Abstract
Caves have been used for much more than just exploring throughout Earth's history. Caves have been used for shelter, for religious purposes, and for burial sites. They were even used for food storage, before refrigeration, because they are cool and have constant high humidity. But how are caves formed? What causes those fantastic formations in caves? How do cave formations change as you go deeper in the cave? Get ready for an adventure as you visit a local cave and learn more in this science fair project!Objective
To learn more about speleology, and to count the number of speleothems versus distance into a cave.
Introduction
What do you think about when you hear the word cave? Do you think about a large, dark, scary place like Batman's Batcave? Caves are actually places of geological wonder and they are a variety of sizes. A cave is defined as an underground void large enough for a human to enter. There are four major causes of cave formation: rainfall, lava, waves, and microbes. There are several kinds of caves, including solution caves, primary caves, sea caves, and glacier caves. Solution caves are formed by dissolution in limestone or in other kinds of soluble rock, caused by rainfall, along with groundwater mixed with carbonic acid (H2CO3) trickling down through limestone to the water table and dissolving the limestone over time. Solution caves are usually formed when the area is under the water table. The solution cave comes to light once the water tables falls. When the water table falls, secondary mineral deposits, known as speleothems, start to grow. As rainwater trickles through the limestone ceiling, it picks up carbon dioxide (CO2) and minerals, such as calcium carbonate. Calcium carbonate is also known as calcite, the main ingredient of limestone, and is derived from marine shells. Water carries the dissolved calcium carbonate through the rock where it hits the air in the cave and hardens. The hardened material collects and forms the speleothem. Stalactites, stalagmites, and helictites are all examples of speleothems.
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| Figure 1. These are examples of helictites in Jenolan Caves in Australia. Helictites seem to defy gravity because of the way they twist around. (Wikipedia, 2008.) |
Primary caves are caves that are formed at the same time as the surrounding rock. An example of this is a lava tube. Instead of dissolving rock, a lava flow will slowly solidify over itself and create a tube. Once the lava flow stops, the lava in the tube drains out, leaving behind the tube. Sea caves are formed by ocean waves hitting a weakened area of rock. Salt water is not as erosive as freshwater so the sea cave is formed by the mechanical process of the wave hitting a weakened cliffside rock.
Glacier caves are formed within a glacier. Water finds its way inside a glacier and melts the ice from within. Air movement can then help enlarge the glacier cave. Another way that glacier caves are formed is through geothermal heat from volcanic vents. An example of this is the Kverkfjoll glacier cave in Iceland. Glaciologists can study glaciers by exploring glacier caves.
![]() Click here to check out the video "Caves by Marie and Michelle" as they explore the California Cavern. This video was produced by DragonflyTV and presented by pbskidsgo.org. |
Caves do not have direct contact with sunlight. This affects the kind of food found within caves and thus, the kinds of animals you find inside. The variety of animals found in caves can be surprising. Everyone is familiar with bats, but there are also snakes that live in the caves and feed on unsuspecting bats. On the floor in some caves, cockroaches feed on the bat feces, called guano. Troglobites are animals that have evolved to live in darkness. These animals have lost the pigment in their skins and in some cases have also lost their eyes. Then there are bacteria called extremeophiles that can survive in the harsh conditions of certain caves.
In this science fair project, you will investigate your nearest cave system and count the number of speleothems you see in different rooms. Do the numbers and colors change as you move into the cave? What about sizes? This science fair project is based on a DragonflyTV episode, "Caves by Marie and Michelle." Click on the link to the right to see what they discovered in their local cave system. Be prepared to be amazed by the speleothems you see!
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| Figure 2. This shows the Giant Crystal Cave in the Naica Caves in Mexico. Note the man standing in the middle! These giant crystals are made of gypsum. (Javier Trueba/Madrid Scientific Films.) |
Terms, Concepts and Questions to Start Background Research
Bibliography
This website has in-depth information about the different kinds of caves and their formations:
This website provides a lot of information about caving, or spelunking:
This NOVA website has a good animation on how different caves were formed. The root website has information on extremeophiles, as well as some spectacular photographs of the Lechugilla Caves, named by some as the most beautiful cave on Earth.
This DVD discusses some of the animals that live in caves. It also has a segment on the Lechugilla Caves.
For help creating graphs, try this website:
Materials and Equipment
The first three items listed below are safety gear. Call the authorities in charge of the cave system that you are interested in exploring and ask what other safety items they recommend, require, and have available. You can also visit this Wikipedia article about caving to get more ideas for what you should have:
Experimental Procedure
Prior to starting this science fair project, you should do your research and become familiar with the different kinds of speleothems.
Variations
Credits
Michelle Maranowski, PhD, Science Buddies
This project is based on the following Dragonfly TV episode:
TPT. (2006). Caves by Marie and Michelle. DragonflyTV, Twin Cities Public Television. Retrieved August 28, 2008, from http://pbskids.org/dragonflytv/show/caves.html
Last edit date: 2008-11-12 11:16:00
If you like this project, you might enjoy exploring careers in Geology.
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Geoscientist Just as a doctor uses tools and techniques, like x-rays and stethoscopes, to look inside the human body, geoscientists explore deep inside a much bigger patient—planet Earth. Geoscientists seek to better understand our planet, and to discover natural resources, like water, minerals, and petroleum oil, which are used in everything from shoes, fabrics, roads, roofs, and lotions to fertilizers, food packaging, ink, roads, and CD’s. The work of geoscientists affects everyone and everything. |
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Geographer When you hear the word geography, you might think of maps and names of state capitals, but the work of geographers is much more than creating maps and identifying places. Geographers look at how people, places, and Earth are connected. They study the economy, social conditions, climate, and topography of a region to help answer questions in urban and regional planning, business, agriculture, and medicine. | |
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