File:Hornitos hidromagmáticos.JPG

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Español: Las formas volcánicas menores asociadas al contacto agua-lava, también denominados

hornitos hidromagmáticos, pseudo-cráteres o conos litorales, son pequeños montículos construidos por fragmentos de lava que se encuentran dispuestos sobre la superficie de algunas coladas. Estas morfologías son construcciones desenraizadas, de planta y alzado variado, cuya distribución espacial parece estar asociada al trazado de las distintas unidades de flujo de una colada y, a la geometría de los diferentes lóbulos de lava. En

Canarias están vinculados al emplazamiento de coladas en ambientes litorales.
English: The minor volcanic forms associated with water-lava interaction, denominated in the

literature as the hydromagmatic toaster, pseudo-craters or littoral cones, are small mounds built by lava fragments are arranged on the surface of many lava flows. It is ungrounded constructions of plan and elevation varied, whose spatial distribution appears to be associated to the path of the various units of a melt flow and the geometry of the different lobes of lava. In the Canary Islands are linked to the emplacement of

lava flows in littorals environments.
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Author Geogranova

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current11:39, 9 March 2015Thumbnail for version as of 11:39, 9 March 20153,099 × 2,129 (1.62 MB)Geogranova (talk | contribs)User created page with UploadWizard

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