From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
Lapilli on Kilauea

Lapilli is a size classification term for tephra, which is material that falls out of the air during a volcanic eruption or during some meteorite impacts.[1] Lapilli (singular: lapillus) means "little stones" in Latin.

By definition lapilli range from 2 to 64 mm (0.08 to 2.52 in) in diameter.[2] A pyroclastic particle greater than 64 mm in diameter is known as a volcanic bomb when molten, or a volcanic block when solid. Pyroclastic material with particles less than 2 mm in diameter is referred to as volcanic ash.[3][4]


Accretionary lapilli in the Mesoproterozoic Stac Fada Member of the Torridonian, of probable impact origin

Lapilli are spheroid-, teardrop-, dumbbell- or button-shaped droplets of molten or semi-molten lava ejected from a volcanic eruption that fall to earth while still at least partially molten. These granules are not accretionary, but instead the direct result of liquid rock cooling as it travels through the air.

Lapilli tuffs are a very common form of volcanic rock typical of rhyolite, andesite and dacite pyroclastic eruptions, where thick layers of lapilli can be deposited during a basal surge eruption. Most lapilli tuffs which remain in ancient terrains are formed by the accumulation and welding of semi-molten lapilli into what is known as a welded tuff.

The heat of the newly deposited volcanic pile tends to cause the semi-molten material to flatten out and then become welded. Welded tuff textures are distinctive (termed eutaxitic), with flattened lapilli, fiamme, blocks and bombs forming oblate to discus-shaped forms within layers. These rocks are quite indurated and tough, as opposed to non-welded lapilli tuffs, which are unconsolidated and easily eroded.

Accretionary lapilli[edit]

Rounded tephra balls are called accretionary lapilli if they consist of volcanic ash particles. Accretionary lapilli are formed in an eruption column or cloud by moisture or electrostatic forces, with the volcanic ash nucleating on some object and then accreting to it in layers before the accretionary lapillus falls from the cloud. Accretionary lapilli are like volcanic hailstones that form by the addition of concentric layers of moist ash around a central nucleus.

This texture can be confused with spherulitic and axiolitic texture.

Armoured (or cored) lapilli[edit]

These lapilli are a variety of accretionary lapilli, though they contain lithic or crystal cores coated by rinds of coarse to fine ash. Armoured lapilli only form in hydroclastic eruptions, where significant moisture is present. The vapour column contains cohesive ash which sticks to particles within it.

See also[edit]


  1. ^ Bron, K.A. (2010). "Accretionary and melt impactoclasts from the Tookoonooka impact event, Australia". In Reimold W.U. & Gibson R.L. Large Meteorite Impacts and Planetary Evolution IV. Special Paper. 465. The Geological Society of America. p. 222. ISBN 978-0-8137-2465-2. Retrieved 22 May 2011.
  2. ^ Fisher, R. V. (1961). "Proposed classification of volcaniclastic sediments and rocks". Geological Society of America Bulletin. 72 (9): 1409–1414. Bibcode:1961GSAB...72.1409F. doi:10.1130/0016-7606(1961)72[1409:PCOVSA]2.0.CO;2.
  3. ^ VHP Photo Glossary: Laplli in USGS Photo Glossary of volcano terms]
  4. ^ How Volcanoes Work

External links[edit]