Venus Mountains



This is an image of a mountain of Venus.
Click on image for full size version (40K GIF)
Image from: NASA

The four main mountain ranges of Venus are named Maxwell Montes, Frejya Montes, Akna Montes, and Danu Montes. These are found on Ishtar Terra.

Mountain ranges are formed by the folding and buckling of a planet's crust. The mountain ranges of Venus, like those of the Earth, are characterized by many parallel, linear, folds and faults.

The presence of mountain ranges on Venus may provide evidence that the planet's surface is in motion.

The Poles of Venus

Radar Image of Northern Hemisphere

Radar Image of Northern Hemisphere (shows altitude)

North Pole Radar Map with Place Names


Venus Mountains



This is an image of mountains on Venus.
Click on image for full size version (40K GIF)
Image from: NASA

The four main mountain ranges of Venus are named Maxwell Montes, Frejya Montes, Akna Montes, and Danu Montes. These are found on Ishtar Terra.

Mountain ranges are formed by the folding and buckling of a planet's crust. The mountain ranges of Venus, like those of the Earth, are characterized by many parallel folds and faults.

The presence of mountain ranges on Venus may provide evidence that the planet's surface is in motion.

The Poles of Venus

Radar Map of Northern Hemisphere

Radar Map of Northern Hemisphere (shows height)

North Pole Radar Map with Place Names


Venus Mountains



This is an image of mountains on Venus.
Click on image for full size version (40K GIF)
Image from: NASA

The four main mountain ranges of Venus are named Maxwell Montes, Frejya Montes, Akna Montes, and Danu Montes. These are found on Ishtar Terra.

Mountain ranges are formed by the folding and buckling of a planet's crust. The presence of mountain ranges on Venus may provide evidence that the planet's surface is in motion.

The Poles of Venus

Radar Map of Northern Hemisphere

Radar Map of Northern Hemisphere (shows height)

North Pole Radar Map with Place Names



Last modified May 18, 2009 by Randy Russell.
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