Pat Suggate
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Pat Suggate CNZM |
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|---|---|
| Born | Richard Patrick Suggate 17 March 1922 Islington, London, England |
| Died | 16 June 2016 (aged 94) Wellington, New Zealand |
| Fields | Geology |
| Institutions | New Zealand Geological Survey |
| Alma mater | University of Oxford |
| Notable awards |
FRSNZ (1963) Hutton Medal (1983) McKay Hammer (2001) CNZM (2003) |
| Spouse | Olwyn Daphne Reynolds (m. 1944; d. 2012) |
Richard Patrick "Pat" Suggate CNZM (17 March 1922 – 16 June 2016) was a New Zealand geologist, known for his research into coal properties and coal rank, and into the advances and retreats of New Zealand's glaciers. From 1974 to 1986 he served as director of the New Zealand Geological Survey.
Born in Islington, London, England, on 17 March 1922, Suggate was the son of Leonard Suggate and Florence Burden. He was educated at the University of Oxford, graduating with a Master of Arts. He married Olwyn Daphne Reynolds in London on 1 November 1944. Suggate served with the Royal Army Ordnance Corps as a lieutenant during World War II.
Emigrating to New Zealand in 1947, Suggate joined the New Zealand Geological Survey. Initially based in Greymouth, he worked with Harold Wellman to investigate the coal resources around Murchison. He went on to make major contributions to geological mapping in New Zealand, and to the effect of coal rank on its properties. He showed how peat is transformed into coal when buried in sedimentary basins, and showed that coal and organic sediments are the origin of gas and oil fields in New Zealand, and not marine deposits as previously believed.
In 1961 Suggate was awarded a Doctor of Science degree by the University of New Zealand through Canterbury University College on the basis of papers submitted.
Suggate rose to become director of the New Zealand Geological Survey in 1974, retiring in 1986. However, he continued to be an active researcher, and developed the Suggate rank scheme, which is used internationally by oil exploration companies to measure the oil and gas potential of sedimentary rocks. In this period he also completed a number of geological mapping projects, and made a significant contribution to research on the advance and retreat of glaciers near Hokitika.
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