This is the third witnessed
meteorite fall in modern California, following Red Canyon Lake on 11 August 2007 and San Juan Capistrano on 15 March 1973, while a few months after this event the
Novato meteorite fell on 17 October 2012. A consortium of over 50 scientists investigated the circumstances of the impact and the properties of the meteorites. The event was recorded by two
infrasound monitoring stations of the
Comprehensive Nuclear-Test-Ban Treaty Organization’s International Monitoring System. The preliminary analyses are indicative of an energy yield of approximately four
kilotons of TNT equivalent. Hiroshima's "
Little Boy" had a yield of about 16 kt. The air burst had approximate coordinates of . Based on the infrasound signal and the brightness of the fireball in photographs and two video records, the incoming meteoroid was estimated to have been in diameter, between the size of a
dishwasher and a
minivan. Before entry in Earth's atmosphere, the meteoroid probably had an
absolute magnitude (H) of roughly 31. The meteoroid entered at a record speed of , the fastest fireball on record from which meteorites were later recovered. It broke apart at an altitude of , the highest breakup event on record resulting in meteorites on the ground. Before entry, the meteoroid moved on an eccentric orbit, stretching from just inside the orbit of Jupiter to the orbit of Mercury. The orbit had a shallow inclination and an orbital period suggesting that this meteoroid originated in the 3:1 mean motion resonance with Jupiter. The CM chondrite
Maribo moved on a similar orbit, but rotated by 120 degrees in the direction of the line of
apsides. The asteroid family that is the source region of CM chondrite-type meteorites is now thought to be located close to the 3:1 mean motion resonance, in low-inclined orbits, and may be the
Eulalia asteroid family. The meteorite type is similar to that of the 1969
Murchison meteorite in Australia. Unlike Murchison, Sutter's Mill shows clear brecciation: fragments of CM lithologies with different aqueous alteration and thermal processing histories are embedded in a fine grained CM matrix material. The Sutter's Mill meteorite originated from near the surface of its parent body. As a whole, Sutter's Mill is harder than Murchison. The pre-rain collected meteorite SM2 was found to contain the mineral
oldhamite (CaS), a mineral that reacts readily with water vapor. This
xenolithic material may have come from
enstatite chondrites impacting on the surface of the CM chondrite parent body in the past. The Sutter's Mill meteorite is used to test sample collection and analysis procedures for NASA's
OSIRIS-REx sample return mission. ==Examples==