Replication Data for: Self-constraining of meandering rivers
<|begin_of_text|><|start_header_id|>system<|end_header_id|> You are a research archivist expert in dataset metadata. Answer the question truthfully.  <|eot_id|><|start_header_id|>user<|end_header_id|> Here is the Description of a dataset. Description:'Meandering rivers are abundantly present on earth, from the largest rivers to the smallest tributaries. The classical view of meandering rivers is a sinuous planform with rounded bends, which grow and migrate until they are cut off. However, many meandering rivers do not show lateral migration and have planforms that are much more complex than this classical view. Based on a detailed palaeogeographic study, we find that low-energy meandering rivers may develop complex planforms with sharp bends, while their self-formed deposits increasingly constrain the lateral mobility of the river channel. This finding is confirmed by data of 48 meandering river reaches of varied scale from around the world, which show that erosion-resistant floodplain deposits are preserved in the river banks when the river energy is below a critical threshold. This' . Please return only a json list of at most 3 Keywords corresponding to the Description:.<|eot_id|><|start_header_id|>assistant<|end_header_id|> {"Answer" : ["Meandering, Planform evolution, Fluvial sedimentology"]} <|eot_id|>
 Here is the Description of a dataset. Description:'Meandering rivers are abundantly present on earth, from the largest rivers to the smallest tributaries. The classical view of meandering rivers is a sinuous planform with rounded bends, which grow and migrate until they are cut off. However, many meandering rivers do not show lateral migration and have planforms that are much more complex than this classical view. Based on a detailed palaeogeographic study, we find that low-energy meandering rivers may develop complex planforms with sharp bends, while their self-formed deposits increasingly constrain the lateral mobility of the river channel. This finding is confirmed by data of 48 meandering river reaches of varied scale from around the world, which show that erosion-resistant floodplain deposits are preserved in the river banks when the river energy is below a critical threshold. This' . Please return only a json list of at most 3 Keywords corresponding to the Description:.
Meandering rivers are abundantly present on earth, from the largest rivers to the smallest tributaries. The classical view of meandering rivers is a sinuous planform with rounded bends, which grow and migrate until they are cut off. However, many meandering rivers do not show lateral migration and have planforms that are much more complex than this classical view. Based on a detailed palaeogeographic study, we find that low-energy meandering rivers may develop complex planforms with sharp bends, while their self-formed deposits increasingly constrain the lateral mobility of the river channel. This finding is confirmed by data of 48 meandering river reaches of varied scale from around the world, which show that erosion-resistant floodplain deposits are preserved in the river banks when the river energy is below a critical threshold. This
Meandering, Planform evolution, Fluvial sedimentology