Lava delta

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Lava delta of Ponta dos Biscoitos, Sant Cruz das Ribeiras, Pico Island

Lava deltas, similar to river deltas form wherever sufficient sub-aerial flows of lava enter standing bodies of water. The lava cools and breaks up as it encounters the water, with the resulting fragments filling in the adjacent seabed topography such that the flow can move further offshore sub-aerially. Lava deltas are generally associated with large-scale, effusive type basaltic volcanism.


Lava deltas are found mainly associated with volcanic islands, particularly those formed at hotspots as they produce the necessary effusive basaltic flows.

The largest lava delta systems known are associated with formation of volcanic type passive margins. Just prior to break-up along the northern Atlantic in the late Paleocene, massive eruptions occurred along the eventual line of break-up. This volcanism, part of the North Atlantic Igneous Province, led to the formation of two extensive lava escarpments, interpreted as deltas,[1] extending from the Faeroes onto the More Margin (the Faeroe-Shetland escarpment) and the Vøring escarpment on the Vøring margin, a combined distance of approximately 1,000 km (620 mi).[2][3] As these deltas were prograding into water of relatively constant depth, they were able to extend as much as 25 km (16 mi) from their original vents.[4]


Aerial view of Kamoamoa lava delta forming, Kilauea
USGS cartoon of lava delta formation

When a sub-aerial lava flow reaches the ocean (or other large body of water), contact with the water causes both rapid cooling of the lava and steam explosions that fragment it. The glassy fragments that are formed, known as hyaloclastites, fall down to the seabed forming foresets. As the seabed topography becomes infilled, the subaerial flow is able to build out. The process continues as long as the lava supply is maintained. Most lava deltas are formed by relatively low viscosity Pahoehoe type flows and the lava reaches the sea via a system of small lava tubes, their entry into the water being marked by a series of steam plumes.[5]


Newly formed lava deltas can be unstable, especially when they are building out over a steeply sloping seabed. Collapse of the frontal part of lava deltas is common during their formation, representing a hazard for any people that are watching from a solidified part of the delta and such areas are normally marked as dangerous.[6] People standing too close to the edge of an active delta are not only at risk from being thrown in the water but from the steam explosions that accompany the collapse as seawater comes into contact with the active lava tube system.


The town of Garachico, Tenerife, built on a lava delta formed during the 1706 eruption

On steep-sided volcanic islands, lava deltas make attractive sites for building and many villages and towns are located on old lava deltas, such as Garachico on Tenerife.


  1. ^ Kiørbøe, L. 1999. Stratigraphic relationships of the Lower Tertiary of the Faeroe Basalt Plateau and the Faeroe-Shetland Basin. In: Fleet, A.J. & Boldy, S.A.R. (eds) Petroleum Geology of Northwest Europe: Proceedings of the 5th Conference, Geological Society, London.
  2. ^ Berndt, C; Planke, S; Alvestad, E; Tsikalas, F; Rasmussen, T (2001), "Seismic volcanostratigraphy of the Norwegian Margin: constraints on tectonomagmatic break-up process", Journal of the Geological Society, 158 (3): 413–426, doi:10.1144/jgs.158.3.413 
  3. ^ Planke, S., and Alvestad, E., 1999. Seismic volcanostratigraphy of the extrusive breakup complexes in the northeast Atlantic: implications from ODP/DSDP drilling. In Larsen, H.C., Duncan, R.A., Allan, J.F., Brooks, K. (Eds.), Proc. ODP, Sci. Results, 163, 3–16 [Online.]
  4. ^ White, R.S., Spitzer, R., Christie, P.A.F. & iSIMM team. 2004. Seismic imaging through basalt flows on the Faroe Shelf. Presentation at Petex.
  5. ^ Mattox, Tari N; Mangan, Margaret T (1997), "Littoral hydrovolcanic explosions: A case study of lava–seawater interaction at Kilauea Volcano", Journal of Volcanology and Geothermal Research, 75: 1–17, doi:10.1016/S0377-0273(96)00048-0 
  6. ^ When Lava Enters the Sea: Growth & Collapse of Lava Deltas, Hawaiian Volcanic Observatory, USGS