Learning target: I can describe a puzzling pattern in the ages of the oldest rocks, connect it to what I already know about rock layers, and write a first explanation that I can test later in the chapter.
Read the description of the phenomenon and study the table and the bar chart. Fill in the notice and wonder table on your own first. Then answer the questions with your partner, talking before you write. There are no wrong answers in q4 and q5; they are your first explanations, and you will come back to them at the end of the chapter to see what changed.
You will need: This worksheet, Pencil, A partner for q3 to q7
Between 1969 and 1972, Apollo astronauts carried about 382 kilograms of moon rock back to Earth. When laboratories measured the ages of the oldest pieces, the answer was about 4.4 to 4.5 billion years. Meteorites, which are pieces of asteroids that fall to Earth, measure even older: about 4.56 billion years. Scientists use those numbers to say the solar system, and Earth with it, formed about 4.5 to 4.6 billion years ago.
Here is the puzzle. Nobody has ever found a rock on Earth that old. The oldest known Earth rock, a gray banded rock from northern Canada called the Acasta Gneiss, is about 4.0 billion years old. The oldest known Earth mineral grains, tiny zircon crystals from the Jack Hills in Western Australia, are about 4.4 billion years old, but the sandstone they sit in is far younger: the grains were washed out of some older rock that no longer exists. The oldest widely accepted fossils, layered microbial mounds called stromatolites, are about 3.5 billion years old. If Earth, the moon and the asteroids formed at nearly the same time, why are Earth's oldest rocks the youngest of the group?
| Sample | Oldest measured age | Where it came from |
|---|---|---|
| Meteorites (pieces of asteroids) | about 4.56 billion years | Fell to Earth; the Canyon Diablo meteorite from Arizona is a famous example |
| Moon rocks (oldest Apollo samples) | about 4.4 to 4.5 billion years | Collected on the moon's surface by astronauts |
| Zircon mineral grains (Jack Hills, Australia) | about 4.4 billion years | Single grains inside a much younger sandstone |
| Acasta Gneiss (northern Canada) | about 4.0 billion years | The oldest known whole rock on Earth |
| Stromatolite fossils (Western Australia) | about 3.5 billion years | The oldest widely accepted evidence of life |
| Earth itself (accepted age) | about 4.54 billion years | Worked out from meteorites and moon rocks, not from any Earth rock |
| I notice (something I can see in the text, table or chart) | I wonder (a question it makes me ask) |
|---|---|
| 1 | |
| 2 | |
| 3 |
If q4 feels hard, start with one of these: 'The oldest Earth rocks are gone because ___, which could not happen on the moon because ___.' Or: 'The moon and the meteorites kept their old rocks because nothing ___ them, but on Earth ___ keeps changing the surface.' You may also draw a quick sketch of what Earth's surface does over millions of years and label it instead of writing a full paragraph.
The moon has no oceans, no rain, almost no air and no moving plates, and its surface is covered with craters that are billions of years old. Earth has only about 200 confirmed impact craters, most of them young. Predict which body has more very old rock exposed at its surface today and explain why, then suggest what that means for a scientist who wants to study the first 500 million years of the solar system. Write a short paragraph with at least two reasons.