Chapter 1 Flashcards

1
Q
  1. What is geology, and what is the difference between physical and historical geology?
A

a. Geology- What is it?
i. Scientific study of the Earth and its major systems.
b. Subdivisions
i. Physicial Geology- Study of Earth’s compisition, structure, and the processes that shape it
ii. Historical Geology- Study of Earth’s history and history of life.

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2
Q

GEOLOGY- Why Study It?

A

• Acquiring Knowledge Needed To:
- Obtain natural resources
- Assess and avoid natural hazards
- Prevent or correct environmental damage
• Expanded Awareness of:
- How beautiful and complex Earth is
- How much our survival depends upon understanding how Earth works

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3
Q

THE SCIENTIFIC METHOD

A

• A systematic, logical way of studying how nature works
• Data is gathered which poses questions
• Hypothesis:
- an attempt to explain the data
- often, more than one is proposed
- tests are devised to find which , if any, are true
• theory: a hypothesis that has tested true
• high probability of being valid

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4
Q

Atmosphere

A

Gaseous envelope surrounding Earth

• 78% Nitrogen, 21% Oxygen, and 1% Argon, carbon dioxide, and others

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5
Q

EARTH’S MAJOR COMPONENTS

A
  • Geosphere: from the Earth’s surface to its center
  • Subdivisions:
  • Crust: outermost and thinnest part of Earth. Two types exist
  • Continental: thicker, variable thickness, and granitic average composition
  • Oceanic: thinner, more uniform in thickness, and basaltic composition
  • Mantle: most of Earth’s volume and mass. Denser rock than crust
  • Core: molten outer core, and solid inner core. Iron and nickel composition
  • Hydrosphere: All of Earth’s water
  • 97% is in the oceans
  • Atmosphere: Gaseous envelope surrounding Earth
  • 78% Nitrogen, 21% Oxygen, and 1% Argon, carbon dioxide, and others
  • Biosphere: All life on Earth
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6
Q

• Hydrosphere

A

: All of Earth’s water

• 97% is in the oceans

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7
Q

• Geosphere

A

from the Earth’s surface to its center
• Subdivisions:
• Crust: outermost and thinnest part of Earth. Two types exist
• Continental: thicker, variable thickness, and granitic average composition
• Oceanic: thinner, more uniform in thickness, and basaltic composition
• Mantle: most of Earth’s volume and mass. Denser rock than crust
• Core: molten outer core, and solid inner core. Iron and nickel composition

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8
Q

• Biosphere

A

All life on Earth

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9
Q

DYNAMIC RELATIONSHIP BETWEEN COMPONENTS

A
  • the Earth’s major components exist in “dynamic equilibrium” (changing balance)
  • a change in any one results in a change in all the others.
  • Not necessarily of the same magnitude
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10
Q
  • continental shelves
A

(below sea level): shallow sea

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11
Q
  • continental slopes
A

(below sea level): steeper slope that connects shallow sea to deep sea

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12
Q
  • oceanic ridges
A

undersea mountain range extending through all the oceans

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13
Q
  • transform faults
A

fractures that cut across a ridge at 90 degree shifting it right or left

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14
Q
  • abyssal plains
A

flat parts of deep ocean

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15
Q
  • volcanic island arcs
A

curving chains of volcanic islands that are next to a trench

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16
Q

• Geologic Time

A

vast spans of time ranging from thousands to billions of years
• Implications:
- most of Earth’s features can be explained by observable processes acting over geologic time spans according to natural laws
- often called “the principle of uniformitarianism” “The present is the key to the past.”

17
Q

• The Rock Cycle

A

continual transformation of rocks from one type to another.

• Caused by internal (underground) and external (surface) processes

18
Q
  • igneous
A

formed when melted rock (magma) cools and solidifies.

19
Q
  • Sedimentary
A

formed when rocks weather and erode into sediment then becomes new rock

20
Q
  • Metamorphic
A

formed when rocks recrystallize without melting, due to heat and pressure deep underground

21
Q

The Hydrologic Cycle

A

continuous transfer of water from one repository to another. For example, from sea to the air, then from the air to the land, and then back to the sea

  • primary water source= oceans
  • primary energy source= sun
  • cycle of evaporation, condensation, precipitation, infiltration, and runoff
  • effect on the Earth’s surface: most erosion, and most sediment and sedimentary rock is due to the water cycle.
22
Q

• Plate Tectonics

A

motion and interaction of rigid, interlocking plate-like segments of Earth.
• Plate interaction causes deformation (bending and breaking)
• This results in tectonic (Earth building) activity such as:
- earthquakes
- volcanism
- mountain formation (orogensis)

23
Q

• Lithosphere:

A
  • crust + uppermost mantle joined as a single rigid unit
  • average thickness= 100 km (62 mi)
  • this is what “plates” are made of
24
Q

• asthenosphere

A
  • highly deformable (plastic) upper mantle

- allows plates to move

25
Q

• Divergent:

A
  • as two plates pull apart and move away from one another
  • as they diverge, magma intrudes into cracks and forms new lithosphere
  • almost all occur along the central part (axis) of oceanic ridges
  • earthquakes and volcanic activity occur here
26
Q

• convergent:

A
  • two plates collide and one is forced down under the other into the mantle where it is “recycled”
  • this causes quakes and violent volcanic activity
  • deep ocean trenches mark where one plate slips under the other
  • volcanic island arcs and continental volcanic arcs form next to them
  • when two continental plates collide, a great mountain range is formed
27
Q

• transform:

A
  • two plates are sliding past one another along a transform fault
  • there is neither creation nor destruction of lithosphere
  • quakes and deformation occur
  • features on opposite sides of the boundary are offset