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A heightmap created with Terragen The same heightmap converted to a 3D mesh and rendered with Anim8or. In computer graphics, a heightmap or heightfield is a raster image used mainly as Discrete Global Grid in secondary elevation modeling. Each pixel stores values, such as surface elevation data, for display in 3D computer graphics.
Figure 1. Vertical arrows show the topographic prominence of three peaks on an island. The dashed horizontal lines show the lowest contours that do not encircle higher peaks. Curved arrows point from a peak to its parent. The prominence of a peak is the least drop in height necessary in order to get from the summit to any higher terrain.
The Karakoram and Hindu Kush are regarded as separate ranges. Accordingly K2 is only in the table below for reference and not shown on the map on this page. The interactive map on this page ranks Himalayan peaks above 7,500 m (24,600 ft) and is more inclusive.
Mount Everest, Earth's highest mountain. A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock.Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (980 ft) above the surrounding land.
Rather, it is a list of peaks at various heights relative to the relevant datum. This is because the Moon has mass asymmetries: the highest point, located on the far side of the Moon, is approximately 6,500 meters higher than Mons Huygens (usually listed as the tallest mountain).
Terrain (from Latin: terra 'earth'), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. In physical geography , terrain is the lay of the land. This is usually expressed in terms of the elevation , slope , and orientation of terrain features.
The first American to climb Everest, Jim Whittaker, joined by Nawang Gombu, reached the summit on 1 May 1963 on the American Mount Everest expedition and on 22 May on the same expedition Tom Hornbein and Willi Unsoeld were the first the traverse the mountain by climbing via the North Face and descending via the South Col.
Other than SRTM30plus, Earth2014 provides information on ice-sheet heights and bedrock (that is, topography below the ice) over Antarctica and Greenland. Another global model is Global Multi-resolution Terrain Elevation Data 2010 (GMTED2010) with 7.5 arc second resolution. It is based on SRTM data and combines other data outside SRTM coverage.