| 释义 |
secondary consequent stream secondary consequent stream[′sek·ən‚der·ē ′kän·sə·kwənt ′strēm] (hydrology) A tributary of a subsequent stream, flowing parallel to or down the same slope as the original consequent stream; it is usually developed after the formation of a subsequent stream, but in a direction consistent with that of the original consequent stream. Also known as subconsequent stream. |