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Title: Edible Rock Layers
Level: Middle School
Time: 60 minutes
KERA Goals: 2.3; 2.35
If you had a few million years, you might be able to catch a glimpse of what happens to beds of rock (called Strata) when they are folded and faulted. Unfortunately, we're not around that long. But, the good news is we can build an experiment that simulates the movement and folding and faulting of rock strata like sandstone, siltstone, limestone, and shale. Even better news is this: once you have built the experiment and have demonstrated how it works, you can eat it!! Yes, eat it!
Once your formation has set, take a look through the side of the dish. You've created in an afternoon a series of strata that would take millions of years to form in nature.
Where are the oldest gelatin strata? Right. On the bottom. And the youngest? On top.
One thing you'll notice is that the banana or fruit cocktail "fossils" are hidden away under a number of other layers. How will they ever be found? Fortunately, things don't get as soft as gelatin, but they do stretch and bend and even break just like the gelatin layers when they are subjected to the heat and pressure generated by the earth.
|There are a number of different ways that our fossils can work their way to the top of the pile. Cut a 4-inch by 4 inch square of the formation, and you'll see how this might happen.|
|Uplifting. First, there are tremendous pressures building up inside the earth. These pressures form mountain ranges, and at the same time they twist flat strata into all sorts of bizarre shapes. Slide a knife under the center of your gelatin square and lift. The strata will bend so far and finally break. Once the pieces are standing on end, you'll see something interesting - one edge of the sandstone with the fossils is now on the surface. If a couple of miniature paleontologists happened to wander across this area right now, they'd probably discover some really tasty fossils!|
|Overthrust. There's another way that strata can get mixed up. Cut another square of gelatin. Gently and evenly push in from opposite sides of the square so that the center rises up and one half flops over on the other half. When this happens in the earth, geologists call it an overthrust.|
One interesting thing. Notice that the older strata are no longer under younger ones. In fact, half of the youngest stratum is on the very bottom. Geologists must study rock strata very carefully to determine their relative ages.
|Faulting. The surface of the earth is full of big cracks called faults. Sometimes the land on one side of the fault will be uplifted, or raised, above the land on the other side. This is one way that fossils can work their way to the surface. |
You can demonstrate the effects of faulting with another square of gelatin. Slice the square into two parts with a spatula. Then use the spatula to lift up one half. If it is raised high enough, the layer containing your fossil bananas will be exposed.
|Erosion. Fortunately for paleontologists (geologists who study fossils), sedimentary rocks are constantly being worn away (eroded) from above by wind and rain, so fossils are constantly being uncovered, We can demonstrate with a cup of warm water and another square of stratified gelatin.|
Place the gelatin on the paper towel on the plate. Tilt the plate over a sink or bowl, which will catch the water, and slowly pour a stream of warm water on one edge. Gradually, the top layers will melt away, exposing the fossil layer.
The wind also erodes sediments. To show this, take a blow dryer, turn it to warm, and aim it at a square of gelatin. In a few minutes the top layers will begin to dissolve. Soon fossils will be uncovered. (Of course, in nature the rocks don't melt. They're just slowly broken down and carried away).
Notice how small pieces of fruit flow out with the melting gelatin. This happens with real fossils too. When paleontologists find a few small bone or shell fragments lying on the ground (which they call float), they often find the rest of the fossil by looking in the rocks directly above it.
Marker beds: Coal beds like the one formed by your graham crackers are very important to paleontologists because they can be seen very easily. A gelatin geologist looking at your formation, for example, could always be sure that wherever she spotted graham crackers she would also be likely to find bananas or fruit cocktail in the next layer. Real fossil hunters often use the dark black coal beds as "markers" because they are easy to spot among all the light gray and brown layers. By knowing where the fossil-rich strata are in relation to the coal, they can zero in on the areas where they are most likely to find fossils. Coal beds are also great places to find fossils because coal formed from decaying plants in swampy areas. Huge fossilized tree trunks have been found in association with coal beds.
Well now, in an hour's time and in the space of a glass pan, you have witnessed a simulation of what happens when sedimentary rocks are formed, and what happens to them when they are acted upon by the forces of nature. These forces have included uplifting, faulting, and erosion. You have been able to make observations that are similar to what geologists and paleontologists see when they work in the field.
When you have completed all demonstrations and experiments on your "gelatin layer cake," cut the remaining gelatin into sections and serve to the class.
Provided by The Society for Mining, Metallurgy, and Exploration, Inc.