Gunung Andrus
Andrus
Gunung api perisai · Antarctica · 2978 m

- Tipe
- Gunung api perisai
- Negara
- Antarctica
- Wilayah
- Antarktika & Scotia / Western Antarctica Volcanic Province
- Ketinggian
- 2978 m
- Koordinat
- -75.800, -132.330
- Letusan terakhir
- Tidak diketahui
- Kondisi tektonik
- Intraplate / Continental crust (> 25 km)
- Bentuk lahan
- Shield
- Batuan utama
- Trachyte / Trachydacite
Ringkasan geologi
Three coalescing trachytic shield volcanoes with a combined volume of 252 km3 formed during the Miocene along a N-S line in the Ames Range of western Marie Byrd Land. The youngest and best exposed is Mount Andrus, the southernmost volcano, where late-stage volcanic activity resumed during the late-Pleistocene or Holocene (Gonzalez-Ferran and Gonzalez-Bonorino 1972, LeMasurier and Thomson 1990). A distinct 4.5-km-wide caldera truncates the summit of Mount Andrus. Weak fumarolic activity was observed in 1977 at Mount Kauffman, the northernmost volcano, which also has a morphologically distinct 3-km-wide summit caldera.
Ringkasan Wikipedia
Ringkasan InggrisMount Andrus is a peak 2 nautical miles southeast of Mount Boennighausen in the southeast extremity of the Ames Range, in Marie Byrd Land, Antarctica.
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