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Drainage Overview - Maricopa County Department of Transportation

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The crossings near 5 West Wash also deserve further attention when developing alignment<br />

alternatives because two tributaries join 5 West Wash near the Deer Valley Road alignment.<br />

Wash 1 confluences with 5 West Wash from the northeast and an unnamed tributary<br />

confluences with 5 West Wash from the south. Additionally, 5 West Wash is roughly<br />

parallel to the Deer Valley Road alignment for approximately 4,000 feet. All three washes<br />

have regulatory floodplains delineated. The combined floodplain width is approximately<br />

6,000 feet along the Deer Valley Road alignment. Significant coordination with FCDMC<br />

and FEMA may be needed because <strong>of</strong> the large extents <strong>of</strong> the regulatory floodplains, the<br />

proximity to the Deer Valley Road alignment, and the distributary nature <strong>of</strong> upstream<br />

flowpaths. For example, two dimensional modeling <strong>of</strong> the watershed may result in a more<br />

refined delineation <strong>of</strong> flood hazards, allowing for smaller drainage crossings.<br />

According to the Wittmann Area <strong>Drainage</strong> Master Study Update (ADMSU) Geomorphic<br />

and Sedimentation Analysis Report (FCDMC, 2005), there are locations within the study<br />

area that may require two-dimensional modeling. Typically these are flat areas with either<br />

braided channels or where no distinct channel is present. The soils in these areas are<br />

generally associated with active alluvial fans or alluvial plains. A map showing the location<br />

<strong>of</strong> the possible two-dimensional modeling areas has been included in Appendix TM3-08.<br />

3.4.2 Geologic Flood Hazards<br />

Flood hazard zones were defined for portions <strong>of</strong> the study area west <strong>of</strong> Trilby Wash in<br />

Geologic Mapping <strong>of</strong> Flood Hazards in Arizona: An Example from the White Tank<br />

Mountains Area, <strong>Maricopa</strong> <strong>County</strong> (1992). Excerpts <strong>of</strong> the mapping have been reproduced<br />

with regulatory floodplains and project boundaries overlaid on the AZGS flood hazard<br />

zones in Appendix TM3-06. Most areas within the study area are classified as areas <strong>of</strong> high<br />

flood potential, H2, which occurs in extensive young deposits where channels are small or<br />

nonexistent. The flooding in these areas is predominantly shallow sheet-flooding, with<br />

broad areas inundated in large flood events. The highest hazard zone, H1, occurs in<br />

extensive young deposits with a distributary channel system. Within the study area, small<br />

localized areas near the CAP were mapped as H1 hazard zones. Typically, proposed<br />

roadway alignments should avoid H1 flood hazard zones when possible. This designation<br />

indicates either an entrenched major drainage or a distributary flow area with potentially<br />

high flow velocities. Mitigation measures that include structural improvements built in<br />

these areas would likely need to be sized for large capacities and have increased<br />

maintenance needs.<br />

3.4.3 Alluvial Fans<br />

Active and inactive alluvial fan systems are located in the study area. These alluvial fans<br />

are sloping, fan-shaped landforms created over long periods <strong>of</strong> time by the transport and<br />

deposition <strong>of</strong> sediment as flows from the White Tank Mountains spread out. The alluvial<br />

fans in this area have been studied in detail as part <strong>of</strong> the Sun Valley Area <strong>Drainage</strong> Master<br />

Plan (SVADMP). The information presented in this section has been taken from the<br />

SVADMP Step 3 Recommended Alternative Report, the CAP Sub-Area (Volume 2)<br />

(FCDMC, 2006). Known problems associated with alluvial fan flooding include spatial<br />

uncertainty <strong>of</strong> water and sediment flow distribution, lack <strong>of</strong> containment within the<br />

relatively flat topographic relief laterally across the fan, avulsive movement <strong>of</strong> defined flow<br />

paths, distributary flow, sheet flooding, scour, and landform aggradation. Relatively steep<br />

091337137, 2011-018, TT005 <strong>Maricopa</strong> <strong>County</strong> <strong>Department</strong> <strong>of</strong> <strong>Transportation</strong><br />

Technical Memorandum 3 Deer Valley Parkway Feasibility Study<br />

<strong>Drainage</strong> <strong>Overview</strong> 14 April 2012

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