The Galkiv chondrite is a single 5 kg stone that fell in the Chernigov
region of Ukraine on 1995 January 12. The composition of olivines in
the meteorite indicate that Galkiv belongs to the H group of ordinary
chondrites. Although the heterogeneity of olivine corresponds to a pet
rologic type 5 and the heterogeneity of low-Ca pyroxene suggests the c
hondrite is type 3, clearly defined chondrule boundaries, the presence
of clinopyroxene, cryptocrystalline glass and rare grains of feldspat
ic plagioclase, structural evidences of shock metamorphism and very lo
w level of terrestrial weathering allow us to classify the meteorite a
s an H4 chondrite of shock stage S3 and weathering grade W0.