Washington Geology, Volume 28, No. 3. May 2001.
by: Sherry L. Weisgarber
We think rocks last forever. The boulder we played on in our parents' front yard when we were children is still there for our grandchildren to enjoy. The rock steps to the church are still in use a hundred years later, and the gravestones in the cemetery still mark where our ancestors were laid to rest. These rocks, to us, have lasted forever. But, if you look closely, change is taking place.
This change is called weathering. The term weathering refers to the destructive processes that change the character of rock at or near the Earth's surface. There are two main types of weathering: mechanical and chemical. Processes of mechanical weathering (or physical disintegration) break up rock into smaller pieces but do not change the chemical composition. The most common; mechanical weathering processes are frost action and abrasion. The processes of chemical weathering (or rock decomposition) transform rocks and minerals exposed to water and atmospheric gases into new chemical compounds (different rocks and minerals), some of which can be dissolved away. The physical removal of weathered rock by water, ice, or wind is called erosion.
Weathering is a long, slow process, which is why we think rocks last forever. In nature, mechanical and chemical weathering typically occur together. Commonly, fractures in rocks are enlarged slowly by frost action or plant growth (as roots pry into the fractures). This action causes more surface area to be exposed to chemical agents. Chemical weathering works along contacts between mineral grains. Crystals that are tightly bound together become looser as weathering products form at their contracts. Mechanical and chemical weathering continue until the rock slowly falls apart into individual grains.
We often think of weathering as destructive and a bad thing because it ruins buildings and statues. However, as rock is destroyed, valuable products are created. The major component of soil is weathered rock. The growth of plants and the production of food is dependent on weathering. Some metallic ores, such as copper and aluminium, are concentrated into economic deposits be weathering. Dissolved products of weathering are carried in solution to the sea, where they nourish marine organisms. And finally, as rocks weather and erode, the sediment eventually becomes rock again - a sedimentary rock.
Tow experiments to illustrate the effects of mechanical and chemical weathering are presented below.
Plaster and Ice
What you need: plaster of paris, water, a small balloon, two empty pint milk cartons (bottom halves only) a freezer.
What to do: (1) Fill the balloon with water until it is the size of a ping-pong ball. Tie a knot at the end. (2) Mix water with plaster of paris until the mixture is as thick as yogurt. Pour half of the plaster in one milk carton and the other half in the other. (3) Push the balloon down into the plaster in one carton until it is about _ inch under the surface. Hold the balloon there until the plaster sets enough so that the balloon doesn't rise to the surface. (4) Let the plaster harden for about 1 hour. (5) Put both milk cartons in the freezer over night. (6) Remove the containers the next day to see what happened.
What to think about: What happened to the plaster that contained the balloon? What happened to the plaster that had no balloon? Why is there a difference? Which carton acted as a control? Why? How does this experiment show what happens when water seeps into a crack in a rock and freezes?
What should have happened: The plaster containing the balloon should have cracked as the water in the balloon froze and expanded. Explain that when the water seeps into cracks in rocks and freezes, it can eventually break rocks apart.
A Sour Trick (Chemical Weathering)
What you need: lemon juice, vinegar, medicine droppers, two pieces each of limestone, calcite, chalk, and quartz.
What to do: (1) Put a few drops of lemon juice on one piece of each of the four rock types. (2) Put a few drops of vinegar on the other piece of each of the four types.
(3) Look and listen carefully each time you add the lemon juice or the vinegar.
What to think about: What happens when you put lemon juice on each rock? What happens when you put vinegar on each rock? Did the lemon juice and vinegar act the same way on each rock? Why did some of the rocks react differently? What does this experiment have to do with weathering?
What should have happened: Lemon juice and vinegar are both weak acids. The lemon juice contains citric acid and the vinegar contains acetic acid. These mild acids can dissolve rocks that contain calcium carbonate. The lemon juice and vinegar should have bubbled or fizzed on the limestone, calcite, and chalk, which all contain calcium carbonate. There should not have been a reaction on the quartz, which does not contain calcium carbonate. Explain the water commonly contains weak acids that dissolve rocks containing calcium carbonate and other minerals.
Source: Ranger Rick's Nature Scope: Geology - The active Earth: National Wildlife Federation, 1988.
Essential science learning benchmarks/objectives
1.1 Uses properties to identify, describe and categorize weathering processes.
1.2 Understands that interactions within and among systems cause changes in matter, energy, and decomposition.
2.1 Develops abilities necessary to do scientific inquiry.
6th -10th grades
Decomposition of rocks:
Mechanical and chemical weathering; observations while conducting experiments.
Observation; hypothesizing; analysing; comparing and contrasting.
45 minutes (not including freezing time).
I HEAR AND I FORGET
I SEE AND I REMEMBER
I DO AND I UNDERSTAND
- Ancient Chinese proverb
Lesson created by Sherry L. Weisgarber
Reprinted with permission from Ohio Geology, Winter 1997, a publication of the Ohio Department of Natural Resources, Division of Geological Survey.
Permission is granted to photocopy these lessons. There is no copyright. Earth Connections No. 4.