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G-5 Flood Control <br /> A critical component in the operation of the Climax facilities is flood protection. Climax has dedicated <br /> significant resources to the protection of the facilities from extreme flood events. Protection of the TSF's from <br /> extreme precipitation events is in accordance with regulatory requirements and FMI corporate standards. <br /> G-5.1 Background <br /> In 2005, W. W. Wheeler and Associates (Wheeler) completed a site-wide hydrological assessment of the <br /> Climax Mine and evaluated its ability to safely handle the flood generated by the PMP event(Wheeler,2005). <br /> As part of that study,Applied Weather Associates performed a hydro-meteorological analysis and developed <br /> a site-specific PMP design storm for the Climax site (Applied Weather Associates, 2005). The 2005 <br /> hydrology study indicated that, under the configuration at that time,the water storage facilities and TSF water <br /> pools at Climax were capable of passing the site-specific PMP in accordance with DRMS and Colorado <br /> Division of Water Resources requirements. <br /> Although no significant impacts to the drainage basins and hydrologic regime have occurred at Climax due to <br /> mine production, the water storage capacity and dam crest elevations of the TSFs change due to tailing <br /> deposition. In order to evaluate the implications of mine operation and closure on the system's flood handling <br /> capabilities, the hydrology model has recently been revised to model the expected site conditions for the <br /> current operating scenarios with a new flood decant riser on Mayflower TSF (Wheeler, 2019). This study <br /> included the use of a new extreme precipitation development tool known as the Colorado-New Mexico <br /> Regional Extreme Precipitation Study (CONM-REPS Tool). This study confirmed that the flood protection <br /> facilities at the Climax Mine were capable of passing the new PMP generated flood and the results were used <br /> to develop the flow capacity design criteria for the new decant riser on Mayflower TSF. <br /> Over the last several years, the State of Colorado Dam Safety Branch of the State Engineer's Office (State <br /> Dam Safety) has updated the tools and methods recommended to be used to perform hydrologic analysis of <br /> water storage dams in the state. These updated tools and methods for water storage dams in Colorado are <br /> described in Guidelines for Hydrological Modeling and Flood Analysis (DWR, 2022) will be used to update <br /> the design storm flood hydrology for the Climax Mine site. The procedures to be used in the flood study <br /> update are summarized below. <br /> G-5.2 Drainage Basins <br /> The Tenmile Creek drainage basin area is generally typical of high mountain basins in the Rocky Mountains. <br /> The slopes of the basin are generally steep and elevations range from a maximum of nearly 14,000 feet along <br /> the eastern boundary,to a minimum of about 10,600 feet at the crest of 5 Dam. The drainage basin is divided <br /> into several sub-basins to model flood impacts on the three primary TSFs and Clinton Reservoir. Figure G-01 <br /> shows the configuration of the various sub-basins and summarizes the drainage areas. The mean basin <br /> elevation for the areas tributary to the three primary TSFs are 11,200 feet for the Robinson TSF, 11,440 feet <br /> for Tenmile TSF, and 11,520 feet for Mayflower TSF. <br /> G-5.3 Soils and Infiltration <br /> The approach now recommended by DWR in Colorado for estimating infiltration losses from direct rainfall is <br /> the Colorado State University— Soil Moisture Accounting (CSU-SMA) approach which can simulate three <br /> distinct types of storm runoff: infiltration-excess, saturation-excess, and subsurface runoff. The CSU-SMA <br /> approach, which also employs the Linear Reservoir baseflow method, is used in conjunction with the Clark <br /> Unit Hydrograph method (for rainfall to runoff transformation) to more accurately reproduce the runoff <br /> response mechanisms that are observed in the diverse terrain across Colorado. <br /> The method requires that various raster datasets describing other pertinent soil properties:%sand,%clay,% <br /> organic matter, and depth to restrictive layer be acquired from the DWR Dam Safety website for the Climax <br /> Mine watershed. These soil property raster files are then used as inputs to the CSU SMApython2 script (a <br /> program for automating ArcGIS calculations) provided by the DWR to characterize each sub basin property <br /> statistically, generating the minimum, maximum, average, range, and standard deviation of each sub-basin <br /> Exhibit G G-19 May 2024 <br />