Science Lesson 2: Collide, Move Apart, and Slide and Triangulation Method Flashcards

1
Q

He proposed the continental drift theory.

A

Alfred Wegener

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2
Q

It is also known as plate margins

A

Plate Boundaries

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3
Q

Used to determine the epicenter by where it intersects

A

Triangulation Method

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4
Q

Two continental crustal plates move toward one another

A

Continental-Continental

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5
Q

Move apart from each other, outwards, tensional force

A

Divergent Plate Boundaries

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6
Q

Uses seismic data collected from at least 3 different locations

A

Triangulation Method

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7
Q

Causes one plate to subduct from the other

A

Oceanic-Oceanic

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8
Q

Slide past horizontally, lateral, shearing force

A

Transform Plate Boundaries

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9
Q

The point on the Earth’s surface vertically above the focus of an earthquake

A

Epicenter

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10
Q

Produces new seafloor

A

Divergent Plate Boundaries

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11
Q

Print out/display screen

A

Seismogram

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12
Q

Relating to an earthquake vibration

A

Seismic

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13
Q

Process at which oceanic crust sinks down the continental crust and goes back to the mantle

A

Subduction

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14
Q

It is a line where large moving plates meet

A

Plate Boundaries

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15
Q

Deep, narrow depression on the ocean seafloor caused by the collision and/or subduction of plates

A

Trench

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16
Q

A depression or lowland region along the separation of plates

A

Rift valley

17
Q

Move towards each other, inwards, compressing force

A

Convergent Plate Boundaries

18
Q

Father of the plate tectonics theory

A

Alfred Wegener

19
Q

The denser oceanic crust move beneath the lighter continental crust

A

Oceanic-Continental

20
Q

Device that detects/measures seismic activity

A

Seismograph

21
Q

3 types of Plate Boundaries:

A

Divergent, Convergent and Transform Boundaries

22
Q

Time interval between the arrival of P-wave and S-wave

A

Lag Time

23
Q

Steps in Locating the Epicenter Using Triangulation Method

A
  1. Obtain data from 3 seismic stations
  2. Subtract arrival time of P and S wave.
  3. Compute for the distance of the epicenter from each seismic station.
    (Time difference x 100/8)
  4. Draw a circle around each seismic station using the distance as its radius.
  5. The intersection part of the 3 circles is the earthquake’s epicenter.