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Rock Identification

Modified from a PowerPoint presentation prepared by J.
Crelling, Southern Illinois University
Characterizing Rocks
There are 3 major types of rocks
IGNEOUS – formed from molten magma
SEDIMENTARY – formed from sediment
(mud, sand, shells, etc,)
METAMORPHIC – formed by applying heat
and pressure to other existing rocks
The Rock Cycle
–a
representation
of the
interrelationship
between
different types
of rocks.
NOTE:
How do rocks
formed at depth
(i.e. all except
extrusive igneous)
get exposed on
the surface???
Characterizing Rocks
The three major characterizing features of
rocks are:
• Colour
• Composition (Mineralogy/Chemistry)
• Texture
Note: Even the most sophisticated
geological classification schemes are
based on these features
Characterising Rocks
Classification by Colour
Colour Index (used mainly for igneous rocks)
• Leucocratic – light colour
• Mesocratic – intermediate colour
• Melanocratic – dark colour
and/or
• Felsic – rich in light coloured minerals
• Mafic – rich in dark coloured minerals
Igneous Rocks
Textures of Igneous Rocks
• Aphanitic – fine-grained. Individual grains
can’t be seen with naked eye
• Phaneritic - grains easily seen with the naked
eye
• Porphyritic – larger grains in finer grains
•
Inclusions
> Xenoliths
> Xenocrysts
Vesicular &
Glassy
Textures
Xenoliths
1

9

5

2

4

8

3

7
6

10

11
12

13
14

15
What % Si02??
66

52

45

1
3
2

4
Colour?
Leucocratic (light)?

i.e. silicic v mafic



Melanocratic (dark)?
Mesocratic (medium)?

Grain size /
Texture?
Phaneritic (coarse)



Aphanitic (fine)?
Medium?

Black
Biotite
shiny?
mica
K feldspar
Pink?

Mineralogy?

Granite

Quartz
Grey vitreous?
A quicker way?
– pink crystals, coarse grained – granite
(then check for other minerals to be sure)
Granodiorite

…plenty of quartz… but no / not much K feldspar…
Colour?

i.e. silicic v mafic

Leucocratic (light)?
Melanocratic (dark)?
Mesocratic (medium)?



Grain size /
Texture?
Phaneritic (coarse)



Aphanitic (fine)?
Medium?

Gabbro

Not
Mafic easy!! – are these green or grey?
Dark?
(pyroxene or I think pale green!! – so…
Plagioclase
white?
amphibole)
Olivine
feldspar
…but if grey 
Mineralogy?
Quartz
Colour?
Leucocratic (light)?

i.e. silicic v mafic



Melanocratic (dark)?
Mesocratic (medium)?

Grain size /
Texture?
Phaneritic (coarse)
Aphanitic (fine)?



Medium?

So what is it?

Rhyolite
Flow banding texture – distinctive 
rhyolite
Colour?

Grain size /
Texture?

Leucocratic (light)?
Melanocratic (dark)?



Mesocratic (medium)?

Phaneritic (coarse)
Aphanitic (fine)?
Larger crystals called??

phenocrysts
…white, so…  ??
Plagioclase feldspar
NB – story?... Think
Bowen’s Reaction
series…

These aren’t crystals
(round – bubble-shaped!)

amygdales
(infilled vesicles)

Medium?

So what is it?

Basalt


What are the holes??
Vesicles

Colour?

mesocratic

so…  ??
andesite
BUT…
What are the GREEN
phenocrysts?

Olivine!!

So…
Thinking of magma
differentiation, what’s the
story here, maybe?
Mafic magma…
Erupted before olivine could
be reabsorbed into melt…
Melt will be relatively
depleted in Mg,Fe  so…
So can’t be andesite
lighter coloured than usual??

So what is it?

Basalt
(vesicular
basalt)
Grain size /
Texture?

Colour?
Leucocratic (light)?
Melanocratic (dark)?



Mesocratic (medium)?

Phaneritic (coarse)
Aphanitic (fine)?
Medium?

So what is it?

Dolerite


Looks pretty light-coloured –
and obviously course-grained

So might think ‘granite’… BUT…
What minerals would you expect?
K feldspar and quartz for a start….

So what is it?

Diorite

Whereas what’s here???
Plagioclase feldspar and mafics…
So what is it?

Andesite
Colour?
Leucocratic (light)?
Melanocratic (dark)?
Mesocratic (medium)?



Grain size /
Texture?
Phaneritic (coarse)
Aphanitic (fine)?
Medium?


So what is it?

Andesite
Colour?
Leucocratic (light)?
Melanocratic (dark)?
Mesocratic (medium)?



Grain size /
Texture?
Phaneritic (coarse)
Aphanitic (fine)?
Medium?


So what is it?

Andesite
Colour?
Leucocratic (light)?
Melanocratic (dark)?
Mesocratic (medium)?



Grain size /
Texture?
Phaneritic (coarse)
Aphanitic (fine)?
Medium?


