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GR 11 > EARTH SCIENCE > Flashcards

EARTH SCIENCE Flashcards

1
Q

AGE OF EARTH

A

4.543 billion years old

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2
Q

a collective layer of gas that envelopes the Earth.

A

Atmosphere

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3
Q

Earth’s four major spheres

A

Atmosphere
Hydrosphere
Biosphere
Geosphere

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4
Q

(1) It shields the Earth and its inhabitants from harmful ultraviolet (UV) radiation from the Sun;
(2) it maintains the warmth of the Earth’s surface; and
(3) it contains all of the essential gases needed to support life.

A

Atmosphere

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5
Q

refers to the bodies of water consisting of freely flowing bodies of water found on the surface of the Earth

A

Hydrosphere

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6
Q

refers to the narrow band on the Earth’s surface where all biological life resides.

A

Biosphere

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7
Q

This sphere covers nearly 71% of the Earth’s surface.

A

Hydrosphere

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8
Q

the largest out of all the spheres, extending from the surface of the Earth down to its center.

A

Geosphere

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9
Q

Layers of Earth Based on Compositional Differences

A

Crust
Mantle
Core

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10
Q

This is the thinnest and outermost layer of the Earth.

A

Crust

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11
Q

two types of crust

A

the continental and oceanic crust.

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11
Q

younger and denser type of crust.

A

oceanic crust.

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12
Q

comprises most of the Earth’s volume

A

Mantle

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13
Q

The boundary between the crust and mantle

A

Mohorovičić discontinuity

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14
Q

core begins at the mantle-core boundary

A

Gutenberg discontinuity

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15
Q

divided into the upper and lower mantle, separated by

A

Repetti discontinuity.

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16
Q

its composition comprises a Fe-Ni (iron and nickel) alloy.

A

Core

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17
Q

Layers of Earth Based on Physical Properties

A

Lithosphere
Asthenosphere
Mesosphere
Outer Core
Inner Core

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18
Q

thick and brittle layer comprising the entire crust and uppermost layer of the upper mantle.

A

Lithosphere

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19
Q

Contrary to popular belief, it is not a “sea of molten rock.” The upper mantle comprises an Mg- and Fe-rich rock called

A

peridotite.

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20
Q

mechanically weak layer consisting of the lower portion of the upper mantle, extending to 660 km.

A

Asthenosphere

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21
Q

-comprised of the lower mantle
-is much stronger and flows with more resistance. Because of the immense pressure from the overlying layers, the strength of this layer increases with depth.

A

Mesosphere

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22
Q

The dominant rock type in this layer (Mesosphere) is a silicate rock called

A

perovskite.

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23
Q

Layer the only one made out of liquid

A

Outer Core

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24
Q

Core’s flow of liquid metals is responsible for the

A

Earth’s magnetic field

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25
Q

The outer-inner core boundary is also known as

A

Lehmann discontinuity.

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26
Q

To be considered a mineral:

A

Naturally-occurring
Inorganic
Homogeneous solid
Has definite chemical composition
Ordered crystalline structure

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26
Q

It refers to the wavelengths of light reflected by the minerals. While it can be tempting to identify a mineral based on its-, it is the least valuable property because many minerals can occur in different colors.

A

Color

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27
Q

It describes how light is reflected from the mineral’s surface.

A

Luster

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28
Q

This refers to the shape of each crystal or an aggregate of crystals.

A

Crystal Habit or Shape.

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29
Q

his is the color of the mineral when it is powdered.

A

Streak

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30
Q

This refers to how resistant a mineral is to scratching.

A

Hardness

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31
Q

refers to the tendency of a mineral to break along preferred planes called zones of weakness.

A

Cleavage or Fracture

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32
Q

This refers to the ratio between a mineral’s weight and the weight of a specific volume of water

A

Density or Specific Gravity

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33
Q

This describes how well a mineral handles stress, such as breaking, crushing, bending, or tearing.

A

Tenacity

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34
Q

This refers to how well light travels through a mineral.

A

Diaphaneity

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35
Q

This describes the magnetic property of a mineral

A

Magnetism

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36
Q

This describes a mineral’s reaction to a strong acid

A

Effervescence

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37
Q

Geologist licking rocks

A

Odor and Taste

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38
Q

-most common mineral group
-most abundant blocks

A

silicates

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39
Q

less abundant mineral group

A

non-silicates

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40
Q

are formed when molten material cools and solidifies.

