Magnetic declination has been measured in many countries, including the U . S . The line of zero declination ( the " agonic line " ) in North America runs from the North Magnetic Pole through Lake Superior and southward into the Gulf of Mexico.
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By convention, declination is positive when magnetic north is east of true north, and negative when it is to the west . " Isogonic lines " are lines on the Earth's surface along which the declination has the same constant value, and lines along which the declination is zero are called " agonic lines ".
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