Chao Phraya River

Definition and stakes

Walter Armstrong Graham,  1911 Encyclopædia Britannica (1911)

“ The country may be best considered geographically in four parts: the northern, including the drainage area of the four rivers which unite near Pak-Nam Po to form the Menam Chao Phaya; the eastern, including the drainage area of the Nam Mun river and its tributaries; the central, including the drainage area of the Meklong, the Menam Chao Phaya and the Bang Pakong rivers; and the southern, including that part of the country which is situated in the Malay Peninsula. Northern Siam is about 60,000 sq. m. in area. ”
Source: Wikisource

William Charles Benett,  Gazetteer of the Province of Oudh Vol-2 -- H. to M. (1877)

“ There are no mountains.
Drainage.—The drainage of the country is carried on by the Gumti and Sai rivers, which in their turn receive small tributary streams. The chief of these is the Bạita, a small perennial stream, which, rising in the Hardoi district, passes through the Malihabad pargana in a south-easterly direction, and falls into the Gumti at a point on its right bank near Kánkrábad. "The Loni, another stream having its source in the Mohanlalganj pargana, passes through it, and joins the river near Salempur on its right bank.
”
Source: Wikisource

H. Warington Smyth,  Notes of a Journey on the Upper Mekong…

“ The scenery of this river is very fine, as all the way from Muang Ngoi, to which we went, it winds through abrupt limestone peaks and ranges, covered with dense forest, and often overhanging the deep quiet river below. But the rapids scattered along its course are furious, and, owing to the shallow water and innumerable sunken rocks, are very dangerous, while quite a high sea runs in them. They differ from most of the big Mekong rapids in that they are caused by rough sloping bottoms of rock ridges, over which the water tears its way. ”
Source: Gutenberg

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