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The Kyle Hills (77°30′S 169°2′E) are a prominent group of volcanic cones, hills, ridges, and peaks that occupy the eastern part of Ross Island, Antarctica, between Mount Terror and Cape Crozier. The hills extend east–west for 8 nautical miles (15 km), rising from sea level at Cape Crozier to about 2,600 metres (8,500 ft) in Mount McIntosh at the western end of the group. Local relief of features is on the order of 200 metres (660 ft).

The hills were named by the Advisory Committee on Antarctic Names (2000) after Philip R. Kyle, Professor of Geochemistry at the New Mexico Institute of Mining and Technology, Socorro, who worked extensively in Antarctica over 28 field seasons, 1969–2000, completing six seasons under New Zealand Antarctic Research Program auspices, 1969–76. He was principal investigator on numerous National Science Foundation research projects in 23 seasons of field work under United States Antarctic Program auspices, 1977–2000, with focus on long-term research of the volcano Mount Erebus, and was in charge of the Mount Erebus Volcano Observatory, 2000.[1]

References

 This article incorporates public domain material from the United States Geological Survey document: "Kyle Hills". (content from the Geographic Names Information System)

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[de] Kyle Hills

Die Kyle Hills sind eine markante Gruppe von Vulkankegeln, Hügeln, Bergkämmen und Gipfeln, die den östlichen Teil der antarktischen Ross-Insel zwischen Mount Terror und dem Kap Crozier einnehmen. Die Ostwestausdehnung des Gebirges beträgt 13 km. Vom Kap Crozier auf Meereshöhe steigen sie bis zum Mount McIntosh im Westen auf etwa 2600 m an. Die lokale Reliefhöhe zwischen den einzelnen Formationen beträgt etwa 200 m.

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- [en] Kyle Hills

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