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- W2113523077 abstract "Abstract On 10 October 1978, a landslide on the coast near Mt Vulcan, North Canterbury, New Zealand, was observed taking place, at high tide, by 2 fishermen. A 4 ha block of massive sandstone, 10 m thick, slid down an impermeable clayey siltstone layer dipping seaward at 22°. The main scarp was formed where the dip of this layer steepened abruptly to 60°. Most of the block slid intact, but, as it passed over the beach, the foot broke into a series of blocks 1 m wide, and its underlying part and edges disintegrated completely. The slow draining nature of the massive sandstone suggests that heavy rainfall (twice normal) of all the preceding 6 months contributed to the failure. More surface water probably gained access to the block from the bedding plane parting that formed the main scarp, than by direct percolation from above. Although there was no seismic disturbance at the time of the slide, earlier earthquakes may have contributed to instability by initiating creep displacement on the bedding plane, and consequent parting. High tide increased buoyancy at the toe and may have reduced frictional forces there." @default.
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- W2113523077 date "1982-10-01" @default.
- W2113523077 modified "2023-09-26" @default.
- W2113523077 title "A bedding-plane landslide near Mt Vulcan, North Canterbury" @default.
- W2113523077 cites W1555930968 @default.
- W2113523077 doi "https://doi.org/10.1080/00288306.1982.10421506" @default.
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