In this episode of Stuff You Should Know, the hosts explore the science behind asteroids and the very real threat they pose to Earth. They explain what asteroids are, how scientists track the 25,000 near-Earth asteroids, and what makes certain ones "potentially hazardous" or even "extinction-class" threats capable of ending most life on the planet.
The episode examines the Chicxulub impact that wiped out the dinosaurs 66 million years ago and details the catastrophic environmental consequences that followed. Looking to the future, the hosts discuss various planetary defense strategies scientists have developed, from kinetic impactors to gravitational tractors, and highlight successful missions like DART that have proven our ability to deflect asteroids. The conversation provides both historical context and practical information about how humanity is preparing to protect Earth from future asteroid impacts.

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Asteroids are ancient rocky bodies from the early solar system, either remnants that never formed into planets or fragments from early planetary collisions. They range vastly in size—from 30 to 35 feet in radius to several hundred kilometers across. Scientists have tracked over 1.8 million known asteroids, with many residing in the asteroid belt between Mars and Jupiter, where Jupiter's immense gravity prevents them from coalescing into a planet.
Modern scientists discover about 1,100 new asteroids annually, focusing particularly on the 25,000 near-Earth asteroids whose orbits bring them close to our planet. Among these, "potentially hazardous asteroids" (PHAs) are those larger than 460 feet and approaching within 4.6 million miles of Earth. Even more concerning are "extinction-class" asteroids greater than 6.2 miles in diameter, which could eradicate virtually all life on Earth. Currently, four known extinction-class asteroids are considered potentially hazardous, though the immediate risk is low.
NASA maintains a close approaches list to track asteroid paths. Notable examples include a 2022 asteroid that came within 1.2 million miles of Earth—the closest in 200 years—and asteroid Apophis, which will pass within 20,000 miles in April 2029, closer than some satellites. Because asteroids reflect far less visible light than planets, NASA employs infrared technology like the NEO-WISE mission to detect and monitor these objects.
Sixty-six million years ago, an asteroid impact caused a mass extinction that eliminated about 75% of all species, including the dinosaurs. The Chicxulub crater, discovered in 1978 near the Yucatan Peninsula, measures between 112 and 124 miles in diameter. The asteroid itself was about 8.7 miles wide and produced an explosion estimated at 100 million megatons—20 to 30 times the combined firepower of every nuclear weapon on Earth.
The impact triggered catastrophic environmental effects: a 15-mile-high tidal wave, global heat pulse that incinerated surface life, sulfuric acid rain that devastated oceans, and a prolonged "nuclear winter" that blocked sunlight and crippled photosynthesis. Scientists estimate it took Earth about 30,000 years to recover. This extinction event cleared ecological niches, allowing mammals to rapidly diversify and eventually setting the stage for human evolution.
Space agencies have developed various approaches to deflect potentially hazardous asteroids, though not all popular ideas are practical. NASA has determined that detonating nuclear weapons on or beneath asteroid surfaces would likely fragment large objects into multiple dangerous pieces. Instead, scientists endorse a "standoff explosion" technique, where nuclear devices detonated near the asteroid would vaporize surface material, creating a jet-like exhaust to push it off course.
Kinetic impactor technology involves slamming a spacecraft into an asteroid to alter its trajectory. The European Space Agency's Don Quixote mission proposes sending two spacecraft: one to gather data on the asteroid's structure and composition, and another to use that information for an optimal impact.
Non-explosive methods include solar lasers that heat the asteroid's surface to create tiny thrusts, and gravitational tractors that use a spacecraft's gravitational pull to subtly alter the asteroid's path. Calculations indicate a 20-ton probe could move a 60-million-ton asteroid in under a year. These safer, controllable approaches work at the micron scale over many years, requiring early detection and decades-long lead time.
The NEAR spacecraft, launched in 1996, became the first to orbit a small solar system body when it reached asteroid Eros in February 2000. Orbiting just four miles above Eros's surface for about a year, NEAR collected extensive data on gravitational field, chemical composition, and surface characteristics, demonstrating the feasibility of detailed asteroid reconnaissance.
