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The geomorphology of the Broadmarsh-Elderslie area : with special reference to hillslope morphology

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McLaren, RG (1971) The geomorphology of the Broadmarsh-Elderslie area : with special reference to hillslope morphology. Honours thesis, University of Tasmania.

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Abstract

The morphology of the Broadmarsh-Elderslie area is very
largely controlled by lithology and structure - variations
in topography, st.re am pattern, and valley and channel
morphology are shown to be closely related to bedrock
changes.
Hillslope morphology is examined in detail. Dolerite
slopes decline by extending basal slopes with accumulated
debris eroded from the summit sections. Differential
protection by vegetation is held to be the main reason for
the differences in form and rate of erosion on north - and southfacing
slopes.
Alluvial terraces can be correlated only within
individual segments of the valley producing a 'ponded' effect.
When casually observed in the field, the channel of the
Jordan River is a picture of disorder. To the contrary, an
analysis of width-depth ratios reveals no significant
variations in channel form.
Large valley meanders, extensive alluvial fans and aprons,
and aeolian deposits provide evidence of marked variations in
former climatic conditions.

Item Type: Thesis (Honours)
Additional Information:

Copyright 1971 the Author. - The University is continuing to endeavour to trace the copyright owner(s) and in the meantime this item has been reproduced here in good faith. We would be pleased to hear from the copyright owner(s).

Date Deposited: 23 Jun 2012 12:49
Last Modified: 11 Mar 2016 05:56
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