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EOSC 210 EXAM QUESTIONS AND ANSWERS ALL CORRECT

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EOSC 210 EXAM QUESTIONS AND ANSWERS ALL CORRECT How do minerals form? - Answer- cooling and crystallization from magma; precipitation from fluid; chemical changes from heat and pressure; precipitation from biogenic activity (biomineralization) How do we identify minerals? - Answer- 1. Physical...

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  • November 19, 2024
  • 14
  • 2024/2025
  • Exam (elaborations)
  • Questions & answers
  • EOSC 210
  • EOSC 210
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Scholarsstudyguide
EOSC 210 EXAM QUESTIONS AND
ANSWERS ALL CORRECT

How do minerals form? - Answer- cooling and crystallization from magma; precipitation
from fluid; chemical changes from heat and pressure; precipitation from biogenic activity
(biomineralization)

How do we identify minerals? - Answer- 1. Physical properties: colour; lustre; streak;
hardness; cleavage; fracture
2. RXN to acid; magnetism; taste; radioactivity; specific gravity; habit

Silicate Minerals classification - Answer- classified based upon the arrangement of their
silicon-oxygen tetrahedra, which controls properties

Igneous - Answer- crystallize from a "melt" (magma)

sedimentary - Answer- either "clastic" grains or biological/chemical precipiation

Metamorphic - Answer- alteration of pre-existing rock

3 agents of metamorphism - Answer- heat, pressure, chemically active fluids

Foliated Rocks - Answer- -platy minerals (chlorite-mica) crystallize perpendicular to
main pressure direction
-pre-existing minerals acquire preferred orientation
-foliation tends to occur in fine grained material
-foliation texture alters with increasing (grade of) metamorphism

Non-foliated Rocks - Answer- no obvious foliation, uniform texture, rocks tend to contain
only one mineral

Common metamorphic rocks - Answer- slate; schist; marble; quartzite

cleavage - Answer- -inclination to break along the planes of weakness
-imparts the tendency to split or break along foliation planes rather than across the
planes

Bowens Reaction Series - Answer- -describes the sequence of minerals that crystallize
form a basaltic melt

, -as the composition of minerals crystallizing from the melt changes, the magma
composition changes, or differentiates, especially if early crystals can be separated from
the melt

Formation of igneous rocks - Answer- -cooling of molten rock (magma or lava)

Intrusive - Answer- -Molten rock (magma) that solidifies with Earth's crust (igneous)
-slow cooling, large crystals

Extrusive - Answer- -molten rock (lava) that solidifies at/near the Earth's surface
(igneous)
-quick cooling, tiny crystals or glassy

Plutonic - Answer- -Intrusive
-slow cooling results in larger crystals (most>1mm)
-phaneritic texture

Volcanic - Answer- -Extrusive
-rapid cooling results in smaller crystals (most<1mm)
-aphanitic texture

Rocks melt by... - Answer- Heat
Reduce pressure
Add volatiles

Mantle Plumes (hot spots) - Answer- -hot plastic mantle material rising from core/mantle
boundary
-as it rises toward crust, decompression results in melting
-accounts for magmatic activity that is not at plate boundaries

How does magma move through crust? - Answer- Diapirism
Stoping
Melting

Diapirism - Answer- rising "blobs" of lower density molten rock

Stoping - Answer- magma intrudes into brittle country rock by force

Melting - Answer- magma melts country rock

Shallow intrusives - Answer- -formed at depths <~2km
-cool more rapidly
-generally fine grained (can even be as fine grained as a lava flow)

Deep intrusives - Answer- -formed at greater than ~2km depth
-Pluton: "blob-shaped" intrusive igneous body

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