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RECLAMATION PLAN <br /> Applicant, George Reed, Inc., request a permit for the removal of 2.5 million tons of <br /> rock, sand, and gravel over a 12 year period, which includes total reclamation, using the <br /> open pit method of extraction with reclamation concurrent with excavation. George <br /> Reed, Inc. is currently extracting sand and gravel from the existing quarry issued a <br /> permit in 1990, QX-90-1. The permitted quarry is expected to be depleted early next <br /> year. This permit would allow applicant to continue operations on contiguous parcels <br /> adjacent to the existing quarry without substantial change in the daily operations as they <br /> currently exist. All extracted materials will be processed at the existing plant located on <br /> the Northside of the Mokelumne River. <br /> I. DESCRIPTION OF ENVIRONMENTAL SETTING: The project site is bounded <br /> to the North by farm land and the Mokelumne River, East by a bluff, South by the <br /> existing quarry operation and West by farm land. All land currently being farmed will <br /> continue to be farmed until excavation commences. <br /> A. MAPS: Maps showing project area, site access and topography attached. <br /> B. GEOLOGY: The project site lies in a valley which is within the ancient flood plain <br /> of the Mokelumne River and is bounded on the east and south by a high natural bluff, <br /> which rises steeply about 35 feet. The Mokelumne River lies to the north and the <br /> valley slopes away gently to the west. The alluvial deposits of soil, sand, gravel and <br /> rock, which form the valley floor, are of recent quaternary origin and of variable <br /> depth and thickness. The silts, sandy silts, and fine sands usually occur at or near the <br /> surface and vary in depth from 0 to 15 feet. Agricultural releveling has significantly <br /> altered (surface materials). Below these silts and fine sands are the coarser sands and <br /> fine and coarse gravels, and finally the larger cobble type rocks. These materials are <br /> roughly sorted into strata of varying depths. Below the lower limits of the alluvial <br /> deposits is a densely compacted grayish colored lava ash of undetermined thickness, <br /> believed to be from the lower or middle Pliocene era. The area has no history of <br /> earthquakes, landslides, subsidence or other geologic instability. The project site is <br /> classified as a Mineral Resource Zone-3 by the Division of Mines and Geology, in <br /> accordance with the California Surface Mining and Reclamation Act of 1975, which <br /> indicates that the site contains potentially significant deposits of aggregate resources. <br /> C. HYDROLOGY: During the January of 1997 excessive rains and flooding along the <br /> Central Valley's rivers, none of the parcels within the project area were inundated or <br /> subjected to over flow from the South bank of the Mokelumne River. There will be <br /> no impact to the ground water. Based on borings,the ground water elevation is <br /> approximately 60' +/-. Excavation depths will not exceed 30 +/- feet. Waste <br /> discharge is not applicable to this application. <br />