Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Variolite
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
==Varieties and occurrence== The variety of mafic igneous rocks that contain varioles are, with rare exceptions, no longer classified as ''variolites'', which is not recommended for usage. Instead, they are designated using the modifier '''variolitic''' in conjunction with the major [[lithology]]. The major varieties of ''variolites'' are variolitic basalts, variolitic pillow lavas and variolitic komatiites.<ref name="NeuendorfOthers2005a"/><ref name="MaitreOthers2005a"/> Variolitic pillow lavas, that have been previously identified as ''variolites'' and also classified as [[spilite]]s, are found in the Durance, [[France]]; on Mont Genvre, France; in [[Devonian]] rocks of [[Germany]]; and as cobbles on the beaches of the [[Strait of Juan de Fuca]] along the northern edge of the [[Olympic Peninsula]].<ref name="Lewis1914a">Lewis, J.V. (1914) ''Origin of Pillow Lava.'' Bulletin of the Geological Society of America. vol. 25, pp. 15-25.</ref><ref name="SnavelyOthers1973a">Snavely, P.D., Maceod, N.S., and Holly, C.W. (1973) ''Miocene tholeiitic basalts of coastal Oregon and Washington and their relations to coeval basalts of the Columbia Plateau.'' Geological Society of America Bulletin. vol. 84, pp. 387–424</ref> Variolitic basalts and variolitic komatiites occur commonly as [[Archean]] lava flows in the [[greenstone belt]]s of South Africa and the [[Canadian Shield]].<ref name="SandstaOthers2011a"/><ref name="FowlerOthers1987a"/> Finally, there is a group of spotted volcanic rocks formerly known to [[France|French]] petrographers as the ''variolites du Drac'' from the locality in which they are found in [[Parc National des Ecrins]], France.<ref name="EB1911">{{Cite EB1911|wstitle=Variolites|volume=27|page=921}}</ref> Additional research has found them to be [[hydrothermal]]ly altered basalt volcanic rocks that contain [[amygdule]]s filled with white [[calcite]] and other secondary minerals.<ref name="Buffet-Croix-Blanche1989a">Buffet-Croix-Blanche, G. (1989) ''Volcans fossiles dans la region du parc national des Ecrins; sept excursions pour une initiation volcanologique sur des lambeaux de volcans dates de 200 millions d'années.'' Parc National des Ecrins, France. 73 p.</ref>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)