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a type of marsh that is a transitional zone between land and an area, such as a slough, bay, or estuary, with salty or brackish water. Sea: a large expanse of saline water connected with an ocean, or a large, usually saline, lake that lacks a natural outlet such as the Caspian Sea and the Dead Sea. In common usage, often synonymous with the ocean.
Blowhole – Hole at the top of a sea-cave which allows waves to force water or spray out of the hole; Channel – Narrow body of water; Cape – Large headland extending into a body of water, usually the sea; Calanque – Narrow inlet on the Mediterranean coast; Cliff – Tall, near vertical rock face; Coast – Area where land meets the sea ...
Bodies of water by sea or ocean (26 C) Archipelagoes by sea or ocean (10 C) ... Landforms of the East China Sea (3 C, 1 P) I. Landforms of the Indian Ocean (17 C, 4 P)
The World Ocean. For example, the Law of the Sea states that all of the World Ocean is "sea", [8] [9] [10] [b] and this is also common usage for "the sea". Any large body of water with "Sea" in the name, including lakes. River – a narrow strip of water that flows over land from a higher elevation to a lower one
This is typically found where rivers meet the ocean or sea. The wildlife found within estuaries is unique as the water in these areas is brackish - a mix of freshwater flowing to the ocean and salty seawater. [20] Other types of estuaries also exist and have similar characteristics as traditional brackish estuaries. The Great Lakes are a prime ...
The brown-ringed sea cucumber was found on a sea slope at a depth of about 4,400 feet, the study said. ... The South China Sea is a contested body of water in southeastern Asia that borders Brunei ...
If the sill depth is deep, water circulation is less restricted, and there is a slow but steady exchange of water between the estuary and the ocean. Fjord-type estuaries can be found along the coasts of Alaska, the Puget Sound region of western Washington state, British Columbia, eastern Canada, Greenland, Iceland, New Zealand, Chile, and Norway.
Sea levels rose significantly after the end of the last ice age about 8,500 years ago, which would have led to the wall and large parts of the landscape being flooded, according to the study authors.