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The Larsemann Hills are a series of low rounded coastal hills along the southeastern shore of Prydz Bay, Antarctica extending for 9 nautical miles (17 km) from Dålk Glacier. They were discovered in February 1935 by Captain Klarius Mikkelsen from the whaling ship Thorshavn, sent out by Norwegian whaling magnate Lars Christensen, and given this name.[1]

Map of Larsemann Hills
Map of Larsemann Hills

The bedrock of the Larsemann Hills contains an unusually high abundance of boron and phosphate minerals and is the location of discovery of four new species of mineral. In 2014, the Stornes Peninsula within the Larsemann Hills was declared an Antarctic Specially Protected Area due to its mineral diversity.[2]


Research stations


As an Antarctic oasis the hills are the home of several Antarctic research stations.


References


  1. "Larsemann Hills". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 31 May 2013.
  2. Carson, Christopher; Grew, Edward. "Protecting the mineral treasures of Antarctica's Larsemann Hills". Earth. American Geosciences Institute. Retrieved 17 June 2017.

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



На других языках


[de] Larsemann Hills

Die Larsemann Hills (norwegisch Larsemann Fjellene) sind eine Reihe niedriger und abgerundeter und Hügel an der Ingrid-Christensen-Küste des ostantarktischen Prinzessin-Elisabeth-Lands. Sie ragen am Südufer der Prydz Bay auf und erstrecken sich ausgehend vom Dålk-Gletscher über eine Länge von 14 km. Das eisfreie Gebiet hat eine Gesamtfläche von rund 40 km².[1]
- [en] Larsemann Hills

[it] Colli Larsemann

I colli Larsemann sono una serie di basse e dolci colline disposte lungo la costa sud-orientale della baia di Prydz, lungo la costa di Ingrid Christensen, nella Terra della Principessa Elisabetta, in Antartide. Il gruppo collinare si estende verso ovest per circa 17 km a partire dal ghiacciaio Dålk e le rocce che lo compongono hanno mostrato un'insolita abbondanza di minerali fosfatici e del boro, tanto che lo studio mineralogico del luogo ha portato alla scoperta di ben quattro nuovi minerali.Proprio in virtù di questa diversità mineralogica, nel 2014 la penisola Stornes, una formazione compresa nei colli Larsemann, è stata dichiarata Area Antartica Specialmente Protetta.[1]



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