Trees contain some of nature's most accurate evidence of the past. Their growth layers, appearing as rings in the cross section of the tree trunk, record evidence of floods, droughts, insect attacks, lightning strikes, and even earthquakes.
Each year, a tree grows. The new growth is called a tree ring. How much the tree grows depends on such things as how much water was available. Because the amount of water available to the tree varies from year to year, scientists can use tree-ring patterns to reconstruct regional patterns of drought and climatic change. This field of study, known as dendrochronology, was begun in the early 1900s by an American astronomer named Andrew Ellicott Douglass.
By counting the rings of a tree, we can pretty accurately determine the age and health of the tree and the growing season of each year.

Modern dendrochronologists seldom cut down a tree to analyze its rings. Instead, core samples are extracted using a borer that's screwed into the tree and pulled out, bringing with it a straw-size sample of wood about 4 millimeters in diameter. The hole in the tree is then sealed to prevent disease.
In this activity, your teacher will give you samples that simulate tree-ring
cores.
Your group will be given four simulated tree-ring cores. The samples came from
the following sources:
Procedure
|
Sample |
Age of Tree |
Year Cut or Cored |
Year Growth Began |
|
1 |
|
1993 |
|
|
2 |
|
|
|
|
3
|
|
|
|
|
4
|
|
|
|

Figure 1: Example of pattern matching in the tree cores.
(Note that your patterns won't look like this.)
Observations and Questions
When you're finished with the activity, click on Back to Teacher Guide at the top of the page.