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Mars’ Interior Unveiled: Insights From the InSight Lander’s Marsquake Data Expose a Layered Interior Structure

by Sophie Lin - Technology Editor

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Mars‘s Interior Reveals Unexpected structure in New Study

Recent findings from NASA’s InSight lander have unveiled a surprising complexity within the interior of Mars. Data collected from marsquakes – seismic events on the Red Planet – indicates that Mars’s interior isn’t as simple as previously thoght, resembling more of a “Rocky road” than a “Millionaire’s Shortbread” as stated by researchers at Imperial College London.Scientists analyzing the marsquake data have discovered nuances in the planet’s interior structure. This suggests that the Martian mantle holds a frozen record of the planet’s tumultuous beginnings. These findings, published across multiple sources including Astrobiology.com, Yahoo News Singapore, BBC Sky at Night Magazine, and Sci.News,indicate that Mars underwent meaningful geological changes in its early history.

The research sheds light on the formation and evolution of terrestrial planets and provides valuable insights into Mars’s unique geological timeline, offering a deeper understanding of the red planet than ever before.The data was orchestrated through the Platforma de Contratacion del Sector Publico and the analyses available through its resources.

How do the observed frequencies and magnitudes of marsquakes contribute to our understanding of tectonic activity on Mars?

Mars’ Interior Unveiled: Insights From the InSight Lander’s Marsquake Data Expose a Layered Interior Structure

Decoding Martian Seismology: The InSight Mission

The NASA InSight (Interior Exploration using Seismic Investigations,Geodesy and Heat transport) mission,landing on Mars in November 2018,revolutionized our understanding of the Red Planet’s internal structure. Unlike previous missions focused on surface features, InSight was specifically designed to probe beneath the Martian surface, utilizing a highly sensitive seismometer to detect marsquakes – the Martian equivalent of earthquakes. This data has allowed scientists to map the planet’s interior, revealing a surprisingly complex and layered composition. Understanding the internal structure of Mars is crucial for deciphering its geological history and potential for past or present habitability.

The Martian Layers: A Detailed Breakdown

InSight’s data confirmed that Mars, like Earth, possesses a distinct layered structure: crust, mantle, and core. However, the specifics differ substantially, offering clues about the planet’s evolution.

The Crust: The Martian crust is estimated to be between 24 to 72 kilometers (15 to 45 miles) thick.This is considerably thicker than Earth’s oceanic crust but comparable to its continental crust. Analysis of marsquake data suggests the crust is relatively fractured,potentially due to impacts and thermal stresses. variations in crustal thickness are also observed, hinting at regional geological differences.

The Mantle: Beneath the crust lies the mantle, extending down to approximately 1,560 kilometers (969 miles). InSight’s data indicates the Martian mantle is less dense than Earth’s. Interestingly, the upper mantle appears to be relatively dry, lacking the water content found in earth’s mantle. This dryness could explain why Mars doesn’t exhibit plate tectonics.

The Core: The core of Mars is divided into two parts: a liquid outer core and a solid inner core. The outer core is estimated to be about 1,830 kilometers (1,140 miles) in radius and is composed primarily of iron, nickel, and sulfur. The finding of a solid inner core, confirmed in 2021, was a major breakthrough. Its radius is estimated to be around 2,040 kilometers (1,270 miles) – surprisingly large,making up roughly half the planet’s radius.

Key Findings from Marsquake Analysis

The InSight mission recorded over 1,300 marsquakes, providing a wealth of data for analysis. Several key findings stand out:

  1. Magnitude and Frequency: Most marsquakes are relatively small, with magnitudes between 2 and 4 on the Richter scale. However, some larger events have been detected, offering deeper insights into the planet’s interior. the frequency of marsquakes also varies, potentially linked to seasonal changes and tectonic stresses.
  2. Seismic Waves and Travel Times: By analyzing the travel times of seismic waves (P-waves and S-waves) through the Martian interior,scientists can determine the density and composition of different layers. S-waves, which cannot travel through liquids, confirmed the presence of a liquid outer core.
  3. the Martian Magnetic Field: The presence of a liquid iron core suggests that Mars once possessed a global magnetic field,similar to Earth’s. Though, the Martian magnetic field is now weak and localized, indicating that the core’s dynamo action ceased billions of years ago.The reasons for this shutdown are still under examination, but might potentially be related to the planet’s small size and lack of plate tectonics.
  4. Crustal Heterogeneity: Variations in seismic wave velocities reveal significant differences in the composition and structure of the Martian crust. This suggests a complex geological history, with regions of varying volcanic activity and impact cratering.

Implications for Planetary Science and Habitability

The insights gained from InSight’s data have profound implications for our understanding of planetary evolution and the potential for life beyond Earth.

Planetary Differentiation: The layered structure of Mars provides valuable clues about the processes of planetary differentiation – the separation of a planet into distinct layers based on density.

Thermal History: The composition and structure of the Martian interior provide constraints on the planet’s thermal history, helping scientists understand how it cooled and evolved over time.

Past Habitability: The presence of water ice in the Martian subsurface,inferred from geological features and orbital data,raises the possibility of past or present habitable environments. Understanding the Martian mantle’s dryness helps constrain models of water delivery and retention on the planet.

* Comparative Planetology: Comparing the interior structure of Mars to that of Earth, Venus, and other terrestrial planets provides insights into the factors that govern

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