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About this activity

Introducción n a las placas Tectónicas.

Created by

Idona Anayte Arenales Fuentes
Idona Anayte Arenales Fuentes
Guatemala

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Introducción n a las placas Tectónicas.

by Idona Anayte Arenales Fuentes
1

La zona sísmica circumpacífica se limita a América y Asia.

2

El hipocentro es el lugar donde se origina el movimiento sísmico.

3

Las vibraciones sísmicas sólo ocurren por actividad volcánica.

4

La cordillera de los Andes no tiene relación con movimientos sísmicos.

5

Los movimientos sísmicos son vibraciones de la corteza terrestre.

6

La escala utilizada para medir la intensidad es la Mercalli modificada.

7

Las placas Nazca y Sudamericana se desplazan en la misma dirección.

8

La actividad volcánica y el diastrofismo son causas principales de movimientos sísmicos.

9

El maremoto es causado cuando el epicentro está en tierra firme.

10

La cordillera de los Andes se formó por la interacción de la Placa Sudamericana y la Nazca.

11

El maremoto se produce cuando el epicentro está en el fondo del mar.

12

La escala de Mercalli mide temperatura.

13

Los sismógrafos se basan en el principio de la inercia para medir movimientos sísmicos.

14

El epicentro se halla sobre la superficie terrestre, en la vertical del hipocentro.

15

La Tierra se mueve.

16

El epicentro se encuentra en el fondo del mar.

17

Las dos zonas sísmicas más activas son la Circumpacífica y la Mediterránea.

 
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