Stalagmites and Stalactites

Stalactites form on the ceiling of a cave when mineral-rich water drips down and leaves behind deposits of minerals like calcium carbonate. Over time, these minerals accumulate and harden into the characteristic icicle-shaped formations.

An example of a stalactite is the formation found in caves, made of mineral deposits dripping down from the ceiling over time. These formations often have a long, cylindrical shape and can vary in size and color depending on the minerals present in the water.

They typically form in caves where they can grow undisturbed for hundreds of years. Stalagmites grow from the floor up and stalactites stick to the ceiling. Dripping water deposits minute amounts of limestone that build up over the years.

+++

You do sometimes find small, rather coarse versions growing under bridges etc.built from bricks or ashlar masonry and mortar. Here, the calcite that is their constituent mineral has been leached from the structure's mortar. However caves in limestone (the rock hosting by far the majority of caves) are the natural home for stalagmites and stalactites, and their related formations.

Stalagmites are rock formations that grow upward from the floor of a cave. They are typically cone-shaped with a pointed tip and can vary in size and shape depending on the minerals in the groundwater that drips from the ceiling of the cave. Stalagmites are created as mineral deposits accumulate over time, forming unique and often intricate patterns.

When a stalagmite and stalactite meet and grow together, they form a column or pillar. This occurs when mineral-rich water drips from the ceiling and deposits mineral material that builds up from the ground.

Yes, stalagmites are typically made of limestone. They form from mineral deposits left behind by dripping water in caves, which contain calcium carbonate. Over time, these deposits accumulate to form the stalagmites.

Stalactites are formations that hang from the ceiling of a cave and are formed by water dripping and leaving mineral deposits behind. Stalagmites are formations that grow up from the cave floor as a result of mineral deposits accumulating from water dripping onto the cave floor. Over time, stalactites and stalagmites can grow towards each other and eventually merge to form a column.

Stalagmites are formed in caves when mineral-rich water drips from the ceiling and deposits minerals on the cave floor. Over time, these mineral deposits accumulate and harden into cone-like structures known as stalagmites.

The world's largest stalactite is located in the Jeita Grotto in Lebanon. It measures at 27 feet long.

Stalagmites are formed when the stalagtite above it drips small amounts of liquid onto it and it slowly hardens and keeps forming upward. It takes about 100 years for a stalagmite to grow 1 inch.

A drip curtain is a narrow strip of fabric, often made of plastic or vinyl, that hangs vertically to direct water away from a window or door. It helps to prevent water from seeping in through gaps or cracks during rain or storms.

No, stalactites grow from the ceiling of a cavern due to mineral-rich water dripping down and leaving behind deposits that accumulate over time. Stalagmites, on the other hand, grow up from the cave floor as mineral deposits build up from dripping water.

Stalagmites grow upwards from the floor of a cave due to the accumulation of mineral-rich water dripping from the ceiling. As the water drips and evaporates, it leaves behind mineral deposits like calcite which gradually build up over time, forming the stalagmite structure. This process can take thousands of years for a stalagmite to reach significant height.

Stalactites grow from the ceiling of a cave. They are formed by mineral-rich water dripping from the cave ceiling and leaving behind deposits of minerals that accumulate over time, creating a cone-like structure.

Ice stalactites are formed when water drips downwards and freezes on the lower end of a surface, such as a roof or icicle. As more water continues to drip and freeze, the stalactite grows in size. Factors such as temperature and humidity levels can affect the formation of ice stalactites.

The tallest stalagmite in Europe is called "Hallelujah" and it is located in the Grotte de Clamouse cave in France, measuring about 70 meters (230 feet) in height.

A pillar a column or sometimes a stalagnate.

When a stalagmite and stalactite meet and grow together, they form a column.

Stalactites typically grow at a rate of 0.01 to 0.02 inches per year. It can take hundreds to thousands of years for a stalactite to grow to a noticeable size, with some of the largest ones taking tens of thousands of years to form.

True. Stalactites are mineral formations that hang from the ceiling of a cavern or cave, formed by dripping water containing minerals that slowly build up over time.

Many caves around the world report having the "world's largest stalagmite," but these are often unsupported claims.

As featured on the BBC series "Planet Earth," the largest recorded stalagmite is in the cave of Cueva San Martin Infierno, Cuba. It measures 62.2 metres (220 feet) high.

There is still the possibility of a larger stalagmite being found, as many cave systems across the world are as of yet unexplored, or have not been documented.

The only statement actually listed is not correct, at least not always. (We're really not ideally set up here for multiple choice questions.)

the answer is: Stalagmites are coned-shaped deposits.

D is correct. Stalagmites are cone-shaped deposits.

+++

As a general rule C is wrong, certainly in limestone; but Iranian cavers recently discovered a beautiful cave formed entirely by dissolution of the salt in a massive rock-salt bed; and this contains really lovely salt-crystal formations!

A more common exception is gypsum - calcium sulphate - which often appears as lovely, fine porcupine quill-like elongated crystals, on the clay which it is its mineral source.

Yes, there are various types of stalactites and stalagmites based on their composition, shape, and formation process. Some common types include soda straws, helictites, and draperies for stalactites, and pillars, shields, and coral garden for stalagmites. Each type has unique characteristics formed under specific conditions in caves.

A soda staw represents the earliest stage of stalactites. A soda straw is like a thin tube attached to the ceiling.