The DART mission in 2022 provided concrete proof of kinetic deflection capabilities. The spacecraft collided with the asteroid Dimorphos at 4.1 miles per second, shifting its path by 11.7 microns per second. While seemingly insignificant, this change accumulates to a 360-meter shift over a year, confirming that with sufficient advance notice—such as decades of warning time—even minor trajectory adjustments can prevent Earth collisions.
1-Page Summary
Asteroids are ancient rocky bodies, either remnants from the early universe that never formed into planets or smashed fragments of early planetary material. These objects range vastly in size—from 30 to 35 feet in radius to several hundred kilometers across. Astronomers have tracked over 1.8 million known asteroids to date.
The asteroid belt between Mars and Jupiter is home to many of these objects. Among them, Ceres stands out as the largest, measuring about 620 miles (1,000 kilometers) across and comprising one third of the asteroid belt's total mass. Jupiter’s immense gravity exerts significant influence on the belt, fracturing many larger bodies into smaller pieces instead of allowing them to form into a planet.
In size, asteroids can be as massive as two and a half times the height of the Empire State Building. Ancient asteroids are either planetary building blocks that never combined into planets or debris from earlier planetary collisions, constantly shaped by Jupiter’s gravitational power.
Asteroid discovery began in earnest during the late 18th and early 19th centuries. Johann Bode’s mathematical observations in the 1770s suggested a missing planet between Mars and Jupiter, spurring astronomers like Giuseppe Piazza to search that region. In 1801, Piazza discovered Ceres, inaugurating a tradition of asteroid detection that persists to this day.
Modern scientists annually discover about 1,100 new asteroids, with a keen focus on the 25,000 asteroids classified as near-Earth asteroids—those whose orbits bring them close to our planet. Not all of these are regarded as equally hazardous. Among them, “potentially hazardous asteroids” (PHAs) are those larger than 460 feet (140 meters) and whose orbits bring them within 4.6 million miles of Earth. Subclasses abound, but PHAs warrant special attention due to their size and proximity.
Even more concerning are “extinction-class” asteroids, defined as those greater than 6.2 miles (10 kilometers) in diameter. Impact from one of these could eradicate virtually all life forms on Earth. Currently, four known extinction-class asteroids are considered potentially hazardous, though the risk of an impact in our era is low.
NASA maintains a close approaches list, tracking the predicted paths of known asteroids relative to Earth. While most entries are airplan ...
Asteroid Discovery, Classification, and Monitoring Systems
Sixty-six million years ago, an asteroid impact led to a global mass extinction that wiped out about 75% of all species on Earth, including the dinosaurs. In 1978, geologists discovered a massive, arc-shaped formation underwater near the Yucatan Peninsula during a survey for an oil company. This formation was soon confirmed as the Chicxulub impact crater, which measures between 112 and 124 miles in diameter.
Asteroid-related iridium, a metal far more prevalent in asteroids than in Earth's crust, was found in unusually high levels in rocks all over the planet from the same period. This iridium layer, marking the end of the Cretaceous 66 million years ago, provided strong evidence that an asteroid impact triggered the mass extinction. The Chicxulub impactor itself was about 8.7 miles wide and produced an explosion estimated at 100 million megatons—20 to 30 times the combined firepower of every nuclear weapon on Earth detonating at once.
The sheer force of the impact caused a sequence of catastrophic environmental effects. Within five seconds, a tidal wave soared 15 miles high, generated by the asteroid smashing into the shallow waters now part of the Gulf of Mexico. The strike vaporized vast amounts of seawater and rock, launching debris into the atmosphere.
This ejected material re-entered the atmosphere, creating immense friction that triggered a global "heat pulse." The resulting thermal radiation incinerated most surface-dwelling organisms almost instantly. After the immediate devastation, sulfur dioxide released into the air returned as sulfuric acid rain. This rapid surge in acidity devastated the oceans, multiplying acidity levels by a hundredfold in a very short time—annihilating plankton and other acid-sensitive marine life. Since plankton form the founda ...
