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2014-01-06_PERMIT FILE - M2014001 (4)
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2014-01-06_PERMIT FILE - M2014001 (4)
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Last modified
8/24/2016 5:38:42 PM
Creation date
1/7/2014 3:16:59 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M2014001
IBM Index Class Name
PERMIT FILE
Doc Date
1/6/2014
Doc Name
permit application (see separate maps)
From
Connell Resources
To
DRMS
Email Name
TAK
Media Type
D
Archive
No
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were eroded, and the process of cutting and filling of channels was so widespread that gravel and <br />sand were deposited in sheet -like beds. The principal streams eroded into the bedrock, cutting <br />and building terraces along the channels. More recent streams, such as Lone Tree Creek in the <br />proposed permit area, have cut through the highly erodible over -lying unconsolidated material in <br />most areas and do not generally have associated alluvial deposition. <br />Traditional organic topsoil on most of the site is thin or non - existent. Most of the soils are <br />shallow to deep loams that are well drained. Over most of the identified sand and gravel deposit <br />is a loamy, wind -mixed veneer layer of soil overburden material varying in depth from less than <br />one inch to six feet. The soil overburden material likely developed from alluvial and eolian <br />deposits of clay, silts, and sands. Over time, erosive forces of wind and water have influenced <br />the soils on the site. Mobile soil particles, such as silt and clay, have eroded from higher <br />topographic positions and have been re- deposited in lower areas. Therefore, swale areas may <br />have finer textured soils than ridgetops. The aggregate deposits and loamy soil overburden <br />material are underlain by a variable pattern of shale and sandstone parent materials. <br />Mine Phasing <br />Connell Resources anticipates mining and reclaiming the proposed Connell Carr Pit site in <br />approximately 15 years. However, the rate of mining and overall life of the mine is dependent <br />on several factors including product demand. Test pits have verified that commercial deposits of <br />sand and gravel exist up to 25 feet below the surface of the ground. In addition to the <br />commercial sand and gravel materials, clay, silt, and other non - marketable materials excavated <br />from the proposed permit area will be used on -site for reclamation. <br />The mining plan currently includes mining in two phases; the first phase south of Lone Tree <br />Creek and the second phase north of the creek (see Exhibit C -5, Pre- Mining/Mining Plan Map). <br />Phase I (288 acres) will be mined from the northwest to the southeast. When Phase I is <br />complete, a temporary crossing will be established through the Lone Tree Creek drainage and <br />Phase II (94 acres) will be mined from east to west. All necessary permits will be obtained and <br />any special construction techniques will be used to reduce impacts and create a stable crossing <br />through the ephemeral drainage. Mining will not occur within the Lone Tree Creek channel. <br />Even though the proposed permit area will be mined in only two phases, integration of mining <br />and reclamation is still applicable. In general, as the pit reaches its maximum depth and edges <br />are completed, they will be backfilled and reclaimed. In areas where the final pit depth has been <br />achieved and operations are no longer present, backfilling and reclamation of pit walls will <br />extend onto the floor. <br />Rough contouring of the pit floor with the Lone Tree Creek drainage will take place during <br />mining while fine contouring and establishing final drainage patterns will be one of the last steps <br />in the reclamation process. The contour blending will avoid steep transitions and create a <br />topography that produces a smooth, relatively low velocity flow from the mined area to the <br />adjacent creek drainage system. Overland flow patterns will be incorporated into this transition <br />so as to connect the pit floor with existing shallow drainage swales. <br />Connell Carr Pit <br />DBMS 112 Permit -application Page 6 <br />
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