Week 4 - Earth Materials Flashcards

1
Q

Why are framework silicates stable?

A

Each silica is sharing its oxygen with another silica atom, making more bonds, the stronger structure is stable.

Made up of one silica (Si4+) and four oxygens (O)
Have a tetrahedral shape, meaning that they can polymerase.

Individual tetrahedra may be polymerized by sharing oxygen atoms between tetrahedra e.g.
rings, chains, sheets, frameworks

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2
Q

What binds minerals in igneous rocks together?

A

Silicate minerals are bound by tetrahedral structures

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3
Q

What is a felsic rock?

A
  • felsic mineral (light colour, low density) e.g. feldspar, quartz
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4
Q

What is a mafic rock?

A
  • mafic mineral (dark colour, high density) e.g. mica sheets, pyroxenes (single chains), Olivines (isolated tetrahedra)
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5
Q

What is the difference between contact and regional metamorphic processes?

A
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6
Q

Is the rock cycle a true cycle?

Why is it important ?

A

Yes

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7
Q

What are the rock forming minerals?

A
Silica (Si)
Oxygen (O)
Aluminium (Al)
Iron (Fe) 
Calcium (Ca) 
Sodium (Na) 
Potassium (K) 
Magnesium (Mg)
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8
Q

List the 3 broad classes of rocks

A
  1. Igneous rocks - formed by solidification of magma - can be extrusive and intrusive
  2. Sedimentary rocks - aggregates deposited by transporting medium such as water, wind or ice; deposits of organic origin; chemical properties
  3. Metamorphic rocks - describe change in mineral assemblage and textures due to elevated temperatures and pressure
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9
Q

What are the implications for these Earth Materials on the landscape?

A
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10
Q

What are the differences between Minerals and Rocks?

A

Minerals - naturally occurring inorganic chemical compounds’ having a specific internal structure and regular chemical composition

Rocks - are natural mixture or aggregates of minerals

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11
Q

What is a Mineral?

A
  • Mostly crystaline
  • Have specific physical properties which reflect both their composition and atomic structure and affect rate of weathering
  • silicates are the most common minerals (make up 95% of Earths crust)
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12
Q

Describe Silicates

A

Made up of one silica (Si4+) and four oxygens (O)
Have a tetrahedral shape, meaning that they can polymerase.

Individual tetrahedra may be polymerized by sharing oxygen atoms between tetrahedra e.g.
rings, chains, sheets, frameworks

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13
Q

What is an Igneous Rock?

What is it made up of?

A
  1. Igneous rocks - formed by solidification of magma, can be..
    Extrusive (volcanic) - cool rapidly at Earth’s surface, fine crystal grain size
    Intrusive (plutonic) - crystallise deep below the surface and cool slowly, coarse grain size
  2. Mostly made of silicate minerals
    - felsic mineral (light colour, low density) e.g. feldspar, quartz
    - mafic mineral (dark colour, high density) e.g. mica sheets, pyroxenes (single chains), Olivines (isolated tetrahedra)
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14
Q

Intrusive Rock Structures

A

Structures when they solidify under the surface:

  • Batholiths - largest
  • Dykes - vertical structures, magma solidified in fractures
  • Sills - horizontal sheets of solidified magma
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15
Q

What is the origin of magma?

A

Basalt Magma - generated from partial melting of ultramafic rocks in the asthenosphere

Granite Magma - generated from partial melting of rocks in lower crust

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16
Q

What are Sedimentary rocks?
List the minerals
List the 3 types

A

Sedimentary rocks - aggregates deposited by transporting medium such as water, wind or ice; deposits of organic origin; chemical properties. *often form in layers or strata

Common minerals:
Quartz - stable and weathering resistant
Clays - formed by weathering feldspar
Carbonates - formed as shells or preciptates

  1. Clastic - fragments of clasts/rocks and mineral particles from weathering and erosion (separated based on particle size) e.g. sandstone, mudstone
  2. Chemical - material carried in solution is precipitated (evaporation) e.g. rock salt
  3. Organic - accumulated remains of plants and animals e.g. limestone
17
Q

What are Metamorphic rocks?

A

Metamorphic rocks - formed from preexisting rocks that have been altered by external forces - describe change in mineral assemblage and textures due to elevated temperatures and pressure

  • have recrystallised in solid state due to changed physical conditions
  • have internal planar structure called ‘foliation’due to alignment micas
  • materials mainly silicates
  • from metamorphism of sedimentary rocks include slate, schist, gneiss
18
Q

What is Dissolution?

A
19
Q

What is Oxidation?

A
20
Q

What is Hydrolysis?

A
21
Q

What is Relief? Slope? Aspect? Topography?

A

Relief - the difference between the highest and lowest point

Slope - relief/run

Aspect - direction of the slope, you tell by the way you are facing the slope

Topographic position - you draw a line along the map, highest point on that line