Jökull


Jökull - 01.12.1983, Side 22

Jökull - 01.12.1983, Side 22
Fig. 1. Icelandic Types of Basalt Volcanoes (Modified from Thorarinsson, 1959 and 1968; and from Thorarinsson and Saemundsson, 1980). NATURE OF ENVIRONMENT FORM OF FEEDER CONDUIT VONCANIC ACTIVITY DURING FORMATION SHORT FISSURE OR TUBULAR CONDUIT LONG FISSURE EFFUSIVE ACTIVITY — Landforms Subareial LAVA RING Type: Eldborg (Hnappadalssýsla) - resuldng from ílowing material LAVA SHIELD Type: Skjaldbreidur LAVA SHIELD ROW Type: Thjófahraun MIXED ACTIVITY Subglacial/ subaerial TABLE MOUNTAIN (STAPI) Type: Herdubreid SUBGLACIAL RIDGE Type: Kálfsdndar Landforms resulting from flowing material and Submarine/ Subaerial TABLE MOUNTAIN (STAPI) Type: Surtsey — Submarine SEAMOUNT Type: Jólnir SUBMARINE RIDGE Type: Eldeyjarbodi hyaloclastites Subglacial * Type: Keilir * Type: Fögrufjöll Landforms resulting from flowing and airborne material SPATTER CONE Type: Búrfell (Hafnaríjördur) SPATTER CONE ROW Types: Threngslaborgir Subaerial SCORIA CONE Type: Búdaklettur SCORIA COEN ROW Type: Vikraborgir — MIXED CONE ROW Type: Lakagígar EXPLOSIVE (OR PHREATO- MAGMATIC) ACTIVITY Landforms resulting from airborne material TEPHRA RING Type: Hveríjall TEPHRA RING ROW Type: Vatnaöldur Subaerial MAAR Type: Graenavatn MAAR ROW Type: Valagjá * These two landforms, Keilir and Fögruíjöll, for which no names are available in English, are the subglacial counterparts to a single subaerial cone and a mixed cone row, respecdvely. 1929) and Rittman’s two classification schemes for „Zentral-Vulkane" and „Linear-Vulkane“ (1936), offered the first comprehensive classifica- tion system for the volcanoes of Iceland. In 1959 (and 1960), he published the first complete classification of the 13 main types of Icelandic volcanoes. In 1968, he published a minor modifica- tion of his earlier classification scheme. Both land- form classifications were based on the relationship of the type of eruptive products (lava, lava and tephra, or tephra), number of eruptions (one or more than one), and the form of the eruptive vent 20 JÖKULL 33. ÁR
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Jökull

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