The Steinheim crater is the smaller partner to the Ries crater. It is located in Alb, Steinheim. It is thought that the two craters were formed 15million years ago. However, there are two theories to how the Steinheim crater formed; either a double meteorite or a 150m fragmentation of one larger impactor as it collided with the earth to form the 24km Reis crater. In either theory, the impactor travelled at around 7.2x104 km/hour impacted the Earth. This meteorite collided with the earth with a similar amount of energy as 100,000 Hiroshima bombs. It is thought that the meteorite hit the earth’s crust at an angle between 30 and 50 degrees which, on impact, caused the pressure to increase by a million bar. As the pressure rises, the temperature also increases to 30,000 degrees causing rocks to disintegrate.