Historical Impacts
Asteroid impacts that are large enough to notice are rare. Until the 18th century European academics simply did not believe that stones could fall from the sky and skepticism persisted even into the 19th century. We now understand that impacts occur all the time in different sizes and places. Most impactors are very small, gravel or baseball sized rocks that burn up as meteors leaving only their burnt dust to float down to the surface and increase the mass of the Earth by tens of thousands of tons every year. Since most of the Earth's surface is ocean or far enough from human habitation most ground impacts are not observed. Weather and vegetation rapidly cover up smaller impact craters so that Greenland, Antartica, Australia and other deserts are exceptionally good places to find meteorites.Nevertheless, there are many recognized impacts that have occurred over the years and we list some of them below ranging from global catastrophes eons ago, to huge explosions that have occurred during human presence on the Earth, to large explosions that have occurred in the past century, to impacts that have occurred in the past few years.
Chicxulub
This K-T fossil boundary also shows a layer of the element iridium which is uncommon on the Earth's surface but much more common in asteroids, as well as burned material that suggests vast firestorms. The amount of burnt materioal in this layer is consistent with everything on the Earth's surface being burned! There are also tsunami (tidal wave) deposits around the Caribbean dating from that time.
Most people believe that the cause of this change was the impact of a large asteroid at Chicxulub, off of the coast of Yucatan, Mexico. There is the unmistakeable site of an ancient asteroid impact, a 180km (100 miles) circular crater filled with minerals that show the effects of high temperature and pressure, shock, and shattering. The gravity map on the right shows concentric rings due to the impact and the white dots label places where sinkholes are found, suggesting creation by subsidence of the crater wall.
Chesapeake Crater
A slightly smaller event about 35 million years ago created the Chesapeake Bay and inundated the East Coast as far inland as the Blue Ridge Mountains. The impact crater is 40km (25 miles) across, and the damage done to the geological layers affects the aquifers in the area to this day.
The Popigai Crater in Siberia was probably created by a 5-8km (5 miles) diameter impactor and may have happened at the same time as Chesapeake Bay. The shock and heating from the impact transformed graphite into diamonds throughout the impact area. The Wikipedia article also has a nice set of pointers to other topics on asteroid impact cratering on Earth.
Meteor Crater
The Meteor Crater in Arizona was created by the impact of an asteroid about 50,000 years ago. This iron asteroid is thought to have been about 25-50m (80-160 ft) in size while the crater is about 1.2km (0.8 mile) in diameter and 200m (650 ft) deep! The explosion was equivalent in energy to a few Mton of TNT, similar to the explosion in 1908 over Tunguska (see below). We think that such impacts occur every thousand years, and there may have been dozens of similar ones since the creation of the Meteor Crater. What makes the Barringer Meteor Crater exceptional is its preservation due to its desert location. Since the impact of this object 50,000 years ago it is likely that some other impact took place that was ten times bigger - but no evidence remains. The Barringer Meteor Crater today is a fascinating tourist attraction and well worth a visit.
Tunguska
Scientists at the Cosmic Materials Space Research have used eyewitness accounts to try to reproduce what the Tunguska explosion sounded like.
The discrepancy between the apparent magnitude of the Tunguska explosion, the lack of recovered material, and the fact that ground zero was apparently not incinerated is probably because the asteroid was completely consumed in the atmosphere, but still created a huge shock wave that punched down to the ground. Detailed simulations by Boslough and Crawford support this conclusion; their work is summarized in an article by the Planetary Society. The result is that an asteroid impact can produce a greater blast on the surface than a point explosion of equivalent energy, and an asteroid smaller than the threshold size of ~100m (330 ft) required for a fireball to reach the ground can still cause great damage.
Sikhote-Alin
Peru
Sudan
It's an amazing story because of the hard work and quick wit of Kowalski and the Catalina Sky Survey, the way the Minor Planet Center coordinated hundreds of observations by amateurs and professionals over the next 20 hours, and the astounding accuracy with which the folks at JPL were able to predict the eventual impact. Within a few hours they knew where it would land within 100km and when it would land within 20sec, and their eventual prediction was accurate to 1km and 1.5sec. A story in the New Scientist describes the expedition that recovered fragments of the meteorite.


![[Chicxulub Crater]](/media/ChicxulubCrater.jpg)
![[Chicxulub crater gravity map.]](/media/Chicxulub_crater_gravity_map.gif)
![[Chesapeake Crater.]](/media/Chesapeake_Crater_profile_view.png)
![[Meteor Crater]](/media/meteorcrater.jpg)
![[Tunguska's trees.]](/media/Tunguska_event_fallen_trees.jpg)
![[Tunguska blast area.]](/media/tunguska_extent.gif)
![[Stamp commemorating the 10th anniversary of the Sikhote-Alin meteorite shower.]](/media/Sikhote-Alin_stamp_1957.jpg)
![[Peru crater.]](/media/070921-meteor-peru_big.jpg)
![[Sudan.]](/media/2008tc3train7_elhassan.jpg)
![[Indonesia.]](/media/indonesia2009_trail.jpg)