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- Introduction to geologic principles
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- There are Four Layers
- Inner Core
- Outer Core
- Mantle
- Crust
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- Asthenospere
- 100-700 km downward
- Hot and fluid
- Lithosphere
- Sphere of rock
- Part of the mantle
- Part of the crust
- Cool and rigid
- Hydrosphere- water covering (the oceans)
- Atmosphere (the gas covering around the planet)
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- The lithosphere
- Is fractured
- in to “plates”
- 11 major plates
- Other smaller “pieces”
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- 1. Divergent Boundaries
- Plates move apart
- Magma fills the zone
- Sea floor spreading
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- 2. Convergent Boundaries
- Plates collide
- Generally one sides
- Under the other
- Leads to inland volcanoes
- (Like the Cascade Range)
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- 3. Transform Fault Boundaries
- Plates slide (grind)
- Past one another
- In opposite directions
- Earthquakes can be
- One result
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- 1. Igneous rock (fire formed)
- Cooled magna in some form
- Process called crystalization
- 2. Sedimentary (settling rock)
- Sediments converted to rock by weight
- Process is called lithification
- 3. Metamorphic (changed form)
- Convert in form by heat and pressure
- Process called metamorphism
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11
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- 1. Intrusive or Plutonic
- Magna cooling beneath the surface
- Crystallizes at depth
- 2. Extrusive or Volcanic
- Magma that cooled or near the surface
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- 1 Aphanitic (Ryolite)
- 2 Phaneritic (Granite)
- 3 Porphyritic (Porphyry)
- large crystals embedded in smaller crystal masses
- 4 Glassy (Obsidian)
- Natural glassy texture (Rapid cooling)
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- Names are based on chemical makeup
- Calcium fledspar, iron, quartz, ect
- Cooling rate is the second factor
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- Tuff
- Ash fragments
- Hot an fused are called
- (welded tuff)
- Volcanic brecca
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- Lava Flows
- Pahoehoe flows-twisted ropy floes
- Aa flows sharp edges
- Lava pours from fissures
- Volcanic Formations
- Shield volcanoes
- Calderas
- Cinder cones
- Lava tubes
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18
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- Dikes
- Form when cracks are filled by lava which then cools
- Stills
- Laccoliths
- Batholiths
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