Historical Asteroid Impacts and Mass Extinction Events
Planetary defense against asteroids involves various approaches, but not all popular ideas—like nuclear explosions—are practical or effective. Over the years, space agencies and scientists have studied and developed a range of strategies to deflect potentially hazardous asteroids away from Earth.
The idea of blowing up an asteroid with a nuclear bomb is a common one, popularized by movies. The logic seems straightforward for smaller asteroids: a nuclear blast could shatter them into harmless fragments. However, the large asteroids that actually threaten Earth would not be neutralized this way. NASA has studied the concept and concluded that if a warhead were detonated on or just under the surface of a large asteroid, it would likely fracture the object into several big chunks—creating multiple dangerous pieces that could still collide with Earth. Official NASA reports, such as one from 2007, confirm that this direct nuclear approach is not a sensible or reliable plan.
Scientists instead endorse a different nuclear technique called a standoff explosion. In this approach, one or more nuclear devices would be detonated near, but not on, the surface of the asteroid. The intense burst of radiation would sear one side, vaporizing material and producing a jet-like exhaust that could push the asteroid away from its collision course with Earth. This method is seen as the only credible nuclear-based deflection technique by the scientific community.
Kinetic impactor technology—sometimes called KID, or "kid cat"—involves slamming a spacecraft into an asteroid to alter its path, much like using a cue ball to knock an eight-ball on a new trajectory. For this to work, scientists need to calculate the mass, composition, and speed of both the asteroid and the spacecraft to maximize deflection. It's a challenging feat, sometimes likened to hitting a speeding cannonball with a bullet.
The European Space Agency’s Don Quixote mission represents a more refined kinetic approach. It envisions sending two spacecraft: one would land on the asteroid to collect critical data about its structure, mass, and composition; the other would then use that information to target the impact for optimal effect. This minimizes guesswork and increases the likelihood of a successful deflection.
Another category of asteroid mitigation uses non-explosive means. One idea involves using lasers—either actual lasers or concentrated sunlight via mirrors—to heat the asteroid’s surface. Inspired by the legendary Archimedes death ray, this method would cause material to vaporize and eject from the asteroid, acting like a series of tiny thrusts that gradually nudge the object off course. These so-called solar lasers requi ...
Asteroid Deflection and Planetary Defense Methods
The NEAR (Near-Earth Asteroid Rendezvous) project marked a significant milestone in asteroid exploration and planetary defense. Launched in February 1996, the NEAR spacecraft's initial notable achievement was a flyby of the asteroid Matilda in June 1997, passing within 753 miles (a little over 1200 kilometers) of its surface. After the Matilda encounter, the spacecraft proceeded to a historic mission: entering orbit around asteroid 433 Eros in February 2000.
Eros, a potato-shaped asteroid approximately 21 miles long and 8 miles wide, became the first small solar system body orbited by a human-made object. The NEAR spacecraft maintained an orbit just four miles above Eros's surface for about a year, during which it accomplished extensive data collection missions. NEAR measured the asteroid's gravitational field, captured high-resolution images, conducted chemical composition analysis, and produced detailed surface maps. Its mission culminated with a landing on Eros, from which it continued to transmit valuable information until extreme cold rendered communication impossible.
The NEAR mission was significant not just for its discoveries but for its demonstration of the feasibility of automated spacecraft reconnaissance of asteroids. It proved that detailed data acquisition on orbital dynamics, composition, and structure is achievable, validating the concept that such thorough reconnaissance is essential prior to any attempt at a deflection mission. By providing a wealth of information that would be critical in targeting future deflection efforts, NEAR established itself as a key precursor for planetary defense strategies.
The next major step in demonstrating asteroid deflection technology came with the DART (Double Asteroid Redirection Test) mission. Launched five years prior to its test, the robotic DART spacecraft aimed to directly test humanity’s ability to alter an asteroid’s path. Its target was Dimorphos, a small moonlet orbiting a larger asteroid. DART was programmed to collide with Dimorphos at a velocity of 4.1 miles per second, a test to determine whether its kinetic impact could modify the asteroid’s orbital ...
Demonstration of Deflection Technology
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