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<br />Green River Floodplain Inundation <br /> <br />11 <br /> <br />June 2005 <br /> <br />Table 2. Floodplain Type, Inundation Flow, Inundated Area, and Distance from the <br />Razorback Spawning Bar for 16 Priority Wetlands. <br /> <br /> Distance from <br />Site Inundation Flow Inundated Area Spawning Bar <br />No.a Floodplain Site Typeb (cfs) (ac) (river mi) <br />1 Thunder Ranch D 13,000" 330 5 <br />2 IMC T 18,600 4 8 <br />3 Stewart Lake D 7,500 570 11 <br />4 Sportsman's Lake D 20,000 132 14 <br />5 Bonanza Bridge D 13,000 23 21 <br />6 Richens/Slaugh T 18,600 45 25 <br />7 Horseshoe Bend D 13,000 17 27 <br />8 The Stirrup D 13,000 20 36 <br />9 Baeser Bend D 13,000 38 38 <br />10 Above Brennan D 13,000 41 45 <br />11 Johnson Bottom D 13,000 146 47 <br />12 Leota Ponds D 13,000 ],016 52 <br />13 Wyasket Lake T/Dd 18,600 850 55 <br />14 Sheppard Bottom De 25,300 1,350 58 <br />15a Old Charley Wash (Main) D ] 4,000 336 60 <br />15b Old Charley Wash (Diked) T 13,000 56 60 <br />16 Lamb Property T 18,600 463 70 <br />Source: modified from Valdez and Nelson (2004). <br />a Corresponds to numbers on Figure 2 <br />b D = depression, T = terrace <br /> <br />" Inundation flows with notched levees as identified in Muth (2004). Valdez and Nelson (2004) reported that levee <br />removal would allow inundation of the Thunder Ranch floodplain at 16,900 cfs. Without levee removal, <br />inundation would require approximately 30,000 cfs. <br /> <br />d Wyasket Lake has little potential to hold water throughout the year and, except for a deep trench and a small <br />depression, acts largely as a terrace floodplain according to Valdez and Nelson (2004). It is treated as a terrace <br />floodplain in this paper. <br /> <br />e Although much of the floodplain area within Sheppard Bottom acts as terrace floodplain according to Valdez and <br />Nelson (2004), the entire area identified as floodable has been considered as depression floodplain in this paper. <br />