Quiz 1 Flashcards

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1
Q

The term “tectonic” (from the Latin
word tectonicus or Greek
word tektonikos Means?

A

To Build

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2
Q

Crust and the upper part of the mantle

A

Lithosphere

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3
Q

• a ductile layer under the solid lithosphere.

• composed of rocks that are partly molten due to high temperature and pressure under the lithosphere.

A

Asthenosphere

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4
Q

A geologist and Navy submarine commander during WW2, part of his mission is to study the deepest part of the ocean floor

A

Harry hest

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5
Q

Thinnest and outermost layer of the earth

A

Crust

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6
Q

Types of crust

A

Continental and Oceanic

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7
Q

A German polar researcher, geophysicist, and meteorologist
Also known as the father of plate tectonics theory

A

Alfred Wegner

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8
Q

• The strength of earthquakes can range from shallow to destructive.

• These earthquakes can be due to collisions, rifting, or slipping between or among the plates.

• Around 90% of eathquakes are felt along the plate margins.

• Earthquakes felt in areas within the plate are mostly due to stress buildup in some continental rifting zones or due to the transfer of energy from other regions.

A

Earthquake distribution

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9
Q

• In determining the epicenter of an earthquake, the difference in arrival time between the primary waves and the secondary waves which comes from a seismograph wave in seismic recording stations.

• Triangulation method is used to find the epicenter.

A

Seismic waves

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10
Q

Types of plate boundaries

A

Convergent: Plates move towards each other.

Divergent: Plates move away from each other.

Transform: Plates slide past each other.

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11
Q

places where tectonic plates collide or come together. When two plates meet, their interactions can result in various geological phenomena.

Convergent boundaries contribute to the formation of mountains, volcanic activity, and earthquakes.

A

Convergent Boundaries

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12
Q

plates move away from each other. This movement results in the creation of new crust as magma rises from the mantle, solidifies, and forms new oceanic crust.

This boundaries are responsible for the continuous reshaping and formation of Earth’s crust.

A

Divergent Boundaries

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13
Q

occurs when two plates slide past each other horizontally. The movement along these boundaries can cause earthquakes, as the plates grind against each other.

This boundaries redistribute stress and accommodate the movement between neighboring plates.

A

Transform Boundaries

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14
Q

• Distribution of volcanoes is mostly found along the plate margins, which can be in an either destructive or constructive boundary.

• Volcanoes are also found in areas where there is subduction of plates.

A

Volcanic Distribution

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15
Q

• Mountains have been formed due to the movement of plates, either apart or toward each other.

• Some are formed underwater or on the seabed, whereas others are formed on top of the continental crust.

A

Mountain Ranges

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16
Q

The solid and fluid layers of Earth, which are the lithosphere and the asthenosphere, respectively.

• Convection current is the driving mechanism of plate movement.

• Due to te differences in the densities of the two crustal features of the lithosphere, when the internal driving force from Earth causes the surface to move, it results in different geologic phenomena such as earthquake and volcanic activities.

A

Plate tectonic theory

17
Q

• also known as plate boundaries have three types: convergent, divergent, and transform.

A

Plate margins

18
Q

•collision between oceanic and continental crust.

•oceanic crust sinks down the continental rust and goes back to the mantle called subduction.

• Trenches are also formed by the intersection of the oceanic and continental crust.

A

Oceanic Continental convergence

19
Q

• collision between two oceanic plates.

• It causes one plate to subduct from the other.

• both oceanic crust have the same density, the one that subducts is the older plate.

A

Oceanic oceanic Convergence

20
Q

•Two continental crust move toward one another.

•Formation of mountains

• Crustal plates meet up occurs, one crust descends to the other continental crust but not toward the mantle.

A

Continental continental Convergence

21
Q

the origin at which earthquake occurs.

A

Hypocenter/focus

22
Q

the point directly above the focus on the surface.

A

Epicenter

23
Q

Bodywave and surface wave

A

Seismic waves

24
Q

Are in the form of primary and secondary waves.

A

Body waves

25
Q

travel through the interior of Earth and through solid and fluid materials. They travel faster than secondary waves.

their velocities varies depending on the location and material in which they move.

their motion is longitudinal, which vibrates along with the direction Particle Motion of its motion.

A

Primary wave/ p waves

26
Q

travel through solid materials only within the interior of the Earth.

velocity is less than that of P-waves.

Their vibrations are perpendicular to the direction of the motion of the waves.

A

Secondary wave/ s wave

27
Q

• occurs on the surface of the lithosphere.

• can be a love wave or Rayleigh wave.

A

Surface wave

28
Q

sweep the surface in a side-to-side movement.

transverse wave

A

Love wave

29
Q

shakes the ground in an up- and-down movement.

A

Rayleigh wave

30
Q

an instrument that detects and measure seismic waves.

A

Seismo graph

31
Q

• internal part of seismograph.

• works as a pendulum that swings back and forth which is attached to a barrel that rotates and makes prints of the ground shaking.

A

Seismic meter

32
Q

• is the most common scale for the magnitude of an earthquake.

• also called local magnitude.

logarithmic scale of the wave amplitude of an earthquake.

A

Richter scale