Difference between revisions of "Magma"

From Conservapedia
Jump to navigation Jump to search
(new entry)
 
Line 1: Line 1:
[[Molten]] [[rock]] that may consolidate at depth or be [[erupt]]ed as [[lava]].
+
[[Image:Magma.jpg|thumb|300px|Sketch of a magma reservoir beneath a volcano and a conduit leading up to a lava dome at the surface. Arrow indicates direction of magma movement from a deeper source.]]'''Magma''' is molten or partially molten rock beneath the Earth's surface. When magma erupts onto the surface, it is called [[lava]]. Magma typically consists of a liquid portion (often referred to as the melt), a solid portion made of minerals that crystallized directly from the melt, solid rocks incorporated into the magma from along the conduit or reservoir, called xenoliths or inclusions, and dissolved gases.
  
Pellant, p. 251
+
[[Category:Geology]]
 
 
=Sources=
 
*Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995)
 
 
 
[[category:geology]]
 

Revision as of 01:19, June 26, 2007

File:Magma.jpg
Sketch of a magma reservoir beneath a volcano and a conduit leading up to a lava dome at the surface. Arrow indicates direction of magma movement from a deeper source.

Magma is molten or partially molten rock beneath the Earth's surface. When magma erupts onto the surface, it is called lava. Magma typically consists of a liquid portion (often referred to as the melt), a solid portion made of minerals that crystallized directly from the melt, solid rocks incorporated into the magma from along the conduit or reservoir, called xenoliths or inclusions, and dissolved gases.