Temple Bar
Location:
- USA
- Arizona
Found: 1998
Group:
- Stone
Type:
- Carbonaceous chondrite
Class:
- Renazzo CR2
Total known weight: 126
A 126 g stone was found by a prospector near the road, 7 miles south of Temple Bar. Classification and mineralogy (M. Killgore, SWML): chondrules range from 0.4 to 4 mm, and comprise ~50 vol%; metal occurs mostly inside chondrules; brownish-yellow phyllosilicates present; olivine, Fa2.3, range Fa0.7–4.3, n = 10; probably little shocked; weathering grade, W5.
Slightly weathered stone which is packed full of chondrules. A CR2 is among the most primitive chondrites formed in the early solar system.



