experimental
Entry: caldera collapse induced tsunami
URI: https://registry.epos-eu.org/ncl/FAIR-Incubator/tcs-TSU/91
A caldera collapse is a typical effect of large volcanic explosions. If the eruption, and hence the caldera collapse, occur underwater, a tsunami can be generated because of the subsidence of the overlying water mass. Hence, the tsunami propagation starts with a leading trough. The amplitude of the tsunami initial condition is a function of the geometry and of the duration of the collapse.
Core metadata
| is a | Concept |
| submitted by | Tendry R |
| accepted on | 11 Mar 2022 00:16:15.024 | 11 Mar 2022 00:13:52.330 |
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| date accepted |
11 Mar 2022 00:16:15.024
| 11 Mar 2022 00:13:52.330
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| date submitted |
11 Mar 2022 00:08:28.186
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| definition |
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| description |
A caldera collapse is a typical effect of large volcanic explosions. If the eruption, and hence the caldera collapse, occur underwater, a tsunami can be generated because of the subsidence of the overlying water mass. Hence, the tsunami propagation starts with a leading trough. The amplitude of the tsunami initial condition is a function of the geometry and of the duration of the collapse.
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| item class |
Concept
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| label |
caldera collapse induced tsunami
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| notation |
91
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| register |
tcs tSU
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| status |
status experimental
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| submitter |
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| type |
register item
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| version info |
3
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Definition
| description |
A caldera collapse is a typical effect of large volcanic explosions. If the eruption, and hence the caldera collapse, occur underwater, a tsunami can be generated because of the subsidence of the overlying water mass. Hence, the tsunami propagation starts with a leading trough. The amplitude of the tsunami initial condition is a function of the geometry and of the duration of the collapse.
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| label |
caldera collapse induced tsunami
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| notation |
91
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| type |
Concept
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