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InSight: Mars’ crust is thin, and its interior is many layered with a molten core

Scientists yesterday released results from the seismometer on the Mars InSight lander that suggest that the crust of the red planet is thin and that its interior is many layered with a molten core.

[T]wo moderate quakes, at magnitude 3.7 and 3.3, have been treasure troves for the mission. Traced to Cerberus Fossae, deep fissures in the crust 1600 kilometers east of the landing site that were suspected of being seismically active, the quakes sent a one-two punch of compressive pressure (P) waves, followed by sidewinding shear (S) waves, barreling toward the lander. Some of the waves were confined to the crust; others reflected off the top of the mantle. Offsets in the travel times of the P and S waves hint at the thickness of the crust and suggest distinct layers within it, Brigitte Knapmeyer-Endrun, a seismologist at the University of Cologne, said in an AGU presentation. The top layer may reflect material ground up in the planet’s first billion years, a period of intense asteroid bombardment, says Steven Hauck, a planetary scientist at Case Western Reserve University.

At 20 or 37 kilometers thick, depending on whether the reflections accurately trace the top of the mantle, the martian crust appears to be thinner than Earth’s continental crust—a surprise. Researchers had thought that Mars, a smaller planet with less internal heat, would have built up a thicker crust, with heat escaping through limited conduction and bouts of volcanism. (Though Mars is volcanically dead today, giant volcanoes dot its surface.) A thin crust, however, might mean Mars was losing heat efficiently, recycling its early crust, rather than just building it up, perhaps through a rudimentary form of plate tectonics, Mojzsis says.

The thin crust provides a solid basis for explaining the large volcanoes and vast lava plains on the planet. Combined with the light gravity, magma would have found an easier path to the surface. Handed this knowledge, planetary geologists can now make a first stab at outlining more precisely the planet’s early volcanic history.

Conscious Choice cover

Now available in hardback and paperback as well as ebook!

 

From the press release: In this ground-breaking new history of early America, historian Robert Zimmerman not only exposes the lie behind The New York Times 1619 Project that falsely claims slavery is central to the history of the United States, he also provides profound lessons about the nature of human societies, lessons important for Americans today as well as for all future settlers on Mars and elsewhere in space.

 
Conscious Choice: The origins of slavery in America and why it matters today and for our future in outer space, is a riveting page-turning story that documents how slavery slowly became pervasive in the southern British colonies of North America, colonies founded by a people and culture that not only did not allow slavery but in every way were hostile to the practice.  
Conscious Choice does more however. In telling the tragic history of the Virginia colony and the rise of slavery there, Zimmerman lays out the proper path for creating healthy societies in places like the Moon and Mars.

 

“Zimmerman’s ground-breaking history provides every future generation the basic framework for establishing new societies on other worlds. We would be wise to heed what he says.” —Robert Zubrin, founder of founder of the Mars Society.

 

All editions are available at Amazon, Barnes & Noble, and all book vendors, with the ebook priced at $5.99 before discount. The ebook can also be purchased direct from my ebook publisher, ebookit, in which case you don't support the big tech companies and I get a bigger cut much sooner.

 

Autographed printed copies are also available at discount directly from me (hardback $24.95; paperback $14.95; Shipping cost for either: $5.00). Just email me at zimmerman @ nasw dot org.

4 comments

  • Chris

    So with a thin crust I would expect the seismometer could pick up the impact of a booster or other item IFF it hit in a relatively close but known location.

  • A thin Martian crust would be somewhat surprising. I’d thought it would be thick for the reasons cited. If Mars is ‘”. . . losing heat efficiently . . “, how, exactly, is that accomplished?

  • Dick Eagleson

    So Mars is a New York pizza and not a Chicago pizza.

  • Max

    I am with Blair Ivey on this one, the Martian moons are not much more than captured astroids, the tidal pull would be insufficient to keep a large hot molten core for this reason, unlike earth. Let’s explore other factors.

    A meteor impact to create a hole in the Martian surface as big as the Helena’s basin “without a thick crust” would’ve broken the planet, or had been filled with molten core lava. (note that Mars does not have rings, or a moon formed from the debris)
    The observed evidence suggest a hypothesis that the Helena’s impact created the Thyrsus bulge on the opposite side of the planet. The fractured “thick” crust allowed the volcanoes to relieve the pressure as the fragments of the surface pushed softly, over millions of years, back into their resting possibly floating position.

    This occurred long after the entire northern hemisphere was flattened thousands of feet lower than the southern hemisphere by what could’ve been an immense impact, or a minutes long plunge through an atmosphere of a gas giant… or through the edge of the sun itself if Mars was a moon of a theoretical missing planet where the astroid belt is now. (something happened to cover Mars with craters… )
    Either way, Mars has had a good reason to still have a molten core.

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