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The Global Volcanism Program has no activity reports for Liado Hayk.
The Global Volcanism Program has no Weekly Reports available for Liado Hayk.
The Global Volcanism Program has no Bulletin Reports available for Liado Hayk.
The Liado Hayk volcanic field (Liado Lake) consists of a dozen closely spaced maars and cinder cones with associated lava fields in the Awash plain NE of Dofen volcano. The morphology of the cones and maars suggested a late Pleistocene or Holocene age (Wood 1979, pers. comm.).
The Global Volcanism Program is not aware of any Holocene eruptions from Liado Hayk. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Liado Hayk page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Debado Gera Hayk||Maar||9° 31' 0" N||40° 12' 0" E|
The Global Volcanism Program has no photographs available for Liado Hayk.
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.
Wood C A, 1979. . (pers. comm.).