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2010-252A (09)
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2010-252A (09)
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Last modified
7/9/2020 4:38:33 PM
Creation date
10/5/2015 10:01:45 AM
Metadata
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Template:
Official Documents
Official Document Type
Report
Approved Date
10/12/2010
Control Number
2010-252A (9)
Agenda Item Number
10.A.3
Entity Name
Comprehensive Plan
Subject
EAR based Amendment 2030 Comprehensive Plan
Chapter 8 Conservation Element
Supplemental fields
SmeadsoftID
13461
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Comprehensive Plan Conservation Element <br />EXISTING CONDITIONS <br />Abiotic Features <br />Geology <br />The land surface of Indian River County is underlain by nearly 10,000 feet of sedimentary rocks <br />(carbonates, sands, and clays) which overlay a "basement" complex of igneous and metamorphic <br />rocks. Within the upper 1,000 feet, sediments consist of limestone, dolomite, sand, clay, and shell <br />beds. These sediments are comprised mainly of unconsolidated clastic material (sand and clay) <br />termed the "clastic zone". This area is known as the Tamiami formation or the Fort Thompson <br />formation. The Anastasia formation, found along the coastal area, consists of quartz sand and shell <br />material (Coquina). <br />Within 200 feet of the surface lies the surficial aquifer system. Overlying sediments are <br />predominantly composed of clastic material (sand and clay) and contain the surficial aquifer. Below <br />the surficial aquifer lies the Hawthorn formation. This formation consists of inter bedded limestone, <br />dolomite, sand, and clay, and is about 250 feet thick in Indian River County. The formation acts as a <br />confining layer between the Floridan and surficial aquifers. <br />The Floridan aquifer system includes the Oldsmar, Lake City and Avon Park limestone formations, <br />the Ocala Group, and the Undifferentiated Oligocene Rock layer. While the Lake City and Oldsmar <br />limestone formations are found over 1,000 feet deep, the Avon Park formation consists of limestone <br />and dolomite, and reaches a thickness of up to 250 feet. Immediately overlying the Avon Park <br />formation is the Ocala Group, consisting of the Inglis, Williston, and Crystal River formations, all <br />composed of limestone. The General Geologic Profile of Indian River County is depicted in Figures <br />8.1 and 8.2. <br />• Commercially valuable minerals <br />In Indian River County, minerals mined for commercial value are limited to sand and gravel. <br />Historically, the primary location for sand mining in the county was the Atlantic Coastal Sand Ridge, <br />generally found parallel and proximate to U.S. Highway #1. Figure 8.3 depicts the location of active <br />mining operations in Indian River County as of July 2008. <br />Locally, the predominant use of sand has been for construction purposes, generally for fill related to <br />building construction in low lying areas and locations where on-site disposal (septic) systems are <br />installed. In the past, sand mined from the ridge has been used to renourish the beach area south of <br />Sebastian Inlet. Due to past mining operations, most of the mining potential of the Atlantic Coastal <br />Sand Ridge has been depleted. As a result, mining operations now occur in areas west of the U.S. <br />Highway #1 corridor. <br />Community Development Department Indian River County 2 <br />
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