Teach the Earth > Geomorphology > Teaching Activities > Stream Terraces

Stream Terraces

Donald T. Rodbell
Union College
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This activity was selected for the On the Cutting Edge Reviewed Teaching Collection

This activity has received positive reviews in a peer review process involving five review categories. The five categories included in the process are

  • Scientific Accuracy
  • Alignment of Learning Goals, Activities, and Assessments
  • Pedagogic Effectiveness
  • Robustness (usability and dependability of all components)
  • Completeness of the ActivitySheet web page

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This activity has benefited from input from faculty educators beyond the author through a review and suggestion process. This review took place as a part of a faculty professional development workshop where groups of faculty reviewed each others' activities and offered feedback and ideas for improvements. To learn more about the process On the Cutting Edge uses for activity review, see http://serc.carleton.edu/NAGTWorkshops/review.html.

This page first made public: Apr 18, 2008


Field work is surveying terraces along the Mohawk River and two of its tributary streams in eastern NY State. Lab write up requires students to present data graphically and to propose an hypothesis that explains the cause of episodic stream incision in the region.

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Undergraduate course in geomorphology

Skills and concepts that students must have mastered

How to recognize stream terraces
How to conduct basic surveying using a stadia rod and abney level

How the activity is situated in the course

This is a 3-week long project that is conducted as part of the fluvial geomorphology component of the course. We usually begin this project in late September when the leaves have begun to fall, so visibility in the deciduous forests is improved and students can see the flights of terraces without much difficulty.


Content/concepts goals for this activity

To have students think about a classic problem in geomorphology–that is, the response of streams to climate change and base level change. Flights of stream terraces between 0.5 and 10 m above modern stream levels are ubiquitous in the northeastern NY (and much of New England, for that matter). The factors responsible for the step wise incision of these streams are numerous and include the draining of Glacial Lake Albany, post glacial isostatic rebound, and climate change via its effects on sediment yield.

The students can see the landforms clearly, and can understand conceptually how they could have formed, but the development of a hypothesis based on field data that they have collected requires them to consider such things as whether the terraces are paired or not, whether they are convergent or divergent with the modern stream, etc. Multiple hypotheses are certainly possible, and the students are asked to develop one and to suggest ways in which it can be tested.

Higher order thinking skills goals for this activity

I have the students read the following papers to give them some background:

Bull, W.B., 1979. Threshold of critical power in streams. Geological Society of America v. 90, p. 453-464.

D. J. Merrits, K.R.V., and E. E. Wohl, 1994. Long river profiles, tectonism, and eustasy: A guide to interpreting fluvial terraces. Journal of Geophysical Research 99, 14031-14050.

Other skills goals for this activity

Students work in groups on this project, though the writing assignment is designed to be completed individually. One team of students presents their results to the class, and this I hope will generate some discussion in which all students are expected to contribute.

Description of the activity/assignment

We spend the first of three lab periods walking up a bedload-dominated stream bed that is a tributary stream to the Mohawk River. We notice the obvious flights of terraces along the stream. I ask the student to count them and walk up on them and think about how they came to be. We then think about how we might survey them, and document their presence. The students have a good idea what we're up to as we have stadia rods and abney levels. Then we go through the routine of measuring terrace heights using the modern stream as a datum. I then divide students into 3 teams and assign each team a different reach of the creek. In total we cover about 1 km., and teams are responsible for measuring the height of stream terraces above the modern stream and measuring with a tape measure their distance upstream from our starting point. On the second week we repeat this exercise on another stream, and then I compile all students data into an Excel spread sheet and ask them to do some simple calculations and plot longitudinal profiles of the modern streams, with terrace remnants plotted above the modern. They do this for both sides of each stream. They also plot a cross section of the stream valley at one point of their choosing to illustrate whether the terraces are paired or unpaired. On the final week, we tour the eastern Mohawk valley looking at much larger terraces that were produced by incision of the Mohawk, and we go to an outcrop of varves deposited in Glacial Lake Albany that crop out at the base of one of the terraces. The students thus get a sense of the large changes in base level that must have affected all the tributary streams in the region.
Has minimal/no quantitative component
Addresses student fear of quantitative aspect and/or inadequate quantitative skills

Determining whether students have met the goals

My evaluations of students work are based on their individual lab reports. Specifically, I evaluate whether they have considered multiple hypotheses for the origin of stream terraces, and whether they have done a good job of testing these hypotheses with the data they have, and whether they have proposed a reasonable means of testing the remaining hypotheses. The students who present their results to the class are also evaluated on the quality of their oral presentations.

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