Sample: POL1


Sample ID: POL1 [1]
Station ID: POL1
AT Num:
Volcano: St. Paul Island
Possible source: St. Paul Island
Eruption:
Collector: Winer, G. S.
Date sampled:
Sample type 1: Tephra Fall
Color:
Final unit:
Text Description: From Feeley and Winer (1999): "Polovina Hill is a cluster of several scoria cones, the largest of which is ~75 m high with a small water pond occupying the floor of the summit crater. The cone is surrounded by a ring of coarse bombs up to 1.5 m across and the surface is covered by poorly sorted ash, lapilli, blocks, and bombs. A borrow pit on the east flank of Polovina Hill exposes a small cross-section of the interior of the cone, which is characterized by poorly bedded and unconsolidated scoriaceous, red and black lapilli and bombs of various sizes ranging up to 0.5 m across. Sample POL1 is a poorly vesiculated tachylitic bomb (~25 cm across) collected near the crater rim."
Sample Location:

References Cited

[1] Evidence for fractionation of Quaternary basalts on St. Paul Island, Alaska, with implications for the development of shallow magma chambers beneath Bering Sea volcanoes, 1999

Feeley, T. C., and Winer, G. S., 1999, Evidence for fractionation of Quaternary basalts on St. Paul Island, Alaska, with implications for the development of shallow magma chambers beneath Bering Sea volcanoes: Lithos, v. 46, n. 4, p. 661-676.