Subject |
has sediment mechanism |
has weather resistance |
has minerology |
has degree of shock metamorphism |
has age |
has shock stage |
is an instance of |
has distinguishing feature |
has fragmentation probability |
has fall location |
has metamorphism mechanism |
has likely origin |
has name |
has weather |
has weathering stage |
has acronym |
has relative abundance |
has prototype |
has value |
has total mass of find |
has peak temperature |
has parent body |
has fall coordinate |
has composition |
is a kind of |
has find date |
has mass |
has image |
has number of find |
has ablative mass loss |
has inclusion minerology |
has shock pressure |
has petrology |
Hammadah al Hamra meteorite | | which depends on its composition | | | | | | | during meteor phase which depends on composition | Hammadah al Hamra | | | based on the locale, region, or nearby town in which the fall occurred | can be severe due to long exposure time to environmental corrosion agents | | HaH | | | lower because the fall was not witnessed | 485755 kg | | | in degrees, minutes and seconds of lattitude and longitude | often minerals not found on Earth | Sahara meteorite | when the meteorite was found | | | 1691 | directly proportional to initial velocity | | | |
S1 shock stage meteorite | | which depends on its composition | | unshocked | | S1 | | | during meteor phase which depends on composition | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | shock metamorphism | | based on the locale, region, or nearby town in which the fall occurred | | | | | | | 485755 kg | | | in degrees, minutes and seconds of lattitude and longitude | often minerals not found on Earth | shocked meteorite | | | | 1691 | directly proportional to initial velocity | | less than 5 GPa | |
winonaite | agglomeration of particles, many of which record individual, diverse histories | low | olivine, orthopyroxene, clinopyroxene, metal with some troilite and some sodic plagioclase | | oldest and most primitive rock in solar system | | | no chondrules | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | ultrametamorphism, partial melting with some melt migration | based on the locale, region, or nearby town in which the fall occurred | | | | 7.1 % of meteorite falls | Winona meteorite | | 1606 kg | less than 950 degree Celsius during its entire history since solidification | asteroid smaller than 100 km in diameter | in degrees, minutes and seconds of lattitude and longitude | IAB-silica related | primitive achondrite | | | | 70 | high because it is more friable than iron meteorite | troilite, metal, daubreilite, schreibersite, graphite | | fine- to coarse-grained equigranular |
HaH 193 | agglomeration of particles, many of which record individual, diverse histories | which depends on its composition | olivine, orthopyroxene, clinopyroxene, metal with some troilite and some sodic plagioclase | unshocked | oldest and most primitive rock in solar system | S1 | S1 shock stage meteorite | no chondrules | during meteor phase which depends on composition | Hammadah al Hamra | shock metamorphism | ultrametamorphism, partial melting with some melt migration | HaH 193 | can be severe due to long exposure time to environmental corrosion agents | W3 | HaH | | Winona meteorite | lower because the fall was not witnessed | 485755 kg | less than 950 degree Celsius during its entire history since solidification | asteroid smaller than 100 km in diameter | 28° 39.28' N., 13° 27.52' E. | IAB-silica related | | October 1996 | 0.259 kg |
 | 1691 | directly proportional to initial velocity | troilite, metal, daubreilite, schreibersite, graphite | less than 5 GPa | fine- to coarse-grained equigranular |