Con‐form′a‐bil″i‐ty (?), n. 1. The state of being conformable.
2. (Geol.) The parallelism of two sets of strata which are in contact.
Webster's Dictionary 1913
Con‐form′a‐bil″i‐ty (?), n. 1. The state of being conformable.
2. (Geol.) The parallelism of two sets of strata which are in contact.