Javascript must be enabled to use all features of this site and to avoid misfunctions
1968 Dasht-e Bayaz and Ferdows earthquake vs. 2006...
HOME
Select category:
Disasters
Select category
NEW

Advertising

Cancel

Search in
Close

1968 Dasht-e Bayaz and Ferdows earthquake vs 2006 Yogyakarta earthquake

1968 Dasht-e Bayaz and Ferdows earthquake
2006 Yogyakarta earthquake
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
Change

2006 Yogyakarta earthquake

Total costsN/A
Deaths 5782

Informations

The 2006 Yogyakarta earthquake (also known as the Bantul earthquake) occurred at 05:54 local time on 27 May with a moment magnitude of 6.4 and a maximum MSK intensity of VIII (Damaging). Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3.1 billion). With limited effects to public infrastructure and lifelines, housing and private businesses bore the majority of damage (the 9th-century Prambanan Hindu temple compound was also affected), and the United States' National Geophysical Data Center classified the total damage from the event as extreme. Although Indonesia experiences very large, great, and giant thrust earthquakes offshore at the Sunda Trench, this was a large strike-slip event that occurred on the southern coast of Java near the city of Yogyakarta. Mount Merapi lies nearby, and during its many previous historical eruptions, large volume lahars and volcanic debris flowed down its slopes where settlements were later built. This unconsolidated material from the stratovolcano amplified the intensity of the shaking and created the conditions for soil liquefaction to occur. Inadequate construction techniques and poor quality materials contributed to major failures with unreinforced masonry buildings (then the most prevalent type of home construction), though other styles fared better.

Source: Wikipedia

More intresting stuff