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Venus terrain

Updated Thursday, 6th April 2006

Images provided by NASA increase our knowledge of the surface of Venus

This page was published over 16 years ago. Please be aware that due to the passage of time, the information provided on this page may be out of date or otherwise inaccurate, and any views or opinions expressed may no longer be relevant. Some technical elements such as audio-visual and interactive media may no longer work. For more detail, see how we deal with older content.

The surface of Venus has been seen by three methods:

1. Landings by a handful of Soviet spacecraft between 1975 and 1982

Venus by Venera 9
The first ever picture from the surface of Venus, by Venera 9 in 1975. The image is distorted by the camera optics. The horizon is visible in the top left and top right corners. Part of the lander can be seen near the lower edge. [Image: NASA]

2. Mapping the height of the surface by downward-looking radar from orbit
This is known as radar altimetry.

Stardate: Mysteries of Venus: article - Terrain inline 2
A colour-coded surface heights of one hemisphere of Venus (blue lowest, red and white highest). At the NASA Jet Propulsion Laboratory site you can find a similar, animated view of the planet.

3. Constructing an image by means of obliquely looking radar
This process is known as imaging radar.

Stardate: Mysteries of Venus: article - Terrain inline 3
A 350 km wide region of Venus, marked by volcanoes, lava flows and fractures [Image: NASA-JPL Photojournal]

Surprisingly, the distribution of impact craters across the surface of Venus is random, suggesting that the entire surface is all pretty much the same age, estimated at about half a billion years. If so, it seems that the whole globe was resurfaced at that time in a global orgy of volcanism, in which case the volcanoes and lava flows we can see today must be survivors from the waning phase of that episode, and are unlikely to be active today.

This behaviour represents a major difference between Venus and the Earth. Both planets are hot inside because of radioactivity. Earth gets rid of its heat continually, by 'plate tectonics': hot new crust is created at 'mid-ocean ridges' and old cold crust is drawn back into the interior at 'subduction zones' such as beneath the Andes.

A possible explanation for Venus's situation is that its internal heat is stored for hundred of millions of years until the old, cold surface breaks apart and is flooded by magma spilling out from the overheated interior. Then things calm down until the global catastrophe is repeated.

A rival theory that can explain the distribution of impact craters is that Venus's volcanism is on the wane but has continued, off and on, to the present day, creating random patches of lava a few hundred km across at sporadic intervals.

Take a closer look at aspects of Venus terrain by taking a virtual journey across the surface:

Lava flows
Mountain belts

Please note these pages include a number of large images which may take a few seconds to load if you have a slow connection to the internet.

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