Ch. 12 - The Dynamic Planet Flashcards

1
Q

Who was the first person to look at the age of the earth?

A

Archbishop James Ussher in the 1650’s

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2
Q

Who was James Hutton and what did he propose?

A

He proposed the Principle of Uniformitarianism in the 1790s.

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3
Q

What is the Principle of Uniformitarianism?

A

This principle claimed that basic geologic processes don’t change over time, they always stay the same

“The present is the key to the past”

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4
Q

What are the two methods of dating geologic formations?

A

Relative Dating

Absolute Dating

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5
Q

What is the Principle of Original Horizontality?

A

States that layers of sediment are originally deposited horizontally under the action of gravity. Sediments, at the bottom of a lake for example, will be oriented horizontally, as long as it’s not disturbed

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6
Q

What is the Principle of Superposition?

A

In any undisturbed sequence of rocks deposited in layers, the youngest layer is on top and the oldest on bottom

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7
Q

What is the Principle of Cross-Cutting Relationships?

A

States that the geologic feature which cuts another is the younger of the two features

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8
Q

What is the difference between Relative Dating and Absolute Dating?

A

Relative Dating: Puts geologic events into more of a sequence of events.

Absolute Dating: Provides actual dates or date ranges, in numbers of years, for rocks.

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9
Q

What is an Isotope?

A

Groups of a certain element (Carbon, Hydrogen, Oxygen, etc) that have different Atomic Masses (12C, 13C, 14C)

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10
Q

How can the Absolute Date of an element/specimen be determined?

A

Radioactive decay is the key.

By calculating the atomic mass, and then referring to the half-life of that specific isotope, the absolute age of the chemical element can be determined

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11
Q

What is the sequence of layers of earth, starting from Core?

A

Core—-Moho Discontinuity—Mantle—Guttensberg Discontinuity—Core

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12
Q

How is the earth’s core composed?

A

There is the Inner and Outer layers of the core

Inner core is solid, and has the highest density

Outer core is molten (composed of iron)

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13
Q

How is the earth’s Mantle composed?

What are the layers ?

A

Lower Mantle - Upper Mantle - Asthenosphere - Uppermost Mantle

Mantle makes up 80% of the earth’s volume, and is made up of solid minerals

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14
Q

How is the Asthenosphere composed?

A

Asthenosphere is not solid, behaves like plastic. All the material above the asthenosphere has immense weight, so the asthenosphere materials below begin to deform.

A driving force in the process of plate tectonics

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15
Q

What are the two types of earth’s crust?

A

Oceanic + Continental

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16
Q

What are the characteristics of Oceanic Crust?

A

Density of 3.0g/cubic centimetre

Mainly composed of Magnesium and Silica (Magnesium is what makes it dark in color)

5km thick on average

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17
Q

What are the characteristics of Continental Crust?

A

Density of 2.7g/cubic centimetre

Mainly composed of Silica and Aluminium minerals

Thickness between 30-60km

18
Q

What is the definition of a “Mineral”?

A

A natural, inorganic solid substance with fixed proportion of elements and definitive crystalline structure. (ex: NaCl, SiO2)

  1. Has to be natural
  2. Inorganic
  3. Solid (Ice is a mineral, water is not)
  4. Fixed proportion of elements
  5. Definitive crystalline structure
19
Q

Which elements make up most of the earth crust’s weight?

A

Oxygen (46%)

Silicon (27%)

Aluminium (8%)

20
Q

What are the six mineral identification methods?

A
  • Luster (how well it reflects light)
  • Colour and streak (color it leaves when you scratch it on a tile)
  • Hardness
  • Cleavage and fracture
  • Heft / Specific Gravity (weight and buoyancy)
  • Reaction with acid
21
Q

What is the definition of a “Rock”?

A

Rock or stone is a natural substance, a solid aggregate of one or more minerals or mineraloids

22
Q

How are Igneous Rocks formed?

A

From the cooling and solidification of magma or lava

23
Q

What is Extrusive Igneous Rock?

A

Magma that cools above the surface of the earth; BASALT, PUMICE, OBSIDIAN

24
Q

What is Intrusive Igneous Rock?

A

Intrusive igneous: Magma that cools below the earth’s surface; GRANITE; GRANODIORITE

25
Q

What is the general composition of Igenous Rock?

A

Felsic (composed of Iron and Silicon)

Mafic (Magnesium; dark in color)

26
Q

What are the two primary sources of Sedimentary Rocks?

A
  1. Clastic (composed of fragments of other rocks)
    Ex: CONGLOMERATE, SANDSTONE, SHALE
  2. Chemical (made through chemical processes)
    Ex: LIMESTONE, COAL
27
Q

What is the order of clastic sedimentary rocks in terms of clast size; biggest to smallest?

A

Breccia/Conglomerate, Sandstone, Siltstone (mudstone), Shale

28
Q

How are Metamorphic Rocks formed?

A

The original rock is subjected to heat and pressure, causing profound physical or chemical change

29
Q

What does foliated and non-foliated mean?

A

Foliation forms when pressure squeezes the flat or elongate minerals within a rock so they become aligned. These rocks develop a platy or sheet-like structure that reflects the direction that pressure was applied in

30
Q

What are common Non-foliated rocks?

A

Marble comes from Limestone

Quartzite comes from Sandstone

31
Q

What are common Foliated rocks?

A

Schist comes from Shale

Gneiss comes from Granite

32
Q

Who originally proposed, but couldn’t prove, the theory of Plate Tectonics / Continental Drift?

A

Alfred Wegener in the early 20th Century

33
Q

How many tectonic plates are on the earth’s lithosphere?

A

14

34
Q

How fast do tectonic plates move on average?

A

A few centimetres per year

35
Q

What are the characteristics of Divergent plate boundaries?

A

Oceanic: Rising of magma pushes the oceanic crust up slightly higher, not perfectly horizontal. A ridge is created.

Continental: Separation of continental crust forms a break in the layer, giving things like a magma a chance to rise through the crust, and potentially reach the earth’s surface

Volcanoes can be formed in this process, as well as rift valleys when continental crust separates faster than magma rises

Mid-Atlantic Ridge

36
Q

What can happen if two Oceanic plates converge?

A

Subduction can occur, if one plate is denser than the other

Trenches can be formed, like Mariana’s trench

Volcanic Island Arcs can form/ Volcanoes

Earthquake can happen

37
Q

What can happen as a result of Oceanic and Continental plates converging?

A
  • When one slab of oceanic crust and a slab of continental crust converge
  • The oceanic crust is denser, so it sinks beneath the continental.
  • Moving deeper and deeper into the earth, the oceanic crust heats up, magma forms, and rises to the earth’s surface creating volcanoes and mountains.
  • Earthquakes can also happen in these boundaries, as well as trenches
  • This example describes Vancouver’s geographic location and physical surroundings.
38
Q

What can happen from two Continental plates converging?

A
  • It’s easier for crust to move upwards when the densities are the same, as opposed to them both sinking.
  • There is still a lot of friction, which can result in earthquakes
  • Volcanoes are unlikely to form in this process, because there is no magma being formed or heating up. Non-volcanic mountains are the usual formation
39
Q

What is the general outcomes of Transform boundaries?

A

Earthquakes, occasionally very intense ones

40
Q

How do you know if it’s a Right Lateral or Left Lateral transform boundary?

A

The direction each plate moves in respect to the other, if you were standing facing the boundary.