Laserfiche WebLink
<br />apply to all areas containing or suspected of containing: (a) <br />natural hazards which include, but shall not be limited to <br />flooding; concentrated runoff; inadequate drainage;... <br /> <br />Section 4.2.3(e) of the Subdivision Regulations requires that any <br />proposed subdivision that lies in an identified flood hazard area <br />or, in the absence of officially identified areas, that is suspected <br />by the County Planning Commission to lie in a flood hazard-prone <br />area, the subdivider shall also submit a study by a professional <br />engineer for approval. A detailed requirement for improvements in <br />areas of potential flood hazard is included in the Archuleta County <br />Building Permit regulations. <br /> <br />~ <br /> <br />3.0 ENGINEERING METHODS <br /> <br />~ <br /> <br />For flooding sources studi~d in detail in the town and county, standard <br />hydrologic and hydraulic study methods were used to determine the flood <br />hazard data required for this study. Floods having recurrence intervals <br />of 10, 50, 100, and 500 years have been selected as having special sig- <br />nificance for flood plain management and for flood insurance premium <br />rates, The analyses reported here reflect current conditions in the <br />watersheds of the flooding sources. <br /> <br />3.1 Hydrologic Analyses <br /> <br />Hydrologic analyses were carried out to establish the peak discharge- <br />frequency relationships for floods of the selected recurrence <br />intervals for each stream studied in detail in the town and county. <br /> <br />. <br /> <br />A regional relationship of basin area to peak discharge was used <br />for the Rio Blanco. Gaging stations located within the upper San <br />Juan River basin (Table 1) were used to establish the regional <br />relationship. The method developed by the U.S. Water Resources <br />Council (Reference 2) was used to determine the floodflow-frequency <br />relationship, based on a log-Pearson Type III distribution for each <br />selected gaging station. Gaging stations used for developing the <br />regional relationship were selected according to the fOllowing <br />criteria: (1) stations having 10 or more years of record, and (2) sta- <br />tions where peak flows are not affected by regulation and diversion, <br /> <br />. <br /> <br />Because the annual peak discharges published in U.S, Geological <br />Survey Water-Supply Paper Nos. 1683, 1925, and 2125 (References 3, 4, <br />and 5, respectively) and Water Resources Data for Colorado (Refer- <br />ence 6) were a mixture of flood flows caused by snowmelt and rainfall <br />events, the regional relationship established by using these annual <br />peak discharges is not accurate for intense rainfall-produced floods. <br />A more detailed method was used for each gaging station to develop <br />regional relationships for this area. The procedures are described <br />as follows: (1) separating the rain and snowmelt data at each <br />gaging station; (2) developing statistics for each type of event; <br />(3) statistically combining the two frequency curves (streamflow <br />records were obtained from the U.S. Geological Survey, Denver Federal <br /> <br />7 <br />