单词 | secondary consequent stream |
释义 | secondary consequent stream [`sek·ǝn´der·ē `kän·sǝ·kwǝnt `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. |
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