To Chumphon Thung Maha Group travel community at Koh Yor Island - Koh Pa island - Koh Wiang Island - Koh Kai Island - Koh Ranpadrankai Island and many more Island up the atmosphere Many islands minimalistic sculpture was created from natural ingredients. Seafood, fresh, clear water and white beach to watch the colorful marine life. Clownfish colorful coral anemone waiting for you to experience the Bay View Beach boat cruise the Great Plains. Spacious unit on a unit on a hotel stay.
Koh Yor breeding center Sea King Mongkut County. Attractions for the study. Summary of mind and relaxation Marine Lat Krabang, Bangkok breeding center in Chumphon. Chumphon is a learning center and a marine ecotourism with the scenery and the natural beauty of New Ewsis and promote academic knowledge. It also supports the involvement of local people. Eco-tourism is a major source of the provinces.
At Koh RanpadRankai Island 15-30 meter diving Famous ranked first in 10 of the most beautiful dive sites in the Gulf of Thailand. Watch marine life, colorful fish and colorful coral anemone fish, the whale shark.
About one of Siam the dune The dunes With a length of over 10 km long and it is very rare that we come across beautiful beaches, clear water. Where we do not have to take a boat out to the island. The surrounding area is also well-protected. Sand dunes are very spacious 2,000 acres. With the highest point total in the dunes, some as high as 30 meters above sea level. It's like climbing a pile of sand on a large scale.
The area is a beach dune Caused by natural phenomena That started to change since the late Pleistocene (Late Pleistocene Epoch or Ice Age) or the end of the last ice age about 1.8 million to 14,000 years before present. The ice cover is melting worldwide. Sea level, lower than the current level.
By the Holocene period (Holocene Epoch) about 14,000 years exocrine present. Global ice melting Above current sea level. Causing intrusion of seawater. (Transgression), resulting in a ground current of the coastal river estuaries and coastal plain water Ma Lake flood he Berd cave flag his pillow, he pitched great and limestone mountains, many of the area turned into an island.
Then, 1,500 years before present Sea retreated to the sea level, the current penetration and retreat of the sea (Regression) 2 times, causing sandbars and islands, shoals blocking Bay (Barrier island) off the sea, some of them behind. valleys, dunes Lost cause sea (Lagoon) in later times.
The coastal areas of the monsoon winds are blowing through. Or a wind storm blew bordered annual installments. The open ocean front No Block Island The beach is less steep The declining sea beach width. The size of a grain of sand There is very little light, called silt. (When he had to make friction between the sand) and the blowing sand with Pamela. The wind was blowing like a coastal dune reclamation (Coastal Dune) or the Sand Dune.
The ground lost at sea (Lagoon) on the deposition of the fossil, the more it becomes a so-called peat Peat (Peat Swamp), which are marine sediments (Marine Clay) made acidic residues are below. Peat soil with peat (Peat Swamp) in the deep sea to the swamp. And the habitats of aquatic wildlife is very shallow peat. Brackish water into fresh water Found Samet more common.
Contact area The most beautiful dunes of the country. Most notably in Thailand at Chumphon.
The area is a beach dune Caused by natural phenomena That started to change since the late Pleistocene (Late Pleistocene Epoch or Ice Age) or the end of the last ice age about 1.8 million to 14,000 years before present. The ice cover is melting worldwide. Sea level, lower than the current level.
By the Holocene period (Holocene Epoch) about 14,000 years exocrine present. Global ice melting Above current sea level. Causing intrusion of seawater. (Transgression), resulting in a ground current of the coastal river estuaries and coastal plain water Ma Lake flood he Berd cave flag his pillow, he pitched great and limestone mountains, many of the area turned into an island.
Then, 1,500 years before present Sea retreated to the sea level, the current penetration and retreat of the sea (Regression) 2 times, causing sandbars and islands, shoals blocking Bay (Barrier island) off the sea, some of them behind. valleys, dunes Lost cause sea (Lagoon) in later times.
The coastal areas of the monsoon winds are blowing through. Or a wind storm blew bordered annual installments. The open ocean front No Block Island The beach is less steep The declining sea beach width. The size of a grain of sand There is very little light, called silt. (When he had to make friction between the sand) and the blowing sand with Pamela. The wind was blowing like a coastal dune reclamation (Coastal Dune) or the Sand Dune.
The ground lost at sea (Lagoon) on the deposition of the fossil, the more it becomes a so-called peat Peat (Peat Swamp), which are marine sediments (Marine Clay) made acidic residues are below. Peat soil with peat (Peat Swamp) in the deep sea to the swamp. And the habitats of aquatic wildlife is very shallow peat. Brackish water into fresh water Found Samet more common.
Contact area The most beautiful dunes of the country. Most notably in Thailand at Chumphon.
At KohWiang island The island in front of the village's fields. No man is an living on island. Some of the beaches Some of the rocks The island has a length of approximately 2.5 kilometers and the highest point is 1,200 feet and is the largest island of the Great Bay field. The island is filled with wild varieties. Such as slipper orchids White County Hawrgairo cycads Ancient trees cliffs and wild bird species chamois, such as diameter near ideal order cliffs, around the island are some beach snorkeling coral diversity
Walking up the hill From the beach to the top It may take more than 3.5 hours
Walking up the hill From the beach to the top It may take more than 3.5 hours
