•  
  •  
 

Authors

Robert Hill

Proposal

Venus has a nearly perfectly random distribution of craters on its surface. This implies that the Venusian surface is the same age. Astronomers have not found tectonic plates on Venus. How does the planet release its internal heat. One solution proposed by astronomers is lid tectonics. The Venusian surface is similar to one giant plate. This plate thickens over time from underplating. Astronomers have suggested that this lid eventually reaches a dynamically unstable situation and will quickly be pulled into the interior of the planet. The reasons for this idea will be explored and evaluated within a creationary history. The relationship between Venusian tectonics and catastrophic plate tectonics will be discussed.

Keywords

Venus, Tectonics, Subduction, Craters

Disclaimer

DigitalCommons@Cedarville provides a publication platform for fully open access journals, which means that all articles are available on the Internet to all users immediately upon publication. However, the opinions and sentiments expressed by the authors of articles published in our journals do not necessarily indicate the endorsement or reflect the views of DigitalCommons@Cedarville, the Centennial Library, or Cedarville University and its employees. The authors are solely responsible for the content of their work. Please address questions to dc@cedarville.edu.

Share

COinS
 
 

To view the content in your browser, please download Adobe Reader or, alternately,
you may Download the file to your hard drive.

NOTE: The latest versions of Adobe Reader do not support viewing PDF files within Firefox on Mac OS and if you are using a modern (Intel) Mac, there is no official plugin for viewing PDF files within the browser window.