Making Fossil Casts
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Age/Grade
Grades 1 through 3
Objectives:
Describe how fossils that are not actual remains of the living organism form.
Create a fossil mold and cast.
Length
45 Minutes
Location
Classroom
Background
Fossils are not always the actual remains of the living organisms. Many fossils are just copies called imprints, molds or casts. Imprints are impressions made by organisms in soft mud that were preserved when the mud solidified. Imprints can be traces of an animal’s activity, rather than its actual remains. The hardened tracks of animals or the burrows of prehistoric worms in solidified mud are examples of fossil imprints.
Molds are made when organisms are totally or partially buried in mud that hardens into rock. Over time ground water may dissolve the organisms, leaving cavities shaped like their bodies. Both imprints and molds are mirror images of the organisms.
If a mold was later filled with mud or mineral material, the hardened filling is called a cast. It is a reproduction that has the same outer shape as the organism. A cast looks like the organism itself, not like its imprint. Paleontologists make casts of fossil molds by filling them with liquids, such as plaster, that harden.
Materials (per student0
Modeling clay about the size of a large walnut (Should be about twice the size of the seashell or other object to be cast)
Paper plate
Small seashell (may be purchased at a craft store) or another distinctively shaped object
Petroleum jelly, such as Vaseline
7 ounce paper cup
Plastic spoon
Plaster of Paris (available from craft store or hardware store)
Tap water
Vocabulary
Fossil
Mold
Cast
Method
Comparison -- Modeling -- Art
Procedure
Extension
The imprint in the clay and the plaster cast are both examples of how fossils form. Pressing the shell into the clay represents burying the shell in mud. In nature, the mud would have hardened into rock around the shell. Removing the shell from the clay represents how the shell dissolves over long periods of time, leaving a cavity called a mold in the rock. The mold produced is a mirror-image imprint of the shell’s outside surface. In nature, this mold would have been filled with sediment, or small particles or rock and minerals that are deposited by water, wind, or ice that hardened into rock. The Plaster of Paris, like sediment, hardened – but in a much shorter period of time. The plaster is a replacement of the shell and is called a cast.Resources
"Fossils Tell of Long Ago," by Aliki. Harper Collins: New York, 1990.
See the "Critical Issues sections of the Badlands" National Park website (http://www.nps.gov/badl/exp/issues.htm#paleontology)
| www.nps.gov/archive/badl/teacher/fossils.htm, last updated: Saturday, 21-Apr-2001 13:56:48 Eastern Daylight Time | Home Page | NPS home |