- Grade Level:
- Kindergarten-Adult Education (general)
- Earth Science, Geography, Geology, Hydrology, Landscapes, Science and Technology
- 25-40 minutes
- Group Size:
- Up to 36
- model, cave, Mammoth Cave
OverviewThis lesson plan is from "Making Connections: A Curriculum Guide to Mammoth Cave National Park, GrK-3", which comprises ten lessons. This is lesson 8 of that set.
Students can watch a cave form in their model landform.
Objective(s)The students will be able to:
- Work productively in small groups to make a cave
- Conceptualize how water carves or creates Mammoth Cave
BackgroundThe two basic kinds of rocks found in the Mammoth Cave area are limestone and sandstone. Limestone is the “soft” rock (more water soluble) that is dissolved more easily by water. Sandstone and shale are the rocks that are on top of the cave. They are “harder” (less water soluble) and don’t let the water soak into the cave.
The limestone was laid down in this part of Kentucky around 270-350 million years ago. At that time Kentucky was further south, close to the equator. A shallow, warm inland sea covered the land. As the animals that lived in that sea died, their hard bodies (shells) fell to the bottom of the ocean. With time and pressure the shells compacted together to form limestone. The limestone in this area is between 700-1200 feet thick. After many years of deposition the sea receded, as the continent slowly drifted north.
The next major geological period to affect the Mammoth Cave area was a glacial period. Glaciers were found to the north of Kentucky. These large glaciers began to melt and formed rivers, which flowed south. This part of Kentucky became the river’s delta. The river left behind additional sand, silt, and sediment it carried with it. This sand and silt became our caprock or the layers of sandstone and shale.
Mammoth Cave was formed when water seeped through cracks in the caprock. The water formed underground rivers that carved large cave passageways in the limestone. It has taken a lot of water and a lot of time to create Mammoth Cave.
- Modeling clay (4 oz. per student or group)
- Sugar cubes (3-6 per cave)
- Warm water
- See-through bowls (1 per student or group)
- Making the Caves Diagram Sheet*
- Clay Caves Activity Sheet*
*Available in the downloadable Lesson Plan at the top of the page.
The teacher asks the students what it takes to make a cave. The teacher writes the student’s answers on the blackboard (rocks, water, time, etc.).
The teacher then explains that there are two types of rock that make up Mammoth Cave. The one that is softer and easily dissolved by water is called limestone. The second is harder and is on top of the limestone. Since it is harder it is a good roof to Mammoth Cave, protecting it. This harder rock is sandstone and shale. It takes a lot longer for water to dissolve this sandstone caprock.
The teacher passes out a lump of clay to each student (or each group of students, approximately 4 oz.) The clay will be the sandstone in our model. The teacher also passes out 3 or 6 sugar cubes, to make different sized caves. The sugar cubes will be the softer limestone in our model.
The students flatten their clay out into a “pancake.” Then they should place the sugar cubes on the clay, so that each cube touches the other, and with at least one cube touching the edge of the clay. Then the students wrap the clay around the sugar cubes, forming a ball. The students need to make sure that at least one sugar cube is exposed. (See attached “Making of the Caves” instruction sheet.)
“Now that we have our rock layers, what do we need to turn it into a cave?” The students should respond water. Each student or group should have a small see through bowl, (cutting the top off 2 liter bottles works well). Instruct the students to put their cave in the water. The students should observe what happens.
The students may observe: 1. That nothing is happening. 2. The cave may bubble for a minute or so until the sugar starts to dissolve. (This reinforces the idea that it takes some time for a cave to form.) 3. The sugar will begin to dissolve leaving a hole behind. The students can remove their cave from the water and look at it.
The class groups back together and notes their observations on the board. The teacher asks the students to fill out their Clay Cave activity sheet.
CLOSURE: We have made models of a limestone cave. For natural places like caves to form we know it takes a long time and the right ingredients. That is why we need to take care of our special natural places.
AssessmentThe teacher is able to evaluate the students during their class discussion and by reading over their activity sheets.
It takes a long time for a cave to form. At Mammoth Cave National Park, water began to dissolve the limestone rock about 10 million years ago. Mammoth Cave is now over 400 miles long! It is the longest know cave system on our entire planet.
- A follow-up activity could be to make rock candy and talk about how that relates to the formations found inside the cave.
- The class may want to visit a cave within the Mammoth Cave region to identify the differences between the sandstone and limestone while being in the field.
- The students could find other items that would dissolve in water, that could act as models for the limestone, and other items that do not dissolve that could be models for the sandstone.