Stalactites and stalagmites

  • Stalactites form on the ceiling of caves and grow downwards.
  • Stalagmites develop from the ground and grow upwards.
  • Both formations are speleotomes, produced by the precipitation of calcium carbonate.
  • Mineralized drops form stalactites and stalagmites through a chemical dissolution process.

Surely sometime in your life you have visited a cave.  Caves are beautiful, fascinating and unique environments on earth where we have an endemic ecosystem.  In the caves we can appreciate certain natural formations that are quite impressive for their beauty and uniqueness.  These formations are called stalactites and stalagmites.  Many people consider these geological formations as true works of art of nature.  It is something worth knowing if you have not seen it before, it will surely surprise you.  But how are stalactites and stalagmites different?  How are they formed?  We will answer all these questions throughout this article.  What are stalactites and stalagmites? Although they have similar names, there are quite remarkable differences between them.  Its formation and structure is different.  Stalactites and stalagmites have one thing in common: they are speleotomes.  This concept refers to the fact that they are mineral deposits that are formed in caves after their formation.  Speleotomes arise as a result of chemical precipitation that arises during the formation of solid elements from a solution.  Both stalactites and stalagmites originate from calcium carbonate deposits.  These formations occur in limestone caves.  It does not mean that it is not the case where it can form in some artificial or anthropic cavities originating in other different mineral deposits.  The main difference between these two formations is the location.  Each one has a different formation process than the other and, therefore, its location within a cave also changes.  We will analyze this in more detail, describing what each one is.  Stalactites We begin with the formations that originate from the ceiling.  Its growth begins at the top of the cave and goes downward.  The start of a stalactite is a drop of mineralized water.  As the drops fall, they leave traces of the calcite behind.  Calcite is a mineral that is composed of calcium carbonate, which is why it precipitates in contact with water.  Over the years, after the fall of successive mineralized drops, more and more calcite is deposited and accumulates.  When this is crowded, we see that it gets bigger and bigger and takes on different shapes.  The most common shape is the cone shape.  The most common is to see a large number of calcite cones with water precipitating from the ceiling.  The size of the cones depends on the amount of water droplets that has been circulating in that area and the time that this flow of drops has been dragging the calcite.  It could be said that stalactites are rock formations that are created from top to bottom.  In the center of the stalactite, there is a conduit through which mineral water continues to circulate.  It is this factor that differentiates them from other geological formations that have a similar appearance.  Stalagmites We now proceed to describe the stalagmites.  On the other hand, they are formations that originate from the ground and develop upwards.  Like the previous ones, stalagmites begin to form through a mineralized drop with calcite.  These falling drops accumulate calcite deposits successively.  The formations here can vary more since they do not have a central conduit like stalactites through which water droplets circulate due to the force of gravity.  One difference is that they are more massive than stalactites.  Due to the formation process, stalagmites have a more rounded shape rather than a cone shape.  It is also more common to see some with irregular formations.  The most common shapes are those straight tubular shapes called macaroni.  Other common formations are the conulitos (they have a structure like a calcified crater), pearls (with a more rounded shape) and some more.  Stalactites and stalagmites are normally facing each other.  It is common to see a stalactite above and perpendicular to it a stalagmite.  This is because the drops that precipitate from the stalactite contain traces of calcite that are deposited on the ground to form the stalagmite. How stalactites and stalagmites are formed

Speleogenesis

Let's analyze the formation process of both deposits. As mentioned before, they are formed by a process of chemical precipitation. These minerals that precipitate are dissolved in water. These formations form because the CO2 dissolved in rainwater forms calcium carbonate upon contact with limestone. Depending on the rainfall pattern and the level of water infiltration, these formations will occur sooner or later. Rainwater seeps through the ground and dissolves the limestone. As a result, these drops form these deposits. Calcium bicarbonate is highly soluble in water and is what forms upon contact with the CO2 brought by rainwater. This bicarbonate produces an outcrop where the CO2 escapes, which, upon reacting, precipitates as calcium carbonate. The calcium carbonate begins to form certain concretions around the point where the drop falls. This only occurs in stalactites, as the drops fall due to the force of gravity, which forces them to fall to the ground. Therefore, the drops eventually spill onto the ground.

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Where to see these formations

You've probably been fascinated if you've never seen these formations before (which isn't the most common). However, we're going to tell you where you can find the largest stalactite and stalagmite formations. Since they form very slowly, they only grow 2,5 cm in length, taking about 4.000 or 5.000 years to form. The largest stalactite in the world can be found in the Nerja Caves, located in the province of Malaga. It is 60 meters long and 18 meters in diameter. It took 450.000 years to fully form.

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On the other hand, the world's largest stalagmite is 67 meters tall and can be found in the Martín Infierno Cave in Cuba. I hope this information has sparked your curiosity about stalactites and stalagmites.

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