InTeGrate Modules and Courses >Water Science and Society > Student Materials > River flow changes over time > Temporary vs. Perennial Streams > Geomorphological
InTeGrate's Earth-focused Modules and Courses for the Undergraduate Classroom
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These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
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Geomorphological

Geomorphological Definition

A stream channel is an area of rapid conveyance of sediment and dissolved constituents during periods of flow. However, not all sediment can be transported during all flows, and this provides a mechanism and particular pattern of sediment sorting that is a hallmark of stream channels not found in terrestrial systems.

Figures 16 and 17. Example of sediment sorting in a river channel (the sand deposit and gravel bar) contrasted to unsorted sediment on the hillslope.

Photo credits: Top Panel: Image used with permission via Creative Commons: "I, Paebi CC-BY-SA-2.5-2.0-1.0], via Wikimdeia Commons". Bottom Panel: Brian Laub

These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
Explore the Collection »