0-521-01647-6 A History of Thailand
- Phitsanulok on ThaiWebsites.com
- Phitsanulok Irrigation Project
|Wikimedia Commons has media related to Nan River.|
- Barr, Sandra M.; Alan. S. Macdonald (October 1987). "Nan River suture zone, northern Thailand". Geology; v. 15; no. 10. Geology (journal). pp. 907–910. doi:10.1130/0091-7613(1987)15<907:NRSZNT>2.0.CO;2. "ABSTRACT: The Nan River suture zone consists of a belt of ophiolitic mafic and ultramafic rocks formed in a back-arc or inter-arc setting, and metasedimentary rocks including epidote-crossite blueschists that may represent an inner-trench sequence. These rocks are probably pre-Permian in age. The Nan River belt forms part of the suture between the Indosinian and Shan-Thai cratonic blocks and is inferred to correlate with the Changning-Shuangjiang suture zone in southern China."