Anmerkung: Die Bezeichnungen beziehen sich, anders als es der rauchende Vulkanschlot in der Abbildung möglicherweise suggeriert, in aller Regel auf die vollständig erkalteten und meist viele Millionen Jahre alten Gesteinskörper, die das Ergebnis der unterirdischen magmatischen Aktivität sind.
Note: As a general rule, in contrast to the smoldering volcanic vent in the figure, these names refer to the fully cooled and usually millions-of-years-old rock formations, which are the result of the underground magmatic activity shown.
Nota: Como regla general, en contraste con el respiradero volcánico latente en la figura, estos nombres se refieren a las formaciones rocosas completamente enfriadas y generalmente de millones de años, que son el resultado de la actividad magmática subterránea que se muestra.
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the
Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License.http://www.gnu.org/copyleft/fdl.htmlGFDLGNU Free Documentation Licensetruetrue
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Captions
Basic types of igneous intrusion. (View details for guide to numbering.)
{{Information |Description={{en|1=Basic types of intrusions}} {{pl|1=Podstawowe typy intruzji}} |Source=Own work by uploader |Author=
Motilla |Date=07.07.2009 |Permission= |other_versions= }} <!--{{ImageUpload|full}}--> [[Category:[[Categ
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Anmerkung: Die Bezeichnungen beziehen sich, anders als es der rauchende Vulkanschlot in der Abbildung möglicherweise suggeriert, in aller Regel auf die vollständig erkalteten und meist viele Millionen Jahre alten Gesteinskörper, die das Ergebnis der unterirdischen magmatischen Aktivität sind.
Note: As a general rule, in contrast to the smoldering volcanic vent in the figure, these names refer to the fully cooled and usually millions-of-years-old rock formations, which are the result of the underground magmatic activity shown.
Nota: Como regla general, en contraste con el respiradero volcánico latente en la figura, estos nombres se refieren a las formaciones rocosas completamente enfriadas y generalmente de millones de años, que son el resultado de la actividad magmática subterránea que se muestra.
to share – to copy, distribute and transmit the work
to remix – to adapt the work
Under the following conditions:
attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the
same or compatible license as the original.
Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the
Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License.http://www.gnu.org/copyleft/fdl.htmlGFDLGNU Free Documentation Licensetruetrue
You may select the license of your choice.
Information
Captions
Basic types of igneous intrusion. (View details for guide to numbering.)
{{Information |Description={{en|1=Basic types of intrusions}} {{pl|1=Podstawowe typy intruzji}} |Source=Own work by uploader |Author=
Motilla |Date=07.07.2009 |Permission= |other_versions= }} <!--{{ImageUpload|full}}--> [[Category:[[Categ
File usage
The following pages on the English Wikipedia use this file (pages on other projects are not listed):