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videography to quantify potential endangered fish habitat versus <br />flow on the San Juan River. This methodology provided macrohabitat <br />morphology information for the San Juan River from the Hogback <br />Diversion (RM 158) to Mexican Hat (RM 52). Video from 1991 has <br />been analyzed and 1992 data analysis is in progress. <br />In the reach between Hogback Diversion (RM 158) and Four Corners <br />(RM 119), the data thus far indicate that maximum side channel <br />habitat area occurred at the highest flows. At the lowest flows <br />examined, side channel area reached its minimum. On the other <br />hand, backwater area was maximized at low flow. Backwater area at <br />midrange flows was fairly constant at a level 46 percent less than <br />the maximum (1991 data). This reach had the most side channel, <br />backwater, and main channel habitat per mile. <br />Between Four Corners (RM 118) and Bluff (RM 68) side channel area <br />was also maximized at the peak flows and minimum at lowest flows <br />(less than 1200 cubic feet per second). With the exception of peak <br />flow, backwater area was maximized at the lowest flows and <br />decreased with increased flow. As observed on the video of the <br />peak flows in 1991 and 1992, the water encroached ephemeral <br />tributary stream channels and arroyos creating a group of <br />backwaters found only at higher flows. Also observed were side <br />channels becoming active that normally are above the water level. <br />As the flow dropped from peak to base flow, there was a steady <br />increase in backwater area. The formation of this backwater habitat <br />appeared to stem from the flow. reaching a threshold where side <br />channels became cut off and formed backwaters. In addition, the <br />decreasing flow exposed and deposited sediment features that caused <br />the formation of a group of low flow backwaters. <br />The reach from Bluff to Mexican Hat (RM 67 to 52) had a distinctly <br />different channel morphology compared to the upper portions of the <br />river. Backwater and side channel habitat in this reach was <br />markedly lower and controlled by the geomorphology of the San Juan <br />canyon. Only at flows of 1,200 cubic feet per second and lower did <br />low velocity habitat appear in the data, other than backwaters <br />formed by tributary channel encroachment. <br />The Remote Sensing and Geographic Information Section is continuing <br />videography collection of the San Juan River during 1993 to <br />validate and refine preliminary findings and further detail flow <br />to habitat relationships. <br />Hydrology and Geomorphic Characterization - Studies were conducted <br />in the areas of: (1) geomorphic characterization; (2) river <br />dynamics; (3) habitat mapping; (4) hydraulic modeling; and (5) <br />hydrology of the San Juan River in 1992. <br />Base Map Preparation - A geographically based digital base map was <br />12 <br />