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<br />I <br /> <br />3 <br /> <br />I <br /> <br />STUDY AREA DESCRIPTION <br /> <br />Study Reach Description <br /> <br />I <br /> <br />Drainage Basin Characteristics <br /> <br />The study reach consists of two sub-reaches: one on South St. Vrain <br />Creek and the other on Middle St. Vrain Creek (see Index Map, Plates <br />2, 3 and 4). The South St. Vrain Creek reach starts from the mouth <br />(confluence with North St. Vrain Creek) as its lower limit and extends <br />approximately 10 miles to the confluence with Middle St. Vrain Creek as <br />its upper limit. Throughout this study reach, it is a front range <br />mountain stream: rather narrow in width and steep in slope (160 feet <br />per mile), except in the downstream portion near Lyons. The Middle St. <br />Vrain Creek reach starts from the mouth as its lower limit and extends <br />approximately eight and one-half miles to Peaceful Valley as its upper <br />limit. It is also a typical mountain stream, with an even steeper <br />slope (about 240 feet per mile). <br /> <br />I <br /> <br />South St. Vrain Creek is located in Boulder County, Colorado. Its <br /> <br /> <br />headquarters originate on the eastern slopes of the continental divide <br /> <br /> <br />at elevations in excess of 13,000 feet above mean sea level. The creek <br /> <br /> <br />flows in a generally northeastward direction and joins North St. Vrain <br /> <br />Creek at Lyons to form St. Vrain Creek, which drains into the South <br /> <br /> <br />Platte River near Platteville, Colorado. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />This study includes the entire South St. Vrain Creek basin which en- <br /> <br /> <br />compasses a drainage area of approximately 92 square miles (see Basin <br /> <br />Map, Plate 1). The major tributary included in the basin is Middle St. <br /> <br /> <br />Vrain Creek which drains an area of 32.4 square miles into South St. <br /> <br /> <br />Vrain Creek at about two miles east of Riverside. Drainage areas at <br /> <br /> <br />different locations in the basin are given in Table 1. <br /> <br />I <br /> <br />Location <br /> <br />South St. Vrain Creek at mouth <br /> <br />South St. Vrain Creek immediately <br />downstream of confluence with <br />Middle St. Vrain Creek <br /> <br />South St. Vrain Creek immediately <br />upstream of confluence with <br />Middle St. Vrain Creek <br /> <br />Middle St. Vrain Creek at mouth <br /> <br />Middle St. Vrain Creek at <br />Peaceful Valley (State Route 72 <br />bridge) <br /> <br />Area (square miles) <br />92 <br />66.7 <br /> <br />The stream valleys in the study area are rather narrow in width. For <br /> <br /> <br />this reason, early development was mainly limited to roads and bridges. <br /> <br /> <br />More recently, however, homes have been built on the banks of Middle <br /> <br /> <br />St. Vrain Creek at Riverside, Raymond and Peaceful Valley, some within <br /> <br /> <br />the floodplains. With this type of floodplain development, flood <br /> <br /> <br />hazards to the communities will continue to increase unless adequate <br /> <br />and sound floodplain regulations are adopted. <br /> <br />I <br /> <br />I <br /> <br />Table 1 <br />Drainage Areas <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />32.4 <br />18.7 <br /> <br />Obstructions to flood flows within the study reach include natural ob- <br /> <br /> <br />structions such as trees, brush and other vegetation growing along the <br /> <br /> <br />streambank and manmade obstructions such as buildings, bridges and cul- <br /> <br /> <br />verts. During floods, these obstructions impede flood flows and cause <br /> <br />backwater conditions that may increase the flood heights upstream of <br /> <br /> <br />the obstruction and velocities downstream of the obstruction. Brush <br /> <br /> <br />washed out during floods is carried along downstream and may collect at <br /> <br /> <br />bridges and in culverts due to channel constrictions, thus creating a <br /> <br />damming effect and overbank flow. As flood flows increase, masses of <br /> <br /> <br />debris may break loose and cause a wall of water and debris to surge <br /> <br /> <br />downstream until another obstruction is encountered. In some instances, <br /> <br />debris may collect to the point where structural capability is exceeded <br /> <br />I <br /> <br />34.3 <br /> <br />I <br /> <br />The mean annual precipitation over the basin is approximately 22 inches, <br />of which 50 percent occurs during the period May through September. <br />Mean temperature ranges from 700 F in July to 25 degrees in January, <br />with an annual average of about 450 F. The basin topography is typical <br />m~untain terrain covered with forest growth. <br /> <br />I <br /> <br />I <br /> <br />I <br />