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Mineral Properties
• Hardness
– Moh’s Scale of Hardness 1-10
– Hardness is the resistance to being scratched
– Find by attempting to scratch minerals with
materials of a known hardness (like your
fingernail 2-2.5 or glass 5.5-6)
Mineral Properties
• Streak = color of powder
– Find by rubbing mineral against a ceramic
streak plate to create powder
• Luster = shine from unweathered surface
– Metallic (shiny like metal)
or non-metallic (dull or
glassy)
Mineral Properties
• Cleavage = breaks along smooth, parallel
sides
• Fracture = uneven breaking surfaces
• Breaking pattern depends on atomic
arrangement of mineral and if zones of
weakness exist
Rock Cycle
• 3 rock types are
igneous,
sedimentary, and
metamorphic.
• Any rock can
change into any
other rock type.
Sedimentary Rocks
• Form due to compaction and cementation
of rock particles
• Divided into 3 groups based on formation:
– Clastic (from other rock pieces)
– Chemical / Crystalline (from solution)
– Bioclastic (from organic materials)
Sedimentary Rocks
• Observable Characteristics:
– Layers of sediments (strata)
– Visible sediments (sand,
pebbles)
– Fossils or shells
– Chemical sedimentary rocks
are composed of only one
mineral (like rock salt from
halite)
Igneous Rocks
• Form when molten rock cools and hardens
• 2 types based on location of formation:
– Intrusive (plutonic): form underground
• cool slowly; large crystals (coarse-grained)
– Extrusive (volcanic): form above ground
• cool quickly; small or no crystals (fine-grained or
glassy)
• Mafic or Felsic based on composition
Igneous Rocks • Observable
Characteristics
– Glassy
– Vesicular texture (gas pockets)
– Interconnected mineral crystals (usually more than one color—like granite)
– Multiple mineral composition
Metamorphic Rocks
• Form due to heat and pressure (recrystallization)
• 2 types based on texture
– Foliated: mineral crystals are aligned (banding is when minerals separate into stripes)
– Non-foliated: interconnected mineral crystals
• 2 types of metamorphism
– Regional: large area of heat and pressure due to plate collision
– Contact: small area of heat due to hot fluids
Metamorphic Rocks
• Observable
Characteristics
– Foliation (minerals
flatten and line up)
– Banding (stripes of
minerals)
– Intergrown mineral
crystals (like marble)
– Foliated mica
– Garnets
Earth Science Reference Tables
• Page 6: Rock Cycle
• Page 6: Igneous Rock Chart
• Page 7: Sedimentary Rock Chart
• Page 7: Metamorphic Rock Chart
• Page 16: Properties of Minerals
Which rock type and why?
• Igneous (intrusive)
• Andesite, pegmatite
• Interconnected
mineral crystals
• Multiple mineral
composition
Which rock type and why?
• Metamorphic
• Gneiss
• Foliated
• Banding
• Stripes of crystals
• NOT layers
Which rock type and why?
• Igneous (intrusive)
• Granite
• Interconnected
mineral crystals
• Multiple mineral
composition
Which rock type and why?
• Sedimentary (clastic)
• Sediments (sand
grains) visible
• Layers of sand
• Strata
A diagram shows a beach and the paragraph
mentions that the headlands are made of diorite
bedrock.
Answer = 2
Answer = 3