Yep, they’re all

andesite!!
Glassy texture, black coloured… so…

How formed?
Super-cooled – so no
time for crystals to
form – usually when
erupted into water

obsidian
Volcanic glass is chemically unstable – out of
equilibrium with surface temperatures – so begins to
crystallise (de-vitrify) – snowflake obsidian
If you see this rock, just note the large green crystals  ??

olivine

…so it’s peridotite (ultramafic) – not dark black as you might
What’s this?
Mantle xenoliths
in basalt
What’s this?
(look at the
massive crystals)

Pegmatite

Forms when late-stage volatiles are injected into country
rock when granite batholith is mostly crystallised
With many thanks to:
•The original author – someone from University of Massachusetts!
•Additional photos from Roger Weller, Conchise College, Arizona:
http://skywalker.cochise.edu/wellerr/rocks/igrocksL.htm

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Rock identification igneous kc

  • 1. Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University
  • 2. Characterizing Rocks There are 3 major types of rocks IGNEOUS – formed from molten magma SEDIMENTARY – formed from sediment (mud, sand, shells, etc,) METAMORPHIC – formed by applying heat and pressure to other existing rocks
  • 3. The Rock Cycle –a representation of the interrelationship between different types of rocks. NOTE: How do rocks formed at depth (i.e. all except extrusive igneous) get exposed on the surface???
  • 4. Characterizing Rocks The three major characterizing features of rocks are: • Colour • Composition (Mineralogy/Chemistry) • Texture Note: Even the most sophisticated geological classification schemes are based on these features
  • 5. Characterising Rocks Classification by Colour Colour Index (used mainly for igneous rocks) • Leucocratic – light colour • Mesocratic – intermediate colour • Melanocratic – dark colour and/or • Felsic – rich in light coloured minerals • Mafic – rich in dark coloured minerals
  • 6. Igneous Rocks Textures of Igneous Rocks • Aphanitic – fine-grained. Individual grains can’t be seen with naked eye • Phaneritic - grains easily seen with the naked eye • Porphyritic – larger grains in finer grains • Inclusions > Xenoliths > Xenocrysts
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  • 14. Colour? Leucocratic (light)? i.e. silicic v mafic  Melanocratic (dark)? Mesocratic (medium)? Grain size / Texture? Phaneritic (coarse)  Aphanitic (fine)? Medium? Black Biotite shiny? mica K feldspar Pink? Mineralogy? Granite Quartz Grey vitreous?
  • 15. A quicker way? – pink crystals, coarse grained – granite (then check for other minerals to be sure)
  • 16. Granodiorite …plenty of quartz… but no / not much K feldspar…
  • 17. Colour? i.e. silicic v mafic Leucocratic (light)? Melanocratic (dark)? Mesocratic (medium)?  Grain size / Texture? Phaneritic (coarse)  Aphanitic (fine)? Medium? Gabbro Not Mafic easy!! – are these green or grey? Dark? (pyroxene or I think pale green!! – so… Plagioclase white? amphibole) Olivine feldspar …but if grey  Mineralogy? Quartz
  • 18. Colour? Leucocratic (light)? i.e. silicic v mafic  Melanocratic (dark)? Mesocratic (medium)? Grain size / Texture? Phaneritic (coarse) Aphanitic (fine)?  Medium? So what is it? Rhyolite
  • 19. Flow banding texture – distinctive  rhyolite
  • 20. Colour? Grain size / Texture? Leucocratic (light)? Melanocratic (dark)?  Mesocratic (medium)? Phaneritic (coarse) Aphanitic (fine)? Larger crystals called?? phenocrysts …white, so…  ?? Plagioclase feldspar NB – story?... Think Bowen’s Reaction series… These aren’t crystals (round – bubble-shaped!) amygdales (infilled vesicles) Medium? So what is it? Basalt 
  • 21. What are the holes?? Vesicles Colour? mesocratic so…  ?? andesite BUT… What are the GREEN phenocrysts? Olivine!! So… Thinking of magma differentiation, what’s the story here, maybe? Mafic magma… Erupted before olivine could be reabsorbed into melt… Melt will be relatively depleted in Mg,Fe  so… So can’t be andesite lighter coloured than usual?? So what is it? Basalt (vesicular basalt)
  • 22. Grain size / Texture? Colour? Leucocratic (light)? Melanocratic (dark)?  Mesocratic (medium)? Phaneritic (coarse) Aphanitic (fine)? Medium? So what is it? Dolerite 
  • 23. Looks pretty light-coloured – and obviously course-grained So might think ‘granite’… BUT… What minerals would you expect? K feldspar and quartz for a start…. So what is it? Diorite Whereas what’s here??? Plagioclase feldspar and mafics…
  • 24. So what is it? Andesite Colour? Leucocratic (light)? Melanocratic (dark)? Mesocratic (medium)?  Grain size / Texture? Phaneritic (coarse) Aphanitic (fine)? Medium? 
  • 25. So what is it? Andesite Colour? Leucocratic (light)? Melanocratic (dark)? Mesocratic (medium)?  Grain size / Texture? Phaneritic (coarse) Aphanitic (fine)? Medium? 
  • 26. So what is it? Andesite Colour? Leucocratic (light)? Melanocratic (dark)? Mesocratic (medium)?  Grain size / Texture? Phaneritic (coarse) Aphanitic (fine)? Medium? 
  • 28. Glassy texture, black coloured… so… How formed? Super-cooled – so no time for crystals to form – usually when erupted into water obsidian
  • 29. Volcanic glass is chemically unstable – out of equilibrium with surface temperatures – so begins to crystallise (de-vitrify) – snowflake obsidian
  • 30. If you see this rock, just note the large green crystals  ?? olivine …so it’s peridotite (ultramafic) – not dark black as you might
  • 32. What’s this? (look at the massive crystals) Pegmatite Forms when late-stage volatiles are injected into country rock when granite batholith is mostly crystallised
  • 33. With many thanks to: •The original author – someone from University of Massachusetts! •Additional photos from Roger Weller, Conchise College, Arizona: http://skywalker.cochise.edu/wellerr/rocks/igrocksL.htm