Important announcement

Dear visitor,

Please note that this OpenCourseWare platform will be replaced at the end of 2026 by a new platform (under the same url ocw.tudelft.nl).

Courses and their contents that are currently available the platform will partly be migrated. URL’s for this content will change and content might be unavailable for some time. In addition, some courses will not be available anymore.

If you are linking to specific courses on this platform (for instance for your students), please take timely measures to avoid problems with access. Possible actions are:

  • Download the materials to your local platform (laptop, server)
  • For educators only (including TU Delft lecturers): Contact us at ocw@tudelft.nl and inform us what course you are using in what context (institute, program, period of use, number of students). We will research (in collaboration with the authors of the course) and decide if we will migrate the course, and if yes, can supply you with a new url.

Thank you.

This lecture is about how to trace the material (sediment) and water from source areas to the sea following a source-to-sink approach. First the source areas are explained. Thereafter, the movement driven by gravity will be treated. In the next will be dealt with glacier movement. Subsequently, the movement driven by water is explained. This is followed by the formation or change of the river gradients. Then an explanation will be given about the flood plains. This lecture ends just before entering the sea. From this point the next lecture will go further.

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