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2024-06-07_PERMIT FILE - M2024026 (22)
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2024-06-07_PERMIT FILE - M2024026 (22)
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Last modified
6/11/2024 7:22:15 AM
Creation date
6/10/2024 10:50:01 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2024026
IBM Index Class Name
Permit File
Doc Date
6/7/2024
Doc Name Note
Exhibit G - Water Information
Doc Name
Application
From
Colorado Sand Company II, LLC
To
DRMS
Email Name
NCG
JLE
EL1
Media Type
D
Archive
No
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Exhibit G <br /> Page 3 <br /> series present within the Permit Area. The soil map units within the Permit Area are classified as well drained to <br /> excessively drained with texture of sand to loamy sand and a hydric rating of zero(0). <br /> The U.S.Fish and Wildlife Service(USFWS)National Wetlands Inventory(NWI)digital wetland mapping National <br /> Wetland Inventory(NWI)digital mapping and National Hydrography Dataset(NHD)digital waterway mapping <br /> resources revealed one stream in the northeast corner of the Permit Area and two wetlands in the southeast section of <br /> the Permit Area(See Exhibit G-3,Figure 3). Upon field verification of this desktop data during the October 2023 <br /> surveys,OHWM indicators were absent and there was no indication of a water course in the vicinity of this NHD- <br /> mapped feature.Therefore,only one waterbody feature was observed and discussed below,subsequently leaving <br /> this feature out of any other surface and groundwater feature maps in this application. <br /> Notable findings of the surveys are described in the following sections: <br /> Surface Water Resources <br /> Based on field observations,no wetlands were identified within the Permit Area. <br /> NWI-mapped wetland locations were investigated and determined to lack one or more of the three criteria necessary <br /> to define a wetland.Although hydrophytic vegetation(saltgrass [Distichlis spicata])was present,hydric soil <br /> indicators were absent,and hydrologic indicators were marginal at best. In addition,the NWI-mapped wetland <br /> locations occur in uplands adjacent to a remnant unlined stock pond historically and artificially fed by a well pump <br /> powered by solar panels. The pumped water required to fill the cattle pond is no longer necessary as cattle <br /> operations have ceased in the Permit Area. <br /> One 0.38-acre manmade stock pond was delineated along an OHWM consisting of a defined bank situated above <br /> mud cracks.The stock pond contained no water at the time of the survey and contained one inlet structure from a <br /> solar-powered well pump and no outlet structures. Vegetation was mostly absent except for intermittent patches of <br /> saltgrass and kochia(Bassia scoparia)along and above the OHWM bench.One NHD-mapped stream located in the <br /> northeast section of the Study Area was further investigated.OHWM indicators were absent and there was no <br /> indication of a watercourse in the vicinity of the NHD-mapped feature.None of the features were observed to have <br /> downstream connectivity to jurisdictional waters. <br /> A request for an Approved Jurisdictional Determination(AJD)decision was submitted to the USACE on February <br /> 8,2024,and granted by the USACE on March 11,2024. The USACE confirmed that the observed surface water <br /> feature is not a jurisdictional water of the U.S.under Section 404 of the Clean Water Act(CWA). Copies of the AJD <br /> request and the USACE AJD letter are included as Exhibit G-1 and G-2. See the Kersey Mine Wetland and <br /> Waterbody Delineation Report(Exhibit G-3)for further detailed information,photographs,and figures. <br /> Groundwater Resources <br /> The Mine Site falls within the South Platte River Valley(USGS,2000). The primary uppermost aquifer in the <br /> Permit Area is the Laramie-Fox Hills aquifer. The sandstone of the uppermost groundwater-bearing unit,the Fox <br /> Hills Sandstone,is approximately 150 to 200 feet thick and is generally comprised of fine-to medium-grained <br /> sandstone and siltstone deposits interbedded with shale and claystone(Robson and Banta, 1987).Historic records <br /> collected along the South Platte River Valley from 1953 to 2012 from 1,669 groundwater wells indicate the depth to <br /> groundwater average per decade over the entire aquifer ranges in depths of between 24 and 32 ft-bgs over the 60- <br /> year record. The average depth to groundwater between 1953 and 1962 was approximately 32 ft-bgs followed by a <br /> rise in average groundwater depth between 2003 to 2012 to 30 ft-bgs following the curtailment of groundwater <br /> Colorado Sand Company II, LLC <br /> Kersey Mine Construction Material Regular(112)Operation Reclamation Permit Application <br /> June 7,2024 <br />
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