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The GEBCO chart series was initiated in 1903 by an international group of geographers and oceanographers, under the leadership of Prince Albert I of Monaco.At that time there was an explosion of interest in the study of the natural world and this group recognized the importance of a set of maps describing the shape of the ocean floor.
The Great Sand Sea is an approximately 72,000 km 2 (28,000 sq mi) sand desert (erg) in the Sahara stretched from western Egypt and eastern Libya in North Africa. Most of the area is covered by sand dunes .
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
The Eastern limits of the Philippine Sea [P 1] and Japan Sea [P 2] and the Southeastern limit of the Sea of Okhotsk. [P 3] On the North. The Southern limits of the Bering Sea [P 4] and the Gulf of Alaska. [P 5] On the East. The Western limit of Coastal waters of Southeast Alaska and Br. Columbia, [P 6] and the Southern limit of the Gulf of ...
The Mediterranean Sea, between Africa and Europe The Atlantic Ocean around the plate boundaries (text is in Finnish). The African and European mainlands are non-contiguous, and the delineation between these continents is thus merely a question of which islands are to be associated with which continent.
The map is available to any computer with an internet connection from the website OpenSeaMap.org. This map is updated daily. Offline Map The map can also be loaded on local data storage and can be used on any PC without internet access. This map will also permit use on other devices, such as GPS devices from Garmin and Lowrance, phones, and PDAs.
Such sea passages are often marked as ‘maritime choke points’ where several nations have conflicting interests, increasing the risk of harm from shipping activities and disputes. [ 84 ] Further, most cable locations are publicly available, [ 84 ] making them an easy target for criminal acts such as disrupting services or stealing cable ...
The Cayman Trough (also known as the Cayman Trench, Bartlett Deep and Bartlett Trough) is a complex transform fault zone pull-apart basin which contains a small spreading ridge, the Mid-Cayman Rise, on the floor of the western Caribbean Sea between Jamaica and the Cayman Islands. [1]