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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Landslip Hill ： ウィキペディア英語版 Landslip Hill Landslip Hill is located on the boundary of Southland and Otago, in the South Island of New Zealand, between Tapanui and Pukerau. It is a debris flow feature associated with the Manuherikia Group of fluvial quartz sandstones. Geologists have described the fossil-bearing rocks as forming part of a sequence of "siliclastic fluvial deltaic sands, conglomerates and silty clays".〔Lindqvist, J. K. and D.T. Pocknall, 1983: Stratigraphy and palynology of Late Oligocene to Miocene lignite bearing sediments, eastern Southland. ''15th Pacific Science Congress tour guide Bf5''.〕 ==Fossil beds== The formation is well known in botanists for its prominent plant fossils of Late Oligocene to Miocene age. The first collection was made at Landslip Hill in 1862 while Sir James Hector was the director of the Geological Survey of Otago. Hector returned to the Landslip Hill deposit in 1869 to make further collections, and in 1884 he proposed the name 'Landslip Hill beds' for the quartz arenite, which is now regarded as being related to the Gore Formation following the work of Lindqvist (1983) and Pocknall (1982).〔Lindqvist, J. K. 1983: Lignite deposition in deltaic plain environments of Late Oligocene to Early Miocene Gore Formation, east Southland. ''15th Pacific Science Congress vol. 1'': abstract.〕 "The plant remains include uncompressed three-dimensional logs, stems, roots and rootlets, and a variety of fruits, some of which can be assigned to modern New Zealand taxa, and others which are no longer present in the local flora". Recent finds include fossils of the genus ''Casuarina''. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Landslip Hill」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.