Generated by GPT-5-mini| Khorat Plateau | |
|---|---|
| Name | Khorat Plateau |
| Subdivision type | Country |
| Subdivision name | Thailand |
| Area total km2 | 155000 |
Khorat Plateau The Khorat Plateau is a broad, elevated plain in northeastern Thailand, forming the central portion of the larger Indochina landmass and bordering the Mekong River valley, the Cardamom Mountains, and the Chao Phraya River basin. It is bounded by provinces such as Nakhon Ratchasima Province, Khon Kaen Province, Ubon Ratchathani Province, and Nakhon Phanom Province and has been important to regional interactions among Ayutthaya Kingdom, Lan Xang, Dai Viet, and later Rattanakosin Kingdom polities. The plateau's cities include Nakhon Ratchasima (Korat), Ubon Ratchathani, Udon Thani, and Khon Kaen, each connecting to national networks like routes used during the Franco-Thai War and projects associated with ASEAN integration.
The plateau occupies much of northeastern Thailand and intergrades with the Mekong River floodplain to the east, the Phetchabun Mountains to the west, and the Dangrek Mountains to the south; principal watersheds include the Mun River, the Chi River, and tributaries flowing toward the Mekong River. Major urban centers such as Nakhon Ratchasima (Korat), Khon Kaen, Udon Thani, and Nong Khai lie on transport corridors linking to Bangkok, Vientiane, Laos, and Cambodia. The plateau's relief varies from low sandstone mesas and escarpments near the Phu Phan Range to broad alluvial flats around the Mun River. Administratively it spans multiple provinces including Surin Province, Sisaket Province, Buri Ram Province, and Roi Et Province.
Geologically the area rests on Permian to Triassic red-bed sandstones and conglomerates, overlain in places by Quaternary alluvium deposited by the Mekong River system and tributaries like the Chi River; the substrate relates to tectonic episodes recorded in Indochina and influences karst development near the Phu Phan Range. Soil types include sandy ultisols and ferralsols that derive from weathered sandstone and siltstone, with patches of fertile alluvium in the Mun River valley and less productive lateritic surfaces on uplands—conditions similar to soils mapped by agencies such as the Royal Forest Department and studied by institutions including Kasetsart University and Chulalongkorn University. The plateau preserves important paleontological and stratigraphic records connected to regional basins investigated by researchers from the Department of Mineral Resources (Thailand) and comparative studies with basins in Vietnam and Cambodia.
The plateau has a tropical savanna climate under the Köppen climate classification with a distinct rainy season influenced by the Southwest Monsoon and a dry season under the Northeast Monsoon; rainfall is concentrated from May to October, while cool-season northeasterly winds bring lower temperatures from November to February. Seasonal variability affects river discharge on the Mun River and Chi River and has driven infrastructure projects like dams on tributaries studied by the Royal Irrigation Department. Historical droughts and floods have been documented in provincial records from Nakhon Ratchasima (Korat), Ubon Ratchathani, and Khon Kaen, prompting responses from agencies such as the Royal Thai Government and regional initiatives under ASEAN frameworks.
Native vegetation historically included deciduous dipterocarp forests and mixed dry evergreen patches, with species assemblages comparable to communities described in surveys by the Royal Forest Department, IUCN, and academic teams from Mahasarakham University; fauna included large mammals historically recorded in hunting chronicles of the Ayutthaya Kingdom and specimens catalogued in the Bangkok National Museum. Habitat conversion for agriculture has reduced contiguous forest, fragmenting populations of species monitored by Wildlife Conservation Society partners and local NGOs; protected areas such as Phu Phan National Park, Khao Yai National Park (at the plateau’s margins), and smaller wildlife sanctuaries conserve remnants of native biota and connect to transboundary conservation initiatives with Laos and Cambodia.
Archaeological sequences on the plateau record prehistoric hunter‑gatherer and agricultural transitions, with sites yielding evidence of pottery, ironworking, and Khmer period remains related to Angkor influence and frontier exchanges with Chenla and later Khmer Empire centers. Excavations and survey projects by teams affiliated with Silpakorn University, Prince of Songkla University, and international collaborators have documented prehistoric sites such as Ban Chiang‑style assemblages and Khmer-era temples related to inscriptions and hydraulic systems similar to those found near Phimai Historical Park and Prasat Hin Phanom Rung. The region’s historical record links to tributary polities mentioned in chronicles of the Lan Xang and contacts recorded during the Bangkok-period reforms under monarchs of the Chakri dynasty.
The plateau is an agricultural heartland specializing in rainfed rice cultivation, cassava, sugarcane, and rubber plantations, supplying markets in Bangkok and export chains mediated by companies headquartered in Samut Sakhon and agribusiness firms documented in trade reports by the Ministry of Commerce (Thailand). Irrigation projects on the Mun River and reservoir schemes undertaken by the Royal Irrigation Department and private firms have changed cropping calendars and enabled multi‑cropping, while urbanization around cities such as Khon Kaen and Nakhon Ratchasima (Korat) has driven industrial estates linked to firms in the Eastern Economic Corridor supply chain. Social and land-tenure issues have featured in studies by Chulalongkorn University and NGOs engaged with communities in Sisaket Province and Surin Province.
Transport arteries across the plateau include Thailand Route 2 (Mittraphap Road), the northeastern railway lines from Bangkok to Nong Khai and branch connections to Ubon Ratchathani, and airport facilities at Udon Thani International Airport and Khon Kaen Airport that link to national and regional hubs such as Don Mueang International Airport and Suvarnabhumi Airport. Cross-border corridors to Laos and Cambodia support trade under ASEAN agreements and projects like the Kunming–Singapore Railway proposals and the East–West Economic Corridor; infrastructure planning involves agencies including the Ministry of Transport (Thailand) and regional development bodies.