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<br /> <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 />2.1 <br />-,.>1'- <br /> <br />crossing at Cemetery Road backs up the flood waters creating <br />localized flooding. Tne two crossings proposed by the town, <br />one between Lincoln and Village Roads and the other downstream <br />from Watson Road, were assumed capable of passing the Inter- <br />mediate Regional Flood, but not the Standard Project Flood. <br />Greater flooding at those locations can be expected during the <br />Standard Project Flood. These crossings are still in the <br />planning stage and no engineering designs are available for <br />review. <br /> <br />Due to the wider flood plain, greater depth of flooding, <br />higher velocity of flow and longer duration of flooding uring <br />a Standard Project Flood, damage would be more extensive than <br />during the Intermediate Regional Flood. Plates I~ through ~ <br />show water surface profiles of the Intermediate Regional and <br />the Standard Project Floods. Depth of flow in the channel can <br />be estimated from these illustrations. Typical cross-sections <br />of the floodplain at selected locations, together with water <br />surface elevations and extent of both floods are shown on <br />Plate 15. <br /> <br />OBSTRUCTIONS <br /> <br />As previously noted there are numerous obstructions to flood <br />)s flow in the study area. Pertinent data on obstructive bridges <br />t' ~~&nd culverts are contained in Table 3. As may be seen from Plates <br />0,.\-1 \,,\ 'I <br />v v 3 through , the effect of obstructions is to raise the water <br />S'/ <br />~~ surface elevation upstream; Obstructive bridges are especially <br />susceptible to structural damage from the forces of floodwater <br />and floating debris. <br /> <br />VELOCITIES OF FLOW <br /> <br />Occurrence of the Intermediate Regional and Standard Project <br />Floods will result from the flows shown in Table 2. Channel bed <br />velocities of both floods are on the order of 7 and 12 feet per <br />second respectively, while overbank velocities average between <br />0.5 and 12 feet per second throughout most of the study area. <br />