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In 1953, the cartographer Marie Tharp generated the first three-dimensional relief map of the ocean floor which proved there was an underwater mountain range in the middle of the Atlantic, along with the Mid-Atlantic Ridge. [7] The survey data was large step towards many more discoveries about the geology of the sea. [6]
The {{Location map}}, {{Location map many}}, and {{Location map+}} templates have parameters to specify an alternative map image. The map displayed as image1 can be used with the relief or AlternativeMap parameters. Examples may be found below or in the following: Template:Location map#Relief parameter; Template:Location map+/relief
name = Atlantic Ocean Name used in the default map caption; image = Atlantic Ocean laea location map.svg The default map image, without "Image:" or "File:" image1 = Atlantic Ocean laea relief location map.jpg An alternative map image, usually a relief map, which can be displayed via the relief or AlternativeMap parameters
Relief map with the East Pacific Rise (shown in light blue), extending south from the Gulf of California. The East Pacific Rise (EPR) is a mid-ocean rise (usually termed an oceanic rise and not a mid-ocean ridge due to its higher rate of spreading that results in less elevation increase and more regular terrain), at a divergent tectonic plate boundary, located along the floor of the Pacific Ocean.
An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between 3,000 meters (9,800 ft) and 6,000 meters (20,000 ft).Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains are among the flattest, smoothest and least explored regions on Earth. [1]
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name = Pacific Ocean Name used in the default map caption; image = Pacific Ocean laea location map.svg The default map image, without "Image:" or "File:" image1 = Pacific Ocean laea relief location map.jpg An alternative map image, usually a relief map, which can be displayed via the relief or AlternativeMap parameters
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