Stone Mountain Tennis Center
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Stone Mountain Tennis Center
The Stone Mountain Tennis Center was a tennis venue at Stone Mountain Park in Stone Mountain, Georgia, USA. It was built to host the tennis events for the 1996 Summer Olympics and the 1996 Summer Paralympics, at a total cost of $22 million. At the time of the Olympics, the complex included over 12,000 seats for tennis fans, a plaza area located around the stadium, and a stadium court plus 15 additional outer courts. The reconfigured stadium held 7,200 people, and two smaller courts seated 4,000 and 2,000. Although the park was in DeKalb County, the Tennis Center itself was in Gwinnett County. The facility played host to the 1997 U.S. Women's Hard Court Championships and the 1998 Davis Cup competition featuring Andre Agassi and Jim Courier, which the U.S. won against Russia. The Stone Mountain Tennis Center also hosted a concert in October 2005 with Roberta Flack and Melba Moore. Since the Olympics, the ownership of the facility has transferred to the State of Georgia's Stone M ...
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Stone Mountain Tennis Center, July 2016
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its Chemical compound, chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the Earth's crust, crust, and most of its interior, except for the liquid Earth's outer core, outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathe ...
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