EARTH´S SYSTEM Flashcards

1
Q
  • Any portion of the universe that can be isolated from the rest of the universe for the purpose of observing and measuring changes.
  • Each system of the earth interacts with one another that allows it to support life.
A

System

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2
Q

A self- contained system (in which the boundary permits the exchange of energy, but not matter, with surroundings).

A

Closed System

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3
Q

Energy and matter flow in and out of the system.

A

Open System

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4
Q

The earth after its formation, differentiated into: crust, mantle, and core

A

Geosphere

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5
Q
  • The process that created the earth´s layered structure
  • the denser material sinks to the center )forming the core)
  • the less denser amterial floated to the top forming the crust.
A

Planetary Differentiation

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6
Q

The thinnest layer rangign from 5 to 80 km thick and occupies greater than 1% of the Earth´s volume.

A

Crust

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7
Q

What is the two types of crust?

A
  1. Oceanic crust

2. Continental crust

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8
Q
  • mostly composed of granitic rocks
  • thicker with an average thickness of 35 km
  • less dense (2.7 g/cm3
  • older (some are 4 billion years old)
A

Continental Crust

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9
Q
  • mostly composed of basaltic rocks
  • the denser and thinner crust (3.0 g/cm3)
  • roughly 7 km thick
    Younger (180 million years old or less)
A

Oceanic Crust

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10
Q

The thickest layer occupying 83% of the Earth´s volume

A

Mantle

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11
Q

The boundary between the crust and the mantle which was named after the seismologist, Andrija Mohorovicic.

A

Mohorovicic Discontinuity

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12
Q

How thick is the mantle?

A

2900 km thick

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13
Q

What´s the estimated temperature of the mantle

A

1000 celcius to 3700 celcius

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14
Q

What is the top part of the mantle primarliy composed of?

A

Peridotite (rock)— made up of olivine (Mg, Fe)2 SiO4

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15
Q

The composition is thought to be the most iron and nickel with some oxygen, sulfur, and silicon.

A

Core

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16
Q

This refers to the boundary between the mantle and the core named after the seismologist Beno Gutenburg.

A

Gutenburg Discontinuity

17
Q

This is the denset portion of the Earth with an average density of 11g/cm^3 to nearly 14 the times the density of water.

A

Core

18
Q

This is defined based on the mechanical properties and is observed using the behavior of seismic waves as it travels through the interior of the earth.

A

Layeing by Physical or Mechanical properties

19
Q
  • primary wave

- passes thorugh solid and liquid

A

P Wave

20
Q
  • Shear Wave

- Does not pass through liquid

A

S Wave

21
Q

This is the upper mantle + the crust. This is also relatively rigid and is known to break due to stress and the site of most earthquakes.

A

Litosphere

22
Q

This is what you call the litosphere when its broken down into large fragments

A

Litospheric Plates

23
Q

¨Weak¨(asthenos) sphere which lies below the litosphere from ~100 km until a depth of 660 km. Also, the litosphere floats above this layer and convection is also thought to occur here.

A

Asthenosphere

24
Q

Due to the small amounts of melting present, it flows like the flow of honey, being very slow.

A

Ductile Behavior