Skip to Main Content
Book Chapter

Morphology, surface structures, and emplacement of lavas produced by Laki, A.D. 1783–1784

By
Marie-Noëlle Guilbaud
Marie-Noëlle Guilbaud
1
Volcano Dynamics Group, Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, UK
Search for other works by this author on:
Stephen Self
Stephen Self
1
Volcano Dynamics Group, Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, UK
Search for other works by this author on:
Thorvaldur Thordarson
Thorvaldur Thordarson
2
Department of Geology and Geophysics, University of Hawaii at Manoa, POST Building Room 614A, 1680 East-West Road, Honolulu, Hawaii 96822, USA
Search for other works by this author on:
Stephen Blake
Stephen Blake
3
Volcano Dynamics Group, Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, UK
Search for other works by this author on:
Published:
January 01, 2005

The A.D. 1783–1784 Laki eruption (Iceland) was one of the largest basaltic eruptions in historical times. In only 8 months, >14 km3 of lava was erupted, creating an ∼600 km2 lava flow field. The flow field presents a wide range of surface morphologies that can be subdivided into shelly, spiny, slabby, and rubbly pāhoehoe types. This report constitutes the first comprehensive description of the Laki lava flow field and links the overall flow field organization seen on aerial photographs with key textural features observed in the field. By examining the transitions between the different surface morphologies, we are able to present a conceptual model for the formation of a rubbly pāhoehoe surface during the emplacement of a lava flow. Patterns in the distribution of surface morphologies in the Laki flow field are combined with information from historic accounts to determine the impact of preexisting topography and changes in lava supply rate on flow morphology. The majority of Laki flows were initially emplaced as inflating pāhoehoe sheets with hummocky margins. These gradually developed rubbly pāhoehoe surfaces through progressive disruption of crust immediately behind the hummocky margin or at the active flow front. This sequence was repeated when fluid lava stored within the interior of the inflating sheet lobes broke through at the flow front to advance the flow. The quasi-absence of 'a'ā-type clinkery crusts shows that the lava never reached the point of continuous surface deformation by tearing of core lava at the leading edge of the flow. The Laki lavas have surface characteristics different from pāhoehoe and 'a'ā, and the term rubbly pāhoehoe is appropriate for the dominant surface texture on the Laki flow field.

You do not currently have access to this article.

Figures & Tables

Contents

GSA Special Papers

Kinematics and dynamics of lava flows

Michael Manga
Michael Manga
Search for other works by this author on:
Guido Ventura
Guido Ventura
Search for other works by this author on:
Geological Society of America
Volume
396
ISBN print:
9780813723969
Publication date:
January 01, 2005

GeoRef

References

Related

Citing Books via

Close Modal
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close Modal
Close Modal