Matches in SemOpenAlex for { <https://semopenalex.org/work/W48218555> ?p ?o ?g. }
Showing items 1 to 57 of
57
with 100 items per page.
- W48218555 endingPage "99" @default.
- W48218555 startingPage "93" @default.
- W48218555 abstract "Abstract Conical mounds of ice have been observed to form in a few hours during violent winter storms along the edge of shore-fast ice near Dunkirk, New York. They occur in lines which parallel depth contours, and are evenly spaced in the manner of beach cusps. The height and spacing of mounds and number of rows vary from year to year depending on such factors as storm duration and intensity, and the position of the edge of the shore-fast ice at the beginning of the storm. The evenly sloping conical mounds have central channels which increase in width lakeward. The ice between the channels forms headlands above the lake surface. Spray-formed levees develop along the headlands and slope gently away from the lake margin. Lake marginal walls of ice are usually vertical. Spray, slush and ice blocks are ejected over the cone as each successive wave is focused by the converging channel walls. Ice blocks, interlayered with frozen slush and dirt, form bedding paralleling the sloping surface of cones, headlands and levees. These features are here termed “ice volcanoes” because their origin is in so many ways analogous to that of true volcanoes." @default.
- W48218555 created "2016-06-24" @default.
- W48218555 creator A5004284984 @default.
- W48218555 creator A5055066093 @default.
- W48218555 creator A5070951468 @default.
- W48218555 creator A5088670383 @default.
- W48218555 date "1973-01-01" @default.
- W48218555 modified "2023-09-27" @default.
- W48218555 title "Ice Volcanoes of the Lake Erie Shore Near Dunkirk, New York, U.S.A." @default.
- W48218555 doi "https://doi.org/10.1017/s0022143000022735" @default.
- W48218555 hasPublicationYear "1973" @default.
- W48218555 type Work @default.
- W48218555 sameAs 48218555 @default.
- W48218555 citedByCount "6" @default.
- W48218555 crossrefType "journal-article" @default.
- W48218555 hasAuthorship W48218555A5004284984 @default.
- W48218555 hasAuthorship W48218555A5055066093 @default.
- W48218555 hasAuthorship W48218555A5070951468 @default.
- W48218555 hasAuthorship W48218555A5088670383 @default.
- W48218555 hasBestOaLocation W482185551 @default.
- W48218555 hasConcept C111368507 @default.
- W48218555 hasConcept C114793014 @default.
- W48218555 hasConcept C120806208 @default.
- W48218555 hasConcept C127313418 @default.
- W48218555 hasConcept C15098985 @default.
- W48218555 hasConcept C152382732 @default.
- W48218555 hasConcept C165205528 @default.
- W48218555 hasConcept C66782727 @default.
- W48218555 hasConceptScore W48218555C111368507 @default.
- W48218555 hasConceptScore W48218555C114793014 @default.
- W48218555 hasConceptScore W48218555C120806208 @default.
- W48218555 hasConceptScore W48218555C127313418 @default.
- W48218555 hasConceptScore W48218555C15098985 @default.
- W48218555 hasConceptScore W48218555C152382732 @default.
- W48218555 hasConceptScore W48218555C165205528 @default.
- W48218555 hasConceptScore W48218555C66782727 @default.
- W48218555 hasIssue "64" @default.
- W48218555 hasLocation W482185551 @default.
- W48218555 hasOpenAccess W48218555 @default.
- W48218555 hasPrimaryLocation W482185551 @default.
- W48218555 hasRelatedWork W2007266279 @default.
- W48218555 hasRelatedWork W2013828340 @default.
- W48218555 hasRelatedWork W2053214310 @default.
- W48218555 hasRelatedWork W2055661326 @default.
- W48218555 hasRelatedWork W2070192581 @default.
- W48218555 hasRelatedWork W2115012406 @default.
- W48218555 hasRelatedWork W2145066355 @default.
- W48218555 hasRelatedWork W2167536656 @default.
- W48218555 hasRelatedWork W2469646072 @default.
- W48218555 hasRelatedWork W3193970338 @default.
- W48218555 hasVolume "12" @default.
- W48218555 isParatext "false" @default.
- W48218555 isRetracted "false" @default.
- W48218555 magId "48218555" @default.
- W48218555 workType "article" @default.