Produced by: Manoj Kumar
A new study reveals that Mars quakes penetrate deep, reshaping theories about its molten core and planetary evolution.
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Meteorite strikes on Mars are 2.5x higher than thought, proving the Red Planet takes cosmic hits regularly.
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Some "marsquakes" aren't tectonic but come from meteoroid impacts, altering how we estimate Martian activity.
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Researchers matched 49 quakes to specific impact craters, linking Mars' surface and seismic events like never before.
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Mars quivers like pudding as seismic waves ripple deep, changing how we map its hidden interior layers.
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Cerberus Fossae's seismic reputation may be flawed—high-frequency quakes there could actually be impacts.
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Mars’ mantle allows seismic waves to travel far, revealing a hidden "highway" beneath its crust.
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Mars’ thin atmosphere can't shield it—making it a cosmic punching bag for meteoroids.
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Rethinking Mars’ seismic wave paths suggests its interior structure may have been misunderstood for decades.
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