Geography
Terrain as complex mountains. Mountain road thong Chai Located in the middle area of the National Park. Shape of the horizontal arrangement mountains along a Northwest-Southeast. Height approx. 1,65 meters from sea level to medium Almost all national park area as a space, there are very few plains mountains. A slope to the Southwest over the North East 910 m, while the lowest point on the Northeast sea level slope along the 210 metre high and low, just east of North Slope area broadens out, rather than low, South West. (Rain-shadow) along the North-East of the County, National Park. Changes to the Earth of the LAN sang National Park area. Change the duration of the breakdown into 3 ranges that appear clear. Different types of soil and rock by khobotwip Approx. time counter is more than a thousand years ago, in the Precambrian era, the second range has changed shape style 2 important terrain feature is the first to raise or bend of the Carboniferous era (about crust. Million years ago). The stone floor phenomenon, khobotwip broadens out into the sea. The third period was an important change is to twist or break the stone floor of the curved or bent upward. Cause of high mountain and Dale on the Hill
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Characteristics of geological changes such as these cause the various types of stone in the national survey found that there are some wide area radiating gneiss are processed stone, such as marble and limestone. And found stone schist/sludge Somewhere near the surface. These stones can be seen on the LAN sang waterfall, which has at least 350 million bales, each year.
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