Webster's Online Dictionary
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Definition: HORNITO

Part of Speech Definition
Noun 1. A low, oven-shaped mound, common in volcanic regions, and emitting smoke and vapors from its sides and summit.[Websters].

Source: Webster's Revised Unabridged Dictionary (1913)

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Date "Hornito" was first used in popular English literature: sometime before 1914. (references)

Etymology:Hornito \Hor*ni"to\, noun. [A diminutive from Spanish horno oven, from Latin expression furnus. See Furnace.]. (references)

Specialty Definition: HORNITO

Domain Definition
Geography Vent situated on lava flow and delivering either blobs of viscous lava, or driblet cones, or ash, and forming a small pipe-like cone. Source: European Union. (references)
Geology A small rootless spatter cone that forms on the surface of a basaltic lava flow (usually pahoehoe) is called a hornito. A hornito develops when lava is forced up through an opening in the cooled surface of a flow and then accumulates around the opening. Typically, hornitos are steep sided and form conspicuous pinnacles or stacks. They are "rootless" because they are fed by lava from the underlying flow instead of from a deeper magma conduit. (references)

Source: compiled by the editor from various references; see credits.

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Definition: HORNITO

Part of SpeechDefinition
Noun1. A low, oven-shaped mound, common in volcanic regions, and emitting smoke and vapors from its sides and summit.[Websters].

Source: Webster's Revised Unabridged Dictionary (1913)

Top

Date "HORNITO" was first used in popular English literature: sometime before 1914. (references)

Etymology:Hornito \Hor*ni"to\, noun. [A diminutive from Spanish horno oven, from Latin expression furnus. See Furnace.]. (references)

Specialty Definition: HORNITO

DomainDefinition
GeographyVent situated on lava flow and delivering either blobs of viscous lava, or driblet cones, or ash, and forming a small pipe-like cone. Source: European Union. (references)
GeologyA small rootless spatter cone that forms on the surface of a basaltic lava flow (usually pahoehoe) is called a hornito. A hornito develops when lava is forced up through an opening in the cooled surface of a flow and then accumulates around the opening. Typically, hornitos are steep sided and form conspicuous pinnacles or stacks. They are "rootless" because they are fed by lava from the underlying flow instead of from a deeper magma conduit. (references)

Source: compiled by the editor from various references; see credits.

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