Terrain
mountainGeneral Condition
Chang Khao Orion It is an ancient site in the group of Wat Pho Ta - Son-in-law. which is a group of ancient sites in the plains area of the northern ridge of Phu Phra Bat The area surrounding the ancient site is a forest. Located near the viewpoint of Phu Phra Bat, Pha Sadet.
The condition of the source is a large rock shack consisting of boulders 3 meters wide, 8 meters long, 1.8 meters high from the ground, stacked on a hollow rock core. inside stone shed and the rock cavity formed by the rock, resulting in the appearance of two interconnected rooms within the stone shed, with an entrance into the stone shed on the north (Pitachai Chatuchai 2010 :61-62)
Phu Phra Bat is a small sandstone mountain. A child in the Phu Phan mountain range or Phu Phan Kham. The average height above sea level is about 320-350 meters. The west of the mountain is steep. and cant descend to the east.
Phu Phan or Phu Phan Kham is a sandstone mountain range that lies in the north-south direction. in the west of Udon Thani Province and Sakon Nakhon Basin
The general condition of Phu Phra Bat is sparse forest. There are natural vegetation types such as hardwood trees, maka wood, red wood, Ching Chang wood, Pradu wood, and deciduous dipterocarp trees. On Phu Phra Bat, there are many open stone terraces, rocks and sandstone sheds scattered around. caused by the action of water and wind on the sandstone.
Because there are quite a lot of hardwood covered. Together with many other natural plants, Phu Phra Bat is classified in the National Reserved Forest Area, “Pah Khuean Nam”, and is the source of many streams such as Huai Hin Lat, Huai Dan Yai, Huai Hin Rong, Huai Nang Usa and Huai Khok Khat. which flows into the east, confluence with the Mekong River at Tha Bo District Nong Khai Province
The plains surrounding the mountains are mainly cultivated for rice and cassava. The eastern valley of Phu Phra Bat is the largest valley characterized by undulating plains. Most of the area is cultivated for rice and cassava. This valley is commonly known as Lup Phan.
Height above mean sea level
314 metersWaterway
Huai Hin Lat, Huai Dan Yai, Huai Hin Rong, Huai Nang Usa, Huai Khok Khad, Huai Mong, Mekong River
Geological conditions
Phu Phra Bat is a sandstone hill. in the Phu Phan Noi mountain range at the edge of the western plateau of Udon Thani Sandstone is white, orange, pebbled, grit consists of quartz, chert, red talc. some igneous rocks with traces There are shale and gravel interspersed. It is in the Phu Phan rock unit, Korat series, in the lower - mid-Cretaceous period, or about 90-140 million years ago. The sandstone in the area has outstanding geological features. Because there are different properties in each floor. and has undergone geological erosion by water and wind. Makes the appearance of the landscape that is strange in many areas, such as Hor Nang Usa, Tham Chang, Father Ta's coffin, Thao Baros coffin, Nang Usa coffin, Pho Ta temple, Phra Ku Nang Usa cave, Nang Usa pond. Quail Stone Shed as well as the geological, physical and geological features found in the sandstone. which is a clear stratum or sedimentary rock For example, showing interleaving layers with gravel layers. An oblique-level display showing a change in water flow direction. (Department of Mineral Resources 2009 :38-39)
various shapes formed from sandstone and gravel sand have different texture The highly durable rock layers protrude into rock sheds. or a layer of rock overlaid on top The less durable rock layers will erode. or being eroded or is a concave part under the hard rock Become a rock shed or a rocky cliff such as Hor Nang Usa, etc.
Archaeological Era
prehistoric age, historical periodera/culture
Dvaravati period, Metal period, Late prehistoric periodArchaeological age
Approximately 3000-2,500 years ago, 14-16 Buddhist centuryTypes of archaeological sites
Habitat, Religious Sitearchaeological essence
The condition of the source is a large rock shed consisting of boulders measuring 3 meters wide, 8 meters long, 1.8 meters high from the ground, stacked on a hollow rock core. (62) Inside the rock shed and the rock cavity that formed the rock formed the appearance of the rooms that are connected within the stone sheds of 2 rooms with the entrance to the stone sheds to the north In addition, in front of the stone shed on the south side, a 25 cm hole was extracted.
Archaeological evidence has been extracted into two 20-centimeter diameter holes in the innermost corner of the chamber and a hole in front of the entrance of the stone shed. Diameter 30 cm. (Pitachai Chatuchai 2010 :61-62)
In the past, not so long ago Villagers used to use the hunter's rice barn as a place to trap animals. and said that paddy was found in this rock shelter, so it was called Chang Khao Nai Pran.
Pitakchai Chatuchai (2010 :63) assumed that from the nature of the source that is a large rock shed and hollow inside which can be used as a shelter from the sun as well Therefore, it is suitable for use as a residence. And the pits resulting from the ground extraction are traces that show their use as a residence or residence of monks in the historical Dvaravati and later periods.
Chaiwat Sirisumsuwan,