Au`to*clas"tic (?), a. [See Auto-
; Clastic.] (Geol.) Broken in place; -- said of
rocks having a broken or brecciated structure due to crushing, in
contrast to those of brecciated materials brought from a
distance.
Au`to*clas"tic (?), a. [See Auto-
; Clastic.] (Geol.) Broken in place; -- said of
rocks having a broken or brecciated structure due to crushing, in
contrast to those of brecciated materials brought from a
distance.