Clarence River lowland floodplain : a morphostratigraphic analysis of a complex Holocene floodplain
The Clarence Holocene fluvio-estuarine basin is, in fact, a double basin (inner and outer) separated by a bedrock barrier which acts as a "double" protector for the inner basin against marine influences. The Clarence fluvio-estuarine basin was inundated by the Holocene sea-level transgression about 8,000 years B.P. and fonned mud basin with tidal deltas at the entrance of the outer basin along the present coast and also, at the northern bedrock passage of the Inner basin. The inner basin...[Show more]
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|Haq_N_1995Pt1.pdf||2.66 MB||Adobe PDF|
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|Huq_N_1995Pt3.pdf||1.24 MB||Adobe PDF|
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