Lesson 2 Flashcards

1
Q

Earth’s Layers

A
  1. Crust
  2. Mantle
  3. Outer Core
  4. Inner Core
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2
Q

Thickness: 32km
Materials: granite rocks
Temp: surface temperature
- 1600º F

A

Continental Crust

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3
Q

Thickness: 8km
Materials: basalt rocks
Temp: surface temperature
- 1600º F

A

Oceanic Crust

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4
Q

Thickness: 2,900 km
Materials: Molten rock called magma
Temp: 1600º F - 4000º F

A

Mantle

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5
Q

Thickness: 2,200 km
Materials: Nickel and iron in liquid state
Temp: 4000º F - 9000º F

A

Outer Core

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6
Q

Thickness: 1,250 km
Materials: Nickel and iron in liquid state
Temp: 9000º F ++

A

Inner Core

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7
Q

The Earth’s outermost surface which makes up 1% of the Earth.

Relative to its size, Earth’s crust is about as thin as an apple’s skin.

It is relatively light and brittle so that most earthquakes occur in this layer.

The crust of the Earth is broken into many pieces called plates.

A

Crust

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8
Q

Although the __?__ does have a thin solid layer at the top, it is composed almost entirely of magma - molten rock inside the earth.

A

Mantle

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9
Q

are caused by the very hot magma at the deepest part of the mantle rising to the top, then cooling and sinking to the bottom, and repeating the cycle over again.

A

Convection Currents

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10
Q

The massive pieces of solid rock that float on the molten material in the mantle below.
These plates move on top of the asthenosphere

A

Lithospheric Plates

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11
Q

Pressures and temperatures in this layer are greater than the mantle and crust.

When the Earth rotates, the liquid in the __?__ spins creating the Earth’s magnetic field.

A

Outer Core

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12
Q

Solid innermost layer of the Earth.

It is about 1,250 km thick and has the greatest pressures, temperatures, and the most dense materials of any layer.

A

Inner Core

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13
Q

is a naturally occurring solid aggregate of minerals and/or mineraloids (mineral-like substance).

A

rock

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14
Q

The Earth’s outer solid layer

A

lithosphere

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15
Q

The scientific study of rocks is called

A

petrology

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16
Q

These are rocks that solidified directly from molten magma. (mother rock)

Examples:
Granite
Basalt
Pumice
Flint

A

Igneous Rock

17
Q

These are formed when igneous rocks are eroded as a sediment under the sea.

Examples
Limestone
Chalk
Sandstone

A

Sedimentary Rock

18
Q

These are made up of igneous and sedimentary rocks of all ages which have been subjected to intense pressure.

Examples:
Slate
Marble
Quartzite

A

Metamorphic Rock

19
Q

is the breakdown of rocks at the Earth’s surface, by the action of rainwater, extremes of temperature, and biological activity.

A

Weathering

20
Q

is the process by which soil and rock particles are worn away and moved elsewhere by gravity, or by a moving transport agent – wind, water or ice.

A

Erosion

21
Q

covers much of the land on Earth.

A

Soil

22
Q

Soil Horizons (Layers)

A

O Horizon (humus)
A Horizon (topsoil)
E Horizon (eluviation layer)
B Horizon (subsoil)
C Horizon (regolith)
R Horizon (bedrock)

23
Q

The top, organic layer of soil, made up mostly of leaf litter and humus (decomposed organic matter).

A

O Horizon

24
Q

The layer called topsoil. Seeds germinate and plant roots grow in this dark-colored layer. It is made up of humus (decomposed organic matter) mixed with mineral particles.

A

A Horizon

25
Q

This eluviation (leaching) layer is light in color. It is made up mostly of sand and silt, having lost most of its minerals and clay as water drips through the soil (in the process of eluviation).

A

E Horizon

26
Q

Also called the subsoil. It contains clay and mineral deposits (like iron, aluminum oxides, and calcium carbonate) that it receives from layers above it when mineralized water drips from the soil above.

A

B Horizon

27
Q

Also called regolith. It consists of slightly broken-up bedrock. Plant roots do not penetrate into this layer and very little organic material is found in this layer.

A

C Horizon

28
Q

The unweathered rock (bedrock) layer that is beneath all the other layers.

A

R Horizon

29
Q

(also known as aquake,tremorortemblor) is the result of a sudden release of energy in theEarth’scrustthat createsseismic waves.

A

earthquake

30
Q

> occurred on October 15, 2013, at8:12 a.m.

> It affected the whole Central Visayasregion, particularly Bohol andCebu. at the epicenter was recorded atMw 7.2

A

2013 Bohol earthquake