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Whenever we speak of cities, towns, or key geographical locations around the Earth, various statistics and pieces of information are associated with these areas. One of the key pieces of information for any global location is its elevation, and this is a general term that tells us how high or low a town or geographic point is, compared to a reference point called a geoid.
Elevation Basics:
When we're talking about the elevation of cities and mountains, the geoid we usually refer to is sea level. So, if we say that a location has an elevation of 1,000 feet (305 m), this means it is 1,000 feet above sea level. Naturally, sea level can vary all around the world, so the definition of 'sea level' used in elevation calculations is simply the mean sea level.
Elevation is the official term used when talking about mountains, too. So when we say that Mount Everest, for example, is 29,029 feet (8,848 m) tall, this is actually a reference to its height above sea level, rather than ground level. Elevation is traditionally measured in meters or feet, with the most common measurement in the United States being feet.
When reading maps, elevation can be displayed in the form of contour or topographic lines. Topographic maps with contour lines show estimated elevation and steepness of various locations and have many uses, both in science and geographic disciplines, as well as engineering and architecture, or even for outdoor activities like orienteering.
Elevation Must Know: