A rendering of the terrain of Australia, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Australia, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Africa, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Africa, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of New Zealand, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of New Zealand, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Antarctica, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from https://www.pgc.umn.edu/data/rema/ was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Antarctica, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from https://www.pgc.umn.edu/data/rema/ was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Japan, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Japan, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of The British Isles, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of The British Isles, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Turkey, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Turkey, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Italy, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Italy, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the regions around the Himalayas, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the regions around the Himalayas, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Iceland, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Iceland, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the Iberian Peninsula, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the Iberian Peninsula, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of New Guinea Island, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of New Guinea Island, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Madagascar, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Madagascar, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from GMTED2010 was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the Australian state of Tasmania, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the Australian state of Tasmania, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the Galápagos Islands, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the Galápagos Islands, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the island of Ireland, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the island of Ireland, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the island of Cyprus, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of the island of Cyprus, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Panama, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to height.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.

A rendering of the terrain of Panama, with the surface displaced by the heightmap data and shaded with a gradient ramp colour mapped to occlusion.

Terrain heightfield data from SRTM was used to displace the surface into a topological terrain representation, although the height of the terrain is not to scale with the 2D map representation, and has been exaggerated for artistic purposes.