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Pyroclastic fall

deposit of material ejected from a volcanic eruption

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 9, 2026
Entity authorityQ2120004
Source-derived summary

A pyroclastic fall deposit is a uniform deposit of material which has been ejected from a volcanic eruption or plume such as an ash fall or tuff. Pyroclastic fallout deposits are a result of:

Ballistic transport of ejecta such as volcanic blocks, volcanic bombs and lapilli from volcanic explosions

Deposition of material from convective clouds associated with pyroclastic flows such as coignimbrite falls

Ejecta carried in gas streaming from a vent. The material under the action of gravity will settle out from an eruption plume or eruption column

Ejecta settling from an eruptive plume or eruption column that is displaced laterally by wind currents and is dispersed over great distances

Structures

The deposits of pyroclastic falls follow a well sorted and well bedded trend. They exhibit mantle bedding—the deposits directly overlie pre-existing topography and maintain a uniform thickness over relatively short distances. Sorting by size is more pronounced than pyroclastic surge or pyroclastic flows. Early settling of crystals and lithic fragments near an eruptive vent and of glassy fragments further away is a common trend witnessed during many eruptions. The St Vincent eruption in 1902 ejected a large eruption column which when settled near the vent contained 73% crystals, and ash deposited in Jamaica 1,600 km away consisted entirely of glass dust.

Dispersal

The distribution of pyroclastic ash depends largely on the direction of wind at intermediate and high altitudes between approximately 4.5 – 13 km. The general trend of pyroclastic dispersal is shown using isopachs (which are analogous to topographic map contours though they illustrate lines of equal thickness rather than elevation) and show the dispersal as elongated with wind direction.

The Krakatoa (Indonesia) eruption of 1883 produced an eruption column which rose to more than 50 km.

Editorial summary

“Pyroclastic fall” enters the record as deposit of material ejected from a volcanic eruption. Crown Archives preserves that source wording while asking what Pyroclastic, fall and deposit can confirm, complicate or overturn.

Editorial reviewA concise reference frame for defining the subject, testing terminology and identifying the institution closest to the evidence. The current lead gives the account dated anchors—1902, 1883—that can be checked directly. The selected authority fields contribute no independent date. Its strongest next move is a source search built around Pyroclastic, fall and deposit.
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“Pyroclastic fall” is worth following because a concise public description often conceals a longer documentary argument. Here, Pyroclastic, fall and deposit provides the most credible route into that argument.

Evidence profile

The citation trail is more important than the brevity of the summary: it shows where individual claims can be examined in context. The source revision retrieved here is dated Jul 9, 2026. The linked authority identifier is Q2120004. None of the 0 selected statements returned an explicit reference. The first chronological checks are 1902 and 1883.

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Source & attribution

This entry incorporates text from Pyroclastic fall” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.