Test 1 Flashcards

(36 cards)

1
Q

How did the solar system form?

A

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

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2
Q

Why is Pluto no longer a planet?

A

It does not have enough gravity to clear its orbit of other debris

not enough gravity due to size of moon

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3
Q

How did the moon form?

A
  • 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
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4
Q

How did the inner layers of the Earth form?

A

differentiation by density

  • Iron/nickel sink to the center
  • silicates stay closer to the surface
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5
Q

define the different layers of Earth’s geosphere

A
Crust
-Silicate Minerals (Silicon and Oxygen Based)
-Low Density
Mantle
-silicate minerals, contains some iron and metals
-medium density
Core
-iron/nickel
-high density
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6
Q

What is the difference between an S wave and a P wave?

A

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

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7
Q

How did Earth’s Early atmosphere and hydrosphere form (and change over time)?

A
  • 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
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8
Q

Solar System Formation: Planets form from debris

A

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)

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9
Q

What is the importance of the biosphere in relation to the atmosphere and hydrosphere?

A

everything affects plants!!!

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10
Q

What two factors control the properties of minerals and how do we classify minerals?

A

Bond Types
Chemical composition

ex. Diamond vs Graphite
Both Carbon - same composition
Different Crystal Structure

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11
Q

how can we test the different properties of different materials

A

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

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12
Q

What are the properties of the Silicate Tetrahedron

A

Silicate Tetrahedron is composed of:
1 silicon atom surrounded by
4 Oxygen atoms
Net charge = -4

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13
Q

Name the properties of quartz

A
Color: Clear
Streak: Clear/White
Luster: Non Metallic
Hardness: > 5.5
Cleavage or Fracture:
Fracture
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14
Q

Name the properties of Potassium Feldspar

A
Color: Pink
Streak: White
Luster: Non Metallic
Hardness:  > 5.5
Cleavage or Fracture:
Cleavage; 2 direction
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15
Q

Name the properties of Mica Biotite

A
Color: Black
Streak: clear, white
Luster: Non Metallic
Hardness: 2.5-3.5
Cleavage or Fracture:
Cleavage; 1 direction
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16
Q

Name the properties of Mica Mucovite

A
Color: White, grey, silvery
Streak: White
Luster: Non Metallic
Hardness: 2
Cleavage or Fracture:
Cleavage; 1 direction
17
Q

Name the properties of Calcite

A
Color: clear
Streak: white
Luster: Non Metallic
Hardness: 2.5-3.5
Cleavage or Fracture:
Cleavage; 3 directions
FIZZES
18
Q

Name the properties of Graphite

A
Color: Silver/Gray
Streak: Gray
Luster: Metallic
Hardness: < 2.5
Cleavage or Fracture:
Cleavage; 1 direction
19
Q

Name the properties of Galena

A
Color: Silver/Gray
Streak: Gray
Luster: Metallic
Hardness:3.5-4.5
Cleavage or Fracture:
Cleavage; 3 direction
20
Q

What are the types of silicate materials

A

Felsic
Intermediate
Mafic

21
Q

What are the properties of Felsic minerals

A
  • 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
22
Q

What are the properties of Mafic Minerals

A
  • silicate minerals containing magnesium and iron
  • “Oceanic” crust
  • DARK
  • Higher density
  • form at higher temperatures, low in the earth
23
Q

What are the properties of igneous rocks

A

Composition/Color

Texture/Crystal Size

24
Q

Name the types of crystal sizes

A

Intrusive

  • Coarse grained
  • slow cooling magma
  • larger crystals

Extrusive

  • fine grained
  • fast cooling lava
  • small crystals
25
Name the properties of Basalt
Composition (color):Mafic | Texture (crystal size): Fine
26
Name the properties of Gabbro
Composition (color): Mafic | Texture (crystal size): Coarse
27
Name the properties of Granite
Composition (color):Felsic | Texture (crystal size): Coarse
28
Name the properties of Rhyolite
Composition (color):Felsic | Texture (crystal size): Fine
29
Name the properties of Andestite
Composition (color):Intermediate | Texture (crystal size): Fine
30
Name the properties of Pumice
Composition (color):Felsic | Texture (crystal size): Vesicular
31
Name the properties of Scoria
Composition (color):Mafic | Texture (crystal size): Vesicular
32
How are Oceanic and Continental crust different in terms of felsic and mafic rocks?
``` Oceanic crust - Mafic rocks like basalt - Thin layer more dense Continental crust - Felsic rocks like granite - Thick layer less dense ```
33
Describe Partial Melting
- Felsic components of the parent rock tend to go into the liquid state first during partial melting - Partial melting results in magmas that are more felsic in composition than the parent rock - as more of the rock melts during partial melting, the magma becomes more mafic than the original melt that formed
34
What are ores
Deposit from which minerals can be extracted profitably
35
What is grade (in terms of ore)
the amount of valuable mineral in each ton of ore, expressed as troy ounces per ton or grams per tonne for precious metals and as a percentage for other metals.
36
What type of magma is the most likely product of partially melting an intermediate rock?
Felsic Magma