The Gravity of Venus (Approximately 0.20–0.30 m/s²) and the Origin of Its Extreme Surface Temperature

This paper presents a rotation-based explanation of gravity, estimating Venus’s surface gravitational acceleration at approximately 0.20–0.30 m/s². It attributes Venus’s extreme heat and volcanic activity to weakened gravity and rising internal heat. Additional observations concerning black holes are included. Detailed calculations will be published separately.

Authors

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-10-14
DOI
https://doi.org/10.5281/zenodo.23371786
Primary Topic
Astro and Planetary Science
Type
preprint
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preprint

The Gravity of Venus (Approximately 0.20–0.30 m/s²) and the Origin of Its Extreme Surface Temperature

Garip Baydemir
Zenodo (CERN European Organization for Nuclear Research)
Astro and Planetary Science
preprint

The Gravity of Venus (Approximately 0.20–0.30 m/s²) and the Origin of Its Extreme Surface Temperature

Garip Baydemir
preprint en

Abstract

This paper presents a rotation-based explanation of gravity, estimating Venus’s surface gravitational acceleration at approximately 0.20–0.30 m/s². It attributes Venus’s extreme heat and volcanic activity to weakened gravity and rising internal heat. Additional observations concerning black holes are included. Detailed calculations will be published separately.

Zenodo (CERN European Organization for Nuclear Research)
Astro and Planetary Science
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