Download presentation
Presentation is loading. Please wait.
Published byEdgar Harvey Modified over 6 years ago
1
IGNEOUS ROCKS Introduction Igneous Compositions Igneous Textures
Classification
2
Igneous Rocks Introduction
3
Rocks Most are aggregates of mineral crystals
PSCI 131: Igneous Rocks – Introduction Rocks Most are aggregates of mineral crystals A few kinds of rocks aren’t made of minerals Granite is made of mineral crystals Obsidian (volcanic glass) has no mineral crystals Images from: geology.com
4
Rocks Igneous Sedimentary Metamorphic
PSCI 131: Igneous Rocks – Introduction Rocks Igneous Sedimentary Metamorphic
5
Igneous Rocks Form by cooling and crystallization of magma
PSCI 131: Igneous Rocks – Introduction Igneous Rocks Form by cooling and crystallization of magma From: en.wikipedia.org From:meteorites.wustl.edu
6
Magma’s chemical composition Magma’s cooling rate
PSCI 131: Igneous Rocks – Introduction Igneous Rocks What kind of igneous rock will form when a magma crystallizes? Depends on: Magma’s chemical composition Magma’s cooling rate
7
Igneous Rocks Igneous Compositions
8
Igneous Rock Compositions
PSCI 131: Igneous Rocks – Compositions Igneous Rock Compositions What minerals the rock is made of Orthoclase Quartz Hornblende From: geology.com
9
Igneous Rock Compositions
PSCI 131: Igneous Rocks – Compositions Igneous Rock Compositions Percentage of dark silicate minerals From: ux1.eiu.edu From: geology.com From: nwnature.net
10
GRANITIC 0-25% dark minerals PSCI 131: Igneous Rocks – Compositions
This GRANITE contains about 10% dark minerals From: geology.com
11
GRANITIC 0-25% dark minerals PSCI 131: Igneous Rocks – Compositions
RHYOLITE is also felsic in composition From: itc.gsw.edu
12
ANDESITIC 25-45% dark minerals PSCI 131: Igneous Rocks – Compositions
DIORITE: This sample is about 40% dark crystals ANDESITE: Another intermediate rock From: nwnature.net From: geology.com
13
BASALTIC 45-85% dark minerals PSCI 131: Igneous Rocks – Compositions
This GABBRO contains about 70% dark minerals BASALT: Light silicate crystals are present, but are too small to see without magnification From: ux1.eiu.edu From: geology.com
14
Igneous Rocks Igneous Textures
15
IGNEOUS TEXTURES Visual appearance, not feel
PSCI 131: Igneous Rocks – Textures IGNEOUS TEXTURES Visual appearance, not feel Usually refers to size of mineral crystals Determined by magma’s rate of cooling
16
Coarse-grained Most crystals visible to naked eye
PSCI 131: Igneous Rocks – Textures Coarse-grained Most crystals visible to naked eye From: geology.com From: nwnature.net
17
Coarse-grained Slow cooling rate deep within crust
PSCI 131: Igneous Rocks – Textures Coarse-grained Slow cooling rate deep within crust Crystals have time to accumulate more atoms & grow large From: windows2universe.org
18
Fine-grained Most crystals not visible to naked eye
PSCI 131: Igneous Rocks – Textures Fine-grained Most crystals not visible to naked eye From: geology.com From: itc.gsw.edu
19
Fine-grained Rapid cooling rate on surface (volcanism)
PSCI 131: Igneous Rocks – Textures Fine-grained Rapid cooling rate on surface (volcanism) Not enough time for crystals to grow large From: bbc.co.uk
20
PORPHYRITIC Two distinct crystal sizes in same rock
PSCI 131: Igneous Rocks – Textures PORPHYRITIC Two distinct crystal sizes in same rock Phenocrysts Groundmass From: geo1.tcu.edu
21
PORPHYRITIC Two distinct crystal sizes in same rock
PSCI 131: Igneous Rocks – Textures PORPHYRITIC Two distinct crystal sizes in same rock Phenocrysts Groundmass From: pitt.edu
22
PORPHYRITIC Two-stage cooling First, slow cooling produces phenocrysts
PSCI 131: Igneous Rocks – Textures PORPHYRITIC Two-stage cooling First, slow cooling produces phenocrysts Then, rapid cooling of remaining magma produces groundmass
23
OTHER TEXTURES GLASSY Very fast cooling
PSCI 131: Igneous Rocks – Textures OTHER TEXTURES GLASSY Very fast cooling No time for any crystals to form
24
OTHER TEXTURES VESICULAR Vesicles (bubbles)
PSCI 131: Igneous Rocks – Textures OTHER TEXTURES VESICULAR Vesicles (bubbles) Gas trapped in rapidly cooling magma From: texasbeyondhistory.net
25
OTHER TEXTURES PYROCLASTIC Ash and rock fragments
PSCI 131: Igneous Rocks – Textures OTHER TEXTURES PYROCLASTIC Ash and rock fragments Violent volcanic eruptions Rock fragments Ash matrix
26
Igneous Rocks CLASSIFICATION
27
CLASSIFICATION Based on texture and composition
PSCI 131: Igneous Rocks – Classification CLASSIFICATION Based on texture and composition Some rocks can be classified based only on texture
28
CLASSIFICATION TABLE PSCI 131: Igneous Rocks – Classification GRANITIC
ANDESITIC BASALTIC COARSE-GRAINED Granite Diorite Gabbro FINE-GRAINED Rhyolite Andesite Basalt GLASSY OBSIDIAN VESICULAR SCORIA (dark) PUMICE (light) PYROCLASTIC WELDED TUFF PORPHYRITIC: Used as a modifier for any of the six basic rock names.
29
End of Igneous Rocks
Similar presentations
© 2024 SlidePlayer.com Inc.
All rights reserved.