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Vegetation of Southeast Asia Studies of Forest Types 1963-1965

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The general surface is gently undulating with scattered low<br />

hills and shallow lakes. Large areas are flooded during the wet<br />

season, but during the dry season the region suffers severely for<br />

lack <strong>of</strong> water. The soils for the most part are thin and poor in<br />

vegetation (Figs. 126, 12).<br />

Two rivers, the Mun and,the Cliee, have thoir sources on the<br />

western flank and flow parallel across the tableland. They join<br />

near Ubon, close to the border <strong>of</strong> southern Laos, and then fall into<br />

the Mekong. A great portion <strong>of</strong> the area is covered with Deciduous<br />

Dipterocarp forest, forming an important source <strong>of</strong> timber for railroad<br />

ties and firewood.<br />

The northern and western borders <strong>of</strong> the plateau range from ^50<br />

to 600 feet (137-183 m.) above sea level. At the city <strong>of</strong> Ubon the<br />

altitude is reported to be about 150 feet ( J *6 m.). The many flattopped<br />

peaks in the Dong Phraya Yen mountains rise to altitudes <strong>of</strong><br />

about £,500 to ^,000 feet (760-1,220 m.), while the Dong Rek escarpment<br />

is generally about 1,500 feet (^5't ra.), and in places rises<br />

to 2,200 feet (670 m.). From this scarp the land falls sharply toward<br />

the Cambodian plain, but northward the slope is gradual to the<br />

Mu-i River.<br />

At the northeastern edge <strong>of</strong> the plateau there is a belt 30 to<br />

iiO miles (50-96 kms.) wide which drains into the Mekong river. In<br />

this strip the largest fresh-water lake in Thailand, Hong Han, is<br />

located on the outsKirte <strong>of</strong> Sakhon Nakhon (Fig. 66). This lake,<br />

with an area <strong>of</strong> about 64.3 square miles (lo square kilometers),<br />

empties into the Mekong by way <strong>of</strong> the Nam Kam river. The belt is<br />

also drained oy numerous other streams tributary to the Mekong.<br />

CljjTiate: The savanna type climate <strong>of</strong> this region is siir.iJa^<br />

in temperature and rainfall'to that <strong>of</strong> northern Thailand. Since<br />

this region is a plateau, relief has less effect on t,ne climate than<br />

it has in northern Thailand. The rainy season coincides with the<br />

southwest monsoon, which becomes more vigorous and brings torrential<br />

rainfall, especially when typhoons from the South China Sea pass<br />

over the region, usually during June through September. The recorded<br />

monthly extremes 01 rainfall in this region range from 0.2 inches<br />

(5.3 :nm.) in January to 9«7 inches (2'ih mm.) in toy. The highest<br />

temperature <strong>of</strong> record is 109° F. ('J3.0°C.) in April aau the lowest<br />

is 'tl°F. (5«1°C.) in January. The dally range <strong>of</strong> temperature :nay<br />

also be more extreme than elsewhere in Thailand. The distribution<br />

<strong>of</strong> seasons is about the same as in northern Thailand.<br />

('•) <strong>Southeast</strong>ern Region<br />

General features; The Chantaburi area, in the southeast, is<br />

separated from the Korat plateau, on the north, by the valley <strong>of</strong> the<br />

Ban Pakong river. On the west it is flanked, by the Chao Phraya plain;

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