An area of plains with water all year round on the West side of the National Park is the thung Sam Roi Yot, which in the past used to be sea or Bay subsequently was blocked by silt, sand and the sea to pull back towards to get fresh water influence from Earth. With the accumulation of silt Plains gradually became brackish water and freshwater rice paddy fields, respectively. Fresh water in thung Sam Roi Yot is part of the cradle from the mount Tanintharyi flowing through the Huai phrodok. Huai khamin Chin Huay Huay Rai of Nong Ta find and then cooled down to the sea by Canal, Red Hill. Another part flows from the Sam ROI Yod mountains. Thung Sam Roi Yot has an average depth of 3 meters of water.Due to his Earth environment Sam Roi Yot is limestone with high slope. Cause a steep cliff and deep Dale With the height of the highest mountain peak in the National Park to 605 meters from sea level to medium. Important peaks include mount mountain tents, straw, chalong. Khao Yai He is much bigger than the cave. He is red. He Tian He was in the Valley on Monday and he stepped this Earth environment area, etc into the limestone has many limestone is a natural effect of erosion or corrosion has become a cave or abyss that large funnel: the cave of glass. Tham Sai Phraya Nakhon cave, etc.
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