Earth's Composition Flashcards

1
Q

Density equation

A

mass / volume

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2
Q

Density of water

A

1 g/cm^3

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3
Q

Average density of earth

A

5.52 g/cm^3

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4
Q

Earth’s Atmosphere

A

Extends 100km above surface, 77% nitrogen, 21% oxygen, 2% argon, water, carbon dioxide

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5
Q

Oblate Spheroid

A

Earth bulges around equator, slightly squashed sphere, makes gravity weaker at the equator

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6
Q

Crust

A

Outermost layer of earth, DENSITY 3 g/cm^3, 100km thick, continental crust is thick and less dense, and oceanic crust is thin but more dense,

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7
Q

Mantle

A

Majority of earth, hot moving rock in upper mantle (taffy like), moves continents, crust to 2900 km, density 3 g/cm^3 at top and 9 g/cm^3 at bottom

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8
Q

Core

A

Mantle to center of earth, outer core is molten, inner core is solid, creates earth’s magnetic field, density 9 g/cm^3 at top and 13 g/cm^3 at center

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9
Q

Order of Earth’s interior

A

crust - mantle- liquid core - solid core (will need to be able to draw)

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10
Q

Seismic Waves

A

earthquakes, helps us understand the internal structure of earth

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11
Q

P waves

A

Travel through liquid and solids, straight line

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12
Q

S Waves

A

Can only travel through solids, shows us the upper mantle is molted, bounces, important for understanding interior

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13
Q

Plate Tectonics

A

Multiple plates make up earth, move over the mantle to form crevasses, faults, or mountains and volcanoes, driven by CONVECTION CURRENT

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14
Q

Pangea

A

Ancient super continent, we know because continents fit together like a puzzle, fossils match on far away continents, rocks of same ancient types

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15
Q

Earthquake Epicenters

A

Earthquakes are when stress builds up between plates, this energy is concentrated at the epicenter

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16
Q

Divergent Boundaries

A

Plates move away from each other, small earthquakes

17
Q

Convergent Boundaries

A

Plates move towards each other, large earthquakes with volcanic activity

18
Q

Transform Boundaries

A

Plates slide past each other, shallow but destructive earthquakes, San Andreas Fault

19
Q

Ring of Fire

A

High are of tectonic activity, 75% of all earthquakes occur here, where tectonic plates meet, all coastline surrounding pacific ocean

20
Q

Earth’s Magnetic Field

A

generated by movement of molten metal in the outer core (swirls since inner core is warmer), geodynamo (cycle between changing electric and magnetic fields), poles move over time and reverse every 100,000 years

21
Q

Magnetosphere of Earth

A

Magnetic field protects us from solar winds, charged particles circle back to poles, when they hit the atmosphere at the poles aurora occurs

22
Q

Solar Wind

A

Harmful, destroys our atmosphere

23
Q

Color of Aurora

A

Depends on what type of molecules are struck by the charged particles and atmospheric level,
green = oxygen 60 miles up
red = oxygen 300 km up
purple and pink = neutral nitrogen
blue = ionized nitrogen at 100km
(colors is from particles dropping in energy)

24
Q

Aurora Ring

A

Where aurora occurs, circle around poles

25
Q

Earth’s Atmosphere Levels

A

Troposphere - Stratosphere - Mesosphere - Thermosphere

26
Q

Troposphere

A

0-12km, contains 75% of the gases in the atmosphere, where we live and where pretty much all weather occurs, thicker at equator and thinner at poles, temp decreases with altitude

27
Q

Tropopause

A

Layer between troposphere and stratosphere, jet stream is here

28
Q

Stratosphere

A

12-50km, contains ozone layer 15-35km (absorbs and scatters suns harmful UV rays), temp increases with altitude due to absorption of UV radiation

29
Q

Mesosphere

A

50-80km, temp decreases with alt., coldest layer, where meteors burn up due to dense friction

30
Q

Mesopause

A

Coldest part of earth’s atmosphere

31
Q

Thermosphere

A

80-100km, Air is very thin and hot, can reach temps of 2000 degrees C from UV radiation, ISS and auroras are found here

32
Q

Ionosphere

A

Contains charged particles that reflect radio waves, enabling long-distance communication

33
Q

Age of Earth

A

4.55 billion years, we know from radiometric dating (measuring decay of radioactive material, half-life)

34
Q

Carbon Dioxide levels in the atmosphere due to fossil fuel usage

A

Shot WAY up

35
Q

What carbon dioxide does to earth

A

raises earth’s temp, traps heat

36
Q

Representative Concentration Pathway (RCP)

A

Predictor of how CO2 levels will affect earth depending on their levels

37
Q

Effects of Climate Change

A

higher storm surges, rising sea levels, thermal expansion (water molecules spreading out as they get warmer), stronger storms, heatwaves, melting glaciers, acidic ocean, food insecurity, climate refugees, loss of biodiversity