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6 <br /> Indian River County Page 2 <br /> Project-No . 0041 - 893 <br /> r <br /> - The height and construction type of the observation tower was not provided to us . We <br /> ' presume that the tower's platform will be supported by either timber or concrete columns with <br /> a shallow foundation, system, or may be pile supported, depending on the subsoil conditions . <br /> Generally, ' our work involved subsurface exploration, field permeability testing, laboratory <br /> review and testing, engineering analysis and- preparation of this report which presents the <br /> factual information obtained and our geotechnical recommendations related to design , of the <br /> project components . <br /> ' SITE CONDITIONS <br /> The site settings -are mostly citrus grove with . open grassed areas, and densely wooded <br /> vegetation at the Pelican - Island and Cairns Site respectively . Reference to. the . <br /> S . G. S . <br /> Quadrangle . Map Sebastian, Fla. (dated 1949, photo revised 1970) shows both Pelican Island <br /> . and the - Cairns Site to be relatively flat and at an elevation of approximately +3 feet NGVD . <br /> Per Indian River County requirements, the . minimum; elevation of the road surface will be at <br /> +5 . feet (i . e . , about .2 feet of filling will be needed) : <br /> At Pelican Island north- o <br /> s uth an . <br /> d . east-west trending drainage ditches transect the area. These <br /> were presumably excavated . at some prior time tocontrol water table elevations within the <br /> citrus grove . <br /> The . Soil Survey of IndianRiver County, Florida (SCS) published by the U. S . Department of <br /> Agriculture in January 1987 maps the , pre dominant shallow subsoils - within both Pelican <br /> Island and the Cairns Site as Captiva sands. Soils at. the southern end of Pelican Island along <br /> the Indian River Lagoon are mapped as McKee mucky clay loam. Captiva sand is described <br /> ' as a, nearly level, poorly drained soil that is found in ,narrow, - elongated sloughs that are <br /> between low, dunelike ridges and mangrove swamps . Typically, these areas are mantled by <br /> about 1 /2 foot of very - dark gray fine sand mixed with about 2 percent shell fragments . The <br /> ' underlying soil to a . de th of 6- 1 /2 feet or 'more is described as a fine sand mixed with <br /> p gray <br /> about 2 to 15 percent shell fragments . . McKee mucky clay loam is described as level; very <br /> poorly drained soil that is found in mangrove islands and. swamps at, or near sea level, in, or <br /> adjacent to , the Indian River, Typically, the surface layer is very dark grayish brown mucky <br /> I loam about 1 inch in thickness. It is followed by dark 'gray clay loam, sandy clay, and <br /> sandy loam to a depth of,about 64 /2 feet or more . <br /> Under natural conditions; the SCS reports that the water table in areas of Captiva sand is <br /> between the depths of 10 and 40 inches for 6 to 9 months during most years; and at a depth of <br /> less than 10 inches' for 1 to 3 months during the wet season. However, standing water <br /> reportedly covers the soil for about 1 month in some years. According to the SCS , McKee <br /> ' mucky clay loam remains saturated throughout the year. <br />