Abstract
Geology and archeology are examples of historical sciences. Their practitioners rely on multiple methods for establishing dates and temporal sequences as they seek to construct a history from the available evidence. This project will show you how you can use the method of lichenometry as a method for dating relatively recent events in your area, such as the building of a stone wall, or the occurrence of a rock slide.Objective
The primary objective of this project is to develop sufficient expertise through background research so that you are able to perform a local calibration of lichen growth for lichenometry dating in your area. A secondary objective is to use this calibration to date a manmade or geological feature or disturbance in your area (for example, old stone walls, or a road cut, or a rock slide).
Introduction
A trained geologist can "read" ancient history in layers of rocks. The ability to establish dates and temporal sequences of rock formations is, in fact, essential for piecing together the earth's history. Most of the methods used for dating rocks rely on specialized equipment that can measure the presence or relative proportion of specific isotopes in the rock. In this project, you'll learn a much more accessible method for dating relatively recent events (up to hundreds of years ago, or perhaps as many as ten thousand years ago).
This method of dating rocks is known as "lichenometry." The method is used with lichen species that exhibit predictable growth behavior, and is based on measuring the size of lichen colonies on exposed rock surfaces. All else being equal, those surfaces that have been undisturbed for longer times will have colonies with larger diameters. Since lichen growth rates are dependent on local conditions, growth rates must be calibrated locally. This can be done either by measuring growth rates from year to year (obviously, you won't have time for this!), or by measuring the size of colonies with known dates of origin. The method was first developed by Roland Beschel in the 1950's, by measuring lichen diameters on gravestones of different ages. The burial dates from the gravestones were taken as the starting point for lichen growth, and used to create a graph of lichen diameter vs. age. The graph could then be used to date local gravestones or rocks with unknown dates, by measuring the diameter of lichen colonies.
You can see that this method is fairly simple, at least on the surface. All you need is a ruler and some lichen-bearing rocks with a known history, right? Think for a moment about the assumptions being made. Do lichens really grow at a steady rate? Do you have to make measurements using only one type of rock? How close must the known and unknown rocks be in order for the growth rates to be comparable? Is lichen growth rate determined by mostly by local climate, or microclimate? What about changes in climate over time? It's starting to look a little more complicated, as most things do when you start looking close enough. With careful methodology, however, lichenometry can be a reliable method for dating rocks.
Terms, Concepts and Questions to Start Background Research
To do a project using lichenometry, you should do research that enables you to understand the following terms and concepts:
You'll also need to answer the following question:
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| Rhizocarpon geographicum ("map lichen") on rock at high elevation in the Rocky Mountains. |
Bibliography
Materials and Equipment
Experimental Procedure
Variations
Credits
Andrew Olson, Ph.D., Science Buddies
Idea from Olivia Kurz, Massachusetts State Science Fair
Last edit date: 2006-01-31 14:47:52
If you like this project, you might enjoy exploring careers in Geology.
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