geo.wikisort.org - Mountains

Keating Massif (81°0′S 156°34′E) is a rugged mainly ice-covered massif, 20 kilometres (12 mi) long, rising to approximately 2,370 metres (7,800 ft), and lying northwest. It is located at the southern edge of the head of Byrd Glacier. The feature includes Mount Fries and forms the southwestern boundary of Zeller Glacier in the Churchill Mountains of Antarctica.

Keating Massif was named in honor of New Zealander Colin Keating, who was the country's Secretary for Justice for the period 1997–2000. He had a distinguished 30-year career in the Public Service, mostly with the New Zealand Ministry of Foreign Affairs and Trade, during which time he had a significant Antarctic focus through his work in the Legal Division and then as the Deputy Secretary responsible for Multi Lateral Affairs, which included the Legal and Antarctic Divisions. Later, as the Deputy Secretary responsible for Corporate Affairs, he retained authority for the Antarctic Policy Unit, at a time of considerable changes to the organizational structure of New Zealand Antarctic institutions from 1985 through to 1993. He provided much of the intellectual input behind New Zealand's work leading to the adoption of the Environment Protocol.[1]

References

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

На других языках

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[de] Keating-Massiv

Das Keating-Massiv ist ein schroffes, hauptsächlich vereistes, 20 km langes und bis zu 2370 m hohes Bergmassiv in der antarktischen Ross Dependency. In Churchill Mountains ragt es am südlichen Rand des Kopfendes des Byrd-Gletschers auf. Zu diesem Massiv gehört Mount Fries, im Südwesten grenzt es an den Zeller-Gletscher.

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- [en] Keating Massif

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[fr] Massif Keating

Le massif Keating est un massif montagneux d'Antarctique couvert de glace de 20 km de long dont le point culminant atteint environ 2 370 m d'altitude. Il comprend le mont Fries (en). Il est situé au sud de la langue terminale du glacier Byrd et en bordure sud-ouest du glacier Zeller (en), dans la chaîne Churchill.

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