Roy W Masters: Difference between revisions
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'''Roy W. Masters''' is a researcher based in Norfolk, United Kingdom, associated with the theory of [[planetary expansion]]. He is included in the ''Worldwide List of Dissident Scientists'' compiled by Jean de Climont. | |||
==Biography== | |||
Masters is based in Norfolk, United Kingdom. Detailed biographical information about him is not established in the available public record. | |||
==Work== | |||
Masters is associated with the concept of [[planetary expansion]], part of the broader field of [[Expansion tectonics|expansion tectonics]]. Expansion tectonics is an alternative geological hypothesis holding that the Earth and other planetary bodies have increased in size and surface area over geological time, offering a different account of continental configuration and crustal movement from that of conventional plate tectonics. | |||
==External links== | |||
* [[Expansion tectonics]] | |||
<br /><br /> | <br /><br /> | ||
[[Category:Scientist|Masters Roy]] | [[Category:Scientist|Masters Roy]] | ||
[[Category:Expansion Tectonics]] | [[Category:Expansion Tectonics|Masters Roy]] | ||
[[Category:Worldwide List of Dissident Scientists]] | |||
Latest revision as of 18:39, 17 July 2026
Roy W. Masters | |
|---|---|
| Residence | Norfolk, United Kingdom |
| Known for | planetary expansion |
Roy W. Masters is a researcher based in Norfolk, United Kingdom, associated with the theory of planetary expansion. He is included in the Worldwide List of Dissident Scientists compiled by Jean de Climont.
Biography
Masters is based in Norfolk, United Kingdom. Detailed biographical information about him is not established in the available public record.
Work
Masters is associated with the concept of planetary expansion, part of the broader field of expansion tectonics. Expansion tectonics is an alternative geological hypothesis holding that the Earth and other planetary bodies have increased in size and surface area over geological time, offering a different account of continental configuration and crustal movement from that of conventional plate tectonics.
External links