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aureole
(redirected from aureoles)

   Also found in: Encyclopedia, Hutchinson 0.01 sec.
au·re·ole  (ôr-l) also au·re·o·la (ô-r-l)
n.
1. A circle of light or radiance surrounding the head or body of a representation of a deity or holy person; a halo.
2. Astronomy See corona.

[Middle English, from Late Latin (corna) aureola, golden (crown), feminine of Latin aureolus, golden, from aureus, from aurum, gold.]

aureole [ˈɔːrɪˌəʊl], aureola [ɔːˈriːələ]
n
1. (Fine Arts & Visual Arts / Art Terms) (esp in paintings of Christian saints and the deity) a border of light or radiance enveloping the head or sometimes the whole of a figure represented as holy
2. a less common word for halo
3. (Astronomy) another name for corona [2]
[from Old French auréole, from Medieval Latin (corōna) aureola golden (crown), from Latin aureolus golden, from aurum gold]

aureole  (ôr-l)
1. A band of metamorphic rock surrounding a body of cooled magma. Aureoles form through the process of contact metamorphism. See more at contact metamorphism.
2. See corona.
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.aureoleaureole - the outermost region of the sun's atmosphere; visible as a white halo during a solar eclipse
nimbus, nimbus cloud, rain cloud - a dark grey cloud bearing rain
glowing, radiance, glow - the amount of electromagnetic radiation leaving or arriving at a point on a surface
2.aureoleaureole - an indication of radiant light drawn around the head of a saint
lightness, light - the visual effect of illumination on objects or scenes as created in pictures; "he could paint the lightest light and the darkest dark"
Translations
aureole [ˈɔːrɪəʊl] Naureola f
aureole
n (Astron) → Korona f; (because of haze) → Hof m, → Aureole f; (Art) → Aureole f


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? Mentioned in ? References in periodicals archive
 
Furthermore, many of the methods and the rationale discussed in this article can also be applied in surface geochemical exploration, which is based on leaking hydrocarbons creating distinctive diagenetic aureoles that are direct indicators for hydrocarbon pools at depth (e.
Proximal intrusive bodies, as indicated by the presence of aeromagnetic anomalies with coincident, regionally developed aureoles of quartz-pyrite hornfels, marble and skarn;
Metamorphic aureoles around the granitic rocks are estimated to extend on the order of 1 km from the granitic rocks (Gordey and Anderson, 1993).
 
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