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- W1995705235 abstract "The Rangitaiki Plain, eastern Bay of Plenty, New Zealand, is the geographic expression of an active continental back-arc rift known as the Taupo Volcanic Zone. The rift is characterized by tectonic subsidence at rates of 0.4–2.0 mm/year and is bounded by faults and marginal uplift at approximately 1.0 mm/year. Since 6.5 ka, the Rangitaiki Plain prograded at least 10 km, due to volcanoclastic sediment supplied by three major rivers, to reach its present location at about 1.8 ka. At this time a linear coast was formed, cliffed to the west in marine sediments and unwelded ignimbrites and extending as far east as a greywacke headland at Whakatane. In the tectonically subsiding Rangitaiki Plain, an abundant supply of sediment overwhelms the tectonic control on coastal evolution. Further east, a wide embayment at Ohiwa remained little changed from 6.5 to ca. 2 ka, when the coastline in the plain prograded as far as the Whakatane headland and longshore drift began to provide it with a substantial volume of sediment. Barrier spits formed rapidly and sedimentation has effectively closed and partially infilled the embayment. Ohiwa estuary, despite its location in the actively uplifting margin of the continental rift, remained submerged until sufficient sediment was available to contribute to the coastline-straightening process. The Bay of Plenty coastline is presently in a near-equilibrium state." @default.
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- W1995705235 date "1992-01-01" @default.
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- W1995705235 title "Holocene coastal evolution in a continental rift setting; Bay of Plenty, New Zealand" @default.
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- W1995705235 doi "https://doi.org/10.1016/1040-6182(92)90043-2" @default.
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