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Activity 5: Stratigraphy

READING THE CHAPTERS OF TIME

Summary:

By pretending that containers of sand are rock layers, students identify how old their container of sand is by keying out the plastic dinosaurs and other prehistoric animals the sand contains.

Instructional Method: Activity

Goal:

  • Introduce the concept of stratigraphy through identification of dinosaur and other prehistoric animal fossils and show how fossils are invaluable in determining the age of rock layers.

Objectives: Students will be able to:

  • Distinguish index fossils.
  • Use fossils to determine rock ages.

Time:

Setup: 60 min
Activity: 45 min

Materials Needed:

Vocabulary:

absence

fold

paleontologist

abundance

fossil

prehistoric

chronology

geologist

species

dinosaur

index fossil

stratigraphy

erosion

Law of Superpostion

unconformity

fault

Law of Uniformitarianism



Background:

Stratigraphy is the study of rock layers and their relative ages. In geology, the Law of Superposition suggests that rocks in the deepest layers are older than the rocks near the surface. Therefore rock layers can be thought of as pages in a history book that was written backwards with the most current events in the front and the most ancient history in the back. However, various geologic forces can disrupt rock sequence chronology.

When erosion removes layers near the surface, and later in time more layers are deposited over the exposed rock, an entire time period ends up missing from the sequence. These "missing pages" are called unconformities.

Tectonic forces like folding and faulting create especially confusing rock stratigraphy. Faults mix up rock sequences. Imagine taking a book, cutting it in half and gluing the right half on top of the left half. Now as you read down through the book you eventually encounter pages in the wrong order (first the right half and then much later the corresponding left half).

Folding occurs when rock layers are bent upwards and downwards like waves. When enough force squishes the folds, they can flop over on to each other in the same manner waves do as they approach a beach. When this happens entire portions of a rock sequence can be turned upside down. It's like cutting out the middle of your history book, flipping the cut section over and then gluing it back. Now if you were to read this history book you might think that Christopher Columbus sailed to the New World before the Pilgrims arrived in New England but after Neil Armstrong landed on the Moon!

If you think that is confusing, now imagine folding, faulting, and eroding the same history book several times. Only then would you truly have typical geologic stratigraphy!

One of the main reasons geologists study fossils is to help them sort out all the confusion that can occur in studying rock sequences. Long before radioactive dating was used to tell ages, geologist were using fossils to age rock layers. Even today a rock layer with a lot of different fossils can be more precisely aged (and less expensively) by a knowledgeable paleontologist than it can be by uranium dating.

In the last 3 billion years, billions of different species have come and gone - far too many for one person to know them all. This is why some paleontologists specialize on the plants and animals of a particular time period, while others study a single type of plant or animal and how it evolved and/or went extinct over several time periods. What makes fossils so useful to aging rock is that an individual species seldom lasts more than 2 million years; it either evolves into a new species or goes extinct. When paleontologists compare the temporal overlap of several fossils at once, looking for presence, abundance, and absence, they can more precisely pinpoint the exact age of a rock layer.

The best kinds of fossils for stratigraphy are those that are found world wide, are abundant within every location in which they exist, are easily preserved, and are formed from animals which lived in several different environments and evolved into new forms quickly or went extinct suddenly. These kinds of fossils are called index fossils.

In this activity we will use toy examples of real fossils to age imaginary rock layers. You will be provided a list of fossils and their ages to help you with the task.

Instructional Procedures:

  1. Present background information.
  2. Fill containers with sand. Identify which container is going to represent a specific time period.
  3. Consult Prehistoric Animal Chronology Key and bury all appropriate and available toy animals into the sand of corresponding containers - see photos.
  4. Pass out a completed container to each student (or group of students).
  5. Instruct students to excavate sand for animals, and then use the key to try to figure out what kinds of animals they have and what time period their container represents.
  6. Once all students have correctly identified their container, have the entire class try to stack the containers from oldest to youngest.
  7. Next demonstrate, while encouraging inquiry from students, how combinations of erosion, faulting, and folding could mix up the sequence, and how by going back to fossil stratigraphy the confusion could be sorted out.

Discussion:

Discuss with the kids which prehistoric animals were the most and least successful and why (based on the time periods they spanned). Discuss how finding a new fossil, never before discovered, is very exciting and helpful because it helps geologists more accurately go back and re-evaluate stratigraphies constructed before the discovery was made. Discuss what kinds of skills and subjects would be good to study in school for somebody interested in a career in geology or paleontology.

Variations:

Instead of searching for and purchasing authentic small plastic dinosaurs, print, laminate, and cut out a complete set of fossils from the download file.

Extension:

  • Arrange some containers (based on prehistoric animals you place in them) so that they accurately reflect more than one time period. Arrange some containers so that 2 or more containers are from the same time period. Arrange the overall selection of containers so that some time periods are not represented by any containers. These variations make more realistic and challenging stratigraphy.
  • Cut the plastic dinosaurs and prehistoric animals into 2 or 3 pieces and only put 1-2 pieces in the containers. Also try adding toys not on the Key (perhaps an army man or a pokemon) and have the kids treat it as a new fossil discovery. This more accurately shows what little information paleontologist have to work with, and increases the students use of their detective skills.
  • Have the students research and give an oral presentation on either a particular dinosaur from their container and/or the time period that their container represents.

Included National Parks and other sites:

Agate Fossil Beds National Monument
Alibates Flint Quarries National Monument
Dinosaur National Monument
Florissant Fossil Beds National Monument
Fossil Butte National Monument
Grand Staircase-Escalante National Monument
Hagerman Fossil Beds National Monument
John Day Fossil Bed National Monument
Petrified Forest National Park

Photos:

allosaurus neanderthal woolly rhino
anklyosaurus nothorynchous Time Period set 1
apatosaurus pachycephalosaurus Time Period set 2
archaeopteryx parasolophus Time Period set 3
brachiosaurus plateosaurus Time Period set 4
crocodile plesiosaurus Time Period set 5
cynognathus polacanthus Time Period set 6
dilophosaurus protoceratops Time Period set 7
dimatryma pterodon Time Period set 8
dimetrodon raptor Time Period set 9
diplodocus sabertooth Time Period set 10
duckbill shark Time Period set 11
edmontosaurus spinosaurus Time Period set 12
horse stegosaurus Time Period set 13
ichthyosaurus styracosaurus Time Period set 14
iguanadon triceratops Time Period set 15
mammoth turtle Containers with animals
moropus tyrannosaurus Containers with animals stacked

Utah Science Core:

Kindergarten Standard 2 Objective 1
4th Grade Standard 4 Objective 1,2

 

Did You Know?

small herd of Pronghorn Antelope

Pronghorn, once roaming the plains of North America in numbers second only to Bison, can be found at Bryce Canyon National Park. They are the fastest land mammal on the continent and only the second fastest mammalian runner in the whole world, reaching speeds of up to 60 mph! More...