Agrotermos

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Formación de tsunamis

Tsunamis are most frequently caused by earthquakes, but can also result from landslides, volcanic eruptions, and very infrequently by meteorites or other impacts upon the ocean surface. Tsunamis are generated primarily by tectonic dislocations under the sea which are caused by shallow focus earthquakes along areas of subduction. The upthrusted and downthrusted crustal blocks impart potential energy into the overlying water mass with drastic changes in the sea level over the affected region. The energy imparted into the water mass results in tsunami generation, i.e. energy radiating away from the source region in the form of long period waves.

Generación de olas

francés

Creado

2023-04-12T16:30:06

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

skos:notation

4aa648ac

génération de tsunami

inglés

Creado

2019-09-04T12:02:37

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

skos:notation

4aa648ac

tsunami generation

portugués (Brasil)

Creado

2025-05-27T14:58:42Z

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

skos:notation

4aa648ac

geração de tsunami

URI

http://aims.fao.org/aos/agrovoc/c_4aa648ac

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Creado 9/4/19, 12:02, última modificación 5/27/25, 14:58