Subject |
has weather resistance |
has olivine shock metamorphism |
is independent of |
has shock pressure |
has acronym |
has olivine composition |
has image |
has weather |
has relative abundance |
has fragmentation probability |
has weathering stage |
has number of fragment |
has find date |
has comment |
has orthopyroxene shock metamorphism |
has plagioclase shock metamorphism |
has degree of shock metamorphism |
has mass |
has shock diagnostic mineral |
has name |
be shock |
has fall location |
is an instance of |
has pyroxene composition |
has shock stage |
has composition |
has value |
has fall coordinate |
has ablative mass loss |
classified by |
Acfer 041 | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Acfer 315 | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Beeler | which depends on its composition | | | | | |
 | can be severe due to long exposure time to environmental corrosion agents | | during meteor phase which depends on composition | | | 1924 | | | | | 8.64 kg | | Beeler | | Ness County, Kansas | meteorite find | | | often minerals not found on Earth | lower because the fall was not witnessed | 38° 32' N., 100° 13' W. | directly proportional to initial velocity | |
Bison | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Crocker's Well | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
DaG 599 | which depends on its composition | planar fractures, undulatory extinction, irregular fractures | the nature and degree of thermal metamorphism or aqueous alteration | 15 to 20 GPa | DaG | Fa% 32 |
 | can be severe due to long exposure time to environmental corrosion agents | | during meteor phase which depends on composition | W3 | 2 | 1998 | very recrystalized | clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures | undulatory extinction | weakly shocked | 0.781 kg | orthopyroxene for enstatite chondrite | based on the locale, region, or nearby town in which the fall occurred | before, during or after other types of metamorphism | Dar al Gani plateau, Libyan Sahara Desert | LL6 chondrite | Fs% 13.3 | S3 | bronzite, olivine and minor oligoclase | lower because the fall was not witnessed | 26° 54.96' N. 16° 40.39' E. | directly proportional to initial velocity | A. Sexton, I.A. Franchi, Open University, UK. Meteoritical Bulletin No 83 |
Dhofar 011 | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
EET 92012 | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Ensisheim | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
HaH 046 | which depends on its composition | | | | HaH | | | can be severe due to long exposure time to environmental corrosion agents | | during meteor phase which depends on composition | | | when the meteorite was found | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | Hammadah al Hamra | Hammadah al Hamra meteorite | | | bronzite, olivine and minor oligoclase | lower because the fall was not witnessed | in degrees, minutes and seconds of lattitude and longitude | directly proportional to initial velocity | |
Lake Labyrinth | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Naryilco | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Sahara 97012 | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Sahara 97037 | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |
Y-82067 | low | | | | | | | | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | LL6 chondrite | | | bronzite, olivine and minor oligoclase | | in degrees, minutes and seconds of lattitude and longitude | high because it is more friable than iron meteorite | |