Grade Level:
5-8
Objective:
To learn what sand reveals about the process of erosion.
Methods:
Investigate a variety of sand types.
Materials:
[Note: Sand guide, data sheet and story sheet are PDF files. If you
do not have the free
Acrobat Reader, download it.]
*Note to teacher: You will need two samples of sand.
For the first (Sample A), any sand sample collected along a river's
edge will work. The higher the quartz content, the easier it will be
for the students to identify. For the second (Sample B), any biotic
sand containing shells, coral, etc. will do. These are most often collected
along island beaches.
Time Needed:
One to two class periods
Content Background:
See About Sand
Assessment:
Students complete the Sand Data and Sand Story Sheets
Brainstorm
with your students:
- What does sand look like?
- What is sand made of?
- Where do you find sand?
- Where does sand come from?
Distribute sand samples:
Have students look at sand
sample A and guide them in their observations by asking:
- How do the grains differ
from each other?
- Is the sand a single
color or many colors?
- Is the sand all one
thing or a mixture of many things?
- Can you determine what
the sand is composed of?
- Are all grains the
same size, texture or shape?
- How can each of these
differences be used to learn about the sand?
- Where did the sand
come from?
- How did it get to where
it was collected?
This can lead to a good
review of the rock cycle and concepts of weathering, erosion, transport,
and deposition (sedimentation). For instance, if the sand comes from
rock fragments and minerals, how does the rock get broken up? (physical
and chemical weathering) How do grains of sand get smooth and
round? (mechanical abrasion during transport) Why is some sand
large-grained or coarse? (less erosive processes or time) Why
is some sand very fine-grained? (greater exposure to erosive processes
or time) What do you think you can tell about the history of this
sand? (parent material, weathering and transport processes, approximate
age)
For the teacher:
Sample A was collected
along the banks of a riverbed. It is completely abiotic in nature
and is produced by the wearing down of different kinds of rocks and
minerals. It is mostly quartz (clear grains) which is harder than
other rocks, so it remains after softer rocks have eroded away. The
grains are mostly rounded, smooth, and polished, indicating that it
was eroded by water. It is fairly well sorted for size. Since sorting
and rounding all take time, it has probably traveled some distance
from its original source. Its origin is continental rock.
Now look at sand sample
B. Compare it to sample A for angularity, sorting and grain size,
color, texture and composition. How is it different?
For the teacher:
Sample B is mostly white
in color with some pink. There are bits of shell and coral therefore
the sand is mostly biotic in nature. This sand is not well sorted
by size and the grains are angular and coarse and it is therefore
of relatively recent origin. This sand has not traveled far and is
therefore quite close to its origin. It is island sand.
Give students the Sand
Guide and explain how to classify sand by it size, its composition,
and its angularity. Remind them that the appearance of the sand can
give us clues about its history. Their task will be to examine sand
from different localities and to fill out a Sand Data Sheet for each
different sample.
Top