Mendukilo Caves

Mendukilo caves

GEOLOGY

How have they been formed?
What evidence is there of their creation?

The Mendukilo caves were formed due to the erosion of the limestone rock by which they are formed by CO2, which was dissolved in the ocean water that covered the area 140 million years ago. This happened due to the fact that 140 million years ago in the town of Astitz there was a tropical ocean of which remains are still found, such as certain coral reefs located inside the cave as well as some remains of mollusks and marine animals. that previously inhabited this ocean that was in Navarre.

A karst is produced by the indirect dissolution of calcium carbonate from limestone rocks due to the action of slightly acidic waters. Water becomes acidic when it becomes enriched in carbon dioxide, for example when it passes through soil, and reacts with carbonate, forming bicarbonate, which is soluble. The surface and underground waters dissolve the rock and create galleries and caves that, due to partial subsidence, form sinkholes and, due to total subsidence, form canyons. Many other karst forms, depending on whether they occur on the surface or are geomorphological that appear in underground cavities. (Karst is a slow dissolution process that takes millions of years to develop, every hundred years the advance in the rock is approximately 5 mm, abundant especially in limestone rocks but also in others such as evaporites, such as gypsum and salt or quartzites and dolomites.
This process goes through three main stages. The first is known as juvenile where the dissolution of the limestone massif occurs creating calcium bicarbonate, then surface and underground waters penetrate into the cracks of the rocks, and finally they dissolve little by little until creating caves or other characteristic forms of this relief.)

What endokarst forms are there?

In the Mendukilo cave there are different and very varied endokarstic forms, such as:

Chasms: Deep wells formed from a fissure or crevice in the ground, generally caused by a karst erosive process or collapse of the roof of a cave or lower gallery, through which the water seeps and generates the well.

Sump: it is a type of circular sinkhole that acts as a natural drain for rainwater or for rivers or streams.

Siphons: Place where a gallery descends below the water table (Water level in an aquifer).

Galleries: Duct connecting two or more adjoining rooms, generally narrower than one room and longer.

Rooms: Cavity inside a cave formed by the widening of the horizontal ducts of the cave.

Stalagmites: Endokarstic form formed by the decantation of solutions and the accumulation of calcium carbonate in the soil of a limestone cave.

Stalactites: Endokarstic form that hangs from the roof of a limestone rock cave and is formed by the accumulation of calcium carbonate forming a kind of fang.

Geodes: Rocky cavity, normally closed, covered with crystals and other mineral materials. It is not really a mineral but a composition of magmatic, crystalline and sedimentary formations

Calcite geode: Rocky cavity almost always closed, in which the minerals are crystallized

Columns: Union between a stalactite and a stalagmite that forms a structure that connects the roof to the cave floor, formed by solid sedimented materials.

Macaroni: Straight tubes that have an inner tube. They can reach meters in length and their growth can lead to a stalactite.

Pineapples: Bulbous stalactites that form when a stalactite grows partially submerged in water, creating a thickening by acquiring matter at the tip.

Anemolytes: Endokarstic forms similar to stalactites deformed by air currents that cause the stalactite not to grow straight but with a certain curvature.

Turnips/Udders/Beets: Endokarst form generated by the union of a shield with a stalactite.

Shields: Endokarstic forms formed from the ground by water flowing from a crack in calcite, adding fine layers of this material.