Where
Does the Water Go?
Objectives:
Students
will:
- demonstrate that
water will follow cracks in the bedrock as it travels underground.
- determine how cave
passages form along cracks in the bedrock.
Materials:
- Large, flat container
(at least 3inches deep) filled with water, then frozen
- Cookie sheet (with
raised edges) or brownie/lasagna pan
- Hammer or rock
- Hot water
Procedure:
- Turn the container
upside down and empty the block of ice onto the cookie sheet. (Dipping
it in warm water will loosen the ice.)
- Tell the class
that the block of ice represents limestone.
- Hit the block
of ice once or twice with the hammer. What happens? Ask the class how
limestone might become cracked in the natural world. Discuss cracking
due to uplift and major earthquakes.
- Review with the
students where rainwater can go once it hits the ground. (Some will
evaporate, some will run along the surface into watersheds, and some
will seep into the ground.) What happens to the water when it seeps
through the soil? Review carbonic acid formation. What happens when
this carbonic acid reaches the bedrock? Review the concept of limestone
dissolution.
- How do the students
think the carbonic acid will travel through the limestone? What route
will it take? Use the cracked ice as an example. The acidic water should
flow preferentially through the cracks.
- Raise one end
of the cookie sheet and support it with a book. Pour hot water over
the ice at the high end. Where does the water go? How does it travel?
Watch as the water dissolves the ice, just as carbonic acid dissolves
limestone. The resulting "cave" passages are formed along the pre-existing
cracks. In the earth, does the water enter only from the high end of
the rock? Chances are the water will drain over the earth equally as
though the water was being poured over the top of the whole ice sheet.
Raising the sheet represents a hill or mountain area where water will
flow at the top and collect at the bottom, or the valley.
- Discuss how caves
form in the natural world. There are several kinds of formation processes:
stream erosion, lava tubes, sea caves, ice caves, acid formed caves,
etc. What types of caves will form in extensively cracked limestone?
What is an example of this? (Wind Cave is an excellent example being 110.90
miles long under only one square mile of surface).
This activity is
available as an Adobe PDF.
|
Caves
& Karst
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