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Showing posts with the label Scattered Disc

The Ultra-Reflective Frozen Methane Plains of Dwarf Planet Eris

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In the dark, outermost reaches of the Solar System, far beyond the orbit of Neptune and the classical Kuiper Belt, lies a massive icy world that fundamentally reshaped our understanding of planetary science. Discovered in 2005, 136199 Eris is the most massive dwarf planet in our solar system, boasting a mass approximately 27 percent greater than that of Pluto despite being slightly smaller in physical diameter. Floating in the scattered disc —a sparsely populated, dynamically unstable region of icy debris—Eris exists as a frozen relic from the earliest epochs of planetary accretion, preserved in an ultra-deep freeze that has remained virtually undisturbed for over four billion years. Unlike the reddish, organic-rich surfaces of other trans-Neptunian objects , Eris shines with an extraordinary, almost blinding brilliance. Its surface possesses a geometric albedo of approximately 0.96, reflecting nearly all the sunlight that strikes it. This hyper-reflective nature suggests a highl...

The Reflective Methane Glaciers and Dense Interior of Dwarf Planet Eris

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Orbiting within the scattered disc of the outer Solar System, the dwarf planet 136199 Eris represents one of the most massive and structurally dense planetary bodies beyond the orbit of Neptune. Discovered in January 2005 at the Palomar Observatory , Eris occupies an extreme, highly inclined trajectory that carries it from a perihelion of 37.9 astronomical units (AU) out to an aphelion of approximately 97.5 AU. With an orbital inclination of roughly 44 degrees relative to the ecliptic plane, the body traverses regions of space far removed from the primary planetary disk, taking nearly 559 Earth years to complete a single revolution around the Sun. The sheer mass and physical scale of Eris played a central role in formalizing the modern astronomical definition of a dwarf planet , establishing a distinct class of massive trans-Neptunian objects governed by unique thermodynamic and geological regimes. ...

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