Subject |
has iron metal and iron sulfide |
has oxidized iron content |
has weather resistance |
has metal abundance |
has refractory inclusion abundance |
is an instance of |
has total iron content |
has distinguishing feature |
has metal iron content |
has fragmentation probability |
has fall location |
has name |
has chondrule abundance |
has relative abundance |
has abundance |
has prototype |
has degree of aqueous alteration |
has oxidation state |
has total mass of find |
has volatile content |
has matrix abundance |
has composition |
is a kind of |
has number of find |
has ablative mass loss |
has synonym |
has chondrule mean diameter |
CH chondrite | | | low | 20 % by volume | 0.1 % by volume | | | elemental carbon | | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | about 70 % by volume | 8 % of meteorite falls | rare relative to other chondrite types | ALH 85085 meteorite | none | | 2577 kg | low | 5 % by volume | often minerals not found on Earth | type 3 chondrite | 36 | high because it is more friable than iron meteorite | | 0.02 millimeters |
CK3 chondrite | | | low | 0.01 % by volume | 4 % by volume | | | elemental carbon | | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | 15 % by volume | 8 % of meteorite falls | rare relative to other chondrite types | ??? meteorite | none | | 2577 kg | | 75 % by volume | often minerals not found on Earth | type 3 chondrite | 36 | high because it is more friable than iron meteorite | | 0.7 millimeters |
CO chondrite | | | low | 1 to 5 % by volume | 13 % by volume | | | elemental carbon | | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | 48 % by volume | 8 % of meteorite falls | rare relative to other chondrite types | Ornans meteorite | none | | 2577 kg | | 34 % by volume | often minerals not found on Earth | type 3 chondrite | 36 | high because it is more friable than iron meteorite | | 0.15 millimeters |
CV chondrite | | | low | 0 to 5 % by volume | 10 % by volume | | | elemental carbon | | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | 45 % by volume | 8 % of meteorite falls | rare relative to other chondrite types | Vigarano meteorite | weak | | 2577 kg | | 40 % by volume | iron-rich olivine, calcium aluminum inclusions | type 3 chondrite | 36 | high because it is more friable than iron meteorite | | 1.0 millimeters |
E3 chondrite | | zero | which depends on its composition | in volume % | in volume % | | | | | during meteor phase which depends on composition | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | in volume % | | | | none | highly reduced with very little FeO | 1 kg | | in volume % | often minerals not found on Earth | type 3 chondrite | 1 | directly proportional to initial velocity | E chondrite | millimeters |
H3 chondrite | 75 % of total iron | | low | 10 % by volume | 0.1 to 1 % by volume | | high | | 12 to 21 % | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | 60 to 80 % by volume | 85.7 % of meteorite falls | most common chondrite observed from falls | | none | | 349 kg | | 10 to 15 % by volume | often minerals not found on Earth | type 3 chondrite | 9 | high because it is more friable than iron meteorite | bronzite chondrite | 0.3 millimeters |
K chondrite | | | low | 0 % by volume (included in matrix abundance) | less than 0.1 % by volume | | | | | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | 27 % by volume | 85.7 % of meteorite falls | | Kakangari meteorite | none | | 20461 kg | | 73 % by volume (including metal) | often minerals not found on Earth | type 3 chondrite | 1030 | high because it is more friable than iron meteorite | | 0.6 millimeters |
L3 chondrite | 50 % of total iron | | low | 5 % by volume | 0.1 to 1 % by volume | | low | | 5 to 10 % | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | 60 to 80 % by volume | 85.7 % of meteorite falls | most common chondrite observed from falls | | none | | 131 kg | | 10 to 15 % by volume | often minerals not found on Earth | type 3 chondrite | 10 | high because it is more friable than iron meteorite | hypersthene chondrite | 0.7 millimeters |
LL3 chondrite | 20 % of total iron | | low | 2 % by volume | 0.1 to 1 % by volume | | low | | about 2 % | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | 60 to 80 % by volume | 85.7 % of meteorite falls | most common chondrite observed from falls | | none | | 90 kg | | 10 to 15 % by volume | bronzite, olivine and minor oligoclase | type 3 chondrite | 5 | high because it is more friable than iron meteorite | amphoterite | 0.9 millimeters |
Rumuruti | | | low | 0.1 % by volume | 0 % by volume | type 3 chondrite | | | | high because it is more friable than iron meteorite | Sahara | Rumuruti | greater than 40 % by volume | 85.7 % of meteorite falls | | Rumuruti meteorite | none | highly oxidized | 20461 kg | | 36 % by volume | enriched in 17O isotope | | 1030 | high because it is more friable than iron meteorite | rumurutiite | 0.4 millimeters |