Earth Impact Effects Program

Robert Marcus, H. Jay Melosh, and Gareth Collins

Please note: the results below are estimates based on current (limited) understanding of the impact process and come with large uncertainties; they should be used with caution, particularly in the case of peculiar input parameters. All values are given to three significant figures but this does not reflect the precision of the estimate. For more information about the uncertainty associated with our calculations and a full discussion of this program, please refer to this article

Your Inputs:

Distance from Impact: 100.00 km ( = 62.10 miles )
Projectile diameter: 5.00 meters ( = 16.40 feet )
Projectile Density: 8000 kg/m3
Impact Velocity: 36000.00 km per second ( = 22400.00 miles per second ) (Your chosen velocity is higher than the maximum for an object orbiting the sun)
Impact Angle: 90 degrees
Target Density: 1000 kg/m3
Target Type: Ice


Energy before atmospheric entry: 3.39 x 1020 Joules = 8.11 x 104 MegaTons TNT
The average interval between impacts of this size somewhere on Earth during the last 4 billion years is 6.6 x 105years

Major Global Changes:

The Earth is not strongly disturbed by the impact and loses negligible mass.
The impact does not make a noticeable change in the tilt of Earth's axis (< 5 hundreths of a degree).
The impact does not shift the Earth's orbit noticeably.

Atmospheric Entry:

The projectile begins to breakup at an altitude of 137000 meters = 448000 ft
The projectile bursts into a cloud of fragments at an altitude of 31800 meters = 104000 ft
The residual velocity of the projectile fragments after the burst is 31300 km/s = 19400 miles/s
The energy of the airburst is 8.33 x 1019 Joules = 1.99 x 104 MegaTons.
Large fragments strike the surface and may create a crater strewn field. A more careful treatment of atmospheric entry is required to accurately estimate the size-frequency distribution of meteoroid fragments and predict the number and size of craters formed.

Air Blast:

What does this mean?

The air blast will arrive approximately 5.3 minutes after impact.
Peak Overpressure: 73900 Pa = 0.739 bars = 10.5 psi
Max wind velocity: 136 m/s = 305 mph
Sound Intensity: 97 dB (May cause ear pain)
Damage Description:

Tell me more...

Click here for a pdf document that details the observations, assumptions, and equations upon which this program is based. It describes our approach to quantifying the important impact processes that might affect the people, buildings, and landscape in the vicinity of an impact event and discusses the uncertainty in our predictions. The processes included are: atmospheric entry, impact crater formation, fireball expansion and thermal radiation, ejecta deposition, seismic shaking, and the propagation of the atmospheric blast wave.

Recent improvements in the airblast calculation are described here.

Earth Impact Effects Program Copyright 2004, Robert Marcus, H.J. Melosh, and G.S. Collins
These results come with ABSOLUTELY NO WARRANTY