Javascript must be enabled to use all features of this site and to avoid misfunctions
1973 Eldfell vs. 1968 Dasht-e Bayaz and Ferdows...
HOME
Select category:
Disasters
Select category
NEW

Advertising

Cancel

Search in
Close

1973 Eldfell vs 1968 Dasht-e Bayaz and Ferdows earthquake

1973 Eldfell
1968 Dasht-e Bayaz and Ferdows earthquake
Change

1973 Eldfell

Total costsN/A
Deaths 1

Informations

Eldfell is a volcanic cone just over 200 metres (660 ft) high on the Icelandic island of Heimaey. It formed in a volcanic eruption, which began without warning on the eastern side of Heimaey, in the Westman Islands, on 23 January 1973. The name means Hill of Fire in Icelandic. The eruption caused a major crisis for the island and led to its temporary evacuation. Volcanic ash fell over most of the island, destroying around 400 homes, and a lava flow threatened to close off the harbour, the island's main income source via its fishing fleet. An operation was mounted to cool the advancing lava flow by pumping sea water onto it, which was successful in preventing the loss of the harbour. After the eruption, the islanders used heat from the cooling lava flows to provide hot water and to generate electricity. They also used some of the extensive tephra, fall-out of airborne volcanic material to extend the runway at the island's small airport and as landfill on which 200 new houses were built.

Source: Wikipedia
Change

1968 Dasht-e Bayaz and Ferdows earthquake

Total costsN/A
Deaths 15000

Informations

The Dasht-e Bayaz and Ferdows earthquakes occurred in Dashte Bayaz, Kakhk and Ferdows, Iran in late August and early September 1968. The mainshock measured 7.4 on the moment magnitude scale and had a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. Damage was heavy in the affected areas with thousands of lives lost in the first event and many hundreds more in the second strong event.

Source: Wikipedia

More intresting stuff