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rock > metamorphic rock > altered chondrite > thermally altered chondrite > type 5 chondrite > L5 chondrite
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L5 chondrite comparison table
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 metamorphism mechanism has fall date has weathering stage have composition has fall description 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 value has fall coordinate has ablative mass loss classified by
Beenhamwhich depends on its composition     
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on compositionthermal metamorphismrecorded by eyewitness or inferred from dating methods    1937veined   44.4 kg Beenham township 25, range 30E., in Union County, New Mexicometeorite find  lower because the fall was not witnessed36° 13 N., 103° 39' W.directly proportional to initial velocity 
Cat Mountainwhich depends on its composition     
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on compositionthermal metamorphismrecorded by eyewitness or inferred from dating methods    1980/81Impact Melt Breccia     Cat Mountain Tucson, Arizonameteorite find  lower because the fall was not witnessed32° 8.9' N., 111° 6.7' W.directly proportional to initial velocity 
DaG 636which depends on its compositionplanar fractures, undulatory extinction, irregular fracturesthe nature and degree of thermal metamorphism or aqueous alteration15 to 20 GPaDaGFa% 25.3
can be severe due to long exposure time to environmental corrosion agents during meteor phase which depends on compositionthermal metamorphismrecorded by eyewitness or inferred from dating methodsW2  31998contains metal flakesclinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fracturesundulatory extinctionweakly shocked2.975 kgorthopyroxene for enstatite chondritebased on the locale, region, or nearby town in which the fall occurredbefore, during or after other types of metamorphismDar al Gani plateau, Libyan Sahara DesertL5 chondriteFs% 21.2S3lower because the fall was not witnessed26° 52.86' N. 16° 32.95' E.directly proportional to initial velocityA. Sexton, Open University, UK. Meteoritical Bulletin No 84
Ghubaralow     
meteorite falls
high because it is more friable than iron meteoritethermal metamorphismrecorded by eyewitness or inferred from dating methods 21.33% iron. Black xenolithic, unequilbrated host  1954      Ghubara Ghubara, OmanL5 chondrite   Latitude 19 degrees 13 minutes 40 seconds North, Longitude 56 degrees 8 minutes 34 seconds Easthigh because it is more friable than iron meteorite 
Mount Tazerzaitwhich depends on its compositionsharp optical extinction, irregular fracturesthe nature and degree of thermal metamorphism or aqueous alterationless than 5 GPa  
negligible due to quick recovery of meteorite before corrosion begins during meteor phase which depends on compositionshock metamorphismAugust 21, 1991  what witnesses saw or what was recorded by instruments   sharp optical extinction, irregular fracturessharp optical extinction, irregular fracturesunshocked110 kgorthopyroxene for enstatite chondriteMt. Tazerzaitbefore, during or after other types of metamorphismTahoua, Republic of NigerS1 shock stage chondrite S1higher because the fall was witnessed18° 42' N., 4° 48' E.directly proportional to initial velocity 

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