FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2007779478> ?p ?o ?g. }

• W2007779478 endingPage "319" @default.
• W2007779478 startingPage "299" @default.
• W2007779478 abstract "Secondary hydroeruptions occur in pyroclastic-flow deposits when water or ice is trapped beneath hot pyroclastic debris and rapidly heated to steam. These eruptions display various styles of activity including fumarolic degassing, tephra fountaining, and explosive cratering. The deposits, which occupy the layer 3 stratigraphic position on the top of pyroclastic-flow units, can be distinguished from ash-cloud material by lateral thickness variation, clast composition, and other sedimentary features. The ejecta of secondary hydroeruptions comprise a subset of hydrovolcanic pyroclastic deposits. A small secondary hydroeruption observed on the Mount St. Helens pumice plain in 1981 produced tephra that was emplaced ballistically, by deposition from base surges, and by fallout from an eruption column. Stratigraphic descriptions and grain-size analysis of the ejecta from several secondary craters on the pumice plain demonstrate that the bedforms produced by a hydroeruption change with crater diameter. In particular, craters of small diameter are surrounded by interbedded ripple-laminated ash horizons and nonstratified, fines-depleted units; large craters have ejecta ramparts comprised of coarse dunes and antidunes. These bedform changes are related to a progressive increase in eruptive energy, which produces base surges of greater power and eruptive columns of greater height. We suggest that the style of activity displayed during a secondary hydroeruption is controlled by both the total thermal energy of the system and the permeability of the pyroclastic overburden." @default.
• W2007779478 created "2016-06-24" @default.
• W2007779478 creator A5031030927 @default.
• W2007779478 creator A5042440796 @default.
• W2007779478 date "1987-07-01" @default.
• W2007779478 modified "2023-09-26" @default.
• W2007779478 title "Secondary hydroeruptions in pyroclastic-flow deposits: Examples from Mount St. Helens" @default.
• W2007779478 cites W1964097615 @default.
• W2007779478 cites W1964604457 @default.
• W2007779478 cites W1973956725 @default.
• W2007779478 cites W1986242260 @default.
• W2007779478 cites W2000277215 @default.
• W2007779478 cites W2032670345 @default.
• W2007779478 cites W2034259986 @default.
• W2007779478 cites W2039862561 @default.
• W2007779478 cites W2043318629 @default.
• W2007779478 cites W2056861465 @default.
• W2007779478 cites W2067994323 @default.
• W2007779478 cites W2070209458 @default.
• W2007779478 cites W2079253170 @default.
• W2007779478 cites W2081910176 @default.
• W2007779478 cites W2086436959 @default.
• W2007779478 cites W2088938774 @default.
• W2007779478 cites W2096247430 @default.
• W2007779478 cites W2148982676 @default.
• W2007779478 cites W2158219760 @default.
• W2007779478 doi "https://doi.org/10.1016/0377-0273(87)90081-3" @default.
• W2007779478 hasPublicationYear "1987" @default.
• W2007779478 type Work @default.
• W2007779478 sameAs 2007779478 @default.
• W2007779478 citedByCount "41" @default.
• W2007779478 countsByYear W20077794782012 @default.
• W2007779478 countsByYear W20077794782013 @default.
• W2007779478 countsByYear W20077794782015 @default.
• W2007779478 countsByYear W20077794782017 @default.
• W2007779478 countsByYear W20077794782020 @default.
• W2007779478 crossrefType "journal-article" @default.
• W2007779478 hasAuthorship W2007779478A5031030927 @default.
• W2007779478 hasAuthorship W2007779478A5042440796 @default.
• W2007779478 hasConcept C102879941 @default.
• W2007779478 hasConcept C113754120 @default.
• W2007779478 hasConcept C114793014 @default.
• W2007779478 hasConcept C120806208 @default.
• W2007779478 hasConcept C121332964 @default.
• W2007779478 hasConcept C127313418 @default.
• W2007779478 hasConcept C127592171 @default.
• W2007779478 hasConcept C1276947 @default.
• W2007779478 hasConcept C138170599 @default.
• W2007779478 hasConcept C146348940 @default.
• W2007779478 hasConcept C17409809 @default.
• W2007779478 hasConcept C179537507 @default.
• W2007779478 hasConcept C20113989 @default.
• W2007779478 hasConcept C53771952 @default.
• W2007779478 hasConcept C5900021 @default.
• W2007779478 hasConcept C62520636 @default.
• W2007779478 hasConcept C6494504 @default.
• W2007779478 hasConcept C75268469 @default.
• W2007779478 hasConcept C87457978 @default.
• W2007779478 hasConcept C92150305 @default.
• W2007779478 hasConcept C95869378 @default.
• W2007779478 hasConceptScore W2007779478C102879941 @default.
• W2007779478 hasConceptScore W2007779478C113754120 @default.
• W2007779478 hasConceptScore W2007779478C114793014 @default.
• W2007779478 hasConceptScore W2007779478C120806208 @default.
• W2007779478 hasConceptScore W2007779478C121332964 @default.
• W2007779478 hasConceptScore W2007779478C127313418 @default.
• W2007779478 hasConceptScore W2007779478C127592171 @default.
• W2007779478 hasConceptScore W2007779478C1276947 @default.
• W2007779478 hasConceptScore W2007779478C138170599 @default.
• W2007779478 hasConceptScore W2007779478C146348940 @default.
• W2007779478 hasConceptScore W2007779478C17409809 @default.
• W2007779478 hasConceptScore W2007779478C179537507 @default.
• W2007779478 hasConceptScore W2007779478C20113989 @default.
• W2007779478 hasConceptScore W2007779478C53771952 @default.
• W2007779478 hasConceptScore W2007779478C5900021 @default.
• W2007779478 hasConceptScore W2007779478C62520636 @default.
• W2007779478 hasConceptScore W2007779478C6494504 @default.
• W2007779478 hasConceptScore W2007779478C75268469 @default.
• W2007779478 hasConceptScore W2007779478C87457978 @default.
• W2007779478 hasConceptScore W2007779478C92150305 @default.
• W2007779478 hasConceptScore W2007779478C95869378 @default.
• W2007779478 hasIssue "4" @default.
• W2007779478 hasLocation W20077794781 @default.
• W2007779478 hasOpenAccess W2007779478 @default.
• W2007779478 hasPrimaryLocation W20077794781 @default.
• W2007779478 hasRelatedWork W1995921143 @default.
• W2007779478 hasRelatedWork W2007779478 @default.
• W2007779478 hasRelatedWork W2014253982 @default.
• W2007779478 hasRelatedWork W2040052008 @default.
• W2007779478 hasRelatedWork W2142810043 @default.
• W2007779478 hasRelatedWork W2267411227 @default.
• W2007779478 hasRelatedWork W2758189968 @default.
• W2007779478 hasRelatedWork W2806614900 @default.
• W2007779478 hasRelatedWork W3152429885 @default.
• W2007779478 hasRelatedWork W799938208 @default.
• W2007779478 hasVolume "32" @default.
• W2007779478 isParatext "false" @default.
• W2007779478 isRetracted "false" @default.

• next