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rock > igneous rock > differentiated meteorite > differentiated achondrite > asteroidal achondrite > HED meteorite > eucrite > DaG 609
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DaG 609 comparison table
Subject has weather resistance has minerology has number of fragment has degree of shock metamorphism has shock stage is an instance of has distinguishing feature has fragmentation probability has fall location has metamorphism mechanism has likely origin has solidification mechanism has weather has weathering stage has letter designation has acronym has relative abundance has value has total mass of find has pyroxene composition has fall coordinate has characteristic mineral has composition is a kind of has comment has find date has mass has image has number of find has origin has ablative mass loss has shock pressure has solidification timescale classified by be an acronym for has petrology
Dar al Gani meteoritewhich depends on its composition      during meteor phase which depends on compositionDar al Gani plateau, Libyan Sahara Desert   can be severe due to long exposure time to environmental corrosion agents  DaG lower because the fall was not witnessed485755 kg in degrees, minutes and seconds of lattitude and longitude often minerals not found on EarthSahara meteorite when the meteorite was found  1691meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimaldirectly proportional to initial velocity     
eucriteloworthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica    no chondruleshigh because it is more friable than iron meteoritestrewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity cumulates, crystallized melts, impact mixingextrusion onto the surface of the planet or asteroid via a volcanic eruption  AUEC 7.1 % of meteorite falls 231 kg in degrees, minutes and seconds of lattitude and longitudeanorthite-pigeonite Ca-richsilicates (with very few exceptions)basalt    234 Vestahigh because it is more friable than iron meteorite very rapid Howardite, Eucrite, Diogenitecoarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated
S3 shock stage meteoritewhich depends on its composition  weakly shockedS3  during meteor phase which depends on compositionstrewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocityshock metamorphism        485755 kg in degrees, minutes and seconds of lattitude and longitude often minerals not found on Earthshocked meteorite    1691meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimaldirectly proportional to initial velocity15 to 20 GPa    
DaG 609which depends on its compositionorthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica2weakly shockedS3eucriteno chondrulesduring meteor phase which depends on compositionDar al Gani plateau, Libyan Sahara Desertshock metamorphismcumulates, crystallized melts, impact mixingextrusion onto the surface of the planet or asteroid via a volcanic eruptioncan be severe due to long exposure time to environmental corrosion agentsW2AUECDaG lower because the fall was not witnessed231 kgFs% 27-6326° 53.13' N. 16° 34.81' E.anorthite-pigeonite Ca-richoften minerals not found on Earth iron-rich, monomict, with chromite grains19980.696 kg
234 Vestadirectly proportional to initial velocity15 to 20 GPavery rapidA. Sexton, Open University, UK. A. Sexton, Meteoritical Bulletin No 83Howardite, Eucrite, Diogenitecoarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated

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