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Tanah is the Malay/Indonesian word for soil, land or island. It can be found in topography. Tanah Abang – a market district in Jakarta, Indonesia; Tanah Datar – a regency in West Sumatra, Indonesia; Tanah Lot – a temple in Bali, Indonesia; Tanah Merah (disambiguation)
The first modern KBBI dictionary was published during the 5th Indonesian Language Congress on 28 October 1988. The first edition contains approximately 62,000 entries. The dictionary was compiled by a team led by the Head of the Language Center, Anton M. Moeliono , with chief editors Sri Sukesi Adiwimarta and Adi Sunaryo.
Indonesia as a whole had 5,132,000 hectares (19,810 sq mi) of such gardens. [78] The number peaked at about 10,300,000 hectares (40,000 sq mi) in 2010. [79] Central Java is considered the pekarangans' center of origin, according to Oekan Abdoellah et al.; the gardens later spread to East Java in the twelfth century.
A traditional Batak Toba house in North Sumatra. With few exceptions, the peoples of the Indonesian archipelago share a common Austronesian ancestry (originating in Taiwan, c. 6,000 years ago [4]) or Sundaland, a sunken area in Southeast Asia, and the traditional homes of Indonesia share a number of characteristics, such as timber construction and varied and elaborate roof structures. [4]
Tanah Lot (Balinese: ᬢᬦᬄᬮᭀᬢ᭄) is a rock formation off the Indonesian island of Bali. It is home to the ancient Hindu pilgrimage temple Pura Tanah Lot (literally "Tanah Lot temple"), a popular tourist and cultural icon for photography.
Tanah Datar Regency is a landlocked regency (kabupaten) in West Sumatra province, Indonesia. The regency has an area of 1,337.1 km 2 and had a population of 338,484 at the 2010 Census, [ 3 ] which rose to 371,704 at the 2020 Census. [ 4 ]
The Indonesian Wikipedia (Indonesian: Wikipedia bahasa Indonesia, WBI for short) is the Indonesian language edition of Wikipedia. It is the fifth-fastest-growing Asian-language Wikipedia after the Japanese, Chinese, Korean, and Turkish language Wikipedias. It ranks 25th in terms of depth among Wikipedias.
The main processes of soil formation of oxisols are weathering, humification and pedoturbation due to animals. These processes produce the characteristic soil profile.They are defined as soils containing at all depths no more than ten percent weatherable minerals, and low cation exchange capacity.