Tuya or table mountain

Tuyas form during subglacial volcanic eruptions where the eruption completely melts the overlying glacier. The result is a small shield volcano (basalt flows) capping a mass of tephra formed as the eruption melted the overlying ice.

Bibliographic Details
Other Authors: Wojtal, Steven F.
Language:unknown
Published: Oberlin College Library 1997
Subjects:
Petrology
Igneous
Iceland
Mývatn
Sudar
Table Mountain
glacier
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,1624
id ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1624
record_format openpolar
spelling ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1624 2023-05-15T16:21:36+02:00 Tuya or table mountain Wojtal, Steven F. Zone: 28, Easting: 410893, Northing: 7277100 65.60363 -16.93358 Mývatn Iceland Sudar Pingeyjarsysla Holocene 1997-08 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,1624 unknown Oberlin College Library wojtals_pcd_031 http://server15963.contentdm.oclc.org/u?/p15963coll1,1624 For research and educational use only. For all other uses please contact the Oberlin College. Geology Department 35 mm Kodachrome slide. Oberlin College. Geology Department. Petrology Igneous Iceland 1997 ftohiocolleges 2022-05-18T11:55:36Z Tuyas form during subglacial volcanic eruptions where the eruption completely melts the overlying glacier. The result is a small shield volcano (basalt flows) capping a mass of tephra formed as the eruption melted the overlying ice. Other/Unknown Material glacier Iceland Mývatn Five Colleges of Ohio Digital Collections Mývatn ENVELOPE(-16.985,-16.985,65.600,65.600) Sudar ENVELOPE(150.833,150.833,62.717,62.717) Table Mountain ENVELOPE(69.031,69.031,-48.668,-48.668)
institution Open Polar
collection Five Colleges of Ohio Digital Collections
op_collection_id ftohiocolleges
language unknown
topic Petrology
Igneous
Iceland
spellingShingle Petrology
Igneous
Iceland
Tuya or table mountain
topic_facet Petrology
Igneous
Iceland
description Tuyas form during subglacial volcanic eruptions where the eruption completely melts the overlying glacier. The result is a small shield volcano (basalt flows) capping a mass of tephra formed as the eruption melted the overlying ice.
author2 Wojtal, Steven F.
title Tuya or table mountain
title_short Tuya or table mountain
title_full Tuya or table mountain
title_fullStr Tuya or table mountain
title_full_unstemmed Tuya or table mountain
title_sort tuya or table mountain
publisher Oberlin College Library
publishDate 1997
url http://server15963.contentdm.oclc.org/u?/p15963coll1,1624
op_coverage Zone: 28, Easting: 410893, Northing: 7277100
65.60363
-16.93358
Mývatn
Iceland
Sudar Pingeyjarsysla
Holocene
long_lat ENVELOPE(-16.985,-16.985,65.600,65.600)
ENVELOPE(150.833,150.833,62.717,62.717)
ENVELOPE(69.031,69.031,-48.668,-48.668)
geographic Mývatn
Sudar
Table Mountain
geographic_facet Mývatn
Sudar
Table Mountain
genre glacier
Iceland
Mývatn
genre_facet glacier
Iceland
Mývatn
op_source 35 mm Kodachrome slide. Oberlin College. Geology Department.
op_relation wojtals_pcd_031
http://server15963.contentdm.oclc.org/u?/p15963coll1,1624
op_rights For research and educational use only. For all other uses please contact the Oberlin College. Geology Department
_version_ 1766009602023882752

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