A Char, also known as chora, is a dynamic landform created by sediment deposition. These land masses typically emerge as islands within river channels or along riverbanks. Characterized by their transient nature, chars are surrounded by water bodies such as rivers, lakes, seas, or oceansand their existence and characteristics depend largely on hydrological and sedimentary processes.
Geology
Formation in oceans The oceanic char, often referred to as sandbars or islands, emerge as a result of the accumulation of sediment deposited by ocean currents, tides, and waves.
See also Island
References