https://wikimd.com/index.php?action=history&feed=atom&title=GeodeGeode - Revision history2026-04-04T02:39:08ZRevision history for this page on the wikiMediaWiki 1.44.2https://wikimd.com/index.php?title=Geode&diff=5632212&oldid=prevPrab: CSV import2024-04-19T19:49:35Z<p>CSV import</p>
<p><b>New page</b></p><div>[[File:Geode_inside_outside.jpg|Geode inside outside|thumb]] [[File:Chalcedon_Maroko_Sidi_Rahal.JPG|Chalcedon Maroko Sidi Rahal|thumb|left]] [[File:Amethyst_and_drusy_quartz_cathedrals_in_Crystal_Mountain_Museum.jpg|Amethyst and drusy quartz cathedrals in Crystal Mountain Museum|thumb|left]] '''Geodes''' are geological secondary formations within sedimentary and volcanic rocks. Geodes are essentially hollow, spherical to oblong masses of mineral matter that form from the filling of vesicles (voids) in volcanic or sedimentary rocks by minerals deposited from hydrothermal fluids or by the dissolution of sediments and precipitation of minerals from groundwater. The term "geode" is derived from the Greek word ''Geoides'', meaning "earthlike," a reference to the rounded shape of these formations.<br />
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==Formation==<br />
Geodes form in several different geological settings. One common environment is in the bubbles of volcanic rocks. Over time, these bubbles can get filled with a variety of minerals, including [[quartz]], [[calcite]], and [[amethyst]], through the action of groundwater. Another setting for geode formation is in sedimentary rocks such as limestone or dolostone, where they form as a result of the dissolution of the surrounding rock and subsequent mineral deposition from groundwater.<br />
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The process begins with the formation of a hollow in rock, which can be caused by factors such as the decomposition of organic material trapped within the rock, the dissolution of minerals by groundwater, or the presence of gas bubbles in volcanic lava. Over time, mineral-laden water seeps into the hollow and begins to deposit its mineral load. The minerals precipitate from the water, gradually filling the void. The type of mineral deposited depends largely on the chemistry of the groundwater in the area.<br />
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==Composition and Types==<br />
The outer shell of a geode is typically composed of chalcedony or another form of silica. The interior can be filled with a variety of minerals. Quartz geodes, where the interior is lined with quartz crystals, are among the most common and popular types. Other types include amethyst geodes, filled with purple amethyst crystals, and calcite geodes, which have calcite crystals inside.<br />
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==Locations==<br />
Geodes can be found in many places around the world, but they are particularly abundant in certain areas such as the Midwestern United States (especially in [[Iowa]], [[Indiana]], and [[Kentucky]]), Brazil, Uruguay, and Mexico. The Keokuk area near the intersection of Iowa, Illinois, and Missouri is famous for the high quality and abundance of its geodes, earning it the nickname "The Geode Capital of the World."<br />
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==Collecting and Use==<br />
Geodes are popular among collectors and hobbyists, who often cut them open to reveal the crystals inside. They are also used in jewelry and as decorative items. The unique and beautiful interior of geodes makes them highly sought after for these purposes.<br />
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==Conservation==<br />
While geode collecting is a popular hobby, it is important to practice responsible collecting. This includes obtaining permission to collect on private land, adhering to local regulations regarding mineral collection, and being mindful of the environmental impact of collecting activities.<br />
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[[Category:Geology]]<br />
[[Category:Minerals]]<br />
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