As the inhabitants of an ancient Middle Eastern city now called Tall el-Hammam went about their daily business one day about 3,600 years ago, they had no idea an unseen icy space rock was speeding toward them at about 38,000 mph (61,000 kph).
Flashing through the atmosphere, the rock exploded in a massive fireball about 2.5 miles (4 kilometers) above the ground. The blast was around 1,000 times more powerful than the Hiroshima atomic bomb. The shocked city dwellers who stared at it were blinded instantly. Air temperatures rapidly rose above 3,600 degrees Fahrenheit (2,000 degrees Celsius). Clothing and wood immediately burst into flames. Swords, spears, mudbricks and pottery began to melt. Almost immediately, the entire city was on fire.
Some seconds later, a massive shockwave smashed into the city. Moving at about 740 mph (1,200 kph), it was more powerful than the worst tornado ever recorded. The deadly winds ripped through the city, demolishing every building. They sheared off the top 40 feet (12 m) of the 4-story palace and blew the jumbled debris into the next valley. None of the 8,000 people or any animals within the city survived — their bodies were torn apart and their bones blasted into small fragments.
About a minute later, 14 miles (22 km) to the west of Tall el-Hammam, winds from the blast hit the biblical city of Jericho. Jericho's walls came tumbling down and the city burned to the ground.
No one was exactly sure what had happened, but that layer wasn't caused by a volcano, earthquake or warfare. None of them are capable of melting metal, mudbricks and pottery.
To figure out what could, our group used the Online Impact Calculator to model scenarios that fit the evidence. Built by impact experts, this calculator allows researchers to estimate the many details of a cosmic impact event, based on known impact events and nuclear detonations.
It appears that the culprit at Tall el-Hammam was a small asteroid similar to the one that knocked down 80 million trees in Tunguska, Russia in 1908. It would have been a much smaller version of the giant miles-wide rock that pushed the dinosaurs into extinction 65 million ago.
We had a likely culprit. Now we needed proof of what happened that day at Tall el-Hammam.
Finding 'diamonds' in the dirt
Our research revealed a remarkably broad array of evidence.
At the site, there are finely fractured sand grains called shocked quartz that only form at 725,000 pounds per square inch of pressure (5 gigapascals) — imagine six 68-ton Abrams military tanks stacked on your thumb.
The destruction layer also contains tiny diamonoids that, as the name indicates, are as hard as diamonds. Each one is smaller than a flu virus. It appears that wood and plants in the area were instantly turned into this diamond-like material by the fireball's high pressures and temperatures.
Experiments with laboratory furnaces showed that the bubbled pottery and mudbricks at Tall el-Hammam liquefied at temperatures above 2,700 F (1,500 C). That's hot enough to melt an automobile within minutes.
The destruction layer also contains tiny balls of melted material smaller than airborne dust particles. Called spherules, they are made of vaporized iron and sand that melted at about 2,900 F (1,590 C).
In addition, the surfaces of the pottery and meltglass are speckled with tiny melted metallic grains, including iridium with a melting point of 4,435 F (2,466 C), platinum that melts at 3,215 F (1,768 C) and zirconium silicate at 2,800 F (1,540 C).
Together, all this evidence shows that temperatures in the city rose higher than those of volcanoes, warfare and normal city fires. The only natural process left is a cosmic impact.
One remaining puzzle is why the city and over 100 other area settlements were abandoned for several centuries after this devastation. It may be that high levels of salt deposited during the impact event made it impossible to grow crops. We're not certain yet, but we think the explosion may have vaporized or splashed toxic levels of Dead Sea salt water across the valley. Without crops, no one could live in the valley for up to 600 years, until the minimal rainfall in this desert-like climate washed the salt out of the fields.
Was there a surviving eyewitness to the blast?
It's possible that an oral description of the city's destruction may have been handed down for generations until it was recorded as the story of Biblical Sodom. The Bible describes the devastation of an urban center near the Dead Sea — stones and fire fell from the sky, more than one city was destroyed, thick smoke rose from the fires and city inhabitants were killed.
Could this be an ancient eyewitness account? If so, the destruction of Tall el-Hammam may be the second-oldest destruction of a human settlement by a cosmic impact event, after the village of Abu Hureyra in Syria about 12,800 years ago. Importantly, it may the first written record of such a catastrophic event.
The scary thing is, it almost certainly won't be the last time a human city meets this fate.
Tunguska-sized airbursts, such as the one that occurred at Tall el-Hammam, can devastate entire cities and regions, and they pose a severe modern-day hazard. As of September 2021, there are more than 26,000 known near-Earth asteroids and a hundred short-period near-Earth comets. One will inevitably crash into the Earth. Millions more remain undetected, and some may be headed toward the Earth now.
Unless orbiting or ground-based telescopes detect these rogue objects, the world may have no warning, just like the people of Tall el-Hammam.
This article was originally published at The Conversation. The publication contributed the article to Live Science's Expert Voices: Op-Ed & Insights.
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Christopher Moore joined the Savannah River Archaeological Research Program staff in 2008. Chris received a B.S. in Anthropology from Appalachian State University in 1997, an M.A. in Anthropology from East Carolina University in 2000, and a Ph.D. in Coastal Resources Management (with a focus in Geoscience) from East Carolina University in 2009. Chris's research interests include geoarchaeology, luminescence (OSL) dating, hunter-gatherer archaeology, Late Quaternary climate and human adaptation, GIS, and remote sensing.