Tonlé Sap

Tonlé sap, en blau escur durant la sason sèca, en blau clar las zonas inondablas.

Tonlé Sap (khmer: ទន្លេសាប AFI: [tunleː saːp], literalament granda ribièra (tonle); pas salada (sève), comunament traduit per «grand lac») es un sistèma idrologic que combina un lac d'aiga doça aigat sasonièrament, lo lac Tonlé Sap, e una ribièra, la ribièra Tonlé Sap de 120 km de long, que religa lo lac al flume Mekong. Forman la part centrala d'un sistèma idrologic complèxe, dins la plana inondabla cambotjana de 12 876 km2 cobèrta d'una mosaïca d'abitats naturals e agricòlas que Mekong torna provesir cada an en aiga e en sediments. La formacion de la plana centrala es la resulta de milions d'annadas de despauses e de descargas aluvialas de Mekong. D'un punt de vista geologic, lo lac e la ribièra Tonlé Sap son una representacion actuala del bacin inferior de Mekong que se desplaça lentament mas de contunh. La fluctuacion annadièra del volum d'aiga de Mekong, completada pel regim de la monson asiatica, provòca una inversion del debit unic del flume Tonlé Sap.

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