Mechanical and chemical weathering are explored. Sandstone, marble, and granite, are compared. Students conclude which rock type weathers the most easily. Students conduct an erosion demonstration to observe erosion in action.
Weathering is the group of forces that change the physical and chemical make up of rock near the Earth's surface. It is the breaking down of rocks and minerals, which change how the surface of the earth looks. The materials left over after the rock breaks down combined with organic materials creates soil. Weathering is a long and very slow process. Weathering occurs through physical or chemical means.
Chemical weathering is the destruction of rock due to water and acids. This changes the chemical make up of rocks. Many times water and rain contain weak acids which react with calcium carbonate found in some rocks and break it down into salt and carbon dioxide.
In mechanical weathering the rocks don't change in their chemical makeup, just their size. The breaking down of rocks due to repeated cycles of freezing and thawing of water in its cracks is weathering. Rocks that are rubbed together by wind or water will weather. Plant roots growing up through a rock can also split and weather the rock. Once rock is weathered and broken down into smaller pieces erosion takes place.
After rocks are weathered and broken down into small pieces, it is easier for them to erode away. Erosion is the picking up or physical removal of rock particles by wind, or water in a stream or river. Animals can also cause erosion by moving from place to place.
1a. Observe simple objects, patterns, and events and report their observations.
1d. Compare things, processes, and events.
1i. Use data to construct a reasonable conclusion.
3a. Know and explain science information specified for the grade level.
4b. Describe or explain observations carefully and report with pictures,
sentences, and models.
4c. Use scientific language in oral and written communication.
5a. Cite examples of how science affects life.
Pre-lab discussion: Ask the students if rocks last forever. Discuss how weathering and erosion change the surface of our earth. Explain to students that in class they are going to greatly speed up geological time and weather rocks immensely during one class period. Look at the pictures of weathering and erosion and discuss how these processes occur naturally in our world.
Instructional procedure:
I. Chemical weathering
II. Mechanical weathering
A. Dry abrasion of rocks
B. Wet abrasion of rocks - Each group will focus on one type of rock. Be sure
that all 3 rock types are represented within the class. Make sure that when the
students are shaking the jars they are all shaking them equivalently hard or else
the results will be skewed.
What should
be observed: The water in the three containers should become
much cloudier as the amounts of shakes increased. The rocks in the three
containers should become more rounded and broken up as the number of shakes
increased. Sandstone should break down the most, then marble, then granite.
However, this depends on your source of rocks and whether the students were
consistently shaking between the different groups.
III. Freeze -- thaw weathering
What this causes in nature: Rocks are mechanically broken down due to
temperature. When rocks warm up they expand and when they cool down they
contract. This repeated cycle causes the rocks to crack. When water seeps into
the cracks it freezes, expands, and makes the cracks larger. This eventually
breaks the rocks into smaller pieces.
IV. Erosion
What this causes in nature: When ocean water continually laps against a beach
or land outcropping, the soil is picked up by the water and deposited in another
place. This causes erosion of the land near water.
What should be observed: If the students build a rock wall between the sand
and the water, less erosion of the sand should occur.
Examples can be kept overnight or longer for further observations of weathering.
Rio Tinto Hands-on Science Curriculum Team