Deltas short course: Difference between revisions

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''contributed by  J. Syvitski ''<br>
''contributed by  J. Syvitski ''<br>
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lecture reviews the difficulty of defining a delta, reviews concepts of distributary channels and avulsion that are so intrinsically important in deltas, reviews recent progress on modeling an dquantifying aggradaton in the delta plain, reviews processes in the marine domain and the concept and effect of relative sea level rise  <br>
This lecture reviews the difficulty of defining a delta, reviews concepts of distributary channels and avulsion that are so intrinsically important in deltas, reviews recent progress on modeling an quantifying aggradation in the delta plain, reviews processes in the marine domain and the concept and effect of relative sea level rise  <br>


[[Media:C1_DeltaDynamicsandTheory.ppt‎|Delta Dynamics and Theory PPT]]
[[Media:C1_DeltaDynamicsandTheory.ppt‎|Delta Dynamics and Theory PPT]]


The second lecture goes into more detail on the CMT: <br>
The second lecture discusses morphology of deltas. It reviews the classical ternary division of deltas into fluvial-dominated, wave-dominated and tidal-dominated deltas. But more complex deltas, influenced by a mix of controlling facotrs, are shown and discussed as well.
There is special emphasis on deltas during sea level fall and periglacial deltas.: <br>


[[Media:CMT_INTROAnnualMeeting2011.ppt|Introduction to CMT]]‎
[[Media:C2_Delta_Morphology.ppt|Delta Morphology PPT]]‎





Revision as of 12:21, 6 January 2014

Deltas: Dynamics, Morphology and Observing of delta processes and human impacts

contributed by J. Syvitski

This lecture reviews the difficulty of defining a delta, reviews concepts of distributary channels and avulsion that are so intrinsically important in deltas, reviews recent progress on modeling an quantifying aggradation in the delta plain, reviews processes in the marine domain and the concept and effect of relative sea level rise

Delta Dynamics and Theory PPT

The second lecture discusses morphology of deltas. It reviews the classical ternary division of deltas into fluvial-dominated, wave-dominated and tidal-dominated deltas. But more complex deltas, influenced by a mix of controlling facotrs, are shown and discussed as well. There is special emphasis on deltas during sea level fall and periglacial deltas.:

Delta Morphology PPT


A overview paper, published in the SEPM Sedimentary record of March 2011 on CSDMS and the vision of plug and play technology is posted here : PDF