sills
Sills are tabular slabs or concordant intrusive (plutonic) sheets of igneous rock that intruded laterally and horizontally, or nearly horizontally, as magma. Sills lie between and parallel to layers of older sedimentary rock, beds of volcanic lava or tuff, or along the direction of foliation in metamorphic rock.
Labels: concordant, igneous rock, intrusive, sill, tabular