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Ash Beds and a Boundary Clay: Dating a Dinosaur Dig
Grade 8 geologic time practice: date layers at a dinosaur dig with ash beds, compare fossils above and below a boundary clay and scale Earth's history.
Grade 8ScienceInteractive · Printable
Aligned toMS-ESS1-4
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What’s included
- Single worksheet
- Auto-graded online
- 1 NGSS standard
- Printable answer key
- 10 questions
- Classroom-ready
Details
- Format
- Interactive · Printable
- Grade
- Grade 8
- Subject
- Science
- Question types
- Fill in the blank, Multiple choice, Sorting, Short answer
About this worksheet
What students practice
- Students use dated ash beds and layer thickness to estimate the ages of rock layers.
- Students use fossils and a worldwide clay layer to match rock records and organize Earth's history.
How to use
Sketch the hillside layers on the board as students read Table 1. Allow calculators for Part 1 and discuss the open response as a class.
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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Ash Beds and a Boundary Clay: Dating a Dinosaur Dig
Use ash dates, fossils and a worldwide clay layer to place rocks in Earth's history.
Part 1: Reading the dig hill
Read the passage and Table 1, then answer questions 1–6.
Two Weeks in the Badlands
1Each July, a university museum runs a two-week dig in the badlands of the northern Great Plains, and it saves a few places for middle school volunteers. This year Beatriz Holmqvist, who is about to start eighth grade, joined the crew. Volunteers brushed loose rock away from bones, sifted crumbly mudstone for tiny teeth and labeled every find with the layer it came from. They worked only inside the marked quarry areas, wore hats and gloves, and left the sharp digging tools to the adult crew.
2The crew leader, Dr. Lise Marchetti, showed the volunteers a hillside where the layers lie flat and undisturbed. Partway up runs a thin, pale clay layer, only about 1 cm thick. The clay holds an unusually large amount of iridium, a metal that is rare in Earth's crust but more common in some asteroids. A clay layer with the same iridium spike, in the same position just above the youngest non-bird dinosaur fossils, has been found at many sites on several continents, both in rocks that formed on land and in rocks from the deep sea floor.
3The hillside also holds two thin beds of volcanic ash. Ash from an eruption settles over a wide area within days, and labs can measure how long ago the crystals in it formed. Table 1 lists every unit of the hillside from the top down, with the fossils the crew has found in each. Because each ash bed settled in a short time, it gives an age for one level of the hill. The layers between the ash beds can be dated only from where they sit compared with the ash.
4Geologists organize Earth's 4.6-billion-year history into a time scale. Its largest divisions are placed where the fossil record changes sharply in rocks around the world. The Paleozoic Era began about 540 million years ago, the Mesozoic Era began 252 million years ago, and the Cenozoic Era began at the time of the boundary clay and continues today. The long stretch before 540 million years ago is called Precambrian time.
5Back at the museum, Beatriz copied a list of major events from a wall display. It appears as Table 2 in Part 2.
| Unit | Position | Rock | Dinosaur fossils | Other fossils, features |
|---|---|---|---|---|
| Unit 5 (top) | 6 to 20 m above clay | Gray sandstone | None found | Mammal teeth, turtle shells, leaves |
| Ash bed Q | 6 m above clay | Volcanic ash | — | Dated 65.85 million years old |
| Unit 4 | 0 to 6 m above clay | Mudstone and coal | None found | Mammal & crocodile teeth, turtle shells |
| Boundary clay | 1 cm thick | Pale clay | None found | Rich in iridium; no fossils |
| Unit 3 | 0 to 4 m below clay | Mudstone | Triceratops bones | Mammal teeth, turtle shells |
| Ash bed P | 4 m below clay | Volcanic ash | — | Dated 66.10 million years old |
| Unit 2 | 4 to 15 m below clay | Sandstone | Duck-billed dinosaur teeth | Crocodile teeth |
| Unit 1 (bottom) | 15 to 25 m below clay | Dark shale | None found | Ammonite shells, sea clams |
About years passed between the forming of ash bed P and ash bed Q.
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