Two stones that fell near Piplia Kalan on 1996 June 20 are identified
as Ca-rich achondrites belonging to the eucrite group. The conditions
of their fall are described, The petrographic description, texture and
chemical composition, the elemental ratios, particularly K/La and Yb/
Sc, and relatively flat rare-earth-element (REE) patterns (6-8x chondr
ite) of bulk samples without any significant Eu anomaly all agree with
the characteristic values found in eucrites. A feldspar-rich fraction
shows a significant positive Eu anomaly. The presence of several diff
erent lithologies and clasts indicates that it is a texturally diverse
breccia, and the chemical analysis suggests that it belongs to the no
ncumulate group of eucrites falling in the Nuevo Laredo trend.