Как по Английски будет 继而

noun

A stream whose course follows the dip of strata (in the manner of a consequent stream) but is at a lower level than the original surface of the underlying geological formation.

adjective

Designating, or characterized by the presence of, a stream or streams whose course follows the dip of strata (in the manner of a consequent stream) but is at a lower level than the original surface of the underlying geological formation.