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".

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). "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.

Some have claimed that Landslip Hill is an impact crater; but reliable sources categorically deny this. Duncan Steel, of the Anglo-Australian Observatory and the University of Adelaide, has suggested that the feature is the remnant of a bolide (asteroid or comet) impact that occurred about 1200 CE. Steel supports his hypothesis with a Māori lament that, he claims, centers on raging fires from the sky, accompanied by tempestuous winds and upheavals in the earth. Others have described the feature as "600 by 900 meters wide and 130 meters deep, and surrounded by a zone of fallen trees, 40 to 80 kilometers wide, dating from eight centuries ago".

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