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These links and readings are provided to support the Sedimentology module at the University of Derby, and are in addition to the classes, and the course and practical notes available from the University of Derby web site. Topics are not necessarily given in exactly the same order as in the course.
Textbook references are to:
TUCKER, M.E. 2001. Sedimentary Petrology: an introduction to the origin of sedimentary rocks. 3rd edition. Blackwell Scientific Publications.
WALKER, R.G. & JAMES, N.P. 1992. Facies Models: Response to Sea Level Change. Geological Association of Canada.
Sediment transport and sedimentary structures
Topic
Bedforms and sedimentary structures
Reading
- Tucker, chapter 2, section 2.3; chapter 3, section 3.2
Online lectures, tutorials & reading
Images
Erosional structures
- Apologies - a lot of the links below have moved, and need to be updated
- Flutes
- Grooves
- Rip-up clasts
- Channels
Depositional structures
- Modern ripple migration
- Tidal ripples and dunes
- Cross-bedded shells
- Upper flow regime
- Graded bedding in turbidites (Bouma A), southern California (NMT)
- .
Post-depositional structures
- Loads
- Loaded flute
- Flame structures
- Slumping
- Soft sediment folds in Quaternary sediments, southern California. Note undeformed overlying strata (NMT)
- Slumping in aeolian sands and sandstones
- Desiccation crack
[Image credits: BSRG - British Sedimentological Research Group; NMT - P.Mozley, Earth and Environmental Sciences, New Mexico Tech]
Video, audio
Watch all of these movies, and make notes on how the various bedform types develop.
- Current ripples and dunes: watch the movies (large files)
- Current ripple migration and climbing ripples: read the text, then watch the movie (large file)
- Current ripples: read the text, then watch the movie (very large file)
- Upper flow regime plane beds: read the text, then watch the movie (large file)
- Wave ripples: read the text, then watch the movie (large file)
Quizzes and tests
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This page is maintained by . Last updated 10 February, 2011 17:40