File:Large fusiform airfall lapillus (Middle Pleistocene, 670 ka; Black Rock Volcano, Millard County, Utah, USA) 2 (30901698873).jpg

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Lapillus from the Pleistocene of Utah, USA. (5.8 cm across at its widest)

Volcanic eruptions produce a large size range of rock fragments (tephra). The smallest grains (less than 1/8 of a millimeter) are referred to as "volcanic dust". Larger than that is "volcanic ash" (1/8 to 2 mm in size). Tephra that is between 2 and 64 mm in size is referred to as "lapilli", or "cinders".

Shown above is a large, fusiform, airfall lapillus composed of scoriaceous basalt. Some plagioclase feldspar phenocrysts are present. During an eruption, a spinning blob of magma was hurled into the air and developed an elongated, twisted shape.

The reddish-brown coloration is from weathering of mafic minerals (FeMg-bearing).

Age: early Middle Pleistocene (sensu traditio), 670 ka

Locality: loose piece from the north-northwestern side of Black Rock Volcano, west of the town of Kanosh, southeastern Millard County, western Utah, USA (vicinity of 38° 48' 31.39" North latitude, 112° 29' 16.88" West longitude)
Date
Source Large fusiform airfall lapillus (Middle Pleistocene, 670 ka; Black Rock Volcano, Millard County, Utah, USA) 2
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/30901698873 (archive). It was reviewed on 10 October 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

10 October 2019

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Date/TimeThumbnailDimensionsUserComment
current00:22, 10 October 2019Thumbnail for version as of 00:22, 10 October 20192,708 × 1,225 (2.17 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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