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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />drainage channel exists through portions of the basin. Several reaches of the major drainage path <br />~ave been altered by man-made activities, These activities include levee construction,' <br />channelization, urban development (buildings and streets), and modifications resulting from <br />farming and ranching operations. In general, stormwater runoff generated within the basin flows <br />into the Tri-Town Drainageway and is conveyed in a northerly direction toward the Saint Vrain <br />River. <br /> <br />The major drainageway for the Tri- Town Basin originates in the vicinity of the City of <br />Dacono. Stormwater runoff generated south of Dacono is combined with runoff from the <br />urbanized area and through the residential streets, ultimately concentrating east of the Birch <br />Street/8th Street intersection. At this location, stormwater runoff is conveyed across 8th Street and <br />State Highway 52 via a cluster of corrugated metal pipes (CMPs), typically less than 4 feet in <br />diameter. A channel/drainage swale conveys stormwater northward across an open field to a man- <br />made channel/berm which directs the runoff in a channel located west of the Towns of Frederick <br />and Firestone. The channel can be typically described as trapezoidal in configuration, bottom, <br />widths vary from four feet to six feet, maximum channel depth ranges from six to twelve feet with <br />IH: I V sideslopes, This channel conveys runoff west along the south side of the Town of <br />Frederick and beneath Main Street in a 6'H x 8'W reinforced concrete box (RCB) culvert. The <br />outlet of the Main Street culvert directs the flow contained in the channel north toward WCR 16 <br />where the major drainageway conveys the runoff via a 6'H x 10'W RCB, The channel continues <br />north for approximately one mile along the west side of the Town of Firestone. Near Firestone, <br />the main channel alignment makes three sharp bends, crossing over the Coalridge Ditch siphon <br />and cutting through the abandoned railroad embankment prior to crossing WCR 13 through a 50- <br />foot wide steel and concrete bridge, Immediately after crossing WCR 13, the channel crosses <br />under WCR 18 through a 17.5-foot steel and timber bridge, Just prior to crossing WCR 20, <br />stormwater runoff conveyed in the major drainageway converges with flow released from the Weld <br />County Tri-Area Sanitation District sewage treatment outfall. From this location, the main <br />channel continues northward approximately one mile where it crosses a lateral from the Godding <br />Ditch before it traverses the Greggerson Dairy to WCR 24 in a series of open ditches and closed <br />conduits, The major drainageway is then carried by the Biederman Ditch north and east to its <br />confluence with the Last Chance Ditch, approximately three-quarters of a mile north of WCR 24, <br />During large flood events, Tri- Town Basin runoff will overflow the Biederman Ditch and combine <br />with out of bank Godding Hollow Basin runoff and proceed over land to the Saint Vrain River, <br />In summary, the major drainageway crosses one abandoned railroad embankment, seven county <br />and/or state roads, two canals, and numerous other minor roads and utilities, <br />Minor erosion of the major drainageway is evident at several locations; this erosion is <br />frequently associated with livestock watering and access. Erosion is also visible at several road <br /> <br />T:IOPENlCoweidOJlcoweldOl tnl rpt.wpd <br /> <br />2.5 <br /> <br />Sepreml:Jt:r 8, 1999 <br />