Search results
Results from the WOW.Com Content Network
The Sutter's Mill meteorite is a carbonaceous chondrite which entered the Earth's atmosphere and broke up at about 07:51 Pacific Time on April 22, 2012, with fragments landing in the United States. [ 6 ] [ 7 ] The name comes from Sutter's Mill , a California Gold Rush site, near which some pieces were recovered.
The first samples of this meteorite fall were recovered close to Sutter's Mill, so it was named the Sutter's Mill meteorite. Several dozen fragments were eventually identified, with a total weight of about a kilogram. The meteorite is classified as a carbonaceous chondrite and contains some of the oldest known material in the Solar System. [17]
Download QR code; Print/export ... Pages in category "Meteorites found in the United States" ... Sutter's Mill meteorite; Sylacauga (meteorite) V.
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!
One of the fragments landed at Sutter's Mill, the very site where gold was first discovered in 1848 that led to the California Gold Rush. Jenniskens found one of three fragments of this CM chondrite on April 24, before rains hit the area. [22] The rapid recovery was made possible because Doppler weather radar detected the falling meteorites.
Get answers to your AOL Mail, login, Desktop Gold, AOL app, password and subscription questions. Find the support options to contact customer care by email, chat, or phone number.
These C chondrite groups are now each named with a standard two-letter CX designation, where C stands for "carbonaceous" (other types of chondrites do not begin with this letter) plus a capital letter in the spot X, which is very often the first letter of the name of a prominent meteorite—often the first to be discovered—in the group. Such ...
A search for meteorites in the Dhofar Desert in the Arabian Peninsula (Dhofar Governorate, Oman, November 2012) A meteorite find is a meteorite that was found by people, but whose fall was not observed. [1] They may have been on Earth's surface for as many as thousands of years and therefore could have been subject to varying amounts of weathering.