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The formation of the Solar System began approximately 4.6 billion years ago when a giant molecular cloud collapsed under gravity, forming a rotating disk of gas and dust around the young Sun. Over millions of years, dust particles collided and clumped together, eventually forming planetesimals, protoplanets, and finally the eight planets, moons, asteroids, and comets we know today. More Less
1990
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These discs extend to several hundred AU—the Hubble Space Telescope has observed protoplanetary discs of up to 1000 AU in diameter in star-forming regions such as the Orion Nebula—and are rather cool, reaching a surface temperature of only about 1,000 K (730 °C; 1,340 °F) at their hottest. Such observations provide modern evidence for the nebular hypothesis.
Image source: Protoplanetary disk
Jun 6, 2011
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A study by Southwest Research Institute, San Antonio, Texas, published June 6, 2011 (called the Grand tack hypothesis), proposes that Jupiter had migrated inward to 1.5 AU. This inward-and-back migration would have sculpted the inner Solar System, truncating Mars's growth and shaping the asteroid belt.
Image source: Grand tack hypothesis
50000 BC
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That impacts continue to happen is evidenced by the impact that created Meteor Crater in Arizona. Formed roughly 50,000 years ago by an iron meteorite, this remarkably well-preserved crater became a key site for studying impact processes on Earth and other planets.
Image source: Meteor Crater
Jun 30, 1908
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That impacts continue to happen is evidenced by the Tunguska event, an enormous air burst over Siberia in 1908 that flattened roughly 2,000 square kilometers of forest. It demonstrated the destructive potential of small bodies striking Earth and remains one of the largest impact events in recorded history.
Image source: Tunguska event
Jul 1994
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That impacts continue to happen is evidenced by the collision of Comet Shoemaker–Levy 9 with Jupiter in 1994. The spectacular string of impacts provided astronomers a rare live view of planetary bombardment, confirming that collisional processes still shape the Solar System today.
Image source: Comet Shoemaker–Levy 9
2006
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A population of main-belt comets discovered in 2006 has also been suggested as a possible source for Earth's water. These icy asteroids blur the line between comets and asteroids and offer another candidate reservoir for the volatile materials delivered to the early Earth.
Image source: Asteroid belt
Jul 19, 2009
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That impacts continue to happen is evidenced by the 2009 Jupiter impact event, when an object—likely an asteroid or comet—struck Jupiter's atmosphere, leaving a dark scar visible to amateur and professional astronomers alike. The event underscored the ongoing role of collisions in the Solar System.
Image source: 2009 Jupiter impact event
Feb 15, 2013
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That impacts continue to happen is evidenced by the Chelyabinsk meteor, which exploded over Russia in 2013. The airburst shattered windows and injured around 1,500 people, highlighting that even modest near-Earth objects pose real hazards in the modern era.
Image source: Chelyabinsk meteor
1543
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This process began with Nicolaus Copernicus in 1543, whose heliocentric model placed the Sun at the center of the Solar System. His work continued over the course of the Scientific Revolution, fundamentally changing humanity's understanding of the cosmos and laying the groundwork for later theories about how the Solar System formed.
Image source: Formation and evolution of the Solar System
1704
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The first recorded use of the term "Solar System" dates from 1704, marking a milestone in how astronomers described the Sun and its orbiting bodies as a unified system. This terminology reflected the growing acceptance of the heliocentric view established during the Scientific Revolution.
Image source: Solar System
1700 - 1799
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This model, known as the nebular hypothesis, was first developed in the 18th century by Emanuel Swedenborg, Immanuel Kant, and Pierre-Simon Laplace. It proposed that the Solar System formed from a rotating cloud of gas and dust that collapsed and flattened into a disc, from which the planets coalesced.
Image source: Nebular hypothesis
1796
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The current standard theory for Solar System formation, the nebular hypothesis, has fallen into and out of favour since its formulation by Emanuel Swedenborg, Immanuel Kant, and Pierre-Simon Laplace in the 18th century. Laplace's mathematical treatment gave the idea its most influential early expression.
Image source: Pierre-Simon Laplace
1935
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In 1935, Eddington went further and suggested that other elements also might form within stars. This insight helped explain the origin of the heavy elements found in the Solar System, which were forged in earlier generations of stars before the Sun's birth cloud collapsed.
Image source: Stellar nucleosynthesis
2008 - 2026
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While a 2008 study suggests that Earth will possibly but likely be slowly vaporized up as a result of tidal interactions with the Sun's weakly-bound outer envelope, a recent study in 2026 has suggested that the Earth is likely to survive the engulfment. The fate of our planet during the Sun's final stages remains an active area of research.
Image source: Future of Earth
2021
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This future development may be similar to the observed detection of MOA-2010-BLG-477L b, a Jupiter-sized exoplanet orbiting its host white dwarf star MOA-2010-BLG-477L. The discovery suggests that giant planets can survive their star's death, offering a preview of what may happen to Jupiter after the Sun becomes a white dwarf.
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