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Difference between revisions of "Igneous intrusive layer"

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[[File:igneous_intrusive_layer.jpg|thumb|300px|right|Created from rocks that have crystallized from the heat of magma.]]
 
[[File:igneous_intrusive_layer.jpg|thumb|300px|right|Created from rocks that have crystallized from the heat of magma.]]

Latest revision as of 17:35, 7 May 2024

This article is about the current version of DF.
Note that some content may still need to be updated.

Created from rocks that have crystallized from the heat of magma.

Igneous intrusive stone layers can consist of granite, diorite, or gabbro, all of which typically contain gold and tetrahedrite.

Gabbro can also contain garnierite (the ore of nickel), kimberlite (which may contain diamonds), and olivine (which may contain native platinum). Granite can contain cassiterite (the ore of tin), bismuthinite (the ore of bismuth), and galena (the ore of lead, plus a 50% chance of silver).

Igneous intrusive layers[edit]

Stone found in igneous intrusive layers[edit]

Stone appearing in both igneous intrusive and igneous extrusive layers[edit]

Gems found in igneous intrusive layers[edit]

Gems appearing in both igneous intrusive and igneous extrusive layers[edit]

* See also: stone found everywhere

In the real world[edit]

Igneous intrusive stone is formed by magma solidification occurring below the surface, as opposed to igneous extrusive stone, which forms above the surface of the earth.

Sedimentary
Igneous
Intrusive
Extrusive
Metamorphic
Ore
Economic
Other