A

Igneous Rocks

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41
Q

When igneous rocks form below the surface of the Earth

A

intrusive igneous or plutonic rocks

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42
Q

When igneous rocks form on the surface

A

extrusive igneous or volcanic rocks.

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43
Q

are formed from loose material called sediments that have been eroded in weathering and then buried and compacted in a process called diagenesis.

A

Sedimentary Rocks

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44
Q

are classified based on the characteristics of their clasts, such as size, angularity/roundedness, and sorting.

A

Clastic Sedimentary Rocks

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44
Q

Chemical sedimentary rocks are formed when water evaporates, leaving behind dissolved minerals. Common examples include halite or rock salt, gypsum, flint, chert, travertine, umber, and limestone rocks.

A

Non-clastic Sedimentary Rocks

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45
Q

When a rock is subjected to certain chemical (addition or removal of chemicals) or physical (change in temperature or pressure) processes that alter its chemical composition, mineralogy, and/or texture

A

Metamorphic Rocks

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46
Q

Type of metamorphic tock that is a rock is the result of deformation

A

foliated rocks.

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47
Q

Type of metamorphic rock usually develop in environments where deformation is minimal and other factors, such as chemically-active fluids, play a larger part in altering the rock.

A

Nonfoliated rocks

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48
Q

geological process in which earth materials are weathered and transported

A

Erosion

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49
Q

Land and water forms in this environment can be found on land and usually involve freshwater.

A

Terrestrial Environments

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50
Q

represent the interface between land and sea. It is here where freshwater meets with seawater.

A

Transitional Environments

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51
Q

These environments can be found in the open waters, from the shallow depths to the deepest portions of the ocean.

A

Marine Environments

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52
Q

branch of geology that studies rock layers, beds, or strata

A

Stratigraphy

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53
Q

the layers on the bottom are the oldest, while the layers above are younger.

A

Law of Superposition

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54
Q

Each stratum extends laterally until it encounters a barrier or obstacle.

A

Law of Lateral Continuity

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55
Q

Strata are deposited horizontally.

A

Law of Original Horizontality

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56
Q

If a geologic body (like an intrusion) or discontinuity (like a fault) cuts across strata, it must be younger than the strata it cuts.

A

Law of Cross-cutting Relationships

57
Q

igneous rock body that forms when magma cuts through sedimentary layers and solidifies before it reaches the surface.

A

intrusion

58
Q

Father of English Geology

A

William Smith

59
Q

Sedimentary strata may contain fossils of plants and animals in a definite and invariable sequence. Thus, the age of a stratum and another stratum in a different location can be correlated if they share the same fossil assemblage.

A

Principle of Faunal Succession

60
Q

the “missing time” represented by the unconformity in a rock sequence.

A

hiatus

61
Q

This type of unconformity is present when there is a missing stratum or strata in the sequence, usually due to a period of non-deposition or erosion.

A

Disconformity

62
Q

When strata are disturbed by forces that cause folding, tilting, and/or faulting, they no longer appear horizontal. The surface is then exposed to erosion, and another set of sedimentary strata is soon deposited on top of the disturbed sequence.

A

Angular unconformity

63
Q

This occurs when sedimentary strata are deposited on top of igneous or metamorphic rock bodies.

A

Nonconformity

64
Q

identifying the age of strata in relation to other strata in a method called

A

relative dating

65
Q

Determining the absolute age of a layer requires certain techniques collectively known as

A

absolute dating.

66
Q

Radioactive isotopes are unstable (parent isotopes) and lose subatomic particles or energy over time in a process called

A

radioactive decay.

67
Q

is the study of fossils linking concepts of geology and biology

A

Paleontology

68
Q

This occurs when pores and open spaces in tissue (such as bone and wood) are filled with minerals precipitated from mineral-rich solutions such as groundwater.
An example of - at work is when silica precipitates inside the wood’s pores, creating petrified wood.

A

Permineralization

69
Q

When organisms buried in sediment dissolve or decay away, it leaves behind a hollow space called - in the organism’s shape. If minerals eventually fill in this hollow space, a - is made.

