Laserfiche WebLink
<br />3. Please refer to attached Exhibit B. The purpose of this spreadsheet is to take a specific look at <br />each of the 25 properties along Gore Creek where structures are affected by the new floodplain. <br /> <br />There are 4 comparisons of the adopted floodplain study vs. new floodplain study: <br />· Base Flood Elevations <br />· Stream Bottom Elevations <br />· Change in Base Flood Elevation compared to Stream Bottom <br />· Volume of flow for the 1 % annual chance flood <br /> <br />Please note the following: <br />· The BFE comparisons tend to fluctuate <br />· The stream bottom elevations tend to fluctuate <br />· From the Buffehr Creek confluence, upstream towards East Vail, there are several areas <br />where there is substantial increases in the overall flood depth, even though the "a" is lower <br />along the entire length of Gore Creek <br /> <br />If the "a" has decreased along the length of Gore Creek, then why would there be ANY increase <br />in BFE when compared to the currently adopted Floodplain Study? <br /> <br />4. Tributary topographic information is very general. How is it possible to determine the Flood <br />Hazard Area when specific channel information is not available? See attached Exhibit F. Also, <br />we have some x-section information on Middle Creek and Mill ~reek West. Should this info be <br />incorporated into the model? (See Item 4 under "Specific Items") <br /> <br />5. . Along Gore Creek, the "Q" only increases 30 cfs at the confluence of Buffehr Creek, (2620 cfs <br />upstream, 2650 cfs at the mouth of Gore Creek) while Buffehr Creek flows at 255 cfs. While we <br />understand that "a" has a timing factor that needs to be considered, should the increase in <br />volume along Gore Creek be greater? <br /> <br />6. Why does the Flood Hazard Area disappear at some bridge crossings and not others? Is it <br />because the crossings are in culverts and not actual bridge spans? <br />· Panel 468 - Buffehr Creek disappears under Circle Drive, but not under Chamonix Lane <br />· Panel 469 - Red Sandstone Creek disappears under four crossings, not including 1-70 <br />· Panel 469 - Spraddle Creek disappears once just before it goes under 1-70 <br />· Panel 493 - Pitkin Creek disappears several times under short spans <br /> <br />Specific Items <br />1. Panel 468: Buffehr Creek is shown overtopping Chamonix Lane. Is this really occurring? A new <br />culvert was installed in 2000 that should be large enough to handle the 1 % annual chance flood. <br />Also, The a has not changed from the 1983 Study, but FHA has shrunk significantly. At Circle <br />Drive crossing, BFE has increased by 4 feet, yet FHA has decreased? See attached Exhibit F. <br /> <br />2. Panel 469: Red Sandstone Creek, on the north side of 1-70 - The FIRMs show an approximate <br />increase in the BFE of 9', just upstream from culvert. This seems a bit excessive since the a has <br />only increased by 30 cfs, and since a note indicates that the culvert will contain the 1 % annual <br />chance flood. <br /> <br />3. Panel488: Mill Creek East flows into an 84" cmp culvert approximately 125 If upsteam of <br />confluence with Gore Creek. Please refer to the attached Exhibit C. <br /> <br />4. Panel 488: Mill Creek West is shown flowing around bridge abutments that are approximately <br />150 If upstream of Hanson Ranch Rd (approx BFE = 8190). A floodplain analysis performed by <br />Sato and Associates in September 2003 shows the bridge contains the 1 % annual chance flood. <br />See attached Exhibit D. <br />