Bua Simma House

Terrain

General Condition

The area around Ban Bua Simma looks like a undulating slope. The area that connects with the Lan Tapak River area and scattered mounds Baan Bua Simma is one of those hills. by a low mound It is about 5 meters higher than the surrounding area that is an agricultural area. There are few large mounds around, namely Non Nok Chaeng, Don Pu Ta, Don Tan and the mound along the entrance to Wat Sa Phang on the north side.

The soil inside the Bua Sim house was made into the soil of the Phon Phisai series. The surrounding area is Phimai soil. The geomorphology is sandstone in the Phu Kradueng rock category. There is a “Huai Nam Lai” flowing through the south of the community. and will eventually flow out into the Chon River, approximately 900 meters to the south.

The condition of the Bua Simma house is now a community. There are densely populated houses. Important archaeological evidence within the community is Bai Sema at Wat Sa Phang. and Ku Ban

Height above mean sea level

Waterway

Nam Chuan, Huai Nam Lai

Geological conditions

The soil inside the Bua Sim house was made into the soil of the Phon Phisai series. Geological characteristics of the archaeological site are classified as Phu Kradueng rocks. The lowest part is sandstone, red, reddish-brown, and reddish-gray. It often contains mica. Some places have thin layers of limestone interspersed. The middle layer consists of sandstone, mudstone, reddish-brown and purple. There are clinker and clinker layers. The rock layers are often covered with thick sediment. Outcropping is rarely found. There are mica sandstone and pebbles. Switch layers appearing at regular intervals. The upper part is alternating powdery sandstone, sandstone, mudstone, and pebbles, calcareous, red-gray and gray-green. The top rock layer outcrops is a red-brown sandstone cliff and has some alternating layers of powdery sandstone. The sandstone layer is 30 cm thick to more than 1 meter. The general rock layer is relatively easily eroded. Conditions of sediment accumulation in rivers with strong currents along the trench. and precipitated on both sides of the river basin, swamp and marsh in a semi-arid climate of 180-145 million years (Department of Mineral Resources 2009:17-18).

Archaeological Era

era/culture

Types of archaeological sites

archaeological essence

Baan Bua Simma is an ancient community. There is evidence of human settlement since the Dvaravati period onwards.

The condition of the Bua Simma house is now a community. There are densely populated houses. Important archaeological evidence within the community is Bai Sema at Wat Sa Phang. and Ku Ban

From the survey of the Fine Arts Department in the past found that Baan Bua Simma can be divided into 4 parts:Baan Bua Simma, Don Pu Ta, Don Tan and Nonok Krang. From the evidence found at that time, both ancient sites and antiquities were found. especially many groups of sema leaves It is assumed that this ancient community has progressed to a certain extent.

Antiques on Don Pu Ta found fragments of clay pots roof tiles Fragments of stucco decorated the building, Fierce Stone, Brali and 3 main sandstone parapets

Nonokkjang, near Don Pu Ta, found 4 parapets and a few fragments of earthenware.

Don Tan found a few fragments of earthenware. But at the entrance of Wat Sa Phang, a dense clay pot was found. clay tobacco pipe crushed stone fragment and the sema leaf group is indeterminate shape Some of the sheets were engraved with patterns, found a total of 12 digits.

Many ancient artifacts were found, such as fragments of pottery. Most of them are coarse-grained earthenware. low temperature sintering In addition, fragments of tough earthenware and porcelain were also found.