Hypsometry - definição. O que é Hypsometry. Significado, conceito
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O que (quem) é Hypsometry - definição

MEASUREMENT OF LAND ELEVATION (RELATIVE TO MEAN SEA LEVEL)
Hypsography; Hypsometric curve; Hypsometric Curve
  • Hypsography of the Earth. Notice that Earth has two peaks in elevation, one for the continents, the other for the ocean floors.
  • Hypsometric curve of Earth as a histogram.

Hypsometry         
·noun That branch of the science of geodesy which has to do with the measurement of heights, either absolutely with reference to the sea level, or relatively.
Hypsometry         
Hypsometry ()ὕψος, Henry George Liddell, Robert Scott, A Greek-English Lexicon, on Perseusμέτρον, Henry George Liddell, Robert Scott, A Greek-English Lexicon, on Perseus is the measurement of the elevation and depth of features of the Earth's surface relative to mean sea level.
hypsography         
[h?p's?gr?fi]
¦ noun the study and mapping of the relative altitudes of different areas of the earth's surface.
Derivatives
hypsographic adjective
hypsographical adjective

Wikipédia

Hypsometry

Hypsometry (from Ancient Greek ὕψος (húpsos) 'height', and μέτρον (métron) 'measure') is the measurement of the elevation and depth of features of the Earth's surface relative to mean sea level.

On Earth, the elevations can take on either positive or negative (below sea level) values. The distribution is theorised to be bimodal due to the difference in density between the lighter continental crust and denser oceanic crust. On other planets within this solar system, elevations are typically unimodal, owing to the lack of oceans on those bodies.