When is tidal heating maximized according to orbital mechanics?
Answer
When moons are locked in orbital resonances with small integer ratios.
Tidal heating is maximized when moons are locked in orbital resonances, ensuring that the point of maximum tidal stress aligns repeatedly, creating a consistent heating cycle.

Related Questions
What is the most potent cause for sustained geological activity on moons far from the Sun?Why does Io lack visible impact craters on its surface?When is tidal heating maximized according to orbital mechanics?What geological feature on Earth's Moon suggests relatively recent, minor tectonic readjustment?Why is Callisto geologically inactive compared to Io or Europa?What observation provides evidence of Enceladus's current geological vitality?What links the presence of subsurface liquid water oceans on both Europa and Enceladus?When analyzing the comparison table, what factor is often more critical than a moon's size in determining its current internal temperature profile?How might Callisto's potential subsurface ocean differ fundamentally from Europa's ocean based on heating mechanisms?What two competing processes define the geological state of a moon, according to the final summary?