A '''river delta''' is the result of a gradual build up of [[sediment]] on the [[continental shelf]] at the mouth of the [[river]]. They can build up, with the aid of deposition due to flooding, until they are higher than the water around them. This results in the river cutting channels through the delta to reach the now further-away ocean. | A '''river delta''' is the result of a gradual build up of [[sediment]] on the [[continental shelf]] at the mouth of the [[river]]. They can build up, with the aid of deposition due to flooding, until they are higher than the water around them. This results in the river cutting channels through the delta to reach the now further-away ocean. |