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A public, magnet high school in Philadelphia, Pennsylvania, offering five arts majors and various athletics and extracurricular activities. The school coordinates are 40.082816°N 74.974393°W, located at 11081 Knights Road.
Learn how to determine longitude using a marine chronometer, which was invented by John Harrison in the 18th century. Find out the astronomical method, the formula, the corrections and the challenges of this navigation technique.
UTM is a map projection system that assigns coordinates to locations on the Earth's surface, ignoring altitude and treating the Earth as a perfect ellipsoid. It divides the Earth into 60 zones, each 6 degrees of longitude wide, and uses a transverse Mercator projection with a standard scale factor of 0.9996.
Geodetic coordinates are a type of curvilinear orthogonal coordinate system used in geodesy based on a reference ellipsoid. They include geodetic latitude (north/south), longitude (east/west), and ellipsoidal height (also known as geodetic height).
GEOREF is a grid-based method of specifying locations on the Earth, using a simpler and more flexible notation than latitude and longitude. It was used mainly for air navigation, and can identify quadrangles, areas, and altitudes with varying degrees of precision.
Learn how astronomers, cartographers and navigators discovered a means of determining the longitude of any place on Earth. The invention of the chronometer by John Harrison in the 18th century was a major breakthrough for accurate navigation at sea.
Learn how to obtain and add geographic coordinates to Wikipedia articles from various sources, such as maps, online services, directories, databases and calculators. Find out the preferred geotagging templates and the licensing information for different tools.
Learn about the history, features and uses of the Mercator projection, a conformal cylindrical map projection presented by Gerardus Mercator in 1569. The Mercator projection is widely used for navigation, web maps and atlases, but it distorts the size and shape of landmasses near the poles.
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