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Science

Scientists Just Figured Out How Pluto Got Its Heart

Edmund Ayitey
Last updated: February 12, 2025 5:17 am
Edmund Ayitey
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When NASA’s New Horizons spacecraft conducted its historic flyby of Pluto, the world held its breath for a glimpse of the dwarf planet.

What the mission revealed was far beyond expectations—a massive, heart-shaped feature etched into Pluto’s icy surface.

The heart, formally known as Tombaugh Regio, isn’t just a striking visual; it’s a key to understanding Pluto’s complex geology, atmosphere, and climate.

Made predominantly of nitrogen ice, with traces of methane and carbon monoxide, this heart-shaped expanse reflects the intricate interactions of Pluto’s unique environment.

But how did Pluto end up with this iconic “heart”?

A new study sheds light on the extraordinary forces that created and sustain it, offering insights into a distant world where ice behaves like living, breathing matter.


A Closer Look at Pluto’s Heart

Pluto’s heart is not just a patch of ice; it’s a dynamic glacier system that covers a vast area of the dwarf planet’s surface.

The left half of the heart, called Sputnik Planum, is a smooth, 1,000-kilometer-wide plain. Beneath this serene-looking surface lies a basin that plunges 4 kilometers deep.

This basin serves as a “cold trap,” attracting nitrogen and carbon monoxide ices, which accumulate over time.

According to researchers from the Université Pierre et Marie Curie in France, the basin’s unique depth and topography make it an ideal reservoir for these volatile ices.

Using data from New Horizons and a complex simulation spanning 50,000 years, scientists have pieced together the fascinating story of how this icy heart came to be.


Why Nitrogen and Carbon Monoxide Dominate

Nitrogen ice plays a starring role in Pluto’s heart. According to lead researcher Tanguy Bertrand, nitrogen’s unique properties—particularly its solid-gas equilibrium—make it behave in a way that causes it to accumulate in the depths of Sputnik Planum.

At the bottom of the basin, the atmospheric pressure is slightly higher, raising the frost temperature for nitrogen.

This makes nitrogen ice more likely to condense in this region, creating a permanent and stable reservoir of ice.

Similarly, carbon monoxide, which shares many of nitrogen’s volatile characteristics, also accumulates in the basin.

Methane, on the other hand, doesn’t follow the same rules.

Instead of being confined to the basin, methane ice spreads across Pluto’s surface, forming a frost that blankets both hemispheres.

For years, scientists speculated that Pluto’s glacier system was fed by a hidden reservoir of nitrogen beneath the surface.

The idea was that an underground source kept replenishing the ice, allowing it to persist over millennia.

However, this new study challenges that assumption. The research suggests that Pluto doesn’t need an underground nitrogen reservoir at all.

Instead, the volatile ices seen on Sputnik Planum are drawn from Pluto’s thin atmosphere and deposited in the basin due to its unique topography and climate.

This finding fundamentally changes how we understand Pluto’s geology and climate.

Rather than relying on hidden reserves, the dwarf planet’s icy landscape evolves slowly in response to its surface conditions and the extreme length of its seasons.

If you could watch Pluto over hundreds or thousands of years, you’d witness its icy heart “beating.”

This isn’t just a poetic metaphor—it’s a result of the slow, seasonal movements of the ice in response to Pluto’s 248-year-long orbit around the Sun.

During Pluto’s lengthy seasons, the shallower regions of Sputnik Planum allow gases and ices to migrate and shift.

The deepest parts of the basin, however, remain frozen in time, serving as a stable anchor for the glacier.

Over time, the ice flows and retracts, subtly shaping the surrounding mountains and valleys.

As Bertrand explained, “The half-heart glacier inside is a really massive glacier, which is not impacted by the seasonal changes.

It probably formed when the basin itself was created and will remain there in the future.

However, it likely flows and retracts over a few hundred kilometers, eroding and reshaping the terrain.”

In other words, Pluto’s heart is alive in its own way, pulsing with slow, deliberate movements that mirror the passage of time on this distant world.


What Makes Pluto So Unique?

One of the most remarkable aspects of Pluto is its icy “cocktail” of nitrogen, methane, and carbon monoxide—substances that don’t naturally exist in this state on Earth.

The extreme cold of Pluto, with temperatures averaging around -375°F (-225°C), creates an environment where these ices can form and persist.

But Pluto’s surface is far from static. The interactions between its thin atmosphere, rugged topography, and volatile ices create a dynamic system that’s still active today.

In fact, scientists believe that Pluto’s icy heart is one of the youngest regions on the planet, with its surface being renewed and reshaped over time.


Why Does Pluto’s Heart Matter?

Understanding Pluto’s heart isn’t just about appreciating its beauty—it’s about unraveling the mysteries of planetary science.

Tombaugh Regio offers clues about the processes that shape icy bodies across the solar system, including moons like Europa and Enceladus.

Moreover, the discovery of Pluto’s dynamic glacier system highlights the complexity of even the most distant worlds.

It challenges assumptions about what’s possible in planetary environments and underscores the importance of continued exploration.


A Beating Heart, Frozen in Time

The more we learn about Pluto, the more we realize how extraordinary this tiny world truly is.

Its heart isn’t just a geological feature—it’s a testament to the forces that shape planets and moons across the cosmos.

Thanks to the groundbreaking work of the New Horizons mission and the researchers who continue to analyze its data, we now have a clearer picture of how this icy heart came to be.

And in doing so, we’ve uncovered a story of resilience, beauty, and dynamic change—one that reminds us just how much there is to discover, even at the edge of our solar system.

So, the next time you look at an image of Pluto, remember: beneath that frozen heart lies a world in motion, beating slowly but steadily against the vast backdrop of space.

Pluto, you’ll always have our hearts.

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