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The 2 Fethiye earthquakes of 1957 virtually fully destroyed the town. The lower central plain from the delta north to Ang Thong Province is a flat, low area with an average of two metres above sea level. In 1542, a two kilometer-long canal, "Khlong Lat Bangkok", was accomplished. In 1608, a seven kilometer-long "Khlong Bang Phrao" canal was completed and has shortened the Chao Phraya's unique route by 18 km (11 mi). In the low alluvial plain which begins below the Chao Phraya Dam, there are numerous small canals (khlong) which break up off from the principle river. Explore Assistens Cemetery, where well-known Danes similar to Hans Christian Andersen are buried. They don't seem to be a part of the Chao Praya system. Then the mountains which are the pure boundary of the Chao Praya watershed type a divide, which has, to some extent, historically isolated Thailand from different Southeast Asian civilisations. To the west, the central plain of Thailand is drained by the Mae Klong and the east by the Bang Pakong River. The Wang River enters the Ping River near Sam Ngao district in Tak Province. The principal tributaries of the Chao Phraya River are the Pa Sak River, the Sakae Krang River, the Nan River (along with its principal confluent the Yom River), the Ping River (with its principal confluent, the Wang River), and كروز السعودية the Tha Chin River.
In Chai Nat, the river then splits into the primary course and the Tha Chin River, which then flows parallel to the primary river and exits in the Gulf of Thailand about 35 kilometres (22 mi) west of Bangkok in Samut Sakhon. The Nan and the Yom River flow almost parallel from Phitsanulok to Chumsaeng within the north of Nakhon Sawan Province. When measured from the most commonly accepted source, which is the confluence of the Ping and Nan River in Nakhon Sawan, the river measures 372 km (231 mi). The Chao Phraya begins at the confluence of the Ping and Nan rivers at Nakhon Sawan (also known as Pak Nam Pho) in Nakhon Sawan province. Provinces alongside the Chao Phraya include, from north to south, Nakhon Sawan Province, Uthai Thani Province, Chai Nat Province, Sing Buri Province, Ang Thong Province, Ayutthaya Province, Pathum Thani Province, Nonthaburi Province, Bangkok, and Samut Prakan Province. The lower Chao Phraya underwent a number of human-made modifications in the course of the Ayutthaya period.
The barely larger northern plains have been farmed for centuries and saw a significant change from the thirteenth century throughout the Sukhothai Kingdom within the 13th and 14th centuries and the Ayutthaya Kingdom that succeeded it when rice rising intensified with the introduction of floating rice, a a lot sooner-growing strain of rice from Bengal. After this, it flows south for 372 kilometres (231 mi) from the central plains to Bangkok and the Gulf of Thailand. Further north and into the plains of the Ping and the Nan the elevation is over 20 m. Nonetheless, when measured from the longest source, which is the origin level of the Nan River within the Luang Prabang Vary, the river measures 1,112 km (691 mi). The Tha Chin River is the foremost distributary of the Chao Phraya River. The expanse of the Chao Phraya and Tha Chin Rivers and their distributaries, beginning at the purpose at which the distributaries diverge, together with the land amid the triangle formed by the outermost and innermost distributary, form the Chao Phraya delta. The many distributaries of the Chao Phraya delta are interconnected by canals that serve each for irrigation and for transportation. Southern portions of the divide's boundary correspond much less to the nation's political border, because isolation on this space was prevented by the benefit of transportation along the lowlands surrounding the Gulf of Thailand, permitting a unified Thai civilisation to extend past the watershed with out challenge.