This is an image of Venus.
Click on image for full size
NASA

The Cooling of Venus

The following may be the history of Venus.

  • Venus formed about 4 Billion Years ago.
  • at the conclusion of forming it continued to be bombarded with leftover material. Many planets still bear the remains of this activity by showing many craters on the surface. Activity on the surface can act to change the craters.
  • Venus warmed from inside, and separated into layers. Because Venus is close to the sun, the atmosphere formed differently than did the Earth's, as sugggested by the Goldilocks idea.
  • After that, Venus started cooling down. The crust began to thicken, just like jello hardens when it is being made. The hardening crust prevented continental drift. This also prevented the recycling of the atmosphere.
  • Despite the thick crust, surface activity, including volcanism, may continue to this day as Venus continues to cool.

Shop Windows to the Universe Science Store!

Enjoy your love of minerals and fossils through jewelry! We have beautiful Nature's Own jewelry in our online store, including earrings, necklaces, and pendants!

Windows to the Universe Community

News

Opportunities

You might also be interested in:

The Earth Scientist, Volume XXVI, Issue 3, Fall 2010

This very special issue of The Earth Scientist is sponsored by the Mineral Information Institute (MII) and the Society for Mining, Metallurgy and Exploration (SME) Foundation and is designed to provide a variety of resources to teachers and students to learn more about minerals and mining....more

The Earliest History of Venus

As the process which formed them came to an end, the planets may have been left in either of the following two states: very warm, separated into layers, with lots of water on the surface, with volcanic...more

What causes a Planet's surface to change its appearance?

Over the course of time there are many things which can cause the surface of a planet to change its appearance. winds, as shown in the example from the Martian surface Monument Valley on Earth is an example...more

The Crust of Venus

Unlike the Earth's crust, the crust of Venus is very rigid. On Earth, the lithosphere can be pushed aside in response to the warmth of the Earth. The crust then subducts, melts, and becomes part of the...more

Volcanism of Venus

The Magellan mission to Venus confirmed that the surface of Venus is definitely volcanic. As shown in this picture, lava flows extend to hundreds of miles across the plains in the foreground. The surface...more

The History of Venus

The Earth-planets formed with the gathering of rocky material and volatiles out of the primitive solar nebula. As they finished forming, the surface continued to be hit by the remanent of planetary material...more

Does Venus Have a Surface in Motion?

Like Mars, there is no plate tectonics on the surface of Venus. The surface of Venus does not *seem* to have changed or moved in billions of years. Unlike the case of Mars, however, careful examination...more

Volcanic Formations of Venus

One reason scientists think that Venus has a thick crust comes from the shape of the volcanoes of Venus. (This is a different reason than in the case of Mars). In the long time in which the volcanoes exist,...more

Shop Windows to the Universe

The Spring 2011 issue of The Earth Scientist is focused on modernizing seismology education. Thanks to IRIS, you can download this issue for free as a pdf. Print copies are available in our online store.

Generous sponsorship of Windows to the Universe is provided by the Hewlett Foundation, the American Geological Institute, the American Geophysical Union, the National Science Foundation, NASA, NCAR, and the CISM and CMMAP projects. NASA CMMAP AGU CISM NCAR Hewlett AGI NSF