Test 1 Flashcards
(36 cards)
How did the solar system form?
Nebular Hypothesis
1) Spinning Nebula
2) Spins Faster - Flattens and Contracts
3) Star “ignites”
4) Planets form from debris
5) Earth’s inner layers form
6) Earth’s moons forms
7) Hydrosphere and atmosphere form
Why is Pluto no longer a planet?
It does not have enough gravity to clear its orbit of other debris
not enough gravity due to size of moon
How did the moon form?
- A protoplanet collided with the earth
- Debris sprayed into space
- The debris coalesced to form the moon
- Craters exist due to impact events since formation
How did the inner layers of the Earth form?
differentiation by density
- Iron/nickel sink to the center
- silicates stay closer to the surface
define the different layers of Earth’s geosphere
Crust -Silicate Minerals (Silicon and Oxygen Based) -Low Density Mantle -silicate minerals, contains some iron and metals -medium density Core -iron/nickel -high density
What is the difference between an S wave and a P wave?
P waves are like a slinky, compression
S waves are like a rope, like doing the wave
S waves are stopped in liquid
Waves change direction when they hit the moho boundary
How did Earth’s Early atmosphere and hydrosphere form (and change over time)?
- Lighter gasses escape Earth’s gravity
- (Hydrogen/Helium)
- Water condenses to form oceans
- Earth’s oceans - formed early
- “Full” by 4 billion years ago
- Layers of atmosphere very by density and composition
Solar System Formation: Planets form from debris
Planets form from the gradual accumulation and collision of material from dust grains to planetesimals to proto-planets to what we see today
(gravity plus collisions)
What is the importance of the biosphere in relation to the atmosphere and hydrosphere?
everything affects plants!!!
What two factors control the properties of minerals and how do we classify minerals?
Bond Types
Chemical composition
ex. Diamond vs Graphite
Both Carbon - same composition
Different Crystal Structure
how can we test the different properties of different materials
color - look @ it
streak - color of powder, scrape against ceramic plate
luster - look @ it (metallic or non-metallic)
hardness - resist to scratching (scratch it)
crystal - shape when originally formed
cleavage - shape when broken
What are the properties of the Silicate Tetrahedron
Silicate Tetrahedron is composed of:
1 silicon atom surrounded by
4 Oxygen atoms
Net charge = -4
Name the properties of quartz
Color: Clear Streak: Clear/White Luster: Non Metallic Hardness: > 5.5 Cleavage or Fracture: Fracture
Name the properties of Potassium Feldspar
Color: Pink Streak: White Luster: Non Metallic Hardness: > 5.5 Cleavage or Fracture: Cleavage; 2 direction
Name the properties of Mica Biotite
Color: Black Streak: clear, white Luster: Non Metallic Hardness: 2.5-3.5 Cleavage or Fracture: Cleavage; 1 direction
Name the properties of Mica Mucovite
Color: White, grey, silvery Streak: White Luster: Non Metallic Hardness: 2 Cleavage or Fracture: Cleavage; 1 direction
Name the properties of Calcite
Color: clear Streak: white Luster: Non Metallic Hardness: 2.5-3.5 Cleavage or Fracture: Cleavage; 3 directions FIZZES
Name the properties of Graphite
Color: Silver/Gray Streak: Gray Luster: Metallic Hardness: < 2.5 Cleavage or Fracture: Cleavage; 1 direction
Name the properties of Galena
Color: Silver/Gray Streak: Gray Luster: Metallic Hardness:3.5-4.5 Cleavage or Fracture: Cleavage; 3 direction
What are the types of silicate materials
Felsic
Intermediate
Mafic
What are the properties of Felsic minerals
- silicate minerals containing little magnesium and iron
- “Continental” crust
- LIGHT (Any pink = felsic!)
- Lower density
- form at lower temperatures, closer to surface
- stable at earth’s surface
What are the properties of Mafic Minerals
- silicate minerals containing magnesium and iron
- “Oceanic” crust
- DARK
- Higher density
- form at higher temperatures, low in the earth
What are the properties of igneous rocks
Composition/Color
Texture/Crystal Size
Name the types of crystal sizes
Intrusive
- Coarse grained
- slow cooling magma
- larger crystals
Extrusive
- fine grained
- fast cooling lava
- small crystals