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z ~ 200 w 1 so s 0 N 120 a of 80 90000 60000 20000 1 1 1 1 10000 I 1 0 1 IIPV d1E ..• V a11116f z soooo 0 z soooo i" w 30000 N a 20000 I 1 1 1 1 1 1 ~ ; 1 1 I 1 1 1 ~ ' 1982 1 1 1 1 ; 1 1 1 1 I 1 1 1 1 1 1 1 I I 1 1 1 1 1 1 1 1 1 Gov .ue .1LLV asst 120000 ~ ; 200000 1 110000 1 1 180000 1983 1 1 ' 1D0000 1 1 0 1 ~ 16000 90 DDD 1 z 1 . 1 i laoooo ~ 60000 1 1 0 v 70000 1 ' .. 120000 ~ w 1 1 1 1 f w 60000 1 1 1= 100000 N 50000 1 I N 80000 40000 1 1 1 1 ~ 1 ~ a 60000 ° 300D0 ; 1 ~ 1 1 nnnnn 1 1 1 1 10 1 1 ' 1981 Do ' 1 1 / 1 1 1 I 1 00 1 1 1 1 1 1 00 1 1 1 / 1 1 1 1 00 1 1 1 1 I 1 1 00 1 1 1 1 1 00 1 1 I 1 1 1 0 rev .lac ... v alaBT 70000 z of 60000 i 50000 E O 40000 W m a 30000 0 ~ 20000 10000 0 2606 2460 2200 200 1 1 1 1 1 1 1 1 1986 1 1 1 1 1 1 I 1 1 1 1 1 1 1 ; 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 I 1 1 1 1 1 I IW! Jl8 ~ILV aalr 2000 N 0 1600 r " 1600 r w 1400 >: 0 1200 W y 1000 J r 800 O ~ 800 400 Fig: 11. Relation between total sediment discharge and spawning period for Colorado squawfish at Mathers Hole (river kilometer 26.4), Yampa River, 1981-87 (courtesy M. Butler). Solid verticnl lines =total spawning period; dnshed verticnl lines = optimum spawning period. 13 1 1 t 1 1 1 1 / 1 i I 1984 1 1 1 1 I 1 1 1 1 I 1 i 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 I 1 I I 1 z soooo 0 Z 40000 E ~°, 30000 N 0 20000