EARTH Flashcards

1
Q

is a Germanic word, which simply means “the ground.”

only the fifth largest planet in the solar system, it is the only world in our solar system with liquid water on the surface.

the third planet from the Sun, and the only place we know of so far that’s
inhabited by living things

A

EARTH

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2
Q

FACTS

A

Age: 4.543 billion years
Distance from Sun: 149.6 million km
Gravity: 9.807 m/s2
Radius: 6,371 km
Mass: 5.972 × 10^24 kg
Population: 7.888 billion (2021)

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3
Q

LAYERS OF EARTH

A

the crust, the mantle, the outer
core, and the inner core.

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4
Q
  • describes the outermost shell of a terrestrial planet

-is generally divided into older, thicker continental crust and younger, denser
oceanic crust.

is the outer layer of the Earth. It is a thin layer between 40 – 60 km thick.

its lightest, most buoyant rock layer. Continental crust covers 41
percent of the Earth’s surface, though a quarter of that area is under the oceans.

A

EARTH CRUST

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5
Q

convergent boundaries occur when a tectonic plate primarily composed of oceanic lithosphere collides with a plate with continental lithosphere. Oceanic crust is much thinner, averaging about
6 km (4 miles) in thickness.

A

OCEANIC-CONTINENTAL

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6
Q

occur when a tectonic plate primarily composed of oceanic lithosphere collides with a plate with continental lithosphere

A

convergent boundaries

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7
Q

is typically 40 km (25 miles) thick continental crust, the outermost layer of
Earth’s lithosphere makes up the planet’s continents and continental shelves and formed near subduction zones at plate boundaries between continental and oceanic tectonic plates.

A

CONTINENTAL CRUST

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8
Q

sits between Earth’s dense, very hot core and its thin outer layer, the crust

plays an important role in the evolution of the crust and provides the thermal
and mechanical driving forces for plate tectonics.

is about 2,900 kilometers (1,802 miles) thick, and makes up a whopping 84
percent of Earth’s total volume.

A

MANTLE

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9
Q

extends from the crust to a depth of about 410 kilometers (255 miles).

mostly solid, but its more malleable regions contribute to tectonic activity.
Two parts of the upper mantle are often recognized as distinct regions in Earth’s interior: the
lithosphere and the asthenosphere.

A

UPPER MANTLE

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10
Q

The lower level of the mantle, it is softer and weaker, particularly in its upper portion where a small amount of melting can occur.

A

asthenosphere

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11
Q

The lower level of the mantle, it is softer and weaker, particularly in its upper portion where a small amount of melting can occur.

extends from about 660 kilometers (410 miles) to about 2,700 kilometers
(1,678 miles) beneath Earth’s surface.

is hotter and denser than the upper
mantle and transition zone. The lower mantle is much less ductile than the upper mantle and
transition one.

A

LOWER MANTLE

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12
Q

starts around 5,000 km below the surface of the planet, and is thought to be
made of solid iron and nickel, due to the extreme pressure forcing the atoms of the metal to
pack together.

A

inner core

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13
Q

is made of two layers: the outer core, which borders the mantle, and the inner core.
The boundary separating these regions is called the Bullen discontinuity.

is responsible for the generation of Earth’s magnetic field.

contains information regarding the earliest history of accretion of the planet.

A

CORE

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14
Q

about 2,200 kilometers (1,367 miles) thick, is mostly composed of liquid iron and
nickel. The NiFe alloy of the outer core is very hot, between 4,500° and 5,500° Celsius (8,132° and
9,932° Fahrenheit).

A

OUTER CORE

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15
Q

is a hot, dense ball of (mostly) iron. It has a radius of about 1,220 kilometers (758 miles).
Earth’s inner core is as hot as the surface of the sun—about 10,000oF (5,500oC). Also, inner core is
solid metal

A

INNER CORE

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