Ch 1: Foundation of the Earth Flashcards

1
Q

What makes an idea scientific?

A

It can tested against observation or experiment

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2
Q

Earth Science is primarily an _______ science.

A

observational

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3
Q

What are Principles

A

Generalizations with exceptions. eg: Principle of Superposition, exception: overturned strata in mountain belts

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4
Q

What is the Principle of Uniformitarianism

A

James Hutton - Ancient features of the Earth are best interpreted in terms of processes that operate at the present day. aka Hutton’s unconformity

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5
Q

What is the Principle of Actualism

A

Ancient features of the Earth are to be interpreted in terms of physical and chemical processes that operate at the present day

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6
Q

What are Laws

A

applied to theories which are very well established and for which no exceptions are known. eg: Law of conservation of energy

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7
Q

Geophysicists

A

Magnetism, gravity, seismic waves

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8
Q

Geologists

A

Mapping, field observations, sampling, chemicla analyses

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9
Q

Paleontologists and Biogeographers

A

Paleontologist: fossils and history of life.
Biogeographers: distribution of living things at the present day.

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10
Q

Hydrologists and Oceanographers

A

Liquid water on the Earth’s surface, sediments deposited on the sea floor

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11
Q

Glaciologists

A

Behavior and distribution of ice. Materials deposited on the landscape by ice

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12
Q

Atmospheric Scientists

A

Meteorologists and climatologists: physics of the atmosphere. Short-term (weather) Long-term (climate)

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13
Q

What is a system?

A

A portion of the universe that can be separated from the rest for the purpose of observing changes>

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14
Q

What is an isolated system?

A

No matter or energy lost or gained.

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15
Q

What is a closed system?

A

No matter lost or gained, energy may be exchanged with surroundings. Earth is a closed system.

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16
Q

What is an open system?

A

Matter and energy exchanged with surroundings

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17
Q

What system is Earth?

A

An almost closed system. Amouts are negligible.

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18
Q

Systems within Earth

A

Atmosphere, Biosphere, Hydrosphere, Geosphere

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19
Q

What are Cycles

A

cycles trace the flow of material or energy through a system. Energy cycle, hydrologic cycle, rock cycle.

20
Q

What is a budget?

A

When a cycle is quantified

21
Q

The Energy Cycle/Budget

A

Drives all the processes that we see operating on the Earth.

22
Q

Energy Pathways inputs

A

Energy inputs: solar radiations, geothermal energy, tidal energy

23
Q

Energy Loss

A

Reflected into space, re-radiated

24
Q

Solar Radiation

A

Energy comes from the sun as light, UV and other types of radiation. About 1.74 x 10^17 watts or 174000 tW

25
Q

Where does Solar Energy go?

A
  • 30% reflected into space (52000tW)
  • < 50% converted to heat and re-radiated (81000tW)
  • < 25%% melts ice and evaporates water into hydrosphere (40000tW)
  • 350tW are converted to winds, currents, waves
  • 40tW captured by living things
26
Q

Geothermal Energy and where does it go?

A

Energy is released within the Earth by slow breakdown of radioactive elements. (about 32tW)

  • Volcanoes and hot springs (0.3tW).
  • Volcanoes under the sea (11tW)
  • Heat loss/Conduction (21tW)
  • Converted into movement: lava. geysers, plate tectonics.
27
Q

Tidal Energy and where does it go?

A

Gravity of the moon raises a bulge in the ocean surface. (27tW)
- Ultimately converted to heat as water moves over the solid Earth.

28
Q

Hydrologic Pathways: Evapotranspiration

A

Evaporations: from the surface water, land
Transpiration: from plants

29
Q

Hydrologic Pathways: Condensation and precipitation

A

Condensation: clouds
Precipitation: rain, snow

30
Q

Hydrologic Pathways: Surface and subsurface flow

A

Melting
Surface flow: glaciers, streams, rivers
Infiltration
Groundwater movement

31
Q

Hydrologic Reservoirs

A

Oceans (97.5%)
Ice Sheets (1.85%)
Groundwater (0.64%)
Lakes, rivers, atmosphere (0.01%)

32
Q

Residence Time

A

Size of reservoir / flow rate = residence time
A measure of how long the average water molecule spends in the reservoir.
Oceans/icecaps: 1000s of years
Streams and rivers: a few weeks
Atmosphere: a few days

33
Q

The Rock cycle

A

Cycling of rock material at surface of the Earth.

34
Q

What is Magma?

A

Molten rock that is underground: solidifies slow = bigger crystals

35
Q

What is Lava?

A

Molten rock on the surface: solidifies fast = smaller crystals

36
Q

How to tell where the magma solidified?

A

Crystal size

37
Q

Temperature range of Magma/Lava

A

800C - 1200C

Felsit (silica rich, pale) - Mafic (iron and magnesium rich, dark)

38
Q

Igneous Rock

A

cooling and solidification: granite and pillow lava

39
Q

Weathering

A

reactions, creature interactions, not erosion. Happens in situ (in place) no movement. Chemical/physical reaction in the material.

40
Q

Erosion

A

caused by exposure. requires transportation. The wearing away of land or soil by the action of wind, water or ice.

41
Q

Sediment

A

Reduced pieces. May be deposited

42
Q

Sedimentary Rock

A

Lithification

43
Q

Lithification

A

the process in which sediments compact under pressure

44
Q

Metamorphism

A

Heat and pressure, without melting

45
Q

Metamorphic rocks

A

New minerals, change in texture, fabric