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- Diabase, diorite, gabbro, granite, pegmatite, and peridotiteIntrusive igneous rocks crystallize below Earth's surface, and the slow cooling that occurs there allows large crystals to form. Examples of intrusive igneous rocks are: diabase, diorite, gabbro, granite, pegmatite, and peridotite.geology.com/rocks/igneous-rocks.shtml
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Dacite
QAPF Diagram for Dacite: A QAPF diagram is a method of classifying igneous rocks …
Basalt
Basalt is a dark-colored, fine-grained, igneous rock composed mainly of …
Diorite
Diorite is an intrusive igneous rock of intermediate composition. Uses of …
Granite
Granite is a coarse-grained, light-colored igneous rock composed mainly of …
Pumice
Pumice is an extrusive igneous rock with a vesicular texture and very low specific …
Obsidian
These glassy rocks are named "tachylyte." Are There Other Glassy Igneous Rocks? …
Rhyolite
These rocks have similar compositions but different cooling conditions. Explosive …
Pegmatite
Pegmatite is an intrusive igneous rock with very large crystals that forms in the later …
Rock Collections
A comprehensive collection of 36 different sedimentary, metamorphic and igneous …
Fire Opal
Fire opal is defined by its fiery yellow, fiery orange or fiery red background color. …
WEBIgneous rock - Intrusive, Magma, Plutonic: Erosion of volcanoes will immediately expose shallow intrusive bodies such as volcanic necks and diatremes (see Figure 6). A volcanic neck is the “throat” of a volcano …
WEBJan 11, 2021 · Intrusive igneous rocks have relatively large crystals that are easy to see. Intrusive igneous rocks are also called plutonic. A pluton is an igneous rock body that forms within the crust. Granite is the most …
WEBMay 3, 2024 · dike. igneous rock, any of various crystalline or glassy rocks formed by the cooling and solidification of molten earth material. Igneous rocks constitute one of the three principal classes of rocks, the others …
4.4 Intrusive Igneous Rocks – Principles of Earth Science
WEB4.4 Intrusive Igneous Rocks. In most cases, a body of hot magma is less dense than the rock surrounding it, so it has a tendency to creep upward toward the surface. It does so in a few different ways: When magma …
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