Scientists shocked by size of Mars’ liquid core

NASA scientists have used data from the seismology sensors on the InSight probe to understand Mars's internal structure. The probe has detected small quakes since 2019, revealing that Mars's crust is thinner than expected, ranging from 24 to 72 kilometers thick. The planet's core is larger than anticipated, with a radius of 1,830 kilometers, indicating a thinner mantle. This thin mantle likely cannot sustain the pressures needed for the mineral bridgmanite to stabilize, which on Earth blankets the core and slows heat loss. The absence of this mineral on Mars would have led to rapid cooling, initially allowing strong convection in the core and a global magnetic field. However, due to rapid cooling, Mars no longer has a global magnetic field today.

What have NASA scientists studied regarding Mars?

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What does the data from the seismology reveal about Mars's crust?

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What is the significance of the size of Mars's liquid and metallic core?

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How does the absence of a mineral bridge affect Mars's cooling process?

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What is the current state of Mars's global magnetic field?

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