Earth's Most Catastrophic Collisions: A History of Asteroid Impacts

EARTH'S MOST CATASTROPHIC COLLISIONS: A HISTORY OF ASTEROID IMPACTS

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Asteroid impacts have played a dramatic role in shaping the planet's geology, climate, and the evolution of life.

From ancient extinction events to modern-day cosmic close calls, here are some of the most remarkable and consequential asteroid impacts in Earth's history.

CHICXULUB CRATER

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The Chicxulub crater, located underneath the Yucatán Peninsula in Mexico, was formed around 66 million years ago when a massive asteroid, approximately 6 miles in diameter, struck the Earth.

The impact unleashed the energy equivalent of 100 teratons of TNT, triggering devastating megatsunamis over 100 meters tall, launching debris across the globe, and igniting wildfires that engulfed up to 70% of Earth's forests.

It is widely accepted that the cataclysmic climate disruptions and global ecological collapse resulting from the Chicxulub impact event were the primary cause of the Cretaceous-Paleogene extinction, wiping out around 75% of plant and animal species on Earth at the time, including all non-avian dinosaurs.

TUNGUSKA EVENT

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The Tunguska event was an enormous explosion that occurred on the morning of June 30, 1908 in a remote part of Siberia, flattening over 2,000 square kilometers of forest.

The blast, estimated to have released energy equivalent to 3-30 megatons of TNT, was most likely caused by an asteroid or comet fragment 50-100 meters wide entering the atmosphere at high speed and exploding 5-10 km above the surface.

Despite the massive scale of the explosion, due to the remote location there were no confirmed human casualties, although one eyewitness account suggests that up to three people may have died from the blast effects.


VREDEFORT CRATER

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The Vredefort impact structure in South Africa, formed 2.023 billion years ago, is the largest verified impact structure on Earth with an estimated original crater diameter of 170-300 km.

The impactor, thought to have been 20-25 km wide, struck with such force that it created a central uplift known as the Vredefort Dome and significantly distorted the surrounding geology, including the Witwatersrand Basin where the discovery of gold in 1886 within the overturned crater rim rocks proved immensely consequential.

Although the original crater has long since eroded away, the remaining complex, multi-ringed structure provides a stunning glimpse into the magnitude of this ancient cataclysm.

SUDBURY BASIN

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The Sudbury Basin, located in Ontario, Canada, is the third-largest known impact crater on Earth, with an original diameter estimated at 130 km.

Formed 1.849 billion years ago in the Paleoproterozoic era by the impact of a 10-15 km wide asteroid or chondritic comet, the Sudbury structure is also one of the oldest impact craters still preserved on the planet's surface.

The heat and pressure from this cataclysmic impact melted the underlying rock, creating deposits of nickel, copper, palladium, gold, and platinum group metals that have made the Sudbury Basin one of the world's most productive mining regions.

MANICOUAGAN RESERVOIR

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The Manicouagan Reservoir in Quebec, Canada is an annular lake that fills a large, well-preserved impact crater roughly 100 km in diameter, making it the sixth-largest confirmed impact structure on Earth by rim-to-rim diameter.

The 70 km diameter reservoir lake surrounds René-Levasseur Island, the central uplift of the crater, which rises up to 952 m in elevation at Mont Babel and together create a prominent "eye" visible from space.

Dating to approximately 214 million years ago in the Late Triassic epoch, the Manicouagan crater was formed by the impact of a 5 km wide asteroid in an event that predates the Triassic-Jurassic mass extinction by over 12 million years.

POPIGAI IMPACT STRUCTURE

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The Popigai impact structure in Siberia, Russia is tied with Manicouagan as the fourth largest confirmed impact crater on Earth, with a diameter of approximately 100 km.

Formed around 35.7 million years ago during the late Eocene epoch by the impact of a multi-kilometer wide asteroid, the Popigai event coincides with the Eocene-Oligocene extinction and may have been synchronous with the Chesapeake Bay and Toms Canyon impacts.

The immense shock pressures from the Popigai impact instantaneously converted graphite in the ground into a 13.6 km wide field of "impact diamonds", including unique nanocrystalline diamonds and large quantities of lonsdaleite, a hexagonal diamond polymorph that is significantly harder than regular cubic diamonds.

CHELYABINSK METEOR

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On February 15, 2013, a 20-meter diameter, 12,000-ton asteroid entered the atmosphere over Chelyabinsk, Russia, exploding at an altitude of 23.3 km with a force equivalent to 400-500 kilotons of TNT, or about 20-30 times the Hiroshima bomb.

The explosion generated a bright flash, a strong shockwave, and thousands of meteorite fragments.

While the meteor itself caused no direct injuries, the shockwave shattered windows and damaged buildings, injuring over 1,500 people in an elliptical region spanning a few tens of kilometers.

Dashcam and security camera videos of the intensely bright fireball and the delayed arrival of the explosive shockwave provided an unprecedented public visual record of a large meteor impact event.

BARRINGER CRATER

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Meteor Crater in Arizona, also known as Barringer Crater, is a 1.2 km wide, 170 m deep impact crater formed approximately 50,000 years ago by the impact of a 50 m diameter nickel-iron meteorite.

As one of the best-preserved impact craters on Earth, Meteor Crater played a crucial role in resolving the debate about the impact origin of craters in the early 20th century, with key evidence including the discovery of meteorite fragments, shatter cones, and shocked quartz.

The crater has served as an important research and educational site, notably being used in the 1960s and 70s to train NASA astronauts in preparation for the Apollo missions to the Moon

SYLACAUGA METEORITE

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On November 30, 1954, a grapefruit-sized fragment of the Sylacauga meteorite crashed through the roof of a house in Oak Grove, Alabama, bounced off a radio, and struck 34-year-old Ann Elizabeth Fowler Hodges, who was napping on a couch, leaving her badly bruised.

The meteorite fall, which was witnessed as a bright fireball visible from three states despite occurring in the early afternoon, is the only confirmed case in history of a person being directly struck by a space rock.

Two sizable fragments of the H4 chondrite were recovered—the 3.86 kg Hodges fragment and the 1.68 kg McKinney fragment found by a farmer the next day—and both ended up in museum collections after ownership disputes and public interest in the sensational event faded.

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