˜yÐÄvlog

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geoid

[ jee-oid ]

noun

  1. an imaginary surface that coincides with mean sea level in the ocean and its extension through the continents.
  2. the geometric figure formed by this surface, an ellipsoid flattened at the poles.


geoid

/ ˈ»åÏô¾±Ëɔɪ»å /

noun

  1. a hypothetical surface that corresponds to mean sea level and extends at the same level under the continents
  2. the shape of the earth
“Collins English Dictionary — Complete & Unabridged†2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

geoid

/ Âáŧ′´Ç¾±»å′ /

  1. The hypothetical surface of the Earth that coincides everywhere with mean sea level and is perpendicular, at every point, to the direction of gravity. The geoid is used as a reference surface for astronomical measurements and for the accurate measurement of elevations on the Earth's surface.
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Other ˜yÐÄvlog Forms

  • ²µ±ð·´Ç¾±î€ƒd²¹±ô adjective
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˜yÐÄvlog History and Origins

Origin of geoid1

First recorded in 1880–85, geoid is from the Greek word ²µ±ð´Ç±ð¾±»åḗs earthlike. See geo-, -oid
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Example Sentences

Examples have not been reviewed.

As a result, if all of Earth's ocean existed under gravity without factors like wind and tides, the planet would more closely resemble a geoid: Imagine a golf ball melted to the point where some of its dimples expanded and other collapsed, and you have a good approximation a geoid's appearance.

From

These plumes, along with the nearby mantle structure, are believed to form the "gravity" hole because it winds up being the lowest point in that geoid, creating its biggest gravitational anomaly.

From

Forte also claimed the computer simulations did not accurately project the actual shape of Earth as a geoid.

From

“But the geoid low in the Indian Ocean is one of the most profound gravitational anomalies on our planet.â€

From

This produces an exaggerated visualization of our planet’s gravitational high and low spots called the global geoid.

From

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