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		<summary type="html">&lt;p&gt;Article written and Venn diagram created.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;== Stalactite vs. Stalagmite ==&lt;br /&gt;
Stalactites and stalagmites are types of speleothems, or cave formations, that are created by the deposition of minerals.&amp;lt;ref name=&amp;quot;ref1&amp;quot; /&amp;gt;&amp;lt;ref name=&amp;quot;ref2&amp;quot; /&amp;gt; The primary mineral involved in these formations is calcite, a form of calcium carbonate.&amp;lt;ref name=&amp;quot;ref3&amp;quot; /&amp;gt;&amp;lt;ref name=&amp;quot;ref4&amp;quot; /&amp;gt; They form when rainwater seeps through cracks in limestone, dissolving the calcite.&amp;lt;ref name=&amp;quot;ref1&amp;quot; /&amp;gt; As this water drips into a cave, it deposits the minerals, which build up over long periods to create these distinct structures.&amp;lt;ref name=&amp;quot;ref5&amp;quot; /&amp;gt; When a stalactite and a stalagmite grow together, they form a column.&amp;lt;ref name=&amp;quot;ref3&amp;quot; /&amp;gt;&lt;br /&gt;
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=== Comparison Table ===&lt;br /&gt;
{| class=&amp;quot;wikitable&amp;quot;&lt;br /&gt;
|-&lt;br /&gt;
! Category !! Stalactite !! Stalagmite&lt;br /&gt;
|-&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Location&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Hangs from the ceiling of a cave.&amp;lt;ref name=&amp;quot;ref3&amp;quot; /&amp;gt;&amp;lt;ref name=&amp;quot;ref1&amp;quot; /&amp;gt;&lt;br /&gt;
| Rises from the floor of a cave.&amp;lt;ref name=&amp;quot;ref3&amp;quot; /&amp;gt;&lt;br /&gt;
|-&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Growth Direction&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Grows downwards.&lt;br /&gt;
| Grows upwards.&lt;br /&gt;
|-&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Shape&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Typically icicle-shaped, long, and thin with a pointed tip.&amp;lt;ref name=&amp;quot;ref3&amp;quot; /&amp;gt;&amp;lt;ref name=&amp;quot;ref2&amp;quot; /&amp;gt; It can start as a hollow tube called a &amp;quot;soda straw&amp;quot;.&lt;br /&gt;
| Generally has a broader base and a more rounded or flattened top.&amp;lt;ref name=&amp;quot;ref2&amp;quot; /&amp;gt; It is solid and does not begin as a hollow structure.&lt;br /&gt;
|-&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Formation Process&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Formed by mineral-rich water dripping from the cave ceiling. The minerals are deposited before the water droplet falls.&amp;lt;ref name=&amp;quot;ref1&amp;quot; /&amp;gt;&lt;br /&gt;
| Formed from the mineral deposits left by water droplets that fall to the cave floor.&amp;lt;ref name=&amp;quot;ref1&amp;quot; /&amp;gt;&lt;br /&gt;
|-&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Etymology&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| From the Greek word &amp;#039;&amp;#039;stalaktos&amp;#039;&amp;#039;, meaning &amp;quot;dripping&amp;quot;.&lt;br /&gt;
| From the Greek word &amp;#039;&amp;#039;stalagmias&amp;#039;&amp;#039;, meaning &amp;quot;the result of dripping&amp;quot;.&lt;br /&gt;
|-&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Mnemonic Device&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| &amp;quot;Stalac&amp;#039;&amp;#039;&amp;#039;tites&amp;#039;&amp;#039;&amp;#039; hold on &amp;#039;&amp;#039;&amp;#039;tight&amp;#039;&amp;#039;&amp;#039; to the ceiling,&amp;quot; or contain the letter &amp;#039;c&amp;#039; for &amp;#039;ceiling&amp;#039;.&amp;lt;ref name=&amp;quot;ref5&amp;quot; /&amp;gt;&lt;br /&gt;
| &amp;quot;Stalag&amp;#039;&amp;#039;&amp;#039;mites&amp;#039;&amp;#039;&amp;#039; &amp;#039;&amp;#039;&amp;#039;might&amp;#039;&amp;#039;&amp;#039; reach the ceiling,&amp;quot; or contain the letter &amp;#039;g&amp;#039; for &amp;#039;ground&amp;#039;.&amp;lt;ref name=&amp;quot;ref5&amp;quot; /&amp;gt;&lt;br /&gt;
|}&lt;br /&gt;
&lt;br /&gt;
[[File:Venn_diagram_Differences_between_Stalactite_versus_Stalagmite_comparison.png|thumb|center|800px|alt=Venn diagram for Differences between Stalactite and Stalagmite|Venn diagram comparing Differences between Stalactite and Stalagmite]]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
=== Composition and Types ===&lt;br /&gt;
While the most common stalactites and stalagmites are speleothems found in limestone caves, these formations can be composed of other materials as well. Besides calcite, they can contain other minerals such as other carbonates, opal, chalcedony, and limonite.&amp;lt;ref name=&amp;quot;ref3&amp;quot; /&amp;gt; The color of these formations can be influenced by their mineral content, with pure calcite being white or colorless, and impurities like iron adding shades of red, orange, or black.&amp;lt;ref name=&amp;quot;ref1&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Formations similar to stalactites and stalagmites can also occur in environments other than caves. These include lava tubes, where molten lava can create &amp;quot;lava stalactites&amp;quot; or &amp;quot;lavacicles&amp;quot;. Ice stalactites, commonly known as icicles, form when water drips and freezes.&amp;lt;ref name=&amp;quot;ref4&amp;quot; /&amp;gt; Additionally, these structures can form on man-made concrete structures due to the leaching of calcium ions.&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;br /&gt;
&amp;lt;references /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
[[Category:Comparisons]]&lt;/div&gt;</summary>
		<author><name>Dwg</name></author>
		
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