Konsei-pira
| Konsei-pira | ||
|---|---|---|
| location | Queen Maud Land , East Antarctica | |
| part of | Queen Fabiola Mountains | |
|
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| Coordinates | 71 ° 23 ′ S , 35 ° 29 ′ E | |
Konsei-Pira ( transcription of Japanese 混成ピラ , Hybrid cliff ' ) is a 300 m high, made of Migmatite existing top cliff in East Antarctic Queen Maud Land . In the Queen Fabiola Mountains it rises immediately north of the Yamato Glacier on the western edge of Mount Fukushima .
Japanese scientists took measurements in 1960 and named it in 1972.
Web links
- Konsei-pira in the Composite Gazetteer of Antarctica (English)