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The coastline paradox states that a coastline does not have a well-defined length. Measurements of the length of a coastline behave like a fractal, being different at different scale intervals (distance between points on the coastline at which measurements are taken). The smaller the scale interval (meaning the more detailed the measurement ...
Dymaxion map of the world with the 30 largest countries and territories by area. This is a list of the world's countries and their dependencies, ranked by total area, including land and water. This list includes entries that are not limited to those in the ISO 3166-1 standard, which covers sovereign states and dependent territories.
This was the beginning of the coastline problem, which is a mathematical uncertainty inherent in the measurement of boundaries that are irregular. [6] The prevailing method of estimating the length of a border (or coastline) was to lay out n equal straight-line segments of length l with dividers on a map or aerial photograph. Each end of the ...
Perhaps the "perimeter" measurement is instead the length of the land boundary? Then the percentage would be closer to 50%, which seems more plausible to me. pne (talk) 13:04, 3 July 2008 (UTC) (ADD) The reason the Norwegian coast to land ratio is so high is because of the small crevices in the coastline.
The total coastline of the world is much less than the sum of all individual countries; Even though islands seem to be included in the coastline (explicitely mentioned for Canada), it is stated that Norway's coastline is 25k km (also explicitely counting small islands), but then the length of the island coastline alone is supposed to be 58k km
While you can, in theory, get to the subatomic level to measure a coastline, erosion and tides are going to create enough variation that your efforts will be meaningless. When two countries survey their coastline or boarder, they will come up with different values if they use different spatial resolutions and chosen discreet interval.
In localities where the coastline is deeply indented and cut into, or if there is a fringe of islands along the coast in its immediate vicinity, the method of straight baselines joining appropriate points may be employed in drawing the baseline from which the breadth of the territorial sea is measured.
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