A

mold and cast

70
Q

These organisms are preserved when they fall into a viscous tree sap which hardens into -

A

amber

71
Q

Soft-bodied organisms and delicate plant parts can be conserved via -. This happens when these organisms are buried in sediment and eventually dissolve, leaving behind a thin layer of carbon outlining the organism’s shape.

A

Carbonization

72
Q

Organisms can also be exceptionally preserved when they are encased in ice

A

Freezing

73
Q

can tell a lot about how an organism lived–how it moved, what it ate, and other types of behavior.

A

trace fossils

74
Q

tool geologists use to classify and date rocks and fossils. Instead of numerical ages, time is divided into eons, eras, periods, epochs, and ages

A

The Geologic Time Scale

75
Q

era; The formation of the Earth; magma ocean; intense bombardment of space bodies (“Late Heavy Bombardment”)

A

Hadean Eon

76
Q

era; Life begins as prokaryotic bacteria; Blue-green algae start to produce oxygen in the atmosphere

A

Archean Eon

77
Q

era; Multicellular life emerges

A

Proterozoic Eon

78
Q

era; Multicellular life flourishes and diversifies (“Cambrian Explosion”)

A

Cambrian Period

79
Q

era; “Age of Invertebrates”

A

Ordovician Period

80
Q

era; Emergence of plants on land

A

Silurian Period

81
Q

era; “Age of Fishes”; Towards the end, true amphibians emerged

A

Devonian Period

82
Q

era; “Age of Amphibians”

A

Carboniferous Period

83
Q

Amphibians diversified; large coal swamps formed

A

Mississippian

83
Q

Emergence of reptiles

A

Pennsylvanian

83
Q

era; Existence of Pangaea; the largest mass extinction in Earth’s history occurred towards the end (“The Great Paleozoic Extinction”)

A

Permian Period

84
Q

era; Dinosaurs emerged; start of the Age of Reptiles; first true mammals (therapsids) emerged as well

A

Triassic Period

85
Q

era; Dinosaurs dominated the Earth; the first birds emerged

A

Jurassic Period

85
Q

era; first flowering plants emerged (angiosperms); marked the end of the Age of Reptiles with the Cretaceous-Tertiary Extinction (“K-T Extinction”)

A

Cretaceous Period

86
Q

era; start of the Age of Mammals

A

Paleogene Period

87
Q

era; Mammals and birds evolved into modern forms; hominids, the ancestors of humans, appeared towards the end

A

Neogene Period

88
Q

Evidence of Continental Drift Theory

A

Continental Jigsaw Puzzle
fossils
Similar rock types and geologic features
ancient climates

89
Q

New oceanic crust forms in the axis of this ridge system. Because of this, rocks become progressively older and thicker with sediment away from the axis.

A

seafloor spreading

90
Q

7 Major Plates

A

African plate
Antarctic plate
Eurasian plate
Indo-Australian plate
North American plate
Pacific Plate
South American plate

91
Q

Minor plates

A

Philippine Sea plate
Juan de Fuca plate
Cocos plate
Nazca plate
Scotia plate and
Arabian plate

92
Q

are formed when two plates move apart relative to each other.

A

Divergent Plate Boundaries (Constructive Margins)

93
Q

are the sites where plates move towards each other

A

Convergent Boundaries (Destructive Margins)

94
Q

a collision or one plate going under the other

A

subduction process

95
Q

When an oceanic plate converges with a continental plate

A

Oceanic-Continental Plates Convergence - Mariana Trench

96
Q

occur when two continental plates move towards each other.

A

Continental-Continental Plates Convergence - Himalayan mountain range

97
Q

Because continental crust is too thick and buoyant to be subducted, most crustal material is deformed and pushed up instead. This results in the accumulation of sediments and rocks along the margin, forming mountain belts in a process called

A

orogeny

98
Q

when two oceanic plates collide.

A

Oceanic-Oceanic Plates Convergence - volcanic island arc or island arc.

99
Q

two plates sliding past each other

A

Transform Plate Boundaries (Conservative Margins)

100
Q

are linear breaks on the ocean floor that run perpendicular to oceanic ridges.

A

Fracture zones

101
Q

occur when one block of earth slips past another block along surfaces called faults or fault planes and generates ground shaking.

A

Earthquakes

102
Q

are waves that travel through the interior of the Earth.

A

Body Waves

103
Q

These are the fastest seismic waves and can travel through solid, liquid, and gas. These waves push and pull the rocks in the direction the wave is traveling. They are also called compressional waves because of this behavior.

A

Primary Waves

104
Q

These waves cause the rocks to shake up and down at right angles to the direction of the traveling wave. They are also called shear waves.

A

Secondary Waves

105
Q

waves that can only travel on the surface of the Earth

A

Surface waves

106
Q

These waves are responsible for shaking the ground horizontally and vertically in an S-like pattern.

A

Love Waves

107
Q

These waves move in a rolling motion similar to ocean waves.

A

Rayleigh Waves

108
Q

is the study of earthquakes.

A

Seismology

109
Q

refers to the qualitative measurement of ground shaking at a particular location, depending on the damage to property, life, and nature.

A

intensity

110
Q

the size of the earthquake.

A

Magnitude

111
Q

The hanging wall moves down relative to the footwall in a normal fault.

A

Normal Faults

112
Q

the hanging wall moves up relative to the footwall.

A

Reverse Faults

113
Q

blocks move horizontally to one another due to shearing forces.

A

Strike-Slip Faults

114
Q

ombining shearing and tensional or compressional forces would result in an

A

Oblique-Slip Faults

115
Q

form of mass wasting where large amounts of earth move down a slope under the influence of gravity.

A

landslide

116
Q

sudden sinking of the Earth’s surface due to the movement of the earth underneath.

A

Subsidence

117
Q

sudden sinking of the Earth’s surface due to the movement of the earth underneath but occurs when sediments are saturated with water.

A

Liquefaction

118
Q

geological process where hot molten rock from underneath the earth reaches the surface through an opening in the ground.

A

Volcanism

119
Q

describes how the molten material was ejected, whether it was violent (explosive eruptions), non-explosive (effusive eruptions), or what caused the eruption (hydrothermal, phreatic, phreatomagmatic, etc.).

A

eruption

120
Q

The hot, molten material is called - when it’s underground

A

magma

121
Q

The hot, molten material is called - when it reaches the surface.

A

lava

122
Q

are large dome-shaped volcanoes with broad gentle slopes and large craters.

A

Shield Volcanoes

123
Q

volcano that are steeper and have smaller craters They are usually made up of loose pyroclastic material called scoria, a dark-colored igneous rock that is highly vesicular (has lots of vesicles or cavities) and made from extruded basaltic magma.

A

Cinder cones

124
Q

volcano that’s symmetrical steep-sided cone-shaped morphology. Alternating layers of viscous andesitic lava flows, volcanic ash, and cinders are responsible for their shape.

A

composite volcano

125
Q

is the primary source of precipitation and cloud formation in the atmosphere and, thus, a significant factor when predicting the weather.

A

Water Vapor

126
Q

These are minuscule solid and liquid particles that are suspended in the air. - include smoke, pollen, sea salt, dust, airborne microorganisms, and other natural or man-made sources.

A

Aerosols

127
Q

It is a form of oxygen with three oxygen atoms in each molecule (O3).

A

Ozone

128
Q

Parts of the Atmosphere

A

Troposphere
Stratosphere
Mesosphere
Thermosphere

129
Q

This is the lowest layer of the atmosphere. In this layer, temperature decreases with increasing altitude. The - is the most crucial layer for meteorologists because all weather phenomena occur here.

A

Troposphere

130
Q

The temperature in this region increases with altitude because the ozone layer is located here.

A

Stratosphere

131
Q

protects us from meteors by burning up most meteors and asteroids before they reach the Earth’s surface.

A

Mesosphere

132
Q

Temperatures start to rise again in this layer due to oxygen and nitrogen atoms’ constant absorption of high-energy radiation from the Sun. It is in this layer where satellites orbit around the Earth.

A

Thermosphere

133
Q

refers to the conditions of the atmosphere in a region over a short period of time.

A

Weather

134
Q

is the long-term behavior of the atmosphere over a region.

A

climate

135
Q

These are thin, wispy, and white clouds that resemble hair.

A

Cirrus clouds

136
Q

These are thin layers of clouds that cover extensive portions of the sky.

A

Stratus clouds

137
Q
A
138
Q
A
139
Q
A
140
Q
A

GR 11 (18 decks)

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