Caribou Tuya
id:
caribou-tuya-201-10353160
title:
Caribou Tuya
text:
Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation. Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to hyaloclastite deposits from the base upward. Locally the sections are capped by subaerial basaltic lava flows. Samples of the glassy pillow basalts and hyaloclastites along with crystalline basalt flows were
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Caribou_Tuya
date created:
date modified:
2023-09-25T05:01:18Z
main entity:
{"identifier":"Q5039522","url":"https://www.wikidata.org/entity/Q5039522"}
image:
fields total:
13
integrity:
13