Worksheet
Footprints in the Dry Riverbed: Placing Layers in Deep Time
Grade 8 geologic time practice: use a riverbank's layers, dinosaur tracks and fossil age ranges to date rocks, find missing time and explain era boundaries.
Grade 8ScienceInteractive · Printable
Aligned toMS-ESS1-4
What’s included
- Single worksheet
- Auto-graded online
- 1 NGSS standard
- Printable answer key
- 11 questions
- Classroom-ready
Details
- Format
- Interactive · Printable
- Grade
- Grade 8
- Subject
- Science
- Question types
- Fill in the blank, Multiple choice, Circle the answer, Sorting, Short answer
About this worksheet
What students practice
- Students use layer order and fossil age ranges to place rock layers in geologic eras.
- Students find a gap in the rock record and explain how era boundaries are set by changes in fossils.
- Students compute how long parts of Earth's 4.6-billion-year history lasted.
How to use
Read the passage together and model how to use one row of Table 2 before students start. Part 2 works well as a partner activity; finish with the open response.
Curriculum
NGSS standard covered
Explain how rock strata and fossils are used to organize Earth's 4.6-billion-year history.
Preview
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Footprints in the Dry Riverbed: Placing Layers in Deep Time
Use rock layers, fossil ranges and the geologic time scale to date a riverbank.
Part 1: The riverbank layers
Read the passage, Table 1 and Table 2, then answer questions 1–6.
The Summer the River Dropped
1Last summer was the driest that the wheat-growing town of Corliss had seen in decades. Cattle ponds shrank to mud, and the river that runs past the town dropped so low that a long stretch of its bed dried out. One August evening, eighth grader Beatriz Halvorsen walked the dry riverbed with her uncle, who farms wheat and raises cattle on the land above it. On a flat shelf of gray limestone, she found a line of large three-toed footprints, each longer than her forearm.
2A geologist from the state geological survey, Dr. Winifred Osei-Brandt, came out the next week to measure and photograph the tracks before the river rose again. She explained that footprints are trace fossils. They do not preserve the animal's body, but they record something it did. The tracks show that a large three-toed dinosaur once walked across soft, limy mud here. Oyster shells in the same limestone suggest that the mud lay near the edge of shallow, salty water. Later the mud hardened and was buried under more layers.
3Above the riverbed rises a bluff about 16 m high. Dr. Osei-Brandt described its layers from the top down (Table 1). The layers lie flat, one on top of another, and are not folded, tilted or broken. In a quarry 5 km away, the same track limestone sits on top of a darker limestone that does not crop out at the river, so she added it as the last row of the table. She split open loose chunks of each layer with a rock hammer, wearing safety glasses, and searched them for fossils. In layer C she found ripple marks but no fossils.
4Dr. Osei-Brandt also brought a chart of age ranges for some fossils (Table 2) and the main divisions of the geologic time scale (Table 3). Scientists divide Earth's 4.6-billion-year history into long spans of time. She told Beatriz to look closely at where the eras begin and end, and at which fossils first appear or last appear near those times. In October, heavy rains finally came, and the river covered the tracks again, but the survey's photographs keep a record of them.
| Layer | Rock | Thickness | Fossils found |
|---|---|---|---|
| A (top) | Sand and gravel | 2 m | Mammoth tooth |
| B | Gray shale | 6 m | Ammonite shells |
| C | Sandstone | 8 m | None found |
| D (riverbed) | Gray limestone | 3 m | Dinosaur tracks, oysters |
| E (quarry only) | Dark limestone | 10 m | Trilobites |
| Fossil group | First appears | Last appears |
|---|---|---|
| Trilobites | 521 Ma | 252 Ma |
| Ammonites | 409 Ma | 66 Ma |
| Dinosaurs (not birds) | 233 Ma | 66 Ma |
| Mammoths | 5 Ma | about 0.004 Ma |
Based only on its dinosaur tracks, layer D formed no more than million years ago and no less than million years ago.
- A. It formed at the same time as layer E, since both lack ammonite shells.
- B. It lies on top of layer D and under layer B, so it formed after D and before B.
- C. It formed after layer A, because the river cut through it most recently.
- D. It formed before layer D, because sandstone takes longer to form than limestone.
Layer A was laid down at least million years after layer B.
- A. Layer A sank down through the shale until it rested on top of layer B.
- B. The mammoth tooth was carried down from a younger layer that once sat above A.
- C. For a long time, layers were worn away here or were not laid down at all.
- D. Shale forms so slowly that layer B took about 61 million years to build up.
- A. The tracks were made last summer, when the dry riverbed was still soft mud.
- B. The dinosaur that made the tracks lived at the same time as the trilobites in layer E.
- C. When layer D formed, a large dinosaur walked on soft mud near shallow, salty water here.
- D. When layer D formed, this place was dry wheat land much like it is today.
Part 2: Fitting the layers into the time scale
Use Table 3 together with Tables 1 and 2 to answer questions 6–11.
| Division | Began | Ended |
|---|---|---|
| Cenozoic Era | 66 Ma | Today |
| Mesozoic Era | 252 Ma | 66 Ma |
| Paleozoic Era | 539 Ma | 252 Ma |
| Precambrian time | 4,600 Ma | 539 Ma |
| Cenozoic | Mesozoic | Paleozoic |
|---|---|---|
Precambrian time covers about % of Earth's 4,600-million-year history.
The Mesozoic Era lasted million years. That is about times as long as the Cenozoic Era so far.
- A. That is when several groups, like ammonites and dinosaurs, vanish from the rocks.
- B. That is when the oldest rocks on Earth formed, so the counting starts there.
- C. That is about halfway through Earth's history, so it splits time into two equal parts.
- D. That is when mammoths first appear, so a new era begins with them.
TrilobitesAmmonitesDinosaurs (not birds)Mammoths
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