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Active deformation is explored in this course, introducing the criteria by which active deformation can be identified and located. The emphasis is on the interaction between tectonic and other geomorphic processes in shaping the landscape and the way in which the nature of the underlying deformation can be identified and quantified from an analysis of topography.
The interactions of active earth deformation and geomorphic processes are explored in this course, The emphasis is on how the combination of processes shape the landscape and how the nature of the underlying deformation can be identified and quantified from an analysis of topography. The discussion is not restricted to surface processes, but includes relevant applications of geophysical methods, Quaternary dating techniques and integration with underlying crustal structure. Topics will be selected from the following: i). The contribution and separation of isostatic and tectonic processes; ii). the use of geomorphic stratigraphic datum surfaces to document the growth and evolution of folds and faults; iii). methods of dating deformation rates and events and an introduction to the range of applications for this field of research; iv). basic methods of modeling tectonically and paleoclimatically forced hillslope evolution over geomorphic timescales.
Students successfully completing this course will:Have a general understanding of the interactions between tectonic and geomorphic processes, particularly the response to active folding and faulting.Have a general knowledge of the range of techniques used to investigate active deformation processes.Have some knowledge of techniques appropriate for dating active tectonic events and resulting landforms.Acquire a basic understanding of hillslope processes and the various forcing factors driving the geomorphic responses Be aware of current research trends.
Subject to approval of the Head of Department.
Jarg Pettinga
Jocelyn Campbell , Jamie Shulmeister and Philip Tonkin
James McKean (Visiting Erskine Fellow)
Assessment details will be given out at the beginning of the course and the course is expected to include a practical assignment involving up to four 1–day field trips in the April study break and comprising 40% of the total marks.
Burbank, Douglas West. , Anderson, Robert S; Tectonic geomorphology ; Blackwell Science, 2001.
Prior basic knowledge of geomorphology and structural geology terminology and the general nature of tectonic processes, particularly those of the origin of folding and faulting, is assumed.This course involves up to four days fieldwork scheduled for the April study break. A contribution of $25 per student will be payable.
Domestic fee $660.00
International Postgraduate fees
* All fees are inclusive of NZ GST or any equivalent overseas tax, and do not include any programme level discount or additional course-related expenses.
For further information see Geological